Dissolved material and recent sediment from the Amazon continental she
lf have been analyzed for hydrocarbons to study the sources and potent
ial fate of the transported organic matter. Dissolved n-alkanes are pr
esent at low concentrations (ppb level) and are dominated by lipids fr
om marine phytoplankton with carbon number maxima (C-max) at C-18/C-22
and an even-to-odd carbon predominance < C-30 (CPI17-27 from 0.18 to
0.54). In the sediments, bimodal distributions of n-alkane chain lengt
h suggest a mixed input of terrestrial (C-max at C-27/C-29/C-31 and CP
I25-33 from 0.75 to 1.82) and phytoplanktonic/microbial (C-max at C-20
and CPI15-33 from 0.38 to 0.62) organic matter. Sesquiterpenes were t
he most significant cyclic compounds in all the dissolved samples anal
yzed reflecting a contribution from resinous trees to the terrestrial
organic pool. On the other hand, enhanced concentrations of these comp
ounds in the dissolved phase on the northwest portion of the Amazon sh
elf, contrasting with decreased concentrations in the sediment samples
, suggest that dissolved lipids are released from solid phase in the i
ntensely stirred seabed. Structured organic matter in the sediment has
been characterized as being composed of, on average: 19% plant cuticl
es, 25% woody tissue, 13% pollens and spores, 24% amorphous material,
7% bituminite and 12% altered organic material.