A weathering hypothesis for glaciation at high atmospheric pCO2 during the Late Ordovician-Reference-Cited by-同舟云学术

A weathering hypothesis for glaciation at high atmospheric pCO2 during the Late Ordovician

Published:1999-08 Issue:1-2 Volume:152 Page:173-187
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Kump L.R,Arthur M.A,Patzkowsky M.E,Gibbs M.T,Pinkus D.S,Sheehan P.M

Publisher

Elsevier BV

Subject

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

Reference73 articles.

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3. Anomalous 13C enrichment in modern marine organic carbon;Arthur;Nature,1985

4. Geochemical and climatic effects of increased marine organic carbon burial at the Cenomanian/Turonian boundary;Arthur;Nature,1988

5. Oxygen and carbon isotopic composition of Silurian brachiopods: implications for coeval seawater and glaciations;Azmy;Geol. Soc. Am. Bull.,1998

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