Dole effect in the north of the South China Sea from sediment core PC27 and PC83

DOI

Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM.Dole effect was calculated following the method (delta18Oatm - delta18Osurf) of Huang et al. (2020; doi:10.1126/sciadv.aba4823) and Extier et al. (2018; doi:10.1016/j.quascirev.2018.02.008).

Identifier
DOI https://doi.org/10.1594/PANGAEA.952524
Related Identifier IsPartOf https://doi.org/10.1594/PANGAEA.952540
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.952524
Provenance
Creator Yang, Xiaoqiang; Su, Zhihua; Wei, Gangjian ORCID logo; Zhang, Tingwei ORCID logo; Chen, Qiong ORCID logo
Publisher PANGAEA
Publication Year 2024
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 667 data points
Discipline Earth System Research
Spatial Coverage (112.544W, 16.615S, 113.389E, 17.659N); South China Sea