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- W4241133814 abstract "The history of atmospheric carbon dioxide on Earth began with the release of the gas from beneath the surface of the newly formed planet. The concentration of pCO2 remained extremely high from Precambrian times to at least the Devonian Period, perpetuated by the release of extremely large amounts of CO2 through plate tectonic processes and associated subduction and volcanism. Following a peak of atmospheric CO2 of 3000 ppm at about 440 mya, there was a sharp decline associated with a drop in global temperatures during the late Carboniferous and through much of the Permian. This was followed by a rapid rise in CO2 at the Permian-Triassic boundary, brought on by massive volcanic eruptions in Siberia. Atmospheric CO2 rose from about 500–600 ppm in the Early Triassic period to a peak of about 1100 ppm in the Cretaceous, although each of the Cretaceous CO2 proxies tells a different story. There was a general decline in pCO2 levels throughout the Cenozoic, with some notable exceptions. The Paleocene—Eocene transition, about 56 mya, was marked by rapid, large-scale warming. Some authors however consider that the major Miocene climatic changes were in fact driven by orbital forcing." @default.
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- W4241133814 date "2021-01-01" @default.
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- W4241133814 title "History of Greenhouse Gas Warming: CO2" @default.
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- W4241133814 doi "https://doi.org/10.1016/b978-0-08-102908-4.00019-9" @default.
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