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• W2000935538 abstract "The Paleozoic stands out in geochemical reconstructions as a time of unusually high organic carbon burial and disturbed O2 and CO2 regimes. The anomaly is apparently of terrestrial origin. Evidence and explanations for reconstructed trends are sought in the terrestrial record. The correspondence between reconstructed O2 and fusinite abundance in coal, a possible proxy for charcoal formation and fire activity, is ambiguous due to problems of data quality and interpretation. Patterns in Silurian, Devonian, and Carboniferous plant evolution are consistent with stress imposed by progressive CO2 starvation followed by leveling out, as predicted in reconstructions. I hypothesize that the Paleozoic disturbance was caused by bottlenecks in the cycling of lignin and other refractory compounds synthesized by land plants, and that these bottlenecks were eventually reduced by the evolution of more effective decomposer organisms and/or reduction of the refractory fraction in land plant biomass." @default.
• W2000935538 created "2016-06-24" @default.
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• W2000935538 date "1991-12-01" @default.
• W2000935538 modified "2023-09-24" @default.
• W2000935538 title "Phanerozoic atmospheric reconstructions: a terrestrial perspective" @default.
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• W2000935538 doi "https://doi.org/10.1016/0031-0182(91)90181-p" @default.
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