Abiotic synthesis of graphite in hydrothermal vents

Deciphering the origin, age, and composition of deep marine organic carbon remains a challenge for understanding the dynamics of the marine carbon cycle. Here, the authors identify (sub)micron-sized graphite emanating from both high and low temperature hydrothermal vents along the East Pacific Rise,...

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Autores principales:	Emily R. Estes, Debora Berti, Nicole R. Coffey, Michael F. Hochella, Andrew S. Wozniak, George W. Luther
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2019
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/a76258f0a10b419ea8005190f7f8f6f5
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spelling	oai:doaj.org-article:a76258f0a10b419ea8005190f7f8f6f52021-12-02T17:01:48ZAbiotic synthesis of graphite in hydrothermal vents10.1038/s41467-019-13216-z2041-1723https://doaj.org/article/a76258f0a10b419ea8005190f7f8f6f52019-11-01T00:00:00Zhttps://doi.org/10.1038/s41467-019-13216-zhttps://doaj.org/toc/2041-1723Deciphering the origin, age, and composition of deep marine organic carbon remains a challenge for understanding the dynamics of the marine carbon cycle. Here, the authors identify (sub)micron-sized graphite emanating from both high and low temperature hydrothermal vents along the East Pacific Rise, and suggest graphite is a source of old carbon in the deep ocean.Emily R. EstesDebora BertiNicole R. CoffeyMichael F. HochellaAndrew S. WozniakGeorge W. LutherNature PortfolioarticleScienceQENNature Communications, Vol 10, Iss 1, Pp 1-6 (2019)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Emily R. Estes Debora Berti Nicole R. Coffey Michael F. Hochella Andrew S. Wozniak George W. Luther Abiotic synthesis of graphite in hydrothermal vents
description	Deciphering the origin, age, and composition of deep marine organic carbon remains a challenge for understanding the dynamics of the marine carbon cycle. Here, the authors identify (sub)micron-sized graphite emanating from both high and low temperature hydrothermal vents along the East Pacific Rise, and suggest graphite is a source of old carbon in the deep ocean.
format	article
author	Emily R. Estes Debora Berti Nicole R. Coffey Michael F. Hochella Andrew S. Wozniak George W. Luther
author_facet	Emily R. Estes Debora Berti Nicole R. Coffey Michael F. Hochella Andrew S. Wozniak George W. Luther
author_sort	Emily R. Estes
title	Abiotic synthesis of graphite in hydrothermal vents
title_short	Abiotic synthesis of graphite in hydrothermal vents
title_full	Abiotic synthesis of graphite in hydrothermal vents
title_fullStr	Abiotic synthesis of graphite in hydrothermal vents
title_full_unstemmed	Abiotic synthesis of graphite in hydrothermal vents
title_sort	abiotic synthesis of graphite in hydrothermal vents
publisher	Nature Portfolio
publishDate	2019
url	https://doaj.org/article/a76258f0a10b419ea8005190f7f8f6f5
work_keys_str_mv	AT emilyrestes abioticsynthesisofgraphiteinhydrothermalvents AT deboraberti abioticsynthesisofgraphiteinhydrothermalvents AT nicolercoffey abioticsynthesisofgraphiteinhydrothermalvents AT michaelfhochella abioticsynthesisofgraphiteinhydrothermalvents AT andrewswozniak abioticsynthesisofgraphiteinhydrothermalvents AT georgewluther abioticsynthesisofgraphiteinhydrothermalvents
_version_	1718382044703096832

Abiotic synthesis of graphite in hydrothermal vents

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