Palaeovaranus lismonimenos Georgalis & Čerňanský & Klembara 2021, n. sp.
Creators: name: Georgalis, Georgios L.
name: Čerňanský, Andrej
name: Klembara, Jozef
Publisher: name: Zenodo
Year: 2021
Subjects: Biodiversity
Taxonomy
Animalia
Chordata
Reptilia
Palaeovaranus
Palaeovaranus lismonimenos

description: Palaeovaranus lismonimenos n. sp.
(Figs 37B, D; 38-40; 41B; 42; 43)
urn:lsid:zoobank.org:act: 3C906259-DAB5-4B97-A1BB-7860695A76B8
HOLOTYPE. — An almost complete parietal (NHMW 2019 /0047/0001).
ETYMOLOGY. — The new name originates from the Greek word “λησμονημένος” (“lismonimenos”) meaning “forgotten”, alluding to the fact that the holotype specimen was forgotten and unnoticed inside a museum drawer for more than a century.
TYPE LOCALITY. — Imprecisely known locality, Phosphorites du Quercy, Department of Lot or Tarn-et-Garonne, Occitanie, southern France; probably late Eocene, around MP 17 (see Distribution below).
DIAGNOSIS. — The 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 supratemporal processes with the parietal plate.
REFERRED SPECIMENS. — A complete parietal (MNHN.F.QU17177) and a partial parietal (UM BFI 1873), both from juvenile individuals. Tentatively also, two frontals (MNHN.F.QU17175 and UM PRA 8).
DISTRIBUTION. — The holotype parietal NHMW 2019/0047/0001, the referred parietal MNHN.F.QU17177, and the tentatively referred frontal MNHN.F.QU17175, all originate from impre-
cisely known localities in the Department of Lot or that of Tarnet-Garonne, within the Phosphorites du Quercy. The referred parietal UM BFI 1873 originates from the late Eocene (MP 17) of Bouffie (= La Bouffie), Quercy (Department of Lot), while the tentatively referred frontal UM PRA 8 originates from the coeval, late Eocene (MP 17) locality of Les Pradigues, also in Quercy (but in the Department of Tarn-et-Garonne). Accordingly, we here sug- gest that the specimens with imprecise locality date (including the holotype), originate also from late Eocene locality(ies), potentially also around the MP 17 stage.
DESCRIPTION
Holotype NHMW 2019 /0047/0001 (Figs 37B, D; 38-40; 41B) The holotype NHMW 2019 /0047/0001 has a length of its parietal table 14.5 mm (measured in mid-line). The parietal table is anteroposteriorly elongate (Figs 37B; 38B; 39A). The anterolateral process is slender. The dorsolateral crest is distinctly developed. It extends posterolaterally and dorsally. Its margin is distinctly crenulated. The crenulation consists of several more or less shallow and long notches. The anterior end of the dorsolateral crest reaches the tip of the anterolateral process. The dorsolateral crests and the anterior margin of the parietal limit a triangular field. Its deepest portion is pierced by the parietal foramen. The foramen lies in about the midlength of the anterior half of the parietal table. The surface of the triangular field is covered by small, but distinct mounds, most of them bearing the longitudinal crests on their surfaces. The median crest is short and its posterior pointed portion fits between the two anteriorly pointed anterolateral processes of the triangular median field (Fig. 39A). The supratemporal fossa is large and is inclined ventrolaterally.
The ventral surface is smooth (Figs 37D; 38A; 39B). The anterior margin of the parietal fossa lies anterior to the level of the junctions of the anterolateral margins of the supratemporal processes with the parietal plate. The ventral cranial crest is rather low and runs closely medially to the lateral margin of the parietal table. The postfoveal crest passes along the medial margin of the root portion of the supratemporal process (Fig. 38A).
REMARKS
The two smaller specimens MNHN.F.QU17177 and UM BFI 1873 (Fig. 42), which we herein assign to Palaeovaranus lismonimenos n. sp. were originally described by Augé (2005) who also provided drawings of both (his Figs 194 and 195 respectively) and referred them to as “ Necrosaurus eucarinatus ” (see Discussion below about the status of this name). MNHN.F.QU17177 has a length of the parietal table 11.5 mm (measured in the mid-line) (Fig. 42A, B); thus, it is smaller than the holotype parietal NHMW 2019 /0047/0001 (14.5 mm). The right supratemporal process is completely preserved in MNHN.F.QU17177; it extends posterolaterally (Fig. 42A, B). The dorsolateral crests of the specimen MNHN.F.QU17177 bear slightly developed crenulations and do not meet in the mid-line, as is also the case in the still smaller specimen UM BFI 1873 (Fig. 42C, D). In this smallest specimen UM BFI 1873, the ornamentation is weakly developed and the dorsolateral crests are still more distantly placed one to another than in MNHN.F.QU17177. We may interpret this here by the hypothesis that during ontogenetic growth, the dorsolateral crests move one to another and finally fuse together in about their posterior portions to form a median crest. As a consequence, large anterior and small posterior median triangular fields are produced (Fig. 42). If so, the anatomy of three different size stages presented and discussed herein represent the first evidence of the medial movement of the dorsolateral crests to their final fusion in the median plane in adult specimens. We suppose the same process of the origin of the similar morphology of the dorsal surface of parietal in Palaeovaranus cayluxi.
Although there is no palaeovaranid frontal material in the NHMW collection, there have been previously described such elements from the Phosphorites du Quercy (Fig. 43).
Augé (2005) described the frontal MNHN.F.QU17175 as belonging to “ Necrosaurus cayluxi ” and that of the specimen UM PRA 8 as “ Necrosaurus eucarinatus ”. In contrast to Palaeovaranus cayluxi, however, both these frontals have the same type of mounds as those present in the dorsal surface of the parietals of Palaeovaranus lismonimenos n. sp. (Fig. 43). To the contrary, the dorsal surfaces of all three known parietals of Palaeovaranus cayluxi have no such type of ornamentation, as that exhibited in Palaeovaranus lismonimenos n. sp. Thus, it is highly probable that these two frontals belong to Palaeovaranus lismonimenos n. sp. and we accordingly, tentatively assign them to our new species.
description: Published as part of Georgalis, Georgios L., Čerňanský, Andrej & Klembara, Jozef, 2021, Osteological atlas of new lizards from the Phosphorites du Quercy (France), based on historical, forgotten, fossil material, pp. 219-293 in Geodiversitas 43 (9) on pages 253-258, DOI: 10.5252/geodiversitas2021v43a9, http://zenodo.org/record/4720776