HR: 0800h
AN: B11C-0626 [Abstracts]
TI: Biofilm function and variability in a hydrothermal ecosystem: insights from environmental genomes
AU: * Meyer-Dombard, D R
EM: drmd@uic.edu
AF: UIC, 845 W. Taylor, Chicago, IL 60607,
AU: Raymond, J
EM: jason.raymond@ucmerced.edu
AF: UC, 5200 N. Lake Ave, Merced, CA 95343,
AU: Shock, E L
EM: eshock@asu.edu
AF: ASU, PO Box 871404, Tempe, AZ 85287,
AB:
The ability to adapt to variable environmental conditions is key to survival for all organisms, but may be especially
crucial to microorganisms in extreme environments such as hydrothermal systems. Streamer biofilm
communities (SBCs) made up of thermophilic chemotrophic microorganisms are common in alkaline-chloride
geothermal environments worldwide, but the in situ physiochemical growth parameters and requirements of
SBCs are largely unknown [1]. Hot springs in Yellowstone National Park's alkaline geyser
basins support SBC growth. However, despite the relative geochemical homogeneity of source pools and
widespread ecosystem suitability in these regions (as indicated by energetic profiling [2]), SBCs are not
ubiquitous in these ecosystems. The ability of hydrothermal systems to support the growth of SBCs, the
relationship between these geochemically driven environments and the microbes that live there, and the function
of individuals in these communities are aspects that are adressed here by applying environmental genomics.
Analysis of 16S rRNA and total membrane lipid extracts have revealed that community composition of SBCs in
"Bison Pool" varies as a function of changing environmental conditions along the outflow channel. In addition, a
significant crenarchaeal component was discovered in the "Bison Pool" SBCs. In general, the SBC bacterial
diversity triples while the archaeal component varies little (from 3 to 2 genera) in a 5-10°C gradient with
distance from the source. While these SBCs are low in overall diversity, the majority of the taxa identified
represent uncultured groups of Bacteria and Archaea. As a result, the community function of these taxa and their
role in the formation of the biofilms is unknown. However, recent genomic analysis from environmental DNA
affords insight into the roles of specific organisms within SBCs at "Bison Pool," and integration of these data with
an extensive corresponding geochemical dataset may indicate shifting community function with geochemical
variability. For example, calculations of energy availability and genomic data indicate a myriad of potential
heterotrophic and autotrophic metabolic functions present at "Bison Pool" (genes for all known autotrophic C-
fixation pathways, H2, CO, and formate oxidation, cellulose degredation, and Fe and As redox), as well as
oxygenic and anoxygenic photosynthesis. These microbial communities and their environments are ideal for
coordination of geochemical and genomic data, enabling informed analysis of SBC function and growth criteria.
[1] Jahnke, L. et al. (2001) AEM 67, 5179-5189
[2] Meyer-Dombard, D. et al. (2005) Geobiology 3, 211-227
DE: 0410 Biodiversity
DE: 0439 Ecosystems, structure and dynamics (4815)
DE: 0448 Geomicrobiology
DE: 0450 Hydrothermal systems (1034, 3017, 3616, 4832, 8135, 8424)
SC: Biogeosciences [B]
MN: 2007 Fall Meeting