Palaeontological and Molecular Evidence Linking Arthropods, Onychophorans, and other Ecdysozoa
- 1.9k Downloads
Membership of Arthropoda in a clade of molting animals, the Ecdysozoa, has received a growing body of support over the past 10 years from analyses of DNA sequences from many genes together with morphological characters involving the cuticle and its molting. Recent analyses based on broad phylogenomic sampling strengthen the grouping of cycloneuralian worms and arthropods as Ecdysozoa, identify the velvet worms (Phylum Onychophora) as the closest living relatives of arthropods, and interpret segmentation as having separate evolutionary origins in arthropods and annelid worms. Determining whether the water bears (Phylum Tardigrada) are more closely related to onychophorans and arthropods or to unsegmented cycloneuralians such as roundworms (Nematoda) is an open question. Fossil taxa such as the Cambrian anomalocaridids provide a combination of arthropod and cycloneuralian characters that is not observed in any living ecdysozoan. Fossils break up long branches and help to resolve the sequence of character acquisition at several critical nodes in the arthropod tree, notably in a suite of Cambrian lobopodians that may include the stem groups of each of the major panarthropod lineages.
KeywordsCambrian Expressed sequence tags Fossils Lobopodians Phylogenomics
Arthropods—jointed-legged animals including insects, crustaceans, arachnids, centipedes, and millipedes—make up most of the described diversity of life on Earth. As such, the shape of the arthropod tree has a particular importance in that it serves as a crude proxy for the shape of known animal diversity as a whole. Fossil assemblages demonstrate that arthropod megadiversity has been a fact of life since the early Cambrian, a span of 520 million years. For example, in the early Cambrian Chengjiang Lagerstätte of China, the oldest of the diverse “Burgess Shale-type faunas” that provide windows into soft-part preservation and the diversity of unmineralized animals in the main burst of the Cambrian radiation, arthropods make up over 40% of described species and 60% of specimens in collections (Hou et al. 2004a).
Modern understanding of genetics was largely developed from an arthropod, the fly Drosophila. The burgeoning field of evolutionary developmental biology (“evo–devo”) owes as much to Drosophila as did genetics in the era of T. H. Morgan’s “fly room.” Much of what we now know about how animal bodies are patterned at the genetic level was unraveled from Drosophila. In recent years, the genetics of development in other arthropod models have supplemented the picture from flies, and arthropods remain at the forefront of evo–devo. The availability of complete genomes from 12 Drosophila species (Clark et al. 2007—12 Drosophila Genome Consortium) is a measure of how quickly arthropod comparative genomics is accelerating.
This review attempts to seek common ground between approaches to arthropod origins and affinities that are often treated in isolation. I will argue that a phylogenomic approach (evolutionary inference based on DNA sequences from large numbers of genes) offers a compelling solution to the placement of arthropods in the broader context of animal evolution. In most respects, the “molecular tree” for arthropods is readily interpreted in the context of current and classical homology schemes based on comparative anatomy; molecular and morphological estimates of phylogeny are in good agreement. Fossils allow us to increase the density of taxonomic sampling for a subset of characters—morphological characters—and examine the influence of character states recorded in extinct taxa for understanding deep branch points near the origin of arthropods. The conclusion is that genomic, anatomical, and palaeontological evidence converges on a hypothesis in which arthropods and velvet worms are close relatives in an assemblage of molting animals that has a unique evolutionary origin.
Articulata versus Ecdysozoa: Implications for Arthropod Origins
Just 12 years ago, the origin of arthropods was almost invariably presented in the context of their inheriting the segmentation of their body from a shared ancestor with segmented worms, the Annelida (i.e., earthworms, leeches, polychaete worms). Since it was formalized taxonomically by Cuvier in the early nineteenth century, the Articulata hypothesis proposed that segmentation in annelids and arthropods had a single origin. This kind of segmentation is a character complex involving a suite of serially repeated structures along the body axis. These include segmented muscles, body cavities, appendages (if the parapodia of annelids are homologized with the limbs of arthropods), and excretory organs, as well as a ladder-like nerve cord with segmental ganglia and connectives and the addition of new segments from a posterior growth zone (Scholtz 2002, 2003).
Both hypotheses, Articulata and arthropods + cycloneuralians (named Ecdysozoa, as discussed below), resolve the closest relatives of arthropods to be two other animal phyla that share paired, segmental, ventrolateral appendages; these arthropod relatives are the Phylum Onychophora and the Phylum Tardigrada. Onychophora, commonly known as velvet worms, includes around 200 species living in tropical and warm temperate forests (Fig. 1D). They are carnivorous worms with one pair of antennae, a pair of jaws, a pair of slime glands, and a variable number of pairs of unjointed trunk legs called lobopods or onchopods. Tardigrades (Fig. 1E) are known from ca 960 species that inhabit the marine, freshwater and limno-terrestrial realms. Tardigrades are microscopic (mostly less than a half millimeter in length), and share four pairs of trunk legs that have terminal claws. The assemblage of arthropods, onychophorans, and tardigrades is collectively known as Panarthropoda (Nielsen 2001) or Aiolopoda (Hou and Bergström 2006).
When arthropods are resolved as Ecdysozoa, annelids instead group with other phyla that share with them spiral cleavage (a stereotypical arrangement of the initial cell divisions in the embryo) and a distinctive kind of larva called a trochophore (characterized by special arrangements of bands of cilia), such as molluscs and flatworms (Platyhelminthes). Annelids are members of the clade Spiralia or Lophotrochozoa (see Giribet et al. 2009 for a review of the evolutionary history of Spiralia). The Panarthropoda–Cycloneuralia assemblage is the basis for the Ecdysozoa hypothesis (Aguinaldo et al. 1997), originally established using data from the small nuclear ribosomal subunit, 18S rRNA, and corroborated in numerous subsequent analyses using that gene (Giribet 2003). Ecdysozoa (in combination with annelids being spiralians) is similarly the best-supported hypothesis using data from numerous other genes and combinations of molecular data, such as the combined large (28S) and small nuclear ribosomal subunits (Mallatt et al. 2004; Petrov and Vladychenskaya 2005; Mallatt and Giribet 2006), those two genes were analyzed together with an additional 11 nuclear protein-coding genes (Baguñà et al. 2008), or with complete mitochondrial genomes and eight nuclear-protein coding genes (Bourlat et al. 2008). Other kinds of molecular data likewise find that Ecdysozoa is a natural group, as witnessed by analyses using such diverse genetic data sources as myosin heavy chain II (Ruiz-Trillo et al. 2002), Na+/K+-ATPase α-subunit (Kusche et al. 2005), specific sets of microRNAs (Sempere et al. 2007), seven nuclear housekeeping genes (Helmkampf et al. 2008), Hox gene signatures (de Rosa et al. 1999; Balavoine et al. 2002), or a combined analysis of 71 protein-coding genes (Philippe et al. 2005). A complete mitochondrial genome for an onychophoran shows its protein-coding genes to support affinities with priapulids and arthropods (that is, Ecdysozoa), and annelids are nested in a spiralian clade that also includes molluscs, as is usual for molecular data (Podsiadlowksi et al. 2008). The retrieval of Ecdysozoa as a grouping, together with the alliance of annelids with molluscs and other spiral-cleaving animals rather than with arthropods, is a recurring theme of animal phylogenetics.
In addition to its molecular support, the ecdysozoans share a character complex related to the cuticle and the fact that it is molted with growth. Where known, molting in the various ecdysozoan phyla is induced by similar ecdysone hormones, and the ecdysozoan phyla lack cilia used for locomotion. The layering of the cuticle also shows detailed similarities in the different ecdysozoan groups, including differentiated epi-, exo-, and endocuticle, with the former itself being trilaminate (Schmidt-Rhaesa et al. 1998). Ecdysozoans share a unique tissue-specific immunoreactive marker in the neural tissue (Haase et al. 2001).
The morphological debate over Articulata versus Ecdysozoa is viewed by some authorities as a stalemate (Schmidt-Rhaesa 2004, 2007; Jenner and Scholtz 2005)—a block of complex but conflicting characters supports both hypotheses. From available data, molecular evidence is much more clearly decisive in that Ecdysozoa is independently retrieved by many kinds of sequence data (Telford et al. 2008), whereas Articulata—despite the best efforts of Ecdysozoa’s critics (e.g., Wägele and Misof 2001)—is neither retrieved nor is better supported than Ecdysozoa with any kind of molecular data (Giribet 2003).
Quite separate from the (morphological but not molecular) conflict with Articulata, another challenge to Ecdysozoa has come from the Coelomata hypothesis, which posits that arthropods belong to a clade in which the internal organs are housed in a fluid-filled body cavity (a coelom). This coelomate group (wherein arthropods group with coleomate animals such as vertebrates) does not include the nematodes, which are acoelomate, and thus contradicts the Ecdysozoa. The exclusion of nematodes and the resulting failure to retrieve Ecdysozoa is, however, influenced by a systematic bias toward high rates of character loss in the genome of the widely analyzed nematode Caenorhabditis elegans (Copley et al. 2004). Correcting for these losses or for fast-evolving sequences in C. elegans overturns Coelomata in favor of Ecdysozoa (Copley et al. 2004; Dopazo and Dopazo 2005; Irimia et al. 2007). As discussed below, fast-evolving genes can lead to spurious groupings where lineages are grouped based on convergent similarity rather than sharing common ancestry.
The following section describes a new phylogenomic dataset that adds to the body of genetic evidence in favor of arthropods as ecdysozoans and annelids as spiralians. This carries the consequence that the closest relatives of panarthropods are not segmented, coelomate animals like annelids, but rather are nonsegmented, mostly acoelomate worms with terminal mouths.
EST Data and the Relationships of Arthropods
Until recently, trees based on molecular data were derived from analyses of small numbers of genes, the constraint being that DNA sequences were obtained by direct sequencing involving targeted polymerase chain reaction (PCR). One of the objectives of the Assembling the Protostome Tree of Life project, on which I have collaborated with funding from the U.S. National Science Foundation, has been to approach the problem of animal phylogeny using a broader-scale genetic sample, a method that has come to be known as phylogenomics.
Expressed sequence tags or ESTs permit evolutionary relationships to be reconstructed based on short fragments of hundreds or thousands of genes (Philippe and Telford 2006). ESTs are fished out by sequencing random clones derived from a complementary DNA library (complementary DNA is stable and represents only expressed DNA sequences). These strongly expressed fragments allow 150 genes to be identified as equivalent across a sample of 71 multicellular animals (i.e., metazoans) and six non-metazoans (Dunn et al. 2008).
Results discussed herein are derived from the analysis presented by Dunn et al. (2008). In numerous instances, these were the first phylogenomic data for phyla, including for groups like nematomorphs, rotifers (wheel animals), nemerteans (ribbon worms), phoronids, brachiopods (lamp shells), and sipunculans (peanut worms), as well as for major arthropod groups like myriapods and pycnogonids (the latter being the sea spiders). Concerning deep nodes in the Bilateria (animals with left–right body symmetry, like ourselves), ESTs corroborate a picture that had generally been drawn from small numbers of genes, giving support for a basic split of the bilaterians into two groups, Protostomia and Deuterostomia. These taxonomic names date back to the nineteenth century, when zoologists recognized that the adult mouth of animals could originate from different openings in embryos, either from the blastopore, the original opening of the embryonic gut (a condition known as protostomy, giving rise to the name Protostomia) or else the mouth could form as a new opening, with the blastopore instead usually becoming the anus (deuterostomy). Arthropods are protostomes, we are deuterostomes. The protostomes themselves divide into two natural groups, spiralians and ecdysozoans. Annelids fall within the Spiralia (closest to the brachiopods, phoronids, and nemerteans) and arthropods within the Ecdysozoa.
The closest relative or sister group of Arthropoda is clearly resolved from the EST data—Onychophora, rather than Tardigrada, is most closely related to arthropods (a result also retrieved by Roeding et al. 2007 using ESTs from a different onychophoran species). Indeed, the only relationship in the Ecdysozoa that is sensitive to the choice of evolutionary model and taxon sampling (i.e., the species included in the analysis) is the position of tardigrades. For the full (77 species) taxon sample, tardigrades fall inside the Cycloneuralia, closest to the nematodes and nematomorphs (Fig. 2A), as in the traditional “aschelminth” interpretation of tardigrades (see Giribet 2003; the now-abandoned grouping Aschelminthes as found in older textbooks includes the Cycloneuralia), rather than grouping with the panarthropods. Other EST analyses that sampled fewer species similarly found tardigrade—nematode and onychophoran—arthropod clades (Roeding et al. 2007).
The position of tardigrades is observed to be influenced by the position of several groups that are unstable with respect to their position on the tree. Dunn et al. (2008) quantified how labile taxa were by using a leaf-stability metric (sensu Thorley and Wilkinson 1999), finding that the most unstable branches were concentrated in one region of the tree, the so-called Platyzoa. Platyzoa is an assemblage of mostly minor phyla that group together with the true flatworms, platyhelminths; within Spiralia and Ecdysozoa, leaf stability values were higher. Reanalysis of the data with just the 64 most stable lineages included explored the effect of unstable taxa, finding that few relationships were disrupted across the tree. The only change within the Ecdysozoa when comparing the full 77-species analysis and the pruned (64-species) analysis was the placement of tardigrades. The reduced taxonomic sampling found tardigrades to group as sister to onychophorans and arthropods (Fig. 2B), conforming to the Panarthropoda (Nielsen 2001) or Aiolopoda (Hou and Bergström 2006) hypothesis. This tree thus favors a single origin for paired, segmental, ventrolateral appendages as shared by the three panarthropod/aiolopodan phyla.
In summary, EST data validate Ecdysozoa and group the annelid worms with other phyla sharing spiral cleavage (and thus reject the Articulata). They are equivocal on the question of whether tardigrades are panarthropods—as had generally been endorsed by arthropod phylogeneticists since the mid-1990s (e.g., Dewell and Dewell 1997; Budd 2001; Nielsen 2001)—or are nested within the other main clade of ecdysozoans, the Cycloneuralia. In effect, this mirrors a longstanding controversy over the affinities of tardigrades, which have been observed to possess a mélange of arthropod and cycloneuralian characters. Arthropod-like features of tardigrades include the paired ventrolateral appendages, cross-striated muscles that attach at inpocketings of the cuticle, and similar sensory structures. On the other hand, cycloneuralian-like characters seen in tardigrades include a telescopic mouth cone and rows of platelets called placoids in the pharynx bulb (Giribet 2003; Kristensen 2003). The latest assessment of brain anatomy in tardigrades likewise constrains their systematic position to either sister group of Onychophora + Arthropoda, as in Fig. 2B, or closer to Cycloneuralia (Zantke et al. 2008), as in Fig. 2A. The tardigrade brain is arranged as an unsegmented ring around the esophagus, rather like the condition that gives Cycloneuralia its name. The position of tardigrades in the Ecdysozoa is an open question.
Ecdysozoa and Palaeontology
Under the Articulata framework, the origin of arthropods was seen in the context of onychophorans and arthropods (and, variably, tardigrades) sharing segmentation via common ancestry with Annelida. Some recent advocates of Articulata have drawn on palaeontology as a supporting argument in favor of Articulata as a natural group, citing “annelid–arthropod intermediates” from the fossil record (Wägele and Misof 2001), with the counter-claim that no fossil data are consistent with cycloneuralians being allied to lobopodian panarthropods.
I shall leave the first claim (taking it as given that a century or more of palaeontologists interpreted their data in the context of what was then the standard zoological framework, i.e., Articulata as a natural group), and challenge the second claim. Even before the concept of Ecdysozoa had taken hold in the molecular systematics literature, palaeontologists had recognized that anomalocaridids—a Cambrian group that includes the largest predators in Cambrian ecosystems (Whittington and Briggs 1985; Chen et al. 1994)—in particular possessed a suite of characters shared with either cycloneuralians and tardigrades or with tardigrades and arthropods (Hou et al. 1995). These features include circumoral sclerites/a radial mouth apparatus, segmentation, and paired appendages. Initially, this overlapping suite of characters was interpreted in the context of affinities of anomalocaridids to either cycloneuralians or to arthropods (i.e., assuming that one of the sets of similarities was convergent). Like Hou et al. (1995), Waggoner (1996) identified similarities in the mouth cone, circumoral ring, and pharynx armature of anomalocaridids and cycloneuralians, but in contrast, he considered all of these taxa to be allied to the Arthropoda and their similarities being potentially homologous. A resolution in which Cambrian lobopodian worms and anomalocaridids are a grade in the arthropod stem group (Budd 1996, 1997, 1999, 2001; Dewell et al. 1999; Zhang and Briggs 2007; Fig. 3) similarly accommodates Cycloneuralia as sister group to the Panarthropoda (Budd 2003), as is generally upheld for Ecdysozoa (Fig. 2B). Character combinations in Cambrian fossils, like a terminal mouth with a mouth cone in an animal with segmentally arranged lobopodial limbs and annulation of the cuticle but without complete segment-defining rings (Kerygmachela; see Budd 1999, Fig. 28 for the mouth cone), are comprehensible in an Ecdysozoa framework (Dewell et al. 1999). Numerous subsequent palaeontological studies have cast arthropod origins in terms of a panarthropod–cycloneuralian sister group relationship (e.g., Bergström and Hou 2003; Dzik 2003; Hou and Bergström 2006; Almeida et al. 2008; Liu et al. 2008). Perhaps the most compelling evidence in favor of Ecdysozoa from palaeontology is provided by the mélange of priapulid-like, onychophoran-like and arthropod-like characters in the Cambrian lobopodians, which are singled out for discussion below.
In light of the Ecdysozoa hypothesis and the sister group relationship of Onychophora and Arthropoda that is clearly supported by EST data (Roeding et al. 2007; Dunn et al. 2008), we can reexamine segmentation characters previously upheld as supporting arguments in defence of Articulata as a natural group. Although the homology of segmentation in annelids and arthropods was questioned from the establishment of Ecdysozoa, it has generally been accepted that the arthropod segmentation character set was present in the common ancestor of all panarthropods. This situation needs to be revised in light of new findings. We now recognize that a “rope-ladder” ventral nerve cord with segmental commissures joining the ganglia (masses of neural tissue that are arranged one pair per segment in arthropods) is a derived character of arthropods alone (Mayer and Harzsch 2007, 2008). Onychophorans have a decoupling of their commissures and segmental leg nerves (Mayer and Harzsch 2007, 2008). Tardigrades have four pairs of ganglia in the nerve cord (i.e., strictly segmental ganglia, lined up with the four leg-bearing segments), but the most recent study of their nervous system suggests that these ganglia lack commissures (Zantke et al. 2008). Likewise, the limb musculature of tardigrades is not precisely segmental, with each leg having a different compliment of muscles (Schmidt-Rhaesa and Kulessa 2007). These results from onychophorans and tardigrades further weaken the Articulata concept because its advocates have to account for similarities in arthropods and annelids that are not distributed across the entire Panarthropoda or the onychophoran–arthropod clade. Indeed, whether a rope-ladder nerve cord is even a basic character of Annelida itself is itself questionable, owing to the diversity of nervous system arrangements in different annelid groups that make it unclear whether or not the common ancestor of all annelids had this kind of highly organized nerve cord (Müller 2006). Other purported segmentation characters of Annelida and Arthropoda have likewise been critiqued and rejected in recent studies. For example, Mayer (2006) documented fundamental differences in how the excretory organs (nephridia) develop between onychophorans and annelids that weaken a character, “segmentally arranged metanephridia,” that had traditionally been cited as a defining character of Articulata.
Just as powerful is the observation that the genetic basis of segmentation in some kinds of annelids differs more from arthropods than was known when earlier studies cited similarities in segmentation genes as an argument in defense of Articulata (Scholtz 2002, 2003). Expression of the segmentation genes engrailed, wingless, and hedgehog in the polychaete annelids Capitella and Hydroides shows patterns dissimilar to the highly conserved segment polarity patterns seen in arthropods, weakening the case for the segmentation process having a common origin in the two groups (Seaver and Kaneshige 2006).
Cambrian Lobopodians: Can They Root the Arthropod Tree?
Something that is not widely appreciated is that most of the major competing hypotheses for the deepest nodes of the arthropod tree represent a debate over where we place the root of the tree (Giribet et al. 2005, Fig. 1; see Gregory 2008 for an introduction to evolutionary trees). Several currently debated hypotheses—notably the position of the sea spiders (pycnogonids) and the debate over whether myriapods group with other jawed arthropods (Mandibulata) or with chelicerates (Paradoxopoda)—in fact agree as far as the branching arrangement of major arthropod groups goes, but they differ in where the root of the tree is found. The root is the branch at the base of a tree, the lineage that connects a group to its closest relatives in another group, in this case, the connection between the common ancestor all arthropods and the next most closely allied group, the onychophorans. Here, we could look to fossils as an additional source of data for tackling this kind of rooting question, not the least because fossils may include branches that diverged before the features of crown groups had evolved (i.e., early fossils may include members of the onychophoran and arthropod stem groups; see Fig. 3 for an example of how the latter are depicted on a tree).
Among the Cambrian lobopodians, the most compelling candidates for stem-group arthropods are emerging from recent work on lobopodians from the early Cambrian (520 million years old) of China, specifically from animals named Jianshanopodia (Liu et al. 2006b) and Megadictyon (Liu et al. 2007). The importance of these new lobopodians derives from characters shared with other Cambrian panarthropods that have been allied to anomalocaridids or otherwise placed in the arthropod stem group.
The gut morphology of the new Chinese lobopodians is strikingly similar to stem group arthropods and fossil crown group arthropods. The kind of segmentally repeated midgut glands documented by Butterfield (2002) and García-Bellido and Collins (2007) in Leanchoilia (Fig. 5C) and other arthropods is shared by Kerygmachela (Fig. 5A: “mg”), Pambdelurion (Budd 1997, Fig. 11.9), and the lobopodians Jianshanopodia (Liu et al. 2006b, Fig. 3B2, C1, C2) and Megadicyton (Liu et al. 2007, Fig. 2L, M). The detailed structure of these glands—with an internal structure of lamellae on a submillimetric scale, as depicted by Butterfield (2002, Fig. 4) in thin section—provides a good indication of their homology, and they can thus be considered to indicate arthropod affinities for a lobopodian (character A in Fig. 3).
An example of how fossils can be placed on the stem lineage of a major panarthropod group comes from an unexpected source, the nervous system. Uniquely among the Cambrian fossil panarthropods, the ventral nerve cord has been documented in some specimens of the Cambrian lobopodian Paucipodia (Fig. 4A) by Hou et al. (2004b). Paired pigment patches at regular spacing along the presumed nerve cord are interpreted as ganglia. Their regular spacing with respect to the appendages (the lobopods) compares more closely to the strictly segmental ganglia of arthropods than to the unganglionated nerve cord of onychophorans (Mayer and Harzsch 2007, 2008). If this interpretation of the fossils is correct, and if onychophorans record a stage in which segmentation of the nerve cord is evolving (rather than being secondarily reduced), Paucipodia is resolved above Onychophora on the arthropod stem lineage, despite its decidedly lobopodian trunk construction.
The three-dimensionally preserved Orstenotubulus (Maas et al. 2007) provides another example of how fossil lobopodians can illuminate the origin of panarthropod characters. Fossils are extracted by acid preparation and can be examined without the confounding effects of compaction. The cuticle of Orstenotubulus evamuellerae is like that of onychophorans in being annulated with a hexagonal surface microtexture, and the legs bear presumed sensory structures that are similar in detail to the dermal papillae of extant Onychophora (Maas et al. 2007). Other characters are more broadly shared with several Cambrian lobopodians, such as paired spines serially arranged along the body axis on conical humps or domes (Fig. 4B). A mid-ventral slit-like opening at the posterior end of the fossil makes an interpretation as the genital opening (gonopore) probable, and it is unpaired like that of onychophorans.
The Cambrian lobopodians may also contribute to broader questions of the panarthropod stem group. The early Cambrian worm Facivermis has been described as showing features consistent with the transition from priapulid-style burrowing and lobopodian-style creeping on the seafloor (Liu et al. 2006a, 2008). Structures previously misinterpreted as tentacles are actually five pairs of lobopodial appendages, behind which the body is divided into a slender region devoid of appendages and a pyriform posterior region that bears circlets of hooks. The notion that some of the Cambrian lobopodians are, rather coarsely put, “priapulids with legs,” predates the Ecdysozoa hypothesis (Dzik and Krumbiegel 1989) and may prove to be an additional argument in defence of Ecdysozoa.
Character Evolution in the Arthropod Stem Group: An Example
Lobopodians such as Jianshanopodia and Megadictyon, discussed in the preceding section, are fossils positioned in the lower part of the arthropod stem group (see Fig. 3). Compelling candidates also represent the upper part of the stem group, more closely related to extant arthropods. The systematic position of Fuxianhuiida, an early Cambrian group from China, in the arthropod stem group has received broad consensus (Chen et al. 1995; Hou and Bergström 1997; Budd 2002, 2008; Bergström and Hou 1998, 2005; Waloszek et al. 2005, 2007), despite varying interpretations of head structures. The following discussion focuses on how these fossils inform on the sequence of character acquisition in the arthropod head and trunk limbs.
The trunk appendages of fuxianhuiids (Fig. 6C) likewise add insights into the arthropod stem-lineage, and I adopt the morphological interpretation shared by Bergström and Hou (1998, 2005) and Waloszek et al. (2005). The trunk limbs have two branches, as in many Palaeozoic arthropods (such as trilobites, to cite the most familiar example), but the outer branch is a simple rounded flap that lacks strong setae. The limb stem is composed of many (ca 20) short articles without clear differentiation of a basal unit or protopodite. However, pivot joints are formed between the articles as in other arthropods, and this construction of the trunk limbs can be regarded as an evolutionary novelty shared by fuxianhuiids and crown-group arthropods.
Identifying fossils like the fuxianhuiids as stem group arthropods serves to break up the branch between the arthropod crown group and extant outgroups such as Onychophora or even lower stem group arthropods such as Cambrian lobopodians and anomalocaridids (Fig. 3), and illuminates the sequence of character acquisition at the base of the Arthropoda. We can infer, for example, that jointed appendages, an outer limb branch (an exite), a stiffened tergal exoskeleton, compound eyes, and a hypostome are characters that evolved before the crown group node for the Arthropoda (jointed appendages and compound eyes probably evolved earlier than the fuxianhuiids, as evidenced by their presence in anomalocaridids: Fig. 5B). Fuxianhuia and the arthropod crown group are separated by fossil taxa like Leanchoilia, which have flattened limb bases with spiny inner margins (character F in Fig. 3) and a fringe of strong setae on the outer margins of the exites (Fig. 5C) as also seen in living marine arthropods. The arthropod crown group (indicated by character G in Fig. 3) shares certain features not present in the stem group fossils, notably a reduced number of articles in the inner limb branch (only five to seven articles excluding the terminal claw versus eight in Leanchoilia) and more rod-like rather than flap-like outer limb branches. The fossils that sample the arthropod stem group thus demonstrate that “typical” arthropod characters (features shared by all crown group arthropods but not by extant onychophorans) did not evolve in a single burst of evolutionary innovation but rather in a stepwise manner. Fossils can offer unique insights by exposing the sequence of character acquisition in ancient evolutionary radiations.
In Support of Total Evidence
This review has deliberately adopted a pro-molecules, pro-morphology, and pro-fossils tone. Denigrating or dismissing molecular data because we sometimes retrieve anomalous groupings from single genes is futile; molecular systematics is here to stay, and phylogeny reconstruction is certainly a more vibrant field thanks to the availability of its enormous character sample. Likewise, dismissing the value of morphology in phylogenetics is misguided; explaining morphology remains the reason that most biologists conduct phylogenetic analyses in the first place, and morphology offers character data of unrivalled complexity as well as the only opportunity to infer relationships for the overwhelming majority of taxa (i.e., extinct diversity) that can be known only as fossils. As for fossils, I adopt the stance that they may not be necessary to retrieve the optimal cladogram for extant diversity within a group, but failure to test whether a tree constructed solely on the basis of still-living species is robust to the inclusion of extinct diversity is ill-advised (Cobbett et al. 2007), and fossils can inform on the sequence of character evolution (Fig. 3 for the arthropods) even when they do not alter the shape of the tree itself. The “arthropods as ecdysozoans” hypothesis has so much explanatory power because it simultaneously accommodates evidence from diverse data sources.
EST studies were funded by two consecutive collaborative grants from the Assembling the Tree of Life (AToL) program of the U.S. National Science Foundation. I thank my collaborators on the Protostome AToL project (Casey Dunn, Gonzalo Giribet, Andreas Hejnol, Mark Martindale, Reinhardt Kristensen, Greg Rouse, Elaine Seaver, Martin Sørensen, and Katrine Worsaae) for stimulating discussion of animal morphology. Discussion with Graham Budd and Alison Daley greatly aided the interpretation of stem group arthropods. For providing images used in the figures, I thank Graham Budd, Diego García-Bellido, Gonzalo Giribet, Reinhardt Kristensen, Lars Ramsköld, Andreas Schmidt-Rhaesa, and Martin Sørensen.
- Almeida WO, Christoffersen ML, Amorim DS, Eloy ECC. Morphological support for the phylogenetic positioning of Pentastomida and related fossils. Biotemas 2008;21:81–90.Google Scholar
- Balavoine G, de Rosa R, Adouette A. Hox clusters and bilaterian phylogeny. Mol Phylogenet Evol. 2002;24:266–373.Google Scholar
- Bergström J, Hou X. Chengjiang arthropods and their bearing on early arthropod evolution. In: Edgecombe GD, editor. Arthropod fossils and phylogeny. New York: Columbia University Press; 1998. p. 151–84.Google Scholar
- Bergström J, Hou X. Arthropod origins. Bulletin of Geosciences, Czech Geological Survey. 2003;78:323–34.Google Scholar
- Bergström J, Hou X. Early Palaeozoic non-lamellipedian arthropods. In: Koenemann S, Jenner R, editors. Crustacea and arthropod relationships. Crustac. Issues 2005;16:73–93.Google Scholar
- Budd GE. Stem group arthropods from the Lower Cambrian Sirius Passet fauna of North Greenland. In: Fortey RA, Thomas RH, editors. Arthropod relationships. London: Chapman & Hall; 1997. p. 125–38.Google Scholar
- Budd GE. Arthropods as ecdysozoans: the fossil evidence. In: Legakis A, Sfenthourakis S, Polymeni R, Thessalou-Legaki M, editors. The new panorama of animal evolution. Proceedings of the 18th International Congress of Zoology. Sofia, Moscow: Pensoft; 2003. p. 479–87.Google Scholar
- Dewell RA, Dewell WC. The place of tardigrades in arthropod evolution. In: Fortey RA, Thomas RH, editors. Arthropod relationships. London: Chapman & Hall; 1997. p. 109–23.Google Scholar
- Dewell RA, Budd GE, Castano DF, Dewell WC. The organization of the subesophageal nervous system in tardigrades: insights into the evolution of the arthropod hypostome and tritocerebrum. Zool Anz. 1999;238:191–203.Google Scholar
- Giribet G, Richter S, Edgecombe GD, Wheeler WC. The position of crustaceans within Arthropoda—evidence from nine molecular loci and morphology. In: Koenemann S, Jenner R, editors. Crustacea and arthropod relationships. Crustac. Issues 2005;16:307–52.Google Scholar
- Giribet G, Dunn CW, Edgecombe GD, Hejnol A, Martindale MQ, Rouse GW. Assembling the spiralian Tree of Life. In: Telford MJ, Littlewood DTJ, editors. The evolution of animals. Oxford: Oxford University Press; 2009.Google Scholar
- Gregory TR. Understanding evolutionary trees. Evolution: Education and Outreach. 2008;1:121–37.Google Scholar
- Hou X, Bergström J. Arthropods of the Lower Cambrian Chengjiang fauna, southwest China. Fossils & Strata. 1997;45:1–116.Google Scholar
- Hou X, Bergström J. Dinocarids—anomalous arthropods or arthropod-like worms. In: Rong J, Fang Z, Zhou Z, Zhan R, Wang X, Yuan X, editors. Originations, radiations and biodiversity changes- Evidences from the Chinese fossil record. Beijing: Science; 2006. p. 139–58, 847–50.Google Scholar
- Hou X, Bergström J, Ahlberg P. Anomalocaris and other large animals in the Lower Cambrian Chengjiang fauna of southwest China. Geologiska Föreningens i Stockholm Förhandlingar. 1995;117:163–83.Google Scholar
- Hou X, Aldridge RJ, Bergström J, Siveter DJ, Siveter DJ, Feng XH. The Cambrian fossils of Chengjiang, China: the flowering of early animal life. Oxford: Blackwell; 2004a.Google Scholar
- Jenner RA, Scholtz G. Playing another round of metazoan phylogenetics: historical epistemology, sensitivity analysis, and the position of Arthropoda within the Metazoa on the basis of morphology. In: Koenemann S, Jenner R, editors. Crustacea and arthropod relationships. Crustac Issues. 2005;16:355–85.Google Scholar
- Kristensen RM. Comparative morphology: do the ultrastructural investigations of Loricifera and Tardigrada support the clade Ecdysozoa? In: Legakis A, Sfenthourakis S, Polymeni R, Thessalou-Legaki M, editors. The new panorama of animal evolution. Proceedings of the 18th International Congress of Zoology. Sofia, Moscow: Pensoft; 2003. p. 467–77, 2003.Google Scholar
- Liu J, Shu D, Han J, Zhang Z, Zhang X. A large xenusiid lobopod with complex appendages from the Lower Cambrian Chengjiang Lagerstätte. Acta Palaeontol Pol. 2006b;51:215–22.Google Scholar
- Nielsen C. Animal evolution, interrelationships of the living phyla. 2nd ed. Oxford: Oxford University Press; 2001.Google Scholar
- Ramsköld L, Chen J. Cambrian lobopodians: morphology and phylogeny. In: Edgecombe GD, editor. Arthropod fossils and phylogeny. New York: Columbia University Press; 1998. p. 107–50.Google Scholar
- Schmidt-Rhaesa A. Ecdysozoa versus Articulata. Sitzungsberichte der Gesellschaft Naturforschender Freunde zu Berlin. 2004;43:35–49.Google Scholar
- Scholtz G. Is the taxon Articulata obsolete? Arguments in favour of a close relationship between annelids and arthropods. In: Legakis A, Sfenthourakis S, Polymeni R, Thessalou-Legaki M, editors. The new panorama of animal evolution. Proceedings of the 18th International Congress of Zoology. Sofia, Moscow: Pensoft; 2003. p. 489–501, 2003.Google Scholar