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

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

Work of the last forty years has shown that arthropods belong to a larger group of related organisms -Panarthropoda, which also includes many creatures of the Early - Middle Cambrian lagerstätten (Burgess shale, Chengjiang, and Sirius Passet.) These include:

  • Lobopoda (Cambrian - Rec.) including the living Onychophora and recognizibly similar fossil forms like Aysheaia (see also right) and, following the discovery of armored forms from Chengjiang, the bizarre Hallucigenia. In all cases, the body is soft but the limbs have thickened cuticle and are incipiently jointed.


  • Aysheaia from the Burgess Shale.

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  • Tardigrada (Cambrian - Recent). AKA "water-bears." Cute. Miniaturized lobopodans of damp and aquatic habitats. Feed on plant cells. Only fossils known are from Middle cambrian Orsten lagerstätte,


  • A tardigrade.

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  • "Swimming lobopodans" (Cambrian). Paraphyletic. These possessed joined appendages paired with soft swimming appendages in a arrangement reminiscent of proper arthropod biramous appendages. Adding color to this similarity is the fact that in some taxa, these swimming appendages also seem to be house gas-exchange organs. A famous example is the five-eyed Opabinia regalis.


  • Kerygmachela kierkegaardi from Sirius Passet.

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  • Anomalocarida (Cambrian - Devonian). The giant (0.5 m) predators of the Cambrian. Morphologically like the swimming lobopodans but without the walking limbs. All possess one pair of anterior feeding appendages and circular toothy mouths. For more anomalocarid information.

    But cool! In 2009, an anomalocarid was reported from the Devonian of the Hunsrück lagerstätte.


  • Anomalocaris saron from Chengjiang.

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  • Fuxianhuia (Cambrian). Chengjiang form with distinct segmented body cuticle. Has anterior stalked eyes, six pairs of antennae, two - three pairs of simple jointed limbs per body segment. The trunk is divided into an anterior limb-bearing thorax, a posterior abdomen, and ends with a pointed telson.


  • Fuxianhuia portentosa from Chengjiang.

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    Crown Group Arthropoda

    Arthropodan synapomorphies:

  • Cuticular skeleton of most panarthropods was not calcified, so only preserved in rare cases (e.g., Burgess Shale)
  • Some forms ("armored lobopodans") did have calcified plates and spikes; may be represented in Small Shelly Fauna, Early Cambrian.

    Arthropoda (crown group) is united by the following synapmorphies:
    • Jointed appendages
      • In primitive forms most limbs are similar, but in most various limbs are highly specialized
      • Ancestrally limbs seem to be biramous: one branch for locomotion, the other (dorsal) branch being a gill
      • Various derived forms lose either the dorsal or ventral ramus to become uniramous
    • Complete body segmentation
      • Body of primitive forms is homonomous (all body segments are very similar), but in vast majority there is some degree of tagmosis (AKA "tagmatization". Specialization and fusion of body segments and their associated limbs.)
      • Compound eyes


    Marella splendens of Burgess Shale.

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    Internally

  • Nitrogenous waste eliminated by malphigian tubules
  • Heart with pericardium and ostia (sing. ostium). Open circulatory system with large haemocoel (coelomic cavity specialized for the transmission of circulatory fluid).
  • Highly cephalized


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    Arthropod phylogeny at a glance: We have reviewed creatures on the arthropod stem. Crown group Arthropoda breaks down into two groups:

    Primarily based on Regier et al., 2010.

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    Arachnomorpha:

    Contains:

    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 early and mid-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 substantially reduced by extinction events at the end of the Ordovician and the Devonian. By the Permian, they were marginal.

  • 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:
    • Naraoida: Similar to trilobites without calcification or segmentation of thorax
    • Tegopeltida: Similar to trilobites without distinct cephalon

  • Strictly marine.

  • From The Virtual Fossil Museum

  • Body divided into three lobes, two different ways:


  • Very diverse feeding habits, including:

  • 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.

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

    Finally: additional trilobite information.

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    Trilobites and chelicerates are united in the monophyletic group Arachnomorpha: Synapomorphies are subtle, including the loss of the first antenna (recall that crustaceans have two pairs, trilobites only one and chelicerates none). Indeed, a comparison of very early trilobites and chelicerates shows their similarity to their last common ancestor.


    Olenellus a trilobite
    From www.trilobites.info

    Cyamocephalus a chelicerate
    From Palaeos

    Note, for example the post-anal telson (spine), a feature soon lost in trilobites but retained and elaborated in chelicerates.

    Cheliceramorpha

    Characteristic body segmentation:

    E.G. the eurypterid Eurypterus lacustris (right)


    Tagmosis:
    • NO antennae
    • Chelicerae: shred food and transfer to mouth
    • Pedipalps: Second par of limbs often specialized for various functions include seizing prey, walking, and copulation
    • Four pairs of walking legs
    Breath by book gills - specialized psoterior biramous appendages. (book lungs in the terrestrial arachnids, and even trachaea in some specialized small-bodied arachnids) See xiphosuran Limulus polyphemus (right)

    An early representative: Sanctacaris of the Burgess shale. With six major prosomal limbs and numerous minor limbs of the opistosoma.


    Several major groups:

  • An early representative: Sanctacaris of the Burgess shale. With six major prosomal limbs and numerous minor limbs of the opistosoma.


  • Pycnogonida (sea spiders) (Dev. - Rec.)
    • Have chelicerae, but pedipalps ambiguous. Males have specialized limbs behind chelicerae called ovigers for grooming and transporting fertilized egg mass that may be homologous.
    • Very sparse fossil record


  • Xiphosura (horseshoe crabs) (Sil. - Rec.)

    • Aquatic (most marine, but a few fossil brackish and freshwater forms), but can come onto land for short periods of time
    • Fossil record from Silurian onward
    • Early forms and larvae of modern forms are VERY similar to the earliest trilobites.
      Tagmosis:
      • Chelicerae
      • Five pairs of walking legs - i.e. pedipalps not differentiated.


  • Eurypterida (sea scorpions) (Ord. - Per.)
    • Ordovician through Middle Permian, but heyday is Silurian and Devonian
    • Predatory: Either chelicerae, pedipalps, or first walking legs could be developed as powerful claws
    • Anteriormost six segments of opisthosoma typically very broad: form mesosoma - Derived book gills enclosed in gill chambers superficially resembling sternites. These chambers have, on their roof, vascularized gill tracts that apparantly functioned to retain water when the creature was on land.
    • Opisthosoma flexible dorsoventrally, with tergites (half-bands) of cuticle above and sternitesbelow
    • Sixth appendage pair modified as paddle. Based on joint reconstructions thistended to be used in rowing rather than subaqueous flight. Extimated top speed is about 2.5 X body length per second.
    • Reached large sizes (more than 2 m long)
    • Traditionally lumped with Xiphosaura into "Merostomata", but this is probably a paraphyletic assemblage (essentially "marine chelicerates" or "non-arachnid chelicerates")
    • Seem to have been more heavily mineralized than xiphosurans or arachnids, possibly because of larger body size



    .

    Walking: Seem to have been euryhaline. Depositional settings of eurypterid fossils indicate that they ranged from fresh to marine water, that individual animals seemed to be tolerant of a broad range of salinity, and that different groups tended to have preferences for a particular environment. Some have limbs that seem robust enough to allow excursions onto land.

    We have trackways that appear to have been made by brackish-fresh water eurypterids, indicating that, like crabs, they could emerge from the water.

    Eurypterid phylogenies have been proposed, but we should be cautious, as there is no guarantee that Eurypterida is monophyletic with respect to the next group...

    Arachnida (arachnids: scorpions, whip scorpions, pseudoscorpions, mites, ticks, daddy longlegs, spiders, and their extinct allies) (Sil. - Rec.)

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