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Principal Investigator: Wade H. Jeffrey, PhD Co-Principal Investigator: David L. Mitchell, PhD. MD Anderson Cancer Center, Smithville, TX Support Agency: National Science Foundation Location of Study: Polar Glacial Ice Samples |
Bacteria are "hitchhikers" in glaciers; deposited
from above on windborne dust particles and aerosols, overlayered
by thousands of years of deposition and accretion, and finally
returned to the coastal marine environment by glacial calving
and melting. Bacteria have been detected in and cultured from
glacial ice ranging from a few hundred to many thousands of years
old. Evidence suggests that glacial ice cannot support bacterial
growth but rather traps these organisms for considerable lengths
of time in an anabiotic state. In the absence of DNA replication
and repair, we hypothesize that DNA degradation occurs at a significant
rate and that base modifications resulting from spontaneous depurinations,
depyrimidinations, and deaminations accumulate. Although much
of the DNA degradation would be lethal to dividing bacteria, it
is probable that organisms that are successful in recovering from
the ice replicate their DNA using a template containing significant
levels of base modifications; this would lead to a significant
mutation frequency.
In the context of "glacial hitchhiking", we propose
to test the hypothesis that bacteria sustain significant levels
of base damage during glacial entrapment and that this base damage
leads to mutations. In the course of our studies we will culture,
preserve, and characterize a diverse array of bacteria extracted
from glacial ice. We will examine the lethal effects of glaciation
on bacteria using clonability, transcription, protein synthesis,
and fluorescence in situ hybridization using rRNA probes
as biological endpoints. Mutations will be analyzed as heteroduplex
molecules formed after an incipient round of DNA replication using
immoblized mismatch binding protein (mutS). From our work we will
gain insight into basic mechanisms of mutagenesis that may be
relevant to bacterial speciation, diversity and the evolution
of life on earth as well as in extremely cold environments found
elsewhere in our solar system. We also expect to show a correlation
between DNA damage, cell lethality, and mutagenesis with respect
to time spent in the glacier, thus providing a novel and facile
approach for ice core dating.