理解全地球碳循环的框架

Deep Carbon Pub Date : 2019-10-01 DOI:10.1017/9781108677950.011

Cin-Ty A. Lee, Hehe Jiang, R. Dasgupta, M. Torres

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引用次数: 38

摘要

增加了全球风化反馈(状态a到b)的敏感性，从而缓冲了pco2的上升。岩浆活动结束后，物理和化学风化作用持续存在，使pco2降至较低水平。岩浆造山带可以潜在地驱动温室，但由于长期的风化作用，随之而来的是全球变冷。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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A Framework for Understanding Whole-Earth Carbon Cycling

increasing the sensitivity of the global weathering feedback (states a to b), which buffers the rise of pCO 2 . After magmatism ends, physical and chemical weathering persist, driving pCO 2 to low levels. Magmatic orogens can potentially drive greenhouses, but are followed by global cooling due to protracted weathering.

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Deep Carbon

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