10.1594/PANGAEA.948457Løland, Marit HoltenMarit HoltenLøland0000-0002-0721-7574Krüger, YvesYvesKrügerFernandez, AlvaroAlvaroFernandez0000-0003-4765-707XBuckingham, FrancesFrancesBuckingham0000-0001-5793-9121Carolin, Stacy AStacy ACarolin0000-0001-7181-2370Sodemann, HaraldHaraldSodemann0000-0002-8167-0860Adkins, Jess FJess FAdkins0000-0002-3174-5190Cobb, Kim MKim MCobb0000-0002-2125-9164Meckler, Anna NeleAnna NeleMeckler0000-0002-7225-8276PANGAEA2022BorneoDeglaciationFluid inclusionfluid inclusion microthermometryHolocenelast glacial terminationLGMspeleothemstalagmiteTemperaturetropicsDistance, relative, XSample IDTemperature, caveTemperature, cave, standard errorTemperature, correctedTemperature, corrected, standard errorCalendar ageCalendar age, maximum/oldCalendar age, minimum/youngSea levelSea level, standard deviationδ18O, calciteδ18O, waterδ18O, water, standard errorSpeleothem sampleFluid inclusion microthermometryMonte CarloAge, 14C calibration OxCal (Ramsey, 1995)ReconstructedIsotope ratio mass spectrometerDataset10.1038/s41467-022-32712-310.1029/2021GL09693710.1016/j.chemgeo.2011.07.00910.1073/pnas.1411762111302 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalThis 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.114.8334.063Borneo, MalaysiaEuropean Research Councilhttps://doi.org/10.13039/501100000781101001957The Research Council of Norwayhttps://doi.org/10.13039/501100005416262353/F20