Heyl, Taylor P., Panieri, Giuliana, Fornari, Daniel J., Mattingsdal, Rune, Sauer, Simone, Yao, Haoyi, McCartin, Luke, McElwee, Elisabeth, and Shank, Timothy M.
The continental margins of the Arctic Ocean basin contain methane seeps, where transient fluxes of seafloor methane are released due to the thermal dissociation of gas hydrates. An increase in shallow methane seeps identified over the past decade, potentially due to enhanced warming of the Arctic Ocean bottom water and associated destabilization of hydrate structure. Biological communities associated with methane release east of Svalbard in the Barents Sea (Storbanken Crater site, 76° 46.7′N, 35° 43.5′E, depths between 120 m–300 m depths) were investigated using towed camera imagery and ship-based platforms during a 2017 CAGE17-2 cruise on the RV Helmer Hanssen. We analyzed relationships among methane flux data, seafloor habitat characteristics, and biological community structure (i.e., presence and distribution of megafauna and expression of microbial mats) from a total of 14 surveys (6827 images and 40 multicore sediment cores) within the Storbanken Crater area and compared it to 2015 data. Unlike seep expressions at deeper sites (∼1200 m) in the Norwegian margin region, no seep-endemic, chemosynthetic-associated megafaunal species were observed at the shallow surveyed sites and all sites hosted similarly diverse communities of non-seep species, including commercially important fish and crustaceans. Methane concentrations did not markedly differ between the crater and non-crater sites. Rates of methane gas advection through sediments (in the form of flares) were relatively low and concentration of methane was even lower in porewater samples at the crater site. We present the first evidence of methane flare flux and intermittent microbial mat distribution with associated folliculinid ciliates, which suggests a long history of methane emissions and a transient seep environment in spatial and temporal flux. Together, this study presents a critical baseline on the temporal release of arctic methane and benthic biological communities to initiate temporal studies that identify future changes and predict the impact of climate change. • Reduced methane flares along the Norwegian margin and low methane in the sediment suggest a transient seep environment. • Metazoan community structure within the Storbanken Crater area revealed high diversity between crater and non-crater sites. • We present the first evidence of methane release with microbial mat distribution and associated folliculinid ciliates. • No chemosynthetic megafaunal species were observed among areas of seep expression in the areas surveyed. • We provide baseline information on temporal methane release and biological communities in the Arctic. [ABSTRACT FROM AUTHOR]