Distribution
ISs are widespread (Fig 1.6.1) and can occur in very high numbers
in prokaryotic genomes. A recent study concluded that proteins annotated as
Tpases, or as proteins with related functions, are by far the most abundant
functional class in both the prokaryotic and eukaryotic genomic and metagenomic
public data bases (Aziz, et al., 2010) (Fig 1.2.5).
Since the last surveys
(e.g. (Mahillon & Chandler, 1998, Chandler
& Mahillon, 2002)) many new ISs have been identified largely as a
result of the massive increase in available sequenced prokaryotic genomes.
Careful analysis of a number of these has also revealed that some genomes contain
significant levels of truncated and partial ISs devoid of Tpase genes. These
genomic "scars" represent traces of numerous ancestral transposition
events. However, genome annotations are often based simply on the presence of
Tpase genes (e.g. (Touchon & Rocha, 2007))
and do not include the entire DNA sequence with the IS ends. Indeed, a
significant number of solo IS-related IRs have been identified in various
genomes. Small IS fragments are rarely taken into account even though they can
provide important insights into the evolutionary history of the host genome (Figs 1.6.2, 1.6.3 and 1.6.4). Not only can this seriously
impair studies attempting to provide an overview of the evolutionary influence
of TEs on bacterial and archeal genomes, but such fragments may encode
truncated proteins and these could influence gene regulation (e.g. (Cordaux, et al.,
2006, Liu, et al., 2007, Shaheen, et al., 2010)). In bacteria (Stalder et al.,
1990, Salvatore et al., 2001, Gueguen, et al., 2006) and eukaryotes (Rio, 1991, Vos,
et al., 1993)truncated transposases
have been shown to inhibit transposition. One example where annotation of IS fragments
has provided important information is in the obligatory intracellular insect
endosymbiont, Wolbachia, which also
carries high numbers of full-length ISs. The sequence divergence observed
suggests that several waves of IS invasion and elimination have occurred over
evolutionary time (Cerveau et al., 2011).
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