Respiration patterns in the deep ocean
Open accessAbstract
The biological pump affects atmospheric CO 2 levels and fuels most heterotrophic activity in the deep ocean. The efficiency of this pump depends on the rate of carbon fixation, export out of the euphotic zone and the depth of respiration. Here we study the depth dependence of respiration patterns, hence particulate carbon flux, using a compiled data set of sediment oxygen consumption rates. We show that the depth relationship can best be described by a double exponential model. For the upper part of the ocean, our resulting equation is similar to previous flux‐depth relationships but predicted fluxes are significantly larger in deeper waters. This implies a more efficient biological pump. Total oceanic respiration below the shelf break (200 m) is estimated to be 827 Tmol O 2 yr−1.
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Píka, P., Hülse, D., Eglinton, T. I., & Arndt, S. (2023) · Global Biogeochemical Cycles · doi:10.1029/2022gb007636 · Cited by 8 · see citing works
Maffre, P., Goddéris, Y., Hir, G. L., Nardin, É., Sarr, A., & Yannick Donnadieu, A. (2025) · Geoscientific model development · doi:10.5194/gmd-18-6367-2025 · Cited by 8 · see citing works
Food falls in the deep northwestern Weddell Sea
Stauffer, J. B., Purser, A., Griffiths, H. J., Smith, C. R., & Hoving, H. (2022) · Frontiers in Marine Science · doi:10.3389/fmars.2022.1055318 · Cited by 6 · see citing works
Ocean Biogeochemical Fingerprints of Fast‐Sinking Tunicate and Fish Detritus
Luo, J. Y., Stock, C. A. A., Dunne, J. P. P., Saba, G. K., & Cook, L. (2024) · Geophysical Research Letters · doi:10.1029/2023gl107052 · Cited by 5 · see citing works
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FESOM2.1-REcoM3-MEDUSA2: an ocean–sea ice–biogeochemistry model coupled to a sediment model
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Self-citationModeling of scattering properties of mineral aerosols using modified beta function
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Respiration patterns in the dark oceanPreprint
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A Respiratory Assessment of the Biological Carbon Pump Reveals overlooked Carbon FluxesPreprint
Hernández‐Hernández, N., Montero, M. F., Santana‐Falcón, Y., & Arı́stegui, J. (2026) · Research Square · doi:10.21203/rs.3.rs-9920080/v1
- Authors
- Andersson, J. H., Wijsman, J. W. M., Herman, P. M. J., Middelburg, J. J., Soetaert, K., & Heip, C.
- Affiliations
- Netherlands Institute of Ecology–Centre for Estuarine and Marine Ecology Yerseke The Netherlands
- Netherlands Institute of Ecology (NL)
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2004-02
- Volume
- 31
- Issue
- 3
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2081163111
- Cited by
- 91
- References
- 32
- Citations by year
- 2026: 2 · 2025: 4 · 2024: 1 · 2023: 3 · 2022: 3 · 2020: 1 · 2019: 11 · 2018: 2 · 2017: 7 · 2016: 9 · 2015: 9 · 2014: 4 · 2013: 7 · 2012: 3
- FWCI
- 3.39
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Geophysical Research Letters (publishedVersion)
- Data Archiving and Networked Services (DANS) (submittedVersion, other-oa)
- Ghent University Academic Bibliography (Ghent University) (submittedVersion)
- Flanders Marine Institute (Flanders Marine Institute) (submittedVersion)
- KNAW Research Portal (The Royal Netherlands Academy of Arts and Sciences) (submittedVersion, other-oa)
- University of Groningen research database (University of Groningen / Centre for Information Technology) (submittedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Biology and Ecology Research
- Keywords
- biological carbon pump, sediment oxygen consumption, depth dependence, double exponential model, carbon export, euphotic zone, atmospheric CO2
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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