Global carbon isotopic events associated with mass extinction and glaciation in the late Ordovician
- 1 August 1997
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 132 (1-4) , 195-210
- https://doi.org/10.1016/s0031-0182(97)00063-1
Abstract
No abstract availableThis publication has 16 references indexed in Scilit:
- The great latest Ordovician extinction on the South China Plate: Chemostratigraphic studies of the Ordovician-Silurian boundary interval on the Yangtze platformPublished by Elsevier ,2003
- Organic carbon δ13C variations in sedimentary rocks as chemostratigraphic and paleoenvironmental toolsPalaeogeography, Palaeoclimatology, Palaeoecology, 1997
- 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 glaciationPalaeogeography, Palaeoclimatology, Palaeoecology, 1997
- Oxygen and carbon isotopic composition of Ordovician brachiopods: Implications for coeval seawaterGeochimica et Cosmochimica Acta, 1994
- Oxygen and carbon isotopes and event stratigraphy near the Ordovician—Silurian boundary, Anticosti Island QuebecPalaeogeography, Palaeoclimatology, Palaeoecology, 1993
- Climatic and oceanographic isotopic signals from the carbonate rock record and their preservationGeological Magazine, 1992
- Revised World maps and introductionGeological Society, London, Memoirs, 1990
- Changes in marine isotopic composition and the late Ordovician glaciationJournal of the Geological Society, 1990
- The late Ordovician—Early Silurian glacial periodPalaeogeography, Palaeoclimatology, Palaeoecology, 1985
- Chemical Fossils: The Geological Fate of SteroidsScience, 1982