The distribution of group I introns in lichen algae suggests that lichenization facilitates intron lateral transfer.

The nuclear-encoded small subunit ribosomal DNA gene of many lichen-forming green algae in the genus Trebouxia contains a group I intron at Escherichia coli genic position 1512. We studied the evolutionary history of the 1512 intron in Trebouxia spp. (Trebouxiophyceae) by analyzing intron and "host" cell phylogenies. The host trees were constructed by comparing internal transcribed spacer regions of rDNA. Maximum-likelihood, maximum-parsimony, and distance analyses suggest that the 1512 intron was present in the common ancestor of the green algal classes Trebouxiophyceae, Chlorophyceae, and Ulvophyceae. The 1512 intron, however, was laterally transferred at least three times among later-diverging Trebouxia spp. that form lichen partnerships. Intron secondary structure analyses are consistent with this result. Our results support the hypothesis that lichenization may facilitate 1512 group I intron lateral transfer through the close cell-to-cell contact that occurs between the lichen algal and fungal symbionts in the developing lichen thallus.

The cyanobacterial origin and vertical transmission of the plastid tRNA(Leu) group-I intron.

We have surveyed the distribution and reconstructed the phylogeny of the group-I intron that is positioned in the anticodon loop of the tRNA(Leu) gene in cyanobacteria and several plastid genomes. Southern-blot and PCR analyses showed that the tRNA(Leu) intron is found in all 330 land plants that were examined. The intron was also found, and sequenced, in all but one of nine charophycean algae examined. Conversely, PCR analyses showed that the tRNA(Leu) group-I intron is absent from the red, cryptophyte and haptophyte algae, although it is present in three members of the heterokont lineage. Phylogenetic analyses of the intron indicate that it was present in the cyanobacterial ancestor of the three primary plastid lineages, the Rhodophyta, Chlorophyta, and Glaucocystophyta. Its present-day distribution in plastids is consistent with a history of strictly vertical transmission, with no losses in land plants, several losses among green algae, and nearly pervasive loss in the Rhodophyta and its secondary derivatives.