Climate cycling on early Mars caused by the carbonate-silicate cycle
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文摘

A cold early Mars was warmed episodically for ∼10 Myr at a time by an H2–CO2 greenhouse.

Volcanic outgassing rates comparable to those on modern Earth are required.

High H2 outgassing rates are consistent with evidence for a highly reduced martian mantle.

Our hypothesis can be tested by better establishing the time scale for valley formation.

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