Refers to the unique identifier for the sample (as given in sample table)
Description of the mineralogy of the sample
Indication of whether the isotope measurements have been corrected in aragonite samples
NA; paleoData_method has been standardized
Laboratory precision on the d18O measurement
NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
Laboratory precision on the d13C measurement
Original published calibrated age of the sample in years BP
NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
NA; paleoData_isPrimary has been standardized
Calendar age in years BP, method = linInterp
NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
Positive age uncertaintyin years BP, method = linInterp
NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized
Negative age uncertaintyin years BP, method = linInterp
Calendar age in years BP, method = Bchron
Positive age uncertaintyin years BP, method = Bchron
Negative age uncertaintyin years BP, method = Bchron
Calendar age in years BP, method = Bacon
Positive age uncertaintyin years BP, method = Bacon
Negative age uncertaintyin years BP, method = Bacon
Calendar age in years BP, method = OxCal
Positive age uncertaintyin years BP, method = OxCal
Negative age uncertaintyin years BP, method = OxCal
Calendar age in years BP, method = copRa
Positive age uncertaintyin years BP, method = copRa
Negative age uncertaintyin years BP, method = copRa
Calendar age in years BP, method = StalAge
Positive age uncertaintyin years BP, method = StalAge
Negative age uncertaintyin years BP, method = StalAge
Calendar age in years BP, method = linReg
Positive age uncertaintyin years BP, method = linReg
Negative age uncertaintyin years BP, method = linReg
Original d18O measurement- All Stal composite, arranged by age, automatically by sisal2lipd. User beware.
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)
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)"
Original published calibrated age of the sample in years BP- All Stal composite, arranged by age, automatically by sisal2lipd. User beware.
The laboratory number of the dated sample
Uncorrected age of the dated sample in years
Positive uncertainty of the uncorrected age of the dated sample in years
Negative uncertainty of the uncorrected age of the dated sample in years
Indication of whether the date is used in the original age model (opposite of rejected)
238U 2-sigma uncertainty of dated sample in ppb
232Th content of the dated sample in ppt
232Th 2-sigma uncertainty of the dated sample in ppt
230Th/232Th activity ratio of the dated sample
230Th/232Th activity ratio 2-sigma uncertainty of the dated sample
230Th/238U activity ratio of the dated sample
230Th/238U activity ratio 2-sigma uncertainty of the dated sample
234U/238U activity ratio of the dated sample
234U/238U activity ratio 2-sigma uncertainty of the dated sample
Initial 230Th/232Th activity ratio for the detrital correction
Initial 230Th/232Th activity ratio uncertainty for the detrital correction
Description of the half-life used for 230Th and 234U for U/Th samples
Corrected age of the dated sample in years
Positive uncertainty of corrected age of the dated sample in years
Negative uncertainty of corrected age of the dated sample in years
originalDataUrl: 'http://dx.doi.org/10.17864/1947.256' has been replaced by 'https://doi.org/10.17864/1947.256'
pub1_author: '' 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: '' has been replaced by 'Nature Communications'
pub1_title: '' has been replaced by 'Trends and oscillations in the Indian summer monsoon rainfall over the last two millennia'
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)'
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'
d18O (S2LRuTFfyRE5aJ): interpretation1_seasonalityGeneral: 'summerOnly' has been replaced by 'Summer'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '1190'
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)'
d18O (S2LRuTFfyRE5aJ): paleoData_proxyGeneral: 'isotope' has been replaced by 'isotopic'
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)'
uncertaintyHigh (S2LR35k1OhLhym): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LR7CK7GOQgmW): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LR7gBtle7tWG): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LR8JjapzA6Wn): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LR8KG6tw8fMr): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRasjk0RLvG0): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRBczajsHLOo): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRg02DFgVGoS): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRgqiz0df8ON): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRhNZe5edMYI): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRhT8psaw66S): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRkQMgcUc7nI): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRnx7OytSfnz): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRpfzUICe9Ip): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRPIJkuVCoYO): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRQb4xHkecvh): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRQIKKz8Gpmp): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRQXoEf7EAVM): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRr1Nt6kwShM): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRRXD2aexZU2): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRseGiPl8pnl): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRsKGeRBLY7n): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRt1MY8cf558): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRunTss1oTO0): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRW6aiuq0Tcm): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRWINW1yvhPJ): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRyuZBLiEjb3): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRzEI0J8XAaH): interpretation1_scope: '' has been replaced by 'climate'
uncertainty (S2LR00P8WyCkwM): paleoData_notes: '' 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: '' has been replaced by 'd13C'
uncertainty (S2LR00P8WyCkwM): paleoData_method: '' has been replaced by 'standard'
depth (S2LR1vbJz35M37): paleoData_notes: '' 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: '' has been replaced by 'TRUE'
age (S2LR2uCFtCMaQ8): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LR2uCFtCMaQ8): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LR2uCFtCMaQ8): paleoData_method: '' has been replaced by 'linInterp'
uncertaintyHigh (S2LR35k1OhLhym): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LR35k1OhLhym): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LR35k1OhLhym): paleoData_method: '' has been replaced by 'OxCal'
correction (S2LR3WTgF1AmF4): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
correction (S2LR3WTgF1AmF4): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
correction (S2LR3WTgF1AmF4): paleoData_method: '' has been replaced by 'aragonite correction'
correction (S2LR466NTabeAK): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
correction (S2LR466NTabeAK): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
correction (S2LR466NTabeAK): paleoData_method: '' has been replaced by 'aragonite correction'
age (S2LR4tKX8FLvZy): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LR4tKX8FLvZy): paleoData_isPrimary: '' has been replaced by 'TRUE'
age (S2LR4wHnehjlDA): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LR4wHnehjlDA): paleoData_isPrimary: '' has been replaced by 'TRUE'
uncertainty (S2LR6GAbI2miyd): paleoData_notes: '' 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: '' has been replaced by 'd13C'
uncertainty (S2LR6GAbI2miyd): paleoData_method: '' has been replaced by 'standard'
uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LR7CK7GOQgmW): paleoData_method: '' has been replaced by 'linInterp'
uncertaintyLow (S2LR7gBtle7tWG): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LR7gBtle7tWG): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LR7gBtle7tWG): paleoData_method: '' has been replaced by 'linReg'
uncertaintyLow (S2LR8JjapzA6Wn): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LR8JjapzA6Wn): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LR8JjapzA6Wn): paleoData_method: '' has been replaced by 'linInterp'
uncertaintyLow (S2LR8KG6tw8fMr): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LR8KG6tw8fMr): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LR8KG6tw8fMr): paleoData_method: '' has been replaced by 'Bchron'
sampleID (S2LR9DiFPcHfrK): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
uncertaintyLow (S2LRasjk0RLvG0): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRasjk0RLvG0): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRasjk0RLvG0): paleoData_method: '' has been replaced by 'StalAge'
uncertainty (S2LRAwdS0E7DsV): paleoData_notes: '' 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: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRAwdS0E7DsV): paleoData_method: '' has been replaced by 'standard'
uncertaintyLow (S2LRBczajsHLOo): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRBczajsHLOo): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRBczajsHLOo): paleoData_method: '' has been replaced by 'Bchron'
age (S2LRbWzEvw6Isf): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRbWzEvw6Isf): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRbWzEvw6Isf): paleoData_method: '' has been replaced by 'Bchron'
age (S2LRCCMGOpwCsE): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRCCMGOpwCsE): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRCCMGOpwCsE): paleoData_method: '' has been replaced by 'StalAge'
uncertainty (S2LRcdUQcbYAU1): paleoData_notes: '' 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: '' has been replaced by 'd13C'
uncertainty (S2LRcdUQcbYAU1): paleoData_method: '' has been replaced by 'precision'
age (S2LRDf4TIbhsUn): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRDf4TIbhsUn): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRDf4TIbhsUn): paleoData_method: '' has been replaced by 'OxCal'
uncertainty (S2LRdr8i3fPtiJ): paleoData_notes: '' 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: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRdr8i3fPtiJ): paleoData_method: '' has been replaced by 'precision'
uncertaintyHigh (S2LRg02DFgVGoS): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRg02DFgVGoS): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRg02DFgVGoS): paleoData_method: '' has been replaced by 'linReg'
depth (S2LRG4UBBCUyVZ): paleoData_notes: '' 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: '' has been replaced by 'TRUE'
age (S2LRG9c5gXlIEd): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRG9c5gXlIEd): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRG9c5gXlIEd): paleoData_method: '' has been replaced by 'linReg'
uncertaintyHigh (S2LRgqiz0df8ON): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRgqiz0df8ON): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRgqiz0df8ON): paleoData_method: '' has been replaced by 'StalAge'
uncertaintyHigh (S2LRhNZe5edMYI): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRhNZe5edMYI): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRhNZe5edMYI): paleoData_method: '' has been replaced by 'OxCal'
uncertaintyLow (S2LRhT8psaw66S): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRhT8psaw66S): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRhT8psaw66S): paleoData_method: '' has been replaced by 'OxCal'
sampleID (S2LRhtNuD8v5RL): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
age (S2LRHWLvxbHdBM): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRHWLvxbHdBM): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRHWLvxbHdBM): paleoData_method: '' has been replaced by 'OxCal'
correction (S2LRiptM0AYJDU): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
correction (S2LRiptM0AYJDU): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
correction (S2LRiptM0AYJDU): paleoData_method: '' has been replaced by 'aragonite correction'
sampleID (S2LRjbVnr4UHpk): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRkQMgcUc7nI): paleoData_method: '' has been replaced by 'Bchron'
uncertainty (S2LRKxMHMj0F3j): paleoData_notes: '' 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: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRKxMHMj0F3j): paleoData_method: '' has been replaced by 'precision'
depth (S2LRm7FhHMhwZO): paleoData_notes: '' 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: '' has been replaced by 'TRUE'
uncertainty (S2LRMKcreLaiut): paleoData_notes: '' 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: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRMKcreLaiut): paleoData_method: '' has been replaced by 'standard'
age (S2LRmWHUNyeMak): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRmWHUNyeMak): paleoData_isPrimary: '' has been replaced by 'TRUE'
uncertainty (S2LRNhGe61LfDR): paleoData_notes: '' 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: '' has been replaced by 'd13C'
uncertainty (S2LRNhGe61LfDR): paleoData_method: '' has been replaced by 'precision'
age (S2LRNX5npBYgoA): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRNX5npBYgoA): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRNX5npBYgoA): paleoData_method: '' has been replaced by 'StalAge'
uncertaintyHigh (S2LRnx7OytSfnz): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRnx7OytSfnz): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRnx7OytSfnz): paleoData_method: '' has been replaced by 'StalAge'
correction (S2LROW4QpXx4mz): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
correction (S2LROW4QpXx4mz): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
correction (S2LROW4QpXx4mz): paleoData_method: '' has been replaced by 'aragonite correction'
age (S2LRpDsQMm9sy8): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRpDsQMm9sy8): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRpDsQMm9sy8): paleoData_method: '' has been replaced by 'Bchron'
uncertaintyLow (S2LRpfzUICe9Ip): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRpfzUICe9Ip): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRpfzUICe9Ip): paleoData_method: '' has been replaced by 'Bacon'
uncertaintyLow (S2LRPIJkuVCoYO): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRPIJkuVCoYO): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRPIJkuVCoYO): paleoData_method: '' has been replaced by 'copRa'
age (S2LRPtaotogqQx): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRPtaotogqQx): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRPtaotogqQx): paleoData_method: '' has been replaced by 'OxCal'
uncertaintyLow (S2LRQb4xHkecvh): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRQb4xHkecvh): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRQb4xHkecvh): paleoData_method: '' has been replaced by 'OxCal'
uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_method: '' has been replaced by 'Bacon'
uncertaintyLow (S2LRQXoEf7EAVM): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRQXoEf7EAVM): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRQXoEf7EAVM): paleoData_method: '' has been replaced by 'StalAge'
uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRr1Nt6kwShM): paleoData_method: '' has been replaced by 'copRa'
uncertainty (S2LRR2EQb9k57D): paleoData_notes: '' 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: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRR2EQb9k57D): paleoData_method: '' has been replaced by 'precision'
uncertainty (S2LRrEAjVuSXAF): paleoData_notes: '' 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: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRrEAjVuSXAF): paleoData_method: '' has been replaced by 'standard'
uncertaintyHigh (S2LRRXD2aexZU2): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRRXD2aexZU2): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRRXD2aexZU2): paleoData_method: '' has been replaced by 'Bchron'
uncertainty (S2LRSB7ZxE9IML): paleoData_notes: '' 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: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRSB7ZxE9IML): paleoData_method: '' has been replaced by 'standard'
uncertaintyLow (S2LRseGiPl8pnl): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRseGiPl8pnl): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRseGiPl8pnl): paleoData_method: '' has been replaced by 'linInterp'
uncertaintyLow (S2LRsKGeRBLY7n): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRsKGeRBLY7n): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRsKGeRBLY7n): paleoData_method: '' has been replaced by 'OxCal'
uncertainty (S2LRskZ8ft3o6s): paleoData_notes: '' 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: '' has been replaced by 'd13C'
uncertainty (S2LRskZ8ft3o6s): paleoData_method: '' has been replaced by 'standard'
uncertaintyLow (S2LRt1MY8cf558): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRt1MY8cf558): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRt1MY8cf558): paleoData_method: '' has been replaced by 'Bchron'
age (S2LRT3gY7xy6vJ): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRT3gY7xy6vJ): paleoData_isPrimary: '' has been replaced by 'TRUE'
age (S2LRTXXZdQVmto): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRTXXZdQVmto): paleoData_isPrimary: '' has been replaced by 'TRUE'
uncertaintyHigh (S2LRunTss1oTO0): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRunTss1oTO0): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRunTss1oTO0): paleoData_method: '' has been replaced by 'OxCal'
d18O (S2LRuTFfyRE5aJ): paleoData_variableName: 'd18OComposite' has been replaced by 'd18O'
uncertainty (S2LRuzTr63hMYH): paleoData_notes: '' 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: '' has been replaced by 'd13C'
uncertainty (S2LRuzTr63hMYH): paleoData_method: '' has been replaced by 'precision'
age (S2LRvbOaBP57dL): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRvbOaBP57dL): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRvbOaBP57dL): paleoData_method: '' has been replaced by 'copRa'
uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_method: '' has been replaced by 'Bchron'
age (S2LRWD9TJ9g9XB): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRWD9TJ9g9XB): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRWD9TJ9g9XB): paleoData_method: '' has been replaced by 'Bchron'
age (S2LRWiBDQNruT7): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRWiBDQNruT7): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRWiBDQNruT7): paleoData_method: '' has been replaced by 'Bacon'
uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRWINW1yvhPJ): paleoData_method: '' has been replaced by 'linInterp'
uncertainty (S2LRWQy2DCBq7K): paleoData_notes: '' 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: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRWQy2DCBq7K): paleoData_method: '' has been replaced by 'precision'
age (S2LRwVB7UPRXvh): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRwVB7UPRXvh): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRwVB7UPRXvh): paleoData_method: '' has been replaced by 'Bacon'
sampleID (S2LRWZOJbBWsov): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
uncertainty (S2LRXGB9h040ln): paleoData_notes: '' 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: '' has been replaced by 'd13C'
uncertainty (S2LRXGB9h040ln): paleoData_method: '' has been replaced by 'precision'
uncertainty (S2LRypY2qZ2jbC): paleoData_notes: '' 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: '' has been replaced by 'd13C'
uncertainty (S2LRypY2qZ2jbC): paleoData_method: '' has been replaced by 'standard'
uncertaintyLow (S2LRyuZBLiEjb3): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyLow (S2LRyuZBLiEjb3): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRyuZBLiEjb3): paleoData_method: '' has been replaced by 'Bacon'
age (S2LRzDvgX77JVO): paleoData_notes: '' 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: '' has been replaced by '1950'
age (S2LRzDvgX77JVO): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRzDvgX77JVO): paleoData_method: '' has been replaced by 'linInterp'
uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_notes: '' 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: '' has been replaced by '1950'
uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRzEI0J8XAaH): paleoData_method: '' has been replaced by 'Bacon'
d18O (S2LRuTFfyRE5aJ): interpretation1_seasonality: '6,7,8,9' has been replaced by 'Jun-Sep'
d18O (S2LRuTFfyRE5aJ): interpretation1_variable: 'P' has been replaced by 'precipitation'
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)'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonality: 'JJAS' has been replaced by '6,7,8,9'
geo_elevation: '1190' has been replaced by ''
d13CStandard (S2LR00P8WyCkwM): interpretation1_scope: '' has been replaced by 'climate'
d13C (S2LR1lRBQAC1iP): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LR3WTgF1AmF4): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LR466NTabeAK): interpretation1_scope: '' has been replaced by 'climate'
d13CStandard (S2LR6GAbI2miyd): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LR9DiFPcHfrK): interpretation1_scope: '' has been replaced by 'climate'
d18OStandard (S2LRAwdS0E7DsV): interpretation1_scope: '' has been replaced by 'climate'
hasHiatus (S2LRazPRENt47p): interpretation1_scope: '' has been replaced by 'climate'
mineralogy (S2LRBWKbvo13wO): interpretation1_scope: '' has been replaced by 'climate'
d13CPrecision (S2LRcdUQcbYAU1): interpretation1_scope: '' has been replaced by 'climate'
d13C (S2LRcqo665d9DJ): interpretation1_scope: '' has been replaced by 'climate'
d13C (S2LRD7jzKFswB4): interpretation1_scope: '' has been replaced by 'climate'
thickness (S2LRDPDHUoVgF0): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LRdr8i3fPtiJ): interpretation1_scope: '' has been replaced by 'climate'
d18O (S2LRfpFO2d41TG): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LRhtNuD8v5RL): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LRiptM0AYJDU): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LRjbVnr4UHpk): interpretation1_scope: '' has been replaced by 'climate'
thickness (S2LRk84w10shdf): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LRKxMHMj0F3j): interpretation1_scope: '' has been replaced by 'climate'
d18OStandard (S2LRMKcreLaiut): interpretation1_scope: '' has been replaced by 'climate'
thickness (S2LRMY8dzNCCrN): interpretation1_scope: '' has been replaced by 'climate'
d18O (S2LRN9QNRwRWs5): interpretation1_scope: '' has been replaced by 'climate'
d13CPrecision (S2LRNhGe61LfDR): interpretation1_scope: '' has been replaced by 'climate'
d18O (S2LRnUy5e71v36): interpretation1_scope: '' has been replaced by 'climate'
mineralogy (S2LRNvYx5JPQFG): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LROW4QpXx4mz): interpretation1_scope: '' has been replaced by 'climate'
d18O (S2LRQbTNgLuktR): interpretation1_scope: '' has been replaced by 'climate'
d13C (S2LRqmHrDUYyy2): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LRR2EQb9k57D): interpretation1_scope: '' has been replaced by 'climate'
d18OStandard (S2LRrEAjVuSXAF): interpretation1_scope: '' has been replaced by 'climate'
d18OStandard (S2LRSB7ZxE9IML): interpretation1_scope: '' has been replaced by 'climate'
d13CStandard (S2LRskZ8ft3o6s): interpretation1_scope: '' has been replaced by 'climate'
mineralogy (S2LRUHeSivC0qX): interpretation1_scope: '' has been replaced by 'climate'
thickness (S2LRuyjtPZyRVf): interpretation1_scope: '' has been replaced by 'climate'
d13CPrecision (S2LRuzTr63hMYH): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LRWQy2DCBq7K): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LRWZOJbBWsov): interpretation1_scope: '' has been replaced by 'climate'
mineralogy (S2LRx5ivuXi2wz): interpretation1_scope: '' has been replaced by 'climate'
d13CPrecision (S2LRXGB9h040ln): interpretation1_scope: '' has been replaced by 'climate'
d13CStandard (S2LRypY2qZ2jbC): interpretation1_scope: '' has been replaced by 'climate'
d13CStandard (S2LR00P8WyCkwM): interpretation1_scope: 'climate' has been replaced by ''
d13C (S2LR1lRBQAC1iP): interpretation1_scope: 'climate' has been replaced by ''
hasAragoniteCorrection (S2LR3WTgF1AmF4): interpretation1_scope: 'climate' has been replaced by ''
hasAragoniteCorrection (S2LR466NTabeAK): interpretation1_scope: 'climate' has been replaced by ''
d13CStandard (S2LR6GAbI2miyd): interpretation1_scope: 'climate' has been replaced by ''
sisalSampleID (S2LR9DiFPcHfrK): interpretation1_scope: 'climate' has been replaced by ''
d18OStandard (S2LRAwdS0E7DsV): interpretation1_scope: 'climate' has been replaced by ''
hasHiatus (S2LRazPRENt47p): interpretation1_scope: 'climate' has been replaced by ''
mineralogy (S2LRBWKbvo13wO): interpretation1_scope: 'climate' has been replaced by ''
d13CPrecision (S2LRcdUQcbYAU1): interpretation1_scope: 'climate' has been replaced by ''
d13C (S2LRcqo665d9DJ): interpretation1_scope: 'climate' has been replaced by ''
d13C (S2LRD7jzKFswB4): interpretation1_scope: 'climate' has been replaced by ''
thickness (S2LRDPDHUoVgF0): interpretation1_scope: 'climate' has been replaced by ''
d18OPrecision (S2LRdr8i3fPtiJ): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRfpFO2d41TG): interpretation1_scope: 'climate' has been replaced by ''
sisalSampleID (S2LRhtNuD8v5RL): interpretation1_scope: 'climate' has been replaced by ''
hasAragoniteCorrection (S2LRiptM0AYJDU): interpretation1_scope: 'climate' has been replaced by ''
sisalSampleID (S2LRjbVnr4UHpk): interpretation1_scope: 'climate' has been replaced by ''
thickness (S2LRk84w10shdf): interpretation1_scope: 'climate' has been replaced by ''
d18OPrecision (S2LRKxMHMj0F3j): interpretation1_scope: 'climate' has been replaced by ''
d18OStandard (S2LRMKcreLaiut): interpretation1_scope: 'climate' has been replaced by ''
thickness (S2LRMY8dzNCCrN): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRN9QNRwRWs5): interpretation1_scope: 'climate' has been replaced by ''
d13CPrecision (S2LRNhGe61LfDR): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRnUy5e71v36): interpretation1_scope: 'climate' has been replaced by ''
mineralogy (S2LRNvYx5JPQFG): interpretation1_scope: 'climate' has been replaced by ''
hasAragoniteCorrection (S2LROW4QpXx4mz): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRQbTNgLuktR): interpretation1_scope: 'climate' has been replaced by ''
d13C (S2LRqmHrDUYyy2): interpretation1_scope: 'climate' has been replaced by ''
d18OPrecision (S2LRR2EQb9k57D): interpretation1_scope: 'climate' has been replaced by ''
d18OStandard (S2LRrEAjVuSXAF): interpretation1_scope: 'climate' has been replaced by ''
d18OStandard (S2LRSB7ZxE9IML): interpretation1_scope: 'climate' has been replaced by ''
d13CStandard (S2LRskZ8ft3o6s): interpretation1_scope: 'climate' has been replaced by ''
mineralogy (S2LRUHeSivC0qX): interpretation1_scope: 'climate' has been replaced by ''
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonality: '6,7,8,9' has been replaced by 'JJAS'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonalityOriginal: '' has been replaced by '6,7,8,9'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_variableGroup: '' has been replaced by 'P'
thickness (S2LRuyjtPZyRVf): interpretation1_scope: 'climate' has been replaced by ''
d13CPrecision (S2LRuzTr63hMYH): interpretation1_scope: 'climate' has been replaced by ''
d18OPrecision (S2LRWQy2DCBq7K): interpretation1_scope: 'climate' has been replaced by ''
sisalSampleID (S2LRWZOJbBWsov): interpretation1_scope: 'climate' has been replaced by ''
mineralogy (S2LRx5ivuXi2wz): interpretation1_scope: 'climate' has been replaced by ''
d13CPrecision (S2LRXGB9h040ln): interpretation1_scope: 'climate' has been replaced by ''
d13CStandard (S2LRypY2qZ2jbC): interpretation1_scope: 'climate' has been replaced by ''
agelinInterp (S2LR2uCFtCMaQ8): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterp (S2LR2uCFtCMaQ8): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCalUncertaintyHigh (S2LR35k1OhLhym): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCalUncertaintyHigh (S2LR35k1OhLhym): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age (S2LR4tKX8FLvZy): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LR4tKX8FLvZy): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age (S2LR4wHnehjlDA): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LR4wHnehjlDA): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinInterpUncertaintyHigh (S2LR7CK7GOQgmW): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterpUncertaintyHigh (S2LR7CK7GOQgmW): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinRegUncertaintyLow (S2LR7gBtle7tWG): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinRegUncertaintyLow (S2LR7gBtle7tWG): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinInterpUncertaintyLow (S2LR8JjapzA6Wn): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterpUncertaintyLow (S2LR8JjapzA6Wn): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyLow (S2LR8KG6tw8fMr): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyLow (S2LR8KG6tw8fMr): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAgeUncertaintyLow (S2LRasjk0RLvG0): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAgeUncertaintyLow (S2LRasjk0RLvG0): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyLow (S2LRBczajsHLOo): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyLow (S2LRBczajsHLOo): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchron (S2LRbWzEvw6Isf): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchron (S2LRbWzEvw6Isf): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAge (S2LRCCMGOpwCsE): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAge (S2LRCCMGOpwCsE): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCal (S2LRDf4TIbhsUn): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCal (S2LRDf4TIbhsUn): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinRegUncertaintyHigh (S2LRg02DFgVGoS): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinRegUncertaintyHigh (S2LRg02DFgVGoS): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinReg (S2LRG9c5gXlIEd): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinReg (S2LRG9c5gXlIEd): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAgeUncertaintyHigh (S2LRgqiz0df8ON): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAgeUncertaintyHigh (S2LRgqiz0df8ON): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCalUncertaintyHigh (S2LRhNZe5edMYI): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCalUncertaintyHigh (S2LRhNZe5edMYI): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCalUncertaintyLow (S2LRhT8psaw66S): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCalUncertaintyLow (S2LRhT8psaw66S): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCal (S2LRHWLvxbHdBM): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCal (S2LRHWLvxbHdBM): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyHigh (S2LRkQMgcUc7nI): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyHigh (S2LRkQMgcUc7nI): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age (S2LRmWHUNyeMak): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LRmWHUNyeMak): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAge (S2LRNX5npBYgoA): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAge (S2LRNX5npBYgoA): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAgeUncertaintyHigh (S2LRnx7OytSfnz): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAgeUncertaintyHigh (S2LRnx7OytSfnz): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchron (S2LRpDsQMm9sy8): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchron (S2LRpDsQMm9sy8): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBaconUncertaintyLow (S2LRpfzUICe9Ip): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBaconUncertaintyLow (S2LRpfzUICe9Ip): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agecopRaUncertaintyLow (S2LRPIJkuVCoYO): paleoData_units: 'yr BP' has been replaced by 'BP'
agecopRaUncertaintyLow (S2LRPIJkuVCoYO): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCal (S2LRPtaotogqQx): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCal (S2LRPtaotogqQx): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCalUncertaintyLow (S2LRQb4xHkecvh): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCalUncertaintyLow (S2LRQb4xHkecvh): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBaconUncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBaconUncertaintyHigh (S2LRQIKKz8Gpmp): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAgeUncertaintyLow (S2LRQXoEf7EAVM): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAgeUncertaintyLow (S2LRQXoEf7EAVM): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agecopRaUncertaintyHigh (S2LRr1Nt6kwShM): paleoData_units: 'yr BP' has been replaced by 'BP'
agecopRaUncertaintyHigh (S2LRr1Nt6kwShM): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyHigh (S2LRRXD2aexZU2): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyHigh (S2LRRXD2aexZU2): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinInterpUncertaintyLow (S2LRseGiPl8pnl): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterpUncertaintyLow (S2LRseGiPl8pnl): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCalUncertaintyLow (S2LRsKGeRBLY7n): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCalUncertaintyLow (S2LRsKGeRBLY7n): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyLow (S2LRt1MY8cf558): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyLow (S2LRt1MY8cf558): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age (S2LRT3gY7xy6vJ): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LRT3gY7xy6vJ): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age (S2LRTXXZdQVmto): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LRTXXZdQVmto): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageOxCalUncertaintyHigh (S2LRunTss1oTO0): paleoData_units: 'yr BP' has been replaced by 'BP'
ageOxCalUncertaintyHigh (S2LRunTss1oTO0): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxyLumps: '' has been replaced by 'isotope'
d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
agecopRa (S2LRvbOaBP57dL): paleoData_units: 'yr BP' has been replaced by 'BP'
agecopRa (S2LRvbOaBP57dL): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyHigh (S2LRW6aiuq0Tcm): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchron (S2LRWD9TJ9g9XB): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchron (S2LRWD9TJ9g9XB): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBacon (S2LRWiBDQNruT7): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBacon (S2LRWiBDQNruT7): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinInterpUncertaintyHigh (S2LRWINW1yvhPJ): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterpUncertaintyHigh (S2LRWINW1yvhPJ): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBacon (S2LRwVB7UPRXvh): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBacon (S2LRwVB7UPRXvh): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBaconUncertaintyLow (S2LRyuZBLiEjb3): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBaconUncertaintyLow (S2LRyuZBLiEjb3): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
agelinInterp (S2LRzDvgX77JVO): paleoData_units: 'yr BP' has been replaced by 'BP'
agelinInterp (S2LRzDvgX77JVO): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBaconUncertaintyHigh (S2LRzEI0J8XAaH): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBaconUncertaintyHigh (S2LRzEI0J8XAaH): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age_type (S2LcRayqsINzw1d): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRayqsINzw1d): chronData_variableNameOriginal: '' has been replaced by 'ageType'
age_type (S2LcRCHCNxuaZxi): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRCHCNxuaZxi): chronData_variableNameOriginal: '' has been replaced by 'ageType'
age_type (S2LcRFiH4gvFdWk): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRFiH4gvFdWk): chronData_variableNameOriginal: '' has been replaced by 'ageType'
age_type (S2LcRHSaBRMXHFF): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRHSaBRMXHFF): chronData_variableNameOriginal: '' has been replaced by 'ageType'
age_type (S2LcRXpNEfAsaB1): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRXpNEfAsaB1): chronData_variableNameOriginal: '' has been replaced by 'ageType'
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)'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_variable: 'M' has been replaced by 'P'
geo_gcmdLocation: '' has been replaced by 'Asia>Southcentral Asia>India'
archiveType: 'speleothem' has been replaced by 'Speleothem'
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)"'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonalityGeneral: 'Summer' has been replaced by 'summerOnly'
d18OStandardComposite (S2LR6791eWz5KM): interpretation1_scope: '' has been replaced by 'climate'
d13CStandardComposite (S2LRCaXY3l2nYh): interpretation1_scope: '' has been replaced by 'climate'
thicknessComposite (S2LRcvsbZIuf6n): interpretation1_scope: '' has been replaced by 'climate'
entityName (S2LRIi3L7bNHpM): interpretation1_scope: '' has been replaced by 'climate'
mineralogyComposite (S2LRjGtfkhKuaH): interpretation1_scope: '' has been replaced by 'climate'
d13CPrecisionComposite (S2LRLCnhzcT2KE): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrectionComposite (S2LRP7mL4fQN1r): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleIDComposite (S2LRRslnAna0Q6): interpretation1_scope: '' has been replaced by 'climate'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_direction: '' has been replaced by 'negative'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_scope: '' has been replaced by 'climate'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonality: '' has been replaced by '6,7,8,9'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_seasonalityGeneral: '' has been replaced by 'Summer'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_variable: '' has been replaced by 'M'
d18OComposite (S2LRuTFfyRE5aJ): interpretation1_variableDetail: '' has been replaced by 'monsoon@surface'
d13CComposite (S2LRUVrcJsNzTD): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecisionComposite (S2LRyK5qOd0NtE): interpretation1_scope: '' has been replaced by 'climate'
d18OComposite (S2LRuTFfyRE5aJ): paleoData_notes: '' 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: '' has been replaced by 'd18O'
d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxyDetail: '' has been replaced by 'calcite'
d18OComposite (S2LRuTFfyRE5aJ): paleoData_proxyGeneral: '' has been replaced by 'isotope'
d18OComposite (S2LRuTFfyRE5aJ): paleoData_QCCertification: '' has been replaced by 'CH'
d18OComposite (S2LRuTFfyRE5aJ): paleoData_QCnotes: '' 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)"'
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
Sinha, A., Kathayat, G., Cheng, H., Breitenbach, S. F. M., Berkelhammer, M., Mudelsee, M., Biswas, J. and Edwards, R. L.: Trends and oscillations in the Indian summer monsoon rainfall over the last two millennia, Nat. Commun., 6(1), 2015.
Trends and oscillations in the Indian summer monsoon rainfall over the last two millennia
Kathayat, G., Cheng, H., Sinha, A., Yi, L., Li, X., Zhang, H., Li, H., Ning, Y. and Edwards, R. L.: The Indian monsoon variability and civilization changes in the Indian subcontinent, Sci. Adv., 3(12), e1701296, 2017.