Laboratory and field evidence for long-term starvation survival of microorganisms in subsurface terrestrial environments

Details Laboratory and field evidence for long-term starvation survival of microorganisms in subsurface terrestrial environments Laboratory and field evidence for long-term starvation survival of microorganisms in subsurface terrestrial environments

Jul 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997spie.3111..366k&link_type=abstract

Proc. SPIE Vol. 3111, p. 366-377, Instruments, Methods, and Missions for the Investigation of Extraterrestrial Microorganisms, R

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Biogeochemical modeling of groundwater flow and nutrient flux in subsurface environments indicates that inhabitant microorganisms experience severe nutrient limitation. Using laboratory and field methods, we have been testing starvation survival in subsurface microorganisms. In microcosm experiments, we have shown that strains of two commonly isolated subsurface genera, Arthrobacter and Pseudomonas, are able to maintain viability in low-nutrient, natural subsurface sediments for over one year. These non- spore-forming bacteria undergo rapid initial miniaturization followed by a stabilization of cell size. Membrane lipid phospholipid fatty acid (PLFA) profiles of the Pseudomonas are consistent with adaptation to nutrient stress; Arthrobacter apparently responds to nutrient deprivation without altering membrane PLFAs. To test survivability of microorganisms over a geologic time scale, we characterized microbial communities in a sequence of unsaturated sediments ranging in age from modern to > 780,000 years. Sediments were relatively uniform silts in eastern Washington State. Porewater ages at depth (measured by the chloride mass- balance approach) were as old as 3,600 years. Microbial abundance, biomass, and activities (measured by direct counts, culture counts, total PLFAs, and radiorespirometry) declined with sediment age. The pattern is consistent with laboratory microcosm studies of microbial survival: rapid short-term change followed by long-term survival of a proportion of cells. Even the oldest sediments evinced a small but viable microbial community. Microbial survival appeared to be a function of sediment age. Porewater age appeared to influence the makeup of surviving communities, as indicated by PLFA profiles. Sites with different porewater recharge rates and patterns of Pleistocene flooding had different communities. These and other studies provide evidence that microorganisms can survive nutrient limitation for geologic time periods.

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