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Highly fractionated chromium isotopes in Mesoproterozoic-aged shales and atmospheric oxygen

Donald E. Canfield (), Shuichang Zhang, Anja B. Frank, Xiaomei Wang, Huajian Wang, Jin Su, Yuntao Ye and Robert Frei
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Donald E. Canfield: China National Petroleum Corporation
Shuichang Zhang: China National Petroleum Corporation
Anja B. Frank: University of Copenhagen
Xiaomei Wang: China National Petroleum Corporation
Huajian Wang: China National Petroleum Corporation
Jin Su: China National Petroleum Corporation
Yuntao Ye: China National Petroleum Corporation
Robert Frei: University of Copenhagen

Nature Communications, 2018, vol. 9, issue 1, 1-11

Abstract: Abstract The history of atmospheric oxygen through the Mesoproterozoic Era is uncertain, but may have played a role in the timing of major evolutionary developments among eukaryotes. Previous work using chromium isotopes in sedimentary rocks has suggested that Mesoproterozoic Era atmospheric oxygen levels were too low in concentration ( 1% PAL and thus the possibility that a permissive environment existed long before the expansion of various eukaryotic clades.

Date: 2018
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DOI: 10.1038/s41467-018-05263-9

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