Carbon(C)sequestered in the mantle andcrust over geological timescales accounts for more than 99% of allcarbon in the bulk silicate Earth and plays a fundamental role in driving surface biogeochemical cycles,which inv...Carbon(C)sequestered in the mantle andcrust over geological timescales accounts for more than 99% of allcarbon in the bulk silicate Earth and plays a fundamental role in driving surface biogeochemical cycles,which involve only a tiny fraction of Earth's total carbon inventory[1].In addition to CO_(2) released through near surface weathering of sedimentary rocks[2],a substantial,butstill poorly quantified,amount of carbon in the deeper crust and mantle(hereafter referred to as deeply-sourced carbon)could be mobilized by magmatism and metamorphism and then outgassed in volcanic and non-volcanic settings.展开更多
基金supported by the National Key Research and Development Program of China(2020YFA0607700)the National Natural Science Foundation of China(41930642 and 42522211).
文摘Carbon(C)sequestered in the mantle andcrust over geological timescales accounts for more than 99% of allcarbon in the bulk silicate Earth and plays a fundamental role in driving surface biogeochemical cycles,which involve only a tiny fraction of Earth's total carbon inventory[1].In addition to CO_(2) released through near surface weathering of sedimentary rocks[2],a substantial,butstill poorly quantified,amount of carbon in the deeper crust and mantle(hereafter referred to as deeply-sourced carbon)could be mobilized by magmatism and metamorphism and then outgassed in volcanic and non-volcanic settings.
