Phosphonate production by marine microbes: Exploring new sources and potential function

dc.contributor.authorAcker Marianne
dc.contributor.authorHogle Shane L.
dc.contributor.authorBerube Paul M.
dc.contributor.authorHackl Thomas
dc.contributor.authorCoe Allison
dc.contributor.authorStepanauskas Ramunas
dc.contributor.authorChisholm Sallie W.
dc.contributor.authorRepeta Daniel J.
dc.contributor.organizationfi=fysiologia ja genetiikka|en=Physiology and Genetics|
dc.contributor.organization-code1.2.246.10.2458963.20.70712835001
dc.converis.publication-id73953586
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/73953586
dc.date.accessioned2022-10-28T14:20:27Z
dc.date.available2022-10-28T14:20:27Z
dc.description.abstract<p>Phosphonates are organophosphorus metabolites with a characteristic C-P bond. They are ubiquitous in the marine environment, their degradation broadly supports ecosystem productivity, and they are key components of the marine phosphorus (P) cycle. However, the microbial producers that sustain the large oceanic inventory of phosphonates as well as the physiological and ecological roles of phosphonates are enigmatic. Here, we show that phosphonate synthesis genes are rare but widely distributed among diverse bacteria and archaea, including <em>Prochlorococcus</em> and SAR11, the two major groups of bacteria in the ocean. In addition, we show that <em>Prochlorococcus</em> can allocate over 40% of its total cellular P-quota toward phosphonate production. However, we find no evidence that <em>Prochlorococcus</em> uses phosphonates for surplus P storage, and nearly all producer genomes lack the genes necessary to degrade and assimilate phosphonates. Instead, we postulate that phosphonates are associated with cell-surface glycoproteins, suggesting that phosphonates mediate ecological interactions between the cell and its surrounding environment. Our findings indicate that the oligotrophic surface ocean phosphonate pool is sustained by a relatively small fraction of the bacterioplankton cells allocating a significant portion of their P quotas toward secondary metabolism and away from growth and reproduction.<br></p>
dc.identifier.jour-issn0027-8424
dc.identifier.olddbid187691
dc.identifier.oldhandle10024/170785
dc.identifier.urihttps://www.utupub.fi/handle/11111/43206
dc.identifier.urlhttps://www.pnas.org/doi/full/10.1073/pnas.2113386119
dc.identifier.urnURN:NBN:fi-fe2022081154951
dc.language.isoen
dc.okm.affiliatedauthorHogle, Shane
dc.okm.discipline1172 Environmental sciencesen_GB
dc.okm.discipline1181 Ecology, evolutionary biologyen_GB
dc.okm.discipline1172 Ympäristötiedefi_FI
dc.okm.discipline1181 Ekologia, evoluutiobiologiafi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherProceedings of the National Academy of Sciences of the United States of America
dc.publisher.countryUnited Statesen_GB
dc.publisher.countryYhdysvallat (USA)fi_FI
dc.publisher.country-codeUS
dc.relation.articlenumbere2113386119
dc.relation.doi10.1073/pnas.2113386119
dc.relation.ispartofjournalProceedings of the National Academy of Sciences of the United States of America
dc.relation.issue11
dc.relation.volume119
dc.source.identifierhttps://www.utupub.fi/handle/10024/170785
dc.titlePhosphonate production by marine microbes: Exploring new sources and potential function
dc.year.issued2022

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