Xenusion

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Xenusion auerswaldae
Temporal range: Cambrian: Late Stage 2→Early Stage 3
Xenusion P1060077.jpg
Scientific classification e
Kingdom: Animalia
Superphylum: Ecdysozoa
Phylum: "Lobopodia"
Class: Xenusia
Order: Protonychophora
Family: Xenusiidae
Genus: Xenusion
Pompeckj, 1927
Species: † X. auerswaldae
Binomial name
Xenusion auerswaldae
Pompeckj, 1927

Xenusion auerswaldae is an early arthropod/onychophore known from two specimens found in glacial debris in Germany.[1] They probably originated in the Kalmarsund Sandstone of Southern Sweden (Jaeger and Martinsson 1966), which was deposited in the Lower Cambrian (Upper Tommotian–Lower Atdabanian; Stages 2→3).[2] The specimens are not especially well preserved. The older specimen is 10 cm or so in length with a narrow, weakly segmented body. A depression runs up the bottom on all but the rearmost segments. There is a slightly bulbous tail, and each segment beyond that seems to have a single pair of tapering annulated legs similar to the modern onychophore, but without claws. Nine segments are present. There is a spine on each body bump and faint transverse parallel striations on the annulations on the legs. The legs of what is possibly the foremost segments are either missing or not preserved. The head is believed to be missing or is poorly preserved. If Xenusion is an arthropod/onychophore, it is one of the oldest currently known fossils of a mobile, modern animal.

Xenusion has been reinterpreted as an Ediacaran frond animal by Tarlo, and a drawing of that interpretation has been presented by McMenamin. Assuming that the creature is actually a lobopodian, the original specimen would appear to be part of an animal about 20 cm in length. In a photograph presented in The Treatise on Invertebrate Paleontology Volume O, the organism's appearance seems to support the original interpretation more. Further studies of Xenusiid close the possibility of a Rangeomorphy affinity.

References[edit]

  1. ^ Dzik, J.; Krumbiegel, G. N. (1989). "The oldest 'onychophoran' Xenusion: A link connecting phyla?". Lethaia 22 (2): 169. doi:10.1111/j.1502-3931.1989.tb01679.x.  edit
  2. ^ Han, J.; Zhang, Z. -F.; Liu, J. -N. (2008). "A preliminary note on the dispersal of the Cambrian Burgess Shale-type faunas". Gondwana Research 14: 269. doi:10.1016/j.gr.2007.09.001.  edit

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