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Maiocercus celticus is a species of early trigonotarbid arachnid from the Upper Carboniferous of Westhoughton, Lancashire, UK. The species was first described in 1902, with a "new species" being described in 1911 (M. orbicularis) which has been proven as being a junior synonym of M. celticus. M. celticus is the type species of the genus Maiocercus.

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  • Maiocercus (en)
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  • Maiocercus celticus is a species of early trigonotarbid arachnid from the Upper Carboniferous of Westhoughton, Lancashire, UK. The species was first described in 1902, with a "new species" being described in 1911 (M. orbicularis) which has been proven as being a junior synonym of M. celticus. M. celticus is the type species of the genus Maiocercus. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/20201202_Maiocercus_celticus.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Maiocercus_celticus.jpg
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  • †Anthracomartidae (en)
genus
  • ✝Maiocercus (en)
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  • Pocock, 1902 (en)
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  • Fossil of Maiocercus celticus located in Musee d'Histoire Naturelle, Brussels, Belgium. (en)
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  • †Trigonotarbida (en)
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  • ✝M. celticus (en)
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  • * Maiocercus orbicularis Gill, 1911 (en)
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  • Maiocercus celticus is a species of early trigonotarbid arachnid from the Upper Carboniferous of Westhoughton, Lancashire, UK. The species was first described in 1902, with a "new species" being described in 1911 (M. orbicularis) which has been proven as being a junior synonym of M. celticus. M. celticus is the type species of the genus Maiocercus. Originally zoologist Reginald Innes Pocock compared M. celticus to , with later evidence showing that Brachypyge had "opisthosoma which were much longer than wide; with the pleural laminæ of the second and third pleura-bearing terga being inclined slightly backwards" (Brachypyge) with Maiocercus having the “opisthosoma much wider than long; the pleural laminæ of the first, second, third, and fourth sterna being inclined slightly forwards”. The original drawing which showed Maiocercus described a pitting on the underside of the slightly forwarded laminæ, with a non-uniform concavity on the outer margins of them. The concavity is most well-marked in the fifth, sixth, seventh and eighth somites, with the opposite happening on the second, third and fourth somites. (en)
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