Scincoidea, Oppel, 1811Scincoidea, Oppel, 1811
publication ID |
https://doi.org/ 10.5252/geodiversitas2021v43a17 |
publication LSID |
urn:lsid:zoobank.org:pub:E0BAA274-37CB-407B-849A-FD284BBE954B |
persistent identifier |
https://treatment.plazi.org/id/0F23E968-FF83-FF9B-FED3-793ED1A6FC9B |
treatment provided by |
Felipe |
scientific name |
Scincoidea Scincoidea |
status |
|
Scincoidea indet.
MATERIAL EXAMINED. — Two incomplete dentaries: Dentary, MNHN. F.MTC245 ( Fig. 2 View FIG ), bears four tooth loci (the most posterior teeth); Dentary, MNHN. F.MTC244 ( Fig. 3 View FIG ), bears four tooth loci.
DESCRIPTION
Dentaries, MNHN. F.MTC245 ( Fig. 2 View FIG )
This robust, right dentary ( L = 3.7mm) is strongly arched (concave), its posterior part is deep and it distinctly narrows towards the anterior margin. This specimen preserves three incomplete teeth. On the lingual side the subdental shelf (sensu Rage & Augé 2010) is eroded except in the posterior part of the dentary, where it is sub-vertical and meets the dental table nearly at a right angle. It is difficult to assess the presence of a medial sulcus dentalis along the tooth bases, due to the poor preservation of the subdental shelf. A large posterodorsal process extends behind the level of the last tooth and presents a deep, inclined surface which certainly received the anteromedial dentary process of the coronoide. On that surface, a circular cavity located behind the level of the last tooth may mark the position of the anterior end of this process. Posteriorly, the sulcus Meckeli is widely open medially and it gradually narrows towards the anterior end of the specimen. Under the dental table, there is an intramandibular septum, between the level of the last-penultimate tooth positions. It shows no vertical projection.
In lateral view, no labial foramens are exposed. Posteriorly, there is a well-developed labial coronoid process, which bears no trace of contact with an anterolabial dentary process of the coronoid.
Dentition: The three incompletely preserved teeth are pleurodont and robust (amblyodont). They gradually taper towards the apex, the tooth base is enlarged and medially expanded. Two tooth bases are pierced by a large, central replacement cavity and cement deposits around the tooth bases are poorly developed. Apices are broken in all teeth, except perhaps for the last one which seems to bear a rounded crown.
Specimen MNHN. F.MTC244 ( Fig. 3 View FIG )
Incomplete left dentary ( L = 5.1mm) that bears five tooth positions, and two teeth partially preserved. The morphology of dentary MNHN. F.MTC244 is nearly identical to that of
specimen MTC245 (described above). The subdental shelf is arched, vertical and moderately deep and it meets the dental table nearly at a right angle.A sulcus dentalis is present.The teeth are better preserved than those of specimen MTC245 and their apex is obtusely pointed and bears neither cusps nor striations.
The labial surface of the two dentaries bears important marks of alteration, certainly caused by digestive process ( Andrews 1990). It is worth noting that these processes could be at least partially behind the lack of striations on the teeth (see above).
COMPARISONS AND DISCUSSION
On account of the fragmentary nature of these specimens their taxonomic position is difficult to evaluate. In addition, no clear diagnostic features or synapomorphies are present in those dentaries. However, there are some features which, in combination may suggest scincoid relationships:pleurodont dentition, subdental shelf well developed, sub-vertical and forming a nearly right angle with the surface of the dental table, presence of a sulcus dentalis.At this point, it may be objected that those characters are also present in Lacertoidea (and particularly in lacertid lizards). However the first dentary (specimen MNHN. F.MTC245) differs significantly from that of most fossil and extant Lacertoidea in two characters: 1) in lingual view, the presence of a large posterodorsal extension behind the subdental shelf that received the anteromedial dentary process of the coronoid; and 2) in labial view, the dentary has an upwardly directed coronoid process that prevents the extension of the coronoid onto the labial surface of the dentary ( Daza et al. 2015). In lacertid and teiid lizards this process is reduced and the anterolateral dentary process of the coronoid is expanded anteriorly and covers the posterodorsal part of the dentary, generally leaving a clear mark on it ( Augé 2005).
Presence of a mesial and distal crest or of a single longitudinal crest on the tooth crown are certainly primitive within Scincoidea ( Kosma 2004; Richter 1994, 1995; Georgalis et al. 2017). Accessory cusps on the mesial and distal crests are virtually unknown in Scincoidea and skinks tend to have blunt, chisel-shaped tooth crowns ( Smith & Gauthier 2013; Daza et al. 2015) while most lacertids have acute cusps; absence of cusps in the dentaries from Montchenot tend to exclude them from lacertoid lizards.
Absence of striae on the tooth crowns and obtusely pointed teeth without longitudinal crest (in dentary MNHN. F.MTC244) are clearly characters that come into conflict with the generalized scincoid dentition ( Richter 1994; Böhme 2010) or scincid grade sensu Kosma (2004:5). Once again, absence of striae may be du to the poor preservation of these teeth. However, a great number of forms, notably among scincids, depart from this tooth pattern and bear specialized dentitions ( Estes & Williams 1984; Kosma 2004; Augé 2005; Nydam et al. 2013; Bolet & Augé 2014).In addition, this scincid-grade of tooth morphology is also present in some non-scincid taxa, such as some species of Gymnophthalmidae and Gekkonidae ( Nydam et al. 2013; Sumida & Murphy 1987). In addition, the lack of striae may be due to taphonomic pocesses (e.g. digestive process) that affected the enamel.
Recently, several scincoid taxa have been described in the European Paleogene, some forms being referred to scincids (e.g. Bolet et al. 2015; Augé 2005) others to cordylids s.l. ( Bolet & Evans 2013) or to Scincoidea ( Weber 2004; Folie et al. 2005; Bolet & Augé 2014; Augé & Smith 2009; Čerňanský et al. 2016). Most generally, these authors recognized that the distinction between the two families ( Scincidae and Cordylidae ) is difficult. The tooth shape and the arched dentary suggest that the fossils from Montchenot belong more likely to scincids than to cordylids. Unfortunately, these fossils are too incomplete and thus unsuitable for a more specific assignment.
As a last point, some characters of these dentaries, in combination, may suggest amphisbaenian relationships (e.g. well-developed coronoid process, robust teeth and a probable low tooth count). However, their general shape, in particular their strongly arched (concave) ventral border and subdental shelf clearly exclude this possibility. This morphology sharply contrast with the straight ventral border of the dentary that is shown by nearly all amphisbaenian members (see Gans & Montero 2008). Gans (1974) clearly demonstrates that this morphology is tied to the fossorial habits of these lizards.
? Scincoidea indet.
MATERIAL EXAMINED. — MNHN. F.MTC242, one incomplete axis ( Fig. 4 View FIG ).
DESCRIPTION
Terminology follows Hoffstetter & Gasc 1969 and Čerňanský et al. 2014.
The centrum is well-preserved and strongly built but the neural arch is entirely lacking. A posteroventrally oriented intercentrum (second intercentrum) is sutured (not fused) to the base of the centrum and forms a rather short ventral keel in the antero-ventral region of the centrum. A small, slightly anteriorly curved process is fused to the posterior part of the base of the centrum, nearly beneath the condyle articulation. These two reliefs are separated by a deep, rounded trench.
The huge odontoid process covers most of the articulation area in anterior view, it is high (dorso-ventrally elongated) and not markedly expanded anteriorly. In posterior view, the condyle is laterally compressed.
REMARKS
According toČerňanský 2016 the squamate atlas-axis complex may be an important source of new morphological characters that can help to resolve persistent conflicts between morphological and molecular phylogenetic analyses of lizard phylogeny ( Losos et al. 2012). However, only a handful of morphological studies include detailed anatomy of the atlas-axis complex in lizards ( Rieppel 1980, Čerňanský et al. 2019, anguimorph lizards; Čerňanský et al. 2014;Čerňanský 2016; Čerňanský & Stanley 2019 about the atlas-axis in chamaeleonids, Cordyliformes and dibamids respectively; Vaugh et al. 2015, geckos). The work of Hoffstetter & Gasc 1969 develops a wide-ranging comparative study of the atlas-axis complex between lizard families.
The axis from Montchenot bears several phylogenetic significant characters: odontoid process dorso-ventrally elongated; condyle laterally compressed (occurs in nearly all Cordyliformes, Čerňanský 2016: 22); position and suture of intercentra on the ventral region of the centrum. Among Anguimorpha , the intercentra are fused to the centrum in anguid lizards and in varanids the odontoid process is laterally elongated. The condyle of lacertoid lizards is rather rounded and not laterally compressed and most gekkonids have amphicoelous vertebrae. All characters of this axis suggest scincoid relationships. For example, the morphology of the axis of Broadleysaurus (Cordyliformes, Gerrhosauridae ) is very similar to that of the axis from Montchenot (Čerňanský 2016: fig. 8). However, this referral is at best tentative due to the incompleteness of MNHN. F.MTC242 and the very limited number of specimens available for comparisons.
? Scincoidea indet.
MATERIAL EXAMINED. — MNHN. F.MTC242, one incomplete axis ( Fig. 4 View FIG ).
DESCRIPTION
Terminology follows Hoffstetter & Gasc 1969 and Čerňanský et al. 2014.
The centrum is well-preserved and strongly built but the neural arch is entirely lacking. A posteroventrally oriented intercentrum (second intercentrum) is sutured (not fused) to the base of the centrum and forms a rather short ventral keel in the antero-ventral region of the centrum. A small, slightly anteriorly curved process is fused to the posterior part of the base of the centrum, nearly beneath the condyle articulation. These two reliefs are separated by a deep, rounded trench.
The huge odontoid process covers most of the articulation area in anterior view, it is high (dorso-ventrally elongated) and not markedly expanded anteriorly. In posterior view, the condyle is laterally compressed.
REMARKS
According toČerňanský 2016 the squamate atlas-axis complex may be an important source of new morphological characters that can help to resolve persistent conflicts between morphological and molecular phylogenetic analyses of lizard phylogeny ( Losos et al. 2012). However, only a handful of morphological studies include detailed anatomy of the atlas-axis complex in lizards ( Rieppel 1980, Čerňanský et al. 2019, anguimorph lizards; Čerňanský et al. 2014;Čerňanský 2016; Čerňanský & Stanley 2019 about the atlas-axis in chamaeleonids, Cordyliformes and dibamids respectively; Vaugh et al. 2015, geckos). The work of Hoffstetter & Gasc 1969 develops a wide-ranging comparative study of the atlas-axis complex between lizard families.
The axis from Montchenot bears several phylogenetic significant characters: odontoid process dorso-ventrally elongated; condyle laterally compressed (occurs in nearly all Cordyliformes, Čerňanský 2016: 22); position and suture of intercentra on the ventral region of the centrum. Among Anguimorpha , the intercentra are fused to the centrum in anguid lizards and in varanids the odontoid process is laterally elongated. The condyle of lacertoid lizards is rather rounded and not laterally compressed and most gekkonids have amphicoelous vertebrae. All characters of this axis suggest scincoid relationships. For example, the morphology of the axis of Broadleysaurus (Cordyliformes, Gerrhosauridae ) is very similar to that of the axis from Montchenot (Čerňanský 2016: fig. 8). However, this referral is at best tentative due to the incompleteness of MNHN. F.MTC242 and the very limited number of specimens available for comparisons.
MNHN |
Museum National d'Histoire Naturelle |
F |
Field Museum of Natural History, Botany Department |
L |
Nationaal Herbarium Nederland, Leiden University branch |
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.