Bivalve shell horizons in seafloor pockmarks of the last glacial-interglacial transition: A thousand years of methane emissions in the Arctic Ocean

Abstract

We studied discrete bivalve shell horizons in two gravity cores from seafloor pockmarks on theVestnesa Ridge (1200 m water depth) and western Svalbard (798000 N, 068550 W) to provide insight intothe temporal and spatial dynamics of seabed methane seeps. The shell beds, dominated by two genera ofthe family Vesicomyidae: Phreagena s.l. and Isorropodon sp., were 20–30 cm thick and centered at 250–400 cm deep in the cores. The carbon isotope composition of inorganic (d13C from 213.02& to 12.36&)and organic (d13C from 229.28& to 221.33&) shell material and a two-end member mixing model indicatethat these taxa derived between 8% and 43% of their nutrition from chemosynthetic bacteria. In addition,negative d13C values for planktonic foraminifera (26.7& to 23.1&), concretions identified asmethane-derived authigenic carbonates, and pyrite-encrusted fossil worm tubes at the shell horizons indicatea sustained paleo-methane seep environment. Combining sedimentation rates with 14C ages forbivalve material from the shell horizons, we estimate the horizons persisted for about 1000 years betweenapproximately 17,707 and 16,680 years B.P. (corrected). The seepage event over a 1000 year time intervalwas most likely associated with regional stress-related faulting and the subsequent release of overpressurizedfluids.