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
Laboratory precision on the d18O measurement
Laboratory precision on the d13C measurement
Original published calibrated age of the sample in years BP
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
Percentage dead carbon present in dated sample
Calibration method used to convert C14 dates to calendar years
Indication of whether the date is used in the original age model (opposite of rejected)
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
The ages between detph_dating = 3.4mm and depth_dating = 19.65 mm in entity BNT-2 (entity_id = 613) were obtained by fitting the measured pMC values to the IntCal13 (Reimer et al., 2013) dataset. This approach defined the 5% dead carbon applied in deeper sections. See publication for details.
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Changes made as part of LiPDverse vocabulary standardization process
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correction (S2LRzHz3Fqtkfm): paleoData_method: '' has been replaced by 'aragonite correction'
d13CPrecision (S2LR3bPOohgdQg): interpretation1_scope: '' has been replaced by 'climate'
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hasHiatus (S2LRewoh7hTVZF): interpretation1_scope: '' has been replaced by 'climate'
thickness (S2LRHnCpXwaOte): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LRpygiGQER5N): interpretation1_scope: '' has been replaced by 'climate'
d13CStandard (S2LRQgc6nTz4nX): interpretation1_scope: '' has been replaced by 'climate'
mineralogy (S2LRW5ugWY4pbp): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LRY0jnjYbp2i): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LRzHz3Fqtkfm): interpretation1_scope: '' has been replaced by 'climate'
Dem<e9>ny, A., Kern, Z., N<e9>meth, A., Frisia, S., Hatvani, I. G., Czuppon, G., Le<e9>l-?ssy, S., Moln<e1>r, M., <d3>v<e1>ri, M., Sur<e1>nyi, G., Gilli, A., Wu, C.-C. and Shen, C.-C.: North Atlantic influences on climate conditions in East-Central Europe in the late Holocene reflected by flowstone compositions, Quat. Int., 512, 99<96>112, 2019.
Czuppon, G., Dem<e9>ny, A., Le<e9>l-?ssy, S., <d3>vari, M., Moln<e1>r, M., Stieber, J., Kiss, K., K<e1>rm<e1>n, K., Sur<e1>nyi, G. and Haszpra, L.: Cave monitoring in the B<e9>ke and Baradla caves (Northeastern Hungary): implications for the conditions for the formation cave carbonates, Int. J. Speleol., 47(1), 13<96>28, 2018.