A pulse of seafloor oxygenation at the Late Devonian Frasnian-Famennian boundary in South China
Abstract
The Frasnian-Famennian (F-F) mass extinction (~372 Ma) is regarded as one of the ‘Big Five’ mass extinctions events in Phanerozoic. The F-F boundary is characterized by two positive carbonate carbon isotope (δ13Ccarb) excursions, and is coincident with the global deposition of two layers of black shale and bituminous limestone, collectively known as the Lower and Upper Kellwasser events, referring two pulses of oceanic anoxic events that might...
Paper Details
Title
A pulse of seafloor oxygenation at the Late Devonian Frasnian-Famennian boundary in South China
Published Date
Jul 1, 2021
Journal
Volume
218
Pages
103651 - 103651
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