USING RDNA GENES TO UNDERSTAND THE ORIGIN AND EVOLUTION OF SPLICEOSOMAL AND GROUP I INTRONS

Ribosomal DNA genes in lichen algae and lichen fungi are astonishingly rich in spliceosomal and group I introns. We use phylogenetic, secondary structure, and biochemical analyses to understand the evolution of these introns. Despite the widespread distribution of spliceosomal introns in nuclear pre-mRNA genes, their general mechanism of origin remains an open question because few proven cases of recent and pervasive intron origin have been documented. The lichen introns are valuable in this respect because they are undoubtedly of a "recent" origin and limited to the Euascomycetes. Our analyses suggest that rDNA spliceosomal introns have arisen through aberrant reverse-splicing (in trans) of free pre-mRNA introns into r RNAs. We propose that the spliceosome itself (and not an external agent; e.g. transposable elements, group II introns) has given rise to the introns. The rDNA introns are found most often between the flanking sequence G (78%) - intron-G (72%), and their clustered positions on secondary structures suggest that particular r RNA regions are preferred sites (i.e., proto-splice sites) for insertion. Mapping of intron positions on the newly available tertiary structures show that they are found most often in exposed regions of the ribosomes. This again is consistent with an intron origin through reverse-splicing. Remarkably, the distribution and phylogenetic relationships of most group I introns in nuclear rDNA genes are also consistent with a reverse-splicing origin. These data underline the value of lichens as a model system for understanding intron origin and stress the importance of RNA-level processes in the spread of these sequences in nuclear coding regions.     

Analysis of ribosomal protein gene structures: implications for intron evolution

Many spliceosomal introns exist in the eukaryotic nuclear genome. Despite much research, the evolution of spliceosomal introns remains poorly understood. In this paper, we tried to gain insights into intron evolution from a novel perspective by comparing the gene structures of cytoplasmic ribosomal proteins (CRPs) and mitochondrial ribosomal proteins (MRPs), which are held to be of archaeal and bacterial origin, respectively. We analyzed 25 homologous pairs of CRP and MRP genes that together had a total of 527 intron positions. We found that all 12 of the intron positions shared by CRP and MRP genes resulted from parallel intron gains and none could be considered to be “conserved,” i.e., descendants of the same ancestor. This was supported further by the high frequency of proto-splice sites at these shared positions; proto-splice sites are proposed to be sites for intron insertion. Although we could not definitively disprove that spliceosomal introns were already present in the last universal common ancestor, our results lend more support to the idea that introns were gained late. At least, our results show that MRP genes were intronless at the time of endosymbiosis. The parallel intron gains between CRP and MRP genes accounted for 2.3% of total intron positions, which should provide a reliable estimate for future inferences of intron evolution.     

Vertical evolution and intragenic spread of lichen-fungal group I introns

One family within the Euascomycetes (Ascomycota), the lichen-forming Physciaceae, is particularly rich in nuclear ribosomal [r]DNA group I introns. We used phylogenetic analyses of group I introns and lichen-fungal host cells to address four questions about group I intron evolution in lichens, and generally in all eukaryotes: 1) Is intron spread in the lichens associated with the intimate association of the fungal and photosynthetic cells that make up the lichen thallus? 2) Are the multiple group I introns in the lichen-fungi of independent origins, or have existing introns spread into novel sites in the rDNA? 3) If introns have moved to novel sites, then does the exon context of these sites provide insights into the mechanism of intron spread? and 4) What is the pattern of intron loss in the small subunit rDNA gene of lichen-fungi? Our analyses show that group I introns in the lichen-fungi and in the lichen-algae (and lichenized cyanobacteria) do not share a close evolutionary relationship, suggesting that these introns do not move between the symbionts. Many group I introns appear to have originated in the common ancestor of the Lecanorales, whereas others have spread within this lineage (particularly in the Physciaceae) putatively through reverse-splicing into novel rRNA sites. We suggest that the evolutionary history of most lichen-fungal group I introns is characterized by rare gains followed by extensive losses in descendants, resulting in a sporadic intron distribution. Detailed phylogenetic analyses of the introns and host cells are required, therefore, to distinguish this scenario from the alternative hypothesis of widespread and independent intron gains in the different lichen-fungal lineages.     

Distribution of rRNA introns in the three-dimensional structure of the ribosome

More than 1200 introns have been documented at over 150 unique sites in the small and large subunit ribosomal RNA genes (as of February 2002). Nearly all of these introns are assigned to one of four main types: group I, group II, archaeal and spliceosomal. This sequence information has been organized into a relational database that is accessible through the Comparative RNA Web Site (http://www.rna.icmb.utexas.edu/) While the rRNA introns are distributed across the entire tree of life, the majority of introns occur within a few phylogenetic groups. We analyzed the distributions of rRNA introns within the three-dimensional structures of the 30S and 50S ribosomes. Most sites in rRNA genes that contain introns contain only one type of intron. While the intron insertion sites occur at many different coordinates, the majority are clustered near conserved residues that form tRNA binding sites and the subunit interface. Contrary to our expectations, many of these positions are not accessible to solvent in the mature ribosome. The correlation between the frequency of intron insertions and proximity of the insertion site to functionally important residues suggests an association between intron evolution and rRNA function.     

Molecular evolution of eukaryotic genomes: hemiascomycetous yeast spliceosomal introns

As part of the exploratory sequencing program Génolevures, visual scrutinisation and bioinformatic tools were used to detect spliceosomal introns in seven hemiascomycetous yeast species. A total of 153 putative novel introns were identified. Introns are rare in yeast nuclear genes (<5% have an intron), mainly located at the 5′ end of ORFs, and not highly conserved in sequence. They all share a clear non-random vocabulary: conserved splice sites and conserved nucleotide contexts around splice sites. Homologues of metazoan snRNAs and putative homologues of SR splicing factors were identified, confirming that the spliceosomal machinery is highly conserved in eukaryotes. Several introns’ features were tested as possible markers for phylogenetic analysis. We found that intron sizes vary widely within each genome, and according to the phylogenetic position of the yeast species. The evolutionary origin of spliceosomal introns was examined by analysing the degree of conservation of intron positions in homologous yeast genes. Most introns appeared to exist in the last common ancestor of present day yeast species, and then to have been differentially lost during speciation. However, in some cases, it is difficult to exclude a possible sliding event affecting a pre-existing intron or a gain of a novel intron. Taken together, our results indicate that the origin of spliceosomal introns is complex within a given genome, and that present day introns may have resulted from a dynamic flux between intron conservation, intron loss and intron gain during the evolution of hemiascomycetous yeasts.     

The natural history of group I introns

There are four major classes of introns: self-splicing group I and group II introns, tRNA and/or archaeal introns and spliceosomal introns in nuclear pre-mRNA. Group I introns are widely distributed in protists, bacteria and bacteriophages. Group II introns are found in fungal and land plant mitochondria, algal plastids, bacteria and Archaea. Group II and spliceosomal introns share a common splicing pathway and might be related to each other. The tRNA and/or archaeal introns are found in the nuclear tRNA of eukaryotes and in archaeal tRNA, rRNA and mRNA. The mechanisms underlying the self-splicing and mobility of a few model group I introns are well understood. By contrast, the role of these highly distinct processes in the evolution of the 1500 group I introns found thus far in nature (e.g. in algae and fungi) has only recently been clarified. The explosion of new sequence data has facilitated the use of comparative methods to understand group I intron evolution in a broader context and to generate hypotheses about intron insertion, splicing and spread that can be tested experimentally.     

Molecular evolution: introns fall into place

The evolutionary origin of spliceosomal introns remains elusive. The startling success of a new way of predicting intron sites suggests that the splicing machinery determines where introns are added to genes.     

Birth of new spliceosomal introns in fungi by multiplication of introner-like elements

Spliceosomal introns are noncoding sequences that separate exons in eukaryotic genes and are removed from pre-messenger RNAs by the splicing machinery. Their origin has remained a mystery in biology since their discovery because intron gains seem to be infrequent in many eukaryotic lineages. Although a few recent intron gains have been reported, none of the proposed gain mechanisms can convincingly explain the high number of introns in present-day eukaryotic genomes. Here we report on particular spliceosomal introns that share high sequence similarity and are reminiscent of introner elements. These elements multiplied in unrelated genes of six fungal genomes and account for the vast majority of intron gains in these fungal species. Such introner-like elements (ILEs) contain all typical characteristics of regular spliceosomal introns (RSIs) but are longer and predicted to harbor more stable secondary structures. However, dating of multiplication events showed that they degenerate in sequence and length within 100,000 years to eventually become indistinguishable from RSIs. We suggest that ILEs not only account for intron gains in six fungi but also in ancestral eukaryotes to give rise to most RSIs by a yet unknown multiplication mechanism.     

The recent transfer of a homing endonuclease gene

The myxomycete Didymium iridis (isolate Panama 2) contains a mobile group I intron named Dir.S956-1 after position 956 in the nuclear small subunit (SSU) rRNA gene. The intron is efficiently spread through homing by the intron-encoded homing endonuclease I-DirI. Homing endonuclease genes (HEGs) usually spread with their associated introns as a unit, but infrequently also spread independent of introns (or inteins). Clear examples of HEG mobility are however sparse. Here, we provide evidence for the transfer of a HEG into a group I intron named Dir.S956-2 that is inserted into the SSU rDNA of the Costa Rica 8 isolate of D.iridis. Similarities between intron sequences that flank the HEG and rDNA sequences that flank the intron (the homing endonuclease recognition sequence) suggest that the HEG invaded the intron during the recent evolution in a homing-like event. Dir.S956-2 is inserted into the same SSU site as Dir.S956-1. Remarkably, the two group I introns encode distantly related splicing ribozymes with phylogenetically related HEGs inserted on the opposite strands of different peripheral loop regions. The HEGs are both interrupted by small spliceosomal introns that must be removed during RNA maturation.     

Evidence for the late origin of introns in chloroplast genes from an evolutionary analysis of the genus Euglena.

The origin of present day introns is a subject of spirited debate. Any intron evolution theory must account for not only nuclear spliceosomal introns but also their antecedents. The evolution of group II introns is fundamental to this debate, since group II introns are the proposed progenitors of nuclear spliceosomal introns and are found in ancient genes from modern organisms. We have studied the evolution of chloroplast introns and twintrons (introns within introns) in the genus Euglena. Our hypothesis is that Euglena chloroplast introns arose late in the evolution of this lineage and that twintrons were formed by the insertion of one or more introns into existing introns. In the present study we find that 22 out of 26 introns surveyed in six different photosynthesis-related genes from the plastid DNA of Euglena gracilis are not present in one or more basally branching Euglena spp. These results are supportive of a late origin for Euglena chloroplast group II introns. The psbT gene in Euglena viridis, a basally branching Euglena species, contains a single intron in the identical position to a psbT twintron from E.gracilis, a derived species. The E.viridis intron, when compared with 99 other Euglena group II introns, is most similar to the external intron of the E.gracilis psbT twintron. Based on these data, the addition of introns to the ancestral psbT intron in the common ancester of E.viridis and E.gracilis gave rise to the psbT twintron in E.gracilis.     

The intronome of budding yeasts

Whatever their abundance in genomes, spliceosomal introns are the signature of eukaryotic genes. The sequence of Saccharomyces cerevisiae, achieved fifteen years ago, revealed that this yeast has very few introns, but conserved intron boundaries typical for an intron definition mechanism. With the improvement and the development of new sequencing technologies, yeast genomes have been extensively sequenced during the last decade. We took advantage of this plethora of data to compile and assess the intron content of the protein-coding genes of 13 genomes representative of the evolution of hemiascomycetous yeasts. We first observed that intron paucity is a general rule and that the fastest evolving genomes tend to lose their introns more rapidly (e.g. S. cerevisiae versus Yarrowia lipolytica). Noticeable differences were also confirmed for 5' splice sites and branch point sites (BP) as well as for the relative position of the BP. These changes seemed to be correlated with the lineage specific evolution of splicing factors.     

A very high fraction of unique intron positions in the intron-rich diatom Thalassiosira pseudonana indicates widespread intron gain

Although spliceosomal introns are present in all characterized eukaryotes, intron numbers vary dramatically, from only a handful in the entire genomes of some species to nearly 10 introns per gene on average in vertebrates. For all previously studied intron-rich species, significant fractions of intron positions are shared with other widely diverged eukaryotes, indicating that 1) large numbers of the introns date to much earlier stages of eukaryotic evolution and 2) these lineages have not passed through a very intron-poor stage since early eukaryotic evolution. By the same token, among species that have lost nearly all of their ancestral introns, no species is known to harbor large numbers of more recently gained introns. These observations are consistent with the notion that intron-dense genomes have arisen only once over the course of eukaryotic evolution. Here, we report an exception to this pattern, in the intron-rich diatom Thalassiosira pseudonana. Only 8.1% of studied T. pseudonana intron positions are conserved with any of a variety of divergent eukaryotic species. This implies that T. pseudonana has both 1) lost nearly all of the numerous introns present in the diatom-apicomplexan ancestor and 2) gained a large number of new introns since that time. In addition, that so few apparently inserted T. pseudonana introns match the positions of introns in other species implies that insertion of multiple introns into homologous genic sites in eukaryotic evolution is less common than previously estimated. These results suggest the possibility that intron-rich genomes may have arisen multiple times in evolution. These results also provide evidence that multiple intron insertion into the same site is rare, further supporting the notion that early eukaryotic ancestors were very intron rich.     

The evolution of spliceosomal introns: patterns, puzzles and progress

The origins and importance of spliceosomal introns comprise one of the longest-abiding mysteries of molecular evolution. Considerable debate remains over several aspects of the evolution of spliceosomal introns, including the timing of intron origin and proliferation, the mechanisms by which introns are lost and gained, and the forces that have shaped intron evolution. Recent important progress has been made in each of these areas. Patterns of intron-position correspondence between widely diverged eukaryotic species have provided insights into the origins of the vast differences in intron number between eukaryotic species, and studies of specific cases of intron loss and gain have led to progress in understanding the underlying molecular mechanisms and the forces that control intron evolution.     

125 Changing Environmental Conditions and Changes in the Abundances of Rocky Intertidal Seaweeds on Southern California Shores

In a recent study of the North American biogeography of the red algae genus Hildenbrandia , the presence of group I introns were noted in the nuclear SSU rRNA gene of the marine species H. rubra (Hildenbrandiales). Group I introns in the nuclear encoded rRNAs have been previously reported in the Hildenbrandiales as well as the Bangiales. All reported introns within the red algae have been identified as belonging to the IC1 subclass and occur at two insertion sites in the nuclear small subunit rRNA (516 and 1506). However, an unclassified intron was discovered at position 989 in the nuclear SSU rRNA gene of a collection of H. rubra from British Columbia, Canada. We have determined that the intron is a member of the IE subclass and this is the first report of an IE intron and an intron in position 989 in the red algae. Phylogenetic analyses of the intron sequences reveal a close relationship between this group IE intron and similar ascomycete and basidiomycete fungal IE introns in the nuclear SSU rRNA genes at positions 989 and 1199. In addition, a common unique helix (structural signature) in the P13 domain of the Hildenbrandia intron and those of the fungi at the 989 and 1199 IE positions in the nuclear SSU rRNA gene also indicates a close relationship. Hence, this study provides evidence for a possible lateral transfer of the IE intron in position 989 between fungal and red algal nuclear SSU rRNA genes.     

Patterns of intron loss and gain in plants: intron loss-dominated evolution and genome-wide comparison of O. sativa and A. thaliana

Numerous previous studies have elucidated 2 surprising patterns of spliceosomal intron evolution in diverse eukaryotes over the past roughly 100 Myr. First, rates of recent intron gain in a wide variety of eukaryotic lineages have been surprisingly low, far too low to explain modern intron densities. Second, intron losses have outnumbered intron gains over a variety of lineages. For several reasons, land plants might be expected to have comparatively high rates of intron gain and thus to represent a possible exception to this pattern. However, we report several studies that indicate low rates of intron gain and an excess of intron losses over intron gains in a variety of plant lineages. We estimate that intron losses have outnumbered intron gains in recent evolution in Arabidopsis thaliana (roughly 12.6 times more losses than gains), Oryza sativa (9.8 times), the green alga Chlamydomonas reinhardtii (5.1 times), and the Bigelowiella natans nucleomorph, an enslaved green algal nucleus (2.8 times). We estimate that during recent evolution, A. thaliana and O. sativa have experienced very low rates of intron gain of around one gain per gene per 2.6-8.0 billion years. In addition, we compared 8,258 pairs of putatively orthologous A. thaliana-O. sativa genes. We found that 5.3% of introns in conserved coding regions are species-specific. Observed species-specific A. thaliana and O. sativa introns tend to be exact and to lie adjacent to each other along the gene, in a pattern suggesting mRNA-mediated intron loss. Our results underscore that low intron gain rates and intron number reduction are common features of recent eukaryotic evolution. This pattern implies that rates of intron creation were higher during earlier periods of evolution and further focuses attention on the causes of initial intron proliferation.     

An intron-encoded protein assists RNA splicing of multiple similar introns of different bacterial genes

Four group II introns were found in an unusually intron-rich dnaN gene (encoding the beta subunit of DNA polymerase III) of the cyanobacterium Trichodesmium erythraeum, and they have strong similarities to two introns of the RIR gene (encoding ribonucleotide reductase) of the same organism. Of these six introns, only the RIR-3 intron encodes a maturase protein and showed efficient RNA splicing when expressed in Escherichia coli cells. The other five introns do not encode a maturase protein and did not show RNA splicing in E. coli. But these maturase-less introns showed efficient RNA splicing when the RIR-3 intron-encoded maturase protein was co-expressed from a freestanding gene in the same cell. These findings demonstrated that an intron-encoded protein could function as a general maturase for multiple introns of different genes. Major implications may include an intron-mediated co-regulation of the different genes and a resemblance of the evolutionary origin of spliceosomal introns.