Late Changes in Spliceosomal Introns Define Clades in Vertebrate Evolution

The evolutionary origin of spliceosomal introns has been the subject of much controversy. Introns are proposed to have been both lost and gained during evolution. If the gain or loss of introns are unique events in evolution, they can serve as markers for phylogenetic analysis. We have made an exten...

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Published inProceedings of the National Academy of Sciences - PNAS Vol. 96; no. 18; pp. 10267 - 10271
Main Authors Venkatesh, Byrappa, Ning, Yana, Brenner, Sydney
Format Journal Article
LanguageEnglish
Published United States National Academy of Sciences of the United States of America 31.08.1999
National Acad Sciences
National Academy of Sciences
The National Academy of Sciences
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Summary:The evolutionary origin of spliceosomal introns has been the subject of much controversy. Introns are proposed to have been both lost and gained during evolution. If the gain or loss of introns are unique events in evolution, they can serve as markers for phylogenetic analysis. We have made an extensive survey of the phylogenetic distribution of seven spliceosomal introns that are present in Fugu genes, but not in their mammalian homologues; we show that these introns were acquired by actinopterygian (ray-finned) fishes at various stages of evolution. We have also investigated the intron pattern of the rhodopsin gene in fishes, and show that the four introns found in the ancestral chordate rhodopsin gene were simultaneously lost in a common ancestor of ray-finned fishes. These changes in introns serve as excellent markers for phylogenetic analysis because they reliably define clades. Our intron-based cladogram establishes the difficult-to-ascertain phylogenetic relationships of some ray-finned fishes. For example, it shows that bichirs (Polypterus) are the sister group of all other extant ray-finned fishes.
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Contributed by Sydney Brenner
To whom reprint requests should be addressed. E-mail: mcbbv@imcb.nus.edu.sg.
ISSN:0027-8424
1091-6490
DOI:10.1073/pnas.96.18.10267