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Palaeoclimate

CO2 and late Palaeozoic glaciation

Large glacial–interglacial fluctuations occurred during the late Palaeozoic. Geochemical and fossil data show these cycles were marked by coincident shifts in the carbon cycle and terrestrial biosphere.

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Figure 1: Phanerozoic climate and atmospheric composition.

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Correspondence to Timothy S. Myers.

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Myers, T. CO2 and late Palaeozoic glaciation. Nature Geosci 9, 803–804 (2016). https://doi.org/10.1038/ngeo2832

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