Spliceosomal (pre-mRNA) introns have previously been found in eukaryotic pr
otein-coding genes, in the small nuclear RNAs of some fungi, and in the sma
ll- and large-subunit ribosomal DNA genes of a limited number of ascomycete
s. How the majority of these introns originate remains an open question bec
ause few proven cases of recent and pervasive intron origin have been docum
ented. We report here the widespread occurrence of spliceosomal introns (69
introns at 27 different sites) in the small- and large-subunit nuclear-enc
oded rDNA of lichen-forming and free-living members of the Ascomycota. Our
analyses suggest that these spliceosomal introns are of relatively recent o
rigin, i.e., within the Euascomycetes, and have arisen through aberrant rev
erse-splicing tin trans) of free pre-mRNA introns into rRNAs. The spliceoso
me itself, and not an external agent (e.g., transposable elements, group II
introns), may have given rise to these introns. A nonrandom sequence patte
rn was found at sites flanking the rRNA spliceosomal introns. This pattern
(AG-intron-G) closely resembles the proto-splice site (MAG-intron-R) postul
ated for intron insertions in pre-mRNA genes. The clustered positions of sp
liceosomal introns on secondary structures suggest that particular rRNA reg
ions are preferred sites for insertion through reverse-splicing.