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Longobardites parvus

Cephalopoda - Ceratitida - Longobarditidae

Taxonomy
Dalmatites parvus was named by Smith (1914). It is a 3D body fossil. Its type locality is Divide between Troy Canyon and South Fork of American Canyon, which is in an Illyrian marine limestone in Nevada. It is the type species of Neodalmatites.

It was recombined as Neodalmatites parvus by Spath (1951); it was recombined as Longobardites parvus by Silberling and Nichols (1982) and Monnet and Bucher (2005).

Sister species lacking formal opinion data

Synonyms
Synonymy list
YearName and author
1914Dalmatites minutus Smith p. 59 figs. Pl 29, figs 15-21
1914Dalmatites parvus Smith p. 60 figs. Pl. 30, Figs. 1-2,3-4
1951Neodalmatites parvus Spath p. 24
1982Longobardites parvus Silberling and Nichols p. 50 figs. Pl 21, figs 19-25; text-fig 33
2005Longobardites parvus Monnet and Bucher p. 49 figs. 47, 48; pl 31, figs 1-7

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Protostomia
Spiralia
superphylumLophotrochozoa
phylumMollusca
classCephalopodaCuvier 1797
RankNameAuthor
subclassAmmonoidea()
orderCeratitidaHyatt 1884
superfamilyDanubitoidea()
familyLongobarditidae
subfamilyLongobarditinae
genusLongobardites
speciesparvus()

If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.

Longobardites parvus Smith 1914
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Invalid names: Dalmatites minutus Smith 1914 [synonym]
Diagnosis
No diagnoses are available