The Impact of Methane on Microbial Communities at Marine Arctic Gas Hydrate Bearing Sediment

Publikation: Bidrag til tidsskrift/Konferencebidrag i tidsskrift /Bidrag til avisTidsskriftartikelForskningpeer review

DOI

  • Vincent Carrier, UiT The Arctic University of Norway
  • ,
  • Mette M. Svenning, UiT The Arctic University of Norway
  • ,
  • Friederike Gründger
  • Helge Niemann, UiT The Arctic University of Norway, Royal Netherlands Institute for Sea Research - NIOZ, Utrecht University
  • ,
  • Pierre Antoine Dessandier, UiT The Arctic University of Norway
  • ,
  • Giuliana Panieri, UiT The Arctic University of Norway
  • ,
  • Dimitri Kalenitchenko, UiT The Arctic University of Norway

Cold seeps are characterized by high biomass, which is supported by the microbial oxidation of the available methane by capable microorganisms. The carbon is subsequently transferred to higher trophic levels. South of Svalbard, five geological mounds shaped by the formation of methane gas hydrates, have been recently located. Methane gas seeping activity has been observed on four of them, and flares were primarily concentrated at their summits. At three of these mounds, and along a distance gradient from their summit to their outskirt, we investigated the eukaryotic and prokaryotic biodiversity linked to 16S and 18S rDNA. Here we show that local methane seepage and other environmental conditions did affect the microbial community structure and composition. We could not demonstrate a community gradient from the summit to the edge of the mounds. Instead, a similar community structure in any methane-rich sediments could be retrieved at any location on these mounds. The oxidation of methane was largely driven by anaerobic methanotrophic Archaea-1 (ANME-1) and the communities also hosted high relative abundances of sulfate reducing bacterial groups although none demonstrated a clear co-occurrence with the predominance of ANME-1. Additional common taxa were observed and their abundances were likely benefiting from the end products of methane oxidation. Among these were sulfide-oxidizing Campilobacterota, organic matter degraders, such as Bathyarchaeota, Woesearchaeota, or thermoplasmatales marine benthic group D, and heterotrophic ciliates and Cercozoa.

OriginalsprogEngelsk
Artikelnummer1932
TidsskriftFrontiers in Microbiology
Vol/bind11
ISSN1664-302X
DOI
StatusUdgivet - sep. 2020

Se relationer på Aarhus Universitet Citationsformater

ID: 199122501