Recent marine sediments from two cores, collected on the continental slope
of the Nansha Sea, China, have been analyzed for organic matter content, n-
alkane and isoprenoid hydrocarbons, fatty acids, n-alkanols and sterols. Th
e organic carbon contents of the two sediment cores average 0.7 and 0.53%,
respectively, and are higher than those of other sedimentary environments i
n this region. The distributions of various lipid compounds indicate that m
ost of the sedimentary organic matter in the two cores is derived from mari
ne plankton and bacteria, with land-derived organic matter present in relat
ively small amounts. The decrease in relative abundances of shorter chain l
ipids (n-alkanes, n-fatty acids and n-alkanols) with depth is evident, as i
s the biochemical conversion of stenols to stanols in some samples. The low
pristane/phytane ratios may result primarily from microbial activity, and
reflect the occurrence of significant diagenetic alteration of organic matt
er in the two cores. (C) 2000 Elsevier Science Ltd. All rights reserved.