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Abstract

Detailed investigations of the carbon, oxygen and sulphur cycles using a range of proxies, including leaf pore stomata, δ13C, δ34S, and 87/86Sr isotopes, as well as geochemical mass balance modeling, provide detailed evidence of major trends as well as distinct events in the atmosphere-ocean-land system during the Paleozoic and Mesozoic eras (542–65 Ma), including greenhouse Earth periods (CO2 ~2,000–5,000 ppm) and glacial phases (CO2 < 500 ppm), with implications for biological evolution.

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Correspondence to Andrew Y. Glikson .

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Glikson, A.Y. (2014). Palaeozoic and Mesozoic Atmospheres. In: Evolution of the Atmosphere, Fire and the Anthropocene Climate Event Horizon. SpringerBriefs in Earth Sciences. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-7332-5_2

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