2009
DOI: 10.1163/187525409x462395
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Millipedes from the Grès à Voltzia, Triassic of France, with comments on Mesozoic millipedes (Diplopoda: Helminthomorpha: Eugnatha)

Abstract: Hannibaliulus wilsonae, n. gen., n. sp. is described from a series of ten specimens from the early Triassic Grès à Voltzia Lagerstätte of northeast France. e best specimens (holotype and paratype) show a probably equal number of around 44 diplosegments. e a nities of the new species appear to be with the Order Callipodida, but clear apomorphies of that order are not observable on the specimens, both of which appear to be female. Other records of Mesozoic diplopods are brie y discussed and evaluated.

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Cited by 13 publications
(21 citation statements)
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References 16 publications
(29 reference statements)
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“…Furthermore, the Triassic fossil is known to have a body composed of 40–44 body rings and a much longer length (ca 55 mm). Ozopores, pleurotergal setae and spinnerets have not been detected in H.wilsonae (Shear et al 2009).…”
Section: Discussionmentioning
confidence: 93%
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“…Furthermore, the Triassic fossil is known to have a body composed of 40–44 body rings and a much longer length (ca 55 mm). Ozopores, pleurotergal setae and spinnerets have not been detected in H.wilsonae (Shear et al 2009).…”
Section: Discussionmentioning
confidence: 93%
“…Burmanopetaluminexpectatum gen. nov. et sp. nov. can be readily distinguished from Hannibaliuluswilsonae Shear et al 2009, a possibly nematophoran callipodid-like millipede of early Triassic (Anisian) age (ca 243 Mya) by having 'normal' undivided metazonites (vs divided by a wide, shallow transverse depression into anterior and posterior parts, with ventral margins strongly rebordered) and eyes composed of only five ommatidia (vs eyepatches with numerous ommatidia). Furthermore, the Triassic fossil is known to have a body composed of 40–44 body rings and a much longer length (ca 55 mm).…”
Section: Discussionmentioning
confidence: 99%
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“…Fossil millipedes are mainly documented from the Paleozoic because they are relatively abundant in the extensive coal-forest deposits of the upper Carboniferous; they are also well documented in amber deposits, particularly those of the Cenozoic. Only rarely have they been described from the Mesozoic (Dzik, 1981; Jell, 1983; Duy-Jacquemin and Azar, 2004; Rasnitsyn and Golovatch, 2004; Shear et al, 2009; Shear and Edgecombe, 2010; Edgecombe, 2015; Liu et al, 2017). Mesozoic occurrences include two described genera from the Triassic (France and central Siberia), one genus from the Jurassic of Australia, and six genera from the Cretaceous (Mexico, Europe, Lebanon, Mongolia, and Myanmar).…”
Section: Introductionmentioning
confidence: 99%
“…De igual forma el Mesozoico, se caracteriza en general, con escasos registros aislados (Shear et al, 2009); el Cenozoico, también se caracteriza por unos pocos registros de Myriapoda, preservados en ámbar y asignables principalmente a taxones vivientes (Hoffman, 1969;SantiagoBlay y Poinar, 1992;Shear y Edgecombe, 2010;Riquelme et al, 2014a y b).…”
Section: Introductionunclassified