Multiple proxies in the geological record offshore NW Svalbard track shallow subseafloor
diagenesis and seafloor methane seepage during the Last Glacial Maximum (LGM) extent …

Large amounts of methane are trapped within gas hydrate in subseabed sediments in the
Arctic Ocean, and bottom-water warming may induce the release of methane from the …

Natural gas hydrate deposits (NGHD) have been investigated for decades and represent
one of the major methane reservoirs on Earth. They are encountered in sediment of both the …

Cold seep ecosystems are characterized by a dense accumulation of chemosynthetic
communities that utilize the chemical energy contained in fluids. Due to various technical …

Methane seepage occurs across the western Svalbard margin at water depths ranging
from< 300 m, landward from the shelf break, to> 1000 m in regions just a few kilometres from …

The highest concentration of cold seep sites worldwide has been observed along
convergent margins, where fluid migration through sedimentary sequences is enhanced by …

Current estimations of seabed methane release into the ocean (0.4–48 Tg yr− 1) are based
on short‐term observations and implicitly assume that fluxes are constant over time …

Automatic detection of seismic events in ocean bottom seismometer (OBS) data is difficult
due to elevated levels of noise compared to the recordings from land. Popular deep-learning …

Ocean‐bottom seismometers (OBSs) commonly record short‐duration events (SDEs) that
could be described by all of these characteristics:(i) duration< 1 s,(ii) one single‐wave train …

Improved quantification techniques of natural sources is needed to explain variations in
atmospheric methane. In polar regions, high uncertainties in current estimates of methane …