skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Hydrocarbons in waters and particulate material from hydrothermal environments at the East Pacific Rise, 13/sup 0/N

Journal Article · · Org. Geochem.; (United States)

Associated with the fast spreading East Pacific Rise are massive sulfide deposits and large communities of animals. The main food source of these benthic organisms is supplied by symbiotic chemosynthetic activity of sulfur oxidizing bacteria. Biomarker lipids such as hydrocarbons, were analyzed to describe their sources and composition and also the relationships among microorganisms, biological communities, and dissolved and particulate organic materials in this productive area. The organic matter of vent waters is both quantitatively and qualitatively different from the non-vent bottom water. Dissolved hydrocarbon concentrations in warm water from fissures in basalts and hot clear water from smokers are 100 and 400 times more concentrated, respectively, than the water outside active areas. The biomarker compounds from hot clear water are characteristic of thermally mature organic matter as indicated by the 17..cap alpha..(H)->17..beta..(H)-hopane series, and the dominance of 5..cap alpha..(H),14..beta..(H),17..beta..(H)-steranes over the 5..cap alpha..(H),14..cap alpha..(H),17..cap alpha..(H),20R-steranes. The dissolved hydrocarbons from the warm waters may be correlated with bacterial lipid residues as indicated by the presence of isoprenoid hydrocarbons (pristane > phytane) and low molecular weight cyclic hydrocarbons. The water column samples collected near hydrothermally active areas contain bicyclic alkanes with drimane and rearranged drimane skeletons and mature biomarkers. The dissolved lipid matter is found to be degraded more rapidly by microbial activity and thermal processes, especially in the warm water effluent and in the water column around hydrothermal vents, than the lipids of the particulate matter.

Research Organization:
Oregon State Univ., Corvallis (USA)
OSTI ID:
7054702
Journal Information:
Org. Geochem.; (United States), Vol. 12:3
Country of Publication:
United States
Language:
English