13 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
2. Simulation of early Eocene water isotopes using an Earth system model and its implication for past climate reconstruction J. Zhu et al. 10.1016/j.epsl.2020.116164
3. Late Eocene onset of the Proto-Antarctic Circumpolar Current S. Sarkar et al. 10.1038/s41598-019-46253-1
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. Expanded subsurface ocean anoxia in the Atlantic during the Paleocene-Eocene Thermal Maximum W. Yao et al. 10.1038/s41467-024-53423-x
10. 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
11. Are Clay Minerals the Primary Control on the Oceanic Rare Earth Element Budget? A. Abbott et al. 10.3389/fmars.2019.00504
12. Early Eocene vigorous ocean overturning and its contribution to a warm Southern Ocean Y. Zhang et al. 10.5194/cp-16-1263-2020
13. Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth S. Batenburg et al. 10.1038/s41467-018-07457-7