HR: 0800h
AN: P51D-0955 [Abstracts]
TI: Distribution and Diversity of Microorganisms of Deep, Subpermafrost Brine in the Canadian
Arctic
AU: * Boettig, C
EM: cboettig@princeton.edu
AF: Indiana-Princeton-Tennessee Astrobiology Institute (IPTAI)Princeton University, Dept. of Geosciences,
Princeton, NJ 08544
United States
AU: McGown, D
EM: cboettig@princeton.edu
AF: Indiana-Princeton-Tennessee Astrobiology Institute (IPTAI)Princeton University, Dept. of Geosciences,
Princeton, NJ 08544
United States
AU: Davidson, M
EM: markd@princeton.edu
AF: Indiana-Princeton-Tennessee Astrobiology Institute (IPTAI)Princeton University, Dept. of Geosciences,
Princeton, NJ 08544
United States
AU: Onstott, T C
EM: tullis@princeton.edu
AF: Indiana-Princeton-Tennessee Astrobiology Institute (IPTAI)Princeton University, Dept. of Geosciences,
Princeton, NJ 08544
United States
AU: Soffentino, B
EM: bruno@gso.uri.edu
AF: Univ. of Rhode Island, Graduate School of Oceanography, Narragansett, RI 02882
United States
AU: Spivak, A
EM: spivack@gso.uri.edu
AF: Univ. of Rhode Island, Graduate School of Oceanography, Narragansett, RI 02882
United States
AU: D'Hondt, S
EM: dhondt@gso.uri.edu
AF: Univ. of Rhode Island, Graduate School of Oceanography, Narragansett, RI 02882
United States
AU: Miller, S
EM: smiller@bio.fsu.edu
AF: DNA Sequencing and Microarray Facility Florida State University, Dept. of Biological Science,
Tallahassee, FL 32306
United States
AU: Balkwill, D
EM: david.balkwill@med.fsu.edu
AF: Florida State University, Department of Biomedical Sciences, Tallahassee, FL 32306
United States
AU: Pratt, L
EM: prattl@indiana.edu
AF: IPTAI Indiana University, Dept. of Geological Sciences, Bloomington, IN 47405
United States
AU: Ruskeeniemi, T
EM: Timo.Ruskeeniemi@gsf.fi
AF: Geological Survey of Finland, Espoo, Espoo, 02150
Finland
AU: Ahonen, L
EM: lasse.ahonen@gtk.fi
AF: Geological Survey of Finland, Espoo, Espoo, 02150
Finland
AU: Telling, J
EM: telling@geology.utoronto.ca
AF: IPTAI Univ. of Toronto, Dept. of Geology, Toronto, ON M5S 3B1
Canada
AU: Sherwood Lollar, B
EM: bslollar@chem.utoronto.ca
AF: IPTAI Univ. of Toronto, Dept. of Geology, Toronto, ON M5S 3B1
Canada
AU: Frape, S
EM: shaun@sciborg.uwaterloo.ca
AF: Univ. of Waterloo, Department of Earth Sciences, Waterloo, ON N2L 3G1
Canada
AU: Stotler, R
EM: randys@sciborg.uwaterloo.ca
AF: Univ. of Waterloo, Department of Earth Sciences, Waterloo, ON N2L 3G1
Canada
AB:
Saline fracture water (0.3 to 3.7% TDS) trapped beneath 500 meters of frozen Archean metasediment was collected from
boreholes at 880 and 1130 meters depth at Lupin Au mine. Temperatures range from 4 to 10oC, pH from 8 to 9, Eh from
-150 to -190 mV. H2 and CH4 gas concentration range from 20 to 600 nM and 6 to 55 mM, respectively. The cell
density ranged from 400 to 105 cells/ml by direct count. Significant hydrogenase activity was detected only in the
borehole containing the highest cell density and lowest salinity. This activity was associated with relatively low H2
and high CO concentrations. The microbial diversity of fracture water yielding the lowest concentration of CH4 and the
greatest 34S fractionation between sulfate and sulfide (10o/oo) was characterized using the 16S rDNA gene.
The cDNA revealed a predominance of a species that was 95-97% similar Thiohalobaccili and the presence of a species that was
96% similar to Desulfosporosinus. No archaeal PCR product was detected. The molecular, geochemical and isotopic data
suggest cycling of S is occurring under suboxic conditions beneath the permafrost. He concentrations suggest that this
environment has been isolated from the surface for a geologically significant time interval. The persistence of suboxic
conditions in this sequestered ecosystem is either caused by a lack of electron donors relative to electron acceptors or
mixing with surficial lake water through nearby taliks.
DE: 0448 Geomicrobiology
DE: 0456 Life in extreme environments
DE: 0702 Permafrost (0475)
DE: 5430 Interiors (8147)
DE: 6225 Mars
SC: Planetary Sciences [P]
MN: Fall Meeting 2005