E. Lichtfouse et J. Rullkotter, ACCELERATED TRANSFORMATION OF ORGANIC-MATTER BELOW THE SILICA TRANSITION ZONE IN IMMATURE SEDIMENTS FROM THE JAPAN SEA, Organic geochemistry, 21(5), 1994, pp. 517-523
Notable compositional changes of organic matter are observed below the
silica transition zone in thermally immature sediments. The increase
of bitumen ratio, and hopane and sterane isomerization parameters indi
cate an acceleration of the kinetics of the chemical reactions which t
ransform the organic matter. This phenomenon is probably due to the nu
merous mineral and textural changes induced by the transformation of a
morphous biogenic silica into crystalline authigenic silica.