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Revista mexicana de ciencias geológicas

versión On-line ISSN 2007-2902versión impresa ISSN 1026-8774

Rev. mex. cienc. geol vol.24 no.1 Ciudad de México abr. 2007


Revista Mexicana de Ciencias Geológicas


Cranial anatomy of a Maastrichtian (Upper Cretaceous) mosasaur (Squamata, Mosasauridae) from north–east Mexico


Anatomía craneana de un mosasauro (Squamata, Mosasauridae) del Maastrichtiano (Cretácico Superior) del noreste de México


Marie–Céline Buchy1, Eberhard Frey2, Wolfgang Stinnesbeck3, and José Guadalupe López–Oliva4


1 Universität Karlsruhe, Geologisches Institut, Postfach 6980, D–76128 Karlsruhe, Germany. Current address: Museo del Desierto, Apartado Postal 307, 25000 Saltillo, Coahuila, Mexico.

2 Geowissenschaftliche Abteilung, Staatliches Museum für Naturkunde, Erbprinzenstrasse 13, D–76133 Karlsruhe, Germany.

3 Universität Karlsruhe, Geologisches Institut, Postfach 6980, D–76128 Karlsruhe, Germany.

4 Universidad Autónoma de Nuevo León, Facultad de Ciencias de la Tierra, Apartado Postal 104, 67700 Linares, N.L., Mexico.


Manuscript received: January 12, 2005
Corrected manuscript received: December 8, 2006
Manuscript accepted: February 13, 2007



We here describe ihefirsl mosasaur from Mexico known by significanl cranial remains, from ihe late Early Maastrichtian Méndez Formation of Nuevo León, north–east Mexico. The specimen comprises a fragmentary skull and parts of the mandibles. Some anatomical features suggest a juvenile animal. The skull possesses a rostral tuberosity on the premaxilla, as well as a combination of features known from different mosasaur genera, like its frontopremaxillary suture situated caudal to the external naris, its prefrontal and postorbitofrontal being in contact lateral to the orbit, associated with the supra– and infrastapedial processes of its quadrate which almost contact one another. Despite being clearly distinct from any hitherto described mosasaur, the affinities of this specimen with other mosasaurs remain obscure, not only because of incompleteness, but also because of the poorly understood biological significance of the characters used for the classification of Mosasauridae.

Key words: Mosasauridae, Early Maastrichtian, Méndez Formation, north–east Mexico.



Se describe el primer mosasauro conocido por restos de cráneo de México, de la Formación Méndez, del final del Maastrichtiano Temprano, de Nuevo León, noreste de México. El espécimen comprende un cráneo fragmentado y partes de las mandíbulas. Diversas estructuras anatómicas sugieren que este era un animal joven. El cráneo tiene una protuberancia rostral en la premaxila, así como una combinación de estructuras conocidas de diferentes géneros de mosasauros, entre ellas, la sutura frontopremaxilar situada caudalmente a su nariz, el prefrontal y postorbitofrontal están en contacto lateral con la órbita, asociados con los procesos supra e infrastapedial de su cuadrado, los cuales tienen un ligero contacto entre sí. A pesar de ser claramente distintos de cualquier otro mosasauro descrito hasta ahora, las afinidades de este espécimen con otros mosasauros permanecen inciertas, no solamente debido a lo incompleto, sino también porque la significancia biológica de los caracteres utilizados para la clasificación de los mosasauros (Mosasauridae) está pobremente entendida.

Palabras clave: Mosasauridae, Maastrichtiano Temprano, Formación Méndez, noreste de México.



Mosasaurs were Upper Cretaceous marine lizards with possible varanoid affinities (De Braga and Carroll, 1993; Caldwell et al., 1995; Bell, 1997a; Zaher and Rieppel, 1999; Evans et al., 2006). Currently, all mosasaurs are grouped within Mosasauridae (Bell, 1997b). Until recently, Mosasauridae was conceived of as a morphologically homogeneous group, and the classification of Williston (1895, 1897) separating three subfamilies had not been profoundly modified by subsequent analyses (Russell, 1967; De Braga and Carroll, 1993; Bell, 1997b). However, Bell andPolcyn (2005) recently suggested that fin–like limbs evolved at least twice within mosasauroids. Should their results be supported by further analyses, our understanding of the relationships within the group might change drastically.

Mosasaurs are known worldwide and are especially abundant in the Upper Cretaceous sediments of North America and Europe (Williston, 1897, 1898; Dollo, 1904, 1913; Russell, 1967; Lingham–Soliar and Nolf, 1989; Lingham–Soliar, 1992, 1994). During the Late Cretaceous, the European Archipelago and the Western Interior Seaway, as well as the North and South American Pacific coasts, were connected by the Atlantic Ocean (Sohl et al., 1991). However, despite the intermediate geographical position of north–east Mexico between these continuous marine realms, only a single mosasaur has until now been described from there, Amphekepubis johnsoni (Mehl, 1930). The species is based on a pelvic girdle, hind limb bones and nine caudal vertebrae. The exact stratigraphical origin of this material is uncertain, as is the precise geographical location of the find, "about forty miles east and a little north of Monterrey, Nuevo León" (Mehl, 1930, p. 383). From the matrix, Mehl (1930) suggests that it comes from the San Felipe Formation (Coniacian–Santonian) but admits that it could also be younger. Camp (1942, p. 25) and later Lingham–Soliar (1995, p. 171–172) both consider the holotype of Amphekepubis as a member of the genus Mosasaurus.

Additionally, an undetermined fragment of a mosasaur j aw with three incomplete teeth from the Méndez Formation (Campanian–Maastrichtian) of Hualahuises, approximately 10 km north of Linares, N. L., was described by Aranda–Manteca and Stinnesbeck (1993). Some vertebrae and other undescribed postcranial elements belonging to indeterminate mosasaurs from the Méndez Formation of Nuevo León and the neighbouring State Coahuila are kept in the collections of the Universidad Autónoma de Nuevo León, Facultad de Ciencias de la Tierra, Linares (UANL–FCT) and the Museo del Desierto, Saltillo, Coahuila (MUDE), Mexico (Buchy et al., 2005). These fossils indicate a high potential to find mosasaur remains in the uppermost Cretaceous sediments of north–east Mexico.

The specimen we describe here represents the first significant cranial remains of a mosasaur from Mexico. They were collected by G. Barbosa Navéjar, S. Navéjar Torres, and A. Navéjar Ruiz in October and November of 2001 from marls of the Méndez Formation at Rancho Las Barretas, between El Canela and La Escondida, 10 km north–east of Linares, N. L. (24°57'87'' N, 99°30'46'' W; Figure 1). When presenting the material to one of us (J.G. L.–O.) the discoverers described an animal that was 'flying on the ground'. Therefore it appears likely that the rest of the skeleton is still in place. Unfortunately, the discoverers cannot remember the exact location of the find in an uniform landscape.

We here give a description of the remains secured thus far (Figures 2, 3, 4, 5, 6, 7), pending the collection of more material. The specimen is housed in the palaeontological collection of the UANL–FCT, under accession number UANL–FCT–R4.



From the regional geology and marl lithologies covering UANL–FCT–R4, the fossil doubtlessly comes from the Méndez Formation, a lithostratigraphic unit of Campanian–Maastrichtian age (Keller et al., 1997; Stinnesbeck et al., 2001). The Méndez Formation is widely distributed in the Gulf Coast Plain of north–east Mexico, east and south–east of the city of Monterrey (Figure 1). The unit is up to 1,000 m thick and consists of rhythmically bedded marls, shales, and minor sandstones. These were deposited in an open marine shelf environment in water depths of approximately 100 m near Los Ramones, 40 km north–east of Monterrey, and more than 400 m in the La Sierrita region, 40 km east of Montemorelos (Keller et al., 1997; Stinnesbeck et al., 2001). Planktic andbenthic foraminiferal assemblages are rich and diverse throughout the Méndez Formation, whereas macrofossils, like inoceramids, ammonites, and vertebrate remains, are rare and known only from a few locations (Ifrim et al., 2004).

Foraminifers present in the marls adjacent to UANL–FCT–R4 include Heterohelix globulosa, H. striata, H. planata, H. dentata, H. pulchra, H. moremani, H. punctulata, H. glabrans; Pseudoguembelina kempensis, P. costulata, P. palpebra; Pseudotextularia elegans, P. deformis, P. nutalli; Hedbergella holmdelensis, H. monmouthensis; Rugoglobigerina pennyi, R. hexacamerata, R. macrocephala; Gansserina gansseri; Globotruncana aegyptica, G. arca, G. ventricosa, G. linneiana, G. orientalis, G. rosetta, G. esnehensis; Globotruncanita stuarti; Globotruncanella petaloidea.

Datum events and biozones presented within the zonal scheme based on planktic foraminiferal assemblages introduced for the Maastrichtian by Li and Keller (1998), based on Tunisian sections and DSDP sites (525), appear broadly valid throughout the central and western Tethys, including Mexico (e.g. Tantawy et al., 2001; Keller et al., 2002). This zonal scheme subdivides the Maastrichtian into nine zones labelled CF1–CF8a andb (CF for Cretaceous Foraminifera) and thus provides the highest resolution age control known to date for the Maastrichtian. Planktic foraminiferal assemblages obtained from UANL–FCT–R4 marl sample of the Méndez Formation correlate well with this zonal scheme. The presence of G. gansseri marks the base of zone CF 7 (base of the former G. gansseri Zone) while the absence of R. contusa (FAD characterises the base zone CF 6) excludes an age younger than CF 7. The microfossils thus date the ammonite assemblage into the Early Maastrichtian, between 70.39 and 69.56 Ma (Tantawy et al, 2001, fig. 4).



Order Squamata Oppel, 1811
Family Mosasauridae Gervais, 1853
Figures 2, 3, 4, 5, 6, 7

Material. UANL–FCT–R4. Incomplete skull and mandible (Buchy et al, 2005, figs 6, 7).

Origin. Late Early Maastrichtian (Upper Cretaceous) of the Méndez Formation at Rancho Las Barretas, between El Canela and La Escondida, 10 km north–east of Linares, N. L. (24°57'87'' N, 99°30'46'' W; Figure 1).

Preservation. The skull roof, comprising the frontal, most of the parietal, the medial portions of both prefrontals and both postorbitofrontals, as well as the caudal portion of the internarial bar, is preserved in articulation. It extends from the caudal–most extremities of the nares to the caudal part of the intertemporal bar (Figure 3). The rostral–most part of the skull roof was broken in several fragments, and later glued together. The osteology of this area is additionally obscured by surface weathering which exposed the spongiosa in some places.

The median portion of the rostral ramus of the right jugal has moved to the dorsal face of the frontal. The left jugal and the caudal half of the right pterygoid lie adjacent to the left ventral surface of the frontal. Some bone fragments adhere dorsally to the portion of the left jugal ramus, which is now preserved ventral to the right prefrontal and postorbitofrontal, (Figure 3). Prefrontal and postorbitofrontal contact each other ventral to the frontal on the right side of the specimen. On the left, the area were they presumably were in contact is weathered. However, their thickness at the broken right lateral margins of the skull roof indicates that a substantial lateral portion of them is missing. Moreover, if the prefrontal and the postorbitofrontal originally had no contact to one another lateral to the orbit, then the supraorbital notch must have been exceedingly pronounced and obtuse (Figure 3), unlike in any other mosasaur. Presumably the bone fragments preserved on the left jugal ramus are part of the prefrontal and/or postorbitofrontal, which were broken due to compaction and testify to the original contact of the prefrontal and postorbitofrontal lateral to the frontal.

The rostral margin of the orbit, formed by a transverse descending flange of the prefrontal, is situated toward the middle of the prefrontal as it is preserved (Figure 3). In mosasaurs, this margin normally originates around the caudal third of the prefrontal (Russell, 1967: 21); we can therefore estimate that approximately the rostral third of the prefrontal is missing in UANL–FCT–R4.

On the dorsal surface of the frontal, an undulating vein of sediment runs caudomedially from the frontoprefrontal suture until the midline, and is bilaterally symmetrical insofar as can be judged given the displaced jugal (Figure 3). This vein is continuous from weathered to non–weathered areas. It has a constant width and is smooth, without the sharp angles and branching pattern of clear breaks. It instead shows the undulating pattern of a typical suture (see Discussion).

A detached fragment of bone bearing poorly preserved teeth is identified as part of the dentigerous portion of one of the pterygoids (Figure 5).

The intertemporal bar underwent a compression directed ventromediorostrally, as witnessed by the slight counterclockwise rotation of the parietal foramen, and the pattern of cracks running from its corners (Figure 3).

The right quadrate (Figure 6) was tilted rostromedially into the right supratemporal fenestra. Only its ventral half is preserved probably due to collection bias. The caudolateral–most preserved part of the suspensorial ramus of the right parietal broke off from the intertemporal bar and lies now adjacent to the ventral condyle of the quadrate (Figure 6).

The premaxilla is broken 60 mm caudal to its rostral extremity (Figure 2). Caudal to this break, the intermaxillary segment of the internarial bar was pressed ventrally, and lies 3 mm ventral to the surface of the maxillae. The middle segment of the internarial bar is missing. In ventral view, the premaxilla is mostly obscured by matrix.

The dentigerous portions of both maxillae are almost completely preserved and articulate with the rostral extremity of the premaxilla (Figure 2). The dorsal margin of each maxilla was pressed medially and is broken. Some fragments of the dorsal maxillary margins are now preserved tilted ventromedially against the ventral dentigerous part of the maxillae. The entire muzzle unit (as defined by Russell, 1967: 14) was subject to erosion after breakage. All maxillary and premaxillary tooth crowns are broken, and the enamel of the detached preserved fragments of crowns is eroded.

Fragments of bothvomers are preserved between the maxillae, separated by a 45 mm long rod of bone identified as the ventral internarial process of the premaxilla (Figure 2). The right vomer is broken caudally level with the seventh right maxillary tooth; the left vomer is broken 10 mm further rostrally. In ventral view, both are obscured rostrally by matrix and in dorsal view by the maxillae and the premaxilla.

The middle portion of each anterior lower jaw (as defined by Russell, 1967: 49–51) is preserved (Figure 4). As determined by comparison with the upper jaw, the length of the missing rostral portion is at least 50 mm. The intramandibular articulation is also missing. The lateral and medial surfaces of both anterior lower jaws are weathered. The ventral half of the lateral surface of the better preserved right one is damaged, as witnessed by the splenial which is laterally exposed over three quarters of the specimen (in mosasaurs the splenial disappears rostral to the caudal third of the dentary in lateral view [Russell, 1967: 50]). The lateral surface of the rostroventral–most portion of the right splenial of UANL–FCT–R4 is depressed (Figure 4). This depression is most likely the imprint of the dentary and therefore marks its original extension lateral and ventral to the splenial.

Most of the preserved functional dentary teeth lack enamel.



Premaxilla (Figures 2, 3). The rostral extremity of the premaxilla bears a rostrally directed 5 mm thick circular tuberosity the centre of which exhibits a foramen 2 mm in diameter. This tuberosity is situated 10 mm dorsal to the ventral margin of the bone, on the midline. Faint regular wrinkles radiate from the tuberosity. They disappear approximately 10 mm away from the tuberosity. Ventral to the tuberosity, the rostral surface of the premaxilla is vertical and slightly concave. The lateral face of the premaxilla gently curves caudolaterally until the maxillopremaxillary suture. The dorsal surface of the bone is weathered; it apparently also gently curves caudodorsally to form the internarial bar. The foramina of the ophthalmic ramus of the fifth cranial nerve (Russell, 1967) are randomly distributed around the rostral tuberosity.

The maxillopremaxillary suture commences 35 mm caudal to the rostral extremity of the premaxilla. It has a sinusoid outline in lateral view. The internarial portion of the premaxilla emerges from a triangular intermaxillary base.

The internarial process of the premaxilla is drop–shaped in transverse cross–section, with an overall height of 8 to 9 mm and a maximal width of 3 mm. The dorsal margin of this process forms a thin, damaged blade.

The premaxillae extend 55 mm further caudally than the caudal extremity of the external nares and are wedged between the paired rostral processes of the frontal. On this caudal portion, the interpremaxillary suture is distinct. At the rostral break of the preserved portion of skull roof, the frontopremaxillary suture commences 20 mm lateral to the midline. On the dorsal surface of the specimen, the frontopremaxillary suture is visible running straight caudally for approximately 45 mm. It then undulates medially and further joins the midline in a gentle caudomedial curve. In ventral view, the caudal–most portion of the frontopremaxillary suture is situated level with its dorsal counterpart. Its rostral continuation on the left side is obscured by matrix and breakage. On the right side it partly appears as a straight, rostrally directed suture 18 to 19 mm lateral to the midline.

The caudal–most portion of the premaxillae is elevated and forms a median crest, which continues for 65 mm onto the frontal. The premaxillae have a median thickness of 7 mm at the rostral break of the specimen. Laterally, the ventral surface of the premaxillae raises dorsolaterally, and the bones are less than 2 mm in height at their lateral margin.

Maxilla (Figure 2). The ventral margin of the dentigerous portion of the maxilla is straight, horizontal. The maxillary canal is visible on the eroded dorsal surface of the left maxilla, with a diameter of approximately 5 mm.

Because of distortion and erosion of the dorsal–most portion of the maxillae in UANL–FCT–R4, the outline of the lateral margin of the naris (the dorsal margin of the maxilla) can only be reconstructed by reversing the medial compression that the dorsal portion of the right maxilla underwent. The naris commences level with the rostral margin or the middle of the fourth maxillary tooth. The height of the maxilla at the level of the caudal termination of the maxillopremaxillary suture could have reached 75 mm. The dorsal margin of the maxilla can be traced until the seventh maxillary tooth. It was gently concave, and the height of the maxilla was approximately 65 mm at the level of the seventh maxillary tooth.

On the right maxilla, the articular facet for the jugal is visible in lateral view. It is semicircular in outline, commencing level with the middle of the 11th maxillary tooth. The facet can be traced until a point approximately 20 mm further caudally.

Frontal (Figure 3). In dorsal aspect, the rostral processes of the frontal wedging the premaxillae are approximately 20 mm wide and contact the prefrontal laterally. The frontoprefrontal suture commences at the caudal–most point of the naris and runs straight caudally. In ventral aspect, these processes are flat and horizontal for most of their width. Laterally they abruptly curve ventrally and form a thin, longitudinally oriented flange. This flange is bordered laterally by a similar flange formed by the medial–most margin of the prefrontal.

In ventral aspect, the frontoprefrontal suture continues caudally straight until the caudomedial corner of the prefrontal (which was originally ventrally covered by the postorbitofrontal: see Preservation and description of the postorbitofrontal). In dorsal aspect, the frontoprefrontal suture curves laterally, and the frontal overlaps the prefrontal. The frontoprefrontal suture then gently curves caudally, and almost parallels the midline for approximately 60 mm, before it curves caudolaterally until the caudolateral break of the prefrontal. There the frontal forms a rounded caudolateral wing overlapping the postorbitofrontal and reaches its maximum width of 190 mm.

The frontoparietal suture commences at the caudal–most extension of the caudolateral wing of the frontal. It describes an arc rostral to the supratemporal fenestra in ventral and dorsal aspects. However, as is visible along the left lateral break of the specimen, the rostral margin of the supratemporal fenestra is formed by a 17 mm long caudal process of the frontal wedged between a 17 mm long dorsal process and a 11 mm long ventral process of the parietal. Therefore the parietal and frontal interdigitate strongly at that level.

Medial to the supratemporal fenestra, a paired caudal process of the frontal overlaps the parietal. The original dimension of this process cannot be determined due to surface weathering. Medial to this process, the frontoparietal suture runs medially until it reaches the midline.

In ventral view the medial portion of the frontoparietal suture is visible at the same level as it is in dorsal view, 140 mm caudal to the frontopremaxillary suture as measured along the midline. The frontoparietal suture undulates laterally for 5 mm on either side of the midline.

The partial impression of the cerebral hemispheres are probably visible as a pair of shallow sulcus at the caudal end of the olfactory tract (see Camp, 1942: 40–42; Russell, 1967: 21). The olfactory bulbs are enclosed laterally by a paired descending flange commencing approximately 50 mm rostral to the frontoparietal suture. This flange runs rostrally, slightly medially, and is vaulted ventromedially, for 30 mm. Its ventral margin is convex. The flange is 3 mm in maximal dorsoventral height when compared to the ventral surface of the frontal lateral to it. Between the flanges, the oflactory tract is 4 mm wide and approximately 5 mm deep.

Postorbitofrontal (Figure 3). In dorsal view, the postor–bitofrontal as preserved is visible only on the right side of the specimen, rostral and caudolateral to the caudolateral wing of the frontal. It forms the rostrolateral corner of the supratemporal fenestra. It was also exposed lateral to this wing, as is suggested by the lateral break of the specimen (see Preservation). Along this longitudinal break, the pa–rietopostorbitofrontal suture is exposed. It runs vertically in a sinusoidal manner, with a rostrocaudal amplitude of 4 mm. In dorsal aspect, the suture emerges from the caudal–most point of the caudolateral wing of the frontal, and runs caudolaterally until the caudal margin of the supratemporal fenestra.

As is visible along the left lateral break of the specimen, a 15 to 20 mm long, 2 mm thick caudal process of the postorbitofrontal ventrally covers the frontoparietal contact.

In ventral aspect, the medial portion of the postorbitofrontal is subrectangular, poorly preserved on the left side, and covered by the jugal and pterygoid on the right. The caudal margin of the postorbitofrontal is formed by the suture with the parietal. This suture runs medially straight, then curves rostrally, forming the caudal 10 mm of the medial margin of the postorbitofrontal. Further rostrally, the medial margin of the postorbitofrontal as preserved contacts the frontal. The frontopostorbitofrontal suture runs slightly rostrolaterally, then rostrally, and finally curves laterally, forming the rostromedial corner of the postorbitofrontal. The suture runs laterally until the lateral break of the specimen.

As is suggested by the weathering pattern of the specimen (see Preservation), the postorbitofrontal was most likely originally in contact with the prefrontal dorsal to the orbit. In ventral aspect, the rostral margin of the right postorbitofrontal is intact, though partly covered by the jugal and the pterygoid. The right postorbitofrontal extends until 80 mm rostral to the frontoparietal suture, and covers the prefrontal ventrally. At the dorsal margin of the orbit, therefore, the prefrontal was wedged between the frontal dorsally and the postorbitofrontal ventrally.

Prefrontal (Figures 2, 3). The original outline of the supraor–bital wing of both prefrontals is only partly preserved, commencing in dorsal aspect at the lateral–most extension of the frontal as preserved, and gently curving rostromedially.

The ventral surface of the caudal half of the prefrontal is subhorizontal and flat, as is its lateral–most portion, which forms the supraorbital wing. The longitudinal ventrolateral flange of the prefrontal originally contacting the maxilla is partly preserved, approximately 60 mm lateral to the midline. This maxillary flange curves medially, and forms the ventrorostrally sloping rostral margin of the orbit, at the level of the middle of the prefrontal as preserved (see Preservation). It then curves rostrally, and contacts the lateral longitudinal flange of the frontal caudal to the naris.

Rostral to the longitudinal preorbital flange, the ventral surface of the prefrontal is flat, horizontal, mostly obscured by matrix on the left side, and weathered on the right one.

The prefrontojugal suture is most likely visible dorsal to the articular facet for the jugal on the right maxilla. It runs dorsorostrally, dorsally convex, for 15 mm, before fading into the eroded dorsal area of the maxilla.

Parietal (Figures 3, 6),. In dorsal aspect, the parietal forms most of the rostral margin of the supratemporal fossa, the postorbitofrontal forming only its lateral corner. The rostral margin of the supratemporal fossa is almost straight and caudomedially oriented until it reaches the intertemporal bar. The lateral margins of the intertemporal bar form a subcircular horizontal table dorsal to the junction with the rostral margin of the supratemporal fossa, 20 mm caudal to the caudal margin of the parietal foramen. The suspensorial ramus of the parietal emerges from the medial margin of the supratemporal fenestra just caudal to that level.

In dorsal view, the parietal foramen is subrectangular, transversely oriented. The middle of its rostral margin is situated 15 mm caudal to the frontoparietal suture.

The ventral aperture of the parietal foramen is longitudinally oval. Its rostral margin slopes ventrorostrally; its caudal margin is subvertical. Its lateral margins are formed by a pair of descending ridges of the parietal. These ridges extend rostrally onto the frontal. Caudal to the caudal margin of the parietal foramen, the flanges abut against the ventrally curving medial portion of the parietal. The lateral faces of the parietal caudal to the parietal foramen strongly curve ventrally and form the descending medial margins of the supratemporal fenestrae.

A triangular area of smooth bone caudal to the parietal foramen is probably the imprint of the peduncle of the pineal organ (see Camp, 1942: 40–42, fig. 24). This smooth area extends 20 mm caudal to the caudal margin of the parietal foramen. It is caudally prolonged by a low, blunt, median ridge for 20 mm. This ridge abruptly terminates as a caudally pointed triangle. Caudal to it, the median surface of the parietal is poorly preserved, but it apparently curves dorsally. A 3 mm long paired ridge bifurcates laterally on either side, from 5 mm caudal to the extremity of the median ridge, and runs caudally parallel to the midline over approximately 5 mm. Both ridges tend to converge toward the caudal extremity of the specimen.

Quadrate (Figure 6). The ventral condyle of the quadrate is drop–shaped in ventral view, tapering medially.

In rostral view, the lateral margin of the quadrate is concave, curving slightly rostrolaterally toward its preserved dorsal margin, and forms the tympanic wing. As is visible along the dorsal break of the quadrate, the tympanic wing at its ventral base was about 1 mm thick.

The rostromedial margin of the quadrate is dorsola–terally oriented. In medial view, this rostromedial margin consists of a 2 mm thick ridge. A sulcus separates it from a caudomedial process of the quadrate shaft, which forms the caudomedial margin of the quadrate. Seen from caudally, this process merges caudolaterally with the infrastapedial process.

The dorsolateral margin of the infrastapedial process rises mediodorsally and is straight until the level of the middle of the ventral condyle. From there, the dorsal margin of the infrastapedial process forms a transversely flat surface, inclined caudally at an angle of about 40°. Medial to this surface, the infrastapedial process merges with the caudomedial process of the quadrate shaft. The ventral–most extremity of the suprastapedial process is preserved in close proximity, but is separated by 1 to 2 mm of sediment from the infrastapedial process and the caudomedial process of the quadrate shaft.

Jugal (Figures 2, 3). The median portion of the left jugal is preserved in medial view. The preserved portion of the horizontal rostral ramus is 100 mm long, the preserved portion of the ascending dorsal ramus, 40 mm long. They form a 90° angle to one another. The rostral ramus is 20 mm high, 10 mm wide. It is drop–shaped in cross–section, its dorsal margin converging into a ridge, possibly due to compaction and weathering. In cross–section the dorsal ramus is subtriangular, with a maximal rostral width of 8 mm, and a length of 20 mm. Its medial margin abruptly curves laterally at the junction with the horizontal rostral ramus and forms a 7 to 9 mm wide tuberosity. Further details are not preserved, or are distorted in such a way that an interpretation would be unreliable.

Pterygoid (Figures 3, 5). The caudal, quadrate process of the pterygoid is oval in cross–section, and dorsoventrally compressed. Neither its height nor its width can be determined with certainty. The medial process, caudally terminating the pterygoid tooth row, is 10 mm wide, emerging at a right angle from the quadrate process. The isolated portion of pterygoid is L–shaped. As it is preserved, it bears five tooth positions.

As for the jugal, the poor preservation of the bones, one having been pressed against the skull roof and the second extensively weathered, prevents further description.

Vomer (Figure 2). In ventral view the surface of both vom–ers is horizontal laterally, and presents a medial crest until level with the third maxillary tooth. Further rostrally, the lateral margin of the right vomer curves medially, forming the opening for Jacobson's organ, which extends from possibly the rostral margin of the third maxillary tooth to the rostral margin of the fourth maxillary tooth.

In dorsal view, both vomers are flat, horizontal, 15 mm wide bones. The thickness of the bones at their caudal break is 2 mm.

Anterior lower jaw (Figures 4, 7)

Dentary. The dentary originally covered the splenial vent–rolaterally to form the ventral margin of the anterior lower jaw, rostral to the penultimate (as preserved) dentary tooth (see Preservation). As preserved, the ventral margin of the anterior lower jaw is straight, but it cannot be confirmed that it was so originally.

The dorsal margin of the dentary is gently concave. The lateral face is weathered, though it must have been convex rostral to the penultimate (as preserved) dentary tooth. Caudally the lateral face of the dentary becomes vertical and straight. The right dentary has a height of 110 mm at its caudal end and a maximum width of 25 mm. It widens rostrally to 30 mm with a decrease in height to 55 mm.

A shallow sulcus extends from the caudodorsal corner of the lateral surface of the dentary, directed rostroventrally until a point 15 mm ventral to the caudal extremity of the caudal–most preserved tooth. This lateral sulcus appears to have a medial counterpart that runs from the caudodorsal corner of the dentary to the alveolus of the caudal–most preserved tooth. These sulcus might represent the facets for the coronoid.

The anterior inferior alveolar foramen opens at the level of the caudal margin of the fifth (as preserved) dentary tooth, and extends to the level of the rostral margin of the seventh (as preserved) dentary tooth. Its ventral margin is concave, formed by the splenial, while its dorsal margin is straight and formed by the dentary. It is likely, though, because of the extensive weathering, that it was originally smaller and that its original outlines are not preserved.

As visible in cross–section along a break running in the middle of the fourth preserved dentary tooth, the ventrolateral descending flange of the dentary sends a hook medially into the Meckelian canal. This hook houses an inverted hook sent ventrolaterally by the dorsal part of the dentary. Rostrally, as visible on the rostral extremity of the specimen, these hooks become peduncles with flat, respectively dorsal and ventral faces. These peduncles might have been in contact with these flat faces, which would imply that the specimen underwent some lateral distortion. Caudally, only the ventrolateral descending flange sends a thin hook inside the Meckelian canal.

As visible along the same break, the dorsal part of the dentary sends a ventromedial flange forming the mediodorsal corner of the Meckelian canal. This hook is covered medially by the splenial.

Splenial. The splenial forms the ventral half of the medial surface of the anterior lower jaw. Its ventral margin is straight as preserved (see Preservation).

At the rostral break of the specimen, the ventral contact with the dentary is vertical in cross–section. Level with the fourth preserved dentary tooth, the ventral contact with the dentary is of a tongue–and–groove kind. There the splenial wraps the rounded ventral margin of the dentary. A 15 mm high lateral ascending process of the splenial covers the medial face of the ventral descending flange of the dentary, and thus forms the lateral wall of the Meckelian canal. At the caudal break of the specimen, this process reaches 35 mm in height. There the contact with the dentary is subvertical, curving laterally only in its ventral–most portion.

Prearticular. The prearticular is visible along the break level with the fourth preserved dentary tooth, as a vertical lamella of bone sitting inside the Meckelian canal. At the caudal break of the specimen, it covers the medial portion of the splenial laterally. The prearticular thus forms the medial margin of the Meckelian canal.

Surangular. The surangular is exposed in lateral view between the dentary and the prearticular at the caudal–most portion of the specimen, maybe due to surface weathering. It is visible as well at the caudal break of the specimen, dorsal to the prearticular. It is subcircular in cross–section, with a concave ventral margin.

Dentition (Figures 2, 4, 5, 7). There are two tooth positions on each premaxilla, twelve on the right maxilla, and eleven on the left one. According to the position of the last preserved right maxillary tooth (situated 40 mm caudal to the rostral–most point of the articular facet for the jugal), and to the estimated tooth diameter, no more than two teeth are missing caudally, if any. Therefore, the number of teeth per upper jaw ramus is estimated at 14 to 16. Nine tooth positions are documented on each dentary. The number of missing dentary teeth might be two to five, according to the estimated length of the tooth row of the upper jaw.

Because of the broken tooth crowns, the ontogenetic condition of the teeth and therefore the actual diameter of the functional upper teeth are difficult to assess. The upper dentition shows a slight anisodonty, as the two premaxillary and the rostral–most two maxillary crown bases have a ros–trocaudal length of 10 to 12 mm, compared to the estimated basal length of 15 to 17 mm of the more caudally situated maxillary tooth crowns.

All dentary tooth crowns as preserved (i.e., without enamel coverage, and with the apices of functional teeth broken or abraded) have a basal mesiodistal length of 16 to 18 mm, and a height of 22 to 25 mm.

The preserved tooth crowns, most of them being of non–erupted replacement teeth, are slightly and gently curved caudally and medially, with a subcircular basal cross–section. Two mesially and distally aligned carinae divide the crown until the apex into two equal halves, and the cross–section becomes slightly oval apically. The crown gently tapers until 3 to 4 mm below its apex. Then the surface tapers more abruptly and forms a blunt conical apex. Where preserved, the enamel surface is smooth.

The better preserved pterygoid tooth documents a tooth that was at least 20 mm high, slightly more massive than any of the mandibular teeth, and with a sharper apex.


Rostral extension of the frontal, individual age of the specimen. The transverse line visible on the dorsal surface of the frontal (see Preservation; Figure 3) could be a break, although due to its symmetry it much resembles a suture.

If this line is actually a suture, assuming that it marks the rostral extremity of the frontal would mean that another bone, forming partly the medial margin of the naris, surrounds the caudal–most portion of the premaxilla and overlaps the prefrontal laterally. This bone could be part of the maxilla, only if it is assumed that the maxilla forms the internarial bar together with the premaxilla. Such an anatomy has never been observed in any mosasaur (Romer, 1956; Russell, 1967).

Especially because this bone is located medial to the naris, it could also represent the nasal. However, nasals are rarely preserved in mosasaurs (Russell, 1967: 18; Bell, 1997b: 302). If they are, they are reduced in size and situated lateral to the internarial bar, their caudal extremity articulating with the rostral extremity of the frontal (Camp, 1942: 27–28, fig. 14). Regardless of whether nasals in mosasaurs are fused with the frontal or the premaxilla in some taxa, or missing due to a loose connection with the internarial bar in others, as discussed by Camp (1942: 28), it appears highly unlikely that they can form such a well–expressed caudal process as is seen in UANL–FCT–R4.

Another hypothesis is that this structure represents a supernumerary bone (or wormian bone, Gray, 1901: 49–50), which appears as unlikely as the preceding hypotheses, because the bone in UANL–FCT–R4 is overlapping the prefrontal, instead of growing between two bones as would be the case for a supernumerary bone (Gray, 1901; Piveteau, 1954).

A septomaxilla has never been reported for mosas–aurs, and no other dermal bone exists in their rostrofrontal area. Therefore, if this line is a suture, it has to be a suture within the frontal itself. Such an intrafrontal suture could be either pathological, due to a break early in ontogeny. It could also mark the unossified contact of two ossification centres (Gray, 1901; Piveteau, 1954; Romer, 1956). In that latter case, the specimen would be a juvenile, as is also suggested by the presence of an interpremaxillary suture, for in mosasaurs the premaxillae are normally "co–ossified with no indication of a suture" (Russell, 1967: 14). Even if the interpremaxillary suture of UANL–FCT–R4 is exposed in dorsal view only due to surface weathering, it indicates that the fusion of the premaxillae proceeds in a caudal direction during ontogeny, as no interpremaxillary suture is visible on the eroded dorsomedial area of the rostral–most part of the premaxilla. Under the hypothesis of a juvenile animal, the unfused but almost contacting infra– and suprastapedial processes of the quadrate could also be related to young individual age.

Comparative palaeontology. Mosasaurinae, Plioplatecar–pinae andTylosaurinae were characterised by Russell (1967) by features of the opisthotic and basioccipital, and of the postcranial skeleton. These elements are missing in UANL–FCT–R4. Subsequent studies (Wright and Shannon, 1988; Lingham–Soliar, 1992; De Braga and Carroll, 1993) could not define other diagnostic characters of the subfamilies that would allow the identification of UANL–FCT–R4 to subfamilial level. The re–assessment of the relationships among Mosasauridae proposed by Bell (1997b) is of little help, due to the inadequate preservation of UANL–FCT–R4. The few characters defined by Bell (1997b), whose states can be determined in UANL–FCT–R4, yield contradictory results. For example, the large supraorbital process of the prefrontal and the coincidence between the caudal termination of the naris and the rostral termination of the frontoprefrontal suture would place UANL–FCT–R4 within Mosasaurinae. However, the triangular ventrally inflated 'boss' (Bell, 1997b: 305) on the frontal caudal to the olfactory tract, as is seen on UANL–FCT–R4, is one of the unambiguous derived characters of the "Russellosaurinae", new subfamily informally introduced by Bell (1997b; see Bell and Polcyn, 2005) in order to accommodate Tylosaurus and the members of the tribe Plioplatecarpini. However, the genus Hainosaurus, the other member of the subfamily Tylosaurinae sensu Russell, 1967, was not included in Bell's analysis (1997b). Therefore the status of the subfamily remains uncertain under this phylogenetical hypothesis.

Due to its preservation status, UANL–FCT–R4 cannot be referred per se to any of the subfamilies or tribes of the family Mosasauridae.

UANL–FCT–R4 is excluded a priori from the Tylosaurinae sensu Russell (1967) because it lacks a predental premaxillary rostrum. However, it is similar to Tylosaurus in the extension of the premaxillae caudal to the naris and the contact between the prefrontal and the postorbitofrontal lateral to the orbit (Russell, 1967; Everhart, 2005). The rostral tuberosity of the premaxilla in UANL–FCT–R4 and the arrangement of foramina on the rostrodorsal surface of this bone around the tuberosity, are very similar to what is described for Tylosaurus by Russell (1967: 16), but the tuberosity of UANL–FCT–R4 is situated more dorsally.

The morphology of the quadrate clearly excludes UANL–FCT–R4 from both Tylosaurus and Hainosaurus. The infra– and suprastapedial processes of the quadrate of UANL–FCT–R4 are almost in contact, while in Tylosaurus and Hainosaurus the suprastapedial process is not expanded ventrally, and never contacts the reduced infrastapedial process (Russell, 1967; Nicholls, 1988; Lingham–Soliar, 1992; Everhart, 2005).

Among mosasaurs evincing a contact between infra– and suprastapedial processes or processes almost in contact is the plioplatecarpine Selmasaurus (Wright and Shannon, 1988). However, Selmasaurus lacks an inter–temporal table, has a longitudinally oval parietal foramen in dorsal aspect, and the caudolateral wings of its frontal are triangular (Wright and Shannon, 1988, fig. 1). Only in Clidastes propython does the suprastapedial process contact the infrastapedial process and a crest emerging from the quadrate shaft (Russell, 1967; Wright and Shannon, 1988), as in UANL–FCT–R4. Still, UANL–FCT–R4 is excluded from the genus Clidastes in having a more massive and probably more brevirostrine skull, as far as can be judged from what is preserved, and 12 to 14 maxillary and 11 to 14 dentary teeth while Clidastes has 16 to 18 maxillary and dentary teeth (Russell, 1967, 1975). UANL–FCT–R4 also differs from members of the genus Clidastes in having a maxillopremaxillary suture sinusoidal in lateral view, the rostral extremity of the naris situated between the third and fourth maxillary teeth, a subcircular intertemporal table, and a dorsally exposed contact between the prefrontal and the postorbitofrontal lateral to the frontal (Merriam, 1894; Russell, 1967).

The infra– and suprastapedial processes of the quadrate are fused in Globidens, Prognathodon, Plesiotylosaurus and Ectenosaurus (Russell, 1967, 1975; Wright and Shannon, 1988). The latter genus is a very longirostrine plioplatecarpine, sharing with U ANL–FCT–R4 only the thin tympanic wing of their quadrates, and the position of the rostral termination of the naris level with the third maxillary tooth (Russell, 1967: 158). No similarity can be observed between the quadrate of UANL–FCT–R4 and the same bone in Plesiotylosaurus as illustrated by Camp (1942, fig. 11). Globidens has a very massive skull and characteristic low bulbous teeth (Russell, 1975), which are clearly distinct from what is known of UANL–FCT–R4. However, in Globidens too, the prefrontal and postorbitofrontal exclude the frontal from the dorsolateral margin of the orbit. Prognathodon, traditionally considered a plioplatecarpine mosasaur (Russell, 1967), was reassigned by Bell (1997b; see also Bell and Polcyn, 2005) to the tribe Globidensini of the subfamilly Mosasaurinae, together with Globidens and Plesiotylosaurus. This relationship is supported by the fusion of the infra– and suprastapedial processes in these three genera, which is considered convergent in Ectenosaurus. However, UANL–FCT–R4 differs from known members of the genus Prognathodon as diagnosed by Lingham–Soliar and Nolf (1989) in the exposed contact of the prefrontal and postorbitofrontal lateral to the frontal, the subcircular inter–temporal table, and the thin tympanic wing of the quadrate. The sinusoidal maxillopremaxillary suture, and the rounded caudolateral wings of the frontal are also unknown in the genus Prognathodon (Russell, 1967; Welles and Gregg, 1971; Lingham–Soliar and Nolf, 1989).

UANL–FCT–R4 therefore cannot be confidently assigned to any of the previously described taxa sharing with it the close contact (or possibly fusion in adults) of the infra– and suprastapedial processes of their quadrates; the remainder of its skull anatomy yields no further hint at its affinities.



UANL–FCT–R4 is the first substantially documented mosasaur from north–east Mexico and combines features known from genera assigned to different subfamilies. Although it comprises an almost complete skull roof, muzzle and anterior mandibular units, and partial quadrate and jugal, allowing us to draw a reconstruction of its skull (Figure 8), its affinities with other mosasaurs cannot be determined with confidence. This is partly linked with the inadequacy of its preservation compared to claimed taxonomically significant features in mosasaurs, but also we shall argue, with the poor understanding of the biological meaning of these features, not to mention the debatable, current, almost exclusive cladistic approach to phylogeny (see e.g. Vermeij, 1999; Pavlinov, 2003; Hawks, 2004).

As an example, the skull architecture of UANL–FCT–R4 is similar to that of Globidens (Russell, 1975), if not taking into account the massiveness of the skull in the latter genus, and differs from that of Prognathodon (Lingham–Soliar and Nolf, 1989). The skull architecture of Globidens is considered as related to its massiveness and low bulbous teeth, allowing the animal to feed on hard–shelled prey (Russell, 1967, 1975; Schulp, 2005). Interpreting the anatomy of Globidens as a consequence of the feeding strategy having no taxonomical meaning above the genus level, allowed Bell (1997b) to relate it to Prognathodon.

Under this phylogenetic hypothesis of a close relationship between Prognathodon and Globidens, the skull architecture (e.g. the contact between the prefrontal and postorbitofrontal lateral to the frontal, absent in Prognathodon, and extensive in Globidens) is insignificant compared to the fusion of the infra– and suprastapedial processes. We would argue that the fusion of the processes in Globidens can also be linked with the massiveness of the skull. It would appear more taxonomically significant that these processes are also fused inEctenosaurus, having a very longirostrine and slender skull. However, in the most parsimonious tree of Bell (1997b), the fused processes of this taxon are assumed to be convergent. In order to test this hypothesis and judge the plausibility of such convergence, a functional analysis of the features considered would be essential in order to reconstruct the evolutionary pathway.

Similarly, the rostral tuberosity and the random arrangement of the foramina on the premaxilla, if regarded as linked with the anatomy of the cranial nerve V, is in our opinion more phylogenetically significant than the predental rostrum itself. The arrangement of these foramina probably reflects the anatomy of the nerve. The predental rostrum of Tylosaurus could easily be derived from a condition similar to that seen in UANL–FCT–R4 by a rostrodorsal growth of the premaxilla, keeping the internal pattern of the divisions of the cranial nerve. This was already implicitly recognized by Russell (1967), who described a predental rostrum in the mosasaurines Clidastes and Mosasaurus and the plioplatecarpine Ectenosaurus, though exhibiting a paired row of foramina. Moreover, the caudal retreat of the frontopremaxillary suture reinforces the internal bar by placing its inferred weakest point inside the skull roof table (Lingham–Soliar, 1992). UANL–FCT–R4 shares both features with Tylosaurus, despite its lacking the classical, tylosaurine type of predental rostrum. The suggested function of this rostrum is linked with the predatory strategy of the animal (or breeding behaviour), as was discussed by Russell (1967) and Lingham–Soliar (1992). The importance given to this predental rostrum in the diagnosis of the subfamily by Russell (1967: 170; this diagnosis is the latest available for the subfamily, as Bell, 1997b, did not consider all members of it, see above and Bell and Polcyn, 2005), compared to its suggested function, appears disproportionate, especially if the modifications linked with the same function in Globidens, but affecting the entire skull, only diagnose the genus.

We cannot place UANL–FCT–R4 within the phyloge–netical frame currently hypothesised for mosasaurs. Within this frame, its anatomy indicates conflicting affinities, and we do not feel that we possess convincing, biologically supported arguments to define, which one is the better supported. Following Herkner (1999) and Salisbury (2001), we suggest that an analysis focusing on the constructional aspects of the structures resulting in the reconstruction of an evolutionary pathway should greatly help clarifying mosasaurs' systematics, and in peculiar, the affinities of UANL–FCT–R4.



The authors warmly thank Sr. Gustavo Barbosa Navéjar, Ing. Sigifredo Navéjar Torres, and Sr. Alberto Navéjar Ruiz, who discovered and collected the specimen, and transferred it to the UANL–FCT. Special thanks go to M.P. Pedro Rodríguez Saavedra (UANL–FCT), Stefan Unrein (University of Karlsruhe) and René Kastner (Staatliches Museum für Naturkunde Karlsruhe) for preparation. This manuscript was kindly improved by the excellent J. Listón (Glasgow), and it or extracts benefited from comments by M. Caldwell (Edmonton), R. Holmes (Ottawa), E.W.A. Mulder (Maastricht) and other participants of the 1st Mosameeting (Maastricht, 2004); it owes a great deal to K. T. Smith (Yale). I. Ferrusquía–Villafranca and V. H. Reynoso (Mexico City) were thorough reviewers. J.G.L.O. thanks the Instituto Nacional de Antropología y Historia, Monterrey, for support. This research was financially supported by the Deutsche Forschungsgemeinschaft (grants number FR 1314/4–1, FR 1314/6–1, FR 1314/9–1 and 9–2).



Aranda–Manteca, F., Stinnesbeck, W., 1993, Primer registro de mosasauridos en Mexico: Universidad Autónoma de Nuevo León, Actas de la Facultad de Ciencias de la Tierra, 8, 1–8.        [ Links ]

Bell, G.L., 1997a, Introduction to Part IV, Mosasauridae, in Callaway, J.M., Nicholls, E.L. (eds.), Ancient Marine Reptiles: San Diego, USA, Academic Press, 281–292.        [ Links ]

Bell, G.L., 1997b, Aphylogenetic revision of North American and Adriatic Mosasauroidea, in Callaway, J.M., Nicholls, E.L. (eds.), Ancient Marine Reptiles: San Diego, USA, Academic Press, 293–332.        [ Links ]

Bell, G.L., Polcyn, M.J., 2005, Dallasaurus turneri, a new primitive mosasauroid from the Middle Turonian of Texas and comments on the phylogeny of Mosasauridae (Squamata): Netherlands Journal of Geosciences, 84, 177–194.        [ Links ]

Buchy, M.C., Smith, K.T., Frey, E., Stinnesbeck, W., González González, A.H., Ifrim, C., López Oliva, J.G., Poras–Muzquiz, H., 2005, Annotated catalogue of marine squamates (Reptilia) from the Upper Cretaceous of northeastern Mexico: Netherlands Journal of Geosciences, 84, 195–205.        [ Links ]

Caldwell, M.W., Carroll, R.L., Kaiser, H., 1995, The pectoral girdle and forelimb of Carsosaurus marchesetti (Aigialosauridae), with a preliminary phylogenetic analysis of Mosasauroids and Varanoids: Journal of Vertebrate Paleontology, 15(3), 516–531.        [ Links ]

Camp, C.L., 1942, California mosasaurs: Memoirs of the University of California, 13, 1–68.        [ Links ]

De Braga, M., Carroll, R.L., 1993, The origin of mosasaurs as a model of macroevolutionary patterns and processes: Evolutionary Biology, 27, 245–322.        [ Links ]

Dollo, L., 1904, Les Mosasauriens de la Belgique: Bulletin de la Société belge de Géologie, Paléontologie et Hydrologie, Mémoires, 18, 207–216.        [ Links ]

Dollo, L., 1913, Globidens fraasi, mosasaurien mylodonte nouveau du Maastrichtien (Crétacé supérieur) du Limbourg, et l'éthologie de la nutrition chez les mosasaures: Archives de Biologie, 28, 609–626.        [ Links ]

Evans, S. E., Manabe, M., Noro, M., Isaji, S., Yamaguchi, M., 2006, A long–bodied lizard from the Lower Cretaceous of Japan: Palaeontology, 49,1143–1165.        [ Links ]

Everhart, M.J., 2005, Tylosaurus kansasensis, a new species of tylosaurine (Squamata, Mosasauridae) from the Niobrara Chalk of western Kansas, USA: Netherlands Journal of Geosciences, 84, 231–240.        [ Links ]

Gervais, P., 1853, Observations relatives aux reptiles fossiles de France: Comptes rendus de l'Académie des Sciences de Paris, 36, 374–377, 470–474.        [ Links ]

Gray, H., 1901, Anatomy descriptive and surgical: New York, Barnes and Noble, 15th edition, 1096 p.        [ Links ]

Hawks, J., 2004, How much can cladistics tell us about early hominid relationships?: American journal of physical anthropology, 125, 207–219.        [ Links ]

Herkner, B., 1999, Über die evolutionäre Entstehung des Tetrapodenlok omotionsapparates der Landwirbeltiere. Ein konstruktionsmorphologisches Transformationsmodell auf evolutionstheoretischer Grundlage: Carolinea Beihefte, 13, 1–353.        [ Links ]

Ifrim, C., Stinnesbeck, W., López–Oliva, J.G., 2004, Maastrichtian cephalopods from the Méndez Formation at Cerralvo, Nuevo León, northeastern Mexico: Palaeontology, 47: 1575–1627.        [ Links ]

Keller, G., López–Oliva, J.G., Stinnesbeck, W., Adatte, T., 1997, Age, stratigraphy and deposition of near K/T siliciclastic deposits in Mexico: Relation to bolide impact?: Geological Society of America Bulletin, 109, 410–428.        [ Links ]

Keller, G., Adatte, T., Stinnesbeck, W., Affolter, M., Schilli, L., López–Oliva, J.–G., 2002, Multiple spherule layers in the late Maastrichtian of northeastern Mexico: Geological Society of America Special Paper, 356, 145–161.        [ Links ]

Li, L., Keller, G., 1998, Maastrichtian climate, productivity and faunal turnovers in planctic foraminifera on South Atlantic DSDP sites 525Aand 21: Marine Micropaleontology, 33, 55–86.        [ Links ]

Lingham–Soliar, T., 1992, The Tylosaurine mosasaurs (Reptilia, Mosasauridae) from the Upper Cretaceous of Europe and Africa: Bulletin de l'Institut Royal des Sciences naturelles de Belgique, Sciences de la Terre, 62, 171–194.        [ Links ]

Lingham–Soliar, T., 1994, The mosasaur Plioplatecarpus (Reptilia, Mosasauridae) from the Upper Cretaceous of Europe: Bulletin de l'Institut Royal des Sciences naturelles de Belgique, Sciences de la Terre, 64, 177–211.        [ Links ]

Lingham–Soliar, T., 1995, Anatomy and functional morphology of the largest marine reptile known, Mosasaurus hoffmanni (Mosasauridae, Reptilia) from the Upper Cretaceous, Upper Maastrichtian of the Netherlands: Philosophical Transactions of the Royal Society of London, B, 347, 155–180.        [ Links ]

Lingham–Soliar, T., Nolf, D., 1989, The mosasaur Prognathodon (Reptilia, Mosasauridae) from the Upper Cretaceous of Belgium: Bulletin de l'Institut Royal des Sciences naturelles de Belgique, Sciences de la Terre, 59, 137–190.        [ Links ]

Mehl, M.G., 1930, A new genus of mosasaurs from Mexico, and notes on the pelvic girdle of Platecarpus: Denison University, Journal of the Scientific Laboratories, 24, 383–400.        [ Links ]

Merriam, J.C., 1894, Über die Pythonomorphen der Kansas–Kreide: Palaeontographica, 41, 1–39.        [ Links ]

Nicholls, E.L., 1988, The first record of the mosasaur Hainosaurus (Reptilia: Lacertilia) from North America: Canadian Journal of Earth Sciences, 29, 1564–1570.        [ Links ]

Oppel, M., 1811, Die Ordnungen, Familien, und Gattungen der Reptilien als Prodrom einer Naturgeschichte derselben: Munchen, Lindauer, xii + 86 p.        [ Links ]

Pavlinov, I.Y., 2003, The new phylogenetics: an essay: Wulfenia, 10, 1–14.        [ Links ]

Piveteau, J., 1954, Le problème du crâne, in Grassé, P.P. (ed.), Traité de Zoologie, tome XII: Paris, Masson, 1145 p.        [ Links ]

Romer A.S., 1956, Osteology of the reptiles: Chicago, University of Chicago Press, 772 p.        [ Links ]

Russell, D. A., 1967, Systematics and morphology of American Mosasaurs (Reptilia, Sauria): Peabody Museum of Natural History, Yale University, Bulletin, 23, 1–241.        [ Links ]

Russell, D.A., 1975, A new species of Globidens from South Dakota, and a review of Globidentine mosasaurs: Fieldiana Geology, 33 (13), 235–256.        [ Links ]

Salisbury, S.W., 2001, A biomechanical transformation model for the evolution of the eusuchian–type bracing system: Sydney, Australia, University of New South Wales, unpublished PhD thesis, 554pp.        [ Links ]

Schulp, A.S., 2005, Feedingthe mechanical mosasaur: what did Carinodens eat?: Netherlands Journal of Geosciences, 84, 345–358.        [ Links ]

Sohl, N.F, Martínez, R.E., Salmerón–Ureña, P., Soto–Jaramillo, F., 1991, Upper Cretaceous, in Salvador, A. (ed.), The Gulf of Mexico Basin: Boulder, Colorado, Geological Society of America, The Geology of North America, Volume J, 205–215.        [ Links ]

Stinnesbeck, W., Schulte, P., Lindenmaier, F., Adatte, T., Affolter, M., Schilli, L., Stüben, D., Berner, Z., Kramar, U., López–Oliva, J.G., 2001, Late Maastrichtian age of spherule deposits in northeastern Mexico: Implication for Chicxulub scenario: Canadian Journal of Earth Sciences, 38, 229–238.        [ Links ]

Tantawy, A. A., Keller, G., Adatte, T., Stinnesbeck, W., Kassab, A., Schulte, P., 2001, Maastrichtian to Paleocene depositional environment of the Dakhla Formation, Western Desert, Egypt: sedimentology, mineralogy, and integrated micro –and macrofossil biostratigraphies: Cretaceous Research, 22, 795–827.        [ Links ]

Vermeij, G.J., 1999, A serious matter with character–taxon matrices: Paleobiology, 25, 431–433.        [ Links ]

Welles, S.P., Gregg, D.R., 1971, Late Cretaceous marine reptiles of New Zealand: Records of the Canterbury Museum, 9(1), 1–111.        [ Links ]

Williston, S.W., 1895, New or little–known extinct vertebrates: Kansas University Quarterly, 3, 165–176.        [ Links ]

Williston, S.W., 1897, Range and distribution of the mosasaurs: Kansas University Quarterly, 6, 177–189.        [ Links ]

Williston, S.W., 1898, Mosasaurs: University Geological Survey of Kansas, 4, 83–221.        [ Links ]

Wright, K.R., Shannon, S.W., 1988, Selmasarus russelli, a new plioplatecarpine mosasaur (Squamata, Mosasauridae) from Alabama: Journal of Vertebrate Paleontology, 8 (1), 102–107.        [ Links ]

Zaher, H., Rieppel, O., 1999, Tooth implantation and replacement in squamates, with special reference to mosasaur lizards and snakes: American Museum of Natural History Novitates, 3271, 1–19.        [ Links ]

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