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Expanded Sampling Across Ontogeny in Deltasuchus motherali (Neosuchia, Crocodyliformes)

Revealing Ecomorphological Niche Partitioning and Appalachian Endemism in Cenomanian Crocodyliforms

Published online by Cambridge University Press:  30 April 2021

Stephanie K. Drumheller
Affiliation:
University of Tennessee, Knoxville
Thomas L. Adams
Affiliation:
Witte Museum
Hannah Maddox
Affiliation:
University of Tennessee, Knoxville
Christopher R. Noto
Affiliation:
University of Wisconsin, Parkside

Summary

New material attributable to Deltasuchus motherali, a neosuchian from the Cenomanian of Texas, provides sampling across much of the ontogeny of this species. Detailed descriptions provide information about the paleobiology of this species, particularly with regards to how growth and development affected diet. Overall snout shape became progressively wider and more robust with age, suggesting that dietary shifts from juvenile to adult were not only a matter of size change, but of functional performance as well. These newly described elements provide additional characters upon which to base more robust phylogenetic analyses. The authors provide a revised diagnosis of this species, describing the new material and discussing incidents of apparent ontogenetic variation across the sampled population. The results of the ensuing phylogenetic analyses both situate Deltasuchus within an endemic clade of Appalachian crocodyliforms, separate and diagnosable from goniopholidids and pholidosaurs, herein referred to as Paluxysuchidae. This title is also available as Open Access on Cambridge Core.
Type
Element
Information
Online ISBN: 9781009042024
Publisher: Cambridge University Press
Print publication: 03 June 2021
Creative Commons
Creative Common License - CCCreative Common License - BYCreative Common License - NCCreative Common License - ND
This content is Open Access and distributed under the terms of the Creative Commons Attribution licence CC-BY-NC-ND 4.0 https://creativecommons.org/cclicenses/

1 Introduction

Starting in the mid-Cretaceous, the spread of the Western Interior Seaway divided North America in half, an event that should lend itself well to explorations of vicariance in terrestrial and freshwater taxa. However, such analyses are stymied by two separate taphonomic biases. First, the North American record is temporally biased, with spikes in diversity being known in the Aptian–Albian and the Campanian–Maastrichtian with few terrestrial sites in between (Reference Jacobs, Winkler, Tomida, Flynn and JacobsJacobs and Winkler, 1998; Reference Weishampel, Barrett, Coria, eishampel, Dodson and OsmólskaWeishampel et al., 2004; Reference Zanno and MakovickyZanno and Makovicky, 2013). Secondly, what mid-Cretaceous sites we do have are geographically biased as well, concentrated on the western landmass of Laramidia (Reference Ullmann, Varricchio and KnellUllmann et al., 2012; Reference Krumenacker, Simon, Scofield and VarricchioKrumenacker et al., 2016; Reference Prieto-Márquez, Erickson and EbersolePrieto-Márquez et al., 2016). Appalachia, to the east, has remained something of a mystery, but recent discoveries are starting to reveal aspects of the diversity of this understudied landmass (e.g. Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference BrownsteinBrownstein, 2018; Reference Adrian, Smith, Noto and GrossmanAdrian et al., 2019; Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019).

The Woodbine Group outcrops across north-central Texas and is situated within both this temporal and geographic gap. Dating to 96 Ma and situated on the western paleocoastline of Appalachia (Reference Powell and DodgePowell, 1968; Reference DodgeDodge, 1969; Reference Kennedy and CobbanKennedy and Cobban, 1990; Reference Emerson, Emerson, Akers and AkersEmerson et al., 1994; Reference LeeLee, 1997a, Reference Lee1997b; Reference Jacobs, Winkler, Tomida, Flynn and JacobsJacobs and Winkler, 1998; Reference Gradstein, Ogg and SmithGradstein et al., 2004), the Woodbine long has provided tantalizing hints to Appalachian diversity. Unfortunately, fossils from this unit are often fragmentary and isolated, frustrating taxonomic identification beyond broad groupings of Cretaceous organisms (Reference LeeLee, 1997a; Reference HeadHead, 1998; Reference Jacobs, Winkler, Tomida, Flynn and JacobsJacobs and Winkler, 1998; Reference Adams, Polcyn, Mateus, Winkler and JacobsAdams et al., 2011). The Arlington Archosaur Site (AAS) is an unusual outlier amidst other Woodbine localities. The quality of preservation and the density of recovered fossil material are both unusually high, providing a window into the paleoecosystem of the Cenomanian coastline (e.g. Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference BrownsteinBrownstein, 2018; Reference Adrian, Smith, Noto and GrossmanAdrian et al., 2019; Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019).

As its name suggests, the site is particularly rich in archosaurian fossils, with at least four crocodyliform (Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019) and five dinosaur taxa (Reference Main, Noto, Weishampel, Eberth and EvansMain et al., 2014; Reference NotoNoto, 2016) known from the locality. Among these taxa, the most common species recovered from the AAS is the large neosuchian crocodyliform Deltasuchus motherali (Reference Adams, Noto and DrumhellerAdams et al., 2017). Originally described from a single, adult individual, ongoing research and collection of AAS materials have revealed numerous smaller-bodied specimens attributable to this taxon. Furthermore, searches of museum collections at Southern Methodist University (SMU) and the Witte Museum (WM) have resulted in the identification of additional D. motherali elements from Bear Creek (SMU Locality 245) near the south entrance to Dallas–Fort Worth International Airport. Here we describe juvenile to adult Deltasuchus elements, emphasizing ontogenetic change seen across the group. We also expand the original phylogenetic analysis of D. motherali with new elements preserved in these additional specimens, and increase taxon sampling to further explore a seemingly endemic, Appalachian radiation of neosuchians.

Anatomical Abbreviations

– Alveolar and dental positions are named with the first letter of the supporting bone (p for premaxilla, m for maxilla, d for dentary) and the number of the alveolus or tooth counting from mesial to distal along the toothrow; ang, angular; ar, articular; ars, articular sutural surface; cqc, cranioquadrate canal; d, dentary; ects, ectopterygoid sutural surface; fae, foramen aëreum; f, frontal; fio, foramen intermandibularis oralis; fs, frontal sutural surface; gf, glenoid fossa; ics, intercondylar sulcus; j, jugal; js, jugal sutural surface; lac, lacrimal; lac no, lacrimal notch; lac plp, lacrimal posterolateral process; lacs, lacrimal sutural surface; lacrimal; lac js, lacrimal-jugal sutural surface; lhc, lateral hemicondyle; mAME, M. adductor mandibulae externus; mhc, medial hemicondyle; mx, maxilla; mxs, maxillary sutural surface; nar, naris; nas, nasal sutural surface; op, occlusal pit; par, parietal; pars, parietal sutural surface; parops, paroccipital process sutural surface; pmx, premaxilla; pmx mxs, premaxillary-maxillary sutural surface; pob, postorbital bar; pos, postorbital sutural surface; prf, prefrontal; prfp, prefrontal pillar; prfs, prefrontal sutural surface; q, quadrate; qad, quadrate anterodorsal process; qat, adductor tubercle of the quadrate; qd, quadrate dorsal process; qjs, quadratojugal sutural surface; qpt, quadrate pterygoid process; qvf, ventral fossa of the quadrate; qs, quadrate sutural surface; ra, retroarticular process; roe, external otic recess; sp, splenial; sps, splenial sutural surface; sq, squamosal; sqj, spina quadratojugalis; sqs, squamosal sutural surface; sur, surangular; surs, surangular sutural surface; sym, mandibular symphysis; uef, groove for upper ear valve.

Institution Abbreviation

DMNH, Perot Museum of Nature and Science, Dallas, Texas, USA; SMU, Southern Methodist University Shuler Museum of Paleontology, Dallas, Texas, USA; WM, Witte Museum, San Antonio, Texas, USA.

2 Age and Geologic Setting

The Upper Cretaceous (middle to upper Cenomanian) Woodbine Group of Texas represents a series of fully marine to terrestrial rocks deposited as a southward thinning clastic wedge in the Gulf Coast Basin (Figure 1) (Reference DodgeDodge, 1952, Reference Dodge1969; Reference OliverOliver, 1971). Recent studies based on subsurface data classify the Woodbine as a third-order regressive sequence deposited over ~1.5 million years, with source sediments originating from the Ouachita and Arbuckle Mountains of Oklahoma and Arkansas (Reference Ambrose, Hentz and BonafféAmbrose et al., 2009; Reference Adams and CarrAdams and Carr, 2010; Reference Blum and PechaBlum and Pecha, 2014; Reference Hentz, Ambrose and SmithHentz et al., 2014). Its lower boundary is formed by an unconformity with the Grayson Marl (Washita Group) while its upper boundary is formed by an unconformity with the Eagle Ford Group (Reference DodgeDodge, 1969; Reference OliverOliver, 1971; Reference JohnsonJohnson, 1974). Presence of the ammonite zonal marker Conlinoceras tarrentense in the upper Woodbine establishes a minimum age of early middle Cenomanian (~96 million years) (Reference Kennedy and CobbanKennedy and Cobban, 1990; Reference Emerson, Emerson, Akers and AkersEmerson et al., 1994; Reference Jacobs, Winkler, Tomida, Flynn and JacobsJacobs and Winkler, 1998; Reference Gradstein, Ogg and SmithGradstein et al., 2004), with deposition ending no later than 92 million years (Reference Ambrose, Hentz and BonafféAmbrose et al., 2009).

Figure 1  Location and geologic setting of the AAS and Bear Creek. A, stratigraphic column for the Upper Cretaceous of north-central Texas showing the position of the Woodbine Group relative to timescale and adjacent geologic units. Stippled intervals represent terrestrial deposits. Star indicates position of the AAS and Bear Creek sites. Time scale based on Reference Gradstein, Ogg and SmithGradstein et al. (2004). B, generalized map of geologic units in the Fort Worth Basin, showing enlarged area from white box of inset map of Texas.

Woodbine stratigraphy is complex, with differing interpretations arising from surface outcrop and subsurface core and wireline data, themselves derived from widely different locations within the depositional basin (Reference DodgeDodge, 1969; Reference OliverOliver, 1971; Reference JohnsonJohnson, 1974; Reference Ambrose, Hentz and BonafféAmbrose et al., 2009; Reference Adams and CarrAdams and Carr, 2010; Reference Hentz, Ambrose and SmithHentz et al., 2014). In the Dallas–Fort Worth area four units are typically recognized (in ascending order): Rush Creek, Dexter, Lewisville, and Arlington (Reference DodgeDodge, 1969). The lower Rush Creek and Dexter represent marginal to fully marine deposits, while the upper Lewisville and Arlington represent terrigenous fluvio-deltaic environments all influenced by eustatic sea-level changes (Reference Powell and DodgePowell, 1968; Reference OliverOliver, 1971; Reference JohnsonJohnson, 1974; Reference Ambrose, Hentz and BonafféAmbrose et al., 2009; Reference Adams and CarrAdams and Carr, 2010; Reference Hentz, Ambrose and SmithHentz et al., 2014).

The Arlington Archosaur Site (AAS) is situated within the upper Woodbine (Lewisville) and consists of a 200 m long, 5 m thick hillside exposure, with 50 m representing the main fossil quarry (Figure 1B). This outcrop preserves a coastal environment that includes a mixture of marine, freshwater, and terrestrial influences (Reference Noto, Main and DrumhellerNoto et al., 2012; Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019). The outcrop is divided into four distinct facies, recording a transition from primarily terrestrial to primarily marine deposition (Reference MainMain, 2013; Reference Adams, Noto and DrumhellerAdams et al., 2017). The majority of fossils are found in the lowermost facies, which most likely represents a freshwater or brackish wetland deposited within a lower delta plain system (Reference Noto, Main and DrumhellerNoto et al., 2012; Reference MainMain, 2013; Reference Adams, Noto and DrumhellerAdams et al., 2017). The AAS is remarkable for the sheer number and diversity of organisms recovered (at least 37 unique vertebrate taxa to date, as well as invertebrates and plants) and the quality of preservation of the material (Reference NotoNoto, 2015; Reference Adams, Noto and DrumhellerAdams et al., 2017).

Bear Creek (SMU locality 245, Figure 1B) is positioned in the uppermost Woodbine (Arlington) and represents the transition phase of the Woodbine Formation into the deeper marine shale facies of the Eagle Ford Group (Reference LeeLee, 1997a). This site has produced numerous fossil remains, including teeth and bone fragments of crocodyliforms and dinosaurs. The outcrop consists of a lower shaly sandstone unit and an upper sandy shale unit interbedded with thin fossiliferous sandstone that contain dark, lignitic, and carbonaceous layers. Thin units consist of very fine- to fine-grained sandstone with ferruginous cement, iron concretions, chert pebbles, and phosphatic nodules. A phosphatic pebble conglomerate surface, marking a transgressive lag deposit, is rich in reworked vertebrate teeth and small fragments including fishes, frogs, turtles, crocodiles, dinosaurs, and a mammal (Reference LeeLee, 1997a). The uppermost Woodbine preserves a terrigenous coastal depositional system with fluvio-deltaic influences (Reference Powell and DodgePowell, 1968; Reference DodgeDodge, 1969; Reference LeeLee, 1997a, Reference Lee1997b; Reference Jacobs, Winkler, Tomida, Flynn and JacobsJacobs and Winkler, 1998) and represents a low-stand sequence within an early transgressive system tract of the Greenhorn Cycle of Reference Kauffman, Caldwell, Kauffman and CaldwellKauffman and Caldwell (1993).

The taphonomy of these sites is also complex, representing a largely time-averaged assemblage formed through a variety of taphonomic modes, including subaerial exposure, aqueous transport, and predation (Reference Noto, Main and DrumhellerNoto et al., 2012; Reference Main, Noto, Weishampel, Eberth and EvansMain et al., 2014; Reference NotoNoto, 2015; Reference Adams, Noto and DrumhellerAdams et al., 2017). Within the fossil-rich layer of the AAS (Facies A sensu Reference Adams, Noto and DrumhellerAdams et al., 2017), elements are generally well-preserved, if disarticulated. The presence of mixed marine, brackish, freshwater, and terrestrial taxa suggest a parautochthonous assemblage, sampled from across the paleodeltaic system, but common vertebrate coprolites, as well as the high quality of the fossil preservation and the minimal spread of associated skeletal elements, indicate that transport was low energy and fairly minimal (Reference McNulty, Slaughter and DodgeMcNulty and Slaughter, 1968; Reference RussellRussell, 1988; Reference Cumbaa, Shimada and CookCumbaa et al., 2010; Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019).

Most fossils were collected in situ and these elements are a rich, chocolate brown color. The surface quality is high, and the remains are preserved in three dimensions, but a few exhibit minor compression and distortion (e.g. the left maxilla and the right dentary/splenial of DMNH 2013–07–1859). Elements that were collected at or near the surface have been exposed to more extensive weathering and mineral overgrowth, resulting in changes in color, texture, and overall preservational quality. These elements range from a light brown to light gray color, and take on a chalky appearance (e.g. right premaxilla DMNH 2013–07–1636 and left quadrate DMNH 2013–07–0733). A small number exhibit extensive gypsum overgrowth (e.g. DMNH 2014–06–01, a poorly preserved, left angular).

3 Systematic Paleontology

Phylogenetic Definition

– Branch-based clade comprising all taxa more closely related to Paluxysuchus newmani Reference AdamsAdams, 2013, than to either Goniopholis crassidens Reference OwenOwen, 1841 or Pholidosaurus schaumburgensis Reference MeyerMeyer, 1841.

Diagnosis

– Members of this clade are mid- to large-sized neosuchian crocodylomorphs diagnosable not by autapomorphies, but instead by a unique combination of characters present in other clades (specifically Goniopholididae and Tethysuchia): platyrostral mesorostrine skull (shared with some goniopholidids); maxilla festooned, with well-defined anterior wave, projecting laterally and ventrally (shared with some goniopholidids); posterior ramus of prefrontal is long, reaching the median region of the orbits (shared with goniopholidids and pholidosaurids); lacrimal reaches the anteroventral margin of the orbit; jugal does not exceed the anterior margin of orbit (shared with tethysuchians); the posterior ramus of the jugal beneath the infratemporal fenestra is rod-shaped (shared with pholidosaurids); median process of the frontal extends anterior to the tip of the prefrontal (shared with tethysuchians); postorbital with anterolateral process present (shared with goniopholidids and pholidosaurids); contact between the descending process of the postorbital and the ectopterygoid; no external mandibular fenestra (shared with some goniopholidids and pholidosaurids); surangular extends to the posterior region of the retroarticular process; retroarticular process facing dorsally and paddle shaped (shared with pholidosaurids).

Holotype

– DMNH 2013–07–0001, partial skull and mandible.

Referred Material

– DMNH 2013–07–1859, partial skull and mandible; DMNH 2014–06–01, partial mandible; DMNH 2013–07–0079, right dentary and maxilla; DMNH 2013–07–0297, left premaxilla, right premaxilla; DMNH 2013–07–1888, right dentary; DMNH 2013–07–0239, left dentary; DMNH 2013–07–0218, right dentary; DMNH 2013–07–1984, right dentary; DMNH 2013–07–0240, left dentary; DMNH 2013–07–0322, left dentary; DMNH 2013–07–0228, left dentary; DMNH 2013–07–0312, right dentary; DMNH 2013–07–0802, right dentary; DMNH 2013–07–0219, left maxilla; DMNH 2013–07–1404d, left prefrontal; DMNH 2013–07–0733, left quadrate; DMNH 2013–07–0084, left lacrimal; DMNH 2013–07–1871, frontal; DMNH 2013–07–1992, left and right quadratojugals, left and right quadrates; DMNH 2013–07–1993, left lacrimal; DMNH 2013–07–1994, partial right exoccipital; DMNH 2013–07–1995, right prefrontal; DMNH 2013–07–1997, right quadrate; DMNH 2013–07–1975, right prefrontal, left jugal; DMNH 2013–07–0178, teeth; SMU 76810, articulated right surangular and angular; WM 2019–15 Ga, left premaxilla; WM 2019–15 Gb, tooth.

Revised Diagnosis

– A member of Paluxysuchidae differing from other known neosuchians in having the following unique combination of characters and autapomorphies (* = additional characteristics relative to Reference Adams, Noto and DrumhellerAdams et al., 2017): anterior premaxilla ventrally directed, overbites the dentary (shared with goniopholidids and tethysuchians); postnarial fossa present on the premaxilla; dual pseudocanines on both the dentary and maxilla; frontal excluded from the orbital margin (an autapomorphy for the group)*; anterolaterally facing margin on the dorsal portion of the postorbital; deep fossa on the ventral surface of the quadrate (shared with some pholidosaurids); medial quadrate condyle expands ventrally, separated from lateral condyle by deep intercondylar sulcus; the mandibular symphysis extends posteriorly to the level of the eighth dentary alveolus.

4 Description

4.1 General Description

The AAS is extremely rich in fossil crocodyliforms, with multiple individuals and at least four and perhaps five taxa known from the site (Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019). Of these, the best represented taxon is Deltasuchus motherali. The holotype of D. motherali (DMNH 2013–07–0001) includes associated, but disarticulated, craniomandibular elements ascribable to a large, adult neosuchian crocodyliform. The specimen is incomplete, including both premaxillae, maxillae, and nasals, a left postorbital, a left jugal, a right squamosal, both quadrates, a right otoccipital, the basioccipital, both ectopterygoids, and fragments of the pterygoids and dentaries. Based on a reconstructed cranial length of 800 mm, the total body length of the holotype animal is estimated at between 5.6 and 6 m in length. Unlike other large-bodied crocodyliforms known from the mid-Cretaceous of Texas, who exhibit more specialized slender snouts, e.g. Terminonaris and Woodbinesuchus, Deltasuchus has a robust, broadly triangular snout.

Multiple smaller-bodied individuals ascribable to D. motherali are also known from the AAS. By far the most complete specimen, other than the holotype (DMNH 2013–07–0001), belongs to an individual that, when articulated, is roughly half the size of the holotype (DMNH 2013–07–1859). Like the holotype (Reference Adams, Noto and DrumhellerAdams et al., 2017), DMNH 2013–07–1859 includes associated, but disarticulated, cranial and mandibular elements (Figure 2). However, association of these elements to one individual is justified for the following reasons: adjacent elements articulate well along sutural surfaces, all elements were found in close physical proximity to one another within the same bedding plane, and there is no duplication of right and left elements within the skull. At 440 mm in cranial length (measured from the anteriormost tip of the premaxilla, along the midline, to the posteriormost margin of the skull table), this individual would have been between 3.08 and 3.30 m in total body length (sensu Reference SchmidtSchmidt, 1944; Reference BellairsBellairs, 1969; Reference Adams, Noto and DrumhellerAdams et al., 2017).

Figure 2 Subadult D. motherali (DMNH 2013–07–1859). Cranial elements in A, dorsal view and mandible in B, dorsal and lateral views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

DMNH 2013–07–1859 exhibits the following unique combination of characters that can diagnose it to Paluxysuchidae: enlarged supratemporal fenestrae; paired pseudocanines in the maxilla (m4 and m5), posterior process of the premaxilla overlaps anterodorsal surface of the maxilla anterolaterally, then transition to a butt joint posteromedially; anterior process of the frontal extends anterior to the tip of the prefrontal. It can be assigned to D. motherali, as opposed to Terminonaris and Woodbinesuchus also present in the Woodbine, based on its more robust, widely triangular snout shape, ventrally directed premaxilla, and the extremity of the expansion of the pseudocanines, as well as the associated bulging of the lateral margins of the maxilla which accommodate that enlarged dentition (Reference Adams, Noto and DrumhellerAdams et al., 2017).

A second individual (DMNH 2014–06–01) is represented by a partial mandible; including left and right articulars, an articulated left angular and surangular and a disarticulated right angular, surangular, and a small portion of posterior dentary (Figure 3). In addition to the elements on each side articulating with one another, these elements were found in close physical proximity and exhibit matching sizes, though the elements from the left side of the jaw exhibit poorer quality surface preservation. This individual would have been of similar size to, and is morphologically indistinguishable from, DMNH 2013–07–1859, but duplication of elements signifies that they do represent two separate animals.

Figure 3 Mandible elements of D. motherali (DMNH 2014–06–01). Right dentary in A, lateral view; right surangular in B, lateral view; right angular in C, lateral view; left surangular and angular in D, lateral view, dashed line indicating sutural boundary between the angular and surangular; left and right articulars in E, dorsal views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

The second set includes a right maxilla and a right anterior fragment of a dentary that were found in direct association with one another (DMNH 2013–07–0079) (Figure 4A–D). This individual exhibits the paired pseudocanines on both maxilla and dentary expected of the clade, and other than being only slightly larger than the other two juveniles previously described, is morphologically similar to these other specimens. Duplication of elements further differentiates it from DMNH 2013–07–1859. As a comparison of size, the right dentary of DMNH 2013–07–0079 is 34.79 mm wide in ventral view at the level of the d4 alveolus while the right dentary of DMNH 2013–07–1859 is 31.10 mm wide in the same dimension. Scaling the length estimate based on these measurements yields an animal between 3.45 and 3.69 m in total length.

Figure 4 Adult and subadult individuals of D. motherali. DMNH 2013–07–0079 right maxillae in A, dorsal and B, ventral views; right dentary in C, dorsal and D, ventral views; DMNH 2013–07–0297, premaxillae in E, dorsal view; WM 2019–15 Ga, left premaxilla in F, dorsal view. SMU 76810, right surangular and angular in G, lateral view. See text for anatomical abbreviations.

Scale bar equals 5 cm.

Three larger individuals are represented by isolated elements. DMNH 2013–07–0297 are paired premaxillae that articulate along their sutural margin (Figure 4E). The maximum width of the right premaxillae is 44.70 mm, at the level of p4. When compared to the more complete holotype, DMNH 2013–07–0001, which is 74 mm wide in this dimension, scaling between the two suggest an animal that would have been between 3.38 and 3.62 m in total length. WM 2019–15 Ga from Bear Creek is a nearly complete left premaxilla, missing only the narrow posterior process (Figure 4F). The maximum width at the level of p4 is 59.31 mm, indicating a body length of between 4.49 and 4.81 m. The third large individual also comes from Bear Creek. SMU 76810 is an articulated partial right surangular and angular (Figure 4G). It is well-preserved and nearly as large as the surangular of the holotype, DMNH 2013–07–001.

Additionally, at least four left (DMNH 2013–07–0228; DMNH 2013–07–0240 DMNH 2013–07–0322; DMNH 2013–07–0239) (Figure 5A–D) and four right dentaries (DMNH 2013–07–1984; DMNH 2013–07–0218; DMNH 2013–07–0802; DMNH 2013–07–0312) (Figure 5E–H) are known from the site. These dentaries range from highly fragmentary to nearly complete, and all are distinguishable from one another based on size. All exhibit the enlarged d3 and d4 dentition or associated alveoli and the spatulate symphyseal region as seen in this clade. Similar measurements of dentary width at d4 were made to all specimens that included this undamaged portion of bone, yielding the following additional body size estimates: DMNH 2013–07–0228 was 1.38–1.49 m long (based on 13.93 dentary width); DMNH 2013–07–0240 was 1.46–1.56 m long (based on 14.73 mm dentary width); DMNH 2013–07–0802 was 1.65–1.77 m long (based on 16.69 mm dentary width); DMNH 2013–07–0322 was 1.94–2.08 m long (based on 19.57 dentary width); DMNH 2013–07–1984 was 2.03–2.17 m long (based on 20.48 dentary width); DMNH 2013–07–0239 was 2.52–2.70 m (based on 33.07 mm dentary width).

Figure 5 Orthographic image of 3D digital models demonstrating size comparison of dentaries for juvenile and subadult individuals of D. motherali. DMNH 2013–07–0239, left dentary in A, dorsal view; DMNH 2013–07–0322, left dentary in B, dorsal view; DMNH 2013–07–0240, left dentary in C, dorsal view; DMNH 2013–07–0228, left dentary in D, dorsal view; DMNH 2013–07–1984, right dentary in E, dorsal view; DMNH 2013–07–0802, right dentary in F, dorsal view; DMNH 2013–07–0218, right dentary in G, dorsal view; DMNH 2013–07–0312, right dentary in H, lateral view.

Scale bar equals 5 cm.

Taken all together, this yields a minimum estimate of Deltasuchus individuals currently known from the upper Woodbine of 15. These animals ranged from just under 1.5 m long to roughly 6 m in total length, providing a cross section of individuals across much of the ontogenetic history of the group (Figure 6). In fossil crocodyliforms, defining maturity often relies on patterns of sutural closure, especially in vertebrae (Reference BrochuBrochu, 1996; Reference IkejiriIkejiri, 2012). Sutural closure in other elements across the crocodyliform body, especially within the skull, can only provide broad brushstroke patterns of maturity during earliest development, with significant variation observed even within extant taxa (Reference Bailleul, Scannella, Horner and EvansBailleul et al., 2016). While crocodyliform vertebrae are known from the AAS and Bear Creek, as are long bones that could be used for histological analysis, these postcranial elements are not easily associated with any one of the several taxa present at these sites. That leaves our discussion of ontogeny limited to craniomandibular elements. Given the sizes and patterns of sutural closures present in all the specimens described herein, we are confident that we do not have any identifiable neonate remains of Deltasuchus. For the sake of comparison and discussion, we will therefore group the individuals estimated to be less than 2.5 m in length as juveniles, the 2.5 to 4 m-individuals as subadults, and anything above 4 m long as an adult animal.

Figure 6 Size comparison of juvenile (less than 2.5 m), subadult (2.5 to 4.0 m), and adult (greater than 4.0 m) individuals of D. motherali.

Scale bar equals 1 m.

Except where indicated, the element descriptions below refer to the most complete subadult individual, DMNH 2013–07–1859. Several of these elements were not preserved or were fragmentary in the holotype specimen. Other specimens are included to capture morphologies that are not represented in this animal as well as aspects of ontogenetic change observable in each element.

4.2 Premaxilla

DMNH 2013–07–1859 (Video 1) preserves a complete left premaxilla, while DMNH 2013–07–0297 (Video 2) represents a partial left and right premaxillae preserved in three pieces and WM 2019–15 Ga is a large, left premaxilla missing only the posterior process (Figure 7). The anterior terminus of the premaxilla is transversely broad and strongly deflected ventrally, reminiscent of Sarcosuchus (Reference Sereno, Larsson, Sidor and GadoSereno et al., 2001), Kaprosuchus saharicus (Reference Sereno and LarssonSereno and Larsson, 2009), Elosuchus and most members of Goniopholididae (Reference Meunier and LarssonMeunier and Larsson, 2017; Reference Jouve, de Muizon, Cespedes-Paz, Sossa-Soruco and KnollJouve et al., in press), so that the premaxilla occludes anterior to the anterior dentary (Figure 8). This beak-like overbite previously has been interpreted as an adaptation for stabilizing and aligning jaw closure in taxa with elongated snouts with powerful bite forces (e.g. Oceanosuchus in Reference Hua, Buffetaut, Legall and RogronHua et al., 2007). While adult Deltasuchus did not have a particularly narrow snout as compared to Terminonaris and Woodbinesuchus (see Section 6, Discussion), younger members of this taxon, as well as members of its sister taxon, Paluxysuchus (Reference AdamsAdams, 2013), did have comparatively narrow jaws. The presence of this feature is therefore likely due to a combination of factors: (1) inheritance of a plesiomorphic condition, as many taxa in this region of the tree, especially the goniopholidids Anteophthalmosuchus epikrator, Amphicotylus stovalli and Goniopholis kiplingi and the pholidosaurs Chalawan, Sarcosuchus, and Terminonaris, share this trait (Reference Sereno, Larsson, Sidor and GadoSereno et al., 2001; Reference Wu, Russell and CumbaaWu et al., 2001; Reference Andrade, Edmonds, Benton and SchoutenAndrade et al., 2011; Reference Martin, Lauprasert, Buffetaut, Liard and SuteethornMartin et al., 2014; Reference Young, Hastings, Allain and SmithYoung et al., 2016; Reference Ristevski, Young, Andrade and HastingsRistevski et al., 2018); and (2) ontogenetic inertia (sensu Reference Gignac and O’BrienGignac and O’Brien, 2016), given that the stabilizing aspects of this trait would have proven more advantageous to the more slender-snouted juveniles than the broader-faced adults.

Video 1 Orthographic digital model of the left premaxilla from a subadult D. motherali, DMNH 2013–07–1859. Video available at www.cambridge.org/drumheller.

Video 2 Orthographic digital model of the articulated premaxillae from an adult D. motherali, DMNH 2013–07–0297. Video available at www.cambridge.org/drumheller.

Figure 7 Premaxillae of adult and subadult individuals of D. motherali. Orthographic image of 3D digital models of DMNH 2013–07–1859 in A, dorsal, B, ventral, C, medial, and D, lateral views; orthographic image of 3D digital models of DMNH 2013–07–0297 in E, dorsal, F, ventral, G, anterior, and H, lateral views; WM 2019–15 Ga in I, dorsal and J, ventral views. Lateral notch for d4 and d5 occlusal indicated by open-headed arrows. See text for anatomical abbreviations.

Scale bar equals 5 cm.

In lateral view, the premaxilla is triangular-shaped, narrowing and thinning posteriorly to become a flattened, posterior process (Figure 7C, D). Just anterior to the premaxilla-maxillary contact is a large, lateral notch for the reception of the enlarged d4 and d5 pseudocanines. When articulated, the premaxillae completely enclose the dorsally oriented external naris. There are small, posteriorly directed processes on the anteromedial margin of the naris as seen in the holotype (DMNH 2013–07–0001). The dorsal margin of the narial rim is elevated sloping posteriorly to the level of the maxilla. In dorsal view, the posterior process of the premaxilla narrows to a point (Figure 7A, B). The premaxillae would articulate at the midline along an edge-to-edge suture to wedge between the maxillae and extends posteriorly to contact the nasal at the level of m5. The premaxillae exclude the maxillae and nasals from contacting the posterior margin of the naris. In palatal view, five premaxillary alveoli are arranged along the anterior margin, with p2 and p3 being larger than p1 and p4. P5 is not preserved in the holotype DMNH 2013–07–0001 but is present in DMNH 2013–07–0297 and WM 2019–15 Ga as an extremely reduced alveolus directly posterior to p4. P1 through p3 extend ventrally to the same level, while p4 and p5 occur higher in a step wise fashion so that p5 is in line with the palate. The palatal surface is deeply concave with pits for the occlusion of the anterior dentary teeth posterior to the ventrally projected anterior premaxillary teeth (Figure 7B, F, J).

4.3 Maxilla

DMNH 2013–07–1859 preserves both left and right maxillae (Figure 9A–D; Video 3). The right is nearly complete while the left is missing portions of the palate and posterior maxillary process. Two additional partial maxillae (DMNH 2013–07–0079 and DMNH 2013–07–0219) have also been recovered (Figure 9E–I). The dorsal surface is ornamented with shallow pits and grooves but is not as rugose as seen in the adult holotype DMNH 2013–07–0001 (Video 4). In dorsal view, the lateral borders of the maxillae are sinusoidal anteriorly and become straighter toward the posterior process. There is a distinct lateral bulge at the level of m4 and m5. Anterior to this bulge, the maxilla tapers toward the premaxilla, resulting in a narrow rostral constriction at the premaxillomaxillary juncture. In lateral view, the narrow rostral constriction is upturned dorsally at approximately 17° (Figure 9J). Above the alveolar margin, neurovascular foramina are evenly spaced linearly along the length of the maxilla. The maxilla has an edge-to-edge contact with the nasal along its straight dorsomedial margin. The posteromedial margin of the maxilla is overlapped dorsolaterally by the anterolateral portion of the lacrimal and the anterior process of the jugal. As seen with the holotype (DMNH 2013–07–0001), the posterior maxillary process passes lateral to the orbits and ventromedially to the jugal and contacts the anterior process of the ectopterygoid just anterior to the postorbital bar.

Figure 8 Orthographic image of 3D digital model reconstruction of the subadult D. motherali (DMNH 2013–07–1859) demonstrating premaxilla-dentary occlusion and the ventral reflection of the premaxilla in A, dorsal, B, ventral, and C, lateral views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

Video 3 Orthographic digital model of the left maxilla from a subadult D. motherali, DMNH 2013–07–1859. Pathological puncture visible on the dorsal surface of the rostrum. Video available at www.cambridge.org/drumheller.

Video 4 Orthographic digital model of the left maxilla from a subadult D. motherali, DMNH 2013–07–1975. Video available at www.cambridge.org/drumheller.

Figure 9 Orthographic image of 3D digital models of maxillae of juvenile and subadult individuals of D. motherali. DMNH 2013–07–1859 left and right maxillae in A, dorsal, B, ventral views; DMNH 2013–07–1859 right maxilla in C, lateral view; DMNH 2013–07–1859 left maxilla in D, obtuse, E, medial views; DMNH 2013–07–0219 in F, dorsal, G, ventral views; DMNH 2013–07–0079 in H, dorsal, I, ventral, J, lateral views. White arrows indicate a partially healed, bite mark. See text for anatomical abbreviations.

Scale bar equals 5 cm.

The secondary palate is well-preserved in DMNH 2013–07–1859 and DMNH 2013–07–0079 with some minor crushing of the palatal shelves medial to the alveolar margin (Figure 9B). Posteriorly, the maxillary palatal process forms the anterior border of the suborbital fenestra and the posterior maxillary process forms most of the anterolateral border. There are 20 maxillary alveoli in the right maxilla, with 11 preserved in the left of DMNH 2013–07–1859. The alveoli increase in size from the first alveolus to m4 and m5, which are the largest. The diameter of alveoli then decreases in size starting with m6 and remain relatively constant in size thereafter. All maxillary alveoli are separated by septa. In between the alveoli are small pits for the occlusion of the dentary teeth.

4.4 Lacrimal

A complete, left lacrimal (DMNH 2013–07–0084) (Figure 10A, B) and a second, incomplete left lacrimal (DMNH 2013–07–1993) were found in isolation, broadly associated with other D. motherali material. The element is anteriorly elongated, narrowing to insert between the maxilla and nasal. It meets the prefrontal posteromedially along an edge-to-edge suture, resulting in the lacrimal extending further anteriorly than the prefrontal. The anteromedial border of the lacrimal broadly contacts the nasal and the anterolateral border overlaps the maxilla. The posterior margin of the lacrimal forms most of the anterior and anterolateral border of the orbit. On the dorsal surface, an elevated rim is present on the anteromedial margin of the orbit. Lateral to this rim, a smooth, triangular depression, the lacrimal notch, separates the orbital ridge from the posterolateral process of the lacrimal. The narrow posterolateral process extends to fit into a notch on the anterodorsal tip of the jugal.

Figure 10 Orthographic image of 3D digital models of cranial elements of subadult individuals of D. motherali. Left lacrimal DMNH 2013–07–0084 in A, dorsal and B, ventral views; left prefrontal DMNH 2013–07–1404 in C, dorsal, D, ventral and E, anterior views; right prefrontal DMNH 2013–07–1975 in F, posterior view. Right prefrontal DMNH 2013–07–1995 in G, dorsal and H, anterior views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

4.5 Prefrontal

A complete left prefrontal (DMNH 2013–07–1404) and two partial right prefrontals (DMNH 2013–07–1975 and DMNH 2013–07–1995) were also found isolated (Figure 10C–E). A second partial left prefrontal is fused with a partial frontal (DMNH 2013–07–1871) (Figure 11E–H). DMNH 2013–07–1404 does articulate with the frontal of DMNH 2013–07–1859 (Figure 11A–D). In dorsal view, the prefrontal extends anteriorly to a wedge-shaped process and does not contact the maxilla. The posteromedial margin of the prefrontal is deflected for an oblique articulation in the inset groove in the anteromedial corner of the frontal. As a result, the frontal is completely excluded from the medial margin of the orbit. A curved, elevated rim extends along the posterolateral margin of the prefrontal and becomes confluent with the elevated rim on the lacrimal, forming the supraorbital rim. The medial descending prefrontal pillar is mediolaterally expanded and flat with a small triangular medial process. In ventral view, the base of the pillar is ellipsoid.

Figure 11 Cranial elements of subadult individuals of D. motherali. Frontal DMNH 2013–07–1859 in A, dorsal, orthographic image of 3D digital model in B, dorsal, C, ventral, and orthographic image of 3D digital models of D, ventral views; frontal and prefrontal DMNH 2013–07–1871 in E, dorsal, orthographic image of 3D digital model in F, dorsal, G, ventral, and orthographic image of 3D digital models of H, ventral views; parietal DMNH 2013–07–1859 in I, dorsal, orthographic image of 3D digital model in J, dorsal, K, ventral, and orthographic image of 3D digital model in L, ventral views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

4.6 Frontal

The frontals of DMNH 2013–07–1859 are fused. It is a relatively flat and cross-shaped element (Figure 11A–D). The dorsal surface of the frontal is densely ornamented with rounded pits. There is a very slight sagittal ridge extending anteroposteriorly along the length of the dorsal surface. It does not appear to extend to the posterior edge of the preserved frontal. Anterior to the orbits, the median process tapers between the prefrontals to form a wedge between the nasals. This anterior process exceeds the anterior tip of the prefrontal but not the lacrimal. Posterior to the orbits, the frontal expands laterally to meet the postorbital and forms the anteromedial margin of the supratemporal fenestra. The posterolateral margin slopes ventrally to form the supratemporal fossae and excludes the parietal from contact with the postorbital. The posterior process of the frontal contacts the parietal midway between the supratemporal fenestrae in a transverse suture. A descending projection medial to the cristae cranii frontales divides the ventral surface of the anterior median process into two longitudinal grooves. At the level of the postorbitals, the two grooves merge into the single path for the olfactory tract.

A second left frontal, DMNH 2013–07–1871, was also recovered (Figure 11E–H). It is larger than DMNH 2013–07–1858 and is in the range of subadult to adult. Unlike DMNH 2013–07–1858, it is disarticulated from the right frontal and its medial articular margin shows no signs of having been fused at the midline. However, the left prefrontal is completely fused with the frontal with no visible sutural line. This provides strong support to Reference Bailleul, Scannella, Horner and EvansBailleul et al.’s (2016) argument that cranial sutural closure is not a valid means for assessing relative maturity in extant and extinct archosaurs.

4.7 Parietal

The parietal is an unpaired and nearly flat, T-shaped element (Figure 11I–L). Its dorsal surface is sculpted with rounded pits. There is no indication of a sagittal ridge as seen in the frontal. It contacts the frontal anteriorly to form the dorsomedial border of the supratemporal openings. The parietal does not contact the postorbital. The posteromedial margin of the supratemporal opening slopes ventrolaterally to contribute to the supratemporal fossa. The parietal meets the quadrate ventrolaterally. Posteriorly, the parietal expands to meet the squamosal laterally at a parasagittally oriented suture. The transverse posterior margin of the parietal overhangs the occiput and excludes the supraoccipital from the dorsal surface of the cranial table. Lateral to the postparietal the ventral margin of the parietal forms the dorsal surface of the post-temporal fenestra and excludes the squamosal participation in the openings. On the ventral surface, just posterior to the supratemporal fenestra, are two mediolaterally oriented impressions for the middle ear cavity.

4.8 Jugal

The left and right jugals for DMNH 2013–07–1859 are nearly complete (Video 5), while DMNH 2013–07–1975 is a partial left jugal (Figure 12A–E). The jugal of DMNH 2013–07–1859 is remarkably similar to that of P. newmani (SMU 76601) (Figure 12F, G). The jugal is an anteroposteriorly elongate, triradiate element. The lateral surface is ornamented with rounded pits and grooves, as in the holotype (Figure 24B; Video 6). There are a series of neurovascular foramina evenly spaced linearly along the length of the lateral margin of the jugal. The anterior and posterior rami are similar in dorsoventral depth. The anterior ramus forms the lateroventral border of the orbit. In cross-sectional view, the anterior ramus is triangular-shaped and wedges between the posterolateral process of the lacrimal dorsomedially and the maxilla ventrally. The anterodorsal tip has a V-shaped notch for articulation with the posterior process of the lacrimal. The ventral sutural surface with the maxilla is nearly flat and rugose. Ventral to the ascending process of the postorbital bar, the ventromedial surface is rugose for articulation with the ectopterygoid. The narrow posterior ramus of the jugal is straight and rod-shaped, forming the lateroventral border of the infratemporal fenestra. A longitudinal ridge runs along the lateral surface of the posterior process below the infratemporal fenestra. The posterior end mediolaterally contacts the quadratojugal along an anteroposterior groove. The ascending process of the jugal, which forms the lower portion of the postorbital bar, is inset more medially than dorsally midway along the medial margin of the jugal. The anterior tip of the process is curled anterolaterally and articulates with the descending postorbital process to form a dorsoventrally oriented boss that extends anterolaterally from the postorbital bar. The posteromedial surface of the ascending process is inset and rugose for articulation with ascending process of the ectopterygoid. There are two anteroposteriorly aligned foramina, one at the base of the ascending process and the other directly posterior to the process, along the dorsal surface.

Video 5 Orthographic digital model of the right jugal from a subadult D. motherali, DMNH 2013–07–1975. Video available at www.cambridge.org/drumheller.

Video 6 Orthographic digital model of the left jugal from an adult D. motherali, DMNH 2013–07–0001. Video available at www.cambridge.org/drumheller.

Figure 12 Orthographic image of 3D digital models of cranial elements of subadult individuals of D. motherali. Right jugal DMNH 2013–07–1859 in A, dorsal, B, lateral, and C, ventral views; left jugal DMNH 2013–07–1975 in D, lateral and E, medial views. P. newmani right jugal SMU 76601 in F, lateral and G, medial views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

4.9 Squamosal

DMNH 2013–07–1859 preserves both left and right squamosals (Figure 13). The dorsal surface of the squamosal is densely sculpted by rounded pits. The anteromedial edge forms the posterolateral margin of the supratemporal fenestra. The lateral margin of the squamosal narrows anteriorly to underlie the dorsal plate of the postorbital. It is uncertain if it contacts the postorbital bar. The posterior dorsal lamina overhangs the lateral margin of the squamosal and forms the dorsal surface of the external otic recess. The dorsolateral sulcus for the earflap is shallow and extends to the anterolateral margin of the squamosal. The squamosal tapers posterolaterally into a prong like process along the dorsal edge of the paroccipital process and extends beyond the level of the posterior margin of the parietal. The posterior margin is directed medially to contact the parietal and overhang the occiput. Ventrolaterally, it descends to contact the posterodorsal surface of the quadrate posterior to the otic recess and lateral to the paroccipital process. A groove extends along the dorsomedial margin of the paroccipital process, while a groove on the medioventral surface of the paroccipital process forms the roof and lateral wall of the cranioquadrate canal.

Figure 13 Squamosals of subadult individual of D. motherali, DMNH 2013–07–1859. Left in A, dorsal; orthographic image of 3D digital model in B, dorsal, C, ventral; orthographic image of 3D digital model in D, ventral views. Right in E, dorsal; orthographic image of 3D digital model in F, dorsal, G, ventral; orthographic image of 3D digital model in H, ventral, I, lateral, and J, posterior views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

4.10 Quadratojugal

DMNH 2013–07–1992 includes nearly complete right and partial left quadratojugals (Figure 14). They are missing anteriormost projection. As a result, it is not possible to determine how far anterior the quadratojugal extends. The spina quadratojugal is prominent and rounded (Figure 4A, B). The dorsal surface is divided into two distinct regions, a smooth, unornamented medial surface and an ornamented lateral region. Medially, the posterolateral margin of the infratemporal opening is smooth and slightly curved anterolaterally. The lobe-shaped posterior region of the quadratojugal is sculpted with large, rounded pits. It runs parallel to the quadrate to reach the posterolateral corner of the lateral hemicondyle of the quadrate to take part in the craniomandibular joint. The ventral surface is smooth and slightly concave with a rugose lateral margin for the overlapping contact with the quadrate.

Figure 14 Quadratojugal of subadult individual of D. motherali, DMNH 2013–07–1992. Right in A, dorsal; orthographic image of 3D digital model in B, dorsal, C, ventral; orthographic image of 3D digital models in D, ventral views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

4.11 Quadrate

DMNH 2013–07–1859 does not preserve either quadrate. However, DMNH 2013–07–1992 includes nearly complete partial left and partial right quadrates that fits well in the glenoid fossae of the articulars of DMNH 2014–06–01(Figure 15A–F; Video 7).

Video 7 Orthographic digital model of the left quadrate from a subadult D. motherali, DMNH 2013–07–1992. Video available at www.cambridge.org/drumheller.

Figure 15 Orthographic images of 3D digital models of quadrates of juvenile and subadult individuals of D. motherali. Left quadrate DMNH 2013–07–1992 in A, dorsal, B, ventral, and C, posterior views; right quadrate DMNH 2013–07–1992 in D, dorsal, E, ventral, and F, posterior views; left quadrate DMNH 2013–07–0733 in G, dorsal, H, ventral and I, posterior views; right quadrate DMNH 2013–07–1997 in J, dorsal, K, ventral, and L, posterior views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

An additional, slightly larger, partial left quadrate (DMNH 2013–07–0733) is also known. The anterior half, including the anterodorsal and pterygoid processes, is missing (Figure 15G–I; Video 8).

Video 8 Orthographic digital model of the left quadrate from an adult D. motherali, DMNH 2013–07–0733. Video available at www.cambridge.org/drumheller.

In all three elements, the quadratojugal articular surface runs lateral to the quadrate to contact the posterolateral corner of the lateral hemicondyle. Medial to that, the dorsal surface is heavily rugose for articulation with the ventral surface of the squamosal and exoccipital. The expanded mandibular condyle is identical to that of the holotype (DMNH 2013–07–0001) (Video 9) with subdivided lateral and medial hemicondyles, separated by a deep intercondylar sulcus. The narrower medial hemicondyle angles medioventrally as compared to the horizontally aligned lateral hemicondyle.

Video 9 Orthographic digital model of the right quadrate from an adult D. motherali, DMNH 2013–07–0001. Video available at www.cambridge.org/drumheller.

The ventral surface of the quadrate body is dominated by prominent concave crests extending anteriorly from posteromedial margin (Figure 16). In the holotype (DMNH 2013–07–0001), these crests are identified as crest A’ and B (sensu Reference Iordansky, Gans and ParsonsIordansky, 1973) (Figure 16A) and are associated with a deeply recessed fossa. However, this recess is not relatively as deep as that of the holotype, DMNH 2013–07–0001. Like DMNH 2014–06–01, DMNH 2013–07–0733 and DMNH 2013–07–1992 are most likely subadult individuals half the size of the holotype, suggesting that this deep fossa becomes accentuated during ontogenetic maturity and increased size.

Figure 16 Orthographic images of 3D digital models of juvenile, subadult, and adult individuals of D. motherali demonstrating ontogenetic variability in the ventral fossa of the quadrate. Adult right quadrate DMNH 2013–07–0001 (reflected) A, subadult left quadrate DMNH 2013–07–0733 B, subadult left quadrate DMNH 2013–07–1992 C, and juvenile right quadrate DMNH 2013–07–1997 (reflected) D, in medial views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

Another partial right quadrate (DMNH 2013–07–1997) is also known (Figure 15J–L). This specimen is roughly half the size of DMNH 2013–07–1992, described above. While this specimen does have a prominent B crest (sensu Reference Adams, Noto and DrumhellerAdams et al., 2017), it lacks the other crests that are present in subadult to adult members of Deltasuchus. This raises the possibility that it is attributable to one of the other crocodyliform taxa known from the AAS, for whom quadrates are currently unknown. However, given the more modest crests observed in the subadult specimens described above, it is likely that the prominence of these characters is strongly affected by ontogeny, with the crests increasing in size to accommodate the larger muscles associated with jaw closure in more mature individuals. Therefore, we tentatively associate this element with a juvenile Deltasuchus.

4.12 Dentary

The symphyseal region of the mandibular rostrum is spatulate, with a transversely broad and straight anterior margin (Figure 17). Anteriorly, the mandibular symphysis is low with a shallow, concave dorsal surface. In dorsal aspect, the symphyseal portion of the rostrum extends caudally to a point level with the eighth dentary alveolus. Alveoli d1–d4 are procumbent and transversely aligned, with the fourth alveolus lateral and posterior to the first. Alveoli d3 and d4 are nearly confluent and the largest alveoli of the dentary, resulting in dual pseudocanines. Small neurovascular foramina occur on the dorsal surface medial to the alveoli. The alveoli are all separated from each other by bony septae.

Figure 17 Orthographic image of 3D digital models of dentaries of subadult individuals of D. motherali, DMNH 2013–07–1859. Left dentary in A, dorsal, B, ventral, C, lateral, and D, medial views; right dentary and splenial in E, dorsal, F, ventral, and G, medial views. Left dentary of DMNH 2013–07–0240 in H, lateral view. See text for anatomical abbreviations.

Scale bar equals 5 cm.

The mandibular ramus is long and straight with a convex lateral surface. The angle at which the ramus diverges from the symphysis varies slightly with ontogeny, with the smallest specimens (DMNH 2013–07–0228; DMNH 2013–07–1984) (Figure 5G; Video 10, respectively) diverging at an angle of about 20° and the right dentary of DMNH 2013–07–1859 (the most complete subadult) diverging at roughly 30° (Figure 2B; Video 11). Without more complete dentaries in larger individuals, this trend is difficult to map into adults. However, the reconstructed margins of the rostrum of the holotype (DMNH 2013–07–0001), which is the largest specimen currently known, diverge at roughly similar angles to the subadult specimens (Video 12). During growth, this would be reflected as a widening of the snout as the animal grew.

Video 10 Orthographic digital model of the right dentary from a juvenile D. motherali, DMNH 2013–07–1984. Video available at www.cambridge.org/drumheller.

Video 11 Orthographic digital model of the right dentary from a subadult D. motherali, DMNH 2013–07–1859. Video available at www.cambridge.org/drumheller.

Video 12 Orthographic digital model of the right dentary from an adult D. motherali, DMNH 2013–07–0001. Video available at www.cambridge.org/drumheller.

Lateral to teeth d7 and d8, the lateral margin of the dentary is slightly concave for reception of the enlarged maxillary pseudocanines m4 and m5. In occlusal view, the anterior alveoli occur close to the lateral edge and shift medially going posteriorly. The medial surface of the ramus is open, exposing the long Meckelian groove that extends forward to the symphysial margin. The ventral and lateral surfaces of the dentary are smooth and ornamented with small, shallow pits and grooves. Neurovascular foramina along the lateral surface form a shallow groove below the alveolar margin. The right and left dentaries of DMNH 2013–07–1859 are nearly complete, missing only the posterior portions of the rami. In the smaller, complete left dentary of DMNH 2013–07–0240 (Figure 5C; Figure 17H), the posteriormost process is forked dorsoventrally, with a broad posteromedial process and short, narrow posterodorsal and posteroventral processes. The process overlaps the angular laterally before projecting medially to be overlapped by the angular and surangular. The posterior process fits together with the angular and surangular in a tongue and groove articulation so that an external mandibular fenestra is absent (Figure 20).

There are 21 dentary tooth positions preserved in the right dentary of DMNH 2013–07–1859 and 17 in the left. The alveoli increase in size from the first alveolus, which is the smallest, to d3 and d4, which are the largest. D3 and d4 are roughly equal in size, producing the dual pseudocanines as seen in the maxilla. The diameter is reduced at d6 and gradually increase in size through d15, decreasing thereafter.

Figure 18 Lower jaw elements of subadult and adult individuals of D. motherali. Orthographic image of 3D digital models of right surangular DMNH 2014–06–01 in A, lateral, B, medial views; orthographic image of 3D digital models of left surangular and angular DMNH 2014–06–01 in C, lateral, D, medial views; right surangular and angular SMU 76810 in E, lateral view. See text for anatomical abbreviations.

Scale bar equals 5 cm.

Figure 19 Orthographic image of 3D digital models of lower jaw elements of subadult individuals of D. motherali. Left angular DMNH 2013–07–1859 in A, lateral and B, medial views; right angular DMNH 2014–06–01 C, lateral, and D, medial views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

Figure 20 Orthographic image of 3D digital models of left surangular and angular of D. motherali, DMNH 2014–06–01 articulated to show the groove (arrows) for the insertion of the posterior process of the dentary in A, oblique view. Orthographic image of 3D digital reconstruction of the lower jaw with the left dentary of DMNH 2013–07–0240 in B, lateral view. Posteriormost process of dentary missing from 3D model indicated with hatched lines. Orthographic image of 3D digital reconstruction P. newmani lower jaw SMU 76601 (reflected) C, lateral view. See text for anatomical abbreviations.

Not to scale.

4.13 Splenial

The right splenial is still attached to the right dentary of DMNH 2013–07–1859 but has shifted dorsally (Figure 17E–F). The splenial is long and triangular, narrowing anteriorly to extend to the level of the seventh dentary alveolus to participate in the mandibular symphysis. Posteriorly, it widens to the same level as the dentary and forms the medial half of the ventral surface of the mandible. There does appear to be a foramen for the intermandibularis oralis of the trigeminal nerve (CN V) on the anteriormost lateral surface of the splenial, but it is slightly obscured by the shifting of the bone.

4.14 Surangular

The right surangular of DMNH 2013–07–1859 is incomplete, representing only the posterodorsal corner of the element (Figure 2B). However, a similar sized individual (DMNH 2014–06–01) preserves a nearly complete posterior mandible (Figure 18A–D). The surangular forms the narrow dorsal margin of the posterior mandible. It has a nearly flat dorsal margin for the insertion of M. adductor mandibulae externus and the convex lateral surface is sculpted by round pits. It contributes to the lateral wall of the glenoid fossa. The ventral margin is thin with an inset groove for articulation with the angular. Anteriorly, this groove extends dorsolaterally for articulation with the posterodorsal process of the dentary. Anteromedially is a shallow groove for the articulation with the splenial. SMU 76810 preserves the posterodorsal corner of a right surangular (Figure 18E). It is heavily sculptured with large, tightly packed, oval- to rectangular-shaped pits. As with DMNH 2014–06–01, the dorsal surface of the nearly complete retroarticular process is caudoventrally angled in lateral view.

4.15 Angular

DMNH 2014–06–01 preserves a complete right and partial left angulars (Figure 3). DMNH 2013–07–1859 also has a nearly complete left angular and partial right (Figures 2 and 19A–D), while SMU 76810 is only the posterioromost end of the element (Figure 18E). The angular forms the posteroventral portion of the posterior mandible. Its lateral surface is almost entirely sculpted by round pits that become smaller anteriorly and form shallow grooves similar to those seen on the dentary. The posterodorsal margin is rugose and slightly deflected for articulation in the inset groove of the surangular. Posteriorly, the angular narrows to extend to the posterior end of the retroarticular process. An inset groove occurs on the anterolateral process of the angular for articulation with the posteroventral process of the dentary (Figure 20A, B). When articulated, the tongue and groove articulation between the angular, surangular, and posteroventral process of the dentary result in no external mandibular fenestra. This is remarkably similar to that of P. newmani (SMU 76601) (Figure 20C). On the anteroventral margin of the angular is a shallow groove for contact with the splenial. A shallow fossa occurs on the posteromedial surface, ventral to the position of the retroarticular process, for the attachment of the M. pterygoideus ventralis. Medially, a trough-like concavity of the angular forms the floor of the mandibular adductor fossa posteriorly and the Meckelian canal anteriorly.

4.16 Articular

DMNH 2013–07–1859 does not preserve either articular. As with the surangular, the similar sized DMNH 2014–06–01 does preserve complete left and right elements (Figure 21). The articular extends anteroposteriorly the length of the corresponding retroarticular process of the surangular. The glenoid fossa is figure-eight-shaped, composed of two asymmetric depressions bisected by a prominent ridge. A prominent dorsal ridge marks the posterior border of the glenoid fossa. The surangular does not participate in the glenoid surface. The descending ramus of the articular is triangular in cross section, tapering ventrally to a thin lamina that passes along the medial surface of the surangular. Anteriorly, this lamina is directed medially following the prominent ridge that divides the glenoid fossa. In lateral view, the sutural surface for the surangular is slightly concave and tapers posteriorly to become triangular-shaped. In dorsal view, the retroarticular process is elongate and paddle-shaped, with a gently concave dorsal surface. The retroarticular process is oriented horizontally relative to the long axis of the mandible. There is no indication of a foramen aëreum at the anteromedial edge of the retroarticular process.

Figure 21 Orthographic image of 3D digital models of articulars of subadult individuals of D. motherali, DMNH 2014–06–01. Left articular in A, dorsal, B, ventral, C, medial, D, lateral, and E, anterior views; right articular in F, dorsal, G, ventral, H, lateral, I, medial, and J, anterior views. See text for anatomical abbreviations.

Scale bar equals 5 cm.

4.17 Dentition

The teeth of D. motherali are like most crocodyliforms in being conical and circular in cross section (Figure 22). The large teeth referable to the holotype (DMNH 2013–07–0001) are upwards of 55 mm in length and 20 mm in width, and exhibit longitudinal ridges that terminate before the apex and with carinae that lack denticles. The enamel ridges and carinae become less prominent with increasing tooth size. All the teeth exhibit a labial curvature that is more pronounced in the larger crowns. Several juvenile and subadult specimens have complete teeth, as well as replacement teeth, preserved in situ, although much of the subadult material tend to be missing their crowns. The teeth of the juveniles preserve closely spaced, nonanastomosing ridges that terminate shortly before the apex. The carinae are oriented mesiodistally and lack denticles.

Figure 22 Isolated teeth of D. motherali. A, B, DMNH 2013–07–0178 in mesial or distal views WM 2019–15 Gb in C, mesial or distal and D, lingual views.

Scale bar equals 2 cm.

4.18 Pathologies

Several elements attributable to Deltasuchus exhibit pathologies. The left maxilla of DMNH 2013–07–1859 has a deep depression on the dorsal surface of the rostrum, situated near the medial margin and roughly parallel with the m10 alveolus (Figure 9A, D, E). In dorsal view, this feature is 7.77 mm in maximum width, 22.87 mm in maximum length, and 6.34 mm in maximum depth. The margins of this structure are smooth in the interior of the depression, but the sculpturing that characterizes the rest of the maxilla is present, if less defined, at the margins of the structure. The edges of the indentation, as well as the transition from unsculptured to sculptured bone, is smooth with no visible fracturing present in this aspect. In medial view, a wedge of bone is present directly beneath the depression, within the nasal passage. It connects with the roof of the nasal passage, suggesting that it represents the dorsal maxillary bone displaced by the overlying, indented feature. No obvious fracturing is visible, and the wedge is narrowest anteriorly, widening posteriorly. The texture is somewhat fibrous and irregular, but the entire element exhibits minor flattening and deformation, which is particularly visible within the nasal passage. The maxilla is broken just anterior to this pathology, and while the element has been glued back together, portions of the bone are missing from both dorsal and medial margins, further affecting the modified region of the element.

Taken together, this structure appears to be partially healed, localized impact or crushing damage consistent with a bite mark. In modern crocodylians, intraspecific competition often is expressed as bites to the rostra, limbs, and bases of tails, making injuries in these regions fairly common (Reference Webb, Manolis and BuckworthWebb et al., 1982). Similar placement of bite marks in other crocodyliform taxa have been used as evidence of intraspecific competition in other fossil groups (Reference BuffetautBuffetaut, 1983; Reference WilliamsonWilliamson, 1996; Reference Avilla, Fernandes and RamosAvilla et al., 2004; Reference KatsuraKatsura, 2004; Reference Mackness, Cooper, Wilkinson and WilkinsonMackness et al., 2010; Reference Vasconcellos and CarvalhoVasconcellos and Carvalho, 2010). However, the degree of partial healing, partnered with the lack of other serial bite marks or more diagnostic features, makes this specific interpretation somewhat speculative. At best, we can say that the injury is consistent with a deep, if partially healed, puncture (sensu Reference BinfordBinford, 1981). Given the faunal composition of the site, neither medium to large crocodyliforms nor theropod dinosaurs can be completely excluded as potential trace makers.

The fragment of dentary within associated DMNH 2014–06–01 elements also exhibits a bite mark. This one, by comparison, still exhibits crushing damage from the initial impact. It does not fully pierce the cortical bone, making it a pit according to Reference BinfordBinford’s (1981) bite mark classification scheme. The pit is teardrop-shaped, being 6.34 mm in maximum width and 8.64 mm in maximum length, and is U-shaped in cross section. The mark morphology lacks an obvious bisection, which would have been diagnostic of Crocodyliformes (Reference Njau and BlumenschineNjau and Blumenschine, 2006; Reference Drumheller and BrochuDrumheller and Brochu, 2014, Reference Drumheller and Brochu2016; Reference Drumheller, D’Amore, Njau, Woodward and FarlowDrumheller et al., in press), but it is consistent with a large, conical tooth, making a crocodyliform the most likely trace maker from the AAS assemblage. Theropod dinosaurs exhibit ziphodont dentition, which would result in a narrower, more V-shaped mark in cross section (Reference D’Amore and BlumenschineD’Amore and Blumenschine, 2009), and none of the mammals or other toothed vertebrates present at the site would have been large enough to have left this trace (Reference Noto, Main and DrumhellerNoto et al., 2012). Again, however, it is not possible to make a more specific association with any one of the several species present at the site, but intraspecific competition is a possible source of the injury.

5 Phylogenetic Analysis

5.1 Methods

Previous analyses have recovered Deltasuchus motherali forming a clade with Paluxysuchus newmani, basal to Goniopholididae and other neosuchians (Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference AdamsAdams, 2019; Reference Kuzmin, Skutschas, Boitsova and SuesKuzmin et al., 2019; Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019). In order to test the evolutionary relationships of D. motherali and P. newmani within Neosuchia, a set of phylogenetic analyses were conducted using revised character codings for D. motherali that include new information derived from those elements of adult and subadult individuals that do not demonstrate any ontogenetic variability. The first phylogenetic analyses incorporated an updated version of the character-taxon matrix of Reference TurnerTurner (2015) which was modified in later studies by Reference Adams, Noto and DrumhellerAdams et al. (2017) and Reference AdamsAdams (2019 ) (see Appendix S1 for character list). The original dataset by Reference TurnerTurner (2015) initially contained 318 active characters and 101 taxa. Following Reference Kuzmin, Skutschas, Boitsova and SuesKuzmin et al. (2019), the analysis presented here is revised and expanded to include a crocodyliform taxon (TMM 42536–2) from the Upper Cretaceous (early Campanian) Aguja Formation of Brewster County, Texas for a total of 321 osteological characters and 107 crocodylomorpha taxa. TMM 42536–2 was scored for 130 of the 321 characters based on Reference Lehman, Wick, Brink and ShillerLehman et al. (2019).

The second matrix for phylogenetic analysis employed the merged character-taxon matrix originally published by Reference Young, Hastings, Allain and SmithYoung et al. (2016), which was then subsequently revised and expanded by Reference Ristevski, Young, Andrade and HastingsRistevski et al. (2018), who referred to it as the Hastings + Young matrix (H+Y matrix) (Appendix S2). The dataset by Reference Ristevski, Young, Andrade and HastingsRistevski et al. (2018) initially contained 387 morphological characters and 137 taxa but was recently expanded by Reference Lehman, Wick, Brink and ShillerLehman et al. (2019) to include TMM 42536–2, the crocodyliform from the Upper Cretaceous (early Campanian) Aguja Formation of Brewster County, Texas. D. motherali and P. newmani were added to the H+Y matrix for a total of 387 characters and 140 taxa.

The analyses were conducted using TNT v. 1.5 (Reference Goloboff, Farris and NixonGoloboff et al., 2008; Reference Goloboff and CatalanoGoloboff and Catalano, 2016). A heuristic tree search strategy was conducted performing 1,000 replicates of Wagner trees (using random addition sequences) followed by TBR branch swapping (holding 10 trees per replicate). The Turner matrix treated 34 characters as ordered, while 19 characters were treated as ordered for the H+Y matrix. All other characters were equally weighted. The best trees obtained at the end of the replicates were subjected to a final round of TBR branch swapping. Zero-length branches were collapsed if they lack support under any of the most parsimonious reconstructions. Character support of the nodes present in the most parsimonious reconstructions was calculated using bootstrap analysis of 1,000 replicates and the BREMER.RUN script for Bremer support (Reference BremerBremer 1988, Reference Bremer1994). The topologies obtained during the bootstrap replicates are summarized using frequency differences (Groups present/Contradicted, GC), following Reference Goloboff, Farris and KällersjöGoloboff et al. (2003). Phylogenetic nomenclatural and clade definitions follow that of Reference Brochu, Wagner, Jouve, Sumrall and DensmoreBrochu et al. (2009) and Reference TurnerTurner (2015).

5.2 Results

The first analysis using the revised matrix of Reference TurnerTurner (2015) resulted in 4 most parsimonious trees (MPTs), with a length of 1,728 steps, a consistency index (CI) of 0.233, and a retention index (RI) of 0.666 (Figure 23). Within Neosuchia, the strict consensus topology resulted in several differences from those found in Reference Adams, Noto and DrumhellerAdams et al. (2017), Reference AdamsAdams (2019), and Reference Noto, Adams, Drumheller and TurnerNoto et al. (2019). As with previous results, D. motherali was recovered inside Neosuchia in all four MPTs as the sister taxon to P. newmani. This clade is supported by two unambiguous synapomorphies: absence of a mandibular fenestra (character 74.1); postorbital in contact with the ectopterygoid (character 143.0). Unlike previous analyses, Goniopholididae is positioned more basal to the clade containing Paluxysuchus + Deltasuchus (hereafter referred to as Paluxysuchidae). TMM 42536–2 was recovered basal to Paluxysuchidae in all four MPTs. A TMM 42536–2 + Paluxysuchidae + Thalattosuchia + Tethysuchia clade is defined by three synapomorphies: postorbital-jugal contact anterior to jugal (character 16.0); jugal does not exceed the anterior margin of orbit (character 121.0); base of postorbital process of jugal directed dorsally (character 141.1). Differences were also recovered within Eusuchia with the overall typology being more resolved, with fewer polytomies occurring in Crocodylia and Paralligatoridae. A monophyletic clade containing Wannchampsus sp. (formerly known as the Glen Rose Form sensu Reference AdamsAdams, 2014) and Wannchampsus kirpachi was recovered as a sister group to Atoposauridae, and not as a paralligatorid, supporting previous hypothesis of closer affinities between atoposaurids and paralligatorids (Reference TurnerTurner, 2015; Reference Schwartz, Raddatz and WingsSchwartz et al., 2017; Reference Kuzmin, Skutschas, Boitsova and SuesKuzmin et al., 2019). The addition of Kansajsuchus extensus, Turanosuchus aralensis, and the Dzharakuduk paralligatorid resulted in Paralligatoridae showing a similar topology to that of Reference Kuzmin, Skutschas, Boitsova and SuesKuzmin et al. (2019), with Tarsomordeo winkleri and Rugosuchus nonganensis being pulled down to more basal positions. This clade is defined by six synapomorphies: midline ridge on the dorsal surface of frontal and parietal (character 21.1); unsculptured “lobe” on the posterodorsal corner of the squamosal (character 34.1); basisphenoid exposed on the ventral surface of braincase (character 55.0); external nares divided by a septum (character 65.0); sharp ridge along the lateral surface of the angular (character 218.2); width of posterior half of the axial neural spines are narrow (character 257.1).

Figure 23 Strict consensus topology from the first phylogenetic analysis based on the Turner matrix of 107 taxa and 321 characters. Four equally MPTs of 1,728 steps (CI = 0.233 and RI = 0.666) were obtained from a cladistic analysis. Paluxysuchidae are indicated in red. Numbers at each node indicate bootstrap GC values (top number) and Bremer support values (bottom number). Semilunar hash marks indicate stem-based definition and solid circles indicate a node-based taxon.

The results of the second analysis utilizing the H+Y matrix recovered 130 MPTs with 1,285 steps (CI = 0.406, RI = 0.843 Figure 24). Except for the inclusion of D. motherali and P. newmani, the overall typology of the strict consensus tree does not vary from that of Reference Ristevski, Young, Andrade and HastingsRistevski et al. (2018). D. motherali and P. newmani form a monophyletic clade (Paluxysuchidae) basal to Goniopholididae. D. motherali + P. newmani is defined by one synapomorphy: absence of a mandibular fenestra (character 216.1). The most significant difference between Reference Ristevski, Young, Andrade and HastingsRistevski et al. (2018) and this current analysis is the placement of TMM 42536–2 in a basal position within Paluxysuchidae in all 130 MPTs. Paluxysuchus + Deltasuchus + TMM 42536–2 is defined by five synapomorphies: lacrimal reaches the anterodorsal and anteroventral margins of the orbit (characters 120.1 and 122.1); width of anterior process and posterior process of the jugal are subequal in size (character 131.0); surangular extends to posterior end of retroarticular process (character 229.1); surface of the retroarticular process is paddle shaped (character 236.2).

Figure 24 Strict consensus topology from the second phylogenetic analysis based on the H+Y matrix using 140 taxa and 387 characters, resulting in 130 equally MPTs of 1,285 steps (CI = 0.406 and RI = 0.843). Paluxysuchidae are indicated in red. Numbers at each node indicate bootstrap GC values (top number) and Bremer support values (bottom number). Semilunar hash marks indicate stem-based definition and solid circles indicate a node-based taxon.

6 Discussion

6.1 Relationship of Paluxysuchidae and TMM 42536–2

Overall, the results of the phylogenetic analyses confirm the inclusion of both Paluxysuchus newmani and Deltasuchus motherali into a common clade, Paluxysuchidae, clade nov. Of particular interest is the placement of TMM 42536–2 within Paluxysuchidae in the H+Y matrix, a result of clear similarities; triangular form of the lacrimal and its involvement in the orbital margin, jugal not exceeding the anterior margin of the orbit, the anterior and posterior ramus of the jugal being subequal, ventrally expanded medial condyle of the quadrate, and a paddle-shaped retroarticular process projecting dorsally. Reference Lehman, Wick, Brink and ShillerLehman et al. (2019) had recovered TMM 42536–2 in a basal position within Goniopholididae, referring to it as the “Aguja goniopholidid.” In their only comparisons, they distinguished it from the only other purported goniopholidid crocodyliform known from Upper Cretaceous of North America, Denazinosuchus kirtlandicus from New Mexico, based on the presence of a vestigial maxillary fossa, a small mandibular fenestra, and large suborbital fenestra. The shallow maxillary fossa, a character typically used to recognize goniopholidids (character 48.1 in the H+Y matrix), is described as “vestigial (or rudimentary)” (Reference Lehman, Wick, Brink and ShillerLehman et al., 2019: p. 302) and could possibly be analogous to the shallow groove found on the posterior maxillary process of D. motherali, which can be attributed to surface sculpturing or potentially the confluence of several maxillary neurovascular foramina on the lateral margin of the maxilla (Reference Adams, Noto and DrumhellerAdams et al., 2017). It would require five extra steps to retrieve TMM 42536–2 within Goniopholididae in the H+Y matrix as found in Reference Lehman, Wick, Brink and ShillerLehman et al. (2019) and three extra steps in the Turner matrix.

The position of TMM 42536–2 in the Turner matrix places it outside Paluxysuchidae, positioned as a separate, but closely related taxon. It requires only one extra step to retrieve it within that clade. The differences in the two analyses may be a result of the fragmentary nature of TMM 42536–2, with the specimen lacking diagnostic elements (Reference Lehman, Wick, Brink and ShillerLehman et al., 2019). More complete and better-preserved specimens may help resolve the two alternative phylogenies presented here. Additionally, the close connection between TMM 42536–2, D. motherali, and P. newmani strengthens the argument for the early emergence of an endemic crocodyliform assemblage at the beginning of the Early Cretaceous and implies that the transition from the Early to Late Cretaceous may have been more gradual for crocodyliforms (Reference Adams, Noto and DrumhellerAdams et al., 2015, Reference Adams, Noto and Drumheller2017).

6.2 Relationships of Paluxysuchidae and Closely Related Groups

The clade TMM + Paluxysuchidae was recovered as either basal to Goniopholididae + Tethysuchia in the H+Y matrix or to Tethysuchia + Thalattosuchia in the Turner. In the H+Y matrix, it would require only one extra step to position Paluxysuchidae basal to Tethysuchia, while taking four extra steps in the Turner matrix to place it basal to Goniopholididae. The close relationship between Goniopholididae + TMM + Paluxysuchidae + Tethysuchia + Thalattosuchia from the Turner analysis is characterized by eight synapomorphies: nasals do not contribute to the narial border (12.1); anterior edge of choanae situated between the suborbital fenestrae (43.0); dorsal osteoderms have a well-developed process located anterolaterally on dorsal parasagittal osteoderms (95.2); osteoderms without longitudinal keels (100.1); postzygapophyses of axis are poorly developed (152.1); supraoccipital not exposed on the skull roof (170.0); projection of anterior alveoli of the dentary are weakly procumbent (261.1); no midline crest on the basioccipital plate below the occipital condyle (294.0). A Paluxysuchidae + Tethysuchia + Thalattosuchia clade is supported by only one transformation: splenial extensively involved in symphysis in ventral view (76.2). However, there are additional characters shared between these groups that help to diagnose Paluxysuchidae: the posterior ramus of the jugal beneath the infratemporal fenestra is rod-shaped (17.1; shared with pholidosaurids); retroarticular process facing dorsally and paddle shaped (70.3; shared with pholidosaurids); jugal does not exceed the anterior margin of the orbit (121.1; shared with tethysuchians). The results of this analysis support that these characters are not dependent of a tubular-snouted longirostrine condition, as proposed by Reference Pol and GaspariniPol and Gasparini (2009), but are more likely a homoplastic condition (Reference AdamsAdams, 2013).

The H+Y analysis resulted in four synapomorphies for a TMM + Paluxysuchidae + Goniopholididae + Tethysuchia clade: the presence of large depressions on the ventral surface of the premaxilla posterior to either the P1–P2 for reception of the d1 teeth (24.1); the anterior and anterolateral margins of premaxilla are subvertical, and extend ventrally to the rest of the element (26.1); dorsal surface of lacrimal extend laterally over the orbit (56.1); median process of the frontal extends anterior to the tip of the prefrontal (94.0). Presacral dorsal armor considerably wider than long (372.1). A Goniopholididae + Tethysuchia clade is associated with two synapomorphies: the presence of an enlarged foramina and associated fossae on the lateral margin of the posterior maxillae and/or the anterior process of the jugal (47.1); quadrate and squamosal do not laterally enclose the cranioquadrate canal, and it is laterally exposed (204.2). In either analysis, the close affinity of these clades is not surprising as they share a number of morphological features (see Section 5.2, Results) and strengthens the existence of a neosuchian lineage, comprised of mesorostrine platyrostral forms and tubular-snouted longirostrine taxa, that diverges from the lineage that led to Eusuchia (Reference Andrade, Edmonds, Benton and SchoutenAndrade et al., 2011).

6.3 Niche Partitioning and Ontogeny

In crocodyliforms, snout shape (e.g. Reference BrochuBrochu, 2001; Reference Drumheller and WilbergDrumheller and Wilberg, 2020) and tooth shape (e.g. Reference D’Amore, Harmon, Drumheller and TestinD’Amore et al., 2019) have been associated with diet and feeding strategy. Slender snouts and thin, conical teeth are associated with predation on smaller- and softer-bodied prey (i.e. Reference Iordansky, Gans and ParsonsIordansky, 1973; Reference Langston, Gans and ParsonsLangston, 1973; Reference Busby and ThomasonBusby, 1995; Reference McHenry, Clausen, Daniel, Meers and PendharkarMcHenry et al., 2006; Reference Gignac and O’BrienGignac and O’Brien, 2016; Reference Drumheller and WilbergDrumheller and Wilberg, 2020) while blunt snouts and anvil-like teeth are specializations associated with durophagy (e.g. Reference BrochuBrochu, 2001; Reference D’Amore, Harmon, Drumheller and TestinD’Amore et al., 2019; Reference Drumheller and WilbergDrumheller and Wilberg, 2020). Broad U- or V-shaped snouts, especially when partnered with sturdy, conical teeth, are found in taxa that exhibit a more generalist diet, including full-blown macropredation (e.g. Reference BrochuBrochu, 2001; Reference Drumheller and WilbergDrumheller and Wilberg, 2020). Morphometric analyses of snout shape have largely supported these divisions within the crown group (Reference Pierce, Angielczyk and RayfieldPierce et al., 2008; Reference Sadleir and MakovickySadleir and Makovicky, 2008), but inclusion of more distantly related fossil taxa further subdivides Crocodyliformes into two functionally separate slender-snouted and generalist ecomorphotypes (Reference WilbergWilberg, 2017; Reference Drumheller and WilbergDrumheller and Wilberg, 2020).

Adult Deltasuchus specimens exhibit the broadly triangular snout shape that is associated with a generalist diet, but not macropredation, i.e. active predation on taxa that are larger than the predator (Reference Drumheller and WilbergDrumheller and Wilberg, 2020) (Figure 25A, B; Video 13A, 13B, 14A, 14B). Partnered with stout, conical teeth (Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference D’Amore, Harmon, Drumheller and TestinD’Amore et al., 2019), these animals were well-adapted to feeding on the wide diversity of prey items present in the AAS, an interpretation that is further bolstered by the presence of bite marks attributable to this taxon on dinosaurian and turtle material at the site (Reference Noto, Main and DrumhellerNoto et al., 2012; Reference Adrian, Smith, Noto and GrossmanAdrian et al., 2019). However, the diet and feeding strategy can shift through age and ontogeny, and interpretations applicable to adults may not reflect the paleoecology of juveniles.

Video 13 Composite, orthographic digital model of an adult D. motherali cranium and mandible. Video available at www.cambridge.org/drumheller.

Crocodyliforms increase in size by several orders of magnitude during growth and development, which has a direct effect on the prey items available across the range of body sizes seen within a single species (Reference Gignac and O’BrienGignac and O’Brien, 2016; Reference Gignac, Santana and O’BrienGignac et al., 2019). In modern groups, very young individuals are commonly observed to eat a diversity of small-bodied prey, including arthropods, fish, and amphibians (e.g. Reference McIlhennyMcIlhenny, 1935; Reference Ross, Magnusson and RossRoss and Magnusson, 1989), and it is only into adulthood that the blunter-snouted taxa shift away from compliant prey items and take on the generalist diets more commonly associated with their respective rostral and dental morphologies (Reference Drumheller and WilbergDrumheller and Wilberg, 2020).

Video 14 Composite, orthographic digital model of a subadult D. motherali cranium and mandible. Video available at www.cambridge.org/drumheller.

In Deltasuchus, the juvenile material described in this study does exhibit changes in rostral and dental morphology consistent with shifting niche occupation during ontogeny. The angle of the snout widens noticeably between juveniles and subadults. Measurements of the smallest specimen (DMNH 2013–07–0228) suggest that when articulated, the dentaries would have diverged from one another at an angle of about 20°, while the most complete subadult (DMNH 2013–07–1859) had a comparatively wider snout, with dentaries diverging from one another at 30° (Figure 25C, D). The largest adult specimen is the holotype (DMNH 2013–07–0001), but the dentaries associated with this individual are very fragmentary making direct measurement difficult. Extrapolating an angle of the snout from the rostral reconstruction yields a similar angle to the subadult, roughly at 30° (Figure 25).

Figure 25 Orthographic image of 3D digital reconstruction of a D. motherali adult skull in A, dorsal, B, lateral views and a subadult skull in C, dorsal, D, lateral views.

Scale bar equals 10 cm.

Dentition also shifts through ontogeny. Size heterodonty remains fairly consistent, with the paired pseudocanines of both the dentaries and maxillae of all size classes having roughly twice the alveolar diameters of their immediate neighbors across all specimens and size classifications (Table 1). Not all jaw elements contain complete teeth, but in those that do, there is a trend in overall shape with increased size. The teeth from the smallest juveniles (e.g. DMNH 2013–07–0228, DMNH 2013–07–0240, DMNH 2013–07–0312, DMNH 2013–07–0322) are noticeably more slender than those in the subadults (e.g. DMNH 2013–07–1859) and adults (e.g. DMNH 2013–07–0001).

Table 1 Measurements of labiolingual tooth diameters in mms. Teeth are listed by anatomical position (p = premaxilla; m = maxilla; d = dentary) and numbered mesially to distally. Blank = no alveolus preserved for this position on this specimen; – = alveolus is preserved, but is too damaged or incomplete to reliably measure; ? = uncertainty with regards to the dental count; * = tooth/replacement tooth present

ToothSpecimen#
DMNH 2013–07–0001 leftDMNH 2013–07–0001 rightDMNH 2013–07–0297DMNH 2013–07–1859 leftDMNH 2013–07–1859 rightDMNH 2013–07–0079DMNH 2013–07–0239DMNH 2013–07–1888DMNH 2013–07–0219
p19.76.876.15
p220.997.78*
p322.2811.51
p412.427.81
m111.545.576.054.04
m212.4415.456.256.724.57
m317.4515.896.5–*8.04*4.67
m424.5324.8611.6612*8.26
m524.0324.9410.62*11.58*12.82*8.94
m612.97.18.457.844.67
m714.096.817.437.934.29
m815.1815.146.487.066.743.79
m915.2317.446.256.615.18
m1018.196.617.536.75
m1119.2619.226.617.67
m1218.3218.15
m1317.6218.738.26
m1416.9917.55
m1515.6315.9
m1614.0315.3
m1713.82
m1811.63
m1911.06
m208.67
m217.01
m226.91
d111.78*11.58*3.645.51*
d210.21*11.44*5.857.3
d322.13*–*8.6311.4312.54
d423.48*23.45*7.2511.6513.1310.5
d512.6613.32*4.47*6.64*7.797.68
d613.5413.315.44*6.497.197.1
d711.3511.385.04*5.44*6.346.21
d810.245.94*5.79
d95.60*6.36*5.59
d107.46.31*6.417.87?
d11–*7.146.99?*
d128.13*6.72*7.496.64?
d137.17*6.548.346.09?
d146.836.56*7.655.80?
d156.22*–*7.456.89?
d164.11–*6.725.73?
d174.78–*6.36–?
d18–*
d19–*
d20–*
d21–*
d22
d23
d24
ToothSpecimen#
DMNH 2013–07–1984DMNH 2013–07–0218DMNH 2013–07–0322DMNH 2013–07–0802DMNH 2013–07–0240DMNH 2013–07–0228DMNH 2013–07–0312
d13.73*4.09*3.392.712.08
d23.793.812.16
d38.14*7.595.27*4.1
d48.04*8.526.625.00*3.97
d53.814.1*3.913.641.97
d63.82*3.533.412.05
d73.242.373.442.781.96
d82.872.72.932.331.781.96
d93.493.373.521.622.26
d103.714.743.342.191.91*
d11–*5.892.822.42–?
d126.224.74*2.72.86*3.33?
d135.795.10*2.243.81?*
d144.884.63*2.32*4.04?*
d155.634.263.75*33.59?*
d165.393.923.79*2.21*3.89?*
d173.782.83*2.063.73?*
d183.782.20*2.88?*
d193.332.84?*
d202.75*2.57?*
d212.36?*
d22–?
d23–?
d24–?

These two changes during ontogeny suggest a shift in the niche occupied by different size and age Deltasuchus. In the larger context of the site, these changes make sense given the other crocodyliform taxa present in the site. In addition to common Deltasuchus material, the AAS has also yielded crocodyliform fossils from at least three other species representing two distinct ecomorphotypes. Scolomastax was a small-bodied crocodyliform with a short snout and significant size (and probable shape) heterodonty, suggesting that it specialized in hard food items. It is possible that this species was an omnivore or maybe even a herbivore (Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019). Terminonaris and Woodbinesuchus, in comparison, were both large-bodied, slender-snouted and -toothed species (Reference LeeLee, 1997a; Reference Adams, Polcyn, Mateus, Winkler and JacobsAdams et al., 2011) that would have specialized on smaller-bodied, more compliant prey (Reference Drumheller and WilbergDrumheller and Wilberg, 2020). Between these two species, further niche partitioning is suggested based on relative snout length and environmental preference. Terminonaris had a comparatively longer snout, and is found in coastal, nearshore environments. In comparison, Woodbinesuchus exhibited a slightly less longirostrine condition, and seems to be more restricted to freshwater to brackish environments (Reference Jouve and JalilJouve and Jalil, 2020; Reference Jouve, de Muizon, Cespedes-Paz, Sossa-Soruco and KnollJouve et al., in press). The geology of the AAS is complex, including freshwater, brackish, saltwater, and terrestrial input (Reference Adams, Noto and DrumhellerAdams et al., 2017; Reference Noto, Adams, Drumheller and TurnerNoto et al., 2019), and therefore would have preserved organisms in direct association that may not have overlapped significantly in life.

The ontogenetic trajectory of Deltasuchus would have differentiated members of this group from other crocodyliforms in its immediate vicinity throughout life. The more gracile morphology of the juveniles would not lend itself well to consuming hard prey items, but occupying this niche potentially would have brought them into direct competition with Scolomastax. However, even the youngest specimens are not as longirostrine as sympatric Terminonaris and Woodbinesuchus, suggesting that these groups were also responding to pressures to partition niches. With age, increased size and snout robusticity would have moved this taxon into an ecomorphotype that allowed predation on larger and hard-bodied prey items (Reference Drumheller and WilbergDrumheller and Wilberg, 2020), an ecological interpretation that is further bolstered by the presence of bite marks attributable to midsized Deltasuchus on turtles and dinosaurs known from the AAS (Reference Noto, Main and DrumhellerNoto et al., 2012; Reference Adrian, Smith, Noto and GrossmanAdrian et al., 2019). This shifted subadults and adults into a niche that was not occupied by the other large-bodied taxa in this ecosystem, which were all specializing in smaller, more compliant prey (Reference Drumheller and WilbergDrumheller and Wilberg, 2020).

Similar examples of niche partitioning, as reflected by disparate snout and tooth morphologies, are known in other fossil localities with multiple species of sympatric crocodyliforms (e.g. Reference Salas-Gismondi, Flynn and BabySalas-Gismondi et al., 2015), but much of this previous focus has fallen on the morphology of the adult members of these clades. This is most likely being driven by availability of specimens, but in modern settings, dietary pressures seem to be exceptionally high on the youngest crocodylians, suggesting that selection for or against juvenile morphotypes is particularly important with regards to survival into adulthood and sexual maturity (e.g. Reference Gignac and O’BrienGignac and O’Brien, 2016; Reference Gignac and SantanaGignac and Santana, 2016). The ontogenetic trajectory of increasing snout width and robusticity with growth and development, as observed in Deltasuchus, is expected, because it mirrors similar patterns observed qualitatively and quantitatively across all modern crocodylians (Reference Drumheller, Wilberg and SadleirDrumheller et al., 2016; Reference IijimaIijima, 2017). The dietary implications of slender, more gracile juvenile snouts supporting slender dentition transitioning into wider, more robust, sturdier-toothed adult morphologies has been particularly well-explored across nonalligatoroid crocodylians, drawing from both isotopic (Reference Radloff, Hobson and LeslieRadloff et al., 2012) and geometric morphometric evidence (Reference IijimaIijima, 2017). The availability of multiple specimens attributable to Deltasuchus in the AAS system provides a rare opportunity to discuss how juveniles fit into the greater pattern of niche occupation and partitioning among crocodyliforms in this site.

7 Conclusions

The fossil record of terrestrial and freshwater vertebrates, including crocodyliforms, is often highly fragmentary and taphonomically biased. Our knowledge of many taxa is based on single, incomplete specimens. When they are available, ontogenetic series across species provide invaluable information on intraspecific variation, critical to understanding character development in phylogenetic contexts and paleoecological niche shifts during growth and development. An expanded, ontogenetic series attributable to Deltasuchus yields paleoecological information regarding dietary shifts across age and size classifications, illuminating how juveniles fit into the trophic hierarchies and specializations of a crocodyliform-rich ecosystem. This material also provides further support of an endemic group of mid-Cretaceous neosuchians, currently best known from the subcontinent of Appalachia. Herein named Paluxysuchidae, clade nov., this clade encompasses Paluxysuchus (Reference AdamsAdams, 2013), Deltasuchus (Reference Adams, Noto and DrumhellerAdams et al., 2017), and potentially TMM 42536–2 from the Upper Cretaceous (early Campanian) of Texas, and represents a mid-Cretaceous radiation of crocodyliforms that coincided with the opening of the Western Interior Seaway.

Acknowledgments

We thank the Huffines family and R. Kimball of Johnson Development, who provided access to the property on which the AAS is situated. A. Sahlstein, P. Kirchoff, and B. Walker first discovered the site, and a dedicated team of volunteers helped excavate and prepare much of the material over the past 10 years. Thanks to the Perot Museum of Nature and Science, Southern Methodist University, and the Witte Museum for access to research collections. We thank S. Jouve and an anonymous reviewer for their valuable comments that helped improve this manuscript. C. Sumrall prepared additional specimens and provided access to photographic equipment during the COVID-19 quarantine. Taxon silhouettes come from Phylopic (phylopic.org), and were created by S. Werning (Wonder Women) and Smokeybjb (crocodyliform). These images are used under a Creative Commons Attribution-Non-Commercial-Share Alike 3.0 license. This study was supported by funding from the National Geographic Society Conservation Trust grant #C325-16 to C. Noto, National Science Foundation DUE-IUSE GP-IMPACT grant #1600376 to L. McKay and S. Horn, as well as our contributors on Experiment.com.

Editor-in-Chief

  • Colin D. Sumrall

  • University of Tennessee

About the Series

  • The Elements of Paleontology series is a publishing collaboration between the Paleontological Society and Cambridge University Press. The series covers the full spectrum of topics in paleontology and paleobiology, and related topics in the Earth and life sciences of interest to students and researchers of paleontology.

    The Paleontological Society is an international nonprofit organization devoted exclusively to the science of paleontology: invertebrate and vertebrate paleontology, micropaleontology, and paleobotany. The Society’s mission is to advance the study of the fossil record through scientific research, education, and advocacy. Its vision is to be a leading global advocate for understanding life’s history and evolution. The Society has several membership categories, including regular, amateur/avocational, student, and retired. Members, representing some 40 countries, include professional paleontologists, academicians, science editors, Earth science teachers, museum specialists, undergraduate and graduate students, postdoctoral scholars, and amateur/avocational paleontologists.

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Figure 0

Figure 1  Location and geologic setting of the AAS and Bear Creek. A, stratigraphic column for the Upper Cretaceous of north-central Texas showing the position of the Woodbine Group relative to timescale and adjacent geologic units. Stippled intervals represent terrestrial deposits. Star indicates position of the AAS and Bear Creek sites. Time scale based on Gradstein et al. (2004). B, generalized map of geologic units in the Fort Worth Basin, showing enlarged area from white box of inset map of Texas.

Modified from Barnes et al. (1972) and Strganac (2015).
Figure 1

Figure 2 Subadult D. motherali (DMNH 2013–07–1859). Cranial elements in A, dorsal view and mandible in B, dorsal and lateral views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 2

Figure 3 Mandible elements of D. motherali (DMNH 2014–06–01). Right dentary in A, lateral view; right surangular in B, lateral view; right angular in C, lateral view; left surangular and angular in D, lateral view, dashed line indicating sutural boundary between the angular and surangular; left and right articulars in E, dorsal views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 3

Figure 4 Adult and subadult individuals of D. motherali. DMNH 2013–07–0079 right maxillae in A, dorsal and B, ventral views; right dentary in C, dorsal and D, ventral views; DMNH 2013–07–0297, premaxillae in E, dorsal view; WM 2019–15 Ga, left premaxilla in F, dorsal view. SMU 76810, right surangular and angular in G, lateral view. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 4

Figure 5 Orthographic image of 3D digital models demonstrating size comparison of dentaries for juvenile and subadult individuals of D. motherali. DMNH 2013–07–0239, left dentary in A, dorsal view; DMNH 2013–07–0322, left dentary in B, dorsal view; DMNH 2013–07–0240, left dentary in C, dorsal view; DMNH 2013–07–0228, left dentary in D, dorsal view; DMNH 2013–07–1984, right dentary in E, dorsal view; DMNH 2013–07–0802, right dentary in F, dorsal view; DMNH 2013–07–0218, right dentary in G, dorsal view; DMNH 2013–07–0312, right dentary in H, lateral view.

Scale bar equals 5 cm.
Figure 5

Figure 6 Size comparison of juvenile (less than 2.5 m), subadult (2.5 to 4.0 m), and adult (greater than 4.0 m) individuals of D. motherali.

Scale bar equals 1 m.
Figure 6

Video 1 Orthographic digital model of the left premaxilla from a subadult D. motherali, DMNH 2013–07–1859. Video available at www.cambridge.org/drumheller.

Figure 7

Video 2 Orthographic digital model of the articulated premaxillae from an adult D. motherali, DMNH 2013–07–0297. Video available at www.cambridge.org/drumheller.

Figure 8

Figure 7 Premaxillae of adult and subadult individuals of D. motherali. Orthographic image of 3D digital models of DMNH 2013–07–1859 in A, dorsal, B, ventral, C, medial, and D, lateral views; orthographic image of 3D digital models of DMNH 2013–07–0297 in E, dorsal, F, ventral, G, anterior, and H, lateral views; WM 2019–15 Ga in I, dorsal and J, ventral views. Lateral notch for d4 and d5 occlusal indicated by open-headed arrows. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 9

Figure 8 Orthographic image of 3D digital model reconstruction of the subadult D. motherali (DMNH 2013–07–1859) demonstrating premaxilla-dentary occlusion and the ventral reflection of the premaxilla in A, dorsal, B, ventral, and C, lateral views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 10

Video 3 Orthographic digital model of the left maxilla from a subadult D. motherali, DMNH 2013–07–1859. Pathological puncture visible on the dorsal surface of the rostrum. Video available at www.cambridge.org/drumheller.

Figure 11

Video 4 Orthographic digital model of the left maxilla from a subadult D. motherali, DMNH 2013–07–1975. Video available at www.cambridge.org/drumheller.

Figure 12

Figure 9 Orthographic image of 3D digital models of maxillae of juvenile and subadult individuals of D. motherali. DMNH 2013–07–1859 left and right maxillae in A, dorsal, B, ventral views; DMNH 2013–07–1859 right maxilla in C, lateral view; DMNH 2013–07–1859 left maxilla in D, obtuse, E, medial views; DMNH 2013–07–0219 in F, dorsal, G, ventral views; DMNH 2013–07–0079 in H, dorsal, I, ventral, J, lateral views. White arrows indicate a partially healed, bite mark. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 13

Figure 10 Orthographic image of 3D digital models of cranial elements of subadult individuals of D. motherali. Left lacrimal DMNH 2013–07–0084 in A, dorsal and B, ventral views; left prefrontal DMNH 2013–07–1404 in C, dorsal, D, ventral and E, anterior views; right prefrontal DMNH 2013–07–1975 in F, posterior view. Right prefrontal DMNH 2013–07–1995 in G, dorsal and H, anterior views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 14

Figure 11 Cranial elements of subadult individuals of D. motherali. Frontal DMNH 2013–07–1859 in A, dorsal, orthographic image of 3D digital model in B, dorsal, C, ventral, and orthographic image of 3D digital models of D, ventral views; frontal and prefrontal DMNH 2013–07–1871 in E, dorsal, orthographic image of 3D digital model in F, dorsal, G, ventral, and orthographic image of 3D digital models of H, ventral views; parietal DMNH 2013–07–1859 in I, dorsal, orthographic image of 3D digital model in J, dorsal, K, ventral, and orthographic image of 3D digital model in L, ventral views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 15

Video 5 Orthographic digital model of the right jugal from a subadult D. motherali, DMNH 2013–07–1975. Video available at www.cambridge.org/drumheller.

Figure 16

Video 6 Orthographic digital model of the left jugal from an adult D. motherali, DMNH 2013–07–0001. Video available at www.cambridge.org/drumheller.

Figure 17

Figure 12 Orthographic image of 3D digital models of cranial elements of subadult individuals of D. motherali. Right jugal DMNH 2013–07–1859 in A, dorsal, B, lateral, and C, ventral views; left jugal DMNH 2013–07–1975 in D, lateral and E, medial views. P. newmani right jugal SMU 76601 in F, lateral and G, medial views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 18

Figure 13 Squamosals of subadult individual of D. motherali, DMNH 2013–07–1859. Left in A, dorsal; orthographic image of 3D digital model in B, dorsal, C, ventral; orthographic image of 3D digital model in D, ventral views. Right in E, dorsal; orthographic image of 3D digital model in F, dorsal, G, ventral; orthographic image of 3D digital model in H, ventral, I, lateral, and J, posterior views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 19

Figure 14 Quadratojugal of subadult individual of D. motherali, DMNH 2013–07–1992. Right in A, dorsal; orthographic image of 3D digital model in B, dorsal, C, ventral; orthographic image of 3D digital models in D, ventral views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 20

Video 7 Orthographic digital model of the left quadrate from a subadult D. motherali, DMNH 2013–07–1992. Video available at www.cambridge.org/drumheller.

Figure 21

Figure 15 Orthographic images of 3D digital models of quadrates of juvenile and subadult individuals of D. motherali. Left quadrate DMNH 2013–07–1992 in A, dorsal, B, ventral, and C, posterior views; right quadrate DMNH 2013–07–1992 in D, dorsal, E, ventral, and F, posterior views; left quadrate DMNH 2013–07–0733 in G, dorsal, H, ventral and I, posterior views; right quadrate DMNH 2013–07–1997 in J, dorsal, K, ventral, and L, posterior views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 22

Video 8 Orthographic digital model of the left quadrate from an adult D. motherali, DMNH 2013–07–0733. Video available at www.cambridge.org/drumheller.

Figure 23

Video 9 Orthographic digital model of the right quadrate from an adult D. motherali, DMNH 2013–07–0001. Video available at www.cambridge.org/drumheller.

Figure 24

Figure 16 Orthographic images of 3D digital models of juvenile, subadult, and adult individuals of D. motherali demonstrating ontogenetic variability in the ventral fossa of the quadrate. Adult right quadrate DMNH 2013–07–0001 (reflected) A, subadult left quadrate DMNH 2013–07–0733 B, subadult left quadrate DMNH 2013–07–1992 C, and juvenile right quadrate DMNH 2013–07–1997 (reflected) D, in medial views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 25

Figure 17 Orthographic image of 3D digital models of dentaries of subadult individuals of D. motherali, DMNH 2013–07–1859. Left dentary in A, dorsal, B, ventral, C, lateral, and D, medial views; right dentary and splenial in E, dorsal, F, ventral, and G, medial views. Left dentary of DMNH 2013–07–0240 in H, lateral view. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 26

Video 10 Orthographic digital model of the right dentary from a juvenile D. motherali, DMNH 2013–07–1984. Video available at www.cambridge.org/drumheller.

Figure 27

Video 11 Orthographic digital model of the right dentary from a subadult D. motherali, DMNH 2013–07–1859. Video available at www.cambridge.org/drumheller.

Figure 28

Video 12 Orthographic digital model of the right dentary from an adult D. motherali, DMNH 2013–07–0001. Video available at www.cambridge.org/drumheller.

Figure 29

Figure 18 Lower jaw elements of subadult and adult individuals of D. motherali. Orthographic image of 3D digital models of right surangular DMNH 2014–06–01 in A, lateral, B, medial views; orthographic image of 3D digital models of left surangular and angular DMNH 2014–06–01 in C, lateral, D, medial views; right surangular and angular SMU 76810 in E, lateral view. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 30

Figure 19 Orthographic image of 3D digital models of lower jaw elements of subadult individuals of D. motherali. Left angular DMNH 2013–07–1859 in A, lateral and B, medial views; right angular DMNH 2014–06–01 C, lateral, and D, medial views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 31

Figure 20 Orthographic image of 3D digital models of left surangular and angular of D. motherali, DMNH 2014–06–01 articulated to show the groove (arrows) for the insertion of the posterior process of the dentary in A, oblique view. Orthographic image of 3D digital reconstruction of the lower jaw with the left dentary of DMNH 2013–07–0240 in B, lateral view. Posteriormost process of dentary missing from 3D model indicated with hatched lines. Orthographic image of 3D digital reconstruction P. newmani lower jaw SMU 76601 (reflected) C, lateral view. See text for anatomical abbreviations.

Not to scale.
Figure 32

Figure 21 Orthographic image of 3D digital models of articulars of subadult individuals of D. motherali, DMNH 2014–06–01. Left articular in A, dorsal, B, ventral, C, medial, D, lateral, and E, anterior views; right articular in F, dorsal, G, ventral, H, lateral, I, medial, and J, anterior views. See text for anatomical abbreviations.

Scale bar equals 5 cm.
Figure 33

Figure 22 Isolated teeth of D. motherali.A, B, DMNH 2013–07–0178 in mesial or distal views WM 2019–15 Gb in C, mesial or distal and D, lingual views.

Scale bar equals 2 cm.
Figure 34

Figure 23 Strict consensus topology from the first phylogenetic analysis based on the Turner matrix of 107 taxa and 321 characters. Four equally MPTs of 1,728 steps (CI = 0.233 and RI = 0.666) were obtained from a cladistic analysis. Paluxysuchidae are indicated in red. Numbers at each node indicate bootstrap GC values (top number) and Bremer support values (bottom number). Semilunar hash marks indicate stem-based definition and solid circles indicate a node-based taxon.

Figure 35

Figure 24 Strict consensus topology from the second phylogenetic analysis based on the H+Y matrix using 140 taxa and 387 characters, resulting in 130 equally MPTs of 1,285 steps (CI = 0.406 and RI = 0.843). Paluxysuchidae are indicated in red. Numbers at each node indicate bootstrap GC values (top number) and Bremer support values (bottom number). Semilunar hash marks indicate stem-based definition and solid circles indicate a node-based taxon.

Figure 36

Video 13 Composite, orthographic digital model of an adult D. motherali cranium and mandible. Video available at www.cambridge.org/drumheller.

Figure 37

Video 14 Composite, orthographic digital model of a subadult D. motherali cranium and mandible. Video available at www.cambridge.org/drumheller.

Figure 38

Figure 25 Orthographic image of 3D digital reconstruction of a D. motherali adult skull in A, dorsal, B, lateral views and a subadult skull in C, dorsal, D, lateral views.

Scale bar equals 10 cm.
Figure 39

Table 1 Measurements of labiolingual tooth diameters in mms. Teeth are listed by anatomical position (p = premaxilla; m = maxilla; d = dentary) and numbered mesially to distally. Blank = no alveolus preserved for this position on this specimen; – = alveolus is preserved, but is too damaged or incomplete to reliably measure; ? = uncertainty with regards to the dental count; * = tooth/replacement tooth present

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