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
Main Authors: | , , , , , |
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Format: | Article |
Language: | English |
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Nature Portfolio
2022-09-01
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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 |
format | Article |
id | doaj.art-158e6e7c3ab74b588b3a8adf972dada2 |
institution | Directory Open Access Journal |
issn | 2662-4435 |
language | English |
last_indexed | 2024-04-14T07:17:31Z |
publishDate | 2022-09-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Communications Earth & Environment |
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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