Phylum Arthropoda

Tree of Life
 

Phylum Arthropoda



The Cambrian period saw the emergence of group of animals that would conquer the marine environments world wide and go on to make the first pioneering steps onto land. Arthropods comprise the creatures with jointed legs, from fleas to crabs to the extinct trilobites to the extant but primitive horseshoe crab. Since first appearing, probably during the Precambrian, their variability has been nothing short of astonishing, and their impact on the living earth enormous. Arthropods (Greek for jointed feet) comprise the largest phylum of animals and include the Burgessia bella arthropod from Burgess Shaleinsects, arachnids, crustaceans, and many others as given in the table below. Approximately 80% of extant animal species are arthropods, with over a million modern species described and an extensive fossil record dating back to the base on the Cambrian.

Arthropods are most characterized by their jointed limbs and cuticles, which are mainly made of a-chitin. The cuticles of crustaceans are also biomineralized with calcium carbonate, as was that of the extinct trilobite. The cuticle is sufficiently inflexible as to inhibit growth such that it must be periodically replaced by molting, a characteristic that unites nine phyla in Superphylum Ecdysozoa (Arthropoda, Onychophora, Tardigrada, Kinorhyncha, Priapulida, Loricifera, Nematoda and Nematomorpha). The arthropod body plan consists of repeated segments, each with a pair of appendages. The embryos of all arthropods are segmented, 125 million year old Olenellus Cambrian trilobite from Pioche Formationbuilt from a series of repeated modules. The last common ancestor of living arthropods probably consisted of a series of undifferentiated segments, each with a pair of appendages that functioned as limbs. However all known living and fossil arthropods have grouped segments into tagmata in which segments and their limbs are specialized in various ways.

Parvancorina and Spriggina are Ediacaran animals from around 555 Mya that are among the earliest putative arthropods in the fossil record. Bivalve-like fossil shells have been found in China that date to some 541 to 539 million years ago. The earliest Cambrian trilobite fossils date to about 530 million years ago, but because they were already diverse and dispersed worldwide, they certainly must have already existed for a long period. Many arthropods are described from the Burgess Shale dating to some 505 million years ago. A large number of arthropods are also described from the older (525 to 520 million years) Chengjiang Maotianshan Shales. The earliest fossil crustaceans date to about 513 million years ago the earliest fossil shrimp to about 500 million years ago. The eariest identifiable body fossils of land animals are arachnids and chilopods from the late Silurian (419 million year ago) of England. Arthropod ichnofossils from the late Cambrian have been intertidal sand dune deposits in Canada and Wisconsin.

Because of their beauty and their extensive availablity in the fossil record, the trilobite is the unequivocal favorite among fossil collectors. Though trilobites dominated the Paleozoic marine environments, came back strong after several mass extinctions, they faded out by the end of the Permian, their niches on various marine environments taken over by their crustacean cousins. The spiders thrived on land as did the insects. Insects underwent an amazing adaptive radiation. Excluding microbial organisms, modern times are dominated by the insects, with beetles alone making up some 25% of known organisms.

Subphylum
Class
Common Examples
Trilobitamorpha (note1)                                Trilobita Trilobites and Relatives
Aglaspidida or Aglaspida Aglaspids
Chelicerata Arachnida Spiders, scorpions, harvestmen, ticks, and mites
Merostomata Horseshoe crabs and eurypterids.
Pycnogonida Sea spiders
Myriapoda Archipolypoda (note 2) early myriapod
Chilopoda Centipedes
Diplopoda Millipedes
Pauropoda  
Symphyla Garden centipedes
Hexapoda Diplura  
Collembola Springtails
Protura  
Insecta  
Crustacea Branchiopoda Brine shrimp
Remipedia  
Cephalocarida Horseshoe shrimps (no fossil record))
Maxillopoda Barnacles
Ostracoda Seed shrimp
Malacostraca Crabs, mole crabs, lobsters, isopods (woodlice and sowbugs), true shrimps, and Phyllocarids (?)

1 - Trilobitomorpha is a subphylum of the phylum Arthropoda that includes the trilobites. Originally a variety of peculiar forms, mostly from the lower Cambrian, were included as the Class Trilobitoidea. However, the many species do not appear to be closely related to the trilobites or, in many cases, to each other either, and are now generally placed in separate subphyla when classified at all.
2 - The Archipolypoda comprise the early Myriapods that are also often classified under the Diplopoda (millipedes). Archipolypods differed from millipedes, however, in having less coalesced segments, larger head Archipolypodareletive to the body, and large compound eyes. The fossil record indicates appearance of Archipolypoda in the Silurian and extinction at the end of the Carboniferous. Well-preserved specimens are known from the Mazon Creek Formation.

References:

  • Budd, G. E., Butterfield, N. J., and Jensen, S., "Crustaceans and the "Cambrian Explosion?", Science 294 (5549): 2047 (2001).
  • Yuan, X.; Xiao, S., Parsley, R.L., Zhou, C., Chen, Z. and Hu, J., "Towering sponges in an Early Cambrian Lagerstätte: Disparity between nonbilaterian and bilaterian epifaunal tierers at the Neoproterozoic-Cambrian transition", Geology 30 (4): 363–366 (2002).
  • Lin, J. P.; Gon, S.M.; Gehling, J.G.; Babcock, L.E.; Zhao, Y.L.; Zhang, X.L.; Hu, S.X.; Yuan, J.L.; Yu, M.Y.; Peng, J., "A Parvancorina-like arthropod from the Cambrian of South China", Historical Biology 18 (1): 33–45, (2006).
  • Lieberman, B. S., "Testing the Darwinian legacy of the Cambrian radiation using trilobite phylogeny and biogeography", Journal of Paleontology 73 (2): 176 (1999).
  • Jeram AJ, Selden PA, Edwards D. Land animals in the Silurian: arachnids and myriapods from Shropshire, England. Science. ;250:658–661. (1990).
  • MacNaughton RB, Cole JM, Dalrymple RW, Braddy SJ, Briggs DEG, Lukie TD. First steps on land: Arthropod trackways in Cambrian-Ordovician eolian sandstone, southeastern Ontario, Canada. Geology. (2002).
  • Hoxie, C., Late Cambrian Arthropod Trackways in Subaerially Exposed Environments (2005).