The large increase of δ 13Ccarb-depth gradient and the end-Permian mass extinction
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Title
The large increase of δ 13Ccarb-depth gradient and the end-Permian mass extinction
Authors
Keywords
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Journal
Science China-Earth Sciences
Volume 55, Issue 7, Pages 1101-1109
Publisher
Springer Nature
Online
2012-05-19
DOI
10.1007/s11430-012-4416-1
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Note: Only part of the references are listed.- δ13C evidence that high primary productivity delayed recovery from end-Permian mass extinction
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- Multiple S-isotopic evidence for episodic shoaling of anoxic water during Late Permian mass extinction
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- Pattern of δ13Ccarb and implications for geological events during the Permian-Triassic transition in South China
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- Possible causes for a negative shift in the stable carbon isotope ratio before, during and after the end-Permian mass extinction in Meishan, South China
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- Evidence from ammonoids and conodonts for multiple Early Triassic mass extinctions
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- Good Genes and Good Luck: Ammonoid Diversity and the End-Permian Mass Extinction
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- Ecological evolution across the Permian/Triassic boundary at the Kangjiaping Section in Cili County, Hunan Province, China
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- High-resolution carbon isotope changes in the Permian–Triassic boundary interval, Chongqing, South China; implications for control and growth of earliest Triassic microbialites
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