Abstract
Barbara McClintock was the first to suggest that transposons are a
source of genome instability and that genotoxic stress assisted in
their mobilization. The generation of double-stranded DNA breaks
(DSBs) is a severe form of genotoxic stress that threatens the
integrity of the genome, activates cell cycle checkpoints, and, in
some cases, causes cell death. Applying McClintock's stress
hypothesis to humans, are L1 retrotransposons, the most active
autonomous mobile elements in the modern day human genome,
mobilized by DSBs? Here, evidence that transposable elements,
particularly retrotransposons, are mobilized by genotoxic stress
is reviewed. In the setting of DSB formation, L1 mobility may be
affected by changes in the substrate for L1 integration, the DNA
repair machinery, or the L1 element itself. The review concludes
with a discussion of the potential consequences of L1 mobilization
in the setting of genotoxic stress.