Polysaccharide aggregation as a potential sink of marine dissolved organic carbon
The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean 1 . Whereas marine sciences have focused primarily on particle production by phytoplankton growth, particle formation by the assembly of organic macromolecules has almost been neglec...
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| Published in: | Nature (London) Vol. 428; no. 6986; pp. 929 - 932 |
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| Main Authors: | , , , , |
| Format: | Journal Article |
| Language: | English |
| Published: |
London
Nature Publishing Group UK
29.04.2004
Nature Publishing Nature Publishing Group |
| Subjects: | |
| ISSN: | 0028-0836, 1476-4687, 1476-4687 |
| Online Access: | Get full text |
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| Abstract | The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean
1
. Whereas marine sciences have focused primarily on particle production by phytoplankton growth, particle formation by the assembly of organic macromolecules has almost been neglected
2
,
3
. Here we show, by means of a combined experimental and modelling study, that the formation of polysaccharide particles is an important pathway to convert dissolved into particulate organic carbon during phytoplankton blooms, and can be described in terms of aggregation kinetics. Our findings suggest that aggregation processes in the ocean cascade from the molecular scale up to the size of fast-settling particles, and give new insights into the cycling and export of biogeochemical key elements such as carbon, iron and thorium. |
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| AbstractList | The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean. Whereas marine sciences have focused primarily on particle production by phytoplankton growth, particle formation by the assembly of organic macromolecules has almost been neglected. Here we show, by means of a combined experimental and modelling study, that the formation of polysaccharide particles is an important pathway to convert dissolved into particulate organic carbon during phytoplankton blooms, and can be described in terms of aggregation kinetics. Our findings suggest that aggregation processes in the ocean cascade from the molecular scale up to the size of fast-settling particles, and give new insights into the cycling and export of biogeochemical key elements such as carbon, iron and thorium. [PUBLICATION ABSTRACT] The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean(1). Whereas marine sciences have focused primarily on particle production by phytoplankton growth, particle formation by the assembly of organic macromolecules has almost been neglected(2,3). Here we show, by means of a combined experimental and modelling study, that the formation of polysaccharide particles is an important pathway to convert dissolved into particulate organic carbon during phytoplankton blooms, and can be described in terms of aggregation kinetics. Our findings suggest that aggregation processes in the ocean cascade from the molecular scale up to the size of fast-settling particles, and give new insights into the cycling and export of biogeochemical key elements such as carbon, iron and thorium. The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean. Whereas marine sciences have focused primarily on particle production by phytoplankton growth, particle formation by the assembly of organic macromolecules has almost been neglected. Here we show, by means of a combined experimental and modelling study, that the formation of polysaccharide particles is an important pathway to convert dissolved into particulate organic carbon during phytoplankton blooms, and can be described in terms of aggregation kinetics. Our findings suggest that aggregation processes in the ocean cascade from the molecular scale up to the size of fast-settling particles, and give new insights into the cycling and export of biogeochemical key elements such as carbon, iron and thorium.The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean. Whereas marine sciences have focused primarily on particle production by phytoplankton growth, particle formation by the assembly of organic macromolecules has almost been neglected. Here we show, by means of a combined experimental and modelling study, that the formation of polysaccharide particles is an important pathway to convert dissolved into particulate organic carbon during phytoplankton blooms, and can be described in terms of aggregation kinetics. Our findings suggest that aggregation processes in the ocean cascade from the molecular scale up to the size of fast-settling particles, and give new insights into the cycling and export of biogeochemical key elements such as carbon, iron and thorium. The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean. Whereas marine sciences have focused primarily on particle production by phytoplankton growth, particle formation by the assembly of organic macromolecules has almost been neglected. Here we show, by means of a combined experimental and modelling study, that the formation of polysaccharide particles is an important pathway to convert dissolved into particulate organic carbon during phytoplankton blooms, and can be described in terms of aggregation kinetics. Our findings suggest that aggregation processes in the ocean cascade from the molecular scale up to the size of fast-settling particles, and give new insights into the cycling and export of biogeochemical key elements such as carbon, iron and thorium. Tests have demonstrated that the formation and sinking of biogenic particles acts to mediate vertical mass fluxes and drive elemental cycling in the ocean. Many studies have considered particle production via phytoplankton growth. Most studies have overlooked particle formation by the assembly of organic macromolecules. Findings from a combined experimental and modeling study showed that the formation of polysaccharide particles serves as an important pathway for the conversion of dissolved organic carbon into particulate organic carbon during phytoplankton blooms. These formation processes can be accurately described in terms of aggregation kinetics. Insights into the cycling and export of biogeogemical key elements (e.g., carbon, iron, and thorium) are presented. The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean 1 . Whereas marine sciences have focused primarily on particle production by phytoplankton growth, particle formation by the assembly of organic macromolecules has almost been neglected 2 , 3 . Here we show, by means of a combined experimental and modelling study, that the formation of polysaccharide particles is an important pathway to convert dissolved into particulate organic carbon during phytoplankton blooms, and can be described in terms of aggregation kinetics. Our findings suggest that aggregation processes in the ocean cascade from the molecular scale up to the size of fast-settling particles, and give new insights into the cycling and export of biogeochemical key elements such as carbon, iron and thorium. |
| Audience | Academic |
| Author | Riebesell, Ulf Zondervan, Ingrid Rochelle-Newall, Emma Thoms, Silke Engel, Anja |
| Author_xml | – sequence: 1 givenname: Anja surname: Engel fullname: Engel, Anja email: anja.engel@stonybrook.edu organization: Alfred-Wegener-Institut für Polar- und Meeresforschung, Marine Sciences Research Center, Stony Brook University, Leibniz-Institut für Meereswissenschaften, Universität Kiel, Centre IRD de Noumea, BPA5 – sequence: 2 givenname: Silke surname: Thoms fullname: Thoms, Silke email: sthoms@awi-bremerhaven.de organization: Alfred-Wegener-Institut für Polar- und Meeresforschung – sequence: 3 givenname: Ulf surname: Riebesell fullname: Riebesell, Ulf organization: Alfred-Wegener-Institut für Polar- und Meeresforschung, Marine Sciences Research Center, Stony Brook University, Leibniz-Institut für Meereswissenschaften, Universität Kiel, Centre IRD de Noumea, BPA5 – sequence: 4 givenname: Emma surname: Rochelle-Newall fullname: Rochelle-Newall, Emma organization: Laboratoire d'Océanographie de Villefranche sur Mer, Station Zoologique, Marine Sciences Research Center, Stony Brook University, Leibniz-Institut für Meereswissenschaften, Universität Kiel, Centre IRD de Noumea, BPA5 – sequence: 5 givenname: Ingrid surname: Zondervan fullname: Zondervan, Ingrid organization: Alfred-Wegener-Institut für Polar- und Meeresforschung |
| BackLink | http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=15707872$$DView record in Pascal Francis https://www.ncbi.nlm.nih.gov/pubmed/15118723$$D View this record in MEDLINE/PubMed https://hal.science/hal-03506678$$DView record in HAL |
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| ContentType | Journal Article |
| Copyright | Macmillan Magazines Ltd. 2004 2004 INIST-CNRS COPYRIGHT 2004 Nature Publishing Group Copyright Macmillan Journals Ltd. Apr 29, 2004 Distributed under a Creative Commons Attribution 4.0 International License |
| Copyright_xml | – notice: Macmillan Magazines Ltd. 2004 – notice: 2004 INIST-CNRS – notice: COPYRIGHT 2004 Nature Publishing Group – notice: Copyright Macmillan Journals Ltd. Apr 29, 2004 – notice: Distributed under a Creative Commons Attribution 4.0 International License |
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| DOI | 10.1038/nature02453 |
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| Issue | 6986 |
| Keywords | Primary productivity Biological macromolecule Particulate carbon Biogeochemical cycle Modeling Dissolved organic carbon Carbon cycle Bloom Phytoplankton Molecular aggregation Kinetics Formation mechanism Polysaccharide Oceanology |
| Language | English |
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| Snippet | The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean
1
. Whereas marine sciences have focused... The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean. Whereas marine sciences have focused... Tests have demonstrated that the formation and sinking of biogenic particles acts to mediate vertical mass fluxes and drive elemental cycling in the ocean.... The formation and sinking of biogenic particles mediate vertical mass fluxes and drive elemental cycling in the ocean(1). Whereas marine sciences have focused... |
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| SubjectTerms | Bacteria - isolation & purification Bacteria - metabolism Carbon Carbon - chemistry Carbon - metabolism Dissolved organic carbon Earth Sciences Earth, ocean, space Exact sciences and technology External geophysics Humanities and Social Sciences Kinetics letter Marine Marine sciences multidisciplinary Ocean currents Oceanography Oceans and Seas Organic chemistry Particulate organic carbon Physical and chemical properties of sea water Physics of the oceans Phytoplankton Phytoplankton - chemistry Phytoplankton - metabolism Plankton Polysaccharides - chemistry Polysaccharides - metabolism Science Science (multidisciplinary) Sciences of the Universe Seawater - chemistry Seawater - microbiology Solubility Thorium |
| Title | Polysaccharide aggregation as a potential sink of marine dissolved organic carbon |
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