Literature DB >> 31619791

Subducting carbon.

Terry Plank1, Craig E Manning2.   

Abstract

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.

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Year:  2019        PMID: 31619791     DOI: 10.1038/s41586-019-1643-z

Source DB:  PubMed          Journal:  Nature        ISSN: 0028-0836            Impact factor:   49.962


  18 in total

1.  The lithospheric-to-lower-mantle carbon cycle recorded in superdeep diamonds.

Authors:  M E Regier; D G Pearson; T Stachel; R W Luth; R A Stern; J W Harris
Journal:  Nature       Date:  2020-09-09       Impact factor: 49.962

Review 2.  Evolution of Earth's tectonic carbon conveyor belt.

Authors:  R Dietmar Müller; Ben Mather; Adriana Dutkiewicz; Tobias Keller; Andrew Merdith; Christopher M Gonzalez; Weronika Gorczyk; Sabin Zahirovic
Journal:  Nature       Date:  2022-05-25       Impact factor: 49.962

3.  Linking deep CO2 outgassing to cratonic destruction.

Authors:  Zhao-Xue Wang; Sheng-Ao Liu; Shuguang Li; Di Liu; Jingao Liu
Journal:  Natl Sci Rev       Date:  2022-01-08       Impact factor: 23.178

4.  Magnesium isotope geochemistry of the carbonate-silicate system in subduction zones.

Authors:  Shui-Jiong Wang; Shu-Guang Li
Journal:  Natl Sci Rev       Date:  2022-02-26       Impact factor: 23.178

5.  Carbon cycle inverse modeling suggests large changes in fractional organic burial are consistent with the carbon isotope record and may have contributed to the rise of oxygen.

Authors:  Joshua Krissansen-Totton; Michael A Kipp; David C Catling
Journal:  Geobiology       Date:  2021-03-25       Impact factor: 4.216

6.  Reversal of carbonate-silicate cation exchange in cold slabs in Earth's lower mantle.

Authors:  Mingda Lv; Susannah M Dorfman; James Badro; Stephan Borensztajn; Eran Greenberg; Vitali B Prakapenka
Journal:  Nat Commun       Date:  2021-03-17       Impact factor: 14.919

7.  Pervasive subduction zone devolatilization recycles CO2 into the forearc.

Authors:  E M Stewart; Jay J Ague
Journal:  Nat Commun       Date:  2020-12-04       Impact factor: 14.919

8.  India-Asia collision as a driver of atmospheric CO2 in the Cenozoic.

Authors:  Zhengfu Guo; Marjorie Wilson; Donald B Dingwell; Jiaqi Liu
Journal:  Nat Commun       Date:  2021-06-23       Impact factor: 14.919

9.  Massive carbon storage in convergent margins initiated by subduction of limestone.

Authors:  Chunfei Chen; Michael W Förster; Stephen F Foley; Yongsheng Liu
Journal:  Nat Commun       Date:  2021-07-22       Impact factor: 14.919

10.  Deep carbon cycle constrained by carbonate solubility.

Authors:  Stefan Farsang; Marion Louvel; Chaoshuai Zhao; Mohamed Mezouar; Angelika D Rosa; Remo N Widmer; Xiaolei Feng; Jin Liu; Simon A T Redfern
Journal:  Nat Commun       Date:  2021-07-14       Impact factor: 14.919

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