Biology, 06.12.2020 08:20, sean7900

Global cooling across the Eocene-Oligocene transition is hypothesized to be driven by

(a)removal of CO2 from the atmosphere through enhanced weathering

(B)Tectonic reorganizations, establishment of a new circumpolar ocean current, and
glaciation of Antarctica

(C)decrease in global volcanism associated with lower atmospheric CO2 levels

(D)O destabilization of methane hydrates

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Global cooling across the Eocene-Oligocene transition is hypothesized to be driven by

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