Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation

The long-term evolution of the sulfur budget in the lithosphere is poorly constrained. Here, using mass independent isotope fractionation as an indelible tracer, the authors track the pathway of sulfur from the Earth’s surface to punctuated episodes of granitoid magmatism during collisional orogenes...

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Autores principales:	Crystal LaFlamme, Marco L. Fiorentini, Mark D. Lindsay, Thi Hao Bui
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/0eb2699bb0024f38b2960fc3ef994b8d
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id	oai:doaj.org-article:0eb2699bb0024f38b2960fc3ef994b8d
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spelling	oai:doaj.org-article:0eb2699bb0024f38b2960fc3ef994b8d2021-12-02T17:33:18ZAtmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation10.1038/s41467-018-06691-32041-1723https://doaj.org/article/0eb2699bb0024f38b2960fc3ef994b8d2018-10-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-06691-3https://doaj.org/toc/2041-1723The long-term evolution of the sulfur budget in the lithosphere is poorly constrained. Here, using mass independent isotope fractionation as an indelible tracer, the authors track the pathway of sulfur from the Earth’s surface to punctuated episodes of granitoid magmatism during collisional orogenesis.Crystal LaFlammeMarco L. FiorentiniMark D. LindsayThi Hao BuiNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Crystal LaFlamme Marco L. Fiorentini Mark D. Lindsay Thi Hao Bui Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
description	The long-term evolution of the sulfur budget in the lithosphere is poorly constrained. Here, using mass independent isotope fractionation as an indelible tracer, the authors track the pathway of sulfur from the Earth’s surface to punctuated episodes of granitoid magmatism during collisional orogenesis.
format	article
author	Crystal LaFlamme Marco L. Fiorentini Mark D. Lindsay Thi Hao Bui
author_facet	Crystal LaFlamme Marco L. Fiorentini Mark D. Lindsay Thi Hao Bui
author_sort	Crystal LaFlamme
title	Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
title_short	Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
title_full	Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
title_fullStr	Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
title_full_unstemmed	Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
title_sort	atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/0eb2699bb0024f38b2960fc3ef994b8d
work_keys_str_mv	AT crystallaflamme atmosphericsulfurisrecycledtothecrystallinecontinentalcrustduringsupercontinentformation AT marcolfiorentini atmosphericsulfurisrecycledtothecrystallinecontinentalcrustduringsupercontinentformation AT markdlindsay atmosphericsulfurisrecycledtothecrystallinecontinentalcrustduringsupercontinentformation AT thihaobui atmosphericsulfurisrecycledtothecrystallinecontinentalcrustduringsupercontinentformation
_version_	1718379983073705984

Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation

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