Articles | Volume 20, issue 5
https://doi.org/10.5194/bg-20-997-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-20-997-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
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14 Mar 2023
Research article | Highlight paper |
| 14 Mar 2023
| 14 Mar 2023
Model estimates of metazoans' contributions to the biological carbon pump
Jérôme Pinti
CORRESPONDING AUTHOR
VKR Centre for Ocean Life, Technical University of Denmark, 2800 Kongens Lyngby, Denmark
College of Earth, Ocean, and Environment, University of Delaware, Lewes, DE 19958, USA
Tim DeVries
Department of Geography, University of California Santa Barbara, Santa Barbara, CA 93106, USA
Earth Research Institute, University of California Santa Barbara, Santa Barbara, CA 93106, USA
Tommy Norin
VKR Centre for Ocean Life, Technical University of Denmark, 2800 Kongens Lyngby, Denmark
Camila Serra-Pompei
VKR Centre for Ocean Life, Technical University of Denmark, 2800 Kongens Lyngby, Denmark
Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of
Technology, Cambridge, MA 02139, USA
Roland Proud
Pelagic Ecology Research Group, School of Biology, Gatty Marine Laboratory, Scottish Oceans Institute, University of St Andrews, St Andrews, Fife, KY16 8LB, UK
David A. Siegel
Department of Geography, University of California Santa Barbara, Santa Barbara, CA 93106, USA
Earth Research Institute, University of California Santa Barbara, Santa Barbara, CA 93106, USA
Thomas Kiørboe
VKR Centre for Ocean Life, Technical University of Denmark, 2800 Kongens Lyngby, Denmark
Colleen M. Petrik
Department of Oceanography, Texas A&M University, 3146 TAMU, College Station, TX 77843, USA
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92107, USA
Ken H. Andersen
VKR Centre for Ocean Life, Technical University of Denmark, 2800 Kongens Lyngby, Denmark
Andrew S. Brierley
Pelagic Ecology Research Group, School of Biology, Gatty Marine Laboratory, Scottish Oceans Institute, University of St Andrews, St Andrews, Fife, KY16 8LB, UK
André W. Visser
VKR Centre for Ocean Life, Technical University of Denmark, 2800 Kongens Lyngby, Denmark
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Andre Visser, Anton Vergod Almgren, and Athanasios Kandylas
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Global models largely rely on empirical estimates of the rate at which this material is produced and sinks. Here we propose a mechanistic model that tries to capture the most important processes regulating the size and density of particulate organic material from when it is produced by living organisms, through its aggregation and fragmentation into particles of different size and density, degradation by microbes and eventual sinking into the ocean’s interior.
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Our paper provides an overview of all observational climate-related and socioeconomic forcing data used as input for the impact model evaluation and impact attribution experiments within the third round of the Inter-Sectoral Impact Model Intercomparison Project. The experiments are designed to test our understanding of observed changes in natural and human systems and to quantify to what degree these changes have already been induced by climate change.
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The ocean is an important part of the global carbon cycle, taking up about a quarter of the anthropogenic CO2 emitted by burning of fossil fuels and thus slowing down climate change. However, the CO2 uptake by the ocean is, in turn, affected by variability and trends in climate. Here we use carbon measurements in the surface ocean to quantify the response of the oceanic CO2 exchange to environmental conditions and discuss possible mechanisms underlying this response.
Paul J. Tréguer, Jill N. Sutton, Mark Brzezinski, Matthew A. Charette, Timothy Devries, Stephanie Dutkiewicz, Claudia Ehlert, Jon Hawkings, Aude Leynaert, Su Mei Liu, Natalia Llopis Monferrer, María López-Acosta, Manuel Maldonado, Shaily Rahman, Lihua Ran, and Olivier Rouxel
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Silicon is the second most abundant element of the Earth's crust. In this review, we show that silicon inputs and outputs, to and from the world ocean, are 57 % and 37 % higher, respectively, than previous estimates. These changes are significant, modifying factors such as the geochemical residence time of silicon, which is now about 8000 years and 2 times faster than previously assumed. We also update the total biogenic silica pelagic production and provide an estimate for sponge production.
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Short summary
Large numbers of marine organisms such as zooplankton and fish perform daily vertical migration between the surface (at night) and the depths (in the daytime). This fascinating migration is important for the carbon cycle, as these organisms actively bring carbon to depths where it is stored away from the atmosphere for a long time. Here, we quantify the contributions of different animals to this carbon drawdown and storage and show that fish are important to the biological carbon pump.
Large numbers of marine organisms such as zooplankton and fish perform daily vertical migration...
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