Reconciling Late Ordovician (440 Ma) glaciation with very high (14X) CO2 levels
Open Access
- 20 January 1995
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 100 (D1), 1093-1101
- https://doi.org/10.1029/94jd02521
Abstract
No abstract availableKeywords
This publication has 44 references indexed in Scilit:
- Life on Land in the PrecambrianScience, 1994
- Geological Assessment of the Greenhouse EffectBulletin of the American Meteorological Society, 1993
- Past climate and the role of ocean heat transport: Model simulations for the CretaceousPaleoceanography and Paleoclimatology, 1993
- Palaeo-CO2 and climateNature, 1992
- Fractionation of carbon isotopes by phytoplankton and estimates of ancient CO2 levelsGlobal Biogeochemical Cycles, 1992
- Ancient atmospheric C02 pressures inferred from natural goethitesNature, 1992
- History of atmospheric CO2: Constraints from the deep‐sea recordPaleoceanography and Paleoclimatology, 1988
- Migration of glacial centers across Gondwana during Paleozoic EraGSA Bulletin, 1985
- Rotation in solar-type stars. I - Evolutionary models for the spin-down of the sunThe Astrophysical Journal, 1981
- Tentative Paleocontinental Maps for the Early Phanerozoic and ProterozoicThe Journal of Geology, 1978