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There are two distinct types of oceanic deposit. The most common is dominated (> 99%) by methane contained in a structure I clathrate and generally found at depth in the sediment. Here, the methane is isotopically light (δ13C < -60‰) which indicates that it is derived from the microbial reduction of CO2. The clathrates in these deep deposits are thought to have formed in-situ from the microbially-produced methane, as the δ13C values of clathrate and surrounding dissolved methane are similar.[6]
These deposits are located within a mid-depth zone around 300-500 m thick in the sediments (the Gas Hydrate Stability Zone, or GHSZ) where they coexist with methane dissolved in the pore-waters. Above this zone methane is only present in its dissolved form at concentrations that decrease towards the sediment surface. Below it, methane is gaseous. At Blake Ridge on the Atlantic continental rise, the GHSZ started at 190 m depth and continued to 450 m, where it reached equilibrium with the gaseous phase. Measurements indicated that methane occupied 0-9% by volume in the GHSZ, and ~12% in the gaseous zone.[7]
In the less common second type found near the sediment surface some samples have a higher proportion of longer-chain hydrocarbons (
Originally posted by punkinworks
There are billions and billions of tons of methane locked up in the frozen muds of arctic permafrost. These desposits have nothing to due with vulcanism.
There are large deposits of methane on the seafloor in a form as people have mentioned of methane hydrates.
These deposits will have a major effect of global temperatures if they are released.
Methane is released in volcanoes but in small amounts, volcanic gasses are mostly watervapor and hydrogen and sulfur compounds.
Originally posted by pavil
I will have to research it more. I find it hard to believe that temps at the bottom of the ocean floor have changed much, if at all, when the overall change in ocean temp has been relatively so small. It would have to be a substantial increase in water temp to change the water temp at that depth.
Originally posted by pavil
I am sure methane is constantly leaking from the ocean floor in spots. If it were a widespread phenomena it would be easy to detect.
Originally posted by pavil
Personally, I would worry more about the permafrost in the Arctic tundra melting first and releasing it's methane. That would probably happen before ocean temps reach the point of massive methane release.
A section of the Arctic Ocean seafloor that holds vast stores of frozen methane is showing signs of instability and widespread venting of the powerful greenhouse gas, according to the findings of an international research team led by University of Alaska Fairbanks scientists Natalia Shakhova and Igor Semiletov.
Originally posted by K-Raz
reply to post by Nineteen
Volcanic activity off the sea of norway? Didn't know scandinavia was tectonichally active? There are methane deposits all over the planet, and it truly can set of a runaway effect - Same with the sibirian tundra and bogs.
I wish we could end the debate as to wether or not it's man made, and start focusing on what to do about it. The weather wont be getting more pleasant anywhere on the globe.