Ecdysozoa I: Panarthropoda


Ecdysozoa:

Organisms characterized by the regular shedding of an external cuticle and protostomous development.

Panarthropoda:

This lecture focuses on Panarthropoda, the only ecdysozoans with a good fossil record, Burgess Shale priapulids (right) notwithstanding.

Synapomorphy:


The living panarthropod groups:


Fossil Panarthropoda: The Cambrian Chengjiang, Burgess Shale, and Sirius Passet provide a significant record of stem panarthropods. Alas, their literature tends to lack phylogenetic rigor and to conflate creatures that are superficially similar. One often hears group names that are definitely paraphyletic like: We follow the phylogenetic result of Liu et al., 2011 (See also supplementary information). Simplified at right. Our outgroup and starting point is Priaulida, whose members lack segmentation and limbs, and whose mouth consists of radially symmetrical parts that are protracted by hydrostatic action. As we climb the tree, be aware of:


Mureropodia apae from Diario de un Copepodo

Mureropodia apae (early Cambrian) An infaunal creature believably transitional between priapulids and panarthropods, with five pairs of flexible unspecialized limbs, and a proboscis with a terminal mouth.


Aysheaia pedunculata from Biologia - La Vita e la sua Storia

Aysheaia pedunculata (middle Cambrian) The classic Burgess Shale "lobopodan." Sometimes called an ancestral marine onychophoran, but actually lacking many of their synapomorphies. Aysheaia occupies a basal position in recent analyses because of its lack of robust cuticle and specialized mouthparts. I does show the specialization of the first pair of limbs for something (?) like prey capture or as a sense organ.


Chengjiang "lobopodan" Microdyction sinicum from The Virtual Fossil Museum

Stem onychophorans (Cambrian) Closer to Onychophora. Poorly understood prior to 2000. The first representatives to be studied inlucded Hallucigenia of the Cambrian Burgess Shale, a creature so poorly understood as initially to be misrepresented to the public as a stilt-walking worm. The discovery of less extreme armored forms like Microdyction (right) facilitated proper interpretation.

All appear to have specialized anterior appendages.

Considerable Cambrian diversity, then the record falls silent.


Sirius Passet Kerygmachela kierkegaardi Wikipedia
"Dinocarids" (Cambrian). Paraphyletic. These possessed: Interesting examples include: (Aside: In your instructors' opinions, the alleged Cambrian proto-cephalopod Nectocaris pteryx, (Smith and Caron, 2010) belongs somewhere in this region of the tree.)


Chengjiang Anomalocaris saron from Roberto Verzo
Radiodonta (Cambrian). (The derived "dinocarids." Commonly known as "anomalocarida" or "anomalocaridida," we embrace the phylogenetically defined (Liu et al., 2011) name of this monophyletic group.) The giant (0.5 m) top predators of the Cambrian. Morphologically similar to the swimming lobopodans but: For all of you radiodont needs.


Devonian Schinderhannes bartelsi from Palaeos
Schinderhannes bartelsi: In 2009, a small (10 cm) radiodont-like animal Schinderhannes bartelsi was reported from the Devonian of the Hunsrück lagerstätte. Like radiodonts and "dinocarids," it retained impressive great appendages and a circular toothy mouth. In other respects, it is closer to living arthropods: The "mustache" is a unique feature of Schinderhannes. Is it a proper arthropod? Opinion is divided but it is certainly close.


Ediacaran Parvancorina minchami from Trilobites.info
Records and rumors: Reliably identifiable fossils of panarthropods date no farther back than the early Cambrian. Nevertheless, some researchers claim to recognize them in the zoological Rorhschach-test of the Ediacaran. Putative Ediacaran panarthropods might include: Alas, the preservation of Ediacaran fossils typically precludes the identification of potential structures like jointed limbs on tiny Parvancorina, reducing our attempts to identify their affinities to paleontological pareidolia.

Arthropoda:

(Cambrian - Quaternary) Arthropods ("Euarthropoda" of some authors, used herein to refer to the crown group of Arthropoda) with a proper arthrodized (sclerotized and jointed) cuticle covering the body have a copious fossil record, as even unmineralized cuticle is a "tough tissue," facilitating copious preservation in Konzervatlagerstätten. Some groups - Especially trilobites, mineralize their cuticle in addition. During the last twenty years, their phylogenetic pattern has began to come into focus, as well.


Biramous appendage from Copepods from the Bay of Villefranche
Things to keep in mind:

The living euarthropod groups:


Nephila edulis
Chelicerata: (Cambrian - Quaternary) Including


Narceus sp.
Myriopoda: (Silurian - Quaternary) Including


Blue crab - Callinectes sapidus
Pancrustacea: (Cambrian - Quaternary) Including

Arthropod Phylogeny

Molecular and morphological phylogenies of the last decade (especially the molecular analysis of Regier et al., 2010. have resolved the major patterns of the relationships of the living taxa, and major fossil ones. Among Euarthropoda, the arthropod crown group, two major groups are evident:

The major ongoing controversy concerns Pycnogonida - the "sea-spiders," recovered by some as basal chelicerates and by others as the sister taxon to the remaining euarthropods.

Things become more interesting when the fossil arthropods of the Cambrian Konzervatlagerstätten are considered. During the last three years, however, a picture has begun to emerge. A survey of "major" groups.


Nereocaris exilis from Sciency Thoughts
"Bivalve arthropods" (Cambrian). Not to be confused with bivalved members of Euarthropoda like ostrocods, this is a paraphyletic grade at the base of Arthropoda. Basal arthropods like Nereocaris exilis (right) possessed:



Fuxianhuia protensa from Evrim Haberleri
Fuxianhuiida (Cambrian). Chengjiang forms including Fuxianhuia (right) with distinct segmented body cuticle. Has anterior stalked eyes, six pairs of head appendages, two - three pairs of simple jointed limbs per body segment. The trunk is divided into a head-shield, an anterior limb-bearing thorax, a posterior abdomen, and ends with a pointed telson.

Recently, fuxianhuiids have become the poster children of arthropod phylogeny, with spectacular specimens revealing details of the nervous (Ma et al., 2012) and vascular systems (Ma et al., 2014). These reveal that in Fuxianhuia, these systems resemble those of living arthropods. Specifically, the brain is similar to those of most living crustaceans and insects, and its eyes and antennae are innervated similarly by the first and second sets of brain ganglia respectively.

Additional information


Leanchoillia superlata from Wikipedia
"Megacheira" or "Great-appendage arthropods": A striking array of Cambrian arthropods display large raptorial anterior appendages. Examples include Leanchoillia superlata (right) and Yohoia tenuis from the Burgess Shale. Their great appendages are currently thought to be homologous to the antennae of most arthropods and the chelicerae of chelicerates, but not to the forelimbs of anomalocarids. Their position in arthropod phylogeny is debated:

Interpolating these basal groups, we get this basic phylogeny. Now to explore.

Arachnomorpha:

Contains:



Eldredgeops crassituberculata

Trilobita:

Trilobites. (Cambrian - Permian)

Major features:

  • Culturally, are to the Paleozoic Era and to Invertebrate Paleonology what dinosaurs are to the Mesozoic Era and to Vertebrate Paleontology!

  • Extremely common fossil makers, particularly in the early Paleozoic

  • Range from early Cambrian, when they were major players in the "Cambrian explosion" to the Permo-Triassic Extinction. They experienced their peak diversity in the Ordovician and were sequentially reduced by extinction events at the end of the Ordovician and the Devonian. Only a single clade, Proteida, straggled through the late Paleozoic, only to be snuffed at the end Permian extinction.

  • Exoskeletons were highly calcified, and thus very well preserved in comparison to their relatives, who show up only at sites of exceptional preservation (E.G. Konzervatlagerstätten: Chengjiang, Sirius Passet, Burgess Shale.) These relatives include minor groups such as:

  • Strictly marine.


    Trilobite tagmata from Wikipedia
    Trilobite tagmosis: The trilobite body is divided into three regions: Note: Some trilobites of the early Cambrian (E.G. Olenellus) retain a telson, as well.


    Facial suture patterns from Wikipedia
    Facial sutures: The cephala of most trilobites display facial sutures - lines of weakness at which the cuticle of the cephalon breaks apart when the animal molts. In traditional taxonomy, their geometry has great significance. They are classified based on where the suture terminates posterolaterally with respect to the corner of the cephalon:


    Trilobite body divisions
    Anatomy:


    Trilobite ecology: The diversity of eye morphology and degrees of visual acuity in trilobites prefigures their great range of ecological specializations. While most were benthic deposit feeders, some developed the ability to capture larger prey while others got up into the the water column. To scratch the surface:


    Trilobite attacks prey
  • Very diverse feeding habits, including:


    Olenimorph trilobite
  • Chemosymbiotic forms:

    Some forms, particularly of the clade Olenimorpha, found in deep water black shales seem poorly equipped to feed at all. Indeed, they resemble a trilobite imitating an ediacaran mat-animal, with a great many thoracic segments and very broad pleural lobes. Some speculation maintains that they were chemosymbiotic forms analogous to the pogonophoran worms of recent deep sea hydrothermal environments.


  • Pelagic planktonivores:

    During the Ordovician, several groups gave rise to small nektonic plankton eaters. These are characterized by reduced cuticles, and enlarged eyes and limbs.

  • Plankton themselves: the tiny eyeless agnostids:

    A particularly early and distinctive group, the Cambrian agnostids were, themselves, planktonic, experimenting with the trilobite version of the bivalve morphology found today in planktonic crustaceans. Some suggest that these are not actually trilobites. Owing to their highly derived, arguably paedomorphic, nature and our lack of detailed knowledge of the anatomy of other trilobites at similar developmental stages, this has been difficult to assess. Right now, opinion is divided.


    Trilobite development
    Trilobites being arthropods, we have good growth series for many of them, This enables us to identify agnostids as paedomorphic.

    Trilobite systematics: Here we have a problem. Being well known for close to two centuries and principle index taxa for the early Paleozoic, their complex, traditional Linnean taxonomy is studied by a great many professional biostratigraphers. This includes some groups that are probably paraphyletic (See the Prothero text for a full review.) Consequently, few phylogenetic investigations have been conducted of the relationships within Trilobita. (See review by Lieberman and Karin, 2010.) This is bad because trilobites have been used in the study of evolutionary patterns and processes despite our not really knowing their real evolutionary pattern.

    To date, most rigorous phylogenetic analyses have aimed at:

    We await a full-on cladistic analysis encompassing the full range of trilobite diversity. Indeed, we don't really know which trilobites are the basal group. Two candidates are: Resolutions of such issues will influence our view of the ancestral ecology of trilobites.

    Finally: additional trilobite information.

    Additional reading:

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