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Verrucomicrobiota Are Specialist Consumers of Sulfated Methyl Pentoses During Diatom Blooms

Overview
Journal ISME J
Date 2021 Sep 8
PMID 34493810
Citations 48
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Abstract

Marine algae annually sequester petagrams of carbon dioxide into polysaccharides, which are a central metabolic fuel for marine carbon cycling. Diatom microalgae produce sulfated polysaccharides containing methyl pentoses that are challenging to degrade for bacteria compared to other monomers, implicating these sugars as a potential carbon sink. Free-living bacteria occurring in phytoplankton blooms that specialise on consuming microalgal sugars, containing fucose and rhamnose remain unknown. Here, genomic and proteomic data indicate that small, coccoid, free-living Verrucomicrobiota specialise in fucose and rhamnose consumption during spring algal blooms in the North Sea. Verrucomicrobiota cell abundance was coupled with the algae bloom onset and accounted for up to 8% of the bacterioplankton. Glycoside hydrolases, sulfatases, and bacterial microcompartments, critical proteins for the consumption of fucosylated and sulfated polysaccharides, were actively expressed during consecutive spring bloom events. These specialised pathways were assigned to novel and discrete candidate species of the Akkermansiaceae and Puniceicoccaceae families, which we here describe as Candidatus Mariakkermansia forsetii and Candidatus Fucivorax forsetii. Moreover, our results suggest specialised metabolic pathways could determine the fate of complex polysaccharides consumed during algae blooms. Thus the sequestration of phytoplankton organic matter via methyl pentose sugars likely depend on the activity of specialised Verrucomicrobiota populations.

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References
1.
Laine R . A calculation of all possible oligosaccharide isomers both branched and linear yields 1.05 x 10(12) structures for a reducing hexasaccharide: the Isomer Barrier to development of single-method saccharide sequencing or synthesis systems. Glycobiology. 1994; 4(6):759-67. DOI: 10.1093/glycob/4.6.759. View

2.
Varki A . Biological roles of glycans. Glycobiology. 2016; 27(1):3-49. PMC: 5884436. DOI: 10.1093/glycob/cww086. View

3.
Teeling H, Fuchs B, Becher D, Klockow C, Gardebrecht A, Bennke C . Substrate-controlled succession of marine bacterioplankton populations induced by a phytoplankton bloom. Science. 2012; 336(6081):608-11. DOI: 10.1126/science.1218344. View

4.
Field , Behrenfeld , Randerson , Falkowski . Primary production of the biosphere: integrating terrestrial and oceanic components . Science. 1998; 281(5374):237-40. DOI: 10.1126/science.281.5374.237. View

5.
Reintjes G, Fuchs B, Scharfe M, Wiltshire K, Amann R, Arnosti C . Short-term changes in polysaccharide utilization mechanisms of marine bacterioplankton during a spring phytoplankton bloom. Environ Microbiol. 2020; 22(5):1884-1900. DOI: 10.1111/1462-2920.14971. View