Synchronous change in the carbon isotopes, large benthic foraminifera and sea-level recorded in shallow-water carbonate platforms across the Paleocene-Eocene thermal maximum

Juan Li1, Hu Xiumian1, James C Zachos2, Naroa Braceras3 and Aitor Payros3, (1)Nanjing University, School of Earth Sciences and Engineering, Nanjing, China, (2)Univ California Santa Cruz, Santa Cruz, CA, United States, (3)University of the Basque Country, Bilbao, Spain
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