Natural ocean iron fertilization and climate variability over geological periods.
atmospheric carbon dioxide
climate change
geological periods
marine primary producers
ocean iron fertilization
Journal
Global change biology
ISSN: 1365-2486
Titre abrégé: Glob Chang Biol
Pays: England
ID NLM: 9888746
Informations de publication
Date de publication:
Dec 2023
Dec 2023
Historique:
revised:
20
09
2023
received:
18
07
2023
accepted:
27
09
2023
medline:
15
11
2023
pubmed:
19
10
2023
entrez:
19
10
2023
Statut:
ppublish
Résumé
Marine primary producers are largely dependent on and shape the Earth's climate, although their relationship with climate varies over space and time. The growth of phytoplankton and associated marine primary productivity in most of the modern global ocean is limited by the supply of nutrients, including the micronutrient iron. The addition of iron via episodic and frequent events drives the biological carbon pump and promotes the sequestration of atmospheric carbon dioxide (CO
Substances chimiques
Iron
E1UOL152H7
Carbon Dioxide
142M471B3J
Types de publication
Journal Article
Review
Langues
eng
Sous-ensembles de citation
IM
Pagination
6856-6866Subventions
Organisme : National Natural Science Foundation of China
ID : 32170108
Organisme : National Natural Science Foundation of China
ID : 42188102
Organisme : Southern Marine Science and Engineering Guangdong Laboratory
ID : SML2021SP204
Organisme : Science and Technology Innovation 2025 Major Project of Ningbo City
ID : 2022Z189
Informations de copyright
© 2023 John Wiley & Sons Ltd.
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