Chasmataspidida | |
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Scientific classification | |
Kingdom: | Animalia |
Phylum: | Arthropoda |
Subphylum: | Chelicerata |
Class: |
†Chasmataspidida Caster & Brooks, 1956 |
Families & genera | |
†Chasmataspididae Caster & Brooks, 1956
†Diploaspididae Størmer, 1972
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†Chasmataspididae Caster & Brooks, 1956
†Diploaspididae Størmer, 1972
Chasmataspidida (often referred to informally as chasmataspids) is an extinct group of rare chelicerate arthropods. Chasmataspids are probably related to horseshoe crabs (Xiphosura) and/or sea scorpions (Eurypterida). Indeed the first species to be discovered were thought to be unusual fossil horseshoe crabs, while later species were often based on specimens initially misidentified as eurypterids. There is some evidence that chasmataspids were present during the late Cambrian and the group is known sporadically in the fossil record through to the mid-Devonian. Chasmataspids are most easily recognised by having an abdomen divided into a short forepart (or mesosoma) and a longer hindpart (or metastoma) comprising nine segments. There is some debate about whether they form a natural (i.e. monophyletic) group.
The first chasmataspid to be discovered was Chasmataspis laurencii, described by the American palaeontologists Kenneth E. Caster and H. K. Brooks. These Ordovician fossils come from the site of the Douglas Dam in Tennessee, USA. They are the most xiphosuran-like of the known chasmataspid species, with a horseshoe-shaped headshield. Caster & Brooks raised a new family, Chasmataspididae, to accommodate these specimens. The species was redescribed by Jason Dunlop and colleagues.
The next species to be discovered were Diploaspis casteri and Heteroaspis novojilovi; both described by the Norwegian palaeontologist Leif Størmer from the early Devonian of Alken an der Mosel in Germany.
A revision by Markus Poschmann and co-workers recognised H. novojilovi as a synonym of D. casteri. The two genera appear to actually be preservational variants of the same species. Poschmann et al.. also described a second species as Diploaspis muelleri.
Forfarella mitchelli from the early Devonian of the Forfar region in the Midland Valley of Scotland was described by Jason Dunlop and colleagues; although the fossil had actually been recognised as a chasmataspid and provisionally labelled as such some years previously by Charles Waterston. Forfarella mitchelli is not very well preserved, but does show the characteristic chasmataspid body plan.
The stratigraphically youngest chasmataspid is Achanarraspis reedi, described by Lyall Anderson and colleagues from the mid-Devonian Achanarras quarry in Caithness, Scotland; a famous fossil fish locality.