| Abstract: | Suspended particulate materials and bottom sediments from the Cariaco Trench were analysed for lipid content to investigate the diagenesis of organic matter in an anoxic water column and sediment. Distributions of fatty acids, sterols, and the acyclic isoprenoid hydrocarbons, lycopane and 2,6,10,15,19-pentamethyleicosane, support the hypothesis that alteration of organic matter usually attributed to sedimentary diagenesis occurs in the water column. Typical indicators of diagenetic processes, including preferential loss of unsaturated fatty acids, increased abundances of branched fatty acids, stenol-to-stanol conversion, and abundant acyclic isoprenoids, were observed in the water column across the oxic/anoxic interface in the Cariaco Trench. Lipid distributions in the sediment were remarkably uniform with depth. We conclude that organic material delivered to the sediment has been extensively altered in the water column, but that which is buried is preserved without much additional alteration. |
