Abstract
Retrotransposon roo is one of the most active elements in Drosophila melanogaster. The level of nucleotide diversity between copies of roo is very low but structural variation in the 5'-UTR is considerable. Transposition of roo at high frequency (around 5 × 10-2 per generation) has been shown previously in the set of mutation accumulation lines named Oviedo. Here we isolated thirteen individual insertions by inverse PCR and sequenced the 5' end of the elements (between 1663 and 2039 nt) including the LTR, the 5'-UTR and a fragment of 661 nucleotides from the ORF, to study whether the new transposed copies come from a unique variant (the master copy model) or different elements are able to move (the transposon model). The elements in the Oviedo lines presented the same structural variants as the reference genome. Different structural variants were active, a behaviour compatible with the "transposon model" in which the copies localized in multiple sites in the genome are able to transpose. At the level of sequence, the copies of roo in our lines are highly similar to the elements in the reference genome. The phylogenetic tree shows a shallow diversification with unsupported nodes denoting that all the elements currently active are very young. This observation together with the great polymorphism in insertion sites implies a rapid turnover of the elements.
