Title : A major sea-level drop briefly precedes the Toarcian oceanic anoxic event: implication for Early Jurassic climate and carbon cycle.

Pub. Date : 2019 Aug 29

PMID : 31467345






1 Functional Relationships(s)
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1 Indeed, during the deglaciation and the accompanying sea-level rise, the thawing permafrost may have released important quantities of methane into the atmosphere that would have contributed to the Toarcian OAE rapid warming and its characteristic negative carbon isotope excursion. Methane S13 erythroblastosis (avian) oncogene homolog Homo sapiens