Geophysical and geochemical controls on the megafaunal community of a high Arctic cold seep
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Published:2018-07-25
Issue:14
Volume:15
Page:4533-4559
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ISSN:1726-4189
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Container-title:Biogeosciences
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language:en
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Short-container-title:Biogeosciences
Author:
Sen Arunima, Åström Emmelie K. L.ORCID, Hong Wei-LiORCID, Portnov Alexey, Waage MalinORCID, Serov Pavel, Carroll Michael L., Carroll JoLynn
Abstract
Abstract. Cold-seep megafaunal communities around gas hydrate mounds (pingos) in the
western Barents Sea (76∘ N, 16∘ E, ∼400 m
depth) were investigated with high-resolution, geographically referenced
images acquired with an ROV and towed camera. Four pingos associated with
seabed methane release hosted diverse biological communities of mainly
nonseep (background) species including commercially important fish and
crustaceans, as well as a species new to this area (the snow crab
Chionoecetes opilio). We attribute the presence of most benthic
community members to habitat heterogeneity and the occurrence of hard
substrates (methane-derived authigenic carbonates), particularly the most
abundant phyla (Cnidaria and Porifera), though food availability and exposure
to a diverse microbial community is also important for certain taxa. Only one
chemosynthesis-based species was confirmed, the siboglinid frenulate
polychaete Oligobrachia cf. haakonmosbiensis. Overall, the
pingo communities formed two distinct clusters, distinguished by the presence
or absence of frenulate aggregations. Methane gas advection through sediments
was low, below the single pingo that lacked frenulate aggregations, while
seismic profiles indicated abundant gas-saturated sediment below the other
frenulate-colonized pingos. The absence of frenulate aggregations could not
be explained by sediment sulfide concentrations, despite these worms likely
containing sulfide-oxidizing symbionts. We propose that high levels of
seafloor methane seepage linked to subsurface gas reservoirs support an
abundant and active sediment methanotrophic community that maintains high
sulfide fluxes and serves as a carbon source for frenulate worms. The pingo
currently lacking a large subsurface gas source and lower methane
concentrations likely has lower sulfide flux rates and limited amounts of
carbon, insufficient to support large populations of frenulates. Two
previously undocumented behaviors were visible through the images: grazing
activity of snow crabs on bacterial mats, and seafloor crawling of
Nothria conchylega onuphid polychaetes.
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
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