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dc.contributor.authorRojas, Connie A.
dc.contributor.authorDe Santiago Torio, Ana
dc.contributor.authorPark, Serry
dc.contributor.authorBosak, Tanja
dc.contributor.authorKlepac-Ceraj, Vanja
dc.date.accessioned2021-09-27T14:48:03Z
dc.date.available2021-09-27T14:48:03Z
dc.date.issued2021-04
dc.date.submitted2020-10
dc.identifier.issn1664-302X
dc.identifier.urihttps://hdl.handle.net/1721.1/132642
dc.description.abstractThe extent to which nutrients structure microbial communities in permanently stratified lakes is not well understood. This study characterized microbial communities from the anoxic layers of the meromictic and sulfidic Fayetteville Green Lake (FGL), NY, United States, and investigated the roles of organic electron donors and terminal electron acceptors in shaping microbial community structure and interactions. Bacterial communities from the permanently stratified layer below the chemocline (monimolimnion) and from enrichment cultures inoculated by lake sediments were analyzed using 16S rRNA gene sequencing. Results showed that anoxygenic phototrophs dominated microbial communities in the upper monimolimnion (21 m), which harbored little diversity, whereas the most diverse communities resided at the bottom of the lake (∼52 m). Organic electron donors explained 54% of the variation in the microbial community structure in aphotic cultures enriched on an array of organic electron donors and different inorganic electron acceptors. Electron acceptors only explained 10% of the variation, but were stronger drivers of community assembly in enrichment cultures supplemented with acetate or butyrate compared to the cultures amended by chitin, lignin or cellulose. We identified a range of habitat generalists and habitat specialists in both the water column and enrichment samples using Levin’s index. Network analyses of interactions among microbial groups revealed Chlorobi and sulfate reducers as central to microbial interactions in the upper monimolimnion, while Syntrophaceae and other fermenting organisms were more important in the lower monimolimnion. The presence of photosynthetic microbes and communities that degrade chitin and cellulose far below the chemocline supported the downward transport of microbes, organic matter and oxidants from the surface and the chemocline. Collectively, our data suggest niche partitioning of bacterial communities via interactions that depend on the availability of different organic electron donors and terminal electron acceptors. Thus, light, as well as the diversity and availability of chemical resources drive community structure and function in FGL, and likely in other stratified, meromictic lakes.en_US
dc.description.sponsorshipSimons Foundation (Award 327126)en_US
dc.publisherFrontiers Media SAen_US
dc.relation.isversionofhttps://doi.org/10.3389/fmicb.2021.620424en_US
dc.rightsCreative Commons Attribution 4.0 International licenseen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.sourceFrontiersen_US
dc.titleOrganic Electron Donors and Terminal Electron Acceptors Structure Anaerobic Microbial Communities and Interactions in a Permanently Stratified Sulfidic Lakeen_US
dc.typeArticleen_US
dc.identifier.citationRojas, Connie A. et al. "Organic Electron Donors and Terminal Electron Acceptors Structure Anaerobic Microbial Communities and Interactions in a Permanently Stratified Sulfidic Lake." Frontiers in Microbiology 12 (April 2021): 620424. © 2021 Rojas et al.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.relation.journalFrontiers in Microbiologyen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.date.submission2021-04-28T14:30:26Z
mit.journal.volume12en_US
mit.licensePUBLISHER_CC
mit.metadata.statusCompleteen_US


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