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


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).

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Metadata Access
Creator Yang, Xiaoqiang; Su, Zhihua; Wei, Gangjian ; Zhang, Tingwei ; Chen, Qiong
Publisher PANGAEA
Publication Year 2023
Rights Data access is restricted (moratorium, sensitive data, license constraints)
OpenAccess false
Language English
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