Subducting carbon

被引:351
|
作者
Plank, Terry [1 ]
Manning, Craig E. [2 ]
机构
[1] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
[2] Univ Calif Los Angeles, Los Angeles, CA USA
关键词
OCEANIC-CRUST; UPPER-MANTLE; METAMORPHIC DEVOLATILIZATION; VOLATILE CYCLES; MELT INCLUSIONS; ARC VARIATIONS; VOLCANIC ARC; ZONE MAGMAS; ALONG-ARC; SEA-FLOOR;
D O I
10.1038/s41586-019-1643-z
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A hidden carbon cycle exists inside Earth. Every year, megatons of carbon disappear into subduction zones, affecting atmospheric carbon dioxide and oxygen over Earth's history. Here we discuss the processes that move carbon towards subduction zones and transform it into fluids, magmas, volcanic gases and diamonds. The carbon dioxide emitted from arc volcanoes is largely recycled from subducted microfossils, organic remains and carbonate precipitates. The type of carbon input and the efficiency with which carbon is remobilized in the subduction zone vary greatly around the globe, with every convergent margin providing a natural laboratory for tracing subducting carbon.
引用
收藏
页码:343 / 352
页数:10
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