"We used a Thermo Scientificdegrees Trace gas chromato graph equipped with an Rxi5ms column (30 m degrees 0.25 mm, film thickness 1 permilm) and a programmable temperature va porizing (PTV) injector operated in solvent split mode with an evaporation temperature of 60 permil C. The GC was con nected via a GC Isolink with pyrolysis/combustion furnace (at 1400/1000 permilC) and a Conflo IV interface to a DeltaVPlus isotope ratio mass spectrometer. The H+3 factor (Sessions et al., 2001) was determined daily to test measurement linearity of the system and accounted for 5.8 ppm mvpermil1 on average. Reference peaks of H2 bracket nalkanoic acid peaks during the course of a GCIRMS run; two of these peaks were used for the standardization of the isotopic analysis, while the remainders were treated as unknowns to assess pre cision. Except for the case of coelution, precision of these replicates was better than 0.6 permil."
; archiveType changed was originally Lake sediment (LS)
Since temperature and precipitation amounts are anticor- related on an interannual timescale (Fig. 5), we interpret low ?D values to indicate both relatively cool and wet conditions. In addition to fluctuations in mean annual precipitation iso- topes, snowmelt and delivery to plants may vary. We suggest that a high proportional contribution of water derived from snowmelt, after relatively long and wet winters with high amounts of snowfall, can further lead to more negative ?D leaf wax values.
Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of growing season rainfall (relative to total water used by plants) would result in higher deltaD values.
Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of winter snowmelt (relative to total water used by plants) would result in lower deltaD values.
winter snow melting during growing season
This amount effect lowers the summer precipitation isotopic com- position, dampens the seasonality of the mean precipitation of isotopic values and lowers the integrated annual precip- itation isotopic composition. Hence, in drier years average ?D values will be D-enriched relative to wetter years, and likewise warmer years will be D-enriched relative to colder years (Fig. 4b). Given the low precipitation amounts in this arid region today, the amount effect is likely to remain sec-ondary to the temperature controls on isotopic composition apparent in the seasonal cycle.
Invalid variable name ET:duplicate of LS15AIKAB?
Invalid variable name. Check that TSid is valid
fraction of modern 14C activity uncertainty
210Pb, 239+240Pu or 137Cs activity uncertainty
Y if supported 210Pb activity, N if unsupported 210Pb activity
model used to convert 210Pb activity to age (e.g., constant rate of supply)
years before 1950 (calibrated age, or ages that dont need calibration)
was this date used in the age modelpermil
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d2H (LS15AIKA01A1): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS15AIKA01A1): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS15AIKA01A2): interpretation2_basis: 'Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of growing season rainfall (relative to total water used by plants) would result in higher deltaD values.' has been replaced by ''
d2H (LS15AIKA01A2): interpretation2_direction: 'positive' has been replaced by ''
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d2H (LS15AIKA01A2): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
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d2H (LS15AIKA01A2): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS15AIKA01A2): interpretation3_basis: 'Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of winter snowmelt (relative to total water used by plants) would result in lower deltaD values.' has been replaced by ''
d2H (LS15AIKA01A2): interpretation3_direction: 'negative' has been replaced by ''
d2H (LS15AIKA01A2): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS15AIKA01A2): interpretation3_rank: '2' has been replaced by ''
d2H (LS15AIKA01A2): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS15AIKA01A2): interpretation3_seasonality: 'Winter' has been replaced by ''
d2H (LS15AIKA01A2): interpretation3_variable: 'precipitation' has been replaced by ''
d2H (LS15AIKA01A2): interpretation3_variableGroup: 'winter snow melting during growing season' has been replaced by ''
d2H (LS15AIKA01A2): interpretation4_basis: 'This amount effect lowers the summer precipitation isotopic com- position, dampens the seasonality of the mean precipitation of isotopic values and lowers the integrated annual precip- itation isotopic composition. Hence, in drier years average ?D values will be D-enriched relative to wetter years, and likewise warmer years will be D-enriched relative to colder years (Fig. 4b). Given the low precipitation amounts in this arid region today, the amount effect is likely to remain sec-ondary to the temperature controls on isotopic composition apparent in the seasonal cycle.' has been replaced by 'Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of growing season rainfall (relative to total water used by plants) would result in higher deltaD values.'
d2H (LS15AIKA01A2): interpretation4_direction: 'negative' has been replaced by 'positive'
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d2H (LS15AIKA01A2): interpretation4_seasonality: 'Summer' has been replaced by 'Annual'
d2H (LS15AIKA01A2): interpretation4_variable: 'precipitation' has been replaced by 'precipitationIsotope'
d2H (LS15AIKA01A2): interpretation4_variableGroup: 'EffectiveMoisture' has been replaced by 'P_isotope'
d2H (LS15AIKA01A2): interpretation4_variableGroupDirection: 'negative' has been replaced by 'positive'
d2H (LS15AIKA01A2): interpretation4_variableGroupOriginal: 'precipitation amount' has been replaced by ''
d2H (LS15AIKA01A2): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS15AIKA01A2): interpretation5_basis: '' has been replaced by 'Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of winter snowmelt (relative to total water used by plants) would result in lower deltaD values.'
d2H (LS15AIKA01A2): interpretation5_direction: '' has been replaced by 'negative'
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d2H (LS15AIKA01A2): interpretation5_rank: '' has been replaced by '2'
d2H (LS15AIKA01A2): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS15AIKA01A2): interpretation5_seasonality: '' has been replaced by 'Winter'
d2H (LS15AIKA01A2): interpretation5_variable: '' has been replaced by 'precipitation'
d2H (LS15AIKA01A2): interpretation5_variableGroup: '' has been replaced by 'winter snow melting during growing season'
d2H (LS15AIKA01A2): interpretation6_basis: '' has been replaced by 'This amount effect lowers the summer precipitation isotopic com- position, dampens the seasonality of the mean precipitation of isotopic values and lowers the integrated annual precip- itation isotopic composition. Hence, in drier years average ?D values will be D-enriched relative to wetter years, and likewise warmer years will be D-enriched relative to colder years (Fig. 4b). Given the low precipitation amounts in this arid region today, the amount effect is likely to remain sec-ondary to the temperature controls on isotopic composition apparent in the seasonal cycle.'
d2H (LS15AIKA01A2): interpretation6_direction: '' has been replaced by 'negative'
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d2H (LS15AIKA01A2): interpretation6_variable: '' has been replaced by 'precipitation'
d2H (LS15AIKA01A2): interpretation6_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS15AIKA01A2): interpretation6_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS15AIKA01A2): interpretation6_variableGroupOriginal: '' has been replaced by 'precipitation amount'
d2H (LS15AIKA01B): interpretation2_basis: 'Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of growing season rainfall (relative to total water used by plants) would result in higher deltaD values.' has been replaced by ''
d2H (LS15AIKA01B): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS15AIKA01B): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS15AIKA01B): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS15AIKA01B): interpretation2_rank: '1' has been replaced by ''
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d2H (LS15AIKA01B): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS15AIKA01B): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS15AIKA01B): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS15AIKA01B): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS15AIKA01B): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS15AIKA01B): interpretation3_basis: 'Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of winter snowmelt (relative to total water used by plants) would result in lower deltaD values.' has been replaced by ''
d2H (LS15AIKA01B): interpretation3_direction: 'negative' has been replaced by ''
d2H (LS15AIKA01B): interpretation3_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS15AIKA01B): interpretation3_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS15AIKA01B): interpretation3_rank: '2' has been replaced by ''
d2H (LS15AIKA01B): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS15AIKA01B): interpretation3_seasonality: 'Winter' has been replaced by ''
d2H (LS15AIKA01B): interpretation3_variable: 'precipitation' has been replaced by ''
d2H (LS15AIKA01B): interpretation3_variableGroup: 'winter snow melting during growing season' has been replaced by ''
d2H (LS15AIKA01B): interpretation4_basis: 'This amount effect lowers the summer precipitation isotopic com- position, dampens the seasonality of the mean precipitation of isotopic values and lowers the integrated annual precip- itation isotopic composition. Hence, in drier years average ?D values will be D-enriched relative to wetter years, and likewise warmer years will be D-enriched relative to colder years (Fig. 4b). Given the low precipitation amounts in this arid region today, the amount effect is likely to remain sec-ondary to the temperature controls on isotopic composition apparent in the seasonal cycle.' has been replaced by 'Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of growing season rainfall (relative to total water used by plants) would result in higher deltaD values.'
d2H (LS15AIKA01B): interpretation4_direction: 'negative' has been replaced by 'positive'
d2H (LS15AIKA01B): interpretation4_rank: '3' has been replaced by '1'
d2H (LS15AIKA01B): interpretation4_seasonality: 'Summer' has been replaced by 'Annual'
d2H (LS15AIKA01B): interpretation4_variable: 'precipitation' has been replaced by 'precipitationIsotope'
d2H (LS15AIKA01B): interpretation4_variableGroup: 'EffectiveMoisture' has been replaced by 'P_isotope'
d2H (LS15AIKA01B): interpretation4_variableGroupDirection: 'negative' has been replaced by 'positive'
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d2H (LS15AIKA01B): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS15AIKA01B): interpretation5_basis: '' has been replaced by 'Higher isotopic values in the summer compared to the winter (Yao et al., 2013; Bowen and Revenaugh, 2003) suggest that monthly values are indeed driven by temperature. If these seasonal controls also determine interannual variations in the isotopic composition of precipitation then temperature is likely to be a major factor explaining the reconstructed hydrogen isotopic variability. A higher percentage of winter snowmelt (relative to total water used by plants) would result in lower deltaD values.'
d2H (LS15AIKA01B): interpretation5_direction: '' has been replaced by 'negative'
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d2H (LS15AIKA01B): interpretation5_seasonality: '' has been replaced by 'Winter'
d2H (LS15AIKA01B): interpretation5_variable: '' has been replaced by 'precipitation'
d2H (LS15AIKA01B): interpretation5_variableGroup: '' has been replaced by 'winter snow melting during growing season'
d2H (LS15AIKA01B): interpretation6_basis: '' has been replaced by 'This amount effect lowers the summer precipitation isotopic com- position, dampens the seasonality of the mean precipitation of isotopic values and lowers the integrated annual precip- itation isotopic composition. Hence, in drier years average ?D values will be D-enriched relative to wetter years, and likewise warmer years will be D-enriched relative to colder years (Fig. 4b). Given the low precipitation amounts in this arid region today, the amount effect is likely to remain sec-ondary to the temperature controls on isotopic composition apparent in the seasonal cycle.'
d2H (LS15AIKA01B): interpretation6_direction: '' has been replaced by 'negative'
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Updated lipdverse database entry with a changed file.
d2H (LS15AIKA01A2): interpretation1_seasonality: 'mainly growing season, with potential addition effects of snowmelt following wet winters' has been replaced by 'Growing Season'
d2H (LS15AIKA01A2): interpretation1_variable: 'Temperature and Precipitation amount' has been replaced by 'temperature'
d2H (LS15AIKA01A2): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d2H (LS15AIKA01A2): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'
d2H (LS15AIKA01A2): interpretation3_seasonality: 'winter' has been replaced by 'Winter'
d2H (LS15AIKA01A2): interpretation3_variable: 'winter snow melting during growing season' has been replaced by 'precipitation'
d2H (LS15AIKA01A2): interpretation4_seasonality: 'summer (June in modern seasonal cycle)' has been replaced by 'Summer'
d2H (LS15AIKA01A2): interpretation4_variable: 'precipitation amount' has been replaced by 'precipitation'
d2H (LS15AIKA01B): interpretation1_seasonality: 'mainly growing season, with potential addition effects of snowmelt following wet winters' has been replaced by 'Growing Season'
d2H (LS15AIKA01B): interpretation1_variable: 'Temperature and Precipitation amount' has been replaced by 'temperature'
d2H (LS15AIKA01B): interpretation2_seasonality: 'annual' has been replaced by 'Annual'
d2H (LS15AIKA01B): interpretation2_variable: 'P_isotope' has been replaced by 'precipitationIsotope'
d2H (LS15AIKA01B): interpretation3_seasonality: 'winter' has been replaced by 'Winter'
d2H (LS15AIKA01B): interpretation3_variable: 'winter snow melting during growing season' has been replaced by 'precipitation'
d2H (LS15AIKA01B): interpretation4_seasonality: 'summer (June in modern seasonal cycle)' has been replaced by 'Summer'
d2H (LS15AIKA01B): interpretation4_variable: 'precipitation amount' has been replaced by 'precipitation'
Changes made as part of LiPDverse vocabulary standardization process
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deleteThisColumn (NPM147147c): paleoData_summaryStatistic: '' has been replaced by 'average'
uncertainty1s (NPM147147d): paleoData_variableName: 'stdev weighted average' has been replaced by 'uncertainty1s'
uncertainty1s (NPM147147d): paleoData_isPrimary: '' has been replaced by 'FALSE'
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Aichner, B. , Feakins, S. J. , Lee, J. E. , Herzschuh, U. , Liu, X.
Aichner, B., Feakins, S. J., Lee, J. E., Herzschuh, U. and Liu, X.: High-resolution leaf wax carbon and hydrogen isotopic record of the late Holocene paleoclimate in arid Central Asia, Climate of the Past, 11(4), 619–633, doi:10.5194/cp-11-619-2015, 2015.
Highresolution leaf wax carbon and hydrogen isotopic record of the late Holocene paleoclimate in arid Central Asia