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Microbial succession in a marine sediment: Inferring interspecific microbial interactions with marine cable bacteria

Cable bacteria are long, filamentous, multicellular bacteria that grow in marine sediments and couple sulfide oxidation to oxygen reduction over centimetre‐scale distances via long‐distance electron transport. Cable bacteria can strongly modify biogeochemical cycling and may affect microbial communi...

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Autores principales: Liau, Pinky, Kim, Carol, Saxton, Matthew A., Malkin, Sairah Y.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley & Sons, Inc. 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10092204/
https://www.ncbi.nlm.nih.gov/pubmed/36178156
http://dx.doi.org/10.1111/1462-2920.16230
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author Liau, Pinky
Kim, Carol
Saxton, Matthew A.
Malkin, Sairah Y.
author_facet Liau, Pinky
Kim, Carol
Saxton, Matthew A.
Malkin, Sairah Y.
author_sort Liau, Pinky
collection PubMed
description Cable bacteria are long, filamentous, multicellular bacteria that grow in marine sediments and couple sulfide oxidation to oxygen reduction over centimetre‐scale distances via long‐distance electron transport. Cable bacteria can strongly modify biogeochemical cycling and may affect microbial community networks. Here we examine interspecific interactions with marine cable bacteria (Ca. Electrothrix) by monitoring the succession of 16S rRNA amplicons (DNA and RNA) and cell abundance across depth and time, contrasting sediments with and without cable bacteria growth. In the oxic zone, cable bacteria activity was positively associated with abundant predatory bacteria (Bdellovibrionota, Myxococcota, Bradymonadales), indicating putative predation on cathodic cells. At suboxic depths, cable bacteria activity was positively associated with sulfate‐reducing and magnetotactic bacteria, consistent with cable bacteria functioning as ecosystem engineers that modify their local biogeochemical environment, benefitting certain microbes. Cable bacteria activity was negatively associated with chemoautotrophic sulfur‐oxidizing Gammaproteobacteria (Thiogranum, Sedimenticola) at oxic depths, suggesting competition, and positively correlated with these taxa at suboxic depths, suggesting syntrophy and/or facilitation. These observations are consistent with chemoautotrophic sulfur oxidizers benefitting from an oxidizing potential imparted by cable bacteria at suboxic depths, possibly by using cable bacteria as acceptors for electrons or electron equivalents, but by an as yet enigmatic mechanism.
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spelling pubmed-100922042023-04-13 Microbial succession in a marine sediment: Inferring interspecific microbial interactions with marine cable bacteria Liau, Pinky Kim, Carol Saxton, Matthew A. Malkin, Sairah Y. Environ Microbiol Research Articles Cable bacteria are long, filamentous, multicellular bacteria that grow in marine sediments and couple sulfide oxidation to oxygen reduction over centimetre‐scale distances via long‐distance electron transport. Cable bacteria can strongly modify biogeochemical cycling and may affect microbial community networks. Here we examine interspecific interactions with marine cable bacteria (Ca. Electrothrix) by monitoring the succession of 16S rRNA amplicons (DNA and RNA) and cell abundance across depth and time, contrasting sediments with and without cable bacteria growth. In the oxic zone, cable bacteria activity was positively associated with abundant predatory bacteria (Bdellovibrionota, Myxococcota, Bradymonadales), indicating putative predation on cathodic cells. At suboxic depths, cable bacteria activity was positively associated with sulfate‐reducing and magnetotactic bacteria, consistent with cable bacteria functioning as ecosystem engineers that modify their local biogeochemical environment, benefitting certain microbes. Cable bacteria activity was negatively associated with chemoautotrophic sulfur‐oxidizing Gammaproteobacteria (Thiogranum, Sedimenticola) at oxic depths, suggesting competition, and positively correlated with these taxa at suboxic depths, suggesting syntrophy and/or facilitation. These observations are consistent with chemoautotrophic sulfur oxidizers benefitting from an oxidizing potential imparted by cable bacteria at suboxic depths, possibly by using cable bacteria as acceptors for electrons or electron equivalents, but by an as yet enigmatic mechanism. John Wiley & Sons, Inc. 2022-10-17 2022-12 /pmc/articles/PMC10092204/ /pubmed/36178156 http://dx.doi.org/10.1111/1462-2920.16230 Text en © 2022 The Authors. Environmental Microbiology published by Society for Applied Microbiology and John Wiley & Sons Ltd. https://creativecommons.org/licenses/by-nc/4.0/This is an open access article under the terms of the http://creativecommons.org/licenses/by-nc/4.0/ (https://creativecommons.org/licenses/by-nc/4.0/) License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes.
spellingShingle Research Articles
Liau, Pinky
Kim, Carol
Saxton, Matthew A.
Malkin, Sairah Y.
Microbial succession in a marine sediment: Inferring interspecific microbial interactions with marine cable bacteria
title Microbial succession in a marine sediment: Inferring interspecific microbial interactions with marine cable bacteria
title_full Microbial succession in a marine sediment: Inferring interspecific microbial interactions with marine cable bacteria
title_fullStr Microbial succession in a marine sediment: Inferring interspecific microbial interactions with marine cable bacteria
title_full_unstemmed Microbial succession in a marine sediment: Inferring interspecific microbial interactions with marine cable bacteria
title_short Microbial succession in a marine sediment: Inferring interspecific microbial interactions with marine cable bacteria
title_sort microbial succession in a marine sediment: inferring interspecific microbial interactions with marine cable bacteria
topic Research Articles
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10092204/
https://www.ncbi.nlm.nih.gov/pubmed/36178156
http://dx.doi.org/10.1111/1462-2920.16230
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