A phylogenomic perspective on the radiation of ray-finned fishes based upon targeted sequencing of ultraconserved elements

TL;DR

This study uses targeted sequencing of ultraconserved elements to construct a detailed phylogeny of ray-finned fishes, revealing evolutionary relationships and divergence times with high support, and demonstrating an efficient, scalable genomic approach.

Contribution

It introduces a cost-effective, scalable method for phylogenomic data collection in fishes using UCEs, enhancing resolution of their evolutionary history.

Findings

Revealed monophyly of Amia and Lepisosteus (Holostei)

Identified earliest diverging teleost lineages as elopomorphs and osteoglossomorphs

Estimated crown teleosts originated around 270 million years ago

Abstract

Ray-finned fishes constitute the dominant radiation of vertebrates with over 30,000 species. Although molecular phylogenetics has begun to disentangle major evolutionary relationships within this vast section of the Tree of Life, there is no widely available approach for efficiently collecting phylogenomic data within fishes, leaving much of the enormous potential of massively parallel sequencing technologies for resolving major radiations in ray-finned fishes unrealized. Here, we provide a genomic perspective on longstanding questions regarding the diversification of major groups of ray-finned fishes through targeted enrichment of ultraconserved nuclear DNA elements (UCEs) and their flanking sequence. Our workflow efficiently and economically generates data sets that are orders of magnitude larger than those produced by traditional approaches and is well-suited to working with museum specimens. Analysis of the UCE data set recovers a well-supported phylogeny at both shallow and deep time-scales that supports a monophyletic relationship between Amia and Lepisosteus (Holostei) and reveals elopomorphs and then osteoglossomorphs to be the earliest diverging teleost lineages. Divergence time estimation based upon 14 fossil calibrations reveals that crown teleosts appeared ~270 Ma at the end of the Permian and that elopomorphs, osteoglossomorphs, ostarioclupeomorphs, and euteleosts diverged from one another by 205 Ma during the Triassic. Our approach additionally reveals that sequence capture of UCE regions and their flanking sequence offers enormous potential for resolving phylogenetic relationships within ray-finned fishes.