Major issues in the origins of ray‐finned fish (Actinopterygii) biodiversity

Ray‐finned fishes (Actinopterygii) dominate modern aquatic ecosystems and are represented by over 32000 extant species. The vast majority of living actinopterygians are teleosts; their success is often attributed to a genome duplication event or morphological novelties. The remainder are ‘living fossils’ belonging to a few depauperate lineages with long‐retained ecomorphologies: Polypteriformes (bichirs), Holostei (bowfin and gar) and Chondrostei (paddlefish and sturgeon). Despite over a century of systematic work, the circumstances surrounding the origins of these clades, as well as their basic interrelationships and diagnoses, have been largely mired in uncertainty. Here, I review the systematics and characteristics of these major ray‐finned fish clades, and the early fossil record of Actinopterygii, in order to gauge the sources of doubt. Recent relaxed molecular clock studies have pushed the origins of actinopterygian crown clades to the mid‐late Palaeozoic [Silurian–Carboniferous; 420 to 298 million years ago (Ma)], despite a diagnostic body fossil record extending only to the later Mesozoic (251 to 66 Ma). This disjunct, recently termed the ‘Teleost Gap’ (although it affects all crown lineages), is based partly on calibrations from potential Palaeozoic stem‐taxa and thus has been attributed to poor fossil sampling. Actinopterygian fossils of appropriate ages are usually abundant and well preserved, yet long‐term neglect of this record in both taxonomic and systematic studies has exacerbated the gaps and obscured potential synapomorphies. At the moment, it is possible that later Palaeozoic‐age teleost, holostean, chondrostean and/or polypteriform crown taxa sit unrecognized in museum drawers. However, it is equally likely that the ‘Teleost Gap’ is an artifact of incorrect attributions to extant lineages, overwriting both a post‐Palaeozoic crown actinopterygian radiation and the ecomorphological diversity of stem‐taxa.     

Genomic signatures of evolution in Nautilus—An endangered living fossil

Living fossils are survivors of previously more diverse lineages that originated millions of years ago and persisted with little morphological change. Therefore, living fossils are model organisms to study both long‐term and ongoing adaptation and speciation processes. However, many aspects of living fossil evolution and their persistence in the modern world remain unclear. Here, we investigate three major aspects of the evolutionary history of living fossils: cryptic speciation, population genetics and effective population sizes, using members of the genera Nautilus and Allonautilus as classic examples of true living fossils. For this, we analysed genomewide ddRAD‐Seq data for all six currently recognized nautiloid species throughout their distribution range. Our analyses identified three major allopatric Nautilus clades: a South Pacific clade, subdivided into three subclades with no signs of admixture between them; a Coral Sea clade, consisting of two genetically distinct populations with significant admixture; and a widespread Indo‐Pacific clade, devoid of significant genetic substructure. Within these major clades, we detected five Nautilus groups, which likely correspond to five distinct species. With the exception of Nautilus macromphalus, all previously described species are at odds with genomewide data, testifying to the prevalence of cryptic species among living fossils. Detailed F_ST analyses further revealed significant genome‐wide and locus‐specific signatures of selection between species and differentiated populations, which is demonstrated here for the first time in a living fossil. Finally, approximate Bayesian computation (ABC) simulations suggest large effective population sizes, which may explain the low levels of population differentiation commonly observed in living fossils.     

Phylogenetic Timing of the Fish-Specific Genome Duplication Correlates with the Diversification of Teleost Fish

For many genes, ray-finned fish (Actinopterygii) have two paralogous copies, where only one ortholog is present in tetrapods. The discovery of an additional, almost-complete set of Hox clusters in teleosts (zebrafish, pufferfish, medaka, and cichlid) but not in basal actinopterygian lineages (Polypterus) led to the formulation of the fish-specific genome duplication hypothesis. The phylogenetic timing of this genome duplication during the evolution of ray-finned fish is unknown, since only a few species of basal fish lineages have been investigated so far. In this study, three nuclear genes (fzd8, sox11, tyrosinase) were sequenced from sturgeons (Acipenseriformes), gars (Semionotiformes), bony tongues (Osteoglossomorpha), and a tenpounder (Elopomorpha). For these three genes, two copies have been described previously teleosts (e.g., zebrafish, pufferfish), but only one orthologous copy is found in tetrapods. Individual gene trees for these three genes and a concatenated dataset support the hypothesis that the fish-specific genome duplication event took place after the split of the Acipenseriformes and the Semionotiformes from the lineage leading to teleost fish but before the divergence of Osteoglossiformes. If these three genes were duplicated during the proposed fish-specific genome duplication event, then this event separates the species-poor early-branching lineages from the species-rich teleost lineage. The additional number of genes resulting from this event might have facilitated the evolutionary radiation and the phenotypic diversification of the teleost fish.[Reviewing Editor: Martin Kreitman]     

A new time-scale for ray-finned fish evolution

The Actinopterygii (ray-finned fishes) is the largest and most diverse vertebrate group, but little is agreed about the timing of its early evolution. Estimates using mitochondrial genomic data suggest that the major actinopterygian clades are much older than divergence dates implied by fossils. Here, the timing of the evolutionary origins of these clades is reinvestigated using morphological, and nuclear and mitochondrial genetic data. Results indicate that existing fossil-based estimates of the age of the crown-group Neopterygii, including the teleosts, Lepisosteus (gar) and Amia (bowfin), are at least 40 Myr too young. We present new palaeontological evidence that the neopterygian crown radiation is a Palaeozoic event, and demonstrate that conflicts between molecular and morphological data for the age of the Neopterygii result, in part, from missing fossil data. Although our molecular data also provide an older age estimate for the teleost crown, this range extension remains unsupported by the fossil evidence. Nuclear data from all relevant clades are used to demonstrate that the actinopterygian whole-genome duplication event is teleost-specific. While the date estimate of this event overlaps the probable range of the teleost stem group, a correlation between the genome duplication and the large-scale pattern of actinopterygian phylogeny remains elusive.     

Endocranial preservation of a Carboniferous actinopterygian from Lancashire,UK, and the interrelationships of primitive actinopterygians

The gross brain structure of an Upper Carboniferous (ca. 310 Myr ago) ray-finned fish (Actinopterygii) is described from exceptionally well-preserved fossil material from the Burnley region of Lancashire, UK. Previously identified as ''Rhadinichthys'' planti, the species is reassigned to the genus Mesopoma. Morphological characters derived from these data are combined with reviews of cranial skeletal anatomy, enamel composition, oculomoter muscle insertion and paired fin morphology to test and reanalyse hypotheses of primitive actinopterygian interrelationships. Results indicate that ancestral chondrostean (sturgeon and paddlefish) and neopterygian (teleost, amiid and gar) lineages diverged earlier than current theories suggest. Palaeonisciformes, a taxonomic group widely used to include most Palaeozoic actinopterygians, include a significant number of primitive neopterygians, several of which may form a distinct monophyletic clade. Within this revised phylogenetic context, changes in gross brain morphology from primitive conditions, as revealed by fossil data, highlight likely specializations in extant non-teleostean actinopterygians.     

Birth and death of neuropeptide Y receptor genes in relation to the teleost fish tetraploidization

Extensive evidence exists for a genome duplication in the fish lineage leading to the species-rich clade of the teleosts, comprising > 99% of the known actinopterygian (ray-finned) fish species. Our previous studies of the neuropeptide Y receptor (NPYR) gene family suggested an ancestral gnathostome repertoire of 7 genes in 3 subfamilies. However, studies in the zebrafish have earlier identified only 5 NPYR genes, despite the expected increase in gene number due to the teleost tetraploidization. Notably, receptors Y(1), Y(5) and Y(6) were missing in the zebrafish genome database and only Y(8) had been duplicated. We report here an investigation of the evolutionary history of the Y(1) subfamily (Y(1), Y(4), Y(6) and Y(8)) and the Y(5) receptor. Seven basal actinopterygian species and a shark were investigated and a total of 22 gene fragments were cloned and analyzed. Our results show that subtypes Y(1), Y(5) and Y(6) still exist in species representing basal actinopterygian lineages (bichir, sturgeon, gar and bowfin) as well as in some basal teleost lineages. Surprisingly we identified a zebrafish Y(1) receptor, the first Y(1) receptor found in euteleosts. Thus, these findings confirm the ancestral gnathostome repertoire of 7 NPYR genes and show that many of these receptors are present in basal actinopterygians as well as some basal teleosts. NPYR losses seem to have occurred relatively recently in euteleosts because Y(1), Y(5) and Y(6) are absent in the genome databases of two pufferfishes as well as medaka and stickleback and Y(5) and Y(6) are absent in the zebrafish database. A duplicate of Y(8) seems to be the only remaining receptor gene resulting from the teleost tetraploidization. The unexpected absence of the two appetite-stimulating receptors Y(1) and Y(5) in some euteleosts, along with our discovery of duplicates of the peptide ligands NPY and PYY, has implications for the role of the NPY system in euteleost feeding behavior.     

The Morphology and Evolution of the Ear in Actinopterygian Fishes

SYNOPSIS. In this paper we consider various aspects of the anatomyand ultrastructure of the actinopterygian ear and make a numberof suggestions on the possible adaptive significance of thestructural specializations. The focus of the arguments is basedupon the substantial inter-specific variation in teleost auditorysystems as measured anatomically, behaviorally, and physiologically.It is potentially of considerable significance that the majorpoints of inter-specific variation in the teleost ear are associatedwith the gross morphology and ultrastructure of the otolithicorgan most often implicated in sound detection, the sacculus.Analysis of patterns of sacculus ultrastructure has led to theconclusion that there are, in effect, only about five differentsaccular ultrastructural patterns but that these patterns arebroadly found throughout the teleost fishes. Based upon patternsof inter-specific variation in the sacculus and in other aspectsof the ear and more peripheral auditory structures (e.g., swimbladder),it is argued that adaptations encountered in the teleost auditorysystem cannot be used as reliable taxonomic indicators amongfishes. Rather, it is proposed that the teleost auditory systemis quite maleable in the evolutionary sense, and that interspecificsimilarities in many features of the auditory system reflectconvergent evoluuon, rather than phylogenetic affinities. Theactual selective pressures operating in the evoluuon of thefish auditory system are still essentially unknown. In addition,we cannot be certain that similar ear patterns in differentspecies reflect convergent evolution (or common ancestry), orthat conversely, different ear patterns among species reflectdifferences in auditory function.     

Comparative neurochemical features of the innervation patterns of the gut of the basal actinopterygian,Lepisosteus oculatus,and the euteleost,Clarias batrachus

The structure and physiology of enteric system are very similar in all classes of vertebrates, although they have been investigated only occasionally in non‐mammalian vertebrates. Very little is known about the distribution of the neurotransmitters in the gut of actinopterygian fishes. Anatomical and physiological studies of enteric nervous systems in the spotted gar (Lepisosteus oculatus) and airbreathing catfish (Clarias batrachus), a non‐teleost and teleost actinopterygian, respectively, have not been undertaken. This study provides the first comprehensive characterization of the range of neurochemical coding in the enteric nervous system of these two species, including the chemical diversity of the mucosal endocrine cells in the pyloric stomach of Clarias. Autonomic innervation of the secretory glands is also described and reported herein for the first time for fishes. We also report splanchnic (spinal) innervation of the stomach, submucosal ganglia (that also colocalize with nNOS) and caudal intestine of Clarias. In both fish species, numerous 5HT, ChAT, nNOS and TH‐positive nerve fibres have been observed. These discoveries demonstrate that much more physiological and pharmacological data are needed before a comprehensive model of enteric nervous system control in vertebrates can be developed.     

Molecular and fossil evidence place the origin of cichlid fishes long after Gondwanan rifting

Cichlid fishes are a key model system in the study of adaptive radiation, speciation and evolutionary developmental biology. More than 1600 cichlid species inhabit freshwater and marginal marine environments across several southern landmasses. This distributional pattern, combined with parallels between cichlid phylogeny and sequences of Mesozoic continental rifting, has led to the widely accepted hypothesis that cichlids are an ancient group whose major biogeographic patterns arose from Gondwanan vicariance. Although the Early Cretaceous (ca 135 Ma) divergence of living cichlids demanded by the vicariance model now represents a key calibration for teleost molecular clocks, this putative split pre-dates the oldest cichlid fossils by nearly 90 Myr. Here, we provide independent palaeontological and relaxed-molecular-clock estimates for the time of cichlid origin that collectively reject the antiquity of the group required by the Gondwanan vicariance scenario. The distribution of cichlid fossil horizons, the age of stratigraphically consistent outgroup lineages to cichlids and relaxed-clock analysis of a DNA sequence dataset consisting of 10 nuclear genes all deliver overlapping estimates for crown cichlid origin centred on the Palaeocene (ca 65–57 Ma), substantially post-dating the tectonic fragmentation of Gondwana. Our results provide a revised macroevolutionary time scale for cichlids, imply a role for dispersal in generating the observed geographical distribution of this important model clade and add to a growing debate that questions the dominance of the vicariance paradigm of historical biogeography.     

An overview of fossil Ginkgoales

Neither direct fossil evidence nor consensus exists on the origin of the Ginkgoales and their phylogenetic relationships with other seed plants. The bases for assigning most Palaeozoic leaf fossils to Ginkgoales are shaky. There are eight morphogenera considered more or less well defined and useful for classifying Mesozoic leaf and shoot compressions/impressions, and only two or three morphotaxa of anatomically preserved wood fossils have generally been used. About nine genera of ovulate organs, however, have been reported in the Mesozoic. Whole plant reconstructions suggested for a number of well-preserved ginkgoalean plants are enumerated. Their associated (or connected) organs, and their occurrences and distributions are cited in detail. There are three or four major evolutionary lineages so far recognized among Mesozoic Ginkgoales: the Ginkgo-Grenana-Nehvizdyella lineage, the Karkenia lineage, the Yimaia-Toretzia/Umaltolepis lineage and perhaps the Schmeissneria lineage. Ginkgoales may be classified into five to six families, with a number of accessory morphotaxa and unclassified taxa. The general evolutionary trend among ginkgoaleans is reduction of both vegetative and reproductive organs. The reduction trend is seen clearly in the genus Ginkgo and roughly recapitulated in the developmental sequences of the living species. A similar reduction sequence runs in parallel in other lineages of Ginkgoales. Ginkgoales flourished during Jurassic and Early Cretaceous, but a significant radiation of the group had occurred already in Late Triassic when Ginkgoales were present in high taxonomic diversity and showed considerable morphological innovation. Geographically, Ginkgoales are mainly distributed in Laurasia and probably originated there. The earliest records are from Laurasia as is the relict living fossil. Ginkgoales may have lived in various climates and diverse habitats, although most flourished in mesic and temperate climates, and the Late Cretaceous and Cenozoic ginkgos were largely confined to riparian environments.Advances in micro- and ultrastructure studies and chemical investigations on the cuticle and megaspore membrane of ginkgoalean fossils are also summarized. Further studies in these fields may provide useful information on the ecology and palaeoclimatology of Ginkgoales as well as their taxonomy.     

BOOM AND BUST: ANCIENT AND RECENT DIVERSIFICATION IN BICHIRS (POLYPTERIDAE: ACTINOPTERYGII), A RELICTUAL LINEAGE OF RAY‐FINNED FISHES

Understanding the history that underlies patterns of species richness across the Tree of Life requires an investigation of the mechanisms that not only generate young species‐rich clades, but also those that maintain species‐poor lineages over long stretches of evolutionary time. However, diversification dynamics that underlie ancient species‐poor lineages are often hidden due to a lack of fossil evidence. Using information from the fossil record and time calibrated molecular phylogenies, we investigate the history of lineage diversification in Polypteridae, which is the sister lineage of all other ray‐finned fishes (Actinopterygii). Despite originating at least 390 million years (Myr) ago, molecular timetrees support a Neogene origin for the living polypterid species. Our analyses demonstrate polypterids are exceptionally species depauperate with a stem lineage duration that exceeds 380 million years (Ma) and is significantly longer than the stem lineage durations observed in other ray‐finned fish lineages. Analyses of the fossil record show an early Late Cretaceous (100.5–83.6 Ma) peak in polypterid genus richness, followed by 60 Ma of low richness. The Neogene species radiation and evidence for high‐diversity intervals in the geological past suggest a “boom and bust” pattern of diversification that contrasts with common perceptions of relative evolutionary stasis in so‐called “living fossils.”     

Sero‐taxonomy of skeletal macromolecules in living Terebratulid brachiopods

Antibodies prepared against macromolecules isolated from the shells of three living brachiopod genera have proved to be of considerable taxonomic significance, in that the pattern of cross‐reactivity of all three antisera consistently points to a new interpretation for the evolution of the largest extant brachiopod order, the Terebratulida. This new molecular evidence actually complements rather than contradicts the existing morphology‐based taxonomy, since detailed systematic investigation of the taxa in question has already demonstrated subtle but significant morphological differences in the major taxonomic characters which appear to reflect this new interpretation.

As fragments of skeletal macromolecules, including antigenic determinants, are known to survive for many millions of years within the protected micro‐environments provided by enclosing biominerals, these results suggest that such molecular fossils could well provide important insights on at least the high‐level taxonomic relationships of fossil organisms.     

Bony labyrinth morphology in early neopterygian fishes (Actinopterygii: Neopterygii)

Endocasts of the osseous labyrinth have the potential to yield information about both phylogenetic relationships and ecology. Although bony labyrinth morphology is well documented in many groups of fossil vertebrates, little is known for early Neopterygii, the major fish radiation containing living teleosts, gars and the bowfin. Here, we reconstruct endocasts of the bony labyrinth and associated structures for a sample of Mesozoic neopterygian fishes using high‐resolution computed tomography. Our sample includes taxa unambiguously assigned to either the teleost (Dorsetichthys, “Pholidophorus,” Elopoides) and holostean (“Aspidorynchus,” “Caturus,” Heterolepidotus) total‐groups, as well as examples of less certain phylogenetic position (an unnamed parasemionotid and Dapedium). Our models provide a test of anatomical interpretations for forms where bony labyrinths were reconstructed based on destructive tomography (“Caturus”) or inspection of the lateral wall of the cranial chamber (Dorsetichthys), and deliver the first detailed insights on inner ear morphology in the remaining taxa. With respect to relationships, traits apparent in the bony labyrinth and associated structures broadly support past phylogenetic hypotheses concerning taxa agreed to have reasonably secure systematic placements. Inner ear morphology supports placement of Dapedium with holosteans rather than teleosts, while preserved structure in the unnamed parasemionotid is generalized to the degree that it provides no evidence of close affinity with either of the crown neopterygian lineages. This study provides proof‐of‐concept for the systematic utility of the inner ear in neopterygians that, in combination with similar findings for earlier‐diverging actinopterygian lineages, points to the substantial potential of this anatomical system for addressing the longstanding questions in the relationships of fossil ray‐finned fishes to one another and living groups. J. Morphol. 279:426–440, 2018. © 2016 Wiley Periodicals, Inc.     

Palaeobiology of tanaidaceans (Crustacea: Peracarida) from Cretaceous ambers: extending the scarce fossil record of a diverse peracarid group

Diverse assemblages of tanaidacean peracarid crustaceans from western Tethyan continental deposits suggest that the group was relatively common in or around ancient resin‐producing forests. Here we report the results of an examination of 13 tanaidacean specimens from three Cretaceous (Albian to Turonian) French amber deposits. Two new species of the fossil family Alavatanaidae are placed in the previously described Early Cretaceous genus Eurotanais: Eurotanais pyrenaensis sp. nov. from Cenomanian Pyrenean amber (Fourtou, Aude) and Eurotanais seilacheri sp. nov. from Turonian Vendean amber (La Garnache, Vendée). The remaining specimens are placed in three newly erected genera and species (but family incertae sedis): Arcantitanais turpis gen. et sp. nov. from Albian–Cenomanian Charentese amber (Archingeay, Charente‐Maritime), and Tytthotanais tenvis gen. et sp. nov. and Armadillopsis rara gen. et sp. nov. from Pyrenean amber. These are the first formally described fossils that might be related to the paratanaoidean families Nototanaidae and Paratanaidae, sharing with these some putatively derived features and providing possible evidence for the antiquity and morphological stability of these families and the suborder Tanaidomorpha. The distinctive features and character combinations of these fossil taxa are discussed in connection with possible relationships to the living lineages of tanaidaceans. Propagation phase‐contrast X‐ray synchrotron microtomography was used to obtain high‐quality 3D images for some fossils. A discussion is provided on the putative palaeobiology of tanaidaceans and the French resiniferous forest ecosystem. The discovery of these new tanaidaceans extends the palaeogeographical distribution and stratigraphical range of the family Alavatanaidae and sheds new light on the palaeoecology and diversity of tanaidaceans in pre‐angiospermous woodlands.     

An assessment of species limits of the South American mouse genus Oligoryzomys (Rodentia,Cricetidae) using unilocus delimitation methods

Oligoryzomys, as currently understood is formed by 25 living species, is the most diverse genus of the tribe Oryzomyini of the New World subfamily Sigmodontinae of cricetid rodents. Nonetheless, the species richness of Oligoryzomys seems to be an underestimate, given some species complex has been proposed in previous studies, at the time that large geographic areas remain to be sampled, and several taxonomic forms have not been assessed with contemporary approaches. In this study, we present a new assessment of the species diversity of Oligoryzomys based on multiple unilocus species delimitation methods (ABGD, BPP, PTP, GMYC and b GMYC), using 665 cytb gene sequences as evidence (532 gathered from Genbank and 133 obtained in this study). We sampled representatives of almost all currently known species of Oligoryzomys, at the time that extending the geographic coverage to the Central Andes, a large area that was largely unrepresented in previous studies. Phylogenetic relationships, based on a non‐redundant alignment, were inferred via maximum likelihood and Bayesian inference; an ultrametric tree, used in species delimitation analyses, was obtained using multiple secondary calibration points. Results of species delimitation methods are discussed at the light of previous knowledge (e.g., taxonomic history and geographic provenance of samples in relation to type localities) and the morphological assessments of some specimens. Results of the distinct delimitation methods are mostly congruent, being BPP and PTP the most sensible to estimate species delimitation, allowing us to suggest that Oligoryzomys is composed of 30 lineages of species level. Of these, 22 correspond to forms currently considered species; some of these include in their synonymy some forms currently considered valid species (e.g., yatesi would be a synonym of longicaudatus). The remaining eight lineages are candidate species that need to be further evaluated. This study, by advancing taxonomic hypothesis that should be further tested in future studies, constitutes a stepping‐stone for upcoming taxonomic and biogeographic studies centred on Oligoryzomys.     

Fossil‐based comparative analyses reveal ancient marine ancestry erased by extinction in ray‐finned fishes

The marine‐freshwater boundary is a major biodiversity gradient and few groups have colonised both systems successfully. Fishes have transitioned between habitats repeatedly, diversifying in rivers, lakes and oceans over evolutionary time. However, their history of habitat colonisation and diversification is unclear based on available fossil and phylogenetic data. We estimate ancestral habitats and diversification and transition rates using a large‐scale phylogeny of extant fish taxa and one containing a massive number of extinct species. Extant‐only phylogenetic analyses indicate freshwater ancestry, but inclusion of fossils reveal strong evidence of marine ancestry in lineages now restricted to freshwaters. Diversification and colonisation dynamics vary asymmetrically between habitats, as marine lineages colonise and flourish in rivers more frequently than the reverse. Our study highlights the importance of including fossils in comparative analyses, showing that freshwaters have played a role as refuges for ancient fish lineages, a signal erased by extinction in extant‐only phylogenies.     

A Molecular Genetic Timescale for the Diversification of Autotrophic Stramenopiles (Ochrophyta): Substantive Underestimation of Putative Fossil Ages

Background

Stramenopiles constitute a large and diverse eukaryotic clade that is currently poorly characterized from both phylogenetic and temporal perspectives at deeper taxonomic levels. To better understand this group, and in particular the photosynthetic stramenopiles (Ochrophyta), we analyzed sequence data from 135 taxa representing most major lineages. Our analytical approach utilized several recently developed methods that more realistically model the temporal evolutionary process.

Methodology/Principal Findings

Phylogenetic reconstruction employed a Bayesian joint rate- and pattern-heterogeneity model to reconstruct the evolutionary history of these taxa. Inferred phylogenetic resolution was generally high at all taxonomic levels, sister-class relationships in particular receiving good statistical support. A signal for heterotachy was detected in clustered portions of the tree, although this does not seem to have had a major influence on topological inference. Divergence time estimates, assuming a lognormally-distributed relaxed molecular clock while accommodating topological uncertainty, were broadly congruent over alternative temporal prior distributions. These data suggest that Ochrophyta originated near the Proterozoic-Phanerozoic boundary, diverging from their sister-taxon Oomycota. The evolution of the major ochrophyte lineages appears to have proceeded gradually thereafter, with most lineages coming into existence by ∼200 million years ago.

Conclusions/Significance

The evolutionary timescale of the autotrophic stramenopiles reconstructed here is generally older than previously inferred from molecular clocks. However, this more ancient timescale nevertheless casts serious doubt on the taxonomic validity of putative xanthophyte/phaeophyte fossils from the Proterozoic, which predate by as much as a half billion years or more the age suggested by our molecular genetic data. If these fossils truly represent crown stramenopile lineages, then this would imply that molecular rate evolution in this group proceeds in a fashion that is fundamentally incompatible with the relaxed molecular clock model employed here. A more likely scenario is that there is considerable convergent morphological evolution within Heterokonta, and that these fossils have been taxonomically misdiagnosed.     

Tests of turtle phylogeny: molecular, morphological, and paleontological approaches

We present phylogenetic analyses of both molecular and morphological data for the 23 major lineages of living turtles and seven key fossil taxa. Nearly 1 kilobase of cytochrome b sequence, 325 base pairs of 12S ribosomal DNA, and 115 morphological characters contained similar phylogenetic information, although each provided unique information on different nodes of chelonian history. A character-based combinability test (implemented in PAUP*) and a non-parametric test of taxonomic congruence indicated no strong evidence for heterogeneity among data sets, and we used a combined approach to estimate a final phylogeny of the major lineages of living turtles. This approach resulted in a very well-resolved tree, with only a few of the deep branches within the Cryptodira left as an unresolved polytomy. The addition of six relatively complete fossils chosen to help resolve this basal polytomy provided little added resolution to the tree and resulted in a sharp decline in bootstrap proportions for nodes near the fossils. Branch-length analysis and independent dates from the fossil record suggest that these unresolved nodes may represent a rapid radiation of the major cryptodiran lineages 90-120 million years ago.