Fish proliferation and rare-earth deposition by topographically induced upwelling at the late Eocene cooling event.
Journal
Scientific reports
ISSN: 2045-2322
Titre abrégé: Sci Rep
Pays: England
ID NLM: 101563288
Informations de publication
Date de publication:
18 06 2020
18 06 2020
Historique:
received:
30
08
2019
accepted:
13
05
2020
entrez:
20
6
2020
pubmed:
20
6
2020
medline:
15
12
2020
Statut:
epublish
Résumé
The deep-sea clay that covers wide areas of the pelagic ocean bottom provides key information about open-ocean environments but lacks age-diagnostic calcareous or siliceous microfossils. The marine osmium isotope record has varied in response to environmental changes and can therefore be a useful stratigraphic marker. In this study, we used osmium isotope ratios to determine the depositional ages of pelagic clays extraordinarily rich in fish debris. Much fish debris was deposited in the western North and central South Pacific sites roughly 34.4 million years ago, concurrent with a late Eocene event, a temporal expansion of Antarctic ice preceding the Eocene-Oligocene climate transition. The enhanced northward flow of bottom water formed around Antarctica probably caused upwelling of deep-ocean nutrients at topographic highs and stimulated biological productivity that resulted in the proliferation of fish in pelagic realms. The abundant fish debris is now a highly concentrated source of industrially critical rare-earth elements.
Identifiants
pubmed: 32555233
doi: 10.1038/s41598-020-66835-8
pii: 10.1038/s41598-020-66835-8
pmc: PMC7303186
doi:
Substances chimiques
Isotopes
0
Metals, Rare Earth
0
Osmium-187
0
Osmium-188
0
Osmium
2E7M255OPY
Types de publication
Journal Article
Research Support, Non-U.S. Gov't
Langues
eng
Sous-ensembles de citation
IM
Pagination
9896Commentaires et corrections
Type : ErratumIn
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