An organic carbon isotope record of Late Ordovician to Early Silurian marine sedimentary rocks, Yangtze Sea, South China: Implications for CO2 changes during the Hirnantian glaciation-Reference-Cited by-同舟云学术

An organic carbon isotope record of Late Ordovician to Early Silurian marine sedimentary rocks, Yangtze Sea, South China: Implications for CO2 changes during the Hirnantian glaciation

Published:1997-08 Issue:1-4 Volume:132 Page:147-158
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Wang K,Chatterton B.D.E,Wang Y

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference46 articles.

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4. Brenchley, P.J., 1989. The late Ordovician extinction. In: Donovan, S.K. (Ed.), Mass Extinctions: Processes and Evidence. Columbia Univ. Press, New York, pp. 104–132.

5. Bathymetric and isotopic evidence for a short-lived Late Ordovician glaciation in a greenhouse period;Brenchley;Geology,1994

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