(Supplementary Table 1) 230Th/U results for stalagmite Cuba Grande (CG) from Pinar del Rio

Fensterer, Claudia;Scholz, Denis;Hoffmann, Dirk L;Mangini, Augusto;Pajon, Jesus M

Description

We present 22 U-series ages for a stalagmite from north-western Cuba based on multi-collector inductively coupled plasma mass spectrometry (MC-ICPMS) and thermal ionisation mass spectrometry (TIMS). Our results reveal that the stalagmite continuously grew within the last ~1400a. Low uranium content of the sample and thus, extremely low 230Th concentrations limit the precision and accuracy of 230Th/U-dating by TIMS. Samples measured by MC-ICPMS show a high variability of 232Th content along the growth axis with some sections significantly affected by initial 230Th from a detrital phase. An a-priori bulk earth ratio for (238U/232Th) cannot be used to accurately account for this initial 230Th. Using an age model based on the 230Th/U ages determined on samples with low or negligible 232Th concentration, we find that the (238U/232Th) activity ratio of the detrital phase is an order of magnitude larger than the bulk earth value, indicating the importance of an accurately determined correction factor.

Citations (0)

Mentions (0)

Metrics

Dataset Index

0.8

FAIR Score

92%

Citations

1

Mentions

0

Metrics Over Time

Publication Details

DOI

Publisher

PANGAEA

License

Creative Commons Attribution 3.0 Unported

Assigned Domain

Subfield

Pollution

Field

Environmental Science

Domain

Physical Sciences

Confidence Score

42%

Source

Scholar Data Model

Keywords

DISTANCEUranium-238Uranium-238, standard deviationThorium-232Thorium-232, standard deviationThorium-230/Thorium-232 activity ratioThorium-230/Thorium-232 activity ratio, standard deviationThorium-230/Uranium-238 ratioThorium-230/Uranium-238 activity ratio, standard deviationUranium-234/Uranium-238 activity ratioUranium-234, standard deviationAge, datedAge, dated, standard deviationAge, commentSpeleothem sampleMulti-collector inductively coupled plasma mass spectrometer (MC-ICP-MS)Integrierte Analyse zwischeneiszeitlicher Klimadynamik (INTERDYNAMIK)

Normalization Factors

FT

65.38

CTw

1.00

MTw

1.00