HR: 0830h
AN: B41D-0919    [PDF]
TI: Production and Dietary Uptake of PUFA by Piezophilic Bacteria, Implications for Marine Biogeochemistry
AU: * Fang, J
EM: jsfang@iastate.edu
AF: Iowa State University, 360 Science I, Ames, IA 50011
AU: Chan, O
EM: waigor@iastate.edu
AF: Iowa State University, 360 Science I, Ames, IA 50011
AU: Agarkar, N
EM: netra@iastate.edu
AF: Iowa State University, 360 Science I, Ames, IA 50011
AU: Kato, C
EM: katoc@jamstec.go.jp
AF: Japan Marine Science and Technology Center, Department of Marine Ecosystem, Yokosuka, 237 Japan
AU: Sato, T
EM: satot@jamstec.go.jp
AF: Japan Marine Science and Technology Center, Department of Marine Ecosystem, Yokosuka, 237 Japan
AB: Polyunsaturated fatty acids (PUFAs) have been used extensively as proxies for determining the source and preservation of organic matter in marine sediments. However, the origin of polyunsaturated fatty acids in deep-sea sediments is not well understood; the ultimate source of PUFAs is only partially constrained. At issue is whether PUFAs in deep-sea sediments are derived from the primary production of the photic zone or from the in situ piezophilic bacterial production in the deep-sea, or both. In this study, we tested three deep-sea piezophilic strains, Shewanella violacea DSS12, Shewanella benthica DB21MT-2, Moritella yayanosii DB21MT-5, in biosynthesis and dietary uptake of PUFAs. These piezophilic bacteria were characterized by high abundance of unsaturated fatty acids (62-73% of total fatty acids). In particularly, polyunsaturated fatty acids (PUFA) were detected in all piezophiles examined, ranging from 8 to 27% of total fatty acids. M. japonica DSK1 produced 22:6n-3 (cis-4,7,10,13,16,19-docosahexaenoic acid, DHA), whereas the three Shewanella strains produced 20:5n-3 (cis-5,8,11,14,17-eicosapentaenoic acid, EPA) with trace amounts of DHA. The total concentrations of PLFA were higher in strains grown at low pressure (DSK1, 10 Megapascal or MPa, 26,983$\mu$g/g dry wt cells; DSS12, 50 MPa, 23,986 $\mu$g/g), and lower in strains grown at high pressure (DB6705, 85 MPa, 1,901$\mu$g/g; DB21MT-2, 100 MPa, 3,014 $\mu$g/g). When growth media were supplemented with arachidonic acid (AA; C20:4n-6), there was active uptake and cellular incorporation of AA in the hyperpiezophilic bacteria DB21MT-2 (14.7%) and DB21MT-5 (1.4%). No uptake was observed in DSS12. When cells were treated with antibiotic cerulenin, all three strains incorporated AA into cell membranes (13 to 19%). These results suggest that piezophilic bacteria can be an important contributor in producing and reworking of PUFAs in the deep sea, and that that caution must be exercised in using PUFAs in deducing sources of organic matter in the marine sediments.
DE: 0400 Biogeosciences
DE: 1050 Marine geochemistry (4835, 4850)
DE: 4805 Biogeochemical cycles (1615)
DE: 4840 Microbiology
DE: 4850 Organic marine chemistry
SC: Biogeosciences [B]
MN: 2003 Fall Meeting