Major imprint of surface plankton on deep ocean prokaryotic structure and activity.

bacterial activity carbon export deep ocean fluorescent dissolved organic matter marine prokaryotic communities microbial dispersal particle sinking particle-attached surface phytoplankton

Journal

Molecular ecology
ISSN: 1365-294X
Titre abrégé: Mol Ecol
Pays: England
ID NLM: 9214478

Informations de publication

Date de publication:
05 2020
Historique:
received: 12 11 2019
revised: 12 03 2020
accepted: 16 04 2020
pubmed: 24 4 2020
medline: 5 6 2021
entrez: 24 4 2020
Statut: ppublish

Résumé

Deep ocean microbial communities rely on the organic carbon produced in the sunlit ocean, yet it remains unknown whether surface processes determine the assembly and function of bathypelagic prokaryotes to a larger extent than deep-sea physicochemical conditions. Here, we explored whether variations in surface phytoplankton assemblages across Atlantic, Pacific and Indian ocean stations can explain structural changes in bathypelagic (ca. 4,000 m) free-living and particle-attached prokaryotic communities (characterized through 16S rRNA gene sequencing), as well as changes in prokaryotic activity and dissolved organic matter (DOM) quality. We show that the spatial structuring of prokaryotic communities in the bathypelagic strongly followed variations in the abundances of surface dinoflagellates and ciliates, as well as gradients in surface primary productivity, but were less influenced by bathypelagic physicochemical conditions. Amino acid-like DOM components in the bathypelagic reflected variations of those components in surface waters, and seemed to control bathypelagic prokaryotic activity. The imprint of surface conditions was more evident in bathypelagic than in shallower mesopelagic (200-1,000 m) communities, suggesting a direct connectivity through fast-sinking particles that escape mesopelagic transformations. Finally, we identified a pool of endemic deep-sea prokaryotic taxa (including potentially chemoautotrophic groups) that appear less connected to surface processes than those bathypelagic taxa with a widespread vertical distribution. Our results suggest that surface planktonic communities shape the spatial structure of the bathypelagic microbiome to a larger extent than the local physicochemical environment, likely through determining the nature of the sinking particles and the associated prokaryotes reaching bathypelagic waters.

Identifiants

pubmed: 32323882
doi: 10.1111/mec.15454
doi:

Substances chimiques

RNA, Ribosomal, 16S 0

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

1820-1838

Informations de copyright

© 2020 John Wiley & Sons Ltd.

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Auteurs

Clara Ruiz-González (C)

Institut de Ciències del Mar (ICM-CSIC), Barcelona, Spain.

Mireia Mestre (M)

Institut de Ciències del Mar (ICM-CSIC), Barcelona, Spain.
Centro FONDAP de Investigación en Dinámica de Ecosistemas Marinos de Altas Latitudes (IDEAL), Universidad Austral de Chile, Valdivia, Chile.
Centro de Investigación Oceanográfica COPAS Sur-Austral, Departamento de Oceanografía, Universidad de Concepción, Concepción, Chile.

Marta Estrada (M)

Institut de Ciències del Mar (ICM-CSIC), Barcelona, Spain.

Marta Sebastián (M)

Institut de Ciències del Mar (ICM-CSIC), Barcelona, Spain.
Instituto de Oceanografía y Cambio Global, IOCAG, Universidad de Las Palmas de Gran Canaria (ULPGC), Las Palmas, Spain.

Guillem Salazar (G)

Institut de Ciències del Mar (ICM-CSIC), Barcelona, Spain.
Department of Biology, Institute of Microbiology and Swiss Institute of Bioinformatics, ETH Zurich, Zurich, Switzerland.

Susana Agustí (S)

Red Sea Research Center (RSRC), King Abdullah University of Science and Technology, Thuwal, Saudi Arabia.

Enrique Moreno-Ostos (E)

Department of Ecology and Geology, Marine Ecology and Limnology Research Group, CEIMAR, University of Málaga, Málaga, Spain.

Isabel Reche (I)

Departamento de Ecología and Research Unit Modeling Nature (MNat), Universidad de Granada, Granada, Spain.

Xosé Antón Álvarez-Salgado (XA)

Instituto de Investigacións Mariñas (IIM-CSIC), Vigo, Spain.

Xosé Anxelu G Morán (XAG)

Red Sea Research Center (RSRC), King Abdullah University of Science and Technology, Thuwal, Saudi Arabia.

Carlos M Duarte (CM)

Red Sea Research Center (RSRC), King Abdullah University of Science and Technology, Thuwal, Saudi Arabia.

M Montserrat Sala (MM)

Institut de Ciències del Mar (ICM-CSIC), Barcelona, Spain.

Josep M Gasol (JM)

Institut de Ciències del Mar (ICM-CSIC), Barcelona, Spain.
Centre for Marine Ecosystems Research, School of Science, Edith Cowan University, Joondalup, WA, Australia.

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