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The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

Oceanic Anoxia and the End Permian Mass Extinction

Wignall, Paul B., Twitchett, Richard J.·1996·Science
DOI 10.1126/science.272.5265.1155
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Abstract

Data on rocks from Spitsbergen and the equatorial sections of Italy and Slovenia indicate that the world's oceans became anoxic at both low and high paleolatitudes in the Late Permian. Such conditions may have been responsible for the mass extinction at this time. This event affected a wide range of shelf depths and extended into shallow water well above the storm wave base.

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Citations

Cites

Show all 1 references

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Metadata

Authors
Wignall, P. B., & Twitchett, R. J.
Venue
Science
Publisher
American Association for the Advancement of Science (AAAS)
Published
1996-05-24
Volume
272
Issue
5265
Pages
1155-1158
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
DOI
10.1126/science.272.5265.1155
OpenAlex
W1994510458
Cited by
1,196
References
1
FWCI
15.88
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Oceanic Anoxia and the End Permian Mass Extinction. https://app.cochat.ai/papers/10.1126/science.272.5265.1155
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Wignall, P. B., & Twitchett, R. J. (1996). Oceanic Anoxia and the End Permian Mass Extinction. Science. https://doi.org/10.1126/science.272.5265.1155

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.