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• W2959837154 abstract "Abstract Over geological timescales, mountain building or orogenesis is associated with increased weathering, the drawdown of atmospheric CO 2 , and global cooling. However, a multimillion‐year delay appears to exist between peaks in low‐latitude mountain uplift and the maximum extent of Phanerozoic glaciation, implying a more complex causal relationship between the two. Here we show that global silicate weathering can be modulated by orogeny in three distinct phases. High, young mountain belts experience preferential precipitation and the highest erosion. As mountains are denuded, precipitation decreases, but runoff temperature rises, sharply increasing chemical weathering potential and CO 2 drawdown. In the final phase, erosion and weathering are throttled by flatter topography. We conclude that orogeny acts as a capacitor in the climate system, granting the potential for intense transient CO 2 drawdown when mountain ranges are denuded; the mechanism suggests such a scenario potentially happening 10–50 × 10 6 years in the future." @default.
• W2959837154 created "2019-07-23" @default.
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• W2959837154 date "2019-07-26" @default.
• W2959837154 modified "2023-09-25" @default.
• W2959837154 title "A Capacitor‐Discharge Mechanism to Explain the Timing of Orogeny‐Related Global Glaciations" @default.
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• W2959837154 doi "https://doi.org/10.1029/2019gl083368" @default.
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