Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event

The period leading up to the Great Ordovician Biodiversification Event was characterised by stable marine anoxic zones with a substantial increase in atmospheric oxygen occurring only after this, according to uranium isotope analyses of marine carbonates from southern Sweden

Bibliographic Details
Main Authors: Álvaro del Rey, Christian Mac Ørum Rasmussen, Mikael Calner, Rongchang Wu, Dan Asael, Tais W. Dahl
Format: Article
Language:English
Published: Nature Portfolio 2022-09-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-022-00548-w
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author Álvaro del Rey
Christian Mac Ørum Rasmussen
Mikael Calner
Rongchang Wu
Dan Asael
Tais W. Dahl
author_facet Álvaro del Rey
Christian Mac Ørum Rasmussen
Mikael Calner
Rongchang Wu
Dan Asael
Tais W. Dahl
author_sort Álvaro del Rey
collection DOAJ
description The period leading up to the Great Ordovician Biodiversification Event was characterised by stable marine anoxic zones with a substantial increase in atmospheric oxygen occurring only after this, according to uranium isotope analyses of marine carbonates from southern Sweden
first_indexed 2024-04-14T07:17:31Z
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spelling doaj.art-158e6e7c3ab74b588b3a8adf972dada22022-12-22T02:06:15ZengNature PortfolioCommunications Earth & Environment2662-44352022-09-01311710.1038/s43247-022-00548-wStable ocean redox during the main phase of the Great Ordovician Biodiversification EventÁlvaro del Rey0Christian Mac Ørum Rasmussen1Mikael Calner2Rongchang Wu3Dan Asael4Tais W. Dahl5GLOBE Institute, University of CopenhagenGLOBE Institute, University of CopenhagenDepartment of Geology, Lund UniversityNanjing Institute of Geology and Palaeontology, Chinese Academy of SciencesDepartment of Earth and Planetary Sciences, Yale UniversityGLOBE Institute, University of CopenhagenThe period leading up to the Great Ordovician Biodiversification Event was characterised by stable marine anoxic zones with a substantial increase in atmospheric oxygen occurring only after this, according to uranium isotope analyses of marine carbonates from southern Swedenhttps://doi.org/10.1038/s43247-022-00548-w
spellingShingle Álvaro del Rey
Christian Mac Ørum Rasmussen
Mikael Calner
Rongchang Wu
Dan Asael
Tais W. Dahl
Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event
Communications Earth & Environment
title Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event
title_full Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event
title_fullStr Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event
title_full_unstemmed Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event
title_short Stable ocean redox during the main phase of the Great Ordovician Biodiversification Event
title_sort stable ocean redox during the main phase of the great ordovician biodiversification event
url https://doi.org/10.1038/s43247-022-00548-w
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