12 citations as recorded by crossref.

1. Investigating Ocean Deoxygenation During the PETM Through the Cr Isotopic Signature of Foraminifera S. Remmelzwaal et al. 10.1029/2018PA003372
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4. Potential Role of Mid‐Latitude Seaway on Early Paleogene Atlantic Overturning Circulation C. Zhu et al. 10.1029/2023GL102794
5. An alternative model for CaCO3 over-shooting during the PETM: Biological carbonate compensation Y. Luo et al. 10.1016/j.epsl.2016.08.012
6. Projected reversal of oceanic stable carbon isotope ratio depth gradient with continued anthropogenic carbon emissions E. Kwon et al. 10.1038/s43247-022-00388-8
7. Review: Ocean acidification during the Paleocene-Eocene Thermal Maximum T. Yamaguchi et al. 10.5575/geosoc.2022.0056
8. Abrupt Northwest Atlantic deep-sea oxygenation decline preceded the Palaeocene-Eocene Thermal Maximum P. Xue et al. 10.1016/j.epsl.2023.118304
9. Nd isotopic structure of the Pacific Ocean 40–10 Ma, and evidence for the reorganization of deep North Pacific Ocean circulation between 36 and 25 Ma C. McKinley et al. 10.1016/j.epsl.2019.06.009
10. Are Clay Minerals the Primary Control on the Oceanic Rare Earth Element Budget? A. Abbott et al. 10.3389/fmars.2019.00504
11. Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean Y. Zhang et al. 10.5194/cp-16-1263-2020
12. Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth S. Batenburg et al. 10.1038/s41467-018-07457-7