Laminarin is a major molecule in the marine carbon cycle


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jhhehemann [ at ] marum.de

Abstract

Marine microalgae sequester as much CO2 into carbohydrates as terrestrial plants. Polymeric carbohydrates (i.e., glycans) provide carbon for heterotrophic organisms and constitute a carbon sink in the global oceans. The quantitative contributions of different algal glycans to cycling and sequestration of carbon remain unknown, partly because of the analytical challenge to quantify glycans in complex biological matrices. Here, we quantified a glycan structural type using a recently developed biocatalytic strategy, which involves laminarinase enzymes that specifically cleave the algal glycan laminarin into readily analyzable fragments. We measured laminarin along transects in the Arctic, Atlantic, and Pacific oceans and during three time series in the North Sea. These data revealed a median of 26 ± 17% laminarin within the particulate organic carbon pool. The observed correlation between chlorophyll and laminarin suggests an annual production of algal laminarin of 12 ± 8 gigatons: that is, approximately three times the annual atmospheric carbon dioxide increase by fossil fuel burning. Moreover, our data revealed that laminarin accounted for up to 50% of organic carbon in sinking diatom-containing particles, thus substantially contributing to carbon export from surface waters. Spatially and temporally variable laminarin concentrations in the sunlit ocean are driven by light availability. Collectively, these observations highlight the prominent ecological role and biogeochemical function of laminarin in oceanic carbon export and energy flow to higher trophic levels.



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Article
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ISI/Scopus peer-reviewed
Publication Status
Published
Eprint ID
51447
DOI 10.1073/pnas.1917001117

Cite as
Becker, S. , Tebben, J. , Coffinet, S. , Wiltshire, K. H. , Iversen, M. , Harder, T. , Hinrichs, K. U. and Hehemann, J. H. (2020): Laminarin is a major molecule in the marine carbon cycle , Proceedings of the National Academy of Sciences . doi: 10.1073/pnas.1917001117


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