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The Magnitude and Duration of Late Ordovician–Early Silurian Glaciation

Finnegan, Seth, Bergmann, Kristin, Eiler, John M., Jones, David S., Fike, David A., Eisenman, Ian, Hughes, Nigel C., Tripati, Aradhna K., Fischer, Woodward W.·2011·Science

DOI 10.1126/science.1200803

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Carbonate isotopes reveal a link between past ocean temperatures and mass extinction.

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Background
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Authors: Finnegan, S., Bergmann, K., Eiler, J. M., Jones, D. S., Fike, D. A., Eisenman, I., Hughes, N. C., Tripati, A. K., & Fischer, W. W.
Venue: Science
Publisher: American Association for the Advancement of Science (AAAS)
Published: 2011-02-18
Volume: 331
Issue: 6019
Pages: 903-906
ISSN: 0036-8075 (ISSN-L)
1095-9203
DOI: 10.1126/science.1200803
OpenAlex: W2156426644
Cited by: 573
References: 3
FWCI: 21.67
Type: journal article
Language: en
Open access: closed

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The Magnitude and Duration of Late Ordovician–Early Silurian Glaciation

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