In situ development of a methanotrophic microbiome in deep-sea sediments.


Journal

The ISME journal
ISSN: 1751-7370
Titre abrégé: ISME J
Pays: England
ID NLM: 101301086

Informations de publication

Date de publication:
01 2019
Historique:
received: 13 02 2018
accepted: 04 08 2018
revised: 06 07 2018
pubmed: 30 8 2018
medline: 1 8 2019
entrez: 30 8 2018
Statut: ppublish

Résumé

Emission of the greenhouse gas methane from the seabed is globally controlled by marine aerobic and anaerobic methanotrophs gaining energy via methane oxidation. However, the processes involved in the assembly and dynamics of methanotrophic populations in complex natural microbial communities remain unclear. Here we investigated the development of a methanotrophic microbiome following subsurface mud eruptions at Håkon Mosby mud volcano (1250 m water depth). Freshly erupted muds hosted deep-subsurface communities that were dominated by Bathyarchaeota, Atribacteria and Chloroflexi. Methanotrophy was initially limited to a thin surface layer of Methylococcales populations consuming methane aerobically. With increasing distance to the eruptive center, anaerobic methanotrophic archaea, sulfate-reducing Desulfobacterales and thiotrophic Beggiatoaceae developed, and their respective metabolic capabilities dominated the biogeochemical functions of the community. Microbial richness, evenness, and cell numbers of the entire microbial community increased up to tenfold within a few years downstream of the mud flow from the eruptive center. The increasing diversity was accompanied by an up to fourfold increase in sequence abundance of relevant metabolic genes of the anaerobic methanotrophic and thiotrophic guilds. The communities fundamentally changed in their structure and functions as reflected in the metagenome turnover with distance from the eruptive center, and this was reflected in the biogeochemical zonation across the mud volcano caldera. The observed functional succession provides a framework for the response time and recovery of complex methanotrophic communities after disturbances of the deep-sea bed.

Identifiants

pubmed: 30154496
doi: 10.1038/s41396-018-0263-1
pii: 10.1038/s41396-018-0263-1
pmc: PMC6298960
doi:

Substances chimiques

RNA, Ribosomal, 16S 0
Methane OP0UW79H66

Types de publication

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

Langues

eng

Pagination

197-213

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Auteurs

S E Ruff (SE)

Max Planck Institute for Marine Microbiology, Bremen, Germany. emil.ruff@ucalgary.ca.
Department of Geoscience, University of Calgary, Calgary, AB, Canada. emil.ruff@ucalgary.ca.

J Felden (J)

Max Planck Institute for Marine Microbiology, Bremen, Germany.
MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.

H R Gruber-Vodicka (HR)

Max Planck Institute for Marine Microbiology, Bremen, Germany.

Y Marcon (Y)

MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.
Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany.

K Knittel (K)

Max Planck Institute for Marine Microbiology, Bremen, Germany.

A Ramette (A)

Max Planck Institute for Marine Microbiology, Bremen, Germany.
Institute for Infectious Diseases, University of Bern, Bern, Switzerland.

A Boetius (A)

Max Planck Institute for Marine Microbiology, Bremen, Germany. antje.boetius@awi.de.
MARUM Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany. antje.boetius@awi.de.
Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany. antje.boetius@awi.de.

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Animals Hemiptera Insect Proteins Phylogeny Insecticides
Populus Soil Microbiology Soil Microbiota Fungi
Amaryllidaceae Alkaloids Lycoris NADPH-Ferrihemoprotein Reductase Gene Expression Regulation, Plant Plant Proteins

Classifications MeSH