Response of Late Ordovician paleoceanography to changes in sea level, continental drift, and atmospheric pCO2: potential causes for long-term cooling and glaciation
- 1 August 2004
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 210 (2-4) , 385-401
- https://doi.org/10.1016/j.palaeo.2004.02.034
Abstract
No abstract availableKeywords
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