taxonID	type	description	language	source
F75787E0FF9BFFC80251042180C7BE2E.taxon	description	ATOPOSAURUS VON MEYER, 1850 Included species Atoposaurus jourdani (type species, named first in von Meyer, 1850) and Atoposaurus oberndorferi. Distribution Late Jurassic of southern France and south-east Germany. Previous diagnoses and comments Both species of Atoposaurus were named by von Meyer (1850), with Atoposaurus jourdani receiving a full description by von Meyer (1851). Wellnhofer (1971) was the first to present a diagnosis for Atoposaurus based on the specimens from France and Germany, noting the lack of dermal armour, a feature that could be related to either ontogeny or taphonomy (Schwarz & Salisbury, 2005). Subsequently, Atoposaurus and its constituent species have largely been considered to be nomina dubia, and often regarded as juvenile representatives of Alligatorellus and / or Alligatorium (e. g. Clark, 1986; Buscalioni & Sanz, 1988). Clark (1986) considered Alligatorellus, Alligatorium, and Atoposaurus to be the same taxon represented by different growth stages. If this were the case, then Atoposaurus von Meyer, 1850; would retain priority, and Alligatorium Jourdan, 1862, along with Alligatorellus Gervais, 1871, would be synonymized with Atoposaurus. Almost all subsequent phylogenetic analyses have included just Alligatorium based on this conclusion, without consideration of the other taxa. The present analysis is the first to consider both potential species of Atoposaurus as independent OTUs, and finds them to be sister taxa in all cases (Figs 4 – 7), thus supporting their generic assignment. Despite noting the same features in Alligatorellus, Wellnhofer (1971; see also Steel, 1973) stated that the presence of large orbits, a closed internal supratemporal fenestra, and divided external nares were all features defining Atoposaurus. The presence of an inwardly displaced postorbital bar (Steel, 1973) is not clear owing to the preservation of available specimens of Atoposaurus oberndorferi, but does appear to be a feature of Atoposaurus jourdani. Four of the five synapomorphies that we identify for Atoposaurus (S 1 – 3, S 5) are contentious as they could be indicative of a juvenile phase of growth (e. g. Joffe, 1967), but equally probably they could represent the retention of juvenile characteristics through paedomorphism related to the relatively small body size of Atoposaurus. Unfortunately, based on currently available specimens, it is impossible to distinguish between these two hypotheses (Tennant & Mannion, 2014). Revised diagnosis and discussion (S 1) Dorsal cranial bones comprising the skull roof unsculpted (C 1.0): This lack of dermal sculpting, combined with their overall diminutive size, indicates that Atoposaurus specimens might be represented by juveniles. However, it cannot be definitively confirmed that Atoposaurus is a juvenile representative of other contemporaneous atoposaurids based on allometric growth patterns alone (Tennant & Mannion, 2014), and it is likely that Atoposaurus, Alligatorellus, and Alligatorium represent three distinct genera, as our results indicate (Figs 4 – 7). (S 2) External surface of snout unsculpted (C 3.0): We consider this to be a distinct feature from S 1, as in Alligatorellus there is a different pattern of sculpting between the cranial table and the rostrum. Atoposaurus is similar to Alligatorellus in this respect, completely lacking any evidence of cranial ornamentation, although this cannot be assessed properly in Atoposaurus oberndorferi owing to the mode of preservation of the holotype specimen. As with S 1, this character is likely to be highly influenced by either ontogeny or paedomorphism (Joffe, 1967). (S 3) Skull anteroposterior length to orbit length ratio <3.0 (C 27.0): This feature is unique to Atoposaurus, and represents the characteristic proportionally large orbits and short snout of this taxon, noted by Joffe (1967) to be indicative of a juvenile status. Other atoposaurids have a ratio of between 3.0 and 4.0. Karatausuchus has a ratio of 3.36, slightly higher than Alligatorellus bavaricus (3.12), which approaches the state boundary for Atoposaurus, but it is likely that Karatausuchus represents a juvenile specimen of a (probably non-atoposaurid) crocodyliform (Storrs & Efimov, 2000; see below). (S 4) 50 or more caudal vertebrae (C 276.1): Complete axial columns are rarely preserved in specimens previously assigned to Atoposauridae, and the proportional numbers of cervical, dorsal, sacral, and caudal vertebrae remain poorly known, especially for Theriosuchus. Both species of Alligatorellus preserve complete and articulated caudal vertebral series, and have 40 vertebrae each. Montsecosuchus appears to only have 21 caudal vertebrae, and Pachycheilosuchus has just 18 (Rogers, 2003). Protosuchus richardsoni has 39 caudal vertebrae, and Karatausuchus has 46 (Storrs & Efimov, 2000), approaching the number for Atoposaurus, but no other crocodyliform taxon has 50 vertebrae. The presence of 50 or more caudal vertebrae, in all specimens of Atoposaurus in which this feature can be measured, is not known in any other mesoeucrocodylian taxon, and cannot be explained by ontogeny (Tennant & Mannion, 2014); therefore, we regard it as a diagnostic feature for Atoposaurus, irrespective of the ontogenetic stage of the specimens, and therefore consider Atoposaurus to be a valid taxon. (S 5) Osteoderms absent: The lack of osteoderms is unlikely to be a taphonomic artefact (contra Schwarz-Wings et al., 2011), and is either a feature associated with extreme dwarfism in Atoposaurus, or relates to their lack of development in juvenile individuals. The only other putative atoposaurid that is similar in this respect is Karatausuchus, which Storrs & Efimov (2000) described as having reduced dermal ossicles. ATOPOSAURUS JOURDANI VON MEYER, 1850 (TYPE SPECIES) Type locality and horizon Unknown bed, Kimmeridgian (Late Jurassic); Cerin, Ain, France. Type specimen MHNL 15679, articulated partial skeleton comprising dorsally flattened skeleton and skull, missing the posterior-most caudal vertebrae, with distal hindlimbs and distal left forearm preserved as impressions. Referred specimen MHNL 15680 (same locality as type specimen), posterior half of articulated skeleton, including trunk vertebrae and forearms. Previous diagnoses and comments von Meyer (1851) named Atoposaurus jourdani, and described this taxon in a subsequent paper (von Meyer, 1851). We find that a unique combination of metric characters, almost exclusively regarding the relative proportions of the forelimb and hindlimb elements, can be used to distinguish this taxon from Atoposaurus oberndorferi, along with a single autapomorphy. Revised diagnosis and discussion (S 1) Skull mediolateral width to orbit width ratio of 1.80 (C 28.0): This represents the lowest ratio for all atoposaurids, demonstrating that the orbits comprise almost the entire mediolateral width of the skull, separated by the narrow frontals. This is similar to Alligatorellus bavaricus, which also has enlarged orbits, but slightly mediolaterally wider frontals between the orbits (Tennant & Mannion, 2014). (S 2 *) Six cervical vertebrae (C 266.0): This character state is unique amongst all putative atoposaurids, with all others possessing seven cervical vertebrae. We were unable to determine this character state for any specimens assigned to Theriosuchus owing to their preservation and / or incompleteness. This cervical count is distinct from Protosuchus richardsoni (nine) and Hoplosuchus (11), as well as Karatausuchus (eight; Storrs & Efimov, 2000) (Table 2). (S 3) Forelimb length to hindlimb length ratio of 0.63 (C 285.0): This character state is similar to Protosuchus richardsoni (0.65) and Montsecosuchus (0.63). Atoposaurus jourdani is distinct in this respect from other atoposaurids, including Alligatorellus beaumonti, which has a ratio of 0.81, and Atoposaurus oberndorferi, which has a ratio of 0.78. Alligatorellus bavaricus has an intermediate ratio of 0.76 (Table 3). (S 4) Humerus length to femur length ratio of 0.67: This feature is similar to Protosuchus richardsoni (0.66) and Montsecosuchus (0.70). Alligatorellus beaumonti is similar, with a ratio of 0.75, but Alligatorellus bavaricus is quite distinct, with a ratio of 0.89, similar to Atoposaurus oberndorferi (0.89). Karatausuchus also has similar limb proportions, with a ratio of 0.73. Theriosuchus pusillus falls within the range for atoposaurids, with a ratio of 0.76, but T. guimarotae is distinct with a ratio of 0.98, approaching that for Pachycheilosuchus (1.09) and Brillanceausuchus (1.11) (Table 3). (S 5) Radius to tibia length of 0.61 (C 286.0): This character state is similar to Protosuchus richardsoni (0.63) and Montsecosuchus (0.64), along with Pachycheilosuchus (0.64). Theriosuchus pusillus has a proportionally long radius to tibia ratio (0.55), with this value only being exceeded by Karatausuchus (0.47). Based on Wellnhofer (1971), ‘ Alligatorium ’ franconicum has the most extreme value, with a ratio of 0.89, reflecting a proportionally long radius. This value is similar to Brillanceausuchus (0.88). Atoposaurus oberndorferi and Alligatorium meyeri each have a ratio of 0.74, similar to Shamosuchus (0.72) and Hoplosuchus (0.76) (Table 3). (S 6) Metatarsals longitudinally grooved (C 302.0): This feature also characterizes Alligatorellus beaumonti and Montsecosuchus (Tennant & Mannion, 2014), in contrast to the smooth and flat metatarsals that characterize most other mesoeucrocodylians. However, we are cautious in our interpretation of this feature, as there remains the possibility that it could represent post-mortem crushing of the delicate long bones in the tarsus. ATOPOSAURUS OBERNDORFERI VON MEYER, 1850 Type locality and horizon Solnhofen Formation, early Tithonian (Late Jurassic, Hybonoticeras hybonotum ammonoid zone); Kelheim, Eichst € att, Bavaria, Germany. Type specimen TM 3956, near-complete skeleton, missing only the dorsal part of the skull and posterior portion of the tail. Referred specimen BSPG 1901 I 12, a counterpart specimen of a different individual comprising the impression of the complete skull and skeleton in lateral view. Previous diagnoses and comments Wellnhofer (1971) diagnosed Atoposaurus oberndorferi primarily on several size-based characteristics, but these are unlikely to represent diagnostic morphological characters. He also noted the presence of five premaxillary and eight maxillary teeth, but this could not be confirmed via observation of the type specimen because of the way in which it is preserved, and was not illustrated in the figure of the referred specimen in Wellnhofer (1971). Steel (1973) followed the diagnosis of Wellnhofer (1971), and also suggested that the inwardly displaced postorbital bar was diagnostic of Atoposaurus oberndorferi; however, this feature is now recognized as characterizing Atoposauridae (see above). Furthermore, because of the lateral compression of the type specimen, it was not possible to directly confirm the presence of this feature in Atoposaurus oberndorferi, and it is not figured by Wellnhofer (1971), and therefore cannot be supported. We present a revised diagnosis based on examination of the type specimen for Atoposaurus oberndorferi, and tentatively consider it to be a valid taxon based on three ambiguous autapomorphies. Revised diagnosis and discussion (S 1) Skull anteroposterior length to width ratio ~ 2.00 (1.98) (C 25.0): This feature is tentatively considered to be diagnostic for Atoposaurus oberndorferi, as the skull is highly incomplete and preserved only in ventrolateral aspect. This estimated skull length-to-width ratio is high, similar to Eutretauranosuchus (1.97), Montsecosuchus (1.80), which is represented by a mature specimen (Buscalioni & Sanz, 1990 a), and Theriosuchus guimarotae (1.82) (Schwarz & Salisbury, 2005). Atoposaurus jourdani has a much lower ratio (1.28), more similar to Protosuchus (1.31) and Hoplosuchus (1.35). The only taxa that have higher ratios are Alligatorellus (2.06 – 2.21), Alligatorium meyeri (2.26), ‘ Alligatorium ’ franconicum (2.77), and Koumpiodontosuchus (2.04) (Table 3). (S 2) Skull anteroposterior length to orbit length ratio <3.00 (2.86) (C 27.0): As with (S 1), we are cautious with our interpretation of this character state based on the way in which the observed type specimen of Atoposaurus oberndorferi is preserved, exposing the enlarged orbit only in ventral aspect. The only taxon with a lower ratio is Atoposaurus jourdani (2.33), with Alligatorellus and Alligatorium possessing ratio values between 3.0 and 4.0. Protosuchus has a ratio of 4.52 (Table 3), an intermediate value between atoposaurids and higher neosuchians. (S 3) Inwardly (dorsally) displaced splenial on the ventral mandibular surface (C 234.1): In all other taxa we analysed in which the ventral surface of the mandible was exposed, the anterior portion of the splenial is confluent ventrally with the posterior cavity that is formed from the two posteriorly divergent mandibular rami. In Atoposaurus oberndorferi, the splenial is slightly inset at its contact with the dentary, a feature shared only with T. pusillus. The ventral side of the skull and mandibular region is not preserved in Atoposaurus jourdani, and this character state might also be present in that taxon too. Therefore, we are cautious in our retention of Atoposaurus oberndorferi as a distinct, second species of Atoposaurus. ALLIGATORELLUS GERVAIS, 1871 Included species Alligatorellus beaumonti (Gervais, 1871), Alligatorellus bavaricus (Wellnhofer, 1971; sensu Tennant & Mannion, 2014). Distribution Late Jurassic of southern France and south-east Germany. Previous diagnoses and comments Alligatorellus was diagnosed by Wellnhofer (1971) based on its overall size, the shape of its skull, and its relatively large orbits, features that are all more widespread amongst atoposaurids and other smallbodied neosuchians. Wellnhofer (1971) originally described two subspecies of Alligatorellus beaumonti, based on relative sizes and differences and geographical distribution. Most recently, Tennant & Mannion (2014) documented a number of distinguishing characters between Alligatorellus beaumonti beaumonti from France and Alligatorellus beaumonti bavaricus from Germany, and reranked the latter to its own species, Alligatorellus bavaricus. Several of the diagnostic synapomorphies for Alligatorellus, presented below, might be related to ontogenetic factors, such as the heterogeneity of the cranial sculpting and the closed internal supratemporal fenestra (Joffe, 1967). However, these features could also be related to the proposed ‘ dwarfism’ for atoposaurids, and there are other indicators that the available specimens of Alligatorellus represent a reasonably mature state of growth, such as neurocentral fusion and the degree of fusion of the cranial bones (Joffe, 1967; Tennant & Mannion, 2014). Schwarz-Wings et al. (2011) referred a partial skeleton, MB. R. 3632, from the early Tithonian of Franconia, Germany (Gravesia gigas ammonoid zone) to Alligatorellus sp., but Tennant & Mannion (2014) concluded that this specimen could only be referred to as Atoposauridae indet. In most of our analyses, this specimen is recovered as an indeterminate non-atoposaurid taxon (Figs 4, 7 A). However, when we used implied weighting, this specimen groups with the other species of Alligatorellus within Atoposauridae (Fig. 6). Therefore, we tentatively regard its status as Alligatorellus sp. to be valid. Revised diagnosis and discussion (S 1) Cranial table sculpting composed of homogeneous, subcircular shallow pits (C 2.2): The cranial sculpting pattern for Alligatorellus is distinct from that of Atoposaurus, which has a smooth dorsal surface, and from Alligatorium and Theriosuchus in which the sculpting is much more prominent. It is similar to Wannchampsus, which is also lightly sculpted. The reduction or lack of sculpting has been noted in smaller specimens of the basal mesoeucrocodylian Zosuchus (Pol & Norell, 2004 a, b), as well as the protosuchian Gobiosuchus (Osmolska, Hua & Buffetaut, 1997). (S 2) Rostrum unsculpted or relatively less than the cranial table (C 3.1): Similar to (S 1), the sculpting of the rostrum is relatively light compared with Alligatorium meyeri, T. pusillus, and Wannchampsus. Distinct from these taxa, however, is how the degree of sculpting appears to decrease anteriorly for Alligatorellus, with a more prominent pattern on the cranial table, and almost no sculpting on the dorsal surface of the rostrum. This morphology is similar to that seen in the paratype of Isisfordia, which is represented by an adult specimen (Salisbury et al., 2006), and Pachycheilosuchus, which is known from mature individuals (Rogers, 2003). In other taxa represented by mature specimens, such as T. pusillus and Rugosuchus (Wu, Cheng & Russell, 2001 a), sculpting patterns are homogeneous across the entire dorsal surface of the skull. Alligatorium meyeri is unusual in that the degree of sculpting remains the same between the rostrum and cranial table, but anteriorly the subcircular pits become more elongated, a feature visible in the counterpart to its holotype specimen (MNHL 15462), and which helps to distinguish it from Alligatorellus. (S 3) Closed internal supratemporal fenestra (C 16.1): This feature refers to the lack of opening of the internal supratemporal fenestra, as noted by Wellnhofer (1971). In all other specimens we observed, the internal supratemporal fenestra is completely open. Joffe (1967) described the opening as ‘ slit-like’ for T. pusillus, and regarded it as indicative of an immature individual. However, our observations of the paratype specimen (NHMUK PV OR 48330) did not confirm this, and the internal fenestrae appear to be fully open. Because of poor preservation, we were unable to determine whether the morphology of the internal supratemporal fenestra was open or closed in any specimen of Atoposaurus. (S 4) Frontal maximal mediolateral width between the orbits narrower than maximal width of nasals (C 97.1): This character state relates to the proportionally large size of the orbits, which occupy the majority of the mediolateral width of the dorsal surface of the skull, with a proportionally narrow interorbital region composed of the fused frontals. Although this feature is shared by many other neosuchians, including Theriosuchus and Wannchampsus, the frontals are distinctly narrower in Alligatorellus. In protosuchians, such as Protosuchus and Hoplosuchus, the mediolateral width of the frontal is broader than the nasal, because in these taxa the orbit is more laterally facing, and therefore does not occupy as much of the mediolateral width of the skull in dorsal view. (S 5) Broad frontal anterior process with parallel lateral margins, not constricted (C 109.0): This feature is distinct from the morphology described in (S 4), and relates exclusively to the development of the frontals anteriorly to the anterior margin of the orbits, excluding the morphology of any frontal anterior process where present. The broad anterior edge of the frontal with parallel lateral edges in Alligatorellus is similar to paralligatorids, T. pusillus, and Montsecosuchus, but contrasts with T. guimarotae in which the mediolaterally constricted anterior portions of the frontals distinctly underlap the nasals (Schwarz & Salisbury, 2005). (S 6) Flat and unsculpted anterior supratemporal margins (C 119.0): In Alligatorellus bavaricus, the supratemporal rims are flat and unsculpted along their entire medial edge, similar to protosuchians, Pachycheilosuchus, coelognathosuchians, Montsecosuchus, and Koumpiodontosuchus. However, in Alligatorellus beaumonti, there is a slight posterior development of the supratemporal margins, similar to Brillanceausuchus (specimen UP BBR 203). This is distinct from Alligatorium meyeri, Wannchampsus, and all species referred to Theriosuchus, in which the supratemporal rims are consistently well developed along their entire medial margin. (S 7 *) Anterior process of squamosal extends to the posterior orbital margin (C 144.0): This character state appears to be diagnostic for Alligatorellus, although we are cautious in this assignment, as the postorbital region is poorly preserved, and the exact morphology of the postorbital with respect to the other posterior periorbital elements is difficult to assess. However, in the holotypes of Alligatorellus beaumonti and Alligatorellus bavaricus, there is no notable suture on the dorsal surface of the skull table, lateral to the supratemporal fenestra, which would represent the suture between the posterior process of the postorbital and the anterior process of the squamosal. We therefore infer that the anterior process of the squamosal reached the posterior orbital margin. (S 8) Posterodorsal margin of parietals and squamosals completely covers posterodorsal occipital region, excluding the supraoccipital from the dorsal surface of the skull (C 197.1): This feature was proposed by Tennant & Mannion (2014) to be autapomorphic for Alligatorellus, but also appears to be present in a range of neosuchian taxa (e. g. Acynodon adriaticus; Delfino et al., 2008 b) in which the supraoccipital is excluded from the posterodorsal surface of the skull roof. We therefore consider it to only be locally diagnostic for Alligatorellus. In other mesoeucrocodylians, such as Mahajangasuchus (Turner & Buckley, 2008), the supraoccipital is broadly visible in the midline portion of the posterodorsal region of the skull, contacting the parietals. (S 9) Smooth mandibular external surface, lacking sculpting (C 201.0): This feature is difficult to observe in Alligatorellus bavaricus owing to the dorsal flattening of the holotype specimen, although what is visible indicates that the mandible, much like the anterior portion of the skull, lacks any sculpting pattern, unlike the dorsal surface of the cranial table. This is distinct from Theriosuchus and Wannchampsus, in which the sculpting pattern on the external surface of the dentaries and posterior mandibular elements is similar to that of the dorsal surface of the skull. (S 10) Proximal end of the radiale ‘ hatchet-shaped’ (C 290.1): This feature also characterizes MB. R. 3632, and was used to refer this specimen to Alligatorellus (Schwarz-Wings et al., 2011). However, this morphology is also shared by Wannchampsus (Adams, 2014), but is not known in Theriosuchus specimens, owing to lack of preservation of the radiales. In other atoposaurids, the proximal end of the radiale is more expanded equidimensionally, lacking the asymmetry observed in Alligatorellus. (S 11) Proportionally short metatarsal I relative to metatarsals II – IV (C 303.1): In other atoposaurids, metatarsals I – IV are almost equidimensional, possibly reflecting different locomotor adaptations in Alligatorellus. (S 12 *) Dorsal surface of dorsal osteoderms completely sculpted (C 304.0), with parallel and straight anterior and posterior margins (C 308.1), and a longitudinal ridge along entire lateral margin (C 311.1 and C 312.1): The utility of osteoderms in atoposaurid systematics, particularly regarding Alligatorellus, was discussed by Tennant & Mannion (2014). These authors noted that the mediolateral position and anteroposterior extent of the dorsal keel, and its serial variation along the axial column, are diagnostic for Alligatorellus, as well as for other crocodyliforms (e. g. teleosauroids, eusuchians) that preserve a dorsal series of paravertebral osteoderms. (S 13) Caudal osteoderms with smooth, nonserrated edges (C 327.1): This morphology is similar to the osteoderms preserved for T. guimarotae and T. pusillus, but distinct from Brillanceausuchus and Montsecosuchus in which the margins of the caudal osteoderms are serrated. Serrated edges might also be present in caudal osteoderms of MB. R. 3632, based on at least three caudal osteoderms disassociated from the main osteoderm shield preserved on the specimen slab. However, we cannot discount the possibility that these elements are accessory dorsal osteoderms, as found in Montsecosuchus and in the proximal caudal series of Alligatorellus beaumonti. ALLIGATORELLUS BEAUMONTI GERVAIS, 1871 (TYPE SPECIES) ALLIGATORELLUS BEAUMONTI BEAUMONTI WELLNHOFER, 1971 Type locality and horizon Unknown bed, Kimmeridgian (Late Jurassic); Cerin, Ain, France. Type specimen MNHL 15639, part and counterpart slabs comprising a near-complete and articulated skeleton, missing the distal-most caudal vertebrae (preserved as impressions) and part of the left forelimb. Parts of the skull roof and a large portion of the right maxilla, along with several axial fragments, are embedded into the counterpart slab. Referred specimen MNHL 15638, part slab comprising a near-complete and articulated skull and skeleton, missing just the distal-most caudal vertebrae, the right forelimb, and the distal left forelimb, all of which are preserved as impressions. The skull is exposed in ventrolateral aspect. Previous diagnoses and comments Alligatorellus beaumonti was originally named by Gervais (1871) for two specimens from the Late Jurassic of Cerin, eastern France. Subsequently, Wellnhofer (1971) diagnosed these specimens as a distinct subspecies, Alligatorellus beaumonti beaumonti. This was based largely on size differences between these and coeval specimens from Eichst att €, south-east Germany, for which Wellnhofer (1971) erected the subspecies Alligatorellus beaumonti bavaricus (see below). Together these specimens have largely been regarded as representing a single taxon, Alligatorellus beaumonti, by subsequent workers (e. g. Buscalioni & Sanz, 1988; Schwarz-Wings et al., 2011). However, Tennant & Mannion (2014) redescribed the German remains, and observed a number of morphological differences with the French material. They provided a revised diagnosis for Alligatorellus beaumonti, and re-ranked the German material as Alligatorellus bavaricus. Wellnhofer (1971) noted that as in Theriosuchus, the external nares in Alligatorellus beaumonti are divided by an anterior projection of the nasals, a feature that also appears to be shared by Alligatorium meyeri and possibly Alligatorellus bavaricus, although the anterior-most portion of the snout in the holotype of the latter is damaged. Alligatorellus beaumonti is similar to Alligatorium meyeri in the presence of an unsculpted posterolateral ‘ lobe’ of the squamosal, differing from Alligatorellus bavaricus in which the posterolateral corner of the squamosal instead displays orthogonal posterior and lateral edges. Buscalioni & Sanz (1988) suggested that another distinguishing feature between Alligatorellus beaumonti and Alligatorium meyeri is the contribution of the frontal to the supratemporal fenestra in the former; however, this feature is clearly also present in Alligatorium meyeri, and therefore cannot be used to distinguish the two taxa. The presence of a biserial osteoderm shield comprising singular sculpted osteoderms is not diagnostic for Alligatorellus (contra Wellnhofer, 1971), as it also characterizes both T. pusillus and Alligatorium meyeri. Tennant & Mannion (2014) proposed that the frontal width between the orbits being mediolaterally narrower than the nasals is an autapomorphy of Alligatorellus beaumonti; however, this condition is not considered to be diagnostic here, as it is also known in a wide range of neosuchian taxa, and the width of the paired nasals in Alligatorellus bavaricus might have been underestimated. Alligatorellus beaumonti also has the reversed condition to Alligatorellus bavaricus, in that the anterior extension of the frontal exceeds the anterior margin of the orbits, similar to almost all other neosuchian taxa. Revised diagnosis and discussion (S 1 *) Frontal with unsculpted anterior and posterior portions, and sculpted medial surface: We elected not to code this as a distinct character state from that of S 3 in our matrix in order to avoid duplication of character states. Nonetheless, Tennant & Mannion (2014) identified this heterogeneity in sculpting pattern as distinct from other atoposaurids and Theriosuchus, and considered it to be autapomorphic of Alligatorellus beaumonti. (S 2) Surface of rostrum notably less sculpted than cranial table (C 4.1): See S 2 for Alligatorellus for discussion of this character state. (S 3) Relatively large lateral temporal fenestra, approximately 30 % of the size of the orbit (C 20.1): A lateral temporal fenestra of this size with respect to the orbit represents the intermediate condition in our analyses. This relatively large size is unique amongst atoposaurids, but is also shared with T. pusillus, Koumpiodontosuchus (Sweetman et al., 2015), and protosuchians, as well as the advanced neosuchians Shamosuchus (Pol et al., 2009), Isisfordia (Salisbury et al., 2006), and Brillanceausuchus. In other taxa, such as Allodaposuchus precedens, the lateral temporal fenestra approaches the size of the orbit (Buscalioni et al., 2001). (S 4) Smooth contact between maxilla and jugal (C 51.2): As noted above, the pattern of sculpting on the anterior portion of the dorsal surface of the skull is diagnostic for the different species of Alligatorellus. In Alligatorellus bavaricus, the entire dorsal surface is lightly sculpted, but Alligatorellus beaumonti has a smooth contact between the maxilla and jugal, similar to Atoposaurus and Hoplosuchus, although in both of these taxa the entire external surface of the skull is not ornamented. This is distinct from T. guimarotae and T. pusillus, which both have a contact in which the external surface is sculpted to the same degree as the rest of the cranial table, and from Brillanceausuchus, ‘ T. ’ ibericus, ‘ T. ’ sympiestodon, and Montsecosuchus, in which the contact is heavily striated. (S 5 *) Medial longitudinal depression on posterior portion of nasal and anterior portion of frontal (C 74.1): This is diagnostic of Alligatorellus beaumonti as a local autapomorphy, but is also present in the goniopholidid Amphicotylus (Mook, 1942). This condition differs from that in Theriosuchus and a range of paralligatorids, including Brillanceausuchus, in which a distinct midline longitudinal crest develops. (S 6 *) Posteromedial border of supratemporal fenestra forms a low sagittal rim (C 119.1): This feature is considered to be locally autapomorphic, as it is also present in Brillanceausuchus. Alligatorellus bavaricus and Atoposaurus have no supratemporal rim development, and the rims are strongly developed along the whole medial edge of the external supratemporal fenestra in Alligatorium meyeri, T. pusillus, and Wannchampsus (Adams, 2014). (S 7 *) Smooth and unsculpted region on anterior portion of squamosal nearing orbit and posterolateral process of squamosal (C 148.1): This feature appears to be locally diagnostic, but is also shared by Khoratosuchus (Lauprasert et al., 2009). For all other OTUs for which this feature could be scored, the pattern of sculpting did not change between the main body of the squamosal and the immediate postorbital region. (S 8 *) Ratio of forelimb to hindlimb length high (0.8) (C 180.2): This feature is diagnostic for Alligatorellus beaumonti amongst all OTUs for which this character could be scored. Atoposaurus oberndorferi and Alligatorellus bavaricus both have similar ratios, 0.78 and 0.76, respectively, but Atoposaurus jourdani is distinct, with a ratio of 0.63 (Table 3). However, this character state could not be scored for Theriosuchus, or the majority of our outgroup taxa, because of the relative rarity with which these specimens preserve associated and complete limb material. Therefore, although these unusual ratios are diagnostic amongst atoposaurids, we cannot determine whether they are unique or only local autapomorphies. (S 9) Ratio of tibia to femur length low (0.9) (C 300.0): The relative dimensions of the tibia and femur are a feature that is closely shared with MB. R. 3632 (0.91), Hoplosuchus (0.92), Alligatorium meyeri (0.93), and Atoposaurus jourdani (0.94). This ratio far exceeds that for ‘ Alligatorium ’ franconicum (0.64), and is distinct from Alligatorellus bavaricus (0.96) (Table 3). This feature was also noted by Tennant & Mannion (2014), but those authors used a ratio of femur to tibia length. (S 10 *) Nuchal osteoderms reduced, <50 % of the size of the dorsal osteoderms (C 307.1): This feature is distinct from the condition in Alligatorellus bavaricus, Alligatorium meyeri, Montsecosuchus, and Protosuchus, in which the preserved nuchal osteoderms retain the same size and morphology as the dorsal series, or only decrease slightly. (S 11 *) Dorsal keel in dorsal osteoderms shifts laterally in more posterior dorsal osteoderms (C 317.1): The position of the dorsal keel on the dorsal osteoderm series is distinct from that in Alligatorellus bavaricus, in which the morphology is more consistent along the axial column (Tennant & Mannion, 2014). This feature is not present in any other of the OTUs that we sampled, and therefore we consider it to be diagnostic for Alligatorellus beaumonti. (S 12 *) Lateral ridge on sacral osteoderms forms an incipient posterior projection: The posterior development of the lateral keel (as noted in S 9) into an incipient lateral projection amongst the more sacrally positioned osteoderms is diagnostic for Alligatorellus beaumonti. In Alligatorellus bavaricus, the morphology of the keel does not change anteroposteriorly (Tennant & Mannion, 2014), and Theriosuchus, Alligatorium meyeri, and higher neosuchians do not seem to possess this keel at all. ‘ Alligatorium ’ franconicum and Hoplosuchus are convergently similar, in that the lateral keel appears to form an anterolateral process, distinct from the ‘ peg and socket’ articulation described for goniopholidids and T. guimarotae (Schwarz & Salisbury, 2005). We did not incorporate this as a character to avoid duplication and overweighting of the observation that the morphology of the dorsal keel changes axially in Alligatorellus beaumonti (S 11). (S 13 *) Secondary osteoderms present in caudal series (C 328.0): This feature does not appear to be present in any other atoposaurid that preserves caudal osteoderms. Additional comments In the holotype specimen of Alligatorellus beaumonti, the posterior-most maxillary teeth have a more labiolingually compressed, apically pointed morphology than the remaining teeth, similar to the ‘ lanceolate’ morphology exhibited by several species of Theriosuchus (Schwarz & Salisbury, 2005; Lauprasert et al., 2011) and Brillanceausuchus, as well as the bernissartiid Koumpiodontosuchus (Sweetman et al., 2015). This is different to the homodont dentition typically reported for Alligatorellus, which is usually described as possessing simple pseudocaniniform teeth that are smooth and lack ridges or carinae (e. g. Buscalioni & Sanz, 1990 a, b; Thies et al., 1997). However, we do not assign this as a local autapomorphy of Alligatorellus beaumonti as it is only visible for one or two teeth in a specimen that shows strong evidence of dorsal compression. Its validity therefore requires further investigation pending the discovery of more specimens of Alligatorellus. Although this more lanceolate morphology was also figured for the posterior teeth of Alligatorellus bavaricus by Wellnhofer (1971), we have been unable to personally validate this on the figured specimen, and it is not visible on the holotype. Therefore, we urge caution in interpreting Alligatorellus as possessing lanceolate posterior teeth that are homologous to those found in Theriosuchus. Re-running our phylogenetic analysis [excluding ‘ Alligatorellus ’ sp. (MB. R. 3632) and Pachycheilosuchus as before] with Alligatorellus scored as possessing lanceolate posterior teeth, we achieve a single MPT with a length of 793 steps with an unchanged topology. However, the presence of a lanceolate dentition instead becomes the basal condition in the clade containing atoposaurids and higher neosuchians, secondarily lost in Alligatorium meyeri, Brillanceausuchus, ‘ T. ’ ibericus, ‘ T. ’ sympiestodon, and the clade containing Koumpiodontosuchus and coelognathosuchians. ALLIGATORELLUS BAVARICUS WELLNHOFER, 1971 (RE- RANKED BY TENNANT & MANNION, 2014) ALLIGATORELLUS BEAUMONTI BAVARICUS WELLNHOFER, 1971 Type locality and horizon Solnhofen Formation, early Tithonian (Late Jurassic, Hybonoticeras hybonotum zone); Eichst att €, southeast Germany. Type specimen BSPG 1937 I 26, a near-complete skeleton including the skull, lacking only the left forelimb, compressed onto a slab of lithographic limestone. Note that Tennant & Mannion (2014) incorrectly stated that the specimen number was LMU 1937 I 26. Referred specimen A specimen held in the private collection of E. Schopfel was described and referred to Alligatorellus bavaricus by Wellnhofer (1971), from the Wintershof Quarry (Solnhofen Formation, Eichst att €, southeast Germany). Revised diagnosis and discussion (S 1) Concave profile of dorsal surface of snout in lateral view (C 8.0): This feature represents a reversion back to the plesiomorphic state known for Protosuchus (Colbert & Mook, 1951) and Hoplosuchus (Gilmore, 1926), with other atoposaurids and neosuchians usually presenting a straight profile in lateral aspect (with exceptions such as the longirostrine goniopholidid Amphicotylus; Mook, 1942). (S 2) Small, slit-shaped antorbital fenestra, enclosed by nasals (C 13.0 and C 14.1): Alligatorellus bavaricus appears to possess a small, slit-like antorbital fenestra, similar to the notosuchians Gondwanasuchus (Marinho et al., 2013) and Malawisuchus (Gomani, 1997). In other taxa with an antorbital fenestra, including T. guimarotae (Schwarz & Salisbury, 2005), T. pusillus, and ‘ T. ’ ibericus, it is proportionally larger and rounded. Alligatorellus beaumonti does not appear to possess an antorbital fenestra, although part of the snout is embedded in the counterpart slab, with a small opening observable near the posterior margin of the nasals, which could be a diminutive fenestra. The presence of an antorbital fenestra is documented in basal crocodyliforms, including the protosuchians Hoplosuchus (Gilmore, 1926) and Protosuchus haughtoni (Gow, 2000), Zosuchus (Pol & Norell, 2004 a), and thalattosuchians (Leardi et al., 2012), but becomes closed in shartegosuchids, including Fruitachampsa (Clark, 2011). Pachycheilosuchus might have also possessed an antorbital fenestra (Rogers, 2003). (S 3 *) Extremely narrow and short skull, with a low skull width to orbit width ratio (<2.0) (C 28.0): This character state is the lowest value for all atoposaurids, and much lower than all other OTUs in which this character was measurable. For other atoposaurids, this ratio is between 2.15 (Alligatorellus beaumonti) and 2.69 (Atoposaurus jourdani), and the only other taxon that comes close to this range is Wannchampsus (2.77). Brillanceausuchus, Montsecosuchus, and Theriosuchus species all have ratios between 3.0 and 3.5, with the ratio being considerably greater in longirostrine taxa and protosuchians (Table 3). It is likely that this character state is influenced by ontogeny (Joffe, 1967), but the broad distribution of ratios amongst the sampled OTUs, which possess a range of body sizes and ontogenetic states, means that ontogeny is unlikely to entirely control this feature. (S 4) Skull anteroposterior length to supratemporal fenestra length ratio ~ 7.2 (7.18) (C 29.2): The proportional length of the external supratemporal fenestra is similar to Wannchampsus kirpachi (7.53), but distinct from Alligatorium meyeri (6.43) and Alligatorellus beaumonti (6.23), which have proportionally larger external supratemporal fenestrae. Consequently, we consider the proportionally short anteroposterior length of the supratemporal fenestra to skull length to be diagnostic for Alligatorellus bavaricus, because in Montsecosuchus this ratio is considerably higher (8.9) (Table 3), with a much smaller supratemporal fenestra. (S 5 *) Posterior surface of nasals longitudinally crenulated (C 69.0): The longitudinal crenulations on the dorsal surface of the nasals are not known in any other crocodyliform, in which the nasals are dorsally flat and sculpted like the rest of the cranial dorsal surface. (S 6 *) Smooth anterior region of parietal dorsal surface with a transverse frontal – parietal ridge, and shallow emargination at the posterior parietal – squamosal contact (C 117.1) that develops into a thin dorsal groove connected to the supratemporal fenestra (C 147.1): The morphology of the parietal is diagnostic, with a small anterior concavity at the posterodorsal suture contact between the parietal and squamosal, leading to a shallow sulcus along this contact into the posterior margin of the supratemporal fenestra, and a smooth anterior dorsal surface. This is distinct from the condition observed in Theriosuchus in which this contact is deep and expands mediolaterally towards the supratemporal fenestra border, and from Alligatorellus beaumonti and Alligatorium meyeri in which the grooved contact is bordered by raised crests. The presence of a transverse ridge at the parietal – frontal suture distinguishes Alligatorellus bavaricus from all other species, in which this suture is flat. (S 7) Squamosal posterolateral lobe absent (C 139.1):. The squamosal posterolateral lobe is completely absent in Alligatorellus bavaricus, a feature considered to be diagnostic amongst all atoposaurids. (S 8 *) Distinct ridge on proximodorsal edge of scapula (C 280.1): The scapula of Alligatorellus bavaricus can be distinguished from Alligatorellus beaumonti and other atoposaurids based on the presence of a distinct ridge on the proximodorsal surface. In all other specimens we analysed, the proximodorsal edge of the scapula is flat in lateral view, and confluent with the scapular shaft. (S 9) Extremely low radius proximodistal length to humerus length ratio (0.69) (C 288.1): The radius to humerus ratio is extremely low, distinct from other atoposaurids in which the value is closer to 1.0. This low ratio is identical to that for ‘ Alligatorium ’ franconicum and Karatausuchus (Storrs & Efimov, 2000), but higher than in Pachycheilosuchus (0.58). (S 10 *) Low radius proximodistal length to tibia length ratio (0.64) (C 289.1): This value is almost identical to that for Montsecosuchus, Pachycheilosuchus, Atoposaurus jourdani (0.61), and Protosuchus richardsoni (0.63), but much higher than that for Karatausuchus (0.47) and T. pusillus (0.55). Other taxa have proportionally long radii, including Alligatorium meyeri (0.74), Alligatorellus beaumonti (0.71), ‘ Alligatorium ’ franconicum (0.89), and Brillanceausuchus (0.88). (S 11 *) Dorsal osteoderms with longitudinal medial ridge, becoming more laterally placed anteriorly (C 311.1 and C 312.1): This feature pertains to the morphology of the dorsal osteoderm series, which are distinct from those in Alligatorellus beaumonti (Tennant & Mannion, 2014), as well as MB. R. 3632 (Schwarz-Wings et al., 2011). In Alligatorium meyeri and T. pusillus, there is no evidence of a lateral keel.	en	Tennant, Jonathan P., Mannion, Philip D., Upchurch, Paul (2016): Evolutionary relationships and systematics of Atoposauridae (Crocodylomorpha: Neosuchia): implications for the rise of Eusuchia. Zoological Journal of the Linnean Society 177 (4): 854-936, DOI: 10.1111/zoj.12400, URL: http://doi.wiley.com/10.1111/zoj.12400
F75787E0FFBCFFEE05D20100827BB900.taxon	materials_examined	Type locality and horizon Unnamed bed,? Barremian (Early Cretaceous), Babouri-Figuil Basin, north Cameroon. Type specimen UP BBR 201, skull and partial skeleton. Previous diagnoses and comments Despite noting numerous similarities with atoposaurids, Michard et al. (1990) assigned Brillanceausuchus to its own family, Brillanceausuchidae, within Neosuchia. However, a monogeneric family has no systematic purpose, and Brillanceausuchidae has not been used by subsequent workers. Pending the recovery of closely related taxa that do not already form a named clade, we recommend disuse of Brillanceausuchidae. Brillanceausuchus has remained a neglected taxon in phylogenetic and comparative analyses, despite its apparent important morphology in possessing a number of ‘ primitive’ character states (e. g. possession of a partially septated external nares and presence of a biserial osteoderm shield) alongside more ‘ transitional’ morphologies between advanced neosuchians and eusuchians (e. g. reduced ventral exposure of the basisphenoid and procoelous presacral vertebrae) (Michard et al., 1990). It was regarded as an atoposaurid by Salisbury & Frey (2001) and Salisbury et al. (2006), and as an ‘ advanced neosuchian’ by Turner (2015), without additional comment. To our knowledge, the only phylogenetic analysis to include Brillanceausuchus was conducted by Osi € et al. (2007: 174), who commented that its inclusion ‘ gave much less resolution inside Eusuchia due to its incompleteness’ and did not report the results. Discussion Brillanceausuchus possesses procoelous cervical and dorsal vertebrae (Michard et al., 1990), as well as fully pterygoidean choanae that are situated posteriorly to the posterior edge of the suborbital fenestrae, as in eusuchians (Buscalioni et al., 2001; Pol et al., 2009). Many authors have considered the presence of this combination of vertebral and palatal morphologies to imply that the eusuchian condition has evolved in parallel in several different neosuchian lineages, based on the underlying assumption that Brillanceausuchus is an atoposaurid, and therefore more basally positioned within Neosuchia (e. g. Brochu, 1999; Buscalioni et al., 2001; Salisbury et al., 2006). However, our preliminary results indicate that Brillanceausuchus belongs to Paralligatoridae (Figs 4 B, 5, 6, 7), a clade most recently placed within Eusuchia (Turner, 2015). Therefore, the eusuchian condition might not be as homoplasious as previously regarded. Additional material assigned to Brillanceausuchus is currently being prepared, and comprises numerous skeletons (including skulls) preserved in three dimensions (J. Martin, pers. comm., 2015). We await the full description of this material before a comprehensive taxonomic assessment of Brillanceausuchus can be made, and preliminarily assign it to Paralligatoridae. Preliminary emended diagnosis (S 1) proportionally long supratemporal fenestra, with anteroposterior length exceeding that of the orbit, and a skull length to supratemporal fenestra length ratio of <6.0 (5.36) (C 29.0), and a skull width to supratemporal fenestra width ratio of 7.0 (C 30.3); (S 2) sinusoidal lateral nasal borders oblique to one another (C 66.3), with abrupt widening adjacent to maxilla (C 70.1); (S 3) base of jugal postorbital process directed dorsally (C 83.1); (S 4) flat frontal dorsal surface (no longitudinal crest or periorbital rims) (C 100.0); (S 5) parietal – postorbital suture visible on the dorsal surface of the skull roof (C 112.1) and within the supratemporal fenestra (C 113.1); (S 6) concavity at posterodorsal edge of squamosal – parietal contact (C 117.1); (S 7) lateral margins of squamosal and postorbital medially concave in dorsal view (C 134.2), and dorsal surface of squamosal bevelled ventrally (C 138.1), becoming unsculpted anteriorly (C 148.1); (S 8) squamosal posterolateral process elongate, distally tapered (C 143.0) and depressed from skull table (C 140.1); (S 9) basisphenoid ventral surface mediolaterally narrower than basioccipital (C 191.0), and basioccipital with large, well-developed bilateral tuberosities (C 192.1); (S 10) ventrolateral surface of anterior portion of dentary strongly mediolaterally compressed and flat (C 215.0), with grooved ornamentation on external surface (C 227.1); (S 11) retroarticular process projects posteriorly and dorsally recurved (C 242.3); (S 12) posterior dentary teeth occlude medial to opposing maxillary teeth (C 263.0); (S 13) rounded and ovate dorsal osteoderm shape (C 308.0). PACHYCHEILOSUCHUS TRINQUEI, ROGERS 2003	en	Tennant, Jonathan P., Mannion, Philip D., Upchurch, Paul (2016): Evolutionary relationships and systematics of Atoposauridae (Crocodylomorpha: Neosuchia): implications for the rise of Eusuchia. Zoological Journal of the Linnean Society 177 (4): 854-936, DOI: 10.1111/zoj.12400, URL: http://doi.wiley.com/10.1111/zoj.12400
F75787E0FFBCFFEE05D20100827BB900.taxon	description	Pachycheilosuchus trinquei is known from a nearcomplete, disarticulated skeleton and partial skull from the Albian (Early Cretaceous) Glen Rose Formation of Erath County, Texas, USA. Initially described as a possible atoposaurid (Rogers, 2003), a position at the base of Atoposauridae was subsequently demonstrated in the analyses of Turner & Buckley (2008) and Pol et al. (2009). However, more recent analyses have placed Pachycheilosuchus outside of Atoposauridae, either within the basal eusuchian clade Hylaeochampsidae [Buscalioni et al., 2011 (although note that this study used Theriosuchus as an outgroup, and included no definite atoposaurids); Turner & Pritchard, 2015], or just outside the eusuchian radiation (Adams, 2013; Narvaez et al., 2015). Rogers (2003) based his assignment to Atoposauridae primarily on the presence of a jugal with equally broad anterior and posterior processes, and the possession of procoelous presacral vertebrae. However, this jugal morphology is known in other neosuchians, including Paluxy- suchus, as well as thalattosuchians (Adams, 2013). The presence of procoelous vertebrae could be more broadly distributed amongst non-neosuchian eusuchians than previously recognized, and full procoely is not definitively known amongst any atoposaurid species (see also Salisbury & Frey, 2001). Hylaeochampsid affinities are supported by the reinterpretation of a defining character state for Atoposauridae, pertaining to whether the bar between the orbit and supratemporal fenestra is narrow, with sculpting restricted to the anterior surface (Clark, 1994). Buscalioni et al. (2011) regarded this feature to be associated more broadly with ‘ dwarfism’ (as initially proposed for Pachycheilosuchus) or immature specimens, and not a synapomorphy of Atoposauridae. Pachycheilosuchus is additionally unusual in the retention of an antorbital fenestra, to which the maxilla contributes (Rogers, 2003), which is similar to T. guimarotae (Schwarz & Salisbury, 2005) and Alligatorellus bavaricus (Tennant & Mannion, 2014). The present study was not designed to resolve the phylogenetic placement of Pachycheilosuchus, except whether or not to include it within Atoposauridae. We support its exclusion from Atoposauridae, but cannot provide further comment on its placement within Hylaeochampsidae (Buscalioni et al., 2011). It is unusual in that we recover Pachycheilosuchus in a more stemward position than Atoposauridae. We anticipate that inclusion of a broader range of atoposaurid specimens, Theriosuchus species, hylaeochampsids (including Pietraroiasuchus ormezzanoi; Buscalioni et al., 2011), and additional paralligatorids within a larger Neosuchia-focussed data matrix, will help to resolve the position of Pachycheilosuchus and its clearly important role in the ascent of advanced neosuchians and Eusuchia. WANNCHAMPSUS KIRPACHI ADAMS, 2014 The ‘ Glen Rose Form’ has been commonly referred to in neosuchian systematics since it was first briefly mentioned and figured by Langston (1974). Comprising a skull and lower jaw from the Early Cretaceous (late Aptian) Antlers Formation of Montague County, Texas, USA, it was described as resembling the extant dwarfed crocodile Osteolaemus tetraspis, and Langston (1974) also noted similarities to T. pusillus. Subsequently, Adams (2014) erected Wannchampsus kirpachi for two skulls and postcranial material from the late Aptian (Early Cretaceous) Twin Mountains Formation of Comanche County (Texas, USA), and assigned the ‘ Glen Rose Form’ to this taxon. Adams (2014) noted that the skull of Wannchampsus was similar to that of T. pusillus, sharing features such as medial supraorbital rims, and therefore prompting its inclusion in the present analysis and discussion here. However, Wannchampsus is distinct from T. pusillus in: (1) the possession of an enlarged third maxillary tooth (instead present at the fourth position in T. pusillus); (2) the absence of an antorbital fenestra; (3) choanae with an anterior margin close to the posterior edge of the suborbital fenestra (whereas it is more anteriorly placed in T. pusillus); and (4) the definitive presence of procoelous dorsal and caudal vertebrae. We recovered Wannchampsus in a position close to Shamosuchus [Pol et al., 2009; see also Adams (2014) and Turner (2015)], forming a paralligatorid clade with Sabresuchus and Brillanceausuchus. KARATAUSUCHUS SHAROVI EFIMOV, 1976 Karatausuchus sharovi is known only from a single skeleton of a juvenile individual from the Late Jurassic (Oxfordian – Kimmeridgian) Karabastau Formation in southern Kazakhstan. It was considered to be an atoposaurid by Efimov (1976, 1988), but more closely related to paralligatorids by Efimov (1996). Storrs & Efimov (2000) argued that it was a relatively basal crocodyliform owing to the possession of amphiplatyan vertebral centra, and designated it as a questionable atoposaurid. It is generally similar to atoposaurids in being small, at only 160 mm in total anteroposterior body length, but possesses reduced dermal osteoderms, suggestive of a juvenile phase of growth. Intriguingly, Storrs & Efimov (2000) observed over 90 small, labiolingually compressed teeth within the jaws, a feature unique amongst crocodyliforms. It also possesses 46 caudal vertebrae, approaching the condition known for Atoposaurus. However, it has eight cervical vertebrae, placing it intermediate to Protosuchus (nine cervical vertebrae) and the majority of other atoposaurids (seven cervical vertebrae, with the exception of Atoposaurus jourdani, which appears to have six). Karatausuchus is similar to atoposaurids in that its skull length to orbit length ratio is relatively low, between 3.0 and 4.0 (3.37), but the other diagnostic features presented in this study for Atoposauridae cannot be assessed in the single known specimen. Therefore, we agree with Buscalioni & Sanz (1988) that Karatausuchus sharovi is currently too poorly known to be assigned to any family, including Atoposauridae, and regard it as an indeterminate crocodyliform. However, we still tentatively regard it as a valid taxon, owing to the high number of cervical and caudal vertebrae, and the possession of an anomalously high number of teeth. HOPLOSUCHUS KAYI GILMORE, 1926 Gilmore (1926) originally recognized this taxon, based on a near-complete and articulated skeleton from the Late Jurassic Morrison Formation at Dino- saur National Monument (Utah, USA), as a pseudosuchian archosaur. Subsequently, several authors assigned Hoplosuchus kayi to Atoposauridae (Romer, 1956; Kuhn, 1960; Steel, 1973), based on its overall size, and the possession of relatively large, posteriorly placed, and anterolaterally facing orbits. However, Buffetaut (1982) and Osmolska et al. (1997) regarded Hoplosuchus as more similar to protosuchians, but noted that its phylogenetic affinities remained uncertain. In their phylogenetic assessment of Atoposauridae, Buscalioni & Sanz (1988) concluded that Hoplosuchus is a ‘ protosuchian-grade’ crocodyliform. Our examination of this taxon could not confirm any definitive atoposaurid affinities. Hoplosuchus retains features present in basal crocodyliforms, including a small and circular antorbital fenestra, and a triangular lateral temporal fenestra that is nearly as large as the orbit. Potential autapomorphies for Hoplosuchus include: (1) a steeply posteriorly inclined quadrate; (2) the pterygoid bearing a descending process that is extensively conjoined in the mid-line anterior to the basisphenoid; and (3) a lower jaw lacking the external mandibular fenestra (Steel, 1973). Hoplosuchus has slender limbs, the dorsal armour is composed of paired oblong plates, and the caudal region is completely enclosed by dermal ossifications. A full revision of protosuchian crocodyliforms is currently underway (A. Buscalioni, pers. comm., 2014), and we await this before drawing any conclusions about the affinities of Hoplosuchus. Nonetheless, we exclude Hoplosuchus from Atoposauridae. SHANTUNGOSUCHUS CHUHSIENENSIS YOUNG, 1961 Young (1961) initially identified this taxon, based on a near-complete skeleton and skull from the Early Cretaceous Mengyin Formation of Shandong Province, China, as an atoposaurid. This referral was subsequently supported by Steel (1973), who provided an emended diagnosis in his discussion of Atoposauridae. This included: (1) a triangular-shaped skull; (2) closely set teeth deeply implanted in independent alveoli; (3) seven cervical and 18 dorsal vertebrae; (4) short cervical vertebral centra; (5) relatively long dorsal vertebral centra; (6) a slightly shorter ulna than humerus; (7) the tibia significantly exceeding the femur in length; and (8) the forelimbs being proportionally long. However, Buffetaut (1981) and Buscalioni & Sanz (1988) both excluded Shantungosuchus from Atoposauridae. Wu et al. (1994) regarded much of the original interpretation of Young (1961) as incorrect, and revised Shantungosuchus, finding it to be more closely related to protosuchians than to atoposaurids. We concur with these authors and exclude Shantungosuchus chuhsienensis from Atoposauridae, supporting a basal position within Crocodyliformes. However, we note that atoposaurids do share numerous metric features with protosuchians, reflecting their small body size and paedomorphic retention of basal morphologies. INDETERMINATE REMAINS PREVIOUSLY ATTRIBUTED TO ATOPOSAURIDAE Alongside these named taxa, numerous additional remains (primarily teeth) have been referred to Ato- posauridae. These referrals have generally been based on the dental morphotypes that have been regarded as characteristic of Theriosuchus and, in stratigraphical order, comprise: 1. Teeth comparable to those of Theriosuchus were described from two localities from the early Bathonian of southern France (Kriwet et al., 1997). Their referral to Atoposauridae was based on the presence of different morphotypes, and the teeth were thought to represent two distinct species. The first of these ‘ species’ includes several dozen teeth (Larnagol, IPFUB Lar-Cr 1 - 20, and Gardies, IPFUB Gar-Cr 1 - 20). Amongst this set of teeth, Kriwet et al. (1997) identified four gradational morphotypes, based on their inferred positions in the dental arcade. However, their referral to Atoposauridae is based mainly upon them being heterodont, a feature that is not exclusive to either Atoposauridae or Theriosuchus. The second ‘ species’ (Larnagol, IPFUB Lar-Cr 21 - 40) differs in possessing more prominent ridges on the crown surfaces (Kriwet et al., 1997). These were referred to Atoposauridae by Kriwet et al. (1997) based on their inferred heterodonty; however, it cannot be determined whether or not all of these morphotypes belong to the same heterodont taxon, or two or more homodont or heterodont taxa. As atoposaurids are now considered to have a homodont (pseudocaniniform) dental morphology, these teeth cannot be referred to this group. They probably represent at least one (and probably more) small-bodied heterodont taxon, and therefore we consider them to be only referable to Mesoeucrocodylia indet. at present. 2. Small crocodyliform teeth were noted from the Bathonian ‘ stipite’ layers of the Grand Causses (France) by Knoll et al. (2013) and Knoll & Lopez-Anto nanzas ~ (2014), and referred to an indeterminate atoposaurid. No further details were given, and therefore we regard these as representing indeterminate crocodyliforms pending further description of this material. 3. 1391 specimens comprising teeth, osteoderms, and a jaw fragment with teeth, as well as undescribed cranial and postcranial specimens, from the Bathonian of Madagascar were referred to Atoposauridae (Flynn et al., 2006). Based on the description and figures provided, these teeth appear to be pseudocaniniform in morphology, with well-developed mesial and distal carinae and a ridged enamel surface. Although they vary in shape and size (up to 10 mm in apicobasal length), none can be defined as pseudoziphodont, ziphodont, lanceolate, labiolingually compressed, or low-crowned. Based on the brief description, we cannot conclude that these teeth belonged to an atoposaurid, and therefore regard them as Mesoeucrocodylia indet., pending further description. Further examination of this material, along with remains identified as Theriosuchus sp. by Haddoumi et al., [2016 (see above)], will be important in examining evidence for the presence of atoposaurids and Theriosuchus in the Middle Jurassic of Gondwana. 4. Thies & Broschinksi (2001) described teeth from the Kimmeridgian of northern Germany as ‘ Theriosuchus - like’, but identified them as belonging to a small-bodied mesosuchian. Karl et al. (2006) provisionally referred these teeth to Mesoeucrocodylia indet., stating that their morphology is not known for any other crocodylomorph. We follow this decision of Karl et al. (2006), pending the direct comparison of this material with Theriosuchus and other small-bodied crocodyliforms. 5. A fragmentary set of specimens (IVPP V 10613) from the Early Cretaceous of Inner Mongolia, including cranial and mandibular elements, were assigned to cf. Theriosuchus sp. (Wu et al., 1996). However, the material might not be referable to a single individual or even taxon, as it was collected from across an extensive outcrop. The figured osteoderm (Wu et al., 1996) is almost identical in overall morphology to Alligatorellus sp. (MB. R. 3632; Schwarz-Wings et al., 2011), including the position and extent of the lateral keel, and the near-absence of the anterior process of the ilium is similar to that of Montsecosuchus. The dorsal vertebrae possess the ‘ semi-procoelous’ condition, similar to Pachycheilosuchus. The cranioquadrate canal is closed, and therefore IVPP V 10613 can be excluded from Atoposauridae. The external mandibular fenestra is absent, similar to paralligatorids and T. pusillus. Additionally, the parietals bear a longitudinal median ridge on the dorsal surface, which Wu et al. (1996) used to link IVPP V 10613 with Theriosuchus, although this feature is herein shown to be more widespread throughout Neosuchia. Wu et al. (1996) assigned IVPP V 10613 to Therio- suchus based on the broad intertemporal region, raised supratemporal rims, and elevated medial orbital margin, but these features are found in numerous other taxa. Based on this combination of unusual characteristics, we think it likely that IVPP V 10613 comprises more than one taxon, including at least one non-atoposaurid, non- Theriosuchus taxon, and one Theriosuchus - like taxon. We therefore regard IVPP V 10613 as representing Neosuchia indet. pending further study of this material. 6. A skull fragment (NHMUK PV OR 176) was assigned to Theriosuchus sp. from the Berriasian – Barremian of the Isle of Wight, UK (Buffetaut, 1983; Salisbury & Naish, 2011). Buffetaut (1983) assigned the posterior portion of a skull to Theriosuchus sp. based on comparison with the lectotype specimen of T. pusillus (NHMUK PV OR 48216). It has a median longitudinal ridge on the parietal, similar to all specimens assigned to Theriosuchus, but also to Alligatorium meyeri and paralligatorids. The otoccipitals also meet dorsal to the foramen magnum, separating it from the supraoccipitals, a feature shared with T. pusillus, T. guimarotae, and paralligatorids. The contact between the parietal and the squamosal on the dorsal surface, posterior to the external supratemporal fenestra, is also weakly developed, not forming the deep groove that characterizes T. pusillus. Therefore, we cannot determine whether this specimen represents Theriosuchus or another advanced neosuchian, and thus we consider this specimen to represent Neosuchia indet., pending its comparison to a broader set of neosuchians. In addition, Buffetaut (1983) assigned some procoelous vertebrae (the type of ‘ Heterosuchus valdensis ’) from the Early Cretaceous of the UK to Theriosuchus. The presence of procoely indicates that it is not referable to Theriosuchus (see below), and it is instead regarded as an indeterminate neosuchian. 7. Indeterminate remains (primarily teeth) attributed to atoposaurids, usually referred to Theriosuchus based on heterodont tooth morphotypes, have been identified from numerous sites in the Aptian – Albian (late Early Cretaceous) of North America (e. g. Pomes, 1990; Winkler et al., 1990; Cifelli et al., 1999; Eaton et al., 1999; Fiorillo, 1999; Garrison et al., 2007; Oreska, Carrano & Dzikiewicz, 2013). However, because of our removal of Theriosuchus from Atoposauridae, it is more likely that these ‘ atoposaurid’ remains represent other small-bodied taxa. We tentatively consider these remains to represent Mesoeucrocodylia indet., pending further study. 8. Theriosuchus - like teeth (MTM V 2010.243.1) were described from the Santonian of western Hungary (Iharkut), but conservatively referred to Mesoeucrocodylia indet (Osi € et al., 2012). These teeth are lanceolate in crown morphology, and possess pseudoziphodont carinae. Martin et al. (2014 a) briefly mentioned the presence of two additional undescribed maxillae from the same locality, which together with the teeth might be referable to Theriosuchus. As we have recombined the Maastrichtian occurrences of ‘ Theriosuchus ’ into a new taxon, Sa. sympiestodon, it is best that these teeth be regarded as Neosuchia indet., pending further analysis of this material and the possibly associated maxillae. 9. A Theriosuchus - like tooth was described from the Campanian – Maastrichtian of Portugal by Galton (1996). This tooth is distinct from Theriosuchus, possessing a fully ziphodont morphology, and was suggested to instead belong to Bernissartia (Lauprasert et al., 2011). However, here we consider it to belong to an indeterminate neosuchian based on the more widespread distribution of ziphodont dentition. 10. The stratigraphically youngest material assigned to Atoposauridae comes from the middle Eocene Kaninah Formation of Yemen (Stevens et al., 2013). This fragmentary material was tentatively designated as an atoposaurid, based on the presence of a ziphodont tooth crown, a procoelous caudal vertebral centrum, a biserial osteoderm shield (although see below), and polygonal gastral osteoderms. However, none of these characteristics is unambiguously diagnostic under our revised definition of Atoposauridae, and this material probably comprises a small, advanced eusuchian, based on the presence of procoelous caudal vertebrae. The presence of a biserial osteoderm shield is usually considered diagnostic for Atoposauridae; however, our analyses demonstrate that this feature is more widespread amongst smallbodied neosuchians. Furthermore, the material from Yemen is too fragmentary to confidently infer that the osteoderm shield was biserial. Therefore, we regard this material as an indeterminate eusuchian pending the discovery of more complete and better preserved specimens.	en	Tennant, Jonathan P., Mannion, Philip D., Upchurch, Paul (2016): Evolutionary relationships and systematics of Atoposauridae (Crocodylomorpha: Neosuchia): implications for the rise of Eusuchia. Zoological Journal of the Linnean Society 177 (4): 854-936, DOI: 10.1111/zoj.12400, URL: http://doi.wiley.com/10.1111/zoj.12400
