The Magnitude and Duration of Late Ordovician–Early Silurian Glaciation-Reference-Cited by-同舟云学术

The Magnitude and Duration of Late Ordovician–Early Silurian Glaciation

Published:2011-02-18 Issue:6019 Volume:331 Page:903-906
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Finnegan Seth¹,Bergmann Kristin¹,Eiler John M.¹,Jones David S.²,Fike David A.²,Eisenman Ian¹³,Hughes Nigel C.⁴,Tripati Aradhna K.¹⁵,Fischer Woodward W.¹

Affiliation:

1. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.

2. Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA.

3. Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195, USA.

4. Department of Earth Sciences, University of California, Riverside, CA 92521, USA.

5. Department of Earth and Space Sciences and Department of Atmospheric and Oceanic Sciences, Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA 90095, USA.

Abstract

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

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference28 articles.

1. L. A. Frakes J. E. Francis J. I. Syktus Climate Modes of the Phanerozoic (Cambridge Univ. Press Cambridge 1996).

2. Ice and Its Consequences: Glaciation in the Late Ordovician, Late Devonian, Pennsylvanian‐Permian, and Cenozoic Compared

3. GEOCARBSULF: A combined model for Phanerozoic atmospheric O2 and CO2

4. The Late Ordovician Mass Extinction

5. Bathymetric and isotopic evidence for a short-lived Late Ordovician glaciation in a greenhouse period

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