Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events.
Journal
Nature communications
ISSN: 2041-1723
Titre abrégé: Nat Commun
Pays: England
ID NLM: 101528555
Informations de publication
Date de publication:
11 01 2022
11 01 2022
Historique:
received:
21
07
2021
accepted:
08
12
2021
entrez:
12
1
2022
pubmed:
13
1
2022
medline:
13
1
2022
Statut:
epublish
Résumé
During the mid-Cretaceous, the Earth experienced several environmental perturbations, including an extremely warm climate and Oceanic Anoxic Events (OAEs). Submarine volcanic episodes associated with formation of large igneous provinces (LIPs) may have triggered these perturbations. The osmium isotopic ratio (
Identifiants
pubmed: 35017487
doi: 10.1038/s41467-021-27817-0
pii: 10.1038/s41467-021-27817-0
pmc: PMC8752794
doi:
Types de publication
Journal Article
Research Support, Non-U.S. Gov't
Langues
eng
Sous-ensembles de citation
IM
Pagination
239Informations de copyright
© 2022. The Author(s).
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