With an estimated abundance of 1030,
viruses are by far the most abundant biological entity in the oceans. The rapid
turnover of bacteria and archaea by viral lysis indicates the importances of
viruses in geochemical cycling (e.g. see Sean’s blog “Viruses, driving primary
production?”). However, our knowledge on how viral occurrence and impact vary
between regions is still patchy. Cottrell and Kirchman (2012) specifically
wanted to explore the prevalence of virus genes in the genomes of bacteria from
the western Arctic Ocean in comparison to samples from Monterey Bay and
Antarctic waters. In fact, previous studies had shown that the relationship
between viruses and prokaryotes in the Arctic appeared to differ from that in
lower latitudes in terms of both lower bacterial and viral abundances and lower
viral lysis. So far, no study had systematically surveyed virus DNA in genomes
of uncultivated bacteria, although prophages (remember these are the latent forms of bacteriophages in which the viral genes are
incorporated into the bacterial genome without causing disruption of the
bacterial cell) have been found in 60 to 70 % of all sequenced genomes of
cultivated bacteria and about half of all cultivated marine bacteria contain
inducible prophages.
In order to be able to study
uncultivated bacteria, metagenomic analyses were used: the bacterial genomes
were sampled by cloning environmental DNA into a fosmid vector and were
examined for phage genes using basic local alignment search tool (BLAST).
The BLAST analyses using
viral metagenome queries revealed that the number of phage genes in genomes of
uncultivated bacteria was significantly higher in Arctic samples: 2-fold more
viral genes than in the Monterey Bay bacterial DNA and 10-fold more than in the
Antarctic bacterial DNA. However, although the environmental conditions vary a
lot between Arctic, Pacific oceanic and coastal Antarctic waters, the metabolic
pathways in the microbial communities themselves did not differ significantly.
The authors point out that
these results represent a paradox, considering that the rates of viral
mortality in Arctic waters are among the lowest determined for any aquatic
system. So the high observed frequency of virus DNA in the Arctic bacterial
metagenome suggests a substantial viral impact with poor conditions for actual
viral lysis. Possibly the frequency of temperate phages, capable of entering
the lysogenic cycle, is increased in Arctic waters, which has been supported by
previous studies that found a higher abundance of the integrase genes,
indicative of temperate phages. In this case, the viral impact would be majorly
influenced by the factors which trigger the prophage induction leading to
lysis. This could be linked to the hypothesis suggested by Weinbauer et al. (2003) suggesting that lysogeny
is an adaptation to low host abundance and activity, although the authors did
not make this link.
It is interesting how
much the ecology of viruses between Arctic and Antarctic waters differ, the
former one with the lowest, the latter one with the highest rates of bacterial
mortality by viral lysis. Although the underlying mechanisms for this discrepancy
are still unclear, evidence points to there being more differences than
similarities. Also how do these results compare with De Corte et al.’s (2012) findings, suggesting
that host availability and temperature account for 69% of the variation in
viral abundance in Arctic waters? (see Georgia’s blog “Factors influencing viral distribution and abundance along a
latitudinal transect of the North Atlantic Ocean at different depths.”)
Cottrell, M. & Kirchman,
D., 2012. Virus genes in Arctic marine bacteria identified by metagenomic
analysis. Aquatic Microbial Ecology, 66(2), pp.107–116. Available at:
http://www.int-res.com/abstracts/ame/v66/n2/p107-116/
Weinbauer, M., Brettar, I.
& Höfle, M., 2003. Lysogeny and virus-induced mortality of bacterioplankton
in surface, deep, and anoxic marine waters. Limnology and Oceanography,
48(4), pp.1457–1465. Available at: http://www.jstor.org/stable/10.2307/3597469
No comments:
Post a Comment
Note: only a member of this blog may post a comment.