Anomalous fractionation of mercury isotopes in the Late Archean atmosphere

Anomalous fractionation of mercury isotopes in the Late Archean atmosphere

Earth’s surface underwent a dramatic transition ~2.3 billion years ago when atmospheric oxygen first accumulated during the Great Oxidation Event. Here, the authors find that biogenic methane and volcanic emissions played a vital role in the reduced Late Archean atmosphere.

Guardado en:
Detalles Bibliográficos
Autores principales: Aubrey L. Zerkle, Runsheng Yin, Chaoyue Chen, Xiangdong Li, Gareth J. Izon, Stephen E. Grasby
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2020
Materias:
Science
Q
Acceso en línea:https://doaj.org/article/c9bbc92dec7b43008c00e4f13834b0e5
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:c9bbc92dec7b43008c00e4f13834b0e5
record_format dspace
spelling oai:doaj.org-article:c9bbc92dec7b43008c00e4f13834b0e52021-12-02T16:49:14ZAnomalous fractionation of mercury isotopes in the Late Archean atmosphere10.1038/s41467-020-15495-32041-1723https://doaj.org/article/c9bbc92dec7b43008c00e4f13834b0e52020-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-15495-3https://doaj.org/toc/2041-1723Earth’s surface underwent a dramatic transition ~2.3 billion years ago when atmospheric oxygen first accumulated during the Great Oxidation Event. Here, the authors find that biogenic methane and volcanic emissions played a vital role in the reduced Late Archean atmosphere.Aubrey L. ZerkleRunsheng YinChaoyue ChenXiangdong LiGareth J. IzonStephen E. GrasbyNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-9 (2020)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Aubrey L. Zerkle
Runsheng Yin
Chaoyue Chen
Xiangdong Li
Gareth J. Izon
Stephen E. Grasby
Anomalous fractionation of mercury isotopes in the Late Archean atmosphere
description Earth’s surface underwent a dramatic transition ~2.3 billion years ago when atmospheric oxygen first accumulated during the Great Oxidation Event. Here, the authors find that biogenic methane and volcanic emissions played a vital role in the reduced Late Archean atmosphere.
format article
author Aubrey L. Zerkle
Runsheng Yin
Chaoyue Chen
Xiangdong Li
Gareth J. Izon
Stephen E. Grasby
author_facet Aubrey L. Zerkle
Runsheng Yin
Chaoyue Chen
Xiangdong Li
Gareth J. Izon
Stephen E. Grasby
author_sort Aubrey L. Zerkle
title Anomalous fractionation of mercury isotopes in the Late Archean atmosphere
title_short Anomalous fractionation of mercury isotopes in the Late Archean atmosphere
title_full Anomalous fractionation of mercury isotopes in the Late Archean atmosphere
title_fullStr Anomalous fractionation of mercury isotopes in the Late Archean atmosphere
title_full_unstemmed Anomalous fractionation of mercury isotopes in the Late Archean atmosphere
title_sort anomalous fractionation of mercury isotopes in the late archean atmosphere
publisher Nature Portfolio
publishDate 2020
url https://doaj.org/article/c9bbc92dec7b43008c00e4f13834b0e5
work_keys_str_mv AT aubreylzerkle anomalousfractionationofmercuryisotopesinthelatearcheanatmosphere
AT runshengyin anomalousfractionationofmercuryisotopesinthelatearcheanatmosphere
AT chaoyuechen anomalousfractionationofmercuryisotopesinthelatearcheanatmosphere
AT xiangdongli anomalousfractionationofmercuryisotopesinthelatearcheanatmosphere
AT garethjizon anomalousfractionationofmercuryisotopesinthelatearcheanatmosphere
AT stephenegrasby anomalousfractionationofmercuryisotopesinthelatearcheanatmosphere
_version_ 1718383421308272640

Ejemplares similares