Articles | Volume 10, issue 3
https://doi.org/10.5194/esd-10-539-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esd-10-539-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Ocean phosphorus inventory: large uncertainties in future projections on millennial timescales and their consequences for ocean deoxygenation
GEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker
Weg 20, 24105 Kiel, Germany
Angela Landolfi
GEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker
Weg 20, 24105 Kiel, Germany
Andreas Oschlies
GEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker
Weg 20, 24105 Kiel, Germany
Klaus Wallmann
GEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker
Weg 20, 24105 Kiel, Germany
Andrew W. Dale
GEOMAR Helmholtz Centre for Ocean Research Kiel, Düsternbrooker
Weg 20, 24105 Kiel, Germany
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Cited
11 citations as recorded by crossref.
- Accounting for Dissolved Organic Nutrients in an SPBEM-2 Model: Validation and Verification A. Isaev et al. 10.3390/w12051307
- Opportunities for Earth Observation to Inform Risk Management for Ocean Tipping Points R. Wood et al. 10.1007/s10712-024-09859-3
- First regional reference database of northern Adriatic diatom transcriptomes M. Knjaz et al. 10.1038/s41598-024-67043-4
- Carbon Cycle Responses to Changes in Weathering and the Long‐Term Fate of Stable Carbon Isotopes A. Jeltsch‐Thömmes & F. Joos 10.1029/2022PA004577
- Enhanced Organic Carbon Burial in Sediments of Oxygen Minimum Zones Upon Ocean Deoxygenation I. Ruvalcaba Baroni et al. 10.3389/fmars.2019.00839
- Exceeding 1.5°C global warming could trigger multiple climate tipping points D. Armstrong McKay et al. 10.1126/science.abn7950
- Riverine nutrient impact on global ocean nitrogen cycle feedbacks and marine primary production in an Earth system model M. Tivig et al. 10.5194/bg-21-4469-2024
- Organic biogeochemistry in the oxygen-deficient ocean: A review S. Wakeham 10.1016/j.orggeochem.2020.104096
- Nitrogen cycling in sediments on the NW African margin inferred from N and O isotopes in benthic chambers A. Dale et al. 10.3389/fmars.2022.902062
- Paradox of relatively more phospholipids in phytoplankton in phosphorus limited sea B. Gašparović et al. 10.1002/lno.12464
- Contrasting Roles of DOP as a Source of Phosphorus and Energy for Marine Diazotrophs A. Filella et al. 10.3389/fmars.2022.923765
11 citations as recorded by crossref.
- Accounting for Dissolved Organic Nutrients in an SPBEM-2 Model: Validation and Verification A. Isaev et al. 10.3390/w12051307
- Opportunities for Earth Observation to Inform Risk Management for Ocean Tipping Points R. Wood et al. 10.1007/s10712-024-09859-3
- First regional reference database of northern Adriatic diatom transcriptomes M. Knjaz et al. 10.1038/s41598-024-67043-4
- Carbon Cycle Responses to Changes in Weathering and the Long‐Term Fate of Stable Carbon Isotopes A. Jeltsch‐Thömmes & F. Joos 10.1029/2022PA004577
- Enhanced Organic Carbon Burial in Sediments of Oxygen Minimum Zones Upon Ocean Deoxygenation I. Ruvalcaba Baroni et al. 10.3389/fmars.2019.00839
- Exceeding 1.5°C global warming could trigger multiple climate tipping points D. Armstrong McKay et al. 10.1126/science.abn7950
- Riverine nutrient impact on global ocean nitrogen cycle feedbacks and marine primary production in an Earth system model M. Tivig et al. 10.5194/bg-21-4469-2024
- Organic biogeochemistry in the oxygen-deficient ocean: A review S. Wakeham 10.1016/j.orggeochem.2020.104096
- Nitrogen cycling in sediments on the NW African margin inferred from N and O isotopes in benthic chambers A. Dale et al. 10.3389/fmars.2022.902062
- Paradox of relatively more phospholipids in phytoplankton in phosphorus limited sea B. Gašparović et al. 10.1002/lno.12464
- Contrasting Roles of DOP as a Source of Phosphorus and Energy for Marine Diazotrophs A. Filella et al. 10.3389/fmars.2022.923765
Latest update: 06 Mar 2025
Short summary
Oceanic deoxygenation is driven by climate change in several areas of the global ocean. Measurements indicate that ocean volumes with very low oxygen levels expand, with consequences for marine organisms and fishery. We found climate-change-driven phosphorus (P) input in the ocean is hereby an important driver for deoxygenation on longer timescales with effects in the next millennia.
Oceanic deoxygenation is driven by climate change in several areas of the global ocean....
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