The tree of life of fishes is in a state of flux because we still lack a comprehensive phylogeny that includes all major groups. The situation is most critical for a large clade of spiny-finned fishes, traditionally referred to as percomorphs, whose uncertain relationships have plagued ichthyologists for over a century. Most of what we know about the higher-level relationships among fish lineages has been based on morphology, but rapid influx of molecular studies is changing many established systematic concepts. We report a comprehensive molecular phylogeny for bony fishes that includes representatives of all major lineages. DNA sequence data for 21 molecular markers (one mitochondrial and 20 nuclear genes) were collected for 1410 bony fish taxa, plus four tetrapod species and two chondrichthyan outgroups (total 1416 terminals). Bony fish diversity is represented by 1093 genera, 369 families, and all traditionally recognized orders. The maximum likelihood tree provides unprecedented resolution and high bootstrap support for most backbone nodes, defining for the first time a global phylogeny of fishes. The general structure of the tree is in agreement with expectations from previous morphological and molecular studies, but significant new clades arise. Most interestingly, the high degree of uncertainty among percomorphs is now resolved into nine well-supported supraordinal groups. The order Perciformes, considered by many a polyphyletic taxonomic waste basket, is defined for the first time as a monophyletic group in the global phylogeny. A new classification that reflects our phylogenetic hypothesis is proposed to facilitate communication about the newly found structure of the tree of life of fishes. Finally, the molecular phylogeny is calibrated using 60 fossil constraints to produce a comprehensive time tree. The new time-calibrated phylogeny will provide the basis for and stimulate new comparative studies to better understand the evolution of the amazing diversity of fishes.
Funding StatementThis work was supported by NSF awards DEB-0732988 (to REB), DEB-0732838, DEB-1019308 (to GO and CL), DEB-0732819 (EOW), DEB 0732589 (TG), DEB-0732894 (KC), DEB 0963767 (JAL), and DEB-0732969 (GL); GWU Selective Excellence in Diversity of Life program (to RBR); Leading Academic Discipline Project of Shanghai Municipal Education Commission, project number S30701 (CL). The Biodiversity Institute, University of Kansas, provided financial support for the collection used in this study.
— Greenwood et al. (1966)1
“…With the variety of both primitive and advanced teleosts living today, we are most emphatically of the opinion that approaches other than morphological ones would be exceedingly fruitful in the investigation of teleostean interrelationships…”
Our view of the phylogeny and classification of bony fishes is rapidly changing under the influence of molecular phylogenetic studies based on larger and more taxonomically comprehensive datasets. Classification schemes displayed in widely used text books on fish biodiversity (e.g.,2,3) have been based on loosely formulated syntheses (supertrees) and community consensus views of largely disconnected studies. The phylogenetic structure underpinning such classifications has many areas that are notably unresolved and poorly known, providing weak or no justification for many groups that, although formally recognized, are implicitly known to be polyphyletic (e.g. percoids, perciforms, scorpaeniforms). A comprehensive phylogenetic tree for all major groups of fishes has been elusive because explicit analyses including representatives across their diversity have never been accomplished. Detailed morphological cladistic investigations of fish relationships have typically focused on lower taxonomic scales and few attempts to synthesize morphology at higher taxonomic levels proved to be challenging and met limited success (e.g.,4). A recent effort to systematically collect morphological synapomorphies from published records for all currently recognized groups resulted in the first teleost classification based on monophyletic groups5. This effort, however, did not produce a global phylogenetic hypothesis. Similarly, molecular analyses have been limited and many times conflicting in terms of genetic coverage and taxonomic sampling.
As predicted by Greenwood et al.1, development of molecular markers, especially sequences of mitochondrial DNA (mtDNA) genes or complete mitochondrial genomes, catalyzed new views of bony fish relationships by providing a common yardstick of phylogenetic information across vast taxonomic scales6,7,8. Studies based on mitogenomic data proliferated to methodically probe conflicting hypotheses of relationship for several groups at diverse taxonomic levels, many times proposing alternative arrangements supporting new clades unsuspected by previous classifications10,11,12,13. In spite of their new powerful insights, mitogenomic hypotheses were not universally embraced because they represent information from a single locus, prompting corroboration from additional genomic regions. Several nuclear DNA markers were subsequently developed and applied to infer bony fish relationships. The most popular ones include 28S ribosomal subunit14,15,16, tmo4c4 17,18, rhodopsin19,20, rag1 and rag221,22, mll20, irbp23, and rnf21324. Using a systematic approach to scan genomic databases, a larger set of nuclear markers became available in 2007 25, opening a new window to obtaining large multilocus datasets25,26,27,28,66. Recent studies using between 10 and 20 of these nuclear markers for a few hundred taxa27,28,29,30,31,66, have shown improved resolution of phylogenetic relationship at higher and lower taxonomic levels. Many but not all of the mitogenomic hypotheses received support from nuclear gene data, but the discovery of new clades continued with increasing taxonomic sampling. Initially identified by letters (e.g., clades A, B, C, etc.19,23,32), new names were recently proposed for many groupings supported by molecular evidence, such as Stiassnyiformes, Zeiogadiformes, Carangimorpha, Cottimorpha, Ovalentaria, Gobiiformes etc.24,31,33. Validation of these groups (and their proposed names) is pending until a comprehensive study including all taxa is produced. Proliferation of new names is useful for identification of the newly discovered groups, but may create confusion if not systematically organized into a global classification.
Molecular phylogenetic methods (e.g., BEAST34) in combination with fossil evidence also opened a new temporal window to understand bony fish diversification. Attempts to estimate divergence dates among crow-group lineages using this approach (e.g., 35,36,37) frequently produced conflicting views with the paleontological literature38,39,40, sometimes implying large gaps in the fossil record. The discrepancy is larger when divergence estimates for crown teleost lineages have been based on mitogenomic data (e.g.,37,41,115). Nucleotide saturation, compressing basal branch lengths for mtDNA, and the specific approaches used to apply fossils constraints to calibrate the molecular phylogeny may explain this discordance43. Other studies based on several nuclear genes and larger sets of fossil calibration points produced divergence dates more consistent with the fossil record29,66, but a comprehensive time-tree for osteichthyan diversification is not yet available.
The shape of the bony fish tree of life is currently better resolved for the early-branching lineages than for the more apical acanthomorph groups, in particular the percomorphs, a large and diverse group of spiny-finned fishes with uncertain affinities that came to be known as “bush at the top”44. Few basal branching events among osteichthyans remain problematic, for example, the relationships among lungfishes, coelacanths, and tetrapods45,46,47,66. In contrast, the basal branching pattern for early extant actinopterygians (involving polypteriforms, chondrosteans, lepisosteids, Amia and teleosts) have been resolved with confidence based on morphological and DNA sequence evidence66. Similarly, recent molecular studies based on several nuclear genes25 consistently support relationships among major teleost groups: Elopomorpha, Osteoglossomorpha and Euteleostei29,66. The deeper nodes among euteleosts and percomorphs also could be resolved with confidence with this new set of nuclear markers, but a comprehensive phylogeny including all groups is lacking. In this study we report phylogenetic results based on a taxonomically comprehensive dataset with DNA sequences for 21 nuclear genes. A dataset with 1416 taxa was assembled, including four tetrapod and two chondrichthyan outgroups. Bony fish diversity is represented by 1093 genera (of ca. 4300), 369 families (of 502), and all traditionally recognized orders5, making this the most comprehensive dataset ever compiled in systematic ichthyology. Phylogenetic results corroborate many previously established hypotheses, but also provide unprecedented resolution among percomorphs. The uncertain relationships involving most of the extant diversity of percomorphs is resolved into several well-supported groups and, for the first time, we offer a monophyletic definition for Perciformes. Using a set of 60 calibrations, we also provide the most comprehensive hypothesis to date about the tempo of osteichthyan diversification. Considering the new clades obtained in this study and previously published well-supported clades, we propose a new classification for bony fishes based on the nomenclatural scheme recently proposed by Wiley and Johnson5. Our hope is that this explicit proposal will facilitate communication among ichthyologists attempting to chart the rapidly changing landscape of phylogeny and classification of fishes.
Materials and Methods
Molecular data and taxonomic sampling
This study is the main product of the Euteleost Tree of Life Project (EToL). A total of 21 molecular markers with a genome-wide distribution were examined, the majority of which were developed by EToL using a genomic screen pipeline25. This pipeline compared the Danio rerio and Takifugu rubripes genomes to identify single-copy genes with long exons (>800 bp) and divergence levels suggesting they evolve at rates appropriate for phylogenetic resolution among distantly related taxa. Exons markers were sequenced from 11 nuclear genes previously published by our group (kiaa1239, ficd, myh6, panx2, plagl2, ptchd4 (=ptr), ripk4, sidkey, snx33 (=sh3px3), tbr1b (=tbr1), and zic1) and three additional markers, including one intron (hoxc6a) and two exons (svep1, and vcpip), were newly developed for this study using the same approach. Sequence data from seven additional markers, including EToL markers (enc1, gtdc2 (=glyt), and gpr85 (=sreb2)) or markers developed by others (16S mtDNA, rag1, rag2, and rh), were generated for our previous studies (e.g., 25,26,27,28,66,96) or obtained from NCBI, Ensembl, or other genomic databases.
A total of 1184 bony fish taxa were initially targeted for this study and samples were primarily obtained from the tissue repository of the Ichthyology Collection at University of Kansas (1129 samples) or other collections. Of the initial list, samples for 18 taxa either failed to amplify or belonged to duplicate species that were ultimately combined or discarded. Sixty taxa that produced sequence data for one or two genes only were also discarded. Twenty-five additional taxa were excluded from the final matrix because they had low genetic coverage and highly variable phylogenetic placement in preliminary analyses, as identified using bootstrap trees obtained with RAxML v7.349 and the RogueNaRok server50. Our final sampling thus included 1081 taxa and sequence data from 335 additional taxa were obtained from previous EToL studies (e.g., 25,26,27,28,66,96) or public databases (Table S1). In order to minimize missing data, some sequences retrieved from public databases were combined as genus-level composite taxa (52 taxa). DNA extraction, amplification protocols via nested PCR, and primers followed previous studies (e.g., 25,26,27,28,66,96). Primer sequences and optimized PCR conditions used for the three new markers is presented in Table 1. The PCR amplicons obtained were submitted for purification and sequencing in both directions to High Throughput Sequencing Solutions (HTSeq.org) or other core facilities.
Fish diversity is represented in the phylogenetic data matrix by a sample of 1410 bony fish species (of ca. 3100051) plus four tetrapod species and two chondrichthyan outgroups (total 1416 terminals). The taxonomic sampling of bony fishes consists of 1093 genera (of ca. 4300), 369 families (of 502; see below), and all traditionally recognized orders (e.g.,5). Our taxonomic sampling emphasizes representation of percomorph groups, with 1037 (of >15000) species in 201 families. All scientific names were checked against the Catalog of Fishes51. A complete list of material examined is given in Table S1.
*1st and 2nd are primers for the first and nested/seminested (optional) rounds of PCR, respectively.
*1st and 2nd are primers for the first and nested/seminested (optional) rounds of PCR, respectively.
Sequence alignment and phylogenetic analyses
Contigs were assembled from forward and reverse sequences using CodonCode Aligner v3.5.4 (CodonCode Corporation), Sequencher v4 (Gene Codes Corporation), or Geneious Pro v4.5 (Biomatters Ltd.). Exon markers were aligned individually based on their underlying reading frame in TranslatorX52 using the MAFFT aligner53. The hoxc6a and 16S sequences were aligned with MAFFT v6.953 using 1000 iterations and the genafpair algorithm. Because nested PCR is highly prone to cross-contamination, we vetted the data by visually inspecting individual gene trees estimated with the Geneious Tree Builder algorithm in Geneious. To qualitatively assess gene-tree congruence, the final gene alignments were analyzed under maximum likelihood (ML) in RAxML using ten independent runs for each; exon alignments were partitioned by codon position. Alternative approaches to analyze combined data based on species-tree methods that account for gene-tree heterogeneity due to lineage sorting (e.g.,54,55,56,57) could not be applied to this dataset due to high proportion of missing data (see Results).
Individual genes were concatenated using SequenceMatrix v1.7.858 or Geneious. Two datasets were assembled and analyzed separately, one including all 1416 taxa with sequence data from three genes or more (3+ dataset) and a subset including 1020 taxa with sequence data from seven genes or more (7+ dataset). Analyses of the 3+ dataset were performed under maximum likelihood (ML) using two partitioning schemes, a simple one determined arbitrarily with 5 data partitions (3 codon positions across all exons plus 16S and hoxc6a), and a more complex scheme with 24 partitions (a combination of codon positions and individual genes plus 16S and hoxc6a) indicated by PartitionFinder59. To make the PartitionFinder analysis scalable, a representative subset of 201 taxa was run under the Bayesian Information Criterion59. The 7+ dataset was analyzed with the 24-partition scheme only. Analyses for both datasets and partition schemes were conducted in RAxML using 30 independent replicates under the GTRGAMMA model. Nodal support was assessed using the rapid bootstrapping algorithm of RAxML with 1000 replicates estimated under the GTRCAT model60, and the collection of sample trees was used to draw the bibartition frequencies on the optimal tree. All RAxML analyses were conducted in the CIPRES portal v3.1.
For comparison purposes, the 3+ dataset was also analyzed under implied-weighted parsimony61. The optimal tree search and bootstrap trees were set to run independently. Gaps were treated as missing characters and all parsimony uninformative characters were ignored. A relatively mild value of k (20) was chosen arbitrarily due to computational limitations to explore sensitivity of the nodes to other weighting functions. Tree searches were performed in TNT 1.163 using a driven-search strategy combining the following tree-search algorithms: ratchet, drift, sectorial searches and tree fusion. The exhaustiveness of the search parameters was self-adjusted every 2 hits of the current best score. To maximize tree-space exploration, the final searches implemented tree-bisection-reconnection (TBR). A strict consensus of nine equally optimal trees (length 407187 steps; fit 7309.19) was computed. Bootstrap search strategies were relaxed to ten random addition sequences and TBR, saving only one tree per replicate (1000 replicates); bootstrap bipartition frequencies were drawn on the consensus tree.
Divergence time estimates
Time-tree estimation in a Bayesian framework using the complete dataset was computationally infeasible. Thus, we selected a subset of 202 taxa for 18 genes that had representation of: (i) all major bony fish lineages, (ii) lineages encompassing the nodes in which the assignment of fossil calibrations is most informative, (iii) taxa with the highest genetic coverage to minimize missing data in the data matrix (the markers vcpip, svep1, hoxc6a, including a high proportion of missing data, were also excluded). Divergence times were estimated in BEAST v1.7 using the uncorrelated log-normal (UCLN) clock-model34. Sixty calibration points were selected as priors for divergence time estimates, of which 58 are based on previous studies29,64,65,66 and two (calibrations 45 and 60) are proposed here (Appendix 1). However, the actual BEAST analysis conducted for this study included 59 calibrations only (see details under calibration 60, Appendix 1). A starting chronogram that satisfied all priors (e.g., monophyly and initial divergence times) was generated under penalized likelihood in r8s v1.7167 using the RAxML tree. To model branching rates on the tree, a birth-death process was used for the tree prior with initial birth rate = 1.0 and death rate = 0.5. The substitution model was GTR+G with 4 rate classes and the data were partitioned into 4 categories with independent parameter estimation: three codon positions across exons of protein-coding genes plus 16S. Clock and tree priors were linked across partitions. Five replicates of the Markov chain Monte Carlo (MCMC) analyses were each run for 200 million generations, with the topology constrained to that recovered in the phylogenetic analyses of the 3+ dataset (pruned for taxa not included in the subset). Post-run analysis of MCMC log files was assessed using Tracer v. 1.568 and mixing was considered complete if the effective sample size of each parameter was >20034,68. Tree files from the five runs were combined in LogCombiner v1.7.468 with the first 10% of trees from each run discarded as burn-in. The maximum clade credibility tree, with means and 95% highest posterior density of divergence times, was estimated with TreeAnnotator v1.6.168.
The complete tree with 1416 taxa was time-calibrated under penalized likelihood (PL67) with treePL69. The PL model, which assumes rate autocorrelation, has been shown to perform poorly in simulation studies resulting in high stochastic error of divergence time estimates70. To ameliorate this problem, mean highest posterior density estimates of clade ages obtained with the subset in BEAST were imposed as fixed secondary calibrations for the PL analysis, rather than using primary calibrations with minimum and maximum age constrains. A total of 126 secondary calibrations were used for this analysis, including the ages obtained for all major groups in the tree as well as the nodes near which primary calibrations were defined. The rate smoothing parameter was set to 10 based on the cross-validation procedure and the χ2 test in treePL (four smoothing values between 1 and 1000 were compared).
Results and Discussion
The final concatenated alignments included 21 markers with 20853 sites for 1416 taxa in the 3+ dataset and 1020 taxa in the 7+ dataset. The average presence of data (number of sequences per taxon) across the alignments was 41.0% for the 3+ dataset and 48.2% for the 7+ dataset. A summary of dataset features, including data presence, alignment length, and sequence variation for each marker is given in Table 2 (see also Table S1). The new sequences have been deposited in GenBank under accession numbers KC825360-KC831391. The sequence alignment (nexus format), ML tree (newick format), and Table S1 are available from the Dryad repository (DOI:10.5061/dryad.c4d3j). The main phylogenetic hypothesis is summarized in Fig. 1 (24-partition RAxML tree, 3+ dataset, time-calibrated under PL). Fig. 2 provides measures of congruence among alternative analyses (concatenation and gene trees) for all major clades and provides discrete tests for traditional hypotheses in ichthyology. Figs. 3–10 provide more detail on the relationships within selected percomorph clades based on the tree in Fig. 1. The time-calibrated (BEAST) tree for the subset (202 taxa and 18 genes) and 59 calibration points are shown in Fig. 11 (see also Appendix 1); Fig. 12 compares the results of divergence times estimated for major groups with those obtained by other recent multi-locus studies. The complete phylogeny with bootstrap values and taxonomic annotations is depicted in Fig. S1 as a cladogram and can also be visualized online as a time-tree using a fractal explorer and zooming interface at OneZoom73 (also posted at DeepFin).
The basal nodes of the tree and relationships among early branching groups of bony fishes have been well established and thoroughly discussed by recent molecular systematic studies based on similar sets of genes29,66, albeit with reduced taxonomic sampling. Because our results corroborate these hypotheses (e.g. monophyly of Actinopterygii and Holostei, branching order of elopomorphs and osteoglossomorphs; Fig. 1), we refer the reader to those papers for discussion on relationships among lineages from the root of the tree up to the Euteleosteomorpha. The most significant new results involve crown acanthomorph lineages, in particular the unprecedented resolution among percomorphs, represented in this study by 1037 species in 201 families. The proverbial “bush at the top” is now disambiguated into several well-supported clades at the ordinal or supraordinal level, with well-resolved relationships amongst them (Fig. 1). We also provide for the first time a monophyletic definition of Perciformes, sinking into this clade components of Scorpaeniformes, Gasterosteiformes, and Cottiformes (Fig. 10; see also16,74). Among the euacanthomorphs, we find the non-monophyly of Beryciformes (including Stephanoberyciformes) and a sister-group relationship between holocentrids and percomorphs, first recognized by Stiassny and Moore75 and Moore76, but challenged by Johnson and Patterson4.
Based on the topology obtained (Figs. 1-10, S1) we propose a new classification for ordinal and subordinal groups of bony fishes and subsequently discuss some of the most significant findings.
*New markers developed here
Alignment length (sites)
Pairwise identity (%)
Gene for peroxisomal enoyl-CoA hydratase/L-3-hydroxyacyl-CoA dehydrogenase
gtdc2 (= glyt)
Glycosyltransferase-like domain containing 2
Homeo box C6a
Leucine-rich repeat and WD repeat-containing protein, KIAA1239-like
Myosin, heavy polypeptide 6
Pleiomorphic adenoma gene-like 2
Patched domain containing 4
Recombination activating gene 1
Recombination activating gene 2
Receptor-interacting serine-threonine kinase 4
Sorting nexin 3; similar to SH3 and PX domain containing 3 gene
G protein-coupled receptor 85
Sushi, von Willebrand factor type A, EGF and pentraxin domain containing 1
T-box, brain, 1b
Valosin-containing protein p97/p47 complete interacting protein 1
Zic family member 1
*New markers developed here
Revised Classification for Bony Fishes
The nomenclatural arrangement presented in Appendix 2 builds on the existing classification by Wiley and Johnson5 and intends to preserve names and taxonomic composition of groups whenever possible. However, adjustments are made to recognize new well-supported molecular clades, many of which also have been obtained by previous molecular studies (several examples discussed below). Order-level or supraordinal taxa are erected (new) or resurrected on the basis of well-supported clades only (>90% bootstrap values). Current taxon names supported by previous molecular or morphological studies are retained if congruent with our results, even if bootstrap support is low (e.g., Osteoglossocephalai sensu Arratia79 with only 38% bootstrap). In some cases, ordinal or subordinal taxa that were not monophyletic in our analysis are also validated, as long as the incongruence is not supported by strong bootstrap values. Examples include the suborder Blennioidei (not monophyletic here but monophyletic in Wainwright et al.31) and the order Pleuronectiformes (not monophyletic here but monophyletic in Betancur-R. et al.28).
Family names for bony fishes are based on Eschmeyer and Fong89 and van der Laan et al.90, with minor modifications. Consult van der Laan et al.90 for authorship of family names and Wiley and Johnson5 for authorship of ordinal and subordinal names. Our list is not intended as a comprehensive revision of valid family names; instead, it is simply an adaptation of their list based on published studies that we know validate or synonymize family groups using explicit phylogenetic evidence. Unlike Eschmeyer and Fong89 and van der Laan et al.90, we do not recognize the family status of Anotopteridae, Omosudidae (synonyms of Alepisauridae91) or Latidae (synonym of Centropomidae27,92). Also, we recognize the following families, listed in Eschmeyer and Fong89 and van der Laan et al. 90 as synonyms or subfamilies of other families: Botiidae (following Chen et al.93), Diplophidae (following Nelson2; apparently omitted by Eschmeyer and Fong89), Horabagridae (following Sullivan et al.94), Sinipercidae (following Li et al.96), Steindachneriidae (following Roa-Varon and Ortí98), Zanclorhynchidae, the aulopiform Bathysauropsidae and Sudidae (following Davis91), and the pleuronectiform Paralichthodidae, Poecilopsettidae, and Rhombosoleidae (following Chapleau97, Munroe99, Betancur-R. et al.28). A total of 502 families are recognized here, of which 369 (73.5%) were examined. Of these, 146 families included only one representative (39.6%) and 40 (17.9%) of the remaining 223 were rendered non-monophyletic in our analysis (non-monophyletic families are indicated below). For each order/suborder we list all families examined as well as the unexamined families whose taxonomic affinity is expected on the basis of traditional taxonomy or phylogenetic evidence. The list of unexamined families is also intended as a resource that may help fish systematists to direct future sequencing efforts.
A total of 66 orders are classified, three of which are new (Holocentriformes, Istiophoriformes, and Pempheriformes), and 15 are resurrected or validated under a new circumscription. Some ordinal or subordinal names may appear to be new, but most can be found in the literature at various hierarchical levels. As examples, Spariformes is a Bleeker name and Centrarchiformes is a Webber and de Beaufort name. Because priority is not applied to names above the family level, we have not made a thorough attempt to establish first use. Only those three for which no reference could be found are listed as “new.” New infraorders are named in Suborder Cottioidei to circumscribe well-corroborated clades and may conserve the rank of superfamily in subsequent revisions. The ordinal status of 50 percomorph families examined (as well as many others unexamined) belonging to Carangimorphariae, Ovalentariae, and Percomorpharia remains uncertain (i.e.,incertae sedis) due to poor phylogenetic resolution. Percentages in parentheses following names indicate bootstrap support (no bootstrap values shown for redundant groups or monotypic taxa). The complete phylogenetic tree with annotated classification is illustrated in Fig. S1. The new classification scheme presented here should be considered a work in progress (version 1; Appendix 2), as any other hypothesis. It is likely to include involuntary errors and omissions in addition to the many unexamined, sedis mutabilis, and incertae sedis taxa. Updates should be forthcoming as new evidence become available and feedback from experts help refine it. For the most updated version visit DeepFin.
Comparison of classifications
Our results (Appendix 2) invite comparison to the recent classification of Wiley and Johnson5 based on morphological evidence gleamed from many investigators. Of 123 clades recognized by them, 70 (56.9%) are congruent with bootstrap values >95% obtained in this study. Five of these 70 clades are included in our sample by only one family and thus their monophyly is not critically tested. Another six clades (4.9%) are congruent but are supported by lower bootstrap values; seven additional clades (5.7%) are monotypic. Forty clades (32.5%) are incongruent, with some being grossly polyphyletic in our tree. Notable examples are Protacanthopterygii, Smegmamorpharia, and Labriformes. Others are incongruent based on exclusion of subclades and are rendered monophyletic in our classification by the addition or removal of smaller clades. Examples include Stomiatii (inclusion of Osmeriformes sensu stricto), Otomorpha (inclusion of Alepocephaliformes), Neoteleostei (removal of Stomiatiformes), and Lampridiformes (removal of Stylephorus).
There is considerable consensus between morphology and the interrelationships of major clades. For example, the major cohorts of living teleosts and their interrelationships are congruent with the listing convention employed by Wiley and Johnson5; this is also true within many of the major clades (e.g. relationships within Elopomorpha). But there is also incongruence. For example, relationships among early-branching acanthomorph groups differ considerably from previous morphological hypotheses (e.g., Johnson and Patterson4) with lampridiforms, percopsiforms, zeiforms and gadiforms branching off basally relative to polymixiiforms. More explicit tests of new and alternative phylogenetic hypotheses based on multiple analyses of our dataset are presented in Fig. 2.
Novel Clades of Teleost Fishes
The following sections highlight some of the salient features of this global phylogeny and classification of bony fishes, especially in reference to well-established relationships and newly found clades among the euteleosts. We do not attempt to provide a complete account of all taxonomic issues, but to give some perspective and contrast to discuss the evidence supporting novel and established taxa.
Early euteleost lineages: tenuous relationships (Fig. 1)
Our analyses support several recent hypotheses based on molecular data that contradict the consensus based on morphology2,5 relative to the composition of “protacanthopterygians.” Although our results fall short of resolving with confidence circumscription and relationships among taxa in this group (hence Protacathopterygii is a sedis mutabilis taxon in our proposed classification), some relationships are well supported and consistent with previous studies (Fig. 1). First, is the hypothesis that alepocephalid fishes (slickheads) have affinities within Otomorpha, instead of Argentiformes, as proposed by Johnson and Patterson4. This result was first proposed on the basis of mitogenomic data10,41,100,101 and recently corroborated with a subset of the nuclear markers used in this study29. Second, is the sister group relationship of Osmeriformes and Stomiatiformes (=Stomiiformes), first proposed by López et al.21 based on mtDNA and rag1 sequence data. Finally, the position of Lepidogalaxias at the base of the euteleosts rendering Galaxiidae non-monophyletic also was proposed previously102,29 and supported by our data (see also Fig. 2).
Paracanthomorphacea: mitogenomics dixit (Fig. 1)
This name was first introduced as superorder Paracanthopterygii (sensu Greenwood et al.1) to refer to a large group of spiny-finned fishes that included Batrachoidiformes, Gadiformes (with Ophioidei and Zoarcoidei), Gobiesociformes, Lophiiformes, and Percopsiformes. Many other taxa were added and also removed on the basis of conflicting evidence ever since Paracanthopterygii was conceived, but a conservative stance persisted in classifications supporting the original circumscription, with the exclusion of Gobiesociformes2. More recently, mitogenomic data7,8 discovered a sister-group relationship between Zeiformes and Gadiformes, a result also obtained with nuclear genes 19,24,103; the name Zeioigadiformes24 was coined for this new grouping. Miya et al.11 redefined the Paracanthopterygii to include Polymixiidae, Percopsiformes, Gadiformes, and Zeioidei and subsequently Miya et al.13 added to this group the lampridiform genus Stylephorus, which was unexpectedly found to form the sister group of Gadiformes. Analysis of four nuclear markers in addition to mtDNA confirmed this result103, supporting a monophyletic taxon Paracanthopterygii that includes percopsiforms, gadiforms, Stylephorus (placed in its own order Stylephoriformes) and zeiforms, in agreement with our results (Fig. 1, 2). A review of published morphological characters by Borden et al.105 also found significant congruence between this arrangement and morphological character-state distributions for many of the proposed relationships.
Euacanthomorphacea: holocentrids sister to percomorphs (Fig. 1)
Johnson and Patterson4 included polymixiids, percopsids and crown acanthomorphs in their Euacanthopterygii, a taxon not classified by Wiley and Johnson5. We adopt the name but modify the circumscription to recognize a well-supported clade (99% bootstrap) that includes beryciforms, holocentrids and percomorphs. The main issue at this level is delimitation of Beryciformes and relationships of its proposed components to Percomorphaceae. Most classifications2,4 accept separate orders Stephanoberyciformes and Beryciformes, each monophyletic and placed as successive sister-groups of the percomorphs. Molecular data (mitogenomic and smaller subsets of nuclear genes), in contrast, have supported the inclusion of Stephanoberyciformes in the same clade as Beryciformes8,29 and consistently include holocentrids within this clade. Our results, however, reject this hypothesis in favor of recognizing a separate holocentrid clade (proposed here as a new order, Holocentriformes) that is sister to percomorphs (Fig. 1), a result first obtained by Stiassny and Moore75 and Moore 76 but subsequently challenged by Johnson and Patterson4. Despite relatively low support for our holocentrid-percomorph clade (57-69% bootstrap), proportionally more individual gene trees support this relationship (47%) relative to the alternative molecular hypothesis uniting holocentrids with the remaining beryciform groups (20%; Fig. 2). Our new circumscription of Beryciformes is also most similar to that of the order Trachichthyiformes described by Moore76, except that the latter excludes the berycids.
Percomorphaceae: no longer an unresolved bush (Figs. 1-10)
A major contribution from our study has been the disambiguation of the percomorph bush into nine well-supported supraordinal groups (six Series and three Subseries; Fig. 1; Appendix 2): Ophidiimorpharia, Batrachoidimorpharia, Gobiomorpharia (Fig. 3), Scombrimorpharia (Figs. 4 and 5), Carangimorpharia (with three Subseries: Anabantomorphariae, Fig. 6; Carangimorphariae, Fig. 7; and Ovalentariae, Fig. 8), and Percomorpharia (Figs. 9). Furthermore, increased phylogenetic resolution within Percomorpharia allowed the definition of a monophyletic Perciformes (Figs. 9 and 10), for the first time recovered from a vast taxonomic sample. With the exception of the cusk-eels (Ophidiimorpharia) and the toadfishes (Batrachoidimorpharia), whose monophyly has been recognized in most classifications (i.e., 2,5; but see 106,107), the remaining seven supraordinal clades (four Series and three Subseries) have never been discovered by examination of anatomical features. Under different combinations of taxa, however, and based on diverse genetic markers, several of these clades have been obtained, in one form or another, by previous molecular studies (e.g.,7,8,11,12,19,20,24,27,28,29,30,31,32,33).
A corollary of the increased resolution of percomorph relationships is the demise of the Smegmamorpharia sensu Johnson and Patterson4 (see also Wiley and Johnson5; Fig. 2). Elements included in this supraordinal taxon are now scattered throughout the molecular phylogeny, placed within many of the newly found clades with high bootstrap support. For example, the pygmy sunfishes (Elassoma) are back with the other sunfishes (centrarchids), as suggested by earlier classifications and recently confirmed by molecules30. Centrarchids plus elassomatids are placed here in the resurrected order Centrarchiformes (within Percomorpharia, Fig. 9). Mugiliforms (mullets) and atherinomorphs (silversides, needlefishes, halfbeaks, guppies and allies) are placed within Ovalentariae (Fig. 8). The swamp eels and spiny eels (order Synbranchiformes, suborders Synbranchoidei and Mastacembeloidei) are placed with confidence in Anabantomorphariae (Fig. 5), together with armored sticklebacks (Indostomidae), one of the 11 families previously included in the order Gasterosteiformes. The polyphyly of Gasterosteiformes (another large clade assigned to Smegmamorpha) was first pointed out by mitogenomic evidence12. Our results place the sticklebacks, tubesnouts and sand eels (previously assigned to Gasterosteoidei) in our newly defined Perciformes (suborder Cottioidei; Fig. 10) and the rest of the families previously assigned to the suborder Syngnathoidei were relocated to our newly defined order Syngnathiformes within the Scombrimorpharia (Fig. 4, see below).
Phylogenetic resolution within five newly discovered clades, however, will require additional study. Relationships within Syngnathiformes, Scombriformes, Carangimorphariae, Ovalentariae, and Percomorpharia may be challenging to recover given the rapid radiation and diversification of these clades.
Gobiomorpharia: sweepers are out (Fig. 3)
Based on a phylogeny estimated with four mitochondrial markers, Thacker33 resurrected the order Gobiiformes, to accommodate three suborders: Gobioidei (gobies and sleepers), Kurtidoidei (nurseryfish), and Apogonoidei (including apogonids and pempherids). Previous molecular studies have shown affinities between gobioids, apogonids, kurtids and, to some extent, pempherids and dactylopterids8,11,16. There is also morphological evidence supporting a close relationship between gobids and apogonids108,109 as well as between kurtids and apogonids110. Our results provide partial support for the Gobiiformes sensu Thacker33 but we treat it here as a supraordinal group (Gobiomorpharia). A major difference is that our hypothesis segregates the family Pempheridae (sweepers) to its own order (Pempheriformes, together with Glaucosomatidae), within Percomorpharia (Figs. 1, 3, 9).
Scombrimorpharia: sea horses and tunas are close relatives (Figs. 1, 4 and 5)
One of the most unanticipated new percomorph clades is the Scombrimorpharia, grouping such disparate fishes as seahorses and tunas. This clade includes the newly circumscribed orders Syngnathiformes (Fig. 4) and Scombriformes (Fig. 5). Not surprisingly, a close relationship among taxa contained within this group, including syngnathids, mullids, callionymids, dactylopterids, scombrids, stromateids, an others, has never been proposed on morphological grounds. The Syngnathiformes, as defined here (Fig. 4), comprises mostly tropical marine reef-dwellers, traditionally placed in three distinct percomorph orders, including Gasterosteiformes (syngnathids), “Perciformes” (mullids and callionymids) and “Scorpaeniformes” (dactylopterids). Recent molecular studies have emphasized the non-monophyly of Scorpaeniformes74. We have noted above the dissolution of Gasterosteiformes12 and, as discussed below, we provide a restricted definition for Perciformes that includes many scorpaeniform taxa (Fig. 10).
Our new order Scombriformes (Fig. 5) includes most of the families previously grouped in the perciform suborder Scombroidei2 or the order Scombriformes5, except for the barracudas (Sphyraenidae) and the billfishes and swordfishes (here placed in their own order, Istiophoriformes). Sphyraenidae and Istiophoriformes are now firmly placed within Carangimorphariae (Fig. 7) together with disparate taxa such as remoras (Echeneidae), archer fishes (Toxotidae), jacks (Carangidae), flatfishes (Pleuronectiformes), and others (see below). Because billfishes and tunas are not closely related as previously suggested by anatomical studies83 (Fig. 2), the new hypothesis implies that endothermy has evolved at least twice independently in teleosts111,112. This new circumscription of Scombriformes also comprises families belonging to multiple orders in previous classifications, such as Stromateiformes (Centrolophidae, Nomeidae, Ariommatidae, Stromateidae), Trachiniformes (Chiasmodontidae), Icosteiformes (Icosteidae), and Perciformes (Bramidae, Pomatomidae, and Caristiidae). Despite the disparate morphology among members of Scombriformes, most are offshore fishes that inhabit pelagic and/or deep-sea waters.
Anabantomorphariae: freshwater and air breathing (Fig. 6)
Another major percomorph group proposed here is the series Carangimorpharia, including three subseries: Anabantomorphariae, Carangimorphariae, and Ovalentariae (Fig. 1). Species in Anabantomorphariae include representatives placed in three separate orders by Wiley and Johnson5: Synbranchiformes (swamp eels), Gasterosteiformes (Indostomus, the armored stickleback), and Anabantiformes (gouramis) (Fig. 6). While the first two orders belonged to the Smegmamorpharia4,5, the Anabantiformes were placed as incertae sedis in Percomorphacea5. The monophyly of Anabantomorphariae has also been supported on the basis of mitogenomics8,11,12 and nuclear markers28. A remarkable condition shared by members of this novel grouping is their mostly freshwater origin and restriction to Africa and South East Asia (although some members in the family Synbranchidae occur in Mexico, and Central and South America). Most are able to occupy marginal, stagnant waters due to their capacity to tolerate anoxia and to obtain oxygen directly from the air. Anabantiforms have a suprabranchial organ and synbranchids have suprabranchial pouches with respiratory function.
Carangimorphariae: flatfishes and unlikely relatives (Fig. 7)
A close affinity between other seemingly disparate groups, including barracudas, swordfishes, jacks, flatfishes, and others, has been well established by recent molecular studies10,16,19,24,27,28,112 (Fig. 7). This higher-level group has been referred to as ‘‘clade L’’ sensu Chen et al.19 or Carangimorpha by Li et al.24 (see also27,28). In looking for possible anatomical synapomorphies uniting flatfishes, billfishes, and carangids, Little et al.112 found that most taxa share a relatively low number of vertebrae, have multiple dorsal pterygiophores inserting before the second neural spine, and lack supraneurals, among others. However, according to Friedman113, some of these characters are symplesiomorphies while others are absent in the remaining carangimorph groups. It thus seems paradoxical that despite the apparent lack of morphological synapomorphies for carangimorphs there is a strong molecular signal supporting their monophyly, whereas the opposite is true for pleuronectiforms28. For additional insights and discussion on Carangimorphariae we refer the reader to recent studies24,27,28,112,113.
Ovalentariae: sticky eggs (Fig. 8)
Ovalentariae is one of the most spectacular percomorph radiations, including more than 5000 species in some 44 families, grouping seemingly distinct groups such as cichlids, mullets, blennies, and atherinomorphs (atheriniforms, beloniforms, and cyprinodontiforms). This clade was first found on the basis of mitogenomic evidence8,12 and later confirmed with nuclear sequence data23,24,26,31. Our results suggest that this group can be divided into four subgroups (superorders), two of which already existed (Atherninomorphae and Mugilomorphae) and two that are new: (i) Cichlomorphae (Cichlidae plus Pholidichthyidae) and (ii) Blennimorphae (blennioids plus clingfishes, jawfishes and basslets). Many families in Ovalentariae, however, remain incertae sedis (e.g., Embiotocidae and Pseudochromidae). Two different studies have coined a name for this group; first Stiassnyiformes by Li et al.24 and, more recently, Ovalentaria by Wainwright et al.31 for their characteristic demersal, adhesive eggs with chorionic filaments (lost secondarily in some groups). An interesting implication of this phylogenetic hypothesis is that the pharyngeal jaw apparatus (pharyngognathy), present in many members of this clade (e.g., Cichlidae, Pomacentridae, Hemiramphidae), has evolved multiple times in percomorphs31. We refer the reader to Wainwright et al.31 for additional discussion on Ovalentariae.
Percomorpharia: the new bush at the top (Fig. 9)
Percomorpharia is by far the largest percomorph clade, including 11 orders with some of the most prominent ones such as Perciformes, Labriformes, Lophiiformes, and Tetraodontiformes. At least 151 families (105 examined) belong in Percomorpharia, including three of the top ten most diverse families of fishes (i.e., Labridae, Serranidae, and Scorpaenidae)2. More than one third (514) of the species in our bony fish phylogeny are placed in this clade. Previous molecular studies obtained monophyletic groups with a combination of taxa here assigned to Percomorpharia, but with far more limited sampling (e.g., 8,11,16,74). Although most family-level and ordinal groups within Percomorpharia receive high bootstrap support, interrelationships among them are largely unresolved (hence, the new bush at the top; Fig. 9). Several of these groups are newly proposed or resurrected orders under new circumscription (e.g., Uranoscopiformes, Ephippiformes, Pempheriformes). Our new arrangement removes anglerfishes (Lophiiformes) from Paracanthomorphacea, as was suggested by previous classifications78, and places them close to tetraodontiforms, caproids, acanthuriforms, chaetodontids, pomacanthids, ephippids and others (see also 87,114,115). The largest group within Percomorpharia is the order Perciformes.
Perciformes: no longer a taxonomic waste basket (Fig. 10)
For the first time, a monophyletic definition of Perciformes can be recovered from phylogenetic analysis of a comprehensive taxon sampling. The new circumscription of Perciformes reduces significantly the number of included taxa, while retaining remarkable diversity that can be organized into several suborders and infraorders. Nelson’s classification2 included 160 families in Perciformes, making it the largest order of all vertebrates. Our definition indicates unambiguous membership for 38 families and uncertain membership for an additional 42 that were not examined in our study but that have been assigned to either “Perciformes” (10), “Scorpaeniformes” (14), Cottiformes (8), or Trachiniformes (1) in previous classifications2,5. Hence, the maximum possible number of families in the newly defined Perciformes is reduced to 71. This number is closer to the 90 families proposed by Wiley and Johnson5 for their Perciformes, but with a very different composition.
For a long time, Perciformes has been regarded as a “taxonomic waste basket”2,5 with ‘‘percoids’’ scattered throughout Percomorpha and no clear phylogenetic distinction among Percoidei, Perciformes, and Percomorpha74. Earlier molecular studies lacked sufficient sampling to resolve phylogenetic questions among “percoids,” but close relationships among groupers (Serranidae), perches (Percidae), sticklebacks (Gasterosteidae), searobins (Triglidae), icefishes (Notothenioidei), sculpins (Cottoidei), eelpouts (Zoarcoidei) and scorpionfishes (Scorpaenoidei) have been obtained in one form or another, and in different combinations, by several authors16,19,20,23,24,29,74,116. All of these taxa are included in our definition of Perciformes (Fig. 10).
Within Perciformes, we tentatively propose suborders (Notothenioidei, Scorpaenoidei, Trigloidei, Cottoidei) for clades with high support that also represent some well-established groups, but two incertae sedis (Percophidae and Platycephalidae), and several unexamined families remain unclassified. Additional taxon sampling and more data are needed to resolve interrelationships among these taxa. Four suborders/infraorders were recognized as separate orders by Wiley and Johnson5: Percoidei, Scorpaenoidei, Cottioidei, and Gasterosteales (an infraorder of Cottioidei).
The composition of Perciformes obtained from our phylogeny is remarkably similar to a group named “Serraniformes” by Li et al.24. This choice of name is misleading, given that Percidae is included and serranids have historically been considered a family within Perciformes. Adoption of Serraniformes would obliterate the long ichthyological tradition of defining higher taxa with the prefix “perco” for hierarchical groups that contain perciforms (preserved in our classification). Most recently, the same team of researchers (Lautredou et al.116) presented a detailed analysis of this clade using seven nuclear markers and obtained phylogenetic relationships that are generally congruent with our results (Fig. 10), albeit they support a close relationship of Percophidae with notothenioids and divide platycephaloids into three groups. We refer the reader to this paper, as well as others (e.g., Smith and Wheeler16; Smith and Craig74), for more details on taxonomic issues.
A New Timescale of Bony Fish Evolution
In addition to the novel insights regarding the interrelationships of teleost fishes, our study provides the most comprehensively sampled time-tree of bony fish evolution based on 60 calibrations points (Figs. 1, 11). Recent studies that estimated divergence times using multi-locus nuclear approaches had more restricted taxonomic focus and implemented fewer (<36) fossil calibrations29,66. The time-calibrated phylogeny for bony fishes provided here should stimulate macroevolutionary studies of fishes using phylogenetic comparative methods (PCMs).
Although our approach for calibrating the molecular phylogeny is based on a set of common fossil constraints used by the cited studies and others64,65, some differences in the results are evident (Fig. 12). Our estimates of mean divergence dates for early actinopterygian lineages tend to be younger and the divergence of neoteleosts and subtending clades are substantially older relative to those in Near et al.29 (although 95% probability distributions overlap in many cases). Sensitivity of molecular calibrations to different combinations of taxa, molecular markers, and fossil constraints have been discussed extensively by several authors, suggesting that development of better statistical methods and best practice approaches should decrease disparity among estimated ages of clades43,118,119. Compared to earlier studies reporting divergence times among teleost lineages35,36,37,120,121,41, estimates based on multi-locus data and denser taxonomic sampling tend to converge (Fig. 11), suggesting that the current trend to analyze larger data sets with well established fossil constraints will result in robust time trees in the future.
The date estimates presented herein (Figs 1, 2-11, and the OneZoom tree) confirm the notion that divergences of major ray-finned fish lineages are considerably older than the oldest known fossils for their respective groups29,66. Our estimate of 425 Ma for divergence of crown Osteichthyes places the origin of Sarcopterygii and Actinopterygii in the Middle Silurian, with the sarcopterygian crown group evolving in the Early Devonian (409 Ma) and the actinopterygian crown group evolving at the Middle-Late boundary of the Devonian (383 Ma), both of which correspond to the “Age of Fishes”. Although the oldest teleost fossils are from the late Triassic (e.g., †Pholidophorus latiusculus, Norian122), the molecular hypothesis suggests that the initial divergence of crown group Teleostei occurred long before in the Early Permian (283 Ma). Appearance of the three major teleost lineages (Elopomorpha, Osteoglossomorpha and Clupeocephala) took place in a narrow temporal window of 13 million years during this period. Paleoecological conditions surrounding the end Permian mass extinction, which resulted in extinction of up to 96% of all marine species of that time123, might have shaped the evolutionary history of early teleosts.
Recent work suggested that a major burst of teleost diversification, predominantly within Otophysa and Percomorphacea, took place in a relatively short time span between the late Mesozoic and early Cenozoic29,124. Patterns in the fossil record corroborate this idea, revealing an explosive morphological diversification of percomorphs in the aftermath of the end-Cretaceous extinction125. According to our estimates, however, the major lineages within Percomorphaceae (Ophidiiformes, Batrachoidiformes, Gobiomorpharia, Scombrimorpharia, Carangimorpharia, Percomorpharia and Perciformes) originated between 132 Ma and 82 Ma, before the end of the Cretaceous. The same is true for the diversification of many lineages within each of these groups, but explicit analyses using robust PCMs would be necessary to assess rate shifts of lineage diversification through time.
Remaining Challenges and Unresolved Issues
The new shape of the tree of life of bony fishes and the classification reflecting this structure offered by this study leaves many questions unanswered and suggests several directions for future sequencing efforts. Many families not included in the present analysis are listed in the classification and many groups defined as incertae sedis or sedis mutabilis clearly deserve additional study. Relationships for many terminal taxa, such as those within the rapid percomorph radiations, are often poorly resolved, have low bootstrap support, or have dubious resolution due to the combination of missing data, taxon sampling, and or other sources of systematic error. The relatively high proportion of missing data in the 3+ dataset (59%) is likely to have a stronger topological impact at the fine scale (towards the tips); e.g., two sister taxa with little or no genetic overlapping may not be resolved as closely related. Another major factor that may severely compromise phylogenetic inference is compositional heterogeneity (non-stationarity), in particular for gene trees, as suggested by a recent study that examined a fraction of the taxa and markers included here28. Unfortunately, efficient non-stationary approaches to analyze large and heterogeneous multi-locus data sets such as the one presented here currently are not available. Fish orders with dubious internal relationships include the Characiformes, Gymnotiformes, Lophiiformes, Pleuronectiformes, Carangiformes, among others.
Several parts of the fish tree that require additional study include (i) resolution of the relationships among coelacanths, lungfishes and tetrapods46,47,66; (ii) the basal divergence of euteleosteomorph groups and circumscription of Protacanthopterygii, in particular interrelationships of argentiniforms, galaxiiforms, osmeriforms, salmoniforms, esociforms, stomiatiforms and neoteleosts; (iii) interrelationships among components within Scombrimorpharia, Carangimorphariae, Ovalentariae, Percomorpharia, and Perciformes; and (iv) the ordinal status of 55 percomorph families examined (as well as many others unexamined) that remain with uncertain ordinal affiliation (incertae sedis). We predict that these difficult challenges in ichthyology will find renewed sources of evidence with the advent of next generation sequencing approaches and phylogenomics (e.g., 126,127). Reinterpretation of morphology and new studies of developmental patterns will be necessary to reconcile the molecular phylogenetic hypothesis with existing and expanding phenotypic data sets (e.g., 128,129).
CL and GO designed the molecular markers; REB, GO, RBR, KC, JAL, CL, EOW, TG, NIH, KL, TG, and DA designed the taxonomic sampling; GL, DJH, and TL digitized the EToL database; CL, MS, JC, RBR, FZ, TB, MC, DA, ARV, SW, and WCB generated sequence data via PCR and edited chromatograms; RBR and DA downloaded sequences from NCBI, vetted all the sequences compiled, and assembled the datasets; RBR and JAB performed phylogenetic analyses; RBR and GA selected the fossil calibrations and RBR estimated divergence times; RBR, DA, REB made the figures; RBR and EOW proposed the new classification and NIH, GA, GO, and DA made insightful additions; RBR and GO wrote the paper and RB, GO and GA took care of the final editing; all authors contributed to the writing.
AcknowledgementsWe are grateful to K. Mullaney, A. Harris, C. Nichols and T. Makinen for providing laboratory assistance. A. Bentley (Biodiversity Institute, University of Kansas) and W.L. Smith (Field Museum of Natural History) provided tissue samples. A. Acero, H. López-Fernández, and M. Coates made insightful comments on earlier versions of the manuscript. W.N. Eschmeyer and J. Fong provided access to their Catalog of Fishes database.
Calibration points and age prior settings
This section provides details on calibrations and prior settings used for divergence time estimates. Hard lower bounds or minimum age reflect the youngest possible age interpretation of fossils, rather than mid-point of age range [see 1]; soft upper bounds or maximum age indicate the oldest possible fossil age. One geological calibration uses a normal distribution with soft minimum and maximum bounds (calibration 37). For calibration details, refer to the original studies cited under each; prior distributions and settings for some calibrations were adapted for this study.
(1) Gnathostomata. MRCA: Leucoraja, Danio. Hard minimum age: 426.0 Ma. 95% soft maximum age: 519.0 Ma. Prior setting: Lognormal distribution, mean= 6.15, St. Dev.= 0.06 (crown calibration). Calibration source: Broughton et al. .
(2) Osteichthyes. MRCA: Latimeria, Danio. Hard minimum age: 418.0 Ma. 95% soft maximum age: 438.0 Ma. Prior setting: Exponential distribution, mean= 6.66 (crown calibration). Calibration source: Broughton et al. .
(3) Sarcopterygii. MRCA: Latimeria, Lepidosiren. Hard minimum age: 407.0 Ma. 95% soft maximum age: 419.0 Ma. Prior setting: Exponential distribution, mean= 4.00 (crown calibration). Calibration source: Broughton et al. .
(4) Lepidosirenoidei. MRCA: Lepidosiren, Protopterus. Hard minimum age: 70.0 Ma. 95% soft maximum age: 416.0 Ma. Prior setting: Uniform distribution (crown calibration). Calibration source: Broughton et al. .
(5) Tetrapoda. MRCA: Xenopus, Homo. Hard minimum age: 330.0 Ma. 95% soft maximum age: 350.0 Ma. Prior setting: Exponential distribution, mean= 6.69 (crown calibration). Calibration source: Broughton et al. , Benton and Donoghue .
(6) Metatheria. MRCA: Monodelphis, Homo. Hard minimum age: 124.5 Ma. 95% soft maximum age: 139.0 Ma. Prior setting: Exponential distribution, mean= 4.50 (crown calibration). Calibration source: Broughton et al. , Benton and Donoghue .
(7) Human-Mouse. MRCA: Mus, Homo. Hard minimum age: 62.0 Ma. 95% soft maximum age: 101.0 Ma. Prior setting: Exponential distribution, mean= 12.84 (crown calibration). Calibration source: Broughton et al. , Benton and Donoghue .
(8) Actinopterygii (total group). MRCA: Polypterus, Danio. Hard minimum age: 398.0 Ma. 95% soft maximum age: 423.0 Ma. Prior setting: Exponential distribution, mean= 8.35 (stem calibration). Calibration source: Broughton et al. .
(9) Polypteriformes. MRCA: Erpetoichthys, Polypterus. Hard minimum age: 5.0 Ma. 95% soft maximum age: 99.0 Ma. Prior setting: Uniform distribution (crown calibration). Calibration source: Broughton et al. .
(10) Actinopteri (total group). MRCA: Scaphirhynchus, Danio. Hard minimum age: 375.0 Ma. 95% soft maximum age: 415.0 Ma. Prior setting: Exponential distribution, mean= 13.34 (stem calibration). Calibration source: Broughton et al. .
(11) Chondrostei. MRCA: Scaphirhynchus, Polyodon. Hard minimum age: 125.0 Ma. 95% soft maximum age: 246.0 Ma. Prior setting: Exponential distribution, mean= 40.40 (crown calibration). Calibration source: Broughton et al. .
(12) Neopterygii. MRCA: Lepisosteus, Danio. Hard minimum age: 260.0 Ma. 95% soft maximum age: 386.0 Ma. Prior setting: Uniform distribution (crown calibration). Calibration source: Broughton et al. .
(13) Holostei. MRCA: Lepisosteus, Amia. Hard minimum age: 246.0 Ma. 95% soft maximum age: 350.0 Ma. Prior setting: Exponential distribution, mean= 34.70 (crown calibration). Calibration source: Broughton et al. .
(14) Elopomorpha. MRCA: Elops, Halosauropsis. Hard minimum age: 149.0 Ma. 95% soft maximum age: 260.0 Ma. Prior setting: Uniform distribution (crown calibration). Calibration source: Broughton et al. .
(15) Albuliformes + Anguilliformes. MRCA: Albula, Halosauropsis. Hard minimum age: 136.0 Ma. 95% soft maximum age: 216.0 Ma. Prior setting: Exponential distribution, mean= 26.70 (crown calibration). Calibration source: Broughton et al. .
(16) Osteoglossomorpha. MRCA: Hiodon, Arapaima. Hard minimum age: 130.0 Ma. 95% soft maximum age: 260.0 Ma. Prior setting: Uniform distribution (crown calibration). Calibration source: Broughton et al. .
(17) Notopteridae (total group). MRCA: Gymnarchus, Xenomystus. Hard minimum age: 100.0 Ma. 95% soft maximum age: 216.0 Ma. Prior setting: Exponential distribution, mean= 38.73 (crown calibration). Calibration source: Broughton et al. .
(18) Arapaimidae. MRCA: Arapaima, Heterotis. Hard minimum age: 65.5 Ma. 95% soft maximum age: 136.0 Ma. Prior setting: Exponential distribution, mean= 23.55 (crown calibration). Calibration source: Broughton et al. .
(19) Chanidae. MRCA: Chanos, Cromeria. Hard minimum age: 139.0 Ma. 95% soft maximum age: 216.0 Ma. Prior setting: Exponential distribution, mean= 25.70 (crown calibration). Calibration source: Broughton et al. . Comments: Kneriidae is not represented in the taxonomic sampling of Broughton et al. ; modified to include the MRCA of Chanidae plus Kneriidae.
(20) Cobitoidea. MRCA: Hypentelium, Barbatula. Hard minimum age: 60.0 Ma. 95% soft maximum age: 146.5-145.5 Ma, stem ostariophysan †Tischlingerichthys viohli, Late Jurassic, Germany . Prior setting: Exponential distribution, mean= 27.20 (crown calibration). Calibration source: Saitoh et al.  (prior setting adapted for this study).
(21) Cyprinidae. MRCA: Danio, Notemigonus. Hard minimum age: 48.5 Ma. 95% soft maximum age: 146.5-145.5 Ma, stem ostariophysan †Tischlingerichthys viohli (see calibration 20 above). Prior setting: Exponential distribution, mean= 32.70 (crown calibration). Calibration source: Saitoh et al.  (prior setting adapted for this study).
(22) Serrasalmidae + Hemiodontidae. MRCA: Pygocentrus, Hemiodus. Hard minimum age: 61.0 Ma. 95% soft maximum age: 97.0 Ma. Prior setting: Exponential distribution, mean= 12.02 (crown calibration). Calibration source: Broughton et al. .
(23) Callichthyidae. MRCA: Callichthys, Corydoras. Hard minimum age: 58.0 Ma. 95% soft maximum age: 146.5-145.5 Ma, stem ostariophysan †Tischlingerichthys viohli, Late Jurassic, Germany. Prior setting: Exponential distribution, mean= 29.53 (crown calibration). Calibration source: Lundberg et al.  (prior setting adapted for this study).
(24) Ictaluridae + Cranoglanidae. MRCA: Ictalurus, Cranoglanis. Hard minimum age: 63.0 Ma. 95% soft maximum age: 146.5-145.5 Ma, stem ostariophysan †Tischlingerichthys viohli (see calibration 20 above). Prior setting: Exponential distribution, mean= 27.87 (crown calibration). Calibration source: Lundberg et al.  (prior setting adapted for this study).
(25) Ictaluridae. MRCA: Ameiurus, Ictalurus. Hard minimum age: 34.0 Ma. 95% soft maximum age: 63.0 Ma, stem ostariophysan †Tischlingerichthys viohli (see calibration 20 above). Prior setting: Exponential distribution, mean= 10.01 (crown calibration). Calibration source: Lundberg et al.  (prior setting adapted for this study).
(26) Arioidea. MRCA: Gogo, Ariopsis. Hard minimum age: 65.5 Ma. 95% soft maximum age: 146.5 Ma. Prior setting: Exponential distribution, mean= 27.05 (crown calibration). Calibration source: Broughton et al. .
(27) Euteleostei. MRCA: Lepidogalaxias, Takifugu. Hard minimum age: 149 Ma. 95% soft maximum age: 260 Ma. Prior setting: Uniform distribution (crown calibration). Calibration source: Broughton et al. .
(28) Esocidae + Umbridae. MRCA: Esox, Novumbra. Hard minimum age: 76.5 Ma. 95% soft maximum age: 87.5 Ma. Prior setting: Lognormal distribution, mean= 1.09, St. Dev.= 0.8 (stem calibration). Calibration source: Near et al. .
(29) Salmonidae. MRCA: Coregonus, Oncorhynchus. Hard minimum age: 51.8 Ma. 95% soft maximum age: 76.4 Ma. Prior setting: Lognormal distribution, mean= 1.62, St. Dev.= 0.8 (stem calibration). Calibration source: Near et al. .
(30) Percopsidae. MRCA: Percopsis, Aphredoderus. Hard minimum age: 57.0 Ma. 95% soft maximum age: 65.5 Ma. Prior setting: Lognormal distribution, mean= 0.53, St. Dev.= 0.8 (stem calibration). Calibration source: Near et al. .
(31) Aphredoderidae. MRCA: Aphredoderus, Chologaster. Hard minimum age: 34.0 Ma. 95% soft maximum age: 59.0 Ma. Prior setting: Lognormal distribution, mean= 1.90, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(32) Zenopsis + Zeus. MRCA: Zenopsis, Zeus. Hard minimum age: 32 Ma. 95% soft maximum age: 36.5 Ma. Prior setting: Lognormal distribution, mean= 0.23, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(33) Lampridiformes. MRCA: Lophotus, Lampris. Hard minimum age: 56 Ma. 95% soft maximum age: 83.5 Ma. Prior setting: Lognormal distribution, mean= 2.01, St. Dev.= 0.8 (stem calibration). Calibration source: Near et al. . Comments: Lophotus was not examined by Near et al. ; modified to include the MRCA of Lophotus and Lampris.
(34) Holocentridae. MRCA: Myripristis, Sargocentron. Hard minimum age: 50 Ma. 95% soft maximum age: 57.5 Ma. Prior setting: Lognormal distribution, mean= 0.67, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. . Comments: Near et al.  report the fossil as a stem lineage of Myripristinae and assigns it to the divergence of Myripristinae + Holocentrinae. However, their figure S2 shows the calibration placed in the stem of Holocentridae; it should be the crown.
(35) Trachichthyidae. MRCA: Gephyroberyx, Monocentris. Hard minimum age: 32 Ma. 95% soft maximum age: 36.5 Ma. Prior setting: Lognormal distribution, mean= 0.23, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(36) Syngnathiformes (sensu lato). MRCA: Aulostomus, Callionymus. Hard minimum age: 70.5 Ma. 95% soft maximum age: 81 Ma. Prior setting: Lognormal distribution, mean= 1.02, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(37) Aulostomus - Panama Isthmus. MRCA: A. maculatus, A. chinensis. 5% soft minimum age: 2.8 Ma. 95% soft maximum age: 3.5 Ma. Prior setting: Normal distribution, mean= 3.15, St. Dev.= 0.212 (crown calibration). Calibration source: Bowen et al. .
(38) Centriscidae (total group). MRCA: Aeoliscus, Macroramphosus. Hard minimum age: 50 Ma. 95% soft maximum age: 57.5 Ma. Prior setting: Lognormal distribution, mean= 0.67, St. Dev.= 0.8 (stem calibration). Calibration source: Near et al. . Comments: Near et al.  used this as crown calibration one node below (with Aulostomus). Instead, we place it in the stem Centriscidae because the position of this group is unstable.
(39) Syngnathidae (total group). MRCA: Syngnathus, Doryrhamphus. Hard minimum age: 50 Ma. 95% soft maximum age: 57.5 Ma. Prior setting: Lognormal distribution, mean= 0.67, St. Dev.= 0.8 (stem calibration). Calibration source: Near et al. . Comments: Near et al.  noted that there is no phylogenetic resolution for †“Syngnathus” heckeli and †Prosolenostomus lessinii among syngnathids and assigned these fossils as stem calibration points for the MRCA of Fistularia and Syngnathus. However, because Fistularia is not a syngnathid (i.e., lacks body plates), a more appropriate placement for these two fossils (both of which have body plates) is the stem Syngnathidae.
(40) Carangiformes. MRCA: Caranx, Echeneis. Hard minimum age: 56 Ma. 95% soft maximum age: 64 Ma. Prior setting: Lognormal distribution, mean= 0.78, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(41) Echeneidae + Coryphaenidae + Rachycentridae. MRCA: Coryphaena, Echeneis. Hard minimum age: 30 Ma. 95% soft maximum age: 34.5 Ma. Prior setting: Lognormal distribution, mean= 0.17, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(42) Pleuronectoidei. MRCA: Lepidoblepharon, Heteromycteris. Hard minimum age: 50 Ma. 95% soft maximum age: 57.5 Ma. Prior setting: Lognormal distribution, mean= 0.67, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(43) Soleidae + Cynoglossidae. MRCA: Heteromycteris, Symphurus. Hard minimum age: 40.5 Ma. 95% soft maximum age: 50 Ma. Prior setting: Lognormal distribution, mean= 0.95, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. . Comments: Near et al.  placed the calibration one node below (Samaridae + Soleidae + Cynoglossidae) arguing that "Chanet (1994) argues that †Eobuglossus can be identified as a soleid on the basis of the geometry of the ascending process of the blind side premaxilla. We are not convinced that the state in this fossil can be meaningfully distinguished from the condition found in cynoglossids." A placement †Eobuglossus in the Soleidae + Cynoglossidae crown reconciles both opinions.
(44) Bothidae (total group). MRCA: Asterorhombus, Laeops. Hard minimum age: 30 Ma. 95% soft maximum age: 34.5 Ma. Prior setting: Lognormal distribution, mean= 0.17, St. Dev.= 0.8 (stem calibration). Calibration source: Near et al. . Comments: Near et al.  assigned the fossil †Oligobothus to the divergence of Bothidae + Pleuronectidae; it is likely a stem bothid .
(45) Centropomidae (new crown calibration). MRCA: Centropomus, Lates. Hard minimum age: †Eolates gracilis  and †Centropomus . Diagnosis and phylogenetic placement: placement of †Eolates gracilis in Latinae is supported by the presence of posterior pad in infraorbital 1 and by having 10+14 vertebrae; †Eolates gracilis is the earliest branching lineage of Latiinae . Stratigraphic horizon and locality: early Eocene, upper Ypresian, Monte Bolca, Italy. Absolute age estimate: 50 Ma . 95% soft upper bound: 57.5 Ma, based on the FA95 (Marshall ; following Near et al. ). Prior setting: Lognormal distribution, mean= 0.67, St. Dev.= 0.8.
(46) Chaetodontidae (total group). MRCA: Chaetodon, Leiognathus. Hard minimum age: 30 Ma. 95% soft maximum age: 34.5 Ma. Prior setting: Lognormal distribution, mean= 0.17, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(47) Chaetodon + Prognathodes. MRCA: Chaetodon, Prognathodes. Hard minimum age: 7.1 Ma. 95% soft maximum age: 9 Ma. Prior setting: Lognormal distribution, mean= 0.10, St. Dev.= 0.3 (crown calibration). Calibration source: Near et al. .
(48) Leiognathidae. MRCA: Gazza, Leiognathus. Hard minimum age: 11.5 Ma. 95% soft maximum age: 23 Ma. Prior setting: Lognormal distribution, mean= 1.12, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(49) Luvaridae. MRCA: Luvarus, Acanthurus. Hard minimum age: 56 Ma. 95% soft maximum age: 64 Ma. Prior setting: Lognormal distribution, mean= 0.78, St. Dev.= 0.8 (crown calibration). Calibration source: Near et al. .
(50) Siganidae (total group). MRCA: S. argenteus, S. vulpinus. Hard minimum age: 56 Ma. 95% soft maximum age: 64 Ma. Prior setting: Lognormal distribution, mean= 0.78, St. Dev.= 0.8 (stem calibration). Calibration source: Near et al. .
(51) Cichlidae - Heroini. MRCA: Heros, Herichthys. Hard minimum age: 49 Ma. 95% soft maximum age: 143 Ma. Prior setting: Exponential distribution, mean= 31.40 (stem calibration). Calibration source: López-Fernández et al. . Comments: a stem calibration is required because our taxonomic sampling lacks early-branching heroins.
(52) Cichlidae - Geophagini. MRCA: Crenichichla. Hard minimum age: 49 Ma. 95% soft maximum age: 143 Ma. Prior setting: Exponential distribution, mean= 31.40 (terminal-branch calibration). Calibration source: López-Fernández et al. .
(53) Ambloplytes + Pomoxis. MRCA: Ambloplytes, Pomoxis. Hard minimum age: 15.5 Ma. 95% soft maximum age: 18 Ma. Prior setting: Lognormal distribution, mean= 0.10, St. Dev.= 0.5 (crown calibration). Calibration source: Near et al. . Comments: Near et al.  assign †Archoplites to the divergence of Archoplites + Ambloplytes. Because our taxonomic sampling lacks Archoplites, we assign it to the MRCA of Ambloplytes + Pomoxis, following Collar et al.  (i.e., Pomoxis + Archoplites + Ambloplytes).
(54) Tetraodontiformes (total group). MRCA: Triacanthodes, Takifugu. Hard minimum age: 85 Ma. 95% soft maximum age: 122 Ma. Prior setting: Exponential distribution, mean= 11.69 (stem calibration). Calibration source: Alfaro et al. , Alfaro et al. . Comments: Alfaro et al.  and Santini et al.  argue: "The oldest taxon assigned to this clade is the stem tetraodontiform †Cretatriacanthus guidottii from the Santonian of Nardo (Italy). We chose this taxon to date the minimum age rather than other, older [†Plectocretacicus clarae], stem tetraodontiformes because preliminary reexamination of the relationships of extant and fossil tetraodontiforms (Santini, unpublished) casts doubt on their phylogenetic affinities." Although we adopt Santini’s interpretation here, these results should be taken cautiously until explicit evidence challenging the traditional placement of †Plectocretacicus (e.g., ) becomes available.
(55) Tetraodontidae. MRCA: Takifugu, Tetraodon. Hard minimum age: 32 Ma. 95% soft maximum age: 50 Ma. Prior setting: Exponential distribution, mean= 6.01 (crown calibration). Calibration source: Alfaro et al. , Alfaro et al. . Comments: The fossils used by Near et al.  are stem diodontids. While they argue that their assignment is one node below (i.e., divergence of Tetraodontidae + Diodontidae), their figure S2 shows the calibration placed in the stem of this clade; it should be the crown.
(56) Diodontidae + Tetraodontidae. MRCA: Diodon, Tetraodon. Hard minimum age: 50 Ma. 95% soft maximum age: 85 Ma (stem †Cretatriacanthus). Prior setting: Exponential distribution, mean= 11.52 (crown calibration). Calibration source: Alfaro et al.  (prior setting adapted for this study).
(57) Molidae (total group). MRCA: Mola, Ranzania. Hard minimum age: 41 Ma. 95% soft maximum age: 85 Ma (stem †Cretatriacanthus). Prior setting: Exponential distribution, mean= 14.52 (stem calibration). Calibration source: Alfaro et al.  (prior setting adapted for this study).
(58) Aracanidae + Ostraciidae. MRCA: Aracana, Ostracion. Hard minimum age: 50 Ma. 95% soft maximum age: 85 Ma (stem †Cretatriacanthus). Prior setting: Exponential distribution, mean= 11.52 (crown calibration). Calibration source: Alfaro et al.  (prior setting adapted for this study).
(59) Balistidae (total group). MRCA: Rhinecanthus, Abalistes. Hard minimum age: 35 Ma. 95% soft maximum age: 85 Ma (stem †Cretatriacanthus). Prior setting: Exponential distribution, mean= 16.52 (stem calibration). Calibration source: Alfaro et al.  (prior setting adapted for this study).
(60) Chondrichthyes (new crown calibration). MRCA: Leucoraja, Callorhinchus. Hard minimum age: †Chondrenchelys problematica and †Onychoselache. Diagnosis and phylogenetic placement: †Chondrenchelys is the earliest unambiguous fossil holocephalan as supported by several synapomorphies: holostylic jaw suspension; precerebral fontanelle absent; orbit separated from nasal capsule by broad, laterally facing orbitonasal lamina; Meckel's cartilage fused at symphysis; tooth families reduced, among others . †Onychoselache is the oldest stem-group elasmobranch; details of the jaws, braincase and postcranial skeleton demonstrate that Onychoselache is a well-characterized member of the Hybodontiformes . Stratigraphic horizon and locality: both †Chondrenchelys and †Onychoselache are from the Visean (early Mississippian), Glencartholm, Scotland. Absolute age estimate: 338 Ma. 95% soft maximum age: 438 Ma, †Elegestolepis conica, oldest stem chondrichthyan, Middle-Late Llandovery, Angara-Jlim area, Niuya River outcrops and Niuya-Berresova area, Siberian Platform . Prior setting: Exponential distribution, mean= 33.39. Comment: implementation of this calibration was suggested by M. Coates (pers. comm.) after completion of the BEAST analyses. Therefore, it is only used for the PL analysis of the complete tree, as hard minimum and hard maximum age constrains. Although not implemented here, the priors proposed are intended as a reference for future studies.
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