Methane in the seafloor
Methane hydrates are ice-like solids that form when methane (natural gas) combines with seawater at the low temperatures and high pressures of the deep sea. There are also places where methane naturally seeps from the seafloor in bubbles, rising to the surface and into the atmosphere.
Arctic shelf edge
MBARI has participated in three research cruises in the Canadian Beaufort Sea, using an inspection class ROV) to visualize the seafloor and collect samples.
Deep-Sea Chemistry
Northern 2014 Expedition
Hydrates and seeps
In the late 1970s, oceanographers were astounded to discover flourishing communities of animals clustered around deep-sea hydrothermal vents.
Gas Hydrates
Northern 2013 Expedition
Expedition to study methane gas bubbling out of the Arctic seafloor
Sept 21, 2012 – In the remote, ice-shrouded Beaufort Sea, methane (the main component in natural gas) has been bubbling out of the seafloor for thousands of years. MBARI geologist Charlie Paull and his colleagues at the Geological Survey of Canada are trying to figure out where this gas is coming from, how fast it is bubbling out of the sediments, and how it affects the shape and stability of the seafloor.
Science
- Upper-ocean systems
- Midwater research
- Seafloor processes
- Areas of study
- Past research
- Research publications
