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Palaeovaranus lismonimenos

Reptilia - Palaeovaranidae

Taxonomy
Palaeovaranus lismonimenos was named by Georgalis et al. (2021). Its type specimen is NHMW 2019/0047/0001 (incomplete parietal) and is a 3D body fossil. Its type locality is Phosphorites du Quercy (for taxa with non-specific locality data), which is in an Eocene/Miocene terrestrial phosphorite in the Quercy Phosphorites Formation of France.

Synonymy list
YearName and author
2021Palaeovaranus lismonimenos Georgalis et al.

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RankNameAuthor
kingdomAnimalia()
Bilateria
EubilateriaAx 1987
Deuterostomia
phylumChordataHaeckel 1874
subphylumVertebrata
superclassGnathostomata
Osteichthyes()
subclassSarcopterygii()
subclassDipnotetrapodomorpha(Nelson 2006)
subclassTetrapodomorpha()
Tetrapoda
RankNameAuthor
Reptiliomorpha
Anthracosauria
subclassAmphibiosauriaKuhn 1967
Cotylosauria()
Amniota
Sauropsida
classReptilia
Squamata()
Anguimorpha(Fürbringer 1900)
familyPalaeovaranidaeGeorgalis 2017
genusPalaeovaranusZittel 1887
specieslismonimenos

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.

Palaeovaranus lismonimenos Georgalis et al. 2021
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Diagnosis
ReferenceDiagnosis
G. L. Georgalis et al. 2021The parietal of Palaeovaranus lismonimenos n. sp. differs from that of Palaeovaranus cayluxi by the following distinguished features and the combination of features: 1) the dorsolateral crests are rather distinct, extending posterolaterally and dorsally, and their margins are distinctly crenulated; 2) the median crest is short (shorter than the length of the median triangular field measured in the median plane) and its posterior tip fits between the anterolateral processes of the triangular median field; 3) the anterior ends of the dorsolateral crests extend to the tips of the anterolateral processes; 4) the ornamentation of the parietal consists of small, more or less densely arranged mounds having more or less distinctly developed crest; and 5) the anterior margin of the parietal fossa lies anterior to the level of the junctions of the anterolateral margins of the su- pratemporal processes with the parietal plate.
Measurements
No measurements are available
Composition: phosphaticsubp
Environment: terrestrialuc
Locomotion: actively mobilec
Created: 2017-04-17 15:15:35
Modified: 2017-04-17 15:15:35
Source: c = class, subp = subphylum, uc = unranked clade
References: Hendy et al. 2009, Carroll 1988

Age range: base of the Late/Upper Eocene to the top of the Early/Lower Miocene or 37.20000 to 15.97000 Ma

Collections: one only


Time interval Ma Country or state Original ID and collection number
Late/Upper Eocene - Early/Lower Miocene37.2 - 15.97France (Languedoc-Roussillon-Midi-Pyrénées) Palaeovaranus lismonimenos (type locality: 179194)