δ¹⁸Osw benthic-corrected on planktonic foraminifera of sediment core MD01-2378

DOI

AGE follows the GICC05 time scale. To estimate changes of d18Osw of the sea surface and upper thermocline water, we used paired G. ruber and P. obliquiloculata Mg/Ca temperatures and stable isotopes and calculated the d18Osw using the equation of Bemis et al. (1998, doi:10.1029/98PA00070). The ice volume effect was corrected using the benthic d18Osw from the same core.

Identifier
DOI https://doi.org/10.1594/PANGAEA.712514
Related Identifier https://doi.org/10.1594/PANGAEA.712515
Related Identifier https://doi.org/10.1029/2008PA001653
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.712514
Provenance
Creator Zuraida, Rina; Holbourn, Ann E ORCID logo; Nürnberg, Dirk; Kuhnt, Wolfgang; Dürkop, Anke; Erichsen, A
Publisher PANGAEA
Publication Year 2009
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 1323 data points
Discipline Earth System Research
Spatial Coverage (121.788 LON, -13.082 LAT); Timor Sea