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PHYSICAL SCIENCES / BIOLOGICAL SCIENCES / GEOLOGY / ENVIRONMENTAL SCIENCES
Diffusion-controlled metabolism for long-term survival of single isolated microorganisms trapped within ice crystals
Department of Physics, University of California, Berkeley, CA 94720
Contributed by P. Buford Price, August 29, 2007 (received for review July 23, 2007)
Two known habitats for microbial metabolism in ice are surfaces of mineral grains and liquid veins along three-grain boundaries. We propose a third, more general, habitat in which a microbe frozen in ice can metabolize by redox reactions with dissolved small molecules such as CO2, O2, N2, CO, and CH4 diffusing through the ice lattice. We show that there is an adequate supply of diffusing molecules throughout deep glacial ice to sustain metabolism for >105 yr. Using scanning fluorimetry to map proteins (a proxy for cells) and F420 (a proxy for methanogens) in ice cores, we find isolated spikes of fluorescence with intensity consistent with as few as one microbial cell in a volume of 0.16 µl with the protein mapper and in 1.9 µl with the methanogen mapper. With such precise localization, it should be possible to extract single cells for molecular identification.
F420 fluorescence | fluorimetry | ice cores | dissolved molecules | single cells
The authors declare no conflict of interest.
Miteva, V., Sowers, T., Brenchley, J. E. (2005) 11th International Symposium on Microbial Ecology (ISME-11), Vienna, Austria, August 20–25, 2006.
This article contains supporting information online at www.pnas.org/cgi/content/full/0708183104/DC1.
Price, P. B., Rohde, R., Bramall, N., Bay, R. (2006) Eos Trans Am Geophys Union Fall Meeting Suppl 87:U43B-0868.
*To whom correspondence should be addressed. E-mail: bprice{at}berkeley.edu
© 2007 by The National Academy of Sciences of the USA
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