Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM
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The Paleocene-Eocene Thermal Maximum (PETM) is recognized globally by a negative excursion in stable carbon isotope ratios (δ13C) in sedimentary records, termed the carbon isotope excursion (CIE). Based on the CIE, the cause, duration, and mechanisms of recov... ...
