Xue-Ting Wang , Yibo Yang , Daniel E. Ibarra , Xiaobai Ruan , Zhongyi Yan , Jimin Sun , Chun-Sheng Jin
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引用次数: 0
Abstract
The Oligocene features a long-term decrease in atmospheric CO2 levels (pCO2). However, the driving force of the Oligocene pCO2 drawdown remains uncertain. Here, we examine the response of silicate chemical weathering to the Oligocene Asian monsoon enhancement in the tectonically active Tibetan Plateau. On tectonic timescales, the silicate weathering rate is elevated in high-weatherability catchments caused by intensive erosion. On orbital timescales, the degree of silicate alteration displays 405-kyr eccentricity cycles, with amplified oscillations corresponding to a vigorous hydrological cycle. Our geologic records, for the first time, reveal that the strength of silicate weathering feedback and CO2 consumption have increased in a setting of high land surface weatherability. Given the increase in global erosion rate during the Oligocene, the consequent increase in land surface weatherability and weathering feedback strength may modulate the pCO2 decrease.
期刊介绍:
Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.