Gas hydrate, a frozen, naturally‐occurring, and highly‐concentrated form of methane,
sequesters significant carbon in the global system and is stable only over a range of low …

In response to the accelerating processes of marine natural gas hydrate exploration and gas
production from hydrate-bearing sediments, their potential impacts on the environment have …

Ocean warming related to climate change has been proposed to cause the dissociation of
gas hydrate deposits and methane leakage on the seafloor. This process occurs in places …

We demonstrate direct eddy covariance (EC) observations of methane (CH4) fluxes
between the sea and atmosphere from an icebreaker in the eastern Arctic Ocean. EC …

Two areas with cold methane seeps on the outer shelf of the Laptev Sea were studied by
two interdisciplinary expeditions onboard the RV Akademik Mstislav Keldysh in August …

Positive feedbacks (self-reinforcing cycles) within the climate system have the potential to
accelerate human-induced climate change and even shift the Earth's climate system, in part …

Benthic communities below the photic zone are largely reliant on the export of surface-water
primary production and the flux of partially degraded organic matter to the seabed, ie …

Significant reserves of methane (CH 4) are held in the Arctic shelf, but the release of CH 4 to
the overlying ocean and, subsequently, to the atmosphere has been believed to be …

Cold-seep benthic communities in the Arctic exist at the nexus of two extreme environments;
one reflecting the harsh physical extremes of the Arctic environment and another reflecting …

Abstract The Calcare di Base is a carbonate/evaporitic unit formed before the deposition of
the massive halite bodies in the main depozones of the Mediterranean region, and has been …