Following the Permo–Triassic Extinction, large-bodied diapsid reptiles—with a body length >1 m—rapidly expanded their ecological roles. This diversification is reflected in enormous disparity in the development of the rostrum and adductor chamber. However, it is unclear how marked the diversity of the feeding apparatus was in contemporary small-bodied diapsids. Here we describe the remarkably small skull (2.5 cm long) of a saurian reptile, Colobops noviportensis, gen. et sp. nov., from the Triassic New Haven Arkose of Connecticut, USA. The taxon possesses an exceptionally reinforced snout and strikingly expanded supratemporal fossae for adductor musculature relative to any known Mesozoic or Recent diapsid of similar size. Our phylogenetic analyses support C. noviportensis as an early diverging pan-archosaur. Colobops noviportensis reveals extraordinary disparity of the feeding apparatus in small-bodied early Mesozoic diapsids, and a suite of morphologies, functionally related to a powerful bite, unknown in any small-bodied diapsid.
The early Mesozoic Era saw the initial flowering of the major tetrapod clades that dominated terrestrial ecosystems thereafter. The earliest representatives of crown-group Amphibia, Lepidosauria, and Archosauria all appeared during the Triassic Period, such that the interval is now recognized as a key time in the emergence of major vertebrate clades1,2. However, in reviews of vertebrate history, there is a long-running assumption that these clades emerged from unspecialized, generalist ancestors during the Triassic3. However, this does not mean that the stem taxa from which those crown groups emerged did not produce substantial diversity of their own during the Triassic; indeed, recent studies of early pan-archosaur clades have revealed a substantial morphological radiation4,5. Unfortunately, much of our understanding of this record is biased towards large and medium-sized species (>1 m total body length).
In present-day ecosystems, significant morphological and ecological disparity, as well as a substantial proportion of taxonomic diversity, reside in small-bodied animals (<1 m total body length), whereas preservational biases often exclude such species from the fossil record6. These unfortunate biases likely masks a far greater ecomorphological disparity than has generally been appreciated among stem-members of major tetrapod clades radiating during the Permo–Triassic transition in the early Mesozoic. Indeed, recent discoveries of beautifully preserved small-bodied fossils in the mid-Mesozoic of China have refuted the classic hypothesis that the Mesozoic pan-mammals were homogenously small, shrew-like animals7,8.
Here, we substantially expand the ecomorphological disparity of small-bodied vertebrates from the early Mesozoic with a new taxon from the Upper Triassic New Haven Arkose of Connecticut, USA9. The new form is represented by a very small partial skull (total skull length = 2.5 cm) of undetermined ontogenetic state first studied by ref. . The new taxon displays specializations of the feeding apparatus unprecedented in any other known small tetrapod, juvenile or adult. Despite its small body size, the new species possesses hypertrophied attachments for the jaw adductor muscles that fill the transverse width of the postorbital portion of the cranium and a heavily reinforced rostrum with extensive overlap of adjacent bones. The supratemporal fossae in this species are proportionally broader than in any other comparably sized crown-group reptile. Its presence at the dawn of the Mesozoic emphasizes that the major modern vertebrate clades originated in a world populated by small- and large-bodied ecomorphological extremes.
Sauria McCartney, 1802
Archosauromorpha von Huene, 1956
Rhynchosauria? Osborn, 1903b
Colobops noviportensis gen. et sp. nov.
“Sphenodontia indet.” Sues & Baird, 1993
Etymology. From the Greek κολοβός (kolobós) for “docked” or “shortened” and ὤψ (ṓps) for “face”. Refers to the abbreviated rostrum relative to most other known Triassic Diapsida. Novus Portus is a Latinized version of “New Haven”, in reference to the discovery of the fossil in the New Haven Arkose in New Haven County, Connecticut, USA.
Holotype. YPM VPPU 18835 (Yale Peabody Museum, Vertebrate Paleontology Princeton Collection), nearly complete cranium and coronoid process of right mandible, lacking tooth-bearing portions of premaxillae, maxillae, palate, and mandible (Fig. 1).
Locality and horizon. (Based on ref. 9) Near the junction of Routes 6A, 91, and 15 between Meriden and Middletown, CT, USA. The locality is part of the New Haven Arkose, Hartford Basin, Newark Supergroup. ref. 10 dated a section of the New Haven Arkose at 212 ± 2 Ma, indicating a middle Norian age.
Diagnosis. (1) Prominent, symmetrical fontanelle between frontals and parietals in midline (may reflect juvenility); (2) prefrontal and postfrontal contact one another to exclude frontal from orbit; (3) jugal maxillo-palatal junctions transversely broader than postorbital process of jugal; (4) dorsal exposure of postorbital transversely broad, with posteriorly directed process near the transverse midpoint of the supratemporal fenestra (may reflect juvenility); (5) palatine with transversely broad anterior concavity between lateral contact with maxilla and anteromedial contact with vomer.
A series of measures of the Colobops noviportensis holotype is presented in Supplementary Table 1. The rostrum is extremely short proportionally, comprising less than a quarter of the overall length of the skull (Fig. 1a). The proportional height of the skull cannot fully be assessed, as the ventral (and dentigerous) portions of the premaxillae, maxillae, and pterygoids are not preserved. However, the configuration of the palatines and preserved portions of the pterygoid transverse processes suggests that the skull was depressed relative to its length (Fig. 1c). The enlarged orbits are proportionally long and strongly oriented dorsolaterally. A large, dorsally convex piece of bone sitting medial to the jugal is the right coronoid process and the only portion of the mandible preserved. Comparisons with other taxa, where not otherwise referenced, are based on specimens listed in Supplementary Notes 1 and 2.
The rostrum of C. noviportensis is heavily weathered and fragmented, although our µCT scan suggests that much of the dorsal portions of the nasals and maxillae are complete (Fig. 1a). We interpret a narrow splint of bone situated between the lateral margin of the left nasal and the medial margin of the left maxilla as the posterodorsal process of the premaxilla (Fig. 1a, d) based on comparisons with early diverging pan-archosaurs (e.g., Mesosuchus browni, Prolacerta broomi). The presence of this apomorphy supports the identification of Colobops as a pan-archosaur.
The antorbital region of C. noviportensis is exceptionally reinforced. The nasal exhibits a dorsoventrally tall ventrolateral lamina that braces the entire medial surface of the facial process of the maxilla (Fig. 1d), much as in Rhynchosauria (e.g., M. browni, Teyumbaita sulcognathus) and Rhynchocephalia (Clevosaurus hudsoni, Sphenodon punctatus). The prefrontal similarly braces roughly half the dorsoventral height of the facial process of the maxilla in testudinate turtles11,12. The palatine bears an unusually broad prefrontal process that meets the similarly broad orbital contribution of the prefrontal, forming a wide prefrontal pillar bracing the skull roof against the jaws, similar to the transversely broad contact in many lepidosaurs13, turtles11,12, and deeply nested Rhynchosauria14,15. At its juncture with the ectopterygoid, the central portion of the jugal is twice as transversely broad as the ascending (=postorbital process), similar to durophagous squamates such as Adamisaurus magnidentatus16, Chamaeleolis chamaeleonides17, and Dracaena guianensis18.
The large orbits are directed somewhat dorsally, owing in part to the relatively low profile of the preserved skull, similar to modern Sceloporus spp. The prefrontal and postfrontal meet near the anteroposterior midpoint of the orbit, excluding the frontal entirely. The postfrontal is overall anteroposteriorly elongate, nearly excluding the medial process of the postorbital from contacting the parietal. The skull roof has a large, bilaterally symmetrical gap between the frontals and parietals in the midline. We identify this gap as a fontanelle based on the excellent preservation of the remainder of the skull roof and its symmetry on a sagittal plane. The posterior margin of the fontanelle is continuous with the transversely broad parietal foramen. The fontanelle may indicate that the specimen is a very young individual18,19 although fontanelles are maintained to maturity in some iguanians13,20.
The adductor chamber is remarkably voluminous in C. noviportensis; among sampled species—both Mesozoic and Recent (examples in Fig. 2). Indeed, based on a series of measures of early Mesozoic and Recent taxa, C. noviportensis is the smallest to possess such a proportionally broad space for jaw-closing musculature (Fig. 3). The supratemporal fenestra of C. noviportensis is proportionally broader than the orbital and preorbital portions of the skull (Fig. 1a). A similar condition arose independently in deeply nested Rhynchosauria21,22. There is a narrow, midline sagittal crest on the parietals posterior to the parietal foramen, indicating medial expansion of the m. adductor mandibulae profundus and m. pseudotemporalis superficialis. Proportionally, the adductor chamber occupies a similarly large percentage of the postorbital skull width as in hyperodapedontine rhynchosaurs and Trilophosaurus buettneri.
Only small portions of the braincase and splanchnocranium are preserved (Fig. 1b). The supraoccipital has a narrow ascending process that fits between the posteromedial margins of the parietals and small dorsolateral processes that fit against the lateral edges of the supratemporal processes of the parietals. A similar bracing of supraoccipital against braincase occurs in captorhinomorphs23,24. The basioccipital is poorly preserved, represented by a horizontally oriented, flat plate of bone positioned ventral to the supraoccipital. In contrast to modern lepidosaurs, a probable ossified parasphenoid rostrum is preserved in C. noviportensis as a dorsoventrally tall, mediolaterally compressed plate of bone that sits on the midline anterior to the basioccipital. The left epipterygoid is massive, with a thick dorsal process oriented posterodorsally (Fig. 1b), indicating a well-developed m. pseudotemporalis profundus and further reinforcement of the braincase region.
The only portion of the mandible preserved is a large, dorsally convex right coronoid process. It is unclear which mandibular bones contribute to this structure. This element sits posterior to the ectopterygoid, medial to the jugal, and lateral to the pterygoid. The prominence of this portion of the mandible is comparable to some extant lepidosaurs (e.g., Ctenosaura pectinata, Uromastyx hardwickii) and to some early-diverging pan-archosaurs such as Trilophosaurus buettneri25,26. It is strikingly different from the coronoid eminence in other rhynchosaurs, which is formed by the posterodorsal slope of the dentary reaching the dorsally expanded coronoid15.
Characterization of adductor hyperdevelopment
To characterize the relative size of the adductor chamber in C. noviportensis, we plotted the width of the dorsal exposure of the adductor muscle attachments relative to the total postorbital width of the skull in a range of extant and extinct diapsids. In the plot of skull size against adductor chamber width, C. noviportensis represents the smallest sampled diapsid to possess such a degree of adductor hypertrophy in terms of relative width and relative surface area (Fig. 3). The measures of C. noviportensis also fall above our calculated prediction intervals for these values. Measurements from all species used in this study are shown in Supplementary Table 1. Moreover, we identified a number of poorly understood trends in reptilian adductor evolution. In stem-Sauria, whether distantly related to the crown (e.g., the Pennsylvanian Petrolacosaurus kansensis) or closer to it (e.g., the Lopingian Youngina capensis, Fig. 2b), there is no embayment for the muscle mass on the lateral surface of the parietal and the space for the adductor chambers occupies <61% the total width of the postorbital skull. Among Permian and Triassic crown-group diapsids (=Sauria), early members of both lepidosaur and archosaur branches exhibit broader supratemporal fossae for the adductors, between 64% to nearly the full width of the skull in animals with very narrow sagittal crests (Fig. 2a, c–e). This has been noted as a phylogenetic character but never fully quantified27,28,29 (percentage values obtained from dataset presented in Supplementary Table 1).
Within individual species, overall skull size appears to correlate strongly with the relative breadth of the adductor chamber; juveniles recapitulate the transition from Permian Diapsida to crown-group with a small supratemporal fossa with small proportionally modest embayments on the parietal giving way to proportionally larger fossae and deeper parietal embayments. Among modern Lepidosauria30,31 and Archosauria19,32, the dorsal attachments of the adductor musculature on the skull roof grow allometrically, becoming proportionally wider and more prominent relative to the breadth of the skull (example illustrated in Fig. 4) in contrast to other soft tissue structures of the head (e.g., eyes33, brain34,35). Among sampled extant lepidosaurs, such crests occur in later ontogenetic stages of Ctenosaura similis, Iguana iguana, and Sphenodon punctatus (although we also note that size-related traits are sometimes decoupled from ontogeny in lepidosaurs36). Triassic stem-archosaurs with narrow sagittal crests include derived Rhynchosauria, Trilophosaurus buettneri, and Tanystropheus longobardicus. However, all sampled individuals with a sagittal crest—excluding Colobops noviportensis—have post-orbital skull widths >3 cm. If the C. noviportensis holotype represents an adult, the proportional size of its supratemporal fossae exceeds that in any other comparably sized diapsid. If it represents a juvenile, the proportional size of the fossae becomes more remarkable still, as similar-sized juveniles of Recent saurians have far smaller fossae.
To investigate the affinities of C. noviportensis, we integrated the taxon into a phylogenetic analysis with broad sample of Permian and Triassic diapsids (modified from ref. 37). Our phylogenetic analysis supports the hypothesis that C. noviportensis is a pan-archosaur and the earliest divergence within Rhynchosauria (sensu ref. 38), linked by four unambiguous synapomorphies (Fig. 5). One is an anatomical character otherwise unknown in Triassic amniotes: (1) an anterior lamina of the maxilla that laps laterally over the posterior surface of the premaxilla (also present in Mesosuchus browni and Rhynchosaurus articeps). However, the analysis indicates that the clade represented by the Late Triassic C. noviportensis diverged shortly after the Permo–Triassic Extinction, as the oldest-known probable rhynchosaur, Noteosuchus colletti, dates to the Early Triassic22. However, this position is weakly supported; two additional steps produce topologies in which C. noviportensis occupies some positions with pan-Archosauria and a position nested within Sphenodontia, a clade that converged anatomically on rhynchosaurs in numerous skull characters (for exploration of alternative topologies, see Methods). Its exact phylogenetic position may be further obscured if the holotype indeed belongs to a juvenile—juvenile specimens incorporated into morphology-based phylogenies tend to root basal to adults of the same species39,40. However, known juvenile specimens of Hyperodapedon41 already bear many synapomorphies that not only position them within Rhynchosauria, but also within Hyperodapedontinae (Supplementary Note 3). It is also possible that the branch including C. noviportensis and that including all other Rhynchosauria diverged rapidly following the divergence of Rhynchosauria as a whole, such that only a limited time existed for synapomorphies to accrue (suggested for early Diapsida42). Further study of early saurian phylogeny and more material of C. noviportensis are needed to resolve the species’ phylogenetic heritage.
The taxonomic diversity of small-bodied reptiles in early Mesozoic terrestrial faunas has expanded rapidly in the past half century26,43,44. Colobops noviportensis expands this taxonomic diversity of early saurians. It also adds to our understanding of disparity in these taxa, displaying a suite of cranial apomorphies otherwise unknown in Triassic reptiles and indicating a specialized feeding strategy.
Although the C. noviportensis holotype lacks preserved teeth, the well-preserved skull roof enables inferences about the nature of its bite. In extant squamates, the highly differentiated jaw adductor musculature is usually accentuated in one of two ways45,46: (1) the parietals may be embayed medially by deep concavities for the m. pseudotemporalis superficialis and the m. adductor mandibulae externus profundus (as in Ctenosaura pectinata, Iguana iguana47); or (2) the postorbitals and squamosals may be expanded transversely to accommodate the m. adductor mandibulae externus superficialis (as in Pogona vitticeps, Uromastyx hardwickii). In C. noviportensis, both of these traits are present, indicating that both portions of the adductor complex were enlarged.
The different roles the superficial and deep mandibular adductors play in food processing in extant saurians are not well understood. In a variety of extant squamates, electromyography studies show that all components of the mm. adductor mandibulae and mm. pseudotemporalis fire roughly simultaneously during nearly all portions of the feeding cycle48,49. The high coronoid process would have increased the moment arm of the attached jaw muscles, further enhancing the force of jaw closure50. Thus, for an animal of its body size, C. noviportensis likely had a more powerful bite than any other Triassic reptile.
Relatively large jaw muscle attachments in juveniles of modern Diapsida only occur in taxa that occupy ecomorphological extremes throughout ontogeny (e.g., the durophagous Chamaeleolis chamaeleonides17). Juvenile hyperodapedontine rhynchosaurs already possess a narrow sagittal crest41, but the smallest known individuals are more than twice the size of the C. noviportensis holotype. The presence of a fontanelle in the C. noviportensis holotype gives us pause about arguing for its relative ontogenetic state, but the presence of such enlarged adductor chambers in such a small skull is unprecedented regardless.
The expanded space for jaw muscles occurs concomitantly with rostral reinforcement in C. noviportensis, suggesting a functional correlation. The large overlap of the nasal, maxilla, and premaxilla differs from the comparatively little osseous contact between those elements in most early Sauria; indeed, only Rhynchocephalia and the much-larger Rhynchosauria approach this condition. Similarly broad overlap between nasal and maxilla also occurs in known Amphisbaenia (e.g., Rhineura floridana13; R. hatcheri51), highly modified head-first burrowers, some of which engage in durophagy52,53. No known taxon, extinct or extant, combines rostral and palatal expansion and reinforcement in the manner of C. noviportensis.
The best insights into the feeding of C. noviportensis come from the general shape of the adductor chamber. In C. noviportensis, the post-temporal process of the parietal is oriented laterally, as in Sphenodontia13,54 and Rhynchosauridae15,21, rather than posterolaterally as in most pan-lepidosaurs13,55 and pan-archosaurs2,38. These former two taxa share precision bites, in which the dentary tooth row fits within a groove between multiple upper tooth rows; it is possible that the shape of the adductor chamber shared with C. noviportensis indicates a similarly complex dental anatomy. However, the actual use of this highly specialized grooved tooth row likely differed greatly between these taxa. Sphenodon punctatus employs a distinctive, propalinal motion in which the lower tooth row slides mesiodistally between palatal and upper tooth rows56,57, whereas rhynchosaurids likely used a precision-shear bite21,58. These comparisons may indicate a similarly complex dental apparatus in C. noviportensis, but they are equivocal about the precise nature of the bite.
The increasing taxonomic and ecological diversity of Diapsida throughout the Permo–Triassic transition occurred in concert with a transition from relatively simple, unspecialized adductor chambers to a variety of distinct morphologies. The hypertrophied jaw muscles and reinforced rostrum at the small size of C. noviportensis illustrate that the extremes of feeding diversity did not solely involve large-bodied animals. No other known early Mesozoic taxon of similar body size possessed the combination of a powerful biting apparatus and a reinforced bony rostrum.
Reconstructing evolutionary radiations is a key goal of historical biological research. Many recent studies on the morphological histories of small-bodied vertebrate groups have incorporated only samples of extant species59,60. However, any attempt to conceptualize morphological radiations in deep time must be accompanied by continued sampling of the fossil record. Colobops noviportensis represents a combination of morphological traits unknown in extant amniotes, and thus a morphology that would not have been reconstructed in a macroevolutionary analysis based exclusively on extant species. The fossil record, when rigorously sampled and analyzed at all scales, has the potential to expand our understanding of the limits of morphology and ecology.
µCT scanning and three-dimensional reconstruction
YPM VPPU 18835 was µCT scanned at the Laboratory of Integrative Science’s Center for Nanoscale Systems at Harvard University (Cambridge, MA) by A. Pritchard. The specimen was initially scanned at a resolution of 0.01566797 mm for a total of 1812 slices (60 kV, 285 mA). There is a strong contrast between bone and matrix, although the sandstone does contain some similarly radio-opaque clasts. A volume rendering of the µCT data prior to segmentation is presented in Supplementary Fig. 1.
The individual bones of the specimen were segmented in VG Studio Max 3.0. We filtered these out of the resultant segmented bones by identifying textural differences between the dense bone and diffuse sandstone inclusions. Sutural boundaries were easy to identify in the palate and post-orbital regions. Narrow gaps were identified in the rostrum that demarcated the sutures between the nasals and maxillae. The identification of the premaxilla is based on (1) the separation between this element and the overlying maxilla and (2) the clear demarcation of two separate contacts for lateral elements on the lateral surface of the nasals. We were unable to identify a clear contact between the postorbital and jugal on either side. The central portions of the postorbital bars on both sides have been rendered in gray to emphasize the ambiguity of the reconstruction in these areas.
The specimen of Anolis sagrei reconstructed in Fig. 2a was stained using the contrast-staining agent phosphomolybdic acid. The specimen was µCT scanned at the Laboratory of Integrative Science’s Center for Nanoscale Systems at Harvard University (Cambridge, MA, USA) by B.-A. Bhullar. The specimen was initially scanned at a resolution of 0.0206 mm for a total of 1963 slices (80 kV, 85 mA) using a molybdenum target and a one-second exposure.
The scan data of Mesosuchus browni (SAM-PK 6536) used for this phylogenetic analysis was µCT scanned at the University of Texas Austin High-Resolution X-ray Facility by Matt Colbert (Austin, TX, USA). The specimen was scanned at a resolution of 0.07837 mm for a total of 1122 slices (200 kV, 180 mA).
We present a series of supplemental movies in .avi format to accompany the anatomical description of Colobops noviportensis presented in the main text. These include the three-dimensional reconstruction of Colobops noviportensis presented in Fig. 1 (Supplementary Movie 1), animations of the original slice data from our CT scan (Supplementary Movies 2–4), and animated cutaways of the three-dimensional volume rendering of the holotype (Supplementary Movies 5–7). These are also uploaded to Morphobank Project 2649. We also present several CT slices from a scan of Mesosuchus browni (SAM-PK 6536).
Measurements of supratemporal fossa and skull width
To assess the relative contribution of the muscle-bearing supratemporal fossa to the postorbital skull width, we measured the transverse width of the fossae at the anteroposterior midpoint of the supratemporal fenestra in a sample of extant and extinct reptiles (sample listed in Supplementary Notes 1 and 2). We inferred that the supratemporal fossae demarcate the limits and attachments of the jaw adductor musculature in crown-group Reptilia based on the conditions in Sauria (e.g.,45,46) a Level I inference per61. The same inference on stem-group Reptilia (e.g., Youngina capensis) is based on anatomical correlates, a Level II inference. The Recent sample was taken from the Yale Peabody Museum vertebrate zoology collections and measured using millimeter-scale Beads Landing calipers. The fossil sample and those from the National Museum of Natural History collections were measured using a sample of photographs and images in literature of skulls in dorsal view using the measure function in Fiji62. These values were plotted using the “plot” function in R v. 3.3.363. The resulting data points were color-coded and the axes labeled in Adobe Illustrator CC 21.0.2.
The full list of measurements presented in Fig. 3 is presented in Supplementary Table 1. We present a number of individual plots of lepidosaur taxa for which we measured a size-variable series to illustrate size-linked trends in the proportional size of the adductor chamber and supratemporal fossae. We first measured the breadth of the entire postorbital portion of the skull at the anteroposterior midpoint of the supratemporal fenestrae. At the same anteroposterior point, we measured the width of the supratemporal fossae. The proportional measures plotted indicate the relative contribution of the supratemporal fossae to the total postorbital breadth of the skull. The same data points are presented in a plot in which the x-axis is not log-transformed are presented in Supplementary Fig. 2. Plots, in which the x-axis is log-scaled, are presented for the lepidosaurs Sphenodon punctatus (Supplementary Fig. 3), Iguana iguana (Supplementary Fig. 4), Pogona vitticeps (Supplementary Fig. 5), Sceloporus occidentalis (Supplementary Fig. 6), Teius teyou (Supplementary Fig. 7), Physignathus lesuerrii (Supplementary Fig. 8), and Hydrosaurus pustulatus (Supplementary Fig. 9). For Supplementary Fig. 9, an ontogenetic series of skulls of the taxon is presented in dorsal view.
For the subsample of specimens for which the complete or near-complete anteroposterior length of the skull could be measured from scaled photographs, we obtained measures of the total anteroposterior length of the skull from the anterior most tips of the preserved premaxillae. Specimens were excluded when neither the premaxillae nor the margins of the external nares were preserved. We generated a measure of the triangle circumscribed by this length measurement and the transverse width measurement to generate a proxy of the dorsal surface area of the skull (log-transformed and used for the x-axis in Fig. 3c). For each of these skulls, we measured the surface area of the skull roof occupied by the supratemporal fossa from photographs by drawing the boundaries of the opening. The length, width, and supratemporal fossa area measurements were obtained using scaled photographs in Fiji v. 1.0 for OSX62.
Statistics for skull proportions measures
We examined the relationship between (a) the transverse width of the skull and the transverse width of the supratemporal fossae and (b) the transverse width of the skull and the proportional width of the supratemporal fossae using the regression modeling functions in R. The regression models resultant from these analyses and their r2 values are presented in Fig. 3. For both of these linear models, we also present prediction intervals developed using the predict function in R.
To examine the statistical relationships between measures of skull size and supratemporal fossa size (both absolute and proportional), we generated linear models for the relationships in R63. For absolute measurement variables that we plotted and analyzed (transverse breadth of the skull, transverse breadth of the supratemporal fossa, dorsal surface area of the skull), we log-transformed all measurements. We did not transform our proportion measurements (relative width of the supratemporal fossa, relative surface area of the supratemporal fossae), as they did not exhibit an evident binomial distribution. We employ skull width as the descriptive variable for overall skull size rather than anteroposterior length because of the large number of specimens in our dataset that lack a complete rostrum but possess well-preserved skull tables.
We developed linear models in R for the two relationships that exhibited a correlation: (a) the log-transformed values of skull width and supratemporal fossa width and (b) the log-transformed value of skull width and the proportional contribution of the supratemporal fossa to the width of the skull. The resultant equations and r2 values are presented in Fig. 3. In both of these cases, the measurements for C. noviportensis (YPM PU 18835) were excluded from the datasets in order to assess how far the taxon diverged from estimates. We used the log-transformation for raw measurements on the recommendation of ref. 64. However, we did not log-transform the proportion values, again on the recommendation of ref. 64.
For both of these two relationships, we also used the R function for generating prediction intervals. In the case of the absolute measures, the measures for C. noviportensis fall above the maximum-predicted value for the 90% prediction interval. In the case of the model describing the relationship between absolute skull width and the proportional width of the supratemporal fossae, the relative proportions of the supratemporal fossae in C. noviportensis fall above the maximum-predicted value for the 95% prediction interval. For the plot illustrating the proportional contribution of the surface area of the supratemporal fossae to the skull roof, C. noviportensis possesses proportionally larger supratemporal fossae than any other taxon measured of an equivalent skull size.
We analyzed the affinities of Colobops noviportensis using a phylogenetic dataset focused on Permo–Triassic Diapsida. The data matrix used is a modification of ref. 37, itself a combination of refs. 43,65,66. A full listing of material and phylogenetic characters used for the phylogenetic analysis is presented in Supplementary Notes 1 and 2. Modifications to the dataset are presented in Supplementary Notes 3 and 4. The dataset incorporates 57 terminal taxa and 323 characters. Illustrations of key morphological character states are provided in Supplementary Figs. 10–13.
Our parsimony analysis was run in TNT v. 1.167, employing the “Traditional Search” options including 10,000 replicates of Wagner trees (using random addition sequences), followed by tree bisection and reconnection (TBR) holding 10 trees per replicate. The best trees obtained at the end of the replicates were subjected to a final round of TBR branch swapping. We employed Rule 1 of ref. 68 for collapsing zero-length branches. We recovered 2 most-parsimonious trees of 1,100 steps. We employed the STATS.RUN TNT script to obtain the Consistency Index (CI = 0.326) and Retention Index (RI = 0.644) for all trees. We used the Bremer support option in the Trees submenu of TNT, calculating supports based on a new round of TBR, holding trees suboptimal by 15 steps. The most-parsimonious trees infer Colobops noviportensis as the sister taxon of Mesosuchus browni + all other Rhynchosauria. This clade has a Bremer support of 2, but it is not recovered in Bootstrap resampling analyses. We explored alternative phylogenetic positions for C. noviportensis, finding a position among Sphenodontia suboptimal but only by two steps (see Methods). The strict consensus is provided in Supplementary Fig. 14.
The topology is otherwise largely consistent with the parsimony analysis of ref. 37. However, this parsimony analysis does not infer a monophyletic Allokotosauria (defined in ref. 66 as “[t]he least-inclusive clade containing Azendohsaurus madagaskarensis, Flynn et al., 2010, and Trilophosaurus buettneri, Case, 1928a, but not Tanystropheus longobardicus, Bassani, 1886, Proterosuchus fergusi, Broom, 1903, Protorosaurus speneri von Meyer, 1830, or Rhynchosaurus articeps Owen, 1842”). Instead, Trilophosauria is the second divergence within Archosauromorpha following Protorosaurus speneri. Azendohsauridae (including Pamelaria dolichotrachela) is the sister taxon of a Boreopricea funerea + Kuehneosauridae clade.
A Bayesian analysis was run in MrBayes v. 3.269, using the Mk model using a gamma distribution for rate variation across sites. The analysis was performed with a sampling frequency of 1000, two concurrent runs (nruns = 2), and four Metropolis-coupled chains (nchains = 4) for 20,000,000 generations. A relative burn-in of 25% was used. The Potential Scale Reduction Factor (PSRF+) hovered around 1.0 as the runs converged, and the effective sample size (ESS), examined in Tracer v. 1.670 were substantially >200. The output from MrBayes following the 20,000,000 generations is uploaded to the ‘Documents’ section on Morphobank Project 2816. The results of the Bayesian analysis are presented in Supplementary Fig. 15. As in the parsimony analysis, the Bayesian analysis infers Colobops noviportensis as the sister taxon of Mesosuchus browni + all other Rhynchosauria. The clade is not particularly well supported, with a posterior probability of 0.6373.
The topology is consistent in most respects with the strict consensus of the most-parsimonious trees, with a few exceptions. The Bayesian analysis recovered Weigeltisauridae as the earliest-diverging diapsid clade after Orovenator mayorum, rather than Drepanosauromorpha as in the parsimony analysis. The Malagasy Permian diapsids are also not recovered in a single clade, rather occurring in a polytomy with Youngina and Sauria. Macrocnemus is not monophyletic; instead, M. bassanii and M. fuyuanensis form successive sisters to the rest of Tanystropheidae.
Intriguingly, the Bayesian analysis recovers a topology consistent with the parsimony analysis of ref. 37: Kuehneosauridae, Boreopricea funerea, and Trilophosauria form a single clade within Archosauromorpha. This result contrasts with the strict consensus recovered in the current parsimony analysis, in which a Kuehneosauridae + Boreopricea funerea clade is sister to Azendohsauridae. This clade is quite unstable; it is not recovered in the Bootstrap analysis and it has only a Bremer support of 1. The posterior probability of the (Kuehneosauridae + Boreopricea funerea) + Trilophosauria in the Bayesian analysis is 0.7108.
The results of our primary phylogenetic analyses are presented in Supplementary Figs. 14 (for the parsimony analysis) and 15 (for the Bayesian analysis). The limited support values for the phylogenetic position of Colobops noviportensis among Diapsida suggests that alternative phylogenetic hypotheses may be supported by small amounts of additional data. We chose to explore the pre-existing hypothesis that the C. noviportensis (YPM VPPU 18835) represents a sphenodontian rather than a pan-archosaur as originally suggested by ref. 9. To do so, we constrained C. noviportensis to be in a clade with the other Sphenodontia integrated into this analysis (Diphydontosaurus avonis, Planocephalosaurus robinsonae, Clevosaurus hudsoni, and Clevosaurus brasiliensis). The analysis with this constraint enforced was run in TNT v. 1.5 with identical parameters to the main parsimony analysis. The strict consensus of the minimum length trees from this constraint study is presented in Supplementary Fig. 16.
The resulting constraint analysis produced 13 minimum-length trees of 1102 steps (hit 6113 out of 10,000 replicates), with a CI = 0.326 and RI = 0.643. This value is only two steps longer than the most-parsimonious trees reported. In these suboptimal trees, Colobops noviportensis is resolved as the sister taxon of Clevosaurus brasiliensis + Clevosaurus hudsoni. This position of C. noviportensis is not particularly surprising owing to the suite of morphological characters shared between Clevosaurus, derived sphenodontians, and derived pan-archosaurs in this analysis. In these sub-optimal trees, Clevosaurus independently acquired a posterodorsal process of the premaxilla excluding the maxilla from the posterior margin of the naris. Other synapomorphies of the clade of Colobops noviportensis + Clevosaurus recovered by this analysis include: 14:0, frontals unfused to one another in midline; 311:1, ventral lamina of nasal fitting against the full dorsoventral height of dorsal process of maxilla; 315:1, dorsal margin of postorobital bar at same dorsoventral level as dorsal margin of orbit. Each of these represent convergences between derived Sphenodontia and pan-archosaurs.
Frustratingly, the only preserved portions of the holotype skull of Colobops noviportensis includes structures that evolved convergently in derived Rhynchocephalia and Rhynchosauria. Further discoveries, especially elements of the postcranium would be extremely useful in elucidating the affinities of the species. C. noviportensis, however, does possess a number of character states unknown in Sphenodontia, including: 252(0), lacrimal present as distinct ossification; 313(0), postorbital medial process sits posteroventral to postfrontal. The current character data available for C. noviportensis supports its affinity with Rhynchosauria, but we recognize the limited support for that hypothesis and the possibility that revisions to phylogenetic datasets and new discoveries of C. noviportensis will alter the topology.
This published work and the nomenclatural acts it contains have been registered in ZooBank, the proposed online registration system for the International Code of Zoological Nomenclature (ICZN). The ZooBank LSIDs (Life Science Identifiers) can be resolved and the associated information viewed through any standard web browser by appending the LSID to the prefix “http://zoobank.org/”. The LSIDs for this publication are: zoobank.org:act:A1500DA4-6D40-43FF-A771-6C3EEB1DE295 and zoobank.org:act:3C89EFD7-4E31-4C41-BBE3-7141BCE42A72.
The phylogenetic data matrix, inputs and outputs for the MrBayes analysis, the input and linear models for R, and supplemental movies of CT data and three-dimensional volume renderings are available on Morphobank (www.morphobank.org) Project 2816. Original CT data are available from the corresponding authors upon request.
Evans, S. E. At the feet of the dinosaurs: the early history and radiation of lizards. Biol. Rev. 78, 513–551 (2003).
Nesbitt, S. J. The early evolution of archosaurs: relationships and the origin of major clades. Bull. Am. Mus. Nat. Hist. 352, 1–292 (2011).
Carroll, R. L. Vertebrate Paleontology and Evolution (Freeman, New York, 1988).
Stocker, M. R. et al. A dome-headed stem archosaur exemplifies convergence among dinosaurs and their distant relatives. Curr. Biol. 26, 2674–2680 (2016).
Foth, C., Ezcurra, M. D., Sookias, R. B., Brusatte, S. L. & Butler, R. J. Unappreciated diversification of stem archosaurs during the Middle Triassic predated the dominance of dinosaurs. BMC Evol. Biol. 16, 188 (2016).
Mitchell, J. S. Preservation is predictable: quantifying the effect of taphonomic biases on ecological disparity in birds. Paleobiology 41, 353–367 (2015).
Ji, Q., Luo, Z.-X., Yuan, C.-X. & Tabrum, A. R. A swimming mammaliaform from the Middle Jurassic and ecomorphological diversification of early mammals. Science 311, 1123–1127 (2006).
Meng, Q.-J. et al. An arboreal docodont from the Jurassic and mammaliaform ecological diversification. Science 347, 764–768 (2015).
Sues, H.-D. & Baird, D. A skull of a sphenodontian lepidosaur from the New Haven Arkose (Upper Triassic: Norian) of Connecticut. J. Vertebr. Paleontol. 13, 370–372 (1993).
Wang, Z. S., Rasbury, E. T., Hanson, G. N. & Meyers, W. J. Using the U-Pb system of calcretes to date the time of sedimentation of clastic sedimentary rocks. Geochim. Cosmochim. Acta 62, 2823–2835 (1998).
Gaffney, E. S. The comparative osteology of the Triassic turtle. Proganochelys. Bull. Am. Mus. Nat. Hist. 194, 1–263 (1990).
Gaffney, E. S., Parsons, T. S. & Williams, E. E. An illustrated glossary of turtle skull nomenclature. Am. Mus. Novit. 2486, 1–33 (1972).
Gauthier, J. A., Kearney, M., Maisano, J. A., Rieppel, O. & Behlke, A. D. Assembling the squamate tree of life: perspectives from the phenotype and the fossil record. Bull. Peabody Mus. Nat. Hist. 53, 3–308 (2012).
Chatterjee, S. A rhynchosaur from the Upper Triassic Maleri formation of India. Philos. Trans. R. Soc. Lond. B Biol. Sci. 267, 209–261 (1974).
Montefeltro, F. C., Langer, M. C. & Schultz, C. L. Cranial anatomy of a new genus of hyperodapedontine rhynchosaur (Diapsida, Archosauromorpha) from the Upper Triassic of Southern Brazil. Earth Environ. Sci. Trans. R. Soc. Edinb. 101, 27–52 (2010).
Sulimski, A. New data on the genus Adamisaurus Sulimski 1972 (Sauria) from the Upper Cretaceous of Mongolia. Palaeontol. Pol. 38, 43–56 (1978).
Herrel, A. & Holanova, V. Cranial morphology and bite force in Chamaeleolis lizards–adaptations to molluscivory? Zoology 111, 467–475 (2008).
Maisano, J. A. Postnatal skeletal ontogeny in Callisaurus draconoides and Uta stansburiana (Iguania: Phrynosomatidae). J. Morphol. 251, 114–139 (2002).
Rieppel, O. Studies on skeleton formation in reptiles. v. Patterns of ossification in the skeleton of Alligator mississippiensis DAUDIN (Reptilia, Crocodylia). Zool. J. Linn. Soc. 109, 301–325 (1993).
Bellairs, A. d’A. & Kamal, A. M. in Biology of the Reptilia.Vol. 11. Morphology F (eds. Gans, C. & Parsons, T. S.) Ch. 1 (Academic Press, New York, 1981).
Benton, M. J. The Triassic reptile Hyperodapedon from Elgin: functional morphology and relationships. Philos. Trans. R. Soc. B Biol. Sci. 302, 605–718 (1983).
Ezcurra, M. D., Montefeltro, F. & Butler, R. J. The early evolution of rhynchosaurs. Front. Ecol. Evol. 3, 142 (2016).
Heaton, M. J. Cranial anatomy of primitive captorhinid reptiles from the late Pennsylvanian and Early Permian Oklahoma and Texas. Okla. Geol. Surv. Bull. 127, 1–84 (1979).
Price, L. Notes on the brain case of Captorhinus. Proc. Boston Soc. Nat. Hist. 40, 377–386 (1935).
Gregory, J. T. Osteology and relationships of Trilophosaurus. Univ. Tex. Publ. 4401, 273–359 (1945).
Robinson, P. L. An unusual sauropsid dentition. Zool. J. Linn. Soc. 43, 283–293 (1957).
deBraga, M. & Rieppel, O. Reptile phylogeny and the interrelationships of turtles. Zool. J. Linn. Soc. 120, 281–354 (1997).
Dilkes, D. W. The Early Triassic rhynchosaur Mesosuchus browni and the interrelationships of basal archosauromorph reptiles. Philos. Trans. R. Soc. B Biol. Sci. 353, 501–541 (1998).
Gauthier, J. A., Kluge, A. G. & Rowe, T. in The Phylogeny and Classification of the Tetrapoda, Vol. 1 (ed. Benton, M. J.) 103–155 (Clarendon Press, Oxford, 1988).
Jones, M. E. & Lappin, A. K. Bite-force performance of the last rhynchocephalian (Lepidosauria: Sphenodon). J. R. Soc. N. Z. 39, 71–83 (2009).
Bhullar, B.-A. S. A phylogenetic approach to ontogeny and heterochrony in the fossil record: cranial evolution and development in anguimorphan lizards (Reptilia: Squamata). J. Exp. Zool. B Mol. Dev. Evol. 318, 521–530 (2012).
Iordansky, N. N. in Biology of the Reptilia.Vol. 4. Morphology D (eds. Gans, C. & Parsons, T. S.) Ch. 3 (Academic Press, New York, 1974).
Werner, Y. L. & Seifan, T. Eye size in geckos: asymmetry, allometry, sexual dimorphism, and behavioral correlates. J. Morphol. 267, 1486–1500 (2006).
Jirak, D. & Janacek, J. Volume of the crocodilian brain and endocast during ontogeny. PLOS ONE 12, e0178491 (2017).
Bhullar, B.-A. S. et al. Birds have paedomorphic dinosaur skulls. Nature 487, 223–226 (2012).
Petermann, H., Mongiardino Koch, N. & Gauthier, J. A. Osteohistology and sequence of suture fusion reveal complex environmentally influenced growth in the teiid lizard Aspidoscelis tigris — Implications for fossil squamates. Palaeogeogr. Palaeoclimatol. Palaeoecol. 475, 12–22 (2017).
Pritchard, A. C. & Nesbitt, S. J. A bird-like skull in a Triassic diapsid reptile increases heterogeneity of the morphological and phylogenetic radiation of Diapsida. R. Soc. Open Sci. 4, 170499 (2017).
Ezcurra, M. D. The phylogenetic relationships of basal archosauromorphs, with an emphasis on the systematics of proterosuchian archosauriforms. PeerJ 4, e1778 (2016).
Tsai, C.-H. & Fordyce, R. E. Juvenile morphology in baleen whale phylogeny. Naturwissenschaften 101, 765–769 (2014).
Wiens, J. J., Bonett, R. M. & Chippindale, P. T. Ontogeny discombobulates phylogeny: paedomorphosis and higher-level salamander relationships. Syst. Biol. 54, 91–110 (2005).
Benton, M. J. & Kirkpatrick, R. Heterochrony in a fossil reptile: juveniles of the rhynchosaur Scaphonyx fischeri from the Late Triassic of Brazil. Palaeontology 32, 335–353 (1989).
Bever, G. S., Lyson, T. R., Field, D. J. & Bhullar, B.-A. S. Evolutionary origin of the turtle skull. Nature 525, 239–242 (2015).
Pritchard, A. C., Turner, A. H., Irmis, R. B., Nesbitt, S. J. & Smith, N. D. Extreme modification of the tetrapod forelimb in a Triassic diapsid reptile. Curr. Biol. 26, 2779–2786 (2016).
Borsuk-Bialynicka, M., Cook, E., Evans, S. E. & Maryanska, T. A microvertebrate assemblage from the Early Triassic of Poland. Acta Palaeontol. Pol. 44, 167–188 (1999).
Edgeworth, F. H. The Cranial Muscles of Vertebrates, 493 pp. (Cambridge University Press, London, 1935).
Holliday, C. M. & Witmer, L. M. Archosaur adductor chamber evolution: integration of musculoskeletal and topological criteria in jaw muscle homology. J. Morphol. 268, 457–484 (2007).
Oelrich, T. M. The anatomy of the head of Ctenosaura pectinata (Iguanidae). Misc. Publ. Univ. Mich. Mus. Zool. 94, 1–122 (1956).
Herrel, A. & De Vree, F. Jaw and hyolingual muscle activity patterns and bite forces in the herbivorous lizard Uromastyx acanthinurus. Arch. Oral. Biol. 54, 772–782 (2009).
Herrel, A., Cleuren, J. & Vree, F. Quantitative analysis of jaw and hyolingual muscle activity during feeding in the lizard Agama stellio. J. Exp. Biol. 200, 101–115 (1997).
Reilly, S. M., McBrayer, L. D. & White, T. D. Prey processing in amniotes: biomechanical and behavioral patterns of food reduction. Comp. Biochem. Physiol. A Mol. Integr. Physiol. 128, 397–415 (2001).
Kearney, M., Maisano, J. A. & Rowe, T. Cranial anatomy of the extinct amphisbaenian Rhineura hatcherii (Squamata, Amphisbaenia) based on high-resolution X-ray computed tomography. J. Morphol. 264, 1–33 (2005).
Estes, R. & Williams, E. E. Ontogenetic variation in the molariform teeth of lizards. J. Vertebr. Paleontol. 4, 96–107 (1984).
Pregill, G. Durophagous feeding adaptations in an amphisbaenid. J. Herpetol. 18, 186–191 (1984).
Fraser, N. C. The osteology and relationships of Clevosaurus (Reptilia: Sphenodontida). Philos. Trans. R. Soc. Lond. B Biol. Sci. 321, 125–178 (1988).
Jollie, M. T. The head skeleton of the lizard. Acta Zool. 41, 1–64 (1960).
Curtis, N. et al. Predicting muscle activation patterns from motion and anatomy: modelling the skull of Sphenodon (Diapsida: Rhynchocephalia). J. R. Soc. Interface 7, 153–160 (2010).
Gorniak, G. C., Rosenberg, H. I. & Gans, C. Mastication in the tuatara, Sphenodon punctatus (Reptilia: Rhynchocephalia): structure and activity of the motor system. J. Morphol. 171, 321–353 (1982).
Benton, M. J. Tooth form, growth, and function in Triassic rhynchosaurs (Reptilia, Diapsida). Palaeontology 27, 737–776 (1984).
Cooney, C. R. et al. Mega-evolutionary dynamics of the adaptive radiation of birds. Nature 542, 344–347 (2017).
Openshaw, G. H., D’Amore, D. C., Vidal-García, M. & Keogh, J. S. Combining geometric morphometric analyses of multiple 2D observation views improves interpretation of evolutionary allometry and shape diversification in monitor lizard (Varanus) crania. Biol. J. Linn. Soc. 120, 539–552 (2017).
Witmer, L. M. in Functional Morphology in Vertebrate Paleontology (ed. Thomason, J. J.) 19–33 (Cambridge University Press, Cambridge, 1995).
Schindelin, J. et al. Fiji: an open-source platform for biological-image analysis. Nat. Methods 9, 676–682 (2012).
R Core Team. R: A Language and Environment for Statistical Computing (R Foundation for Statistical Computing, Vienna, 2013).
Sokal, R. F. & Rohlf, F. J. Biometry (W. H. Freeman & Company, New York, 1995).
Pritchard, A. C., Turner, A. H., Nesbitt, S. J., Irmis, R. B. & Smith, N. D. Late Triassic tanystropheids (Reptilia, Archosauromorpha) from northern New Mexico (Petrified Forest Member, Chinle Formation) and the biogeography, functional morphology, and evolution of Tanystropheidae. J. Vertebr. Paleontol. 35, e911186 (2015).
Nesbitt, S. et al. Postcranial osteology of Azendohsaurus madagaskarensis (?Middle to Upper Triassic, Isalo Group of Madagascar) and its systematic position among stem archosaurs. Bull. Am. Mus. Nat. Hist. 398, 1–126 (2015).
Goloboff, P. A., Farris, J. S. & Nixon, K. C. TNT, a free program for phylogenetic analysis. Cladistics 24, 774–786 (2008).
Coddington, J. & Scharff, N. Problems with zero-length branches. Cladistics 10, 415–423 (1994).
Ronquist, F. et al. MrBayes 3.2: efficient Bayesian phylogenetic inference and model choice across a large model space. Syst. Biol. 61, 539–542 (2012).
Rambaut, A., Suchard, M. A. & Drummond, A. J. Tracer v. 1.6. Available at http://tree.bio.ed.ac.uk/software/tracer (2014).
We are grateful to R.G. Conrod for originally discovering the specimen in Meriden, CT in 1965 and donating the specimen to the Yale Peabody Museum. Marilyn Fox (YPM VP) further prepared the specimen after the prior publication by ref. 9. We thank C. Mehling and M. Norell (AMNH); A. Henrici (CM); S. Chapman, L. Steel, and P. Barrett (NHMUK); K. de Queiroz and A. Wynn (USNM VZ); J. Cundiff (MCZ); and G. Watkins-Colwell (YPM VZ) for access to curated museum specimens. A. Pritchard is funded by the National Science Foundation (DEB 1501851, BIO 1523871). J.A.G. and B.-A.S.B. received partial financial support from the Yale Peabody Museum of Natural History.
The authors declare no competing interests.
Publisher's note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Electronic supplementary material
About this article
Cite this article
Pritchard, A.C., Gauthier, J.A., Hanson, M. et al. A tiny Triassic saurian from Connecticut and the early evolution of the diapsid feeding apparatus. Nat Commun 9, 1213 (2018). https://doi.org/10.1038/s41467-018-03508-1