In three different and very interesting papers, CAGE, has now documented both prolific seepage and accumulation of hydrocarbon gases partly produced by serpentinization of ultramafic rocks, west of Svalbard. The papers are Plaza-Faverola, et al. (GRL, 2015); Johnson, et al. (Geology, 2015, doi: 10.1130/G3644.1), and Rajan, et al. (GRL, 2012, doi: 10.1029/2011JB008537). Together, these three papers suggest that there is a net positive production of abiotic methane that is temporarily stored as shallow gas hydrates, partly continuously released to the water column and atmosphere, and partly stored over long time in shallow, high-porosity drift sediments. As the gas production and accumulation is completely independent of the existence of a normal petroleum 'source-rock', and is only dependent upon the earth's own heat, mantle rocks (peridotite), and water, the hydrocarbon source is surely of 'renewable' origin (ref. climate discussion).
Article Role of tectonic stress in seepage evolution along the gas h...