Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle

Veins of aragonite in deep ocean trenches can record discharges of CO2-rich paleoseawater and suggest that exposed serpentinized forearcs can act as carbon reservoirs, according to residence time calculations based on geochemical analyses of mantle rocks from offshore Japan.

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Autores principales:	Ryosuke Oyanagi, Atsushi Okamoto, Madhusoodhan Satish-Kumar, Masayo Minami, Yumiko Harigane, Katsuyoshi Michibayashi
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2021
Materias:	Geology QE1-996.5 Environmental sciences GE1-350
Acceso en línea:	https://doaj.org/article/705f607461fe4f1ba644a0b4d6840402
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spelling	oai:doaj.org-article:705f607461fe4f1ba644a0b4d68404022021-12-05T12:08:38ZHadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle10.1038/s43247-021-00317-12662-4435https://doaj.org/article/705f607461fe4f1ba644a0b4d68404022021-12-01T00:00:00Zhttps://doi.org/10.1038/s43247-021-00317-1https://doaj.org/toc/2662-4435Veins of aragonite in deep ocean trenches can record discharges of CO2-rich paleoseawater and suggest that exposed serpentinized forearcs can act as carbon reservoirs, according to residence time calculations based on geochemical analyses of mantle rocks from offshore Japan.Ryosuke OyanagiAtsushi OkamotoMadhusoodhan Satish-KumarMasayo MinamiYumiko HariganeKatsuyoshi MichibayashiNature PortfolioarticleGeologyQE1-996.5Environmental sciencesGE1-350ENCommunications Earth & Environment, Vol 2, Iss 1, Pp 1-10 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	Geology QE1-996.5 Environmental sciences GE1-350
spellingShingle	Geology QE1-996.5 Environmental sciences GE1-350 Ryosuke Oyanagi Atsushi Okamoto Madhusoodhan Satish-Kumar Masayo Minami Yumiko Harigane Katsuyoshi Michibayashi Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle
description	Veins of aragonite in deep ocean trenches can record discharges of CO2-rich paleoseawater and suggest that exposed serpentinized forearcs can act as carbon reservoirs, according to residence time calculations based on geochemical analyses of mantle rocks from offshore Japan.
format	article
author	Ryosuke Oyanagi Atsushi Okamoto Madhusoodhan Satish-Kumar Masayo Minami Yumiko Harigane Katsuyoshi Michibayashi
author_facet	Ryosuke Oyanagi Atsushi Okamoto Madhusoodhan Satish-Kumar Masayo Minami Yumiko Harigane Katsuyoshi Michibayashi
author_sort	Ryosuke Oyanagi
title	Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle
title_short	Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle
title_full	Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle
title_fullStr	Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle
title_full_unstemmed	Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle
title_sort	hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle
publisher	Nature Portfolio
publishDate	2021
url	https://doaj.org/article/705f607461fe4f1ba644a0b4d6840402
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Hadal aragonite records venting of stagnant paleoseawater in the hydrated forearc mantle

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