Mercury isotope evidence for recurrent photic-zone euxinia triggered by enhanced terrestrial nutrient inputs during the Late Devonian mass extinction

Widespread oceanic anoxia marked by globally extensive deposition of organic-rich black shale during the Late Devonian was a major factor in the mass extinctions at the Frasnian-Famennian (FFB, ∼372 million years ago) and Devonian-Carboniferous boundaries (DCB, ∼359 million years ago), although the...

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Bibliographic Details
Published inEarth and planetary science letters Vol. 613; p. 118175
Main Authors Zheng, Wang, Gilleaudeau, Geoffrey J., Algeo, Thomas J., Zhao, Yaqiu, Song, Yi, Zhang, Yuanming, Sahoo, Swapan K., Anbar, Ariel D., Carmichael, Sarah K., Xie, Shucheng, Liu, Cong-Qiang, Chen, Jiubin
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.07.2023
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