Dole effect in the north of the South China Sea from sediment core PC27 and PC83
收藏DataCite Commons2026-05-01 更新2026-05-04 收录
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https://doi.pangaea.de/10.1594/PANGAEA.952524
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资源简介：
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).
提供机构：
PANGAEA
创建时间：
2025-01-28
