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Published in 2021 at "Paleoceanography and Paleoclimatology"
DOI: 10.1029/2020pa004207
Abstract: The worldwide recognition of the Toarcian carbon isotope excursion (T‐CIE) in organic‐rich sedimentary rocks has been linked to an oceanic anoxic event (OAE) which implies the world's deep oceans were anoxic ∼183 Ma. The majority…
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Keywords:
toarcian carbon;
shelf;
epicontinental shelf;
northern european ... See more keywords