Publication Date:
2024-03-25
Description:
This dataset presents cave temperatures over the last glacial termination from stalagmite SC02 from Secret Cave in Mulu, Northern Borneo (4.063°N, 114.833°E). The temperatures are derived by the means of fluid inclusion microthermometry and published in Løland et al., (2022). The study shows that the cave temperature increased by 4.4 ± 0.3 °C (2 SEM) from the Last Glacial Maximum to the Holocene, amounting to 3.6 ± 0.3 °C (2 SEM) when correcting for sea-level induced cave altitude change. Included in the dataset are also the calculated dripwater delta-18O values.
Keywords:
Age, 14C calibration OxCal (Ramsey, 1995); Borneo; Borneo, Malaysia; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Deglaciation; Distance, relative, X; fluid inclusion; fluid inclusion microthermometry; Fluid inclusion microthermometry; Holocene; IRMS; Isotope ratio mass spectrometer; last glacial termination; LGM; Monte Carlo; Reconstructed; Sample ID; SC02_Secret_cave; Sea level; Sea level, standard deviation; speleothem; Speleothem sample; SPS; stalagmite; Temperature; Temperature, cave; Temperature, cave, standard error; Temperature, corrected; Temperature, corrected, standard error; tropics; δ18O, calcite; δ18O, water; δ18O, water, standard error
Type:
Dataset
Format:
text/tab-separated-values, 302 data points
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