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
- 1 August 1997
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 132 (1-4) , 147-158
- https://doi.org/10.1016/s0031-0182(97)00046-1
Abstract
No abstract availableKeywords
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