Version history for s3YUHSmlaj9jhR0xQIVO - Sahiyacave.Sinha.2015

Version: 1.0.21

• lastVersion: 1.0.20
• curator: nicholas
• timestamp: 2025-06-25 22:46:36.089469 UTC
• changes:
  • Paleo Column metadata:
    • d18O (S2LRuTFfyRE5aJ): paleoData_proxyGeneral: ‘((( null ))) isotope /// isotopic’ has been replaced by ‘isotopic’
    • d18O (S2LRuTFfyRE5aJ): paleoData_QCCertification: ‘((( null ))) CH /// CH, CR’ has been replaced by ‘CH, CR’
    • d18O (S2LRuTFfyRE5aJ): paleoData_QCnotes: ‘((( null ))) Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)” /// Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave Speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)”’ has been replaced by ‘Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave Speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)”’
  • Paleo Interpretation metadata:
    • d18O (S2LRuTFfyRE5aJ): interpretation1_seasonality: ‘((( null ))) 6,7,8,9 /// Jun-Sep’ has been replaced by ‘Jun-Sep’
    • d18O (S2LRuTFfyRE5aJ): interpretation1_variable: ‘((( null ))) M /// precipitation’ has been replaced by ‘precipitation’

Version: 1.0.20

• lastVersion: 1.0.19
• curator: nicholas
• timestamp: 2025-06-25 21:22:18.147714 UTC
• changes:
  • Paleo Column metadata:
    • d18O (S2LRN9QNRwRWs5): paleoData_primaryTimeseries: NULL has been replaced by ‘FALSE’
    • d18O (S2LRQbTNgLuktR): paleoData_primaryTimeseries: NULL has been replaced by ‘FALSE’
    • d18O (S2LRfpFO2d41TG): paleoData_primaryTimeseries: NULL has been replaced by ‘FALSE’
    • d18O (S2LRnUy5e71v36): paleoData_primaryTimeseries: NULL has been replaced by ‘FALSE’
    • d18O (S2LRuTFfyRE5aJ): paleoData_notes: ‘Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’ has been replaced by ‘((( null ))) “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’
    • d18O (S2LRuTFfyRE5aJ): paleoData_proxyGeneral: ‘isotopic’ has been replaced by ‘((( null ))) isotope /// isotopic’
    • d18O (S2LRuTFfyRE5aJ): paleoData_QCCertification: ‘CH, CR’ has been replaced by ‘((( null ))) CH /// CH, CR’
    • d18O (S2LRuTFfyRE5aJ): paleoData_QCnotes: ‘Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave Speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)”’ has been replaced by ‘((( null ))) Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)” /// Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave Speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)”’
    • d18O (S2LRuTFfyRE5aJ): paleoData_meetsHoloceneHydroclimateCriteria: NULL has been replaced by ‘TRUE’
    • d18O (S2LRuTFfyRE5aJ): paleoData_primaryTimeseries: NULL has been replaced by ‘TRUE’
  • Paleo Interpretation metadata:
    • d18O (S2LRuTFfyRE5aJ): interpretation1_seasonality: ‘Jun-Sep’ has been replaced by ‘((( null ))) 6,7,8,9 /// Jun-Sep’
    • d18O (S2LRuTFfyRE5aJ): interpretation1_variable: ‘precipitation’ has been replaced by ‘((( null ))) M /// precipitation’

Version: 1.0.19

• lastVersion: 1.0.18
• curator: nicholas
• timestamp: 2024-09-05 21:24:38.561608 UTC
• changes:
  • Paleo Interpretation metadata:
    • uncertainty (S2LR00P8WyCkwM): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LR00P8WyCkwM): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LR00P8WyCkwM): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LR00P8WyCkwM): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LR00P8WyCkwM): interpretation6_scope: NULL has been replaced by ‘isotope’
    • d13C (S2LR1lRBQAC1iP): interpretation2_scope: NULL has been replaced by ‘climate’
    • d13C (S2LR1lRBQAC1iP): interpretation3_scope: NULL has been replaced by ‘climate’
    • d13C (S2LR1lRBQAC1iP): interpretation4_scope: NULL has been replaced by ‘isotope’
    • d13C (S2LR1lRBQAC1iP): interpretation5_scope: NULL has been replaced by ‘isotope’
    • d13C (S2LR1lRBQAC1iP): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LR35k1OhLhym): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LR35k1OhLhym): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LR35k1OhLhym): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LR35k1OhLhym): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LR35k1OhLhym): interpretation6_scope: NULL has been replaced by ‘isotope’
    • correction (S2LR3WTgF1AmF4): interpretation2_scope: NULL has been replaced by ‘climate’
    • correction (S2LR3WTgF1AmF4): interpretation3_scope: NULL has been replaced by ‘climate’
    • correction (S2LR3WTgF1AmF4): interpretation4_scope: NULL has been replaced by ‘isotope’
    • correction (S2LR3WTgF1AmF4): interpretation5_scope: NULL has been replaced by ‘isotope’
    • correction (S2LR3WTgF1AmF4): interpretation6_scope: NULL has been replaced by ‘isotope’
    • correction (S2LR466NTabeAK): interpretation2_scope: NULL has been replaced by ‘climate’
    • correction (S2LR466NTabeAK): interpretation3_scope: NULL has been replaced by ‘climate’
    • correction (S2LR466NTabeAK): interpretation4_scope: NULL has been replaced by ‘isotope’
    • correction (S2LR466NTabeAK): interpretation5_scope: NULL has been replaced by ‘isotope’
    • correction (S2LR466NTabeAK): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LR6GAbI2miyd): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LR6GAbI2miyd): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LR6GAbI2miyd): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LR6GAbI2miyd): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LR6GAbI2miyd): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LR7CK7GOQgmW): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LR7CK7GOQgmW): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LR7CK7GOQgmW): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LR7CK7GOQgmW): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LR7CK7GOQgmW): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR7gBtle7tWG): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR7gBtle7tWG): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR7gBtle7tWG): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR7gBtle7tWG): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR7gBtle7tWG): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR8JjapzA6Wn): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR8JjapzA6Wn): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR8JjapzA6Wn): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR8JjapzA6Wn): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR8JjapzA6Wn): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR8KG6tw8fMr): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR8KG6tw8fMr): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR8KG6tw8fMr): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR8KG6tw8fMr): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LR8KG6tw8fMr): interpretation6_scope: NULL has been replaced by ‘isotope’
    • sampleID (S2LR9DiFPcHfrK): interpretation2_scope: NULL has been replaced by ‘climate’
    • sampleID (S2LR9DiFPcHfrK): interpretation3_scope: NULL has been replaced by ‘climate’
    • sampleID (S2LR9DiFPcHfrK): interpretation4_scope: NULL has been replaced by ‘isotope’
    • sampleID (S2LR9DiFPcHfrK): interpretation5_scope: NULL has been replaced by ‘isotope’
    • sampleID (S2LR9DiFPcHfrK): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRAwdS0E7DsV): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRAwdS0E7DsV): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRAwdS0E7DsV): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRAwdS0E7DsV): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRAwdS0E7DsV): interpretation6_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRBWKbvo13wO): interpretation2_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRBWKbvo13wO): interpretation3_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRBWKbvo13wO): interpretation4_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRBWKbvo13wO): interpretation5_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRBWKbvo13wO): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRBczajsHLOo): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRBczajsHLOo): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRBczajsHLOo): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRBczajsHLOo): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRBczajsHLOo): interpretation6_scope: NULL has been replaced by ‘isotope’
    • d13C (S2LRD7jzKFswB4): interpretation2_scope: NULL has been replaced by ‘climate’
    • d13C (S2LRD7jzKFswB4): interpretation3_scope: NULL has been replaced by ‘climate’
    • d13C (S2LRD7jzKFswB4): interpretation4_scope: NULL has been replaced by ‘isotope’
    • d13C (S2LRD7jzKFswB4): interpretation5_scope: NULL has been replaced by ‘isotope’
    • d13C (S2LRD7jzKFswB4): interpretation6_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRDPDHUoVgF0): interpretation2_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRDPDHUoVgF0): interpretation3_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRDPDHUoVgF0): interpretation4_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRDPDHUoVgF0): interpretation5_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRDPDHUoVgF0): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRKxMHMj0F3j): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRKxMHMj0F3j): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRKxMHMj0F3j): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRKxMHMj0F3j): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRKxMHMj0F3j): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRMKcreLaiut): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRMKcreLaiut): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRMKcreLaiut): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRMKcreLaiut): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRMKcreLaiut): interpretation6_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRMY8dzNCCrN): interpretation2_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRMY8dzNCCrN): interpretation3_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRMY8dzNCCrN): interpretation4_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRMY8dzNCCrN): interpretation5_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRMY8dzNCCrN): interpretation6_scope: NULL has been replaced by ‘isotope’
    • d18O (S2LRN9QNRwRWs5): interpretation2_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRN9QNRwRWs5): interpretation3_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRN9QNRwRWs5): interpretation4_scope: NULL has been replaced by ‘isotope’
    • d18O (S2LRN9QNRwRWs5): interpretation5_scope: NULL has been replaced by ‘isotope’
    • d18O (S2LRN9QNRwRWs5): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRNhGe61LfDR): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRNhGe61LfDR): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRNhGe61LfDR): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRNhGe61LfDR): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRNhGe61LfDR): interpretation6_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRNvYx5JPQFG): interpretation2_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRNvYx5JPQFG): interpretation3_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRNvYx5JPQFG): interpretation4_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRNvYx5JPQFG): interpretation5_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRNvYx5JPQFG): interpretation6_scope: NULL has been replaced by ‘isotope’
    • correction (S2LROW4QpXx4mz): interpretation2_scope: NULL has been replaced by ‘climate’
    • correction (S2LROW4QpXx4mz): interpretation3_scope: NULL has been replaced by ‘climate’
    • correction (S2LROW4QpXx4mz): interpretation4_scope: NULL has been replaced by ‘isotope’
    • correction (S2LROW4QpXx4mz): interpretation5_scope: NULL has been replaced by ‘isotope’
    • correction (S2LROW4QpXx4mz): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRPIJkuVCoYO): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRPIJkuVCoYO): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRPIJkuVCoYO): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRPIJkuVCoYO): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRPIJkuVCoYO): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRQXoEf7EAVM): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRQXoEf7EAVM): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRQXoEf7EAVM): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRQXoEf7EAVM): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRQXoEf7EAVM): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRQb4xHkecvh): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRQb4xHkecvh): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRQb4xHkecvh): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRQb4xHkecvh): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRQb4xHkecvh): interpretation6_scope: NULL has been replaced by ‘isotope’
    • d18O (S2LRQbTNgLuktR): interpretation2_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRQbTNgLuktR): interpretation3_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRQbTNgLuktR): interpretation4_scope: NULL has been replaced by ‘isotope’
    • d18O (S2LRQbTNgLuktR): interpretation5_scope: NULL has been replaced by ‘isotope’
    • d18O (S2LRQbTNgLuktR): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRR2EQb9k57D): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRR2EQb9k57D): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRR2EQb9k57D): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRR2EQb9k57D): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRR2EQb9k57D): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRRXD2aexZU2): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRRXD2aexZU2): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRRXD2aexZU2): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRRXD2aexZU2): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRRXD2aexZU2): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRSB7ZxE9IML): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRSB7ZxE9IML): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRSB7ZxE9IML): interpretation4_scope: NULL has been replaced by ‘isotope’
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    • uncertainty (S2LRSB7ZxE9IML): interpretation6_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRUHeSivC0qX): interpretation2_scope: NULL has been replaced by ‘climate’
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    • mineralogy (S2LRUHeSivC0qX): interpretation4_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRUHeSivC0qX): interpretation5_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRUHeSivC0qX): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): interpretation2_scope: NULL has been replaced by ‘climate’
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    • uncertaintyHigh (S2LRW6aiuq0Tcm): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRWINW1yvhPJ): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRWINW1yvhPJ): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRWINW1yvhPJ): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRWINW1yvhPJ): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRWINW1yvhPJ): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRWQy2DCBq7K): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRWQy2DCBq7K): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRWQy2DCBq7K): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRWQy2DCBq7K): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRWQy2DCBq7K): interpretation6_scope: NULL has been replaced by ‘isotope’
    • sampleID (S2LRWZOJbBWsov): interpretation2_scope: NULL has been replaced by ‘climate’
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    • sampleID (S2LRWZOJbBWsov): interpretation5_scope: NULL has been replaced by ‘isotope’
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    • uncertainty (S2LRXGB9h040ln): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRXGB9h040ln): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRXGB9h040ln): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRXGB9h040ln): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRXGB9h040ln): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRasjk0RLvG0): interpretation2_scope: NULL has been replaced by ‘climate’
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    • uncertaintyLow (S2LRasjk0RLvG0): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRasjk0RLvG0): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRasjk0RLvG0): interpretation6_scope: NULL has been replaced by ‘isotope’
    • hasHiatus (S2LRazPRENt47p): interpretation2_scope: NULL has been replaced by ‘climate’
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    • uncertaintyLow (S2LRsKGeRBLY7n): interpretation5_scope: NULL has been replaced by ‘isotope’
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    • uncertaintyLow (S2LRseGiPl8pnl): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRseGiPl8pnl): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRseGiPl8pnl): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRseGiPl8pnl): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRseGiPl8pnl): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRskZ8ft3o6s): interpretation2_scope: NULL has been replaced by ‘climate’
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    • uncertainty (S2LRskZ8ft3o6s): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRskZ8ft3o6s): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRt1MY8cf558): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRt1MY8cf558): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRt1MY8cf558): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRt1MY8cf558): interpretation5_scope: NULL has been replaced by ‘isotope’
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    • d18O (S2LRuTFfyRE5aJ): interpretation2_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRuTFfyRE5aJ): interpretation3_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRuTFfyRE5aJ): interpretation4_scope: NULL has been replaced by ‘isotope’
    • d18O (S2LRuTFfyRE5aJ): interpretation5_scope: NULL has been replaced by ‘isotope’
    • d18O (S2LRuTFfyRE5aJ): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRunTss1oTO0): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRunTss1oTO0): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRunTss1oTO0): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRunTss1oTO0): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRunTss1oTO0): interpretation6_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRuyjtPZyRVf): interpretation2_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRuyjtPZyRVf): interpretation3_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRuyjtPZyRVf): interpretation4_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRuyjtPZyRVf): interpretation5_scope: NULL has been replaced by ‘isotope’
    • thickness (S2LRuyjtPZyRVf): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRuzTr63hMYH): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRuzTr63hMYH): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRuzTr63hMYH): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRuzTr63hMYH): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRuzTr63hMYH): interpretation6_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRx5ivuXi2wz): interpretation2_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRx5ivuXi2wz): interpretation3_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRx5ivuXi2wz): interpretation4_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRx5ivuXi2wz): interpretation5_scope: NULL has been replaced by ‘isotope’
    • mineralogy (S2LRx5ivuXi2wz): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRypY2qZ2jbC): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRypY2qZ2jbC): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertainty (S2LRypY2qZ2jbC): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertainty (S2LRypY2qZ2jbC): interpretation5_scope: NULL has been replaced by ‘isotope’
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    • uncertaintyLow (S2LRyuZBLiEjb3): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRyuZBLiEjb3): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRyuZBLiEjb3): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyLow (S2LRyuZBLiEjb3): interpretation6_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRzEI0J8XAaH): interpretation2_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRzEI0J8XAaH): interpretation3_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRzEI0J8XAaH): interpretation4_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRzEI0J8XAaH): interpretation5_scope: NULL has been replaced by ‘isotope’
    • uncertaintyHigh (S2LRzEI0J8XAaH): interpretation6_scope: NULL has been replaced by ‘isotope’

Version: 1.0.18

• lastVersion: 1.0.17
• curator: nicholas
• timestamp: 2023-08-10 23:14:34 UTC
• changes:
  • Base metadata:
    • originalDataUrl: ‘http://dx.doi.org/10.17864/1947.256’ has been replaced by ‘https://doi.org/10.17864/1947.256’
  • Publication metadata:
    • pub1_author: NULL has been replaced by ‘Ashish Sinha and Gayatri Kathayat and Hai Cheng and Sebastian F. M. Breitenbach and Max Berkelhammer and Manfred Mudelsee and Jayant Biswas and R. L. Edwards’
    • pub1_journal: NULL has been replaced by ‘Nature Communications’
    • pub1_title: NULL has been replaced by ‘Trends and oscillations in the Indian summer monsoon rainfall over the last two millennia’

Version: 1.0.17

• lastVersion: 1.0.16
• curator: nicholas
• timestamp: 2023-05-31 20:40:09 UTC
• changes:
  • Paleo Column metadata:
    • d18O (S2LRuTFfyRE5aJ): paleoData_notes: ‘((( ((( ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015); paleoData_variableName updated ))) ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’ has been replaced by ‘Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’

Version: 1.0.16

• lastVersion: 1.0.15
• curator: nicholas
• timestamp: 2023-05-30 15:50:23 UTC
• changes:
  • Paleo Column metadata:
    • d18O (S2LRuTFfyRE5aJ): paleoData_notes: ‘Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’ has been replaced by ‘((( ((( ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015); paleoData_variableName updated ))) ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’
    • d18O (S2LRuTFfyRE5aJ): paleoData_QCCertification: ‘CH’ has been replaced by ‘CH, CR’
  • Paleo Interpretation metadata:
    • d18O (S2LRuTFfyRE5aJ): interpretation1_seasonalityGeneral: ‘summerOnly’ has been replaced by ‘Summer’

Version: 1.0.15

• lastVersion: 1.0.14
• curator: nicholas
• timestamp: 2023-05-25 17:55:38 UTC
• notes: Updated lipdverse database entry with a changed file.
• changes:
  • Geographic metadata:
    • geo_elevation: NULL has been replaced by ‘1190’

Version: 1.0.14

• lastVersion: 1.0.13
• curator: nicholas
• timestamp: 2023-05-12 22:09:36 UTC
• changes:
  • Paleo Column metadata:
    • d18O (S2LRuTFfyRE5aJ): paleoData_notes: ‘((( ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015); paleoData_variableName updated ))) ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’ has been replaced by ‘Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’

Version: 1.0.13

• lastVersion: 1.0.12
• curator: nicholas
• timestamp: 2023-03-24 22:26:13 UTC
• changes:
  • Paleo Column metadata:
    • d18O (S2LRuTFfyRE5aJ): paleoData_proxyGeneral: ‘isotope’ has been replaced by ‘isotopic’

Version: 1.0.12

• lastVersion: 1.0.11
• curator: nicholas
• timestamp: 2023-02-13 23:55:53 UTC
• changes:
  • Paleo Column metadata:
    • d18O (S2LRuTFfyRE5aJ): paleoData_notes: ‘((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’ has been replaced by ‘((( ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015); paleoData_variableName updated ))) ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// ((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’

Version: 1.0.11

• lastVersion: 1.0.10
• curator: nicholas
• timestamp: 2023-02-10 14:34:38 UTC
• changes:
  • Paleo Interpretation metadata:
    • uncertaintyHigh (S2LR35k1OhLhym): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LR7CK7GOQgmW): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR7gBtle7tWG): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR8JjapzA6Wn): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LR8KG6tw8fMr): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRasjk0RLvG0): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRBczajsHLOo): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRg02DFgVGoS): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRgqiz0df8ON): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRhNZe5edMYI): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRhT8psaw66S): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRkQMgcUc7nI): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRnx7OytSfnz): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRpfzUICe9Ip): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRPIJkuVCoYO): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRQb4xHkecvh): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRQXoEf7EAVM): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRr1Nt6kwShM): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRRXD2aexZU2): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRseGiPl8pnl): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRsKGeRBLY7n): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRt1MY8cf558): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRunTss1oTO0): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRWINW1yvhPJ): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyLow (S2LRyuZBLiEjb3): interpretation1_scope: NULL has been replaced by ‘climate’
    • uncertaintyHigh (S2LRzEI0J8XAaH): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.10

• lastVersion: 1.0.9
• curator: nicholas
• timestamp: 2023-02-09 16:13:42 UTC
• notes: Updated lipdverse database entry with a changed file.
• changes:
  • Paleo Column metadata:
    • uncertainty (S2LR00P8WyCkwM): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LR00P8WyCkwM): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
    • uncertainty (S2LR00P8WyCkwM): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
    • uncertainty (S2LR00P8WyCkwM): paleoData_method: NULL has been replaced by ‘standard’
    • depth (S2LR1vbJz35M37): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
    • depth (S2LR1vbJz35M37): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
    • depth (S2LR1vbJz35M37): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • age (S2LR2uCFtCMaQ8): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LR2uCFtCMaQ8): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LR2uCFtCMaQ8): paleoData_variableName: ‘agelinInterp’ has been replaced by ‘age’
    • age (S2LR2uCFtCMaQ8): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LR2uCFtCMaQ8): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LR2uCFtCMaQ8): paleoData_method: NULL has been replaced by ‘linInterp’
    • uncertaintyHigh (S2LR35k1OhLhym): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LR35k1OhLhym): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LR35k1OhLhym): paleoData_variableName: ‘ageOxCalUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LR35k1OhLhym): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LR35k1OhLhym): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LR35k1OhLhym): paleoData_method: NULL has been replaced by ‘OxCal’
    • correction (S2LR3WTgF1AmF4): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
    • correction (S2LR3WTgF1AmF4): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
    • correction (S2LR3WTgF1AmF4): paleoData_method: NULL has been replaced by ‘aragonite correction’
    • correction (S2LR466NTabeAK): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
    • correction (S2LR466NTabeAK): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
    • correction (S2LR466NTabeAK): paleoData_method: NULL has been replaced by ‘aragonite correction’
    • age (S2LR4tKX8FLvZy): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LR4tKX8FLvZy): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LR4tKX8FLvZy): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LR4tKX8FLvZy): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • age (S2LR4wHnehjlDA): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LR4wHnehjlDA): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LR4wHnehjlDA): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LR4wHnehjlDA): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • uncertainty (S2LR6GAbI2miyd): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LR6GAbI2miyd): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
    • uncertainty (S2LR6GAbI2miyd): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
    • uncertainty (S2LR6GAbI2miyd): paleoData_method: NULL has been replaced by ‘standard’
    • uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_variableName: ‘agelinInterpUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_method: NULL has been replaced by ‘linInterp’
    • uncertaintyLow (S2LR7gBtle7tWG): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LR7gBtle7tWG): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LR7gBtle7tWG): paleoData_variableName: ‘agelinRegUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LR7gBtle7tWG): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LR7gBtle7tWG): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LR7gBtle7tWG): paleoData_method: NULL has been replaced by ‘linReg’
    • uncertaintyLow (S2LR8JjapzA6Wn): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LR8JjapzA6Wn): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LR8JjapzA6Wn): paleoData_variableName: ‘agelinInterpUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LR8JjapzA6Wn): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LR8JjapzA6Wn): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LR8JjapzA6Wn): paleoData_method: NULL has been replaced by ‘linInterp’
    • uncertaintyLow (S2LR8KG6tw8fMr): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LR8KG6tw8fMr): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LR8KG6tw8fMr): paleoData_variableName: ‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LR8KG6tw8fMr): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LR8KG6tw8fMr): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LR8KG6tw8fMr): paleoData_method: NULL has been replaced by ‘Bchron’
    • sampleID (S2LR9DiFPcHfrK): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
    • uncertaintyLow (S2LRasjk0RLvG0): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRasjk0RLvG0): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRasjk0RLvG0): paleoData_variableName: ‘ageStalAgeUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRasjk0RLvG0): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRasjk0RLvG0): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRasjk0RLvG0): paleoData_method: NULL has been replaced by ‘StalAge’
    • uncertainty (S2LRAwdS0E7DsV): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRAwdS0E7DsV): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRAwdS0E7DsV): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
    • uncertainty (S2LRAwdS0E7DsV): paleoData_method: NULL has been replaced by ‘standard’
    • uncertaintyLow (S2LRBczajsHLOo): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRBczajsHLOo): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRBczajsHLOo): paleoData_variableName: ‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRBczajsHLOo): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRBczajsHLOo): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRBczajsHLOo): paleoData_method: NULL has been replaced by ‘Bchron’
    • age (S2LRbWzEvw6Isf): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRbWzEvw6Isf): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRbWzEvw6Isf): paleoData_variableName: ‘ageBchron’ has been replaced by ‘age’
    • age (S2LRbWzEvw6Isf): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRbWzEvw6Isf): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRbWzEvw6Isf): paleoData_method: NULL has been replaced by ‘Bchron’
    • age (S2LRCCMGOpwCsE): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRCCMGOpwCsE): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRCCMGOpwCsE): paleoData_variableName: ‘ageStalAge’ has been replaced by ‘age’
    • age (S2LRCCMGOpwCsE): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRCCMGOpwCsE): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRCCMGOpwCsE): paleoData_method: NULL has been replaced by ‘StalAge’
    • uncertainty (S2LRcdUQcbYAU1): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRcdUQcbYAU1): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRcdUQcbYAU1): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
    • uncertainty (S2LRcdUQcbYAU1): paleoData_method: NULL has been replaced by ‘precision’
    • age (S2LRDf4TIbhsUn): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRDf4TIbhsUn): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRDf4TIbhsUn): paleoData_variableName: ‘ageOxCal’ has been replaced by ‘age’
    • age (S2LRDf4TIbhsUn): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRDf4TIbhsUn): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRDf4TIbhsUn): paleoData_method: NULL has been replaced by ‘OxCal’
    • uncertainty (S2LRdr8i3fPtiJ): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRdr8i3fPtiJ): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRdr8i3fPtiJ): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
    • uncertainty (S2LRdr8i3fPtiJ): paleoData_method: NULL has been replaced by ‘precision’
    • uncertaintyHigh (S2LRg02DFgVGoS): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRg02DFgVGoS): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRg02DFgVGoS): paleoData_variableName: ‘agelinRegUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRg02DFgVGoS): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRg02DFgVGoS): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRg02DFgVGoS): paleoData_method: NULL has been replaced by ‘linReg’
    • depth (S2LRG4UBBCUyVZ): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
    • depth (S2LRG4UBBCUyVZ): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
    • depth (S2LRG4UBBCUyVZ): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • age (S2LRG9c5gXlIEd): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRG9c5gXlIEd): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRG9c5gXlIEd): paleoData_variableName: ‘agelinReg’ has been replaced by ‘age’
    • age (S2LRG9c5gXlIEd): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRG9c5gXlIEd): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRG9c5gXlIEd): paleoData_method: NULL has been replaced by ‘linReg’
    • uncertaintyHigh (S2LRgqiz0df8ON): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRgqiz0df8ON): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRgqiz0df8ON): paleoData_variableName: ‘ageStalAgeUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRgqiz0df8ON): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRgqiz0df8ON): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRgqiz0df8ON): paleoData_method: NULL has been replaced by ‘StalAge’
    • uncertaintyHigh (S2LRhNZe5edMYI): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRhNZe5edMYI): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRhNZe5edMYI): paleoData_variableName: ‘ageOxCalUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRhNZe5edMYI): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRhNZe5edMYI): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRhNZe5edMYI): paleoData_method: NULL has been replaced by ‘OxCal’
    • uncertaintyLow (S2LRhT8psaw66S): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRhT8psaw66S): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRhT8psaw66S): paleoData_variableName: ‘ageOxCalUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRhT8psaw66S): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRhT8psaw66S): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRhT8psaw66S): paleoData_method: NULL has been replaced by ‘OxCal’
    • sampleID (S2LRhtNuD8v5RL): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
    • age (S2LRHWLvxbHdBM): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRHWLvxbHdBM): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRHWLvxbHdBM): paleoData_variableName: ‘ageOxCal’ has been replaced by ‘age’
    • age (S2LRHWLvxbHdBM): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRHWLvxbHdBM): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRHWLvxbHdBM): paleoData_method: NULL has been replaced by ‘OxCal’
    • correction (S2LRiptM0AYJDU): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
    • correction (S2LRiptM0AYJDU): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
    • correction (S2LRiptM0AYJDU): paleoData_method: NULL has been replaced by ‘aragonite correction’
    • sampleID (S2LRjbVnr4UHpk): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
    • uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_variableName: ‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_method: NULL has been replaced by ‘Bchron’
    • uncertainty (S2LRKxMHMj0F3j): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRKxMHMj0F3j): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRKxMHMj0F3j): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
    • uncertainty (S2LRKxMHMj0F3j): paleoData_method: NULL has been replaced by ‘precision’
    • depth (S2LRm7FhHMhwZO): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
    • depth (S2LRm7FhHMhwZO): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
    • depth (S2LRm7FhHMhwZO): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • uncertainty (S2LRMKcreLaiut): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRMKcreLaiut): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRMKcreLaiut): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
    • uncertainty (S2LRMKcreLaiut): paleoData_method: NULL has been replaced by ‘standard’
    • age (S2LRmWHUNyeMak): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRmWHUNyeMak): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRmWHUNyeMak): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRmWHUNyeMak): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • uncertainty (S2LRNhGe61LfDR): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRNhGe61LfDR): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRNhGe61LfDR): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
    • uncertainty (S2LRNhGe61LfDR): paleoData_method: NULL has been replaced by ‘precision’
    • age (S2LRNX5npBYgoA): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRNX5npBYgoA): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRNX5npBYgoA): paleoData_variableName: ‘ageStalAge’ has been replaced by ‘age’
    • age (S2LRNX5npBYgoA): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRNX5npBYgoA): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRNX5npBYgoA): paleoData_method: NULL has been replaced by ‘StalAge’
    • uncertaintyHigh (S2LRnx7OytSfnz): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRnx7OytSfnz): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRnx7OytSfnz): paleoData_variableName: ‘ageStalAgeUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRnx7OytSfnz): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRnx7OytSfnz): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRnx7OytSfnz): paleoData_method: NULL has been replaced by ‘StalAge’
    • correction (S2LROW4QpXx4mz): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
    • correction (S2LROW4QpXx4mz): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
    • correction (S2LROW4QpXx4mz): paleoData_method: NULL has been replaced by ‘aragonite correction’
    • age (S2LRpDsQMm9sy8): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRpDsQMm9sy8): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRpDsQMm9sy8): paleoData_variableName: ‘ageBchron’ has been replaced by ‘age’
    • age (S2LRpDsQMm9sy8): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRpDsQMm9sy8): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRpDsQMm9sy8): paleoData_method: NULL has been replaced by ‘Bchron’
    • uncertaintyLow (S2LRpfzUICe9Ip): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRpfzUICe9Ip): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRpfzUICe9Ip): paleoData_variableName: ‘ageBaconUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRpfzUICe9Ip): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRpfzUICe9Ip): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRpfzUICe9Ip): paleoData_method: NULL has been replaced by ‘Bacon’
    • uncertaintyLow (S2LRPIJkuVCoYO): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRPIJkuVCoYO): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRPIJkuVCoYO): paleoData_variableName: ‘agecopRaUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRPIJkuVCoYO): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRPIJkuVCoYO): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRPIJkuVCoYO): paleoData_method: NULL has been replaced by ‘copRa’
    • age (S2LRPtaotogqQx): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRPtaotogqQx): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRPtaotogqQx): paleoData_variableName: ‘ageOxCal’ has been replaced by ‘age’
    • age (S2LRPtaotogqQx): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRPtaotogqQx): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRPtaotogqQx): paleoData_method: NULL has been replaced by ‘OxCal’
    • uncertaintyLow (S2LRQb4xHkecvh): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRQb4xHkecvh): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRQb4xHkecvh): paleoData_variableName: ‘ageOxCalUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRQb4xHkecvh): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRQb4xHkecvh): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRQb4xHkecvh): paleoData_method: NULL has been replaced by ‘OxCal’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_variableName: ‘ageBaconUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_method: NULL has been replaced by ‘Bacon’
    • uncertaintyLow (S2LRQXoEf7EAVM): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRQXoEf7EAVM): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRQXoEf7EAVM): paleoData_variableName: ‘ageStalAgeUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRQXoEf7EAVM): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRQXoEf7EAVM): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRQXoEf7EAVM): paleoData_method: NULL has been replaced by ‘StalAge’
    • uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_variableName: ‘agecopRaUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_method: NULL has been replaced by ‘copRa’
    • uncertainty (S2LRR2EQb9k57D): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRR2EQb9k57D): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRR2EQb9k57D): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
    • uncertainty (S2LRR2EQb9k57D): paleoData_method: NULL has been replaced by ‘precision’
    • uncertainty (S2LRrEAjVuSXAF): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRrEAjVuSXAF): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRrEAjVuSXAF): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
    • uncertainty (S2LRrEAjVuSXAF): paleoData_method: NULL has been replaced by ‘standard’
    • uncertaintyHigh (S2LRRXD2aexZU2): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRRXD2aexZU2): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRRXD2aexZU2): paleoData_variableName: ‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRRXD2aexZU2): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRRXD2aexZU2): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRRXD2aexZU2): paleoData_method: NULL has been replaced by ‘Bchron’
    • uncertainty (S2LRSB7ZxE9IML): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRSB7ZxE9IML): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRSB7ZxE9IML): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
    • uncertainty (S2LRSB7ZxE9IML): paleoData_method: NULL has been replaced by ‘standard’
    • uncertaintyLow (S2LRseGiPl8pnl): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRseGiPl8pnl): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRseGiPl8pnl): paleoData_variableName: ‘agelinInterpUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRseGiPl8pnl): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRseGiPl8pnl): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRseGiPl8pnl): paleoData_method: NULL has been replaced by ‘linInterp’
    • uncertaintyLow (S2LRsKGeRBLY7n): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRsKGeRBLY7n): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRsKGeRBLY7n): paleoData_variableName: ‘ageOxCalUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRsKGeRBLY7n): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRsKGeRBLY7n): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRsKGeRBLY7n): paleoData_method: NULL has been replaced by ‘OxCal’
    • uncertainty (S2LRskZ8ft3o6s): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRskZ8ft3o6s): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRskZ8ft3o6s): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
    • uncertainty (S2LRskZ8ft3o6s): paleoData_method: NULL has been replaced by ‘standard’
    • uncertaintyLow (S2LRt1MY8cf558): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRt1MY8cf558): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRt1MY8cf558): paleoData_variableName: ‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRt1MY8cf558): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRt1MY8cf558): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRt1MY8cf558): paleoData_method: NULL has been replaced by ‘Bchron’
    • age (S2LRT3gY7xy6vJ): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRT3gY7xy6vJ): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRT3gY7xy6vJ): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRT3gY7xy6vJ): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • age (S2LRTXXZdQVmto): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRTXXZdQVmto): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRTXXZdQVmto): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRTXXZdQVmto): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • uncertaintyHigh (S2LRunTss1oTO0): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRunTss1oTO0): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRunTss1oTO0): paleoData_variableName: ‘ageOxCalUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRunTss1oTO0): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRunTss1oTO0): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRunTss1oTO0): paleoData_method: NULL has been replaced by ‘OxCal’
    • d18O (S2LRuTFfyRE5aJ): paleoData_variableName: ‘d18OComposite’ has been replaced by ‘d18O’
    • uncertainty (S2LRuzTr63hMYH): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRuzTr63hMYH): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRuzTr63hMYH): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
    • uncertainty (S2LRuzTr63hMYH): paleoData_method: NULL has been replaced by ‘precision’
    • age (S2LRvbOaBP57dL): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRvbOaBP57dL): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRvbOaBP57dL): paleoData_variableName: ‘agecopRa’ has been replaced by ‘age’
    • age (S2LRvbOaBP57dL): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRvbOaBP57dL): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRvbOaBP57dL): paleoData_method: NULL has been replaced by ‘copRa’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_variableName: ‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_method: NULL has been replaced by ‘Bchron’
    • age (S2LRWD9TJ9g9XB): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRWD9TJ9g9XB): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRWD9TJ9g9XB): paleoData_variableName: ‘ageBchron’ has been replaced by ‘age’
    • age (S2LRWD9TJ9g9XB): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRWD9TJ9g9XB): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRWD9TJ9g9XB): paleoData_method: NULL has been replaced by ‘Bchron’
    • age (S2LRWiBDQNruT7): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRWiBDQNruT7): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRWiBDQNruT7): paleoData_variableName: ‘ageBacon’ has been replaced by ‘age’
    • age (S2LRWiBDQNruT7): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRWiBDQNruT7): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRWiBDQNruT7): paleoData_method: NULL has been replaced by ‘Bacon’
    • uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_variableName: ‘agelinInterpUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_method: NULL has been replaced by ‘linInterp’
    • uncertainty (S2LRWQy2DCBq7K): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRWQy2DCBq7K): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRWQy2DCBq7K): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
    • uncertainty (S2LRWQy2DCBq7K): paleoData_method: NULL has been replaced by ‘precision’
    • age (S2LRwVB7UPRXvh): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRwVB7UPRXvh): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRwVB7UPRXvh): paleoData_variableName: ‘ageBacon’ has been replaced by ‘age’
    • age (S2LRwVB7UPRXvh): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRwVB7UPRXvh): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRwVB7UPRXvh): paleoData_method: NULL has been replaced by ‘Bacon’
    • sampleID (S2LRWZOJbBWsov): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
    • uncertainty (S2LRXGB9h040ln): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRXGB9h040ln): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRXGB9h040ln): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
    • uncertainty (S2LRXGB9h040ln): paleoData_method: NULL has been replaced by ‘precision’
    • uncertainty (S2LRypY2qZ2jbC): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
    • uncertainty (S2LRypY2qZ2jbC): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
    • uncertainty (S2LRypY2qZ2jbC): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
    • uncertainty (S2LRypY2qZ2jbC): paleoData_method: NULL has been replaced by ‘standard’
    • uncertaintyLow (S2LRyuZBLiEjb3): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyLow (S2LRyuZBLiEjb3): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyLow (S2LRyuZBLiEjb3): paleoData_variableName: ‘ageBaconUncertaintyLow’ has been replaced by ‘uncertaintyLow’
    • uncertaintyLow (S2LRyuZBLiEjb3): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyLow (S2LRyuZBLiEjb3): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyLow (S2LRyuZBLiEjb3): paleoData_method: NULL has been replaced by ‘Bacon’
    • age (S2LRzDvgX77JVO): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
    • age (S2LRzDvgX77JVO): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • age (S2LRzDvgX77JVO): paleoData_variableName: ‘agelinInterp’ has been replaced by ‘age’
    • age (S2LRzDvgX77JVO): paleoData_datum: NULL has been replaced by ‘1950’
    • age (S2LRzDvgX77JVO): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
    • age (S2LRzDvgX77JVO): paleoData_method: NULL has been replaced by ‘linInterp’
    • uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
    • uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
    • uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_variableName: ‘ageBaconUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
    • uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_datum: NULL has been replaced by ‘1950’
    • uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_inferredMaterial: NULL has been replaced by ‘age’
    • uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_method: NULL has been replaced by ‘Bacon’
  • Paleo Interpretation metadata:
    • d18O (S2LRuTFfyRE5aJ): interpretation1_seasonality: ‘6,7,8,9’ has been replaced by ‘Jun-Sep’
    • d18O (S2LRuTFfyRE5aJ): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’

Version: 1.0.9

• lastVersion: 1.0.8
• curator: nicholas
• timestamp: 2023-01-27 00:05:51 UTC
• changes:
  • Paleo Column metadata:
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_notes: ‘Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’ has been replaced by ‘((( “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) ))) Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015) /// Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’

Version: 1.0.8

• lastVersion: 1.0.7
• curator: nicholas
• timestamp: 2022-09-09 02:14:42 UTC
• changes:
  • Paleo Interpretation metadata:
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonality: ‘JJAS’ has been replaced by ‘6,7,8,9’

Version: 1.0.7

• lastVersion: 1.0.6
• curator: nicholas
• timestamp: 2022-07-28 17:40:46 UTC
• changes:
  • Geographic metadata:
    • geo_elevation: ‘1190’ has been replaced by NULL

Version: 1.0.6

• lastVersion: 1.0.5
• curator: nicholas
• timestamp: 2022-07-15 23:09:48 UTC
• changes:
  • Paleo Interpretation metadata:
    • d13CStandard (S2LR00P8WyCkwM): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13C (S2LR1lRBQAC1iP): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrection (S2LR3WTgF1AmF4): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrection (S2LR466NTabeAK): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CStandard (S2LR6GAbI2miyd): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleID (S2LR9DiFPcHfrK): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandard (S2LRAwdS0E7DsV): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasHiatus (S2LRazPRENt47p): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRBWKbvo13wO): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecision (S2LRcdUQcbYAU1): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13C (S2LRcqo665d9DJ): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13C (S2LRD7jzKFswB4): interpretation1_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRDPDHUoVgF0): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecision (S2LRdr8i3fPtiJ): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRfpFO2d41TG): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleID (S2LRhtNuD8v5RL): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrection (S2LRiptM0AYJDU): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleID (S2LRjbVnr4UHpk): interpretation1_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRk84w10shdf): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecision (S2LRKxMHMj0F3j): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandard (S2LRMKcreLaiut): interpretation1_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRMY8dzNCCrN): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRN9QNRwRWs5): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecision (S2LRNhGe61LfDR): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRnUy5e71v36): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRNvYx5JPQFG): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrection (S2LROW4QpXx4mz): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRQbTNgLuktR): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13C (S2LRqmHrDUYyy2): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecision (S2LRR2EQb9k57D): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandard (S2LRrEAjVuSXAF): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandard (S2LRSB7ZxE9IML): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CStandard (S2LRskZ8ft3o6s): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRUHeSivC0qX): interpretation1_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRuyjtPZyRVf): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecision (S2LRuzTr63hMYH): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecision (S2LRWQy2DCBq7K): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleID (S2LRWZOJbBWsov): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRx5ivuXi2wz): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecision (S2LRXGB9h040ln): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CStandard (S2LRypY2qZ2jbC): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.5

• lastVersion: 1.0.4
• curator: nicholas
• timestamp: 2022-05-18 00:29:32 UTC
• changes:
  • Paleo Interpretation metadata:
    • d13CStandard (S2LR00P8WyCkwM): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13C (S2LR1lRBQAC1iP): interpretation1_scope: ‘climate’ has been replaced by NULL
    • hasAragoniteCorrection (S2LR3WTgF1AmF4): interpretation1_scope: ‘climate’ has been replaced by NULL
    • hasAragoniteCorrection (S2LR466NTabeAK): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13CStandard (S2LR6GAbI2miyd): interpretation1_scope: ‘climate’ has been replaced by NULL
    • sisalSampleID (S2LR9DiFPcHfrK): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OStandard (S2LRAwdS0E7DsV): interpretation1_scope: ‘climate’ has been replaced by NULL
    • hasHiatus (S2LRazPRENt47p): interpretation1_scope: ‘climate’ has been replaced by NULL
    • mineralogy (S2LRBWKbvo13wO): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13CPrecision (S2LRcdUQcbYAU1): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13C (S2LRcqo665d9DJ): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13C (S2LRD7jzKFswB4): interpretation1_scope: ‘climate’ has been replaced by NULL
    • thickness (S2LRDPDHUoVgF0): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OPrecision (S2LRdr8i3fPtiJ): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18O (S2LRfpFO2d41TG): interpretation1_scope: ‘climate’ has been replaced by NULL
    • sisalSampleID (S2LRhtNuD8v5RL): interpretation1_scope: ‘climate’ has been replaced by NULL
    • hasAragoniteCorrection (S2LRiptM0AYJDU): interpretation1_scope: ‘climate’ has been replaced by NULL
    • sisalSampleID (S2LRjbVnr4UHpk): interpretation1_scope: ‘climate’ has been replaced by NULL
    • thickness (S2LRk84w10shdf): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OPrecision (S2LRKxMHMj0F3j): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OStandard (S2LRMKcreLaiut): interpretation1_scope: ‘climate’ has been replaced by NULL
    • thickness (S2LRMY8dzNCCrN): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18O (S2LRN9QNRwRWs5): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13CPrecision (S2LRNhGe61LfDR): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18O (S2LRnUy5e71v36): interpretation1_scope: ‘climate’ has been replaced by NULL
    • mineralogy (S2LRNvYx5JPQFG): interpretation1_scope: ‘climate’ has been replaced by NULL
    • hasAragoniteCorrection (S2LROW4QpXx4mz): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18O (S2LRQbTNgLuktR): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13C (S2LRqmHrDUYyy2): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OPrecision (S2LRR2EQb9k57D): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OStandard (S2LRrEAjVuSXAF): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OStandard (S2LRSB7ZxE9IML): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13CStandard (S2LRskZ8ft3o6s): interpretation1_scope: ‘climate’ has been replaced by NULL
    • mineralogy (S2LRUHeSivC0qX): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonality: ‘6,7,8,9’ has been replaced by ‘JJAS’
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonalityOriginal: NULL has been replaced by ‘6,7,8,9’
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_variableGroup: NULL has been replaced by ‘P’
    • thickness (S2LRuyjtPZyRVf): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13CPrecision (S2LRuzTr63hMYH): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d18OPrecision (S2LRWQy2DCBq7K): interpretation1_scope: ‘climate’ has been replaced by NULL
    • sisalSampleID (S2LRWZOJbBWsov): interpretation1_scope: ‘climate’ has been replaced by NULL
    • mineralogy (S2LRx5ivuXi2wz): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13CPrecision (S2LRXGB9h040ln): interpretation1_scope: ‘climate’ has been replaced by NULL
    • d13CStandard (S2LRypY2qZ2jbC): interpretation1_scope: ‘climate’ has been replaced by NULL
  • Paleo Column metadata:
    • agelinInterp (S2LR2uCFtCMaQ8): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinInterp (S2LR2uCFtCMaQ8): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCalUncertaintyHigh (S2LR35k1OhLhym): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCalUncertaintyHigh (S2LR35k1OhLhym): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • age (S2LR4tKX8FLvZy): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • age (S2LR4tKX8FLvZy): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • age (S2LR4wHnehjlDA): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • age (S2LR4wHnehjlDA): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agelinInterpUncertaintyHigh (S2LR7CK7GOQgmW): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinInterpUncertaintyHigh (S2LR7CK7GOQgmW): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agelinRegUncertaintyLow (S2LR7gBtle7tWG): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinRegUncertaintyLow (S2LR7gBtle7tWG): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agelinInterpUncertaintyLow (S2LR8JjapzA6Wn): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinInterpUncertaintyLow (S2LR8JjapzA6Wn): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchronUncertaintyLow (S2LR8KG6tw8fMr): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchronUncertaintyLow (S2LR8KG6tw8fMr): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageStalAgeUncertaintyLow (S2LRasjk0RLvG0): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageStalAgeUncertaintyLow (S2LRasjk0RLvG0): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchronUncertaintyLow (S2LRBczajsHLOo): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchronUncertaintyLow (S2LRBczajsHLOo): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchron (S2LRbWzEvw6Isf): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchron (S2LRbWzEvw6Isf): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageStalAge (S2LRCCMGOpwCsE): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageStalAge (S2LRCCMGOpwCsE): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCal (S2LRDf4TIbhsUn): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCal (S2LRDf4TIbhsUn): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agelinRegUncertaintyHigh (S2LRg02DFgVGoS): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinRegUncertaintyHigh (S2LRg02DFgVGoS): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agelinReg (S2LRG9c5gXlIEd): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinReg (S2LRG9c5gXlIEd): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageStalAgeUncertaintyHigh (S2LRgqiz0df8ON): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageStalAgeUncertaintyHigh (S2LRgqiz0df8ON): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCalUncertaintyHigh (S2LRhNZe5edMYI): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCalUncertaintyHigh (S2LRhNZe5edMYI): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCalUncertaintyLow (S2LRhT8psaw66S): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCalUncertaintyLow (S2LRhT8psaw66S): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCal (S2LRHWLvxbHdBM): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCal (S2LRHWLvxbHdBM): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchronUncertaintyHigh (S2LRkQMgcUc7nI): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchronUncertaintyHigh (S2LRkQMgcUc7nI): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • age (S2LRmWHUNyeMak): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • age (S2LRmWHUNyeMak): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageStalAge (S2LRNX5npBYgoA): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageStalAge (S2LRNX5npBYgoA): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageStalAgeUncertaintyHigh (S2LRnx7OytSfnz): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageStalAgeUncertaintyHigh (S2LRnx7OytSfnz): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchron (S2LRpDsQMm9sy8): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchron (S2LRpDsQMm9sy8): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBaconUncertaintyLow (S2LRpfzUICe9Ip): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBaconUncertaintyLow (S2LRpfzUICe9Ip): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agecopRaUncertaintyLow (S2LRPIJkuVCoYO): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agecopRaUncertaintyLow (S2LRPIJkuVCoYO): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCal (S2LRPtaotogqQx): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCal (S2LRPtaotogqQx): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCalUncertaintyLow (S2LRQb4xHkecvh): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCalUncertaintyLow (S2LRQb4xHkecvh): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBaconUncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBaconUncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageStalAgeUncertaintyLow (S2LRQXoEf7EAVM): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageStalAgeUncertaintyLow (S2LRQXoEf7EAVM): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agecopRaUncertaintyHigh (S2LRr1Nt6kwShM): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agecopRaUncertaintyHigh (S2LRr1Nt6kwShM): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchronUncertaintyHigh (S2LRRXD2aexZU2): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchronUncertaintyHigh (S2LRRXD2aexZU2): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agelinInterpUncertaintyLow (S2LRseGiPl8pnl): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinInterpUncertaintyLow (S2LRseGiPl8pnl): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCalUncertaintyLow (S2LRsKGeRBLY7n): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCalUncertaintyLow (S2LRsKGeRBLY7n): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchronUncertaintyLow (S2LRt1MY8cf558): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchronUncertaintyLow (S2LRt1MY8cf558): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • age (S2LRT3gY7xy6vJ): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • age (S2LRT3gY7xy6vJ): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • age (S2LRTXXZdQVmto): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • age (S2LRTXXZdQVmto): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageOxCalUncertaintyHigh (S2LRunTss1oTO0): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageOxCalUncertaintyHigh (S2LRunTss1oTO0): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d18O’
    • agecopRa (S2LRvbOaBP57dL): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agecopRa (S2LRvbOaBP57dL): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchronUncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchronUncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBchron (S2LRWD9TJ9g9XB): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBchron (S2LRWD9TJ9g9XB): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBacon (S2LRWiBDQNruT7): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBacon (S2LRWiBDQNruT7): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agelinInterpUncertaintyHigh (S2LRWINW1yvhPJ): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinInterpUncertaintyHigh (S2LRWINW1yvhPJ): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBacon (S2LRwVB7UPRXvh): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBacon (S2LRwVB7UPRXvh): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBaconUncertaintyLow (S2LRyuZBLiEjb3): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBaconUncertaintyLow (S2LRyuZBLiEjb3): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • agelinInterp (S2LRzDvgX77JVO): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • agelinInterp (S2LRzDvgX77JVO): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • ageBaconUncertaintyHigh (S2LRzEI0J8XAaH): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
    • ageBaconUncertaintyHigh (S2LRzEI0J8XAaH): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  • Chron Column metadata:
    • age_type (S2LcRayqsINzw1d): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
    • age_type (S2LcRayqsINzw1d): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’
    • age_type (S2LcRCHCNxuaZxi): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
    • age_type (S2LcRCHCNxuaZxi): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’
    • age_type (S2LcRFiH4gvFdWk): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
    • age_type (S2LcRFiH4gvFdWk): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’
    • age_type (S2LcRHSaBRMXHFF): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
    • age_type (S2LcRHSaBRMXHFF): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’
    • age_type (S2LcRXpNEfAsaB1): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
    • age_type (S2LcRXpNEfAsaB1): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’

Version: 1.0.4

• lastVersion: 1.0.3
• curator: nicholas
• timestamp: 2021-11-17 02:09:55 UTC
• changes:
  • Paleo Column metadata:
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_notes: ‘“the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’ has been replaced by ‘Amount effect: “the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’
  • Paleo Interpretation metadata:
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_variable: ‘M’ has been replaced by ‘P’

Version: 1.0.3

• lastVersion: 1.0.2
• curator: nicholas
• timestamp: 2021-10-05 21:42:36 UTC
• changes:
  • Geographic metadata:
    • geo_gcmdLocation: NULL has been replaced by ‘Asia>Southcentral Asia>India’

Version: 1.0.2

• lastVersion: 1.0.1
• curator: nick
• timestamp: 2021-03-17 01:57:14 UTC
• changes:
  • Base metadata:
    • archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
  • Paleo Column metadata:
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_notes: ‘“the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’ has been replaced by ‘“the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…Speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_QCnotes: ‘Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)”’ has been replaced by ‘Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave Speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)”’
  • Paleo Interpretation metadata:
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonalityGeneral: ‘Summer’ has been replaced by ‘summerOnly’

Version: 1.0.1

• lastVersion: 1.0.0
• curator: nick
• timestamp: 2021-01-12 02:29:36 UTC
• changes:
  • Paleo Interpretation metadata:
    • d13CStandard (S2LR00P8WyCkwM): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13C (S2LR1lRBQAC1iP): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrection (S2LR3WTgF1AmF4): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrection (S2LR466NTabeAK): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandardComposite (S2LR6791eWz5KM): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CStandard (S2LR6GAbI2miyd): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleID (S2LR9DiFPcHfrK): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandard (S2LRAwdS0E7DsV): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasHiatus (S2LRazPRENt47p): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRBWKbvo13wO): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CStandardComposite (S2LRCaXY3l2nYh): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecision (S2LRcdUQcbYAU1): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13C (S2LRcqo665d9DJ): interpretation1_scope: NULL has been replaced by ‘climate’
    • thicknessComposite (S2LRcvsbZIuf6n): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13C (S2LRD7jzKFswB4): interpretation1_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRDPDHUoVgF0): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecision (S2LRdr8i3fPtiJ): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRfpFO2d41TG): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleID (S2LRhtNuD8v5RL): interpretation1_scope: NULL has been replaced by ‘climate’
    • entityName (S2LRIi3L7bNHpM): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrection (S2LRiptM0AYJDU): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleID (S2LRjbVnr4UHpk): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogyComposite (S2LRjGtfkhKuaH): interpretation1_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRk84w10shdf): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecision (S2LRKxMHMj0F3j): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecisionComposite (S2LRLCnhzcT2KE): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandard (S2LRMKcreLaiut): interpretation1_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRMY8dzNCCrN): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRN9QNRwRWs5): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecision (S2LRNhGe61LfDR): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRnUy5e71v36): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRNvYx5JPQFG): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrection (S2LROW4QpXx4mz): interpretation1_scope: NULL has been replaced by ‘climate’
    • hasAragoniteCorrectionComposite (S2LRP7mL4fQN1r): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18O (S2LRQbTNgLuktR): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13C (S2LRqmHrDUYyy2): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecision (S2LRR2EQb9k57D): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandard (S2LRrEAjVuSXAF): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleIDComposite (S2LRRslnAna0Q6): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OStandard (S2LRSB7ZxE9IML): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CStandard (S2LRskZ8ft3o6s): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRUHeSivC0qX): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_direction: NULL has been replaced by ‘negative’
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonality: NULL has been replaced by ‘6,7,8,9’
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Summer’
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_variable: NULL has been replaced by ‘M’
    • d18OComposite (S2LRuTFfyRE5aJ): interpretation1_variableDetail: NULL has been replaced by ‘monsoon@surface’
    • d13CComposite (S2LRUVrcJsNzTD): interpretation1_scope: NULL has been replaced by ‘climate’
    • thickness (S2LRuyjtPZyRVf): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecision (S2LRuzTr63hMYH): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecision (S2LRWQy2DCBq7K): interpretation1_scope: NULL has been replaced by ‘climate’
    • sisalSampleID (S2LRWZOJbBWsov): interpretation1_scope: NULL has been replaced by ‘climate’
    • mineralogy (S2LRx5ivuXi2wz): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CPrecision (S2LRXGB9h040ln): interpretation1_scope: NULL has been replaced by ‘climate’
    • d18OPrecisionComposite (S2LRyK5qOd0NtE): interpretation1_scope: NULL has been replaced by ‘climate’
    • d13CStandard (S2LRypY2qZ2jbC): interpretation1_scope: NULL has been replaced by ‘climate’
  • Paleo Column metadata:
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_notes: NULL has been replaced by ‘“the oxygen isotope of precipi- tation (d18Op) in this region is strongly influenced by spatially integrated upstream changes in the ISM circulation dynamics and rainfall amounts…speleothem d18O profiles from this study (figs. S2 and S3) demonstrate that temporal changes in the Sahiya Cave d18O values reflect local changes in the d18Op at the cave area, which in turn vary inversely with the large-scale variation in ISM rainfall” (Kathayat et al., 2017); “This observa-tion suggests that upstream changes in ISM circulation and rainfall variability rather than changes in the local precipitation amount are the primary drivers of d18O variability at our site. Our observations are consistent with the results from other studies, which suggest that local d18Op variability in some monsoonal and tropical regions reflect upstream changes in regional circulation” (Sinha et al., 2015)’
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxy: NULL has been replaced by ‘d18O’
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxyDetail: NULL has been replaced by ‘calcite’
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_QCCertification: NULL has been replaced by ‘CH’
    • d18OComposite (S2LRuTFfyRE5aJ): paleoData_QCnotes: NULL has been replaced by ‘Author composite available: https://advances.sciencemag.org/content/suppl/2017/12/11/3.12.e1701296.DC1. “In the portions where the d18O profiles from different Sahiya Cave speleothems overlapped, the higher-resolution and better-dated profiles were retained for the composite record (fig. S2)”’

Version: 1.0.0

• curator: nick
• timestamp: 2020-09-29 14:24:54 UTC
• notes: Created from SISALv2