Dating the arthropod tree based on large-scale transcriptome data

Molecular sequences do not only allow the reconstruction of phylogenetic relationships among species, but also provide information on the approximate divergence times. Whereas the fossil record dates the origin of most multicellular animal phyla during the Cambrian explosion less than 540 million years ago(mya), molecular clock calculations usually suggest much older dates. Here we used a large multiple sequence alignment derived from Expressed Sequence Tags and genomes comprising 129genes (37,476 amino acid positions) and 117 taxa, including 101 arthropods. We obtained consistent divergence time estimates applying relaxed Bayesian clock models with different priors and multiple calibration points. While the influence of substitution rates, missing data, and model priors were negligible, the clock model had significant effect. A log-normal autocorrelated model was selected on basis of cross-validation. We calculated that arthropods emerged ~600 mya. Onychophorans (velvet worms) and euarthropods split ~590 mya, Pancrustacea and Myriochelata ~560 mya, Myriapoda and Chelicerata ~555 mya, and 'Crustacea' and Hexapoda ~510 mya. Endopterygote insects appeared ~390 mya. These dates are considerably younger than most previous molecular clock estimates and in better agreement with the fossil record. Nevertheless, a Precambrian origin of arthropods and other metazoan phyla is still supported. Our results also demonstrate the applicability of large datasets of random nuclear sequences for approximating the timing of multicellular animal evolution.     

Explosive radiations and the reliability of molecular clocks: island endemic radiations as a test case

The reliability of molecular clocks has been questioned for several key evolutionary radiations on the basis that the clock might run fast in explosive radiations. Molecular date estimates for the radiations of metazoan phyla (the Cambrian explosion) and modern orders of mammals and birds are in many cases twice as old as the palaeontological evidence would suggest. Could some aspect of explosive radiations speed the molecular clock, making molecular date estimates too old? Here we use 19 independent instances of recent explosive radiations of island endemic taxa as a model system for testing the proposed influence of rapid adaptive radiation on the rate of molecular evolution. These radiations are often characterized by many of the potential mechanisms for fast rates in explosive radiations--such as small population size, elevated speciation rate, rapid rate of morphological change, release from previous ecological constraints, and adaptation to new niches--and represent a wide variety of species, islands, and genes. However, we find no evidence of a consistent increase in rates in island taxa compared to their mainland relatives, and therefore find no support for the hypothesis that the molecular clock runs fast in explosive radiations.     

Limitations of Metazoan 18S rRNA Sequence Data: Implications for Reconstructing a Phylogeny of the Animal Kingdom and Inferring the Reality of the Cambrian Explosion

We document the phylogenetic behavior of the 18S rRNA molecule in 67 taxa from 28 metazoan phyla and assess the effects of among-site rate variation on reconstructing phylogenies of the animal kingdom. This empirical assessment was undertaken to clarify further the limits of resolution of the 18S rRNA gene as a phylogenetic marker and to address the question of whether 18S rRNA phylogenies can be used as a source of evidence to infer the reality of a Cambrian explosion. A notable degree of among-site rate variation exists between different regions of the 18S rRNA molecule, as well as within all classes of secondary structure. There is a significant negative correlation between inferred number of nucleotide substitutions and phylogenetic information, as well as with the degree of substitutional saturation within the molecule. Base compositional differences both within and between taxa exist and, in certain lineages, may be associated with long branches and phylogenetic position. Importantly, excluding sites with different degrees of nucleotide substitution significantly influences the topology and degree of resolution of maximum-parsimony phylogenies as well as neighbor-joining phylogenies (corrected and uncorrected for among-site rate variation) reconstructed at the metazoan scale. Together, these data indicate that the 18S rRNA molecule is an unsuitable candidate for reconstructing the evolutionary history of all metazoan phyla, and that the polytomies, i.e., unresolved nodes within 18S rRNA phylogenies, cannot be used as a single or reliable source of evidence to support the hypothesis of a Cambrian explosion. Received: 9 December 1997 / Accepted: 23 March 1998     

The colonization of land by animals: molecular phylogeny and divergence times among arthropods

Background  

The earliest fossil evidence of terrestrial animal activity is from the Ordovician, ~450 million years ago (Ma). However, there are earlier animal fossils, and most molecular clocks suggest a deep origin of animal phyla in the Precambrian, leaving open the possibility that animals colonized land much earlier than the Ordovician. To further investigate the time of colonization of land by animals, we sequenced two nuclear genes, glyceraldehyde-3-phosphate dehydrogenase and enolase, in representative arthropods and conducted phylogenetic and molecular clock analyses of those and other available DNA and protein sequence data. To assess the robustness of animal molecular clocks, we estimated the deuterostome-arthropod divergence using the arthropod fossil record for calibration and tunicate instead of vertebrate sequences to represent Deuterostomia. Nine nuclear and 15 mitochondrial genes were used in phylogenetic analyses and 61 genes were used in molecular clock analyses.     

The influence of body size and net diversification rate on molecular evolution during the radiation of animal phyla

Background  

Molecular clock dates, which place the origin of animal phyla deep in the Precambrian, have been used to reject the hypothesis of a rapid evolutionary radiation of animal phyla supported by the fossil record. One possible explanation of the discrepancy is the potential for fast substitution rates early in the metazoan radiation. However, concerted rate variation, occurring simultaneously in multiple lineages, cannot be detected by "clock tests", and so another way to explore such variation is to look for correlated changes between rates and other biological factors. Here we investigate two possible causes of fast early rates: change in average body size or diversification rate of deep metazoan lineages.     

The origin of animal phyla and the new phylum Procoelomata

BergstrÖm, Jan 1989 07 15: The origin of animal phyla and the new phylum Procoelomata. Lethaia , Vol. 22, pp. 259–269. Oslo. ISSN 0024–1164.
A model of metazoan evolution presented previously (BergstrÖm 1986 in Zoologica Scripta 15 ) explains deuterostomian characters as derived from protostomian ones through loosening of the constraints in the spiralian type of morphogenesis. This fits phylogenies derived from studies of molecular sequences. The model helps explain (1) the well-known mixture of proto- and deuterostomian features in several groups; (2) the difficulties in making a phylogeny based on comparative anatomy, and (3) the fossil explosion in the Cambrian. Since protostomian features such as a ciliated locomotory sole and a pelagic larva with ciliary bands are widely distributed in branches of the phylogenetic tree, they must have been present in the stem of the tree. Most probably the stem forms were pseudosegmented, which helps explain how segmentation, oligomery and non-segmentation could evolve repeatedly in derived groups. Origination of new phyla involved macroevolutionary changes primarily in the mode of feeding and locomotion. The stem phylum, from which most other phyla appear to have been derived directly, is here named the Procoelomata. Machaeridian-type animals are referred to it. The Ediacaran-type Precambrian fossils Cannot be placed in the metazoan evolutionary tree. * Biochemical evolution, Cambrian fossil explosion, Deuterostomia, eukaryote evolution, Machaeridia. macroevolution, Precambrian fossils. Procoelomata, Protostomia .     

Relaxed phylogenetics and dating with confidence

In phylogenetics, the unrooted model of phylogeny and the strict molecular clock model are two extremes of a continuum. Despite their dominance in phylogenetic inference, it is evident that both are biologically unrealistic and that the real evolutionary process lies between these two extremes. Fortunately, intermediate models employing relaxed molecular clocks have been described. These models open the gate to a new field of “relaxed phylogenetics.” Here we introduce a new approach to performing relaxed phylogenetic analysis. We describe how it can be used to estimate phylogenies and divergence times in the face of uncertainty in evolutionary rates and calibration times. Our approach also provides a means for measuring the clocklikeness of datasets and comparing this measure between different genes and phylogenies. We find no significant rate autocorrelation among branches in three large datasets, suggesting that autocorrelated models are not necessarily suitable for these data. In addition, we place these datasets on the continuum of clocklikeness between a strict molecular clock and the alternative unrooted extreme. Finally, we present analyses of 102 bacterial, 106 yeast, 61 plant, 99 metazoan, and 500 primate alignments. From these we conclude that our method is phylogenetically more accurate and precise than the traditional unrooted model while adding the ability to infer a timescale to evolution.     

Defining phyla: evolutionary pathways to metazoan body plans

SUMMARY Phyla are defined by two sets of criteria, one morphological and the other historical. Molecular evidence permits the grouping of animals into clades and suggests that some groups widely recognized as phyla are paraphyletic, while some may be polyphyletic; the phyletic status of crown phyla is tabulated. Four recent evolutionary scenarios for the origins of metazoan phyla and of supraphyletic clades are assessed in the light of a molecular phylogeny: the trochaea hypothesis of Nielsen; the clonal hypothesis of Dewel; the set-aside cell hypothesis of Davidson et al.; and a benthic hypothesis suggested by the fossil record. It is concluded that a benthic radiation of animals could have supplied the ancestral lineages of all but a few phyla, is consistent with molecular evidence, accords well with fossil evidence, and accounts for some of the difficulties in phylogenetic analyses of phyla based on morphological criteria.     

A phylogeny of the Platyhelminthes: towards a total-evidence solution

We advocate a total-evidence approach for the reconstruction of working phylogenies for the Turbellaria and the phylum Platyhelminthes. Few morphology-based character matrices are available in the systematic literature concerning flatworms, and molecular-based phylogenies are rapidly providing the only means by which we can estimate phylogenies cladistically. Character matrices based on gross morphology and ultrastructure are required and should be internally consistent, i.e. character coding should follow a set of a priori guidelines and character duplication and contradiction is avoided. In order to test our molecular phylogenies we need complementary data sets from morphology. To understand morphological homology we need phylogenetic evidence from independent (e.g. molecular) data. Fully complementary morphological and molecular data sets enable us to validate phylogenetic hypotheses and the combination of these sets in phylogenetic reconstruction utilises all statements of homology. Working phylogenies which include all phylogenetic information not only shed light on individual character evolution, but form a strong basis for comparative studies investigating the origin and evolutionary radiation of the taxonomic group under scrutiny. This revised version was published online in July 2006 with corrections to the Cover Date.     

Considerations for Reconstructing Metazoan History: Signal, Resolution, and Hypothesis Testing

SYNOPSIS. Certain issues of metazoan phytogeny remain difficultto resolve even with advances in phylogenetic theory and moleculartools. This lack of resolution might be due to limited phylogeneticsignal in regions of the metazoan tree. For example, 18S rDNAdata are consistent with a rapid radiation early in the historyof bilaterian animals. Despite this lack of resolution, ourunderstanding of metazoan evolutionary history can be furtheredby extracting phylogenetic signal from data with more appropriateevolutionary models and by explicitly testing alternative hypotheses.I examined 18S rDNA data across a diverse number of phyla toidentify potential problems with using genetic data to reconstructmetazoan history. Although the 18S performs well at the mostgeneral level of metazoan phytogeny, it has shortcomings particularlyamong the non-arthropod protostomes. Examples of parametricbootstrap simulation are given to illustrate how we may beginto address methodological issues when there is limited phylogeneticsignal. These simulations suggest that we are more likely tounderstand the bilaterian radiation event by increasing thelength of nucleotide sequences collected than by employing fastergenes.     

The ITS region of groundwater amphipods: length,secondary structure and phylogenetic information content in Crangonyctoids and Niphargids

The phylogenetic analysis of groundwater amphipods is challenging due to the lack of suitable morphological characters. However, molecular phylogenies based on the 18S and 28S nuclear genes of two Crangonyctoidea species endemic to Iceland, Crymostygius thingvallensis and Crangonyx islandicus, support the taxonomy of these species on the basis of morphological characters. Molecular analyses suggest that the genus Crangonyx is paraphyletic, with the species that is found in Eurasia being highly divergent genetically from the species present in North America and Iceland. Studies of the phylogenetic relationships within the genus Niphargus also warrant further work. The nuclear ITS2 region has recently been proposed as a barcoding marker for plants and animals. In addition, ITS2 has been used to build phylogenies at high taxonomic levels by including its secondary structure. In this study, we want to evaluate the applicability of the ITS region for this group of species and describe its characteristics. The taxonomy of C. thingvallensis, as well as the paraphyly of the genus Crangonyx, is supported herein by phylogenies based on the ITS2 variation. The secondary structure and the length of the ITS2 sequences of the Crangonyctoidea and the Niphargidae species studied are highly variable and are characterized by duplications. The ITS2 sequence of Niphargus plateaui is the longest metazoan sequence deposited in the ITS2 database so far. Although saturation was observed in the nucleotide variation of this marker, the addition of the secondary structure information for the reconstruction of the phylogeny did not add support to the phylogenetic trees. The ITS1 region, which is known to be more variable than ITS2 and bears a large duplication within C. islandicus, was found to be less useful for phylogenetic reconstruction.     

Integrin and cadherin clusters: A robust way to organize adhesions for cell mechanics

The evolutionary emergence of animals is one of the most significant episodes in the history of life, but its timing remains poorly constrained. Molecular clocks estimate that animals originated and began diversifying over 100 million years before the first definitive metazoan fossil evidence in the Cambrian. However, closer inspection reveals that clock estimates and the fossil record are less divergent than is often claimed. Modern clock analyses do not predict the presence of the crown‐representatives of most animal phyla in the Neoproterozoic. Furthermore, despite challenges provided by incomplete preservation, a paucity of phylogenetically informative characters, and uncertain expectations of the anatomy of early animals, a number of Neoproterozoic fossils can reasonably be interpreted as metazoans. A considerable discrepancy remains, but much of this can be explained by the limited preservation potential of early metazoans and the difficulties associated with their identification in the fossil record. Critical assessment of both records may permit better resolution of the tempo and mode of early animal evolution.     

When molecules and morphology clash: reconciling conflicting phylogenies of the Metazoa by considering secondary character loss

Molecular and morphological data sets have yielded conflicting phylogenies for the Metazoa. So far, no general explanation for the existence of this conflict has been suggested. However, I believe that a neglected aspect of metazoan cladistics has introduced a systematic and substantial bias into morphological phylogenetic analyses. Most characters used for metazoan cladistics are coded as binary absence/presence characters. For most of these characters, the absence states are assumed to be uninformative default plesiomorphies, if they are defined at all. This character coding strategy could seriously underestimate the number of informative apomorphic absences or secondary character losses. Because nodes in morphological metazoan phylogenies are typically supported by relatively small numbers of characters each with a potentially strong impact on tree topology, failure to distinguish between primary absence and secondary loss of characters before a cladistic analysis may mislead morphological cladistics. This may falsely suggest conflict with molecular phylogenies, which are not sensitive to this bias. To test the existence of this bias, I compare the phylogenetic placement of a variety of metazoan taxa in molecular and morphological trees. In all instances investigated here, phylogenetic conflict can be resolved by allowing for secondary loss of morphological characters, which were assumed to be primitively absent in cladistic analyses. These findings suggest that we should be cautious in interpreting the results of morphological metazoan cladistic analyses and additionally illustrate the value of a more functional approach to comparative morphology in certain circumstances.     

Molecular clocks and evolutionary relationships: Possible distortions due to horizontal gene flow

Summary This paper discusses recent evidence suggesting that genetic information from one species occasionally transfers to another remotely related species. Besides addressing the issue of whether or not the molecular data are consistent with a wide-spread influence of horizontal gene transfer, the paper shows that horizontal gene flow would not necessarily preclude a linear molecular clock or change the rate of molecular evolution (assuming the neutral allele theory). A pervasive influence of horizontal gene transfer is more than just consistent with the data of molecular evolution, it also provides a unique explanation for a number of possibly conflicting phylogenies and contradictory clocks. This phenomenon might explain why some protein clocks are linear while the superoxide dismutase clock is not, how the molecular data on the phylogeny of apes and Australian song birds are not necessarily in conflict with those based on morphology, and, finally, why the mycoplasmas have an accelerated molecular clock.     

Molecular dating in the genomic era

The comparison of DNA and protein sequences of extant species might be informative for reconstructing the chronology of evolutionary events on Earth. A phylogenetic tree inferred from molecular data directly depicts the evolutionary affinities of species and indirectly allows estimating the age of their origin and diversification. Molecular dating is achieved by assuming the molecular clock hypothesis, i.e., that the rate of change of nucleotide and amino acid sequences is on average constant over geological time. If paleontological calibrations are available, then absolute divergence times of species can be estimated. However, three major difficulties potentially hamper molecular dating : (1) a limited sample of genes and organisms, (2) a limited number of fossil references, and (3) pervasive variations of molecular evolutionary rates among genomes and species. To circumvent these problems, different solutions have been recently proposed. Larger data sets are built with more genes and more species sampled through the mining of an increasing number of genomes. Moreover, independent key fossils are identified to calibrate molecular clocks, and the uncertainty on their age is integrated in subsequent analyses. Finally, models of molecular rate variations are constructed, and incorporated in the so-called relaxed molecular clock approaches. As an illustration of these improvements, we mention that the debated age of the animal (bilaterian metazoans) diversification may have occurred between 642-761 million years ago (Mya), roughly 100 Ma before the Cambrian explosion. Among mammals, the initial diversification of major placental groups may have taken place around 100 Mya, well before the Cretaceous/Tertiary boundary marking the extinction of dinosaurs.     

Conflicting phylogenetic signals at the base of the metazoan tree

A phylogenetic framework is essential for under-standing the origin and evolution of metazoan development. Despite a number of recent molecular studies and a rich fossil record of sponges and cnidarians, the evolutionary relationships of the early branching metazoan groups to each other and to a putative outgroup, the choanoflagellates, remain uncertain. This situation may be the result of the limited amount of phylogenetic information found in single genes and the small number of relevant taxa surveyed. To alleviate the effect of these analytical factors in the phylogenetic recons-truction of early branching metazoan lineages, we cloned multiple protein-coding genes from two choanoflagellates and diverse sponges, cnidarians, and a ctenophore. Comparisons of sequences for alpha-tubulin, beta-tubulin, elongation factor 2, HSP90, and HSP70 robustly support the hypothesis that choanoflagellates are closely affiliated with animals. However, analyses of single and concatenated amino acid sequences fail to resolve the relationships either between early branching metazoan groups or between Metazoa and choano-flagellates. We demonstrate that variable rates of evolution among lineages, sensitivity of the analyses to taxon selection, and conflicts in the phylogenetic signal contained in different amino acid sequences obscure the phylogenetic associations among the early branching Metazoa. These factors raise concerns about the ability to resolve the phylogenetic history of animals with molecular sequences. A consensus view of animal evolution may require investigations of genome-scale characters.     

Estimation of primate speciation dates using local molecular clocks

Protein-coding genes of the mitochondrial genomes from 31 mammalian species were analyzed to estimate the speciation dates within primates and also between rats and mice. Three calibration points were used based on paleontological data: one at 20-25 MYA for the hominoid/cercopithecoid divergence, one at 53-57 MYA for the cetacean/artiodactyl divergence, and the third at 110-130 MYA for the metatherian/eutherian divergence. Both the nucleotide and the amino acid sequences were analyzed, producing conflicting results. The global molecular clock was clearly violated for both the nucleotide and the amino acid data. Models of local clocks were implemented using maximum likelihood, allowing different evolutionary rates for some lineages while assuming rate constancy in others. Surprisingly, the highly divergent third codon positions appeared to contain phylogenetic information and produced more sensible estimates of primate divergence dates than did the amino acid sequences. Estimated dates varied considerably depending on the data type, the calibration point, and the substitution model but differed little among the four tree topologies used. We conclude that the calibration derived from the primate fossil record is too recent to be reliable; we also point out a number of problems in date estimation when the molecular clock does not hold. Despite these obstacles, we derived estimates of primate divergence dates that were well supported by the data and were generally consistent with the paleontological record. Estimation of the mouse-rat divergence date, however, was problematic.     

Heterogeneous genomic molecular clocks in primates

Using data from primates, we show that molecular clocks in sites that have been part of a CpG dinucleotide in recent past (CpG sites) and non-CpG sites are of markedly different nature, reflecting differences in their molecular origins. Notably, single nucleotide substitutions at non-CpG sites show clear generation-time dependency, indicating that most of these substitutions occur by errors during DNA replication. On the other hand, substitutions at CpG sites occur relatively constantly over time, as expected from their primary origin due to methylation. Therefore, molecular clocks are heterogeneous even within a genome. Furthermore, we propose that varying frequencies of CpG dinucleotides in different genomic regions may have contributed significantly to conflicting earlier results on rate constancy of mammalian molecular clock. Our conclusion that different regions of genomes follow different molecular clocks should be considered when inferring divergence times using molecular data and in phylogenetic analysis.     

A new dimension in combining data? The use of morphology and phylogenomic data in metazoan systematics

Giribet, G. 2010. A new dimension in combining data? The use of morphology and phylogenomic data in metazoan systematics. —Acta Zoologica (Stockholm) 91 : 11–19 Animal phylogenies have been traditionally inferred by using the character state information derived from the observation of a diverse array of morphological and anatomical features, but the incorporation of molecular data into the toolkit of phylogenetic characters has shifted drastically the way researchers infer phylogenies. A main reason for this is the ease at which molecular data can be obtained, compared to, e.g., traditional histological and microscopical techniques. Researchers now routinely use genomic data for reconstructing relationships among animal phyla (using whole genomes or Expressed Sequence Tags) but the amount of morphological data available to study the same phylogenetic patterns has not grown accordingly. Given the disparity between the amounts of molecular and morphological data, some authors have questioned entire morphological programs. In this review I discuss issues related to the combinability of genomic and morphological data, the informativeness of each set of characters, and conclude with a discussion of how morphology could be made scalable by utilizing new techniques that allow for non‐intrusive examination of large amounts of preserved museum specimens. Morphology should therefore remains a strong field in evolutionary and comparative biology, as it continues to provide information for inferring phylogenetic patterns, is an important complement for the patterns derived from the molecular data, and it is the common nexus that allows studying fossil taxa with large data sets of molecular data.     

Evolution of the Multicellular Animals

SYNOPSIS. Molecular sequence analysis is providing new insightsinto the study of metazoan relationships. The use of ribosomalRNA sequences is revising many of the metazoan phylogenies thathave been established traditionally with anatomical and embryologicaldata. Four new findings that seem to be well supported by moleculardata, both from the authors' laboratories and from others, aredescribed and discussed. First, the arthropods are members ofa deep primary clade within the protostomes and are not thesister taxa of either the annelids or the mollusks. Second,the lophophorate animals are clearly protostomes and are containedwithin a lophotrochozoan superclade including the mollusks,annelids, and many other phyla. Third, the arthropods togetherwith all other molting animals comprise a second monophyleticsuperclade within the protostomes, the ecdysozoa. Fourth, theplatyhelminthes are contained within the lophotrochozoan superclade.