The seawater carbon inventory at the Paleocene–Eocene Thermal Maximum

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Rapid and sustained surface ocean acidification during the PaleoceneEocene Thermal Maximum

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Evidence for a rapid release of carbon at the Paleocene-Eocene thermal maximum.

The Paleocene/Eocene thermal maximum (PETM) and associated carbon isotope excursion (CIE) are often touted as the best geologic analog for the current anthropogenic rise in pCO2. However, a causal mechanism for the PETM CIE remains unidentified because of large uncertainties in the duration of the CIE's onset. Here, we report on a sequence of rhythmic sedimentary couplets comprising the Paleoce...

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Onset of carbon isotope excursion at the Paleocene-Eocene thermal maximum took millennia, not 13 years.

The Paleocene-Eocene thermal maximum (PETM) may represent the best paleo-analog for rapid and massive carbon release to the ocean and atmosphere. Thus, constraining the carbon release rate at its onset is critical. Wright and Schaller (1) use records from apparently rhythmically layered shelf sediments to argue that the layering is annual and that the onset of the carbon isotope excursion (CIE,...

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ژورنال

عنوان ژورنال: Proceedings of the National Academy of Sciences

سال: 2020

ISSN: 0027-8424,1091-6490

DOI: 10.1073/pnas.2003197117