Molecular Biology and Evolution 19:1637-1639 (2002)
© 2002 Society for Molecular Biology and Evolution
The Paradox of the "Ancient" Bacterium Which Contains "Modern" Protein-Coding Genes
Heather Maughan*, C. William Birky Jr.*
, Wayne L. Nicholson*
,William D. Rosenzweig
and Russell H. Vreeland
*Graduate Interdisciplinary Program in Genetics,
Department of Ecology and Evolutionary Biology,
Department of Veterinary Science and Microbiology, University of Arizona; and
Department of Biology, West Chester University
The isolation of microorganisms from ancient materials and the
verification that they are as old as the materials from which
they were isolated continue to be areas of controversy. Almost
without exception, bacteria isolated from ancient material have
proven to closely resemble modern bacteria at both morphological
and molecular levels. This fact has historically been used by
critics to argue that these isolates are not ancient but are
modern contaminants introduced either naturally after formation
of the surrounding material (for further details, see Hazen
and Roeder 2001

and the reply by Powers, Vreeland, and Rosenzweig
2001

) or because of flaws in the methodology of sample isolation
(reviewed recently in Vreeland and Rosenzweig 2002

). Such criticism
has been addressed experimentally by the development of highly
rigorous protocols for sample selection, surface sterilization,
and contamination detection and control procedures. Using the
most scrupulous and well-documented sampling procedures and
contamination-protection techniques reported to date, Vreeland,
Rosenzweig, and Powers (2000)

reported the isolation of a sporeforming
bacterium,
Bacillus strain 2-9-3, from a brine inclusion within
a halite crystal recovered from the 250-Myr-old Permian Salado
Formation in Carlsbad, NM.
As had been noted in earlier studies, a striking observation
by Vreeland, Rosenzweig, and Powers (2000)

was that the 16S
rDNA of isolate 2-9-3 is 99% identical to that of
Salibacillus marismortui, a bacterium isolated from the Dead Sea in 1936
(Arahal et al. 1999

). In fact, Arahal et al. (1999)

identified
as
S. marismortui three strains with 16S rDNA sequences differing
by 0.01%, suggesting that isolate 2-9-3 might also be classified
as
S. marismortui.
Two groups have since used phylogenetic analyses of 16S rDNA
sequences to argue that isolate 2-9-3 is unlikely to be 250
Myr old. Graur and Pupko (2001)

used a relative rate test to
compare evolutionary rates of 16S rDNA on the branches leading
to isolate 2-9-3 and
S. marismortui and found no differences
between the evolutionary rates. Considering the possibility
that
S. marismortui may also be ancient (Arahal et al. 1999

;
Vreeland, Rosenzweig, and Powers 2000

), they also compared
the evolutionary rates of isolate 2-9-3,
S. marismortui and
Virgibacillus proomi, a close relative of
S. marismortui, and
again found similar rates of evolution (Graur and Pupko 2001

).
More recently, Nickle et al. (2002)

also performed relative
rate tests using 16S rDNA with the same result; the branch leading
to isolate 2-9-3 is not extraordinarily short, as would be expected
of an organism that has not been evolving for millions of years.
Nickle et al. (2002)

used evolutionary rates derived from enteric
bacteria to argue that if isolate 2-9-3 has not been evolving
for 250 Myr, then
S. marismortui must itself have been evolving
5–10 times more slowly than did aphid endosymbionts on
which the rate calculations were based. We note that although
the evolutionary rates calculated from enterics and endosymbionts
are the best estimates we currently possess, it is entirely
likely that rates of sporeformer evolution may indeed be slower
by several orders of magnitude. Sporeformers have been shown
to remain in the metabolically dormant spore state, thus not
replicating their DNA, for conservative estimates of anywhere
from 10
2 to 10
4years between times of growth (Kennedy, Reader,
and Swierczynski 1994

; Nicholson et al. 2000

).
As the analyses discussed above used 16S rDNA genes, the evolution
of which may not be representative of the organism as a whole,
we wanted to know if the similarities between isolate 2-9-3
and
S. marismortui are seen with protein-coding genes as well
as with 16S rDNA genes. We therefore analyzed phylogenetic relationships
between strain 2-9-3 and
S. marismortui, using the spore-forming
bacteria as our comparison group. The rationale for this design
was that the evolutionary rate among the sporeformers would
more closely approximate that of 2-9-3. We used amino acid data
from two genes,
recA and
splB. The
recA gene is found throughout
all bacteria, and its product is required for homologous recombination
and DNA repair. Because of the functional constraints on
recA evolution, it can be used to resolve the older evolutionary
relationships. The
splB gene, on the other hand, has to date
only been reported in gram-positive spore-forming bacteria and
is important in the repair of spore-specific DNA damage resulting
from UV radiation during spore dormancy (Nicholson et al. 2000

).
Because
splB is only found in gram-positive spore-forming bacteria,
it can be assumed to have a more recent origin than
recA has
and might be useful in resolving closer evolutionary relationships.
The results of our analyses are consistent with the phylogenetic
relationships shown by Graur and Pupko (2001)

and Nickle et
al. (2002)

. At the nucleotide level, isolate 2-9-3 and
S. marismortui differed by two nucleotides out of the 404
recA nucleotides
examined. Both of these substitutions are synonymous, making
these two taxa identical at the amino acid level. The phylogenetic
reconstruction (Swofford 1998

) using amino acid sequences of
recA (amino acids were used because of site saturation at the
nucleotide level across distantly related taxa) places 2-9-3
and
S. marismortui in a more recent clade, instead of their
occupying a more basal position as one would predict if the
clade had not been evolving for 250 Myr (
fig. 1 ).
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