Borneo stalagmite SC02 temperature reconstructions over Termination I by the means of fluid inclusion microthermometry

DOI

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.

Identifier
DOI https://doi.org/10.1594/PANGAEA.948457
Related Identifier https://doi.org/10.1038/s41467-022-32712-3
Related Identifier https://doi.org/10.1029/2021GL096937
Related Identifier https://doi.org/10.1016/j.chemgeo.2011.07.009
Related Identifier https://doi.org/10.1073/pnas.1411762111
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.948457
Provenance
Creator Løland, Marit Holten ORCID logo; Krüger, Yves; Fernandez, Alvaro (ORCID: 0000-0003-4765-707X); Buckingham, Frances ORCID logo; Carolin, Stacy A ORCID logo; Sodemann, Harald ORCID logo; Adkins, Jess F ORCID logo; Cobb, Kim M ORCID logo; Meckler, Anna Nele ORCID logo
Publisher PANGAEA
Publication Year 2022
Funding Reference European Research Council https://doi.org/10.13039/501100000781 Crossref Funder ID 101001957 ; The Research Council of Norway https://doi.org/10.13039/501100005416 Crossref Funder ID 262353/F20
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 302 data points
Discipline Earth System Research
Spatial Coverage (114.833 LON, 4.063 LAT); Borneo, Malaysia