Cited by 565Marine and coastal ecosystemsOceanographic and Atmospheric ProcessesPaleontology and Stratigraphy of Fossils

Drivers and mechanisms of ocean deoxygenation.

Oschlies, Andreas, Brandt, Peter, Stramma, Lothar, Schmidtko, Sunke·2018·Nature Geoscience

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Crossref · 10.1038/s41561-018-0152-2

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  • Mechanisms responsible for the other half of the multi-decadal oxygen decline are unclear and are likely related to changes in ventilation and circulation, though changes in biological activity cannot be ruled out.

    “Mechanisms that are responsible for the other half are unclear and are likely related to changes in ventilation and circulation (Brandt et al., 2015;Oschlies et al., 2018), though changes in biological activity cannot be ruled out.”

    From The tropical atlantic observing system (2019) · cites this paper as Oschlies et al., 2018

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References 91 · Cited by 565

Authors
Oschlies, A., Brandt, P., Stramma, L., & Schmidtko, S.
Affiliations
  • Christian-Albrechts-Universität zu Kiel (DE)
  • GEOMAR Helmholtz Centre for Ocean Research Kiel (DE)
Corresponding author
Oschlies, Andreas
Venue
Nature Geoscience
Published
2018-06-11
Volume
11
Issue
7
Pages
467-473
ISSN
  • 1752-0894 (ISSN-L)
  • 1752-0908
OpenAlex
W2805504936
Cited by
565
References
91
Citations by year
2026: 50 · 2025: 75 · 2024: 104 · 2023: 94 · 2022: 72 · 2021: 89 · 2020: 50 · 2019: 25 · 2018: 6
FWCI
27.31
Type
journal article
Language
en
Open access
closed
Locations
  • Nature Geoscience (publishedVersion)
  • Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion)
Funders
Deutsche Forschungsgemeinschaft
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
ocean deoxygenation, ocean warming, oxygen solubility, ocean circulation, ocean mixing, oxygen respiration, biogeochemical feedbacks, ocean thermocline, climate model bias

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