Refers to the unique identifier for the sample (as given in sample table)
NA; paleoData_isPrimary has been standardized
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
((( null ))) "On shorter timescale, we cannot disentangle the different pro- cesses influencing the speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019) /// "On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)
Laboratory precision on the d18O measurement
NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
"δ13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the δ13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the δ13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019)
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
Original published positive uncertainty on the age of the sample in years
NA; paleoData_inferredMaterial has been standardized; paleoData_datum has been standardized
Original published negative uncertainty on the age of the sample in years
Calendar age in years BP, method = Bchron
NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
Positive age uncertaintyin years BP, method = Bchron
NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized
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 = StalAge
Positive age uncertaintyin years BP, method = StalAge
Negative age uncertaintyin years BP, method = StalAge
The laboratory number of the dated sample
Minimum weight of the dated sample in mg
Maximum weight of the dated sample in mg
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 content of the dated sample in ppt
230Th 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
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
d13C (S2LR64Q0qhBLAC): interpretation1_seasonality: '((( null ))) 3,4,5,6,7,8 /// Mar-Aug' has been replaced by 'Mar-Aug'
d13C (S2LR64Q0qhBLAC): interpretation1_seasonalityGeneral: '((( null ))) Summer /// summerOnly' has been replaced by 'summerOnly'
d13C (S2LR64Q0qhBLAC): interpretation1_variable: '((( null ))) P-E /// effectivePrecipitation' has been replaced by 'effectivePrecipitation'
d18O (S2LRwIx2rupVpo): interpretation1_variable: '((( null ))) T /// temperature' has been replaced by 'temperature'
d13C (S2LR64Q0qhBLAC): interpretation1_seasonality: 'Mar-Aug' has been replaced by '((( null ))) 3,4,5,6,7,8 /// Mar-Aug'
d13C (S2LR64Q0qhBLAC): interpretation1_seasonalityGeneral: 'summerOnly' has been replaced by '((( null ))) Summer /// summerOnly'
d13C (S2LR64Q0qhBLAC): interpretation1_variable: 'effectivePrecipitation' has been replaced by '((( null ))) P-E /// effectivePrecipitation'
d18O (S2LRwIx2rupVpo): interpretation1_variable: 'temperature' has been replaced by '((( null ))) T /// temperature'
d13C (S2LR64Q0qhBLAC): paleoData_meetsHoloceneHydroclimateCriteria: '' has been replaced by 'TRUE'
d13C (S2LR64Q0qhBLAC): paleoData_primaryTimeseries: '' has been replaced by 'TRUE'
d18O (S2LRwIx2rupVpo): paleoData_notes: '"On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)' has been replaced by '((( null ))) "On shorter timescale, we cannot disentangle the different pro- cesses influencing the speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019) /// "On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)'
d18O (S2LRwIx2rupVpo): paleoData_meetsHoloceneHydroclimateCriteria: '' has been replaced by 'TRUE'
d18O (S2LRwIx2rupVpo): paleoData_primaryTimeseries: '' has been replaced by 'TRUE'
uncertaintyHigh (S2LR23SuZHg2tm): interpretation2_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LR23SuZHg2tm): interpretation3_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LR23SuZHg2tm): interpretation4_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LR23SuZHg2tm): interpretation5_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LR23SuZHg2tm): interpretation6_scope: '' has been replaced by 'isotope'
mineralogy (S2LR2VpUt8ryEN): interpretation2_scope: '' has been replaced by 'climate'
mineralogy (S2LR2VpUt8ryEN): interpretation3_scope: '' has been replaced by 'climate'
mineralogy (S2LR2VpUt8ryEN): interpretation4_scope: '' has been replaced by 'isotope'
mineralogy (S2LR2VpUt8ryEN): interpretation5_scope: '' has been replaced by 'isotope'
mineralogy (S2LR2VpUt8ryEN): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LR5k5cHtgPV7): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LR5k5cHtgPV7): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LR5k5cHtgPV7): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LR5k5cHtgPV7): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LR5k5cHtgPV7): interpretation6_scope: '' has been replaced by 'isotope'
d13C (S2LR64Q0qhBLAC): interpretation2_scope: '' has been replaced by 'climate'
d13C (S2LR64Q0qhBLAC): interpretation3_scope: '' has been replaced by 'climate'
d13C (S2LR64Q0qhBLAC): interpretation4_scope: '' has been replaced by 'isotope'
d13C (S2LR64Q0qhBLAC): interpretation5_scope: '' has been replaced by 'isotope'
d13C (S2LR64Q0qhBLAC): interpretation6_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRCjzWuimmkl): interpretation2_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRCjzWuimmkl): interpretation3_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRCjzWuimmkl): interpretation4_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRCjzWuimmkl): interpretation5_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRCjzWuimmkl): interpretation6_scope: '' has been replaced by 'isotope'
correction (S2LRDR6YC9Wzjk): interpretation2_scope: '' has been replaced by 'climate'
correction (S2LRDR6YC9Wzjk): interpretation3_scope: '' has been replaced by 'climate'
correction (S2LRDR6YC9Wzjk): interpretation4_scope: '' has been replaced by 'isotope'
correction (S2LRDR6YC9Wzjk): interpretation5_scope: '' has been replaced by 'isotope'
correction (S2LRDR6YC9Wzjk): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LRKAhyygYbB5): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LRKAhyygYbB5): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LRKAhyygYbB5): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LRKAhyygYbB5): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LRKAhyygYbB5): interpretation6_scope: '' has been replaced by 'isotope'
sampleID (S2LROlJkEjS9Fh): interpretation2_scope: '' has been replaced by 'climate'
sampleID (S2LROlJkEjS9Fh): interpretation3_scope: '' has been replaced by 'climate'
sampleID (S2LROlJkEjS9Fh): interpretation4_scope: '' has been replaced by 'isotope'
sampleID (S2LROlJkEjS9Fh): interpretation5_scope: '' has been replaced by 'isotope'
sampleID (S2LROlJkEjS9Fh): interpretation6_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRYgesMl2OtQ): interpretation2_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRYgesMl2OtQ): interpretation3_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRYgesMl2OtQ): interpretation4_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRYgesMl2OtQ): interpretation5_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRYgesMl2OtQ): interpretation6_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRcV1AcpxqJY): interpretation2_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRcV1AcpxqJY): interpretation3_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRcV1AcpxqJY): interpretation4_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRcV1AcpxqJY): interpretation5_scope: '' has been replaced by 'isotope'
uncertaintyHigh (S2LRcV1AcpxqJY): interpretation6_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRksYsm3oIWC): interpretation2_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRksYsm3oIWC): interpretation3_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRksYsm3oIWC): interpretation4_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRksYsm3oIWC): interpretation5_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRksYsm3oIWC): interpretation6_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRtPVFvN10Pd): interpretation2_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRtPVFvN10Pd): interpretation3_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRtPVFvN10Pd): interpretation4_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRtPVFvN10Pd): interpretation5_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRtPVFvN10Pd): interpretation6_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRuGVy3afygQ): interpretation2_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRuGVy3afygQ): interpretation3_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRuGVy3afygQ): interpretation4_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRuGVy3afygQ): interpretation5_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRuGVy3afygQ): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LRuPbC0k2YQw): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LRuPbC0k2YQw): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LRuPbC0k2YQw): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LRuPbC0k2YQw): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LRuPbC0k2YQw): interpretation6_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRwAeFTzzH2W): interpretation2_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRwAeFTzzH2W): interpretation3_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRwAeFTzzH2W): interpretation4_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRwAeFTzzH2W): interpretation5_scope: '' has been replaced by 'isotope'
uncertaintyLow (S2LRwAeFTzzH2W): interpretation6_scope: '' has been replaced by 'isotope'
d18O (S2LRwIx2rupVpo): interpretation2_scope: '' has been replaced by 'climate'
d18O (S2LRwIx2rupVpo): interpretation3_scope: '' has been replaced by 'climate'
d18O (S2LRwIx2rupVpo): interpretation4_scope: '' has been replaced by 'isotope'
d18O (S2LRwIx2rupVpo): interpretation5_scope: '' has been replaced by 'isotope'
d18O (S2LRwIx2rupVpo): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LRyz0yLvk0am): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LRyz0yLvk0am): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LRyz0yLvk0am): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LRyz0yLvk0am): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LRyz0yLvk0am): interpretation6_scope: '' has been replaced by 'isotope'
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 'Alexander Budsky and Denis Scholz and Jasper A Wassenburg and Regina Mertz-Kraus and Christoph Sp√∂tl and Dana FC Riechelmann and Luis Gibert and Klaus Peter Jochum and Meinrat O Andreae'
pub1_journal: '' has been replaced by 'The Holocene'
pub1_pages: '' has been replaced by '1113--1133'
pub1_title: '' has been replaced by 'Speleothem $\updelta$$\less$sup$\greater$13$\less$/sup$\greater$C record suggests enhanced spring/summer drought in south-eastern Spain between 9.7 and 7.8 ka {\textendash} A circum-Western Mediterranean anomaly?'
d13C (S2LR64Q0qhBLAC): paleoData_notes: '((( "��13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the ��13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the ��13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019) ))) "δ13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the δ13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the δ13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019) /// "δ13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the δ13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the δ13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019)' has been replaced by '"δ13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the δ13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the δ13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019)'
d18O (S2LRwIx2rupVpo): paleoData_notes: '((( "On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem ��18O signal. However, on multi-millennial to orbital timescales, ��18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone ��18O values and the interpretation of the ��18O record of the CV flowstone remains challenging, we assume that the ��18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 �� 0.35 to 7.8 �� 0.2 ka, higher growth rates coincide with lower ��18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019) ))) "On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019) /// "On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)' has been replaced by '"On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)'
d13C (S2LR64Q0qhBLAC): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'
uncertaintyHigh (S2LR23SuZHg2tm): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRCjzWuimmkl): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRcV1AcpxqJY): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRksYsm3oIWC): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRtPVFvN10Pd): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRuGVy3afygQ): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyLow (S2LRwAeFTzzH2W): interpretation1_scope: '' has been replaced by 'climate'
uncertaintyHigh (S2LRYgesMl2OtQ): interpretation1_scope: '' has been replaced by 'climate'
d13C (S2LR64Q0qhBLAC): paleoData_notes: '"δ13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the δ13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the δ13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019)' has been replaced by '((( "��13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the ��13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the ��13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019) ))) "δ13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the δ13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the δ13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019) /// "δ13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the δ13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the δ13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019)'
d18O (S2LRwIx2rupVpo): paleoData_notes: '"On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)' has been replaced by '((( "On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem ��18O signal. However, on multi-millennial to orbital timescales, ��18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone ��18O values and the interpretation of the ��18O record of the CV flowstone remains challenging, we assume that the ��18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 �� 0.35 to 7.8 �� 0.2 ka, higher growth rates coincide with lower ��18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019) ))) "On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019) /// "On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '75'
uncertaintyHigh (S2LR23SuZHg2tm): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyHigh (S2LR23SuZHg2tm): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyHigh (S2LR23SuZHg2tm): paleoData_variableName: 'ageBaconUncertaintyHigh' has been replaced by 'uncertaintyHigh'
uncertaintyHigh (S2LR23SuZHg2tm): paleoData_datum: '' has been replaced by '1950'
uncertaintyHigh (S2LR23SuZHg2tm): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LR23SuZHg2tm): paleoData_method: '' has been replaced by 'Bacon'
uncertainty (S2LR5k5cHtgPV7): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LR5k5cHtgPV7): paleoData_variableName: 'd13CStandard' has been replaced by 'uncertainty'
uncertainty (S2LR5k5cHtgPV7): paleoData_measurementMaterial: '' has been replaced by 'd13C'
uncertainty (S2LR5k5cHtgPV7): paleoData_method: '' has been replaced by 'standard'
uncertaintyHigh (S2LRCjzWuimmkl): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_datum has been standardized'
uncertaintyHigh (S2LRCjzWuimmkl): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyHigh (S2LRCjzWuimmkl): paleoData_variableName: 'ageUncertaintyHigh' has been replaced by 'uncertaintyHigh'
uncertaintyHigh (S2LRCjzWuimmkl): paleoData_datum: '' has been replaced by '1950'
uncertaintyHigh (S2LRCjzWuimmkl): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRcV1AcpxqJY): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyHigh (S2LRcV1AcpxqJY): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyHigh (S2LRcV1AcpxqJY): paleoData_variableName: 'ageBchronUncertaintyHigh' has been replaced by 'uncertaintyHigh'
uncertaintyHigh (S2LRcV1AcpxqJY): paleoData_datum: '' has been replaced by '1950'
uncertaintyHigh (S2LRcV1AcpxqJY): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRcV1AcpxqJY): paleoData_method: '' has been replaced by 'Bchron'
correction (S2LRDR6YC9Wzjk): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
correction (S2LRDR6YC9Wzjk): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
correction (S2LRDR6YC9Wzjk): paleoData_method: '' has been replaced by 'aragonite correction'
age (S2LRFYPM2WuDGW): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRFYPM2WuDGW): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRFYPM2WuDGW): paleoData_variableName: 'ageBacon' has been replaced by 'age'
age (S2LRFYPM2WuDGW): paleoData_datum: '' has been replaced by '1950'
age (S2LRFYPM2WuDGW): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRFYPM2WuDGW): paleoData_method: '' has been replaced by 'Bacon'
uncertainty (S2LRKAhyygYbB5): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRKAhyygYbB5): paleoData_variableName: 'd18OStandard' has been replaced by 'uncertainty'
uncertainty (S2LRKAhyygYbB5): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRKAhyygYbB5): paleoData_method: '' has been replaced by 'standard'
uncertaintyLow (S2LRksYsm3oIWC): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyLow (S2LRksYsm3oIWC): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyLow (S2LRksYsm3oIWC): paleoData_variableName: 'ageStalAgeUncertaintyLow' has been replaced by 'uncertaintyLow'
uncertaintyLow (S2LRksYsm3oIWC): paleoData_datum: '' has been replaced by '1950'
uncertaintyLow (S2LRksYsm3oIWC): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRksYsm3oIWC): paleoData_method: '' has been replaced by 'StalAge'
age (S2LRmJHRHpp24z): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRmJHRHpp24z): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRmJHRHpp24z): paleoData_variableName: 'ageStalAge' has been replaced by 'age'
age (S2LRmJHRHpp24z): paleoData_datum: '' has been replaced by '1950'
age (S2LRmJHRHpp24z): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRmJHRHpp24z): paleoData_method: '' has been replaced by 'StalAge'
sampleID (S2LROlJkEjS9Fh): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
depth (S2LRsttW7TPugE): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
depth (S2LRsttW7TPugE): paleoData_units: 'depth_sample' has been replaced by 'mm'
depth (S2LRsttW7TPugE): paleoData_isPrimary: '' has been replaced by 'TRUE'
uncertaintyLow (S2LRtPVFvN10Pd): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyLow (S2LRtPVFvN10Pd): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyLow (S2LRtPVFvN10Pd): paleoData_variableName: 'ageBaconUncertaintyLow' has been replaced by 'uncertaintyLow'
uncertaintyLow (S2LRtPVFvN10Pd): paleoData_datum: '' has been replaced by '1950'
uncertaintyLow (S2LRtPVFvN10Pd): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRtPVFvN10Pd): paleoData_method: '' has been replaced by 'Bacon'
age (S2LRtwRfO7sqi5): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRtwRfO7sqi5): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRtwRfO7sqi5): paleoData_variableName: 'ageBchron' has been replaced by 'age'
age (S2LRtwRfO7sqi5): paleoData_datum: '' has been replaced by '1950'
age (S2LRtwRfO7sqi5): paleoData_isPrimary: '' has been replaced by 'FALSE'
age (S2LRtwRfO7sqi5): paleoData_method: '' has been replaced by 'Bchron'
uncertaintyLow (S2LRuGVy3afygQ): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyLow (S2LRuGVy3afygQ): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyLow (S2LRuGVy3afygQ): paleoData_variableName: 'ageBchronUncertaintyLow' has been replaced by 'uncertaintyLow'
uncertaintyLow (S2LRuGVy3afygQ): paleoData_datum: '' has been replaced by '1950'
uncertaintyLow (S2LRuGVy3afygQ): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyLow (S2LRuGVy3afygQ): paleoData_method: '' has been replaced by 'Bchron'
uncertainty (S2LRuPbC0k2YQw): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRuPbC0k2YQw): paleoData_variableName: 'd13CPrecision' has been replaced by 'uncertainty'
uncertainty (S2LRuPbC0k2YQw): paleoData_measurementMaterial: '' has been replaced by 'd13C'
uncertainty (S2LRuPbC0k2YQw): paleoData_method: '' has been replaced by 'precision'
age (S2LRVNoGLHhMnq): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRVNoGLHhMnq): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRVNoGLHhMnq): paleoData_datum: '' has been replaced by '1950'
age (S2LRVNoGLHhMnq): paleoData_isPrimary: '' has been replaced by 'TRUE'
uncertaintyLow (S2LRwAeFTzzH2W): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_datum has been standardized'
uncertaintyLow (S2LRwAeFTzzH2W): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyLow (S2LRwAeFTzzH2W): paleoData_variableName: 'ageUncertaintyLow' has been replaced by 'uncertaintyLow'
uncertaintyLow (S2LRwAeFTzzH2W): paleoData_datum: '' has been replaced by '1950'
uncertaintyLow (S2LRwAeFTzzH2W): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRYgesMl2OtQ): paleoData_notes: '' has been replaced by 'NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized'
uncertaintyHigh (S2LRYgesMl2OtQ): paleoData_units: 'BP' has been replaced by 'yr BP'
uncertaintyHigh (S2LRYgesMl2OtQ): paleoData_variableName: 'ageStalAgeUncertaintyHigh' has been replaced by 'uncertaintyHigh'
uncertaintyHigh (S2LRYgesMl2OtQ): paleoData_datum: '' has been replaced by '1950'
uncertaintyHigh (S2LRYgesMl2OtQ): paleoData_inferredMaterial: '' has been replaced by 'age'
uncertaintyHigh (S2LRYgesMl2OtQ): paleoData_method: '' has been replaced by 'StalAge'
uncertainty (S2LRyz0yLvk0am): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRyz0yLvk0am): paleoData_variableName: 'd18OPrecision' has been replaced by 'uncertainty'
uncertainty (S2LRyz0yLvk0am): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRyz0yLvk0am): paleoData_method: '' has been replaced by 'precision'
d13C (S2LR64Q0qhBLAC): interpretation1_seasonality: '3,4,5,6,7,8' has been replaced by 'Mar-Aug'
d18O (S2LRwIx2rupVpo): interpretation1_variable: 'T' has been replaced by 'temperature'
geo_elevation: '75' has been replaced by ''
mineralogy (S2LR2VpUt8ryEN): interpretation1_scope: '' has been replaced by 'climate'
d13CStandard (S2LR5k5cHtgPV7): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LRDR6YC9Wzjk): interpretation1_scope: '' has been replaced by 'climate'
d18OStandard (S2LRKAhyygYbB5): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LROlJkEjS9Fh): interpretation1_scope: '' has been replaced by 'climate'
d13CPrecision (S2LRuPbC0k2YQw): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LRyz0yLvk0am): interpretation1_scope: '' has been replaced by 'climate'
ageBaconUncertaintyHigh (S2LR23SuZHg2tm): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBaconUncertaintyHigh (S2LR23SuZHg2tm): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
d13C (S2LR64Q0qhBLAC): paleoData_proxyLumps: '' has been replaced by 'isotope'
d13C (S2LR64Q0qhBLAC): paleoData_proxyLumpsOriginal: '' has been replaced by 'd13C'
ageUncertaintyHigh (S2LRCjzWuimmkl): paleoData_units: 'yr BP' has been replaced by 'BP'
ageUncertaintyHigh (S2LRCjzWuimmkl): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyHigh (S2LRcV1AcpxqJY): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyHigh (S2LRcV1AcpxqJY): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBacon (S2LRFYPM2WuDGW): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBacon (S2LRFYPM2WuDGW): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAgeUncertaintyLow (S2LRksYsm3oIWC): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAgeUncertaintyLow (S2LRksYsm3oIWC): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageStalAge (S2LRmJHRHpp24z): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAge (S2LRmJHRHpp24z): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBaconUncertaintyLow (S2LRtPVFvN10Pd): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBaconUncertaintyLow (S2LRtPVFvN10Pd): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchron (S2LRtwRfO7sqi5): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchron (S2LRtwRfO7sqi5): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageBchronUncertaintyLow (S2LRuGVy3afygQ): paleoData_units: 'yr BP' has been replaced by 'BP'
ageBchronUncertaintyLow (S2LRuGVy3afygQ): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age (S2LRVNoGLHhMnq): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LRVNoGLHhMnq): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
ageUncertaintyLow (S2LRwAeFTzzH2W): paleoData_units: 'yr BP' has been replaced by 'BP'
ageUncertaintyLow (S2LRwAeFTzzH2W): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
d18O (S2LRwIx2rupVpo): paleoData_proxyLumps: '' has been replaced by 'isotope'
d18O (S2LRwIx2rupVpo): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
ageStalAgeUncertaintyHigh (S2LRYgesMl2OtQ): paleoData_units: 'yr BP' has been replaced by 'BP'
ageStalAgeUncertaintyHigh (S2LRYgesMl2OtQ): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
mineralogy (S2LR2VpUt8ryEN): interpretation1_scope: 'climate' has been replaced by ''
d13CStandard (S2LR5k5cHtgPV7): interpretation1_scope: 'climate' has been replaced by ''
d13C (S2LR64Q0qhBLAC): interpretation1_variableGroup: '' has been replaced by 'P-E'
hasAragoniteCorrection (S2LRDR6YC9Wzjk): interpretation1_scope: 'climate' has been replaced by ''
d18OStandard (S2LRKAhyygYbB5): interpretation1_scope: 'climate' has been replaced by ''
sisalSampleID (S2LROlJkEjS9Fh): interpretation1_scope: 'climate' has been replaced by ''
d13CPrecision (S2LRuPbC0k2YQw): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRwIx2rupVpo): interpretation1_variableGroup: '' has been replaced by 'Temperature'
d18O (S2LRwIx2rupVpo): interpretation1_variableGroupDirection: '' has been replaced by 'negative'
d18O (S2LRwIx2rupVpo): interpretation1_variableGroupOriginal: '' has been replaced by 'T'
d18OPrecision (S2LRyz0yLvk0am): interpretation1_scope: 'climate' has been replaced by ''
age_type (S2LcRaRsY3dz7ZL): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRaRsY3dz7ZL): chronData_variableNameOriginal: '' has been replaced by 'ageType'
geo_gcmdLocation: '' has been replaced by 'Europe>Southern Europe>Spain'
archiveType: 'speleothem' has been replaced by 'Speleothem'
d13C (S2LR64Q0qhBLAC): interpretation1_seasonalityGeneral: 'Summer' has been replaced by 'summerOnly'
d18O (S2LRwIx2rupVpo): paleoData_notes: '"On shorter timescale, we cannot disentangle the different pro- cesses influencing the speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)' has been replaced by '"On shorter timescale, we cannot disentangle the different pro- cesses influencing the Speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)'
d13C (S2LR64Q0qhBLAC): interpretation1_direction: '' has been replaced by 'negative'
d13C (S2LR64Q0qhBLAC): interpretation1_scope: '' has been replaced by 'climate'
d13C (S2LR64Q0qhBLAC): interpretation1_seasonality: '' has been replaced by '3,4,5,6,7,8'
d13C (S2LR64Q0qhBLAC): interpretation1_seasonalityGeneral: '' has been replaced by 'Summer'
d13C (S2LR64Q0qhBLAC): interpretation1_variable: '' has been replaced by 'P-E'
d13C (S2LR64Q0qhBLAC): interpretation1_variableDetail: '' has been replaced by '@surface'
d18O (S2LRwIx2rupVpo): interpretation1_scope: '' has been replaced by 'climate'
d18O (S2LRwIx2rupVpo): interpretation1_variable: '' has been replaced by 'T'
d13C (S2LR64Q0qhBLAC): paleoData_notes: '' has been replaced by '"δ13C values reflect the vegetation density and microbiological activity in the soil and are therefore a spring to summer signal...the δ13C values of the CV flowstone should be a sensitive proxy for past spring and summer drought even if aquifer recharge and flow- stone growth predominantly occur during the autumn and winter season (Carrasco et al., 2006). Therefore, we interpret the δ13C values as a proxy for soil microbial activity and vegetation den- sity reflecting changes in the length of the vegetation period and, thus, spring/summer drought." (Budsky et al., 2019)'
d13C (S2LR64Q0qhBLAC): paleoData_proxy: '' has been replaced by 'd13C'
d13C (S2LR64Q0qhBLAC): paleoData_proxyDetail: '' has been replaced by 'calcite'
d13C (S2LR64Q0qhBLAC): paleoData_proxyGeneral: '' has been replaced by 'isotope'
d13C (S2LR64Q0qhBLAC): paleoData_QCCertification: '' has been replaced by 'CH'
d18O (S2LRwIx2rupVpo): paleoData_notes: '' has been replaced by '"On shorter timescale, we cannot disentangle the different pro- cesses influencing the speleothem δ18O signal. However, on multi-millennial to orbital timescales, δ18O values are mainly influenced by North Atlantic temperature changes and seasonal- ity...In summary, although we cannot disentangle the processes affecting the flowstone δ18O values and the interpretation of the δ18O record of the CV flowstone remains challenging, we assume that the δ18O values of the CV flowstone on orbital timescales and during the late Glacial might be related to temperature changes on the North Atlantic, which is supported by the good agreement with the SST records. However, the influence of other parameters, such as seasonality of rainfall, rainfall amount and changes in moisture source(s), cannot be excluded. For the period from 10.5 ± 0.35 to 7.8 ± 0.2 ka, higher growth rates coincide with lower δ18O values, which suggest an additional influence of changes in the amount of autumn/winter precipita- tion on millennial timescales." (Budsky et al., 2019)'
d18O (S2LRwIx2rupVpo): paleoData_proxy: '' has been replaced by 'd18O'
d18O (S2LRwIx2rupVpo): paleoData_proxyDetail: '' has been replaced by 'calcite'
d18O (S2LRwIx2rupVpo): paleoData_proxyGeneral: '' has been replaced by 'isotope'
d18O (S2LRwIx2rupVpo): paleoData_QCCertification: '' has been replaced by 'CH'
Alexander Budsky and Denis Scholz and Jasper A Wassenburg and Regina Mertz-Kraus and Christoph Sp√∂tl and Dana FC Riechelmann and Luis Gibert and Klaus Peter Jochum and Meinrat O Andreae
Budsky, A., Scholz, D., Wassenburg, J. A., Mertz-Kraus, R., Sp<f6>tl, C., Riechelmann, D. F., Gibert, L., Jochum, K. P. and Andreae, M. O.: Speleothem ?13C record suggests enhanced spring/summer drought in south-eastern Spain between 9.7 and 7.8 ka <96> A circum-Western Mediterranean anomaly?, The Holocene, 29(7), 1113<96>1133, 2019.
Speleothem $\updelta$$\less$sup$\greater$13$\less$/sup$\greater$C record suggests enhanced spring/summer drought in south-eastern Spain between 9.7 and 7.8 ka {\textendash} A circum-Western Mediterranean anomaly?