Fossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater

Uncertainty regarding the evolution of the oxygen isotopic composition of seawater casts doubt on past temperature reconstructions. Here, the authors present a new, precise δ18O value for the Neoproterozoic, and propose that ocean temperatures on the eve of the Sturtian glaciation were 15–30 °C warm...

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Autores principales:	F. Hodel, M. Macouin, R. I. F. Trindade, A. Triantafyllou, J. Ganne, V. Chavagnac, J. Berger, M. Rospabé, C. Destrigneville, J. Carlut, N. Ennih, P. Agrinier
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/0950a7b3e5114a5a9f209c9e68ebc889
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spelling	oai:doaj.org-article:0950a7b3e5114a5a9f209c9e68ebc8892021-12-02T15:34:45ZFossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater10.1038/s41467-018-03890-w2041-1723https://doaj.org/article/0950a7b3e5114a5a9f209c9e68ebc8892018-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-03890-whttps://doaj.org/toc/2041-1723Uncertainty regarding the evolution of the oxygen isotopic composition of seawater casts doubt on past temperature reconstructions. Here, the authors present a new, precise δ18O value for the Neoproterozoic, and propose that ocean temperatures on the eve of the Sturtian glaciation were 15–30 °C warmer than present.F. HodelM. MacouinR. I. F. TrindadeA. TriantafyllouJ. GanneV. ChavagnacJ. BergerM. RospabéC. DestrignevilleJ. CarlutN. EnnihP. AgrinierNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-7 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q F. Hodel M. Macouin R. I. F. Trindade A. Triantafyllou J. Ganne V. Chavagnac J. Berger M. Rospabé C. Destrigneville J. Carlut N. Ennih P. Agrinier Fossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater
description	Uncertainty regarding the evolution of the oxygen isotopic composition of seawater casts doubt on past temperature reconstructions. Here, the authors present a new, precise δ18O value for the Neoproterozoic, and propose that ocean temperatures on the eve of the Sturtian glaciation were 15–30 °C warmer than present.
format	article
author	F. Hodel M. Macouin R. I. F. Trindade A. Triantafyllou J. Ganne V. Chavagnac J. Berger M. Rospabé C. Destrigneville J. Carlut N. Ennih P. Agrinier
author_facet	F. Hodel M. Macouin R. I. F. Trindade A. Triantafyllou J. Ganne V. Chavagnac J. Berger M. Rospabé C. Destrigneville J. Carlut N. Ennih P. Agrinier
author_sort	F. Hodel
title	Fossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater
title_short	Fossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater
title_full	Fossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater
title_fullStr	Fossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater
title_full_unstemmed	Fossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater
title_sort	fossil black smoker yields oxygen isotopic composition of neoproterozoic seawater
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/0950a7b3e5114a5a9f209c9e68ebc889
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Fossil black smoker yields oxygen isotopic composition of Neoproterozoic seawater

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