Acerosodontosaurus
Acerosodontosaurus is an extinct genus of neodiapsid reptiles that lived during the Upper Permian of Madagascar.[1][2] The only species of Acerosodontosaurus, A. piveteaui, is known from a natural mold of a single partial skeleton including a crushed skull and part of the body and limbs. The fossil was discovered in marine deposits of the Lower Sakamena Formation. In conjunction with several skeletal characteristics, this may indicate that Acerosodontosaurus individuals were at least partially aquatic.[2]
| Acerosodontosaurus | |
|---|---|
 | |
| Skull diagram | |
Scientific classification  | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Family: | †Tangasauridae |
| Genus: | †Acerosodontosaurus Currie 1980 |
| Type species | |
| †Acerosodontosaurus piveteaui | |
Acerosodontosaurus has generally been considered a "younginiform", part of a paraphyletic grade of Permian diapsids which linked the most basal ("primitive") diapsids (araeoscelidians such as Petrolacosaurus) to more derived ("advanced") diapsids, including the earliest ancestors of modern reptiles such as crocodilians and lizards.[2] However, its position within the grade is controversial. Initially considered a specimen of the contemporaneous Tangasaurus, Acerosodontosaurus was later described as a younginid in 1980[1] and a tangasaurid in 2009.[2] A 2018 study has even supported a hypothesis that it was not a "younginiform" at all, rather that it was an early member of pantestudines, the reptile lineage that would lead to modern turtles.[3]
History
Acerosodontosaurus is known from a single specimen stored at the Museum National d'Histoire Naturalle in Paris, France. This specimen, MNHN 1908-32-57, was referred to Tangasaurus and stayed undescribed until Phillip J. Currie recognized it as a new genus. He described it as Acerosodontosaurus piveteaui in 1980, a name which roughly translates to "Piveteau's needle-toothed lizard". The specific name references Jean Piveteau, a paleontologist who pioneered the study of Permian reptiles of Madagascar.[1]
The specimen was extracted from an unknown locality in the Lower Sakamena Formation, an Upper Permian geological formation in Madagascar. The Sakamena Formation was formed by coastal rift valleys, and can be characterized by a diverse assortment of aquatic, semiaquatic, and terrestrial animals, including many early diapsids. The Acerosodontosaurus specimen is a partial skeleton preserved as a compression fossil within a sandstone nodule. The skeleton is mostly but not entirely articulated, preserving most of the trunk, right forelimb, and small portions of the left forelimb and hindlimbs. Bones on the left side of the skull were displaced as the animal decayed, but the majority of the right side was able to fossilize.[1]
Most of the actual fossilized bones had been eroded away once the specimen was found, although well-preserved molds were left behind in the sandstone. Currie's description was based on latex casts made from the molds.[1] During a 2009 redescription by Constanze Bickelmann, Johannes Mueller, & Robert R. Reisz, new high-fidelity latex molds were created using improved techniques.[2]
Description
The preserved skeleton was about 30 centimeters (12 inches) in length from the tip of the snout to the base of the tail. The tail is unknown, but Currie (1980) estimated that the total length of the animal from snout to tail tip would have been 60 to 70 centimeters (24 to 28 inches). The body was wide and the limbs were of medium length. The overall impression was that of a medium-sized lizard, although Acerosodontosaurus is completely unrelated to true modern lizards.[1] Although the tail is unknown, it could have had a fin-like structure similar to that of Hovasaurus, which has been considered a close relative of Acerosodontosaurus.[2]
Skull
The tip and upper side of the snout were not preserved, but most of the other skull bones are known. The orbits (eye holes) were large, and the skull was longer in front of the eyes than behind them. The lower edge of each orbit was formed by a long forward branch of the jugal bone, which overlies an equally elongated rear branch of the tooth-bearing maxillary bone. The skull was somewhat broader than that of most other "younginiforms", as indicated by the width and curvature of the frontal and prefrontal bones. Nevertheless, it was proportionally similar to that of Hovasaurus.[4] The skull had an estimated total length of 55 millimeters (2.2 inches).[1]
The mandible (lower jaw) was long and slender. The rear part of the mandible, which was formed by the articular bone, bears a facet which connects to the quadrate bone of the cranium to form the jaw joint. Both the quadrate and the corresponding facet on the mandible are very large and strongly built.[2]
The numerous teeth of Acerosodontosaurus are conical, sharply pointed, and somewhat recurved. They are slightly longer towards the front of the skull, but otherwise are similar in size and shape throughout the skull and jaw, in contrast to the condition in earlier diapsids like Petrolacosaurus. Currie (1980) estimated that 37 teeth were present in the maxilla and 32 were in the preserved portion of the mandible, based on both preserved teeth and empty tooth sockets.[1] Under the same criteria but using different latex casts, Bickelmann, Mueller, & Reisz (2009) estimated 36 and 34, respectively.[2] The mandible would have had many more teeth than these estimations, since the front half of the jaw was not preserved. Acerosodontosaurus translates to "Needle-tooth lizard", referring to its high number of needle-like teeth which differ from those of other "younginiforms" in both shape and abundance.[1]
As a diapsid, Acerosodontosaurus had two holes known as temporal fenestrae on each side of the skull, behind the eyes. However, the lower temporal fenestra was not completely enclosed from below. In most early diapsids, such as Petrolacosaurus and Youngina, the lower edge of the lower temporal fenestra is formed by a bony bar composed of the rear branch of the jugal and the forward branch of the quadratojugal bone. Yet Acerosodontosaurus has a short rear branch of the jugal, and is completely missing a quadratojugal, rendering the lower temporal fenestra incompletely enclosed. While many later diapsids also have an incomplete lower temporal fenestra, the only other "younginiform" with such a trait is Hovasaurus.[2]
Vertebrae and ribs
At least 21 vertebrae were present, all from the neck, back, and hip; the tail is missing. The cervical (neck) vertebrae had shorter centra (main components) than the dorsal (back) vertebrae. A small pit (subcentral foramen) was present on both the left and right sides of each vertebral centrum. The neural spines (spinous processes) of the dorsal vertebrae are characteristically tall and rectangular compared to most "younginiforms", though not quite as tall as those of Hovasaurus. The centra are at their maximum length and the neural spines are at their maximum height at the vertebrae directly in front of the hip. The transverse processes (rib facets) were quite short. Although many ribs are incomplete, those that were mostly complete were long and curved, indicating that Acerosodontosaurus was a rather wide-bodied animal. As with most early diapsids, small wedge-like bones known as intercentra fill in the gaps between vertebrae. Numerous small, slender gastralia (belly ribs) were also present.[1][2]
Forelimbs
The forelimbs of Acerosodontosaurus are among the most diagnostic parts of the body. The only preserved portion of the pectoral girdle is a thin, slightly curved bone with tapered tips. This is likely a cleithrum, a bone which is absent in practically all diapsids. The only other neodiapsid known with certainty to retain a cleithrum is Hovasaurus.[2]
The humerus (forearm bone) is incomplete, but the entepicondyle and its corresponding foramen are rather well-developed. The capitulum and trochlea, on the other hand, are poorly differentiated.[2] The radius is twisted and curved, unusually similar to that of the choristodere Champsosaurus. The ulna is hourglass-shaped, straighter and characteristically slightly longer than the radius. Unlike in terrestrial diapsids, the olecranon process of the ulna was absent. Both the radius and ulna were flatter near the wrist and more blocky near the elbow.[1]
As with other early diapsids, Acerosodontosaurus had 11 carpal (wrist) bones. All of the carpals are well-separated. Most are similar in size and shape to those of Hovasaurus, with the exception of the medial centrale, a bone between the radiale and distal carpal I which is much smaller in Acerosodontosaurus. The first metacarpal (the hand bone which connects to the thumb) is small and stout, while the second, third, and fourth (which connect to the index, middle, and ring fingers) are incrementally longer. This contrasts with most other "younginiforms", in which the fourth metacarpal is significantly longer than the third. Hovasaurus is an exception, but even Acerosodontosaurus differs from that genus in that its metacarpals are not as short. The fifth metacarpal (which connects to the little finger) is as short as the first, but has a more "pinched" appearance. Some phalanges (finger bones) are obscured by the overlain skull, but those that are visible are short, with sharp and curved claws.[1][2]
Hip and hindlimbs
The ilium (upper blade of the hip) is fairly similar to that of Hovasaurus and other reptiles, though seemingly slightly thicker. The pubis (forward blade of the hip) is a heavily built bone, strongly curving inwards. As a result, the hips would have been quite wide in life. The outer surface of each pubis has a large, diagonally-oriented tubercule (knob- or ridge-like growth). The plate-like ischium (rear-blade of the hip) is incomplete and was initially overlooked. The femur (thigh bone) is long, curved, and robust, while the tibia and fibula (shin bones) are only preserved near the knee so their form is difficult to determine. No foot bones are preserved.[1][2]
Classification
Initially considered a specimen of Tangasaurus, Currie (1980) subsequently assigned Acerosodontosaurus to the family Younginidae.[1] The next year, his study of Hovasaurus noted that Acerosodontosaurus shared similarities with both tangasaurids and younginids, and he considered it ancestral to both families.[4] Other studies found a similar result, placing it as the most basal member of "Younginiformes".[5] The 2009 redescription of the genus partially deconstructed the concept of a monophyletic "Younginiformes" and assigned it to Tangasauridae.[2] The 2011 description of the basal neodiapsid Orovenator considered tangasaurids to be stemward (further from modern reptiles) compared to younginids,[6] while a 2016 study of archosauromorphs placed Acerosodontosaurus crownward (closer to modern reptiles) compared to Youngina.[7]
Bever et al. (2015) reported Acerosodontosaurus piveteaui as the sister to turtles (but not Claudiosaurus germaini)[8] in the results of their strict consensus for their parsimony analyses recovered from their total character matrix (Extended Data Figure 4) or their cranial-only matrix (Extended Data Figure 6). However, Acerosodontosaurus and Claudiosaurus are not sisters to turtles in the Bayesian analysis of their total character matrix (Extended Data Figure 5) or their cranial only-matrix (Extended Data Figure 7). Schoch & Sues (2018)[9] published the results of a reduced matrix using the previously mentioned matrix with the addition of four characters and Pappochelys rosinae (p. 956) but did not find Acerosodontosaurus or Claudiosaurus as the sister to turtles (Figure 20). Li et al. (2018)[3] also sampled the same reduced matrix (with the addition of eight characters, Eorhynchochelys sinensis, and rescoring of Sinosaurosphargis yunguiensis and Odontochelys semitestacea based on the authors’s re-examination of the material) and found the reduced matrix supported an Acerosodontosaurus-Claudiosaurus clade as the sister to the turtle clade.
A 2018 cladistic analysis of the stem-turtle Eorhynchochelys recovers Acerosodontosaurus as the sister taxa of Claudiosaurus rather than Hovasaurus. Acerosodontosaurus and Claudiosaurus were found to be the earliest pan-testudines, part of the lineage that leads to turtles as well as Eunotosaurus, Pappochelys, Eorhynchochelys, and Odontochelys under a very specific set of parameters (excluding a majority of taxa from the analysis).[3]
Paleobiology
Several skeletal features support the hypothesis that Acerosodontosaurus was aquatic. The olecranon process of the ulna was absent (or not developed into bone), a trait in common with the aquatic nothosaurs, ichthyosaurs, and thalattosaurs, but in contrast to terrestrial reptiles such as Thadeosaurus. Moreover, the radius is twisted (similarly to that of the aquatic champsosaurs), and the wrist has a "relaxed" structure, with the carpals (wrist bones) separated by gaps rather than tightly connected.[2]
References
- Currie, Philip J. (1980). "A new younginid (Reptilia: Eosuchia) from the Upper Permian of Madagascar". Canadian Journal of Earth Sciences. 17 (4): 500–511. Bibcode:1980CaJES..17..500C. doi:10.1139/e80-046.
- Bickelmann, Constanze; Müller, Johannes & Reisz, Robert R. (22 September 2009). "The enigmatic diapsid Acerosodontosaurus piveteaui (Reptilia: Neodiapsida) from the Upper Permian of Madagascar and the paraphyly of "younginiform" reptiles". Canadian Journal of Earth Sciences. 46 (9): 651–661. Bibcode:2009CaJES..46..651S. doi:10.1139/E09-038.
- Li, Chun; Fraser, Nicholas C.; Rieppel, Olivier & Wu, Xiao-Chun (22 August 2018). "A Triassic stem turtle with an edentulous beak". Nature. 560 (7719): 476–479. Bibcode:2018Natur.560..476L. doi:10.1038/s41586-018-0419-1. ISSN 1476-4687. PMID 30135526.
- Currie, P.J. (1981). "Hovasaurus boulei, an aquatic eosuchian from the Upper Permian of Madagascar" (PDF). Palaeontologia Africana. 24: 99–168.
- Evans, Susan E. (1988). "The early history and relationships of the Diapsida". In Benton, M. J. (ed.). The Phylogeny and Classification of the Tetrapods, Volume 1: Amphibians, Reptiles, Birds. Oxford: Clarendon Press. pp. 221–260.
- Reisz, Robert R.; Modesto, Sean P. & Scott, Diane M. (2011-12-22). "A new Early Permian reptile and its significance in early diapsid evolution". Proceedings of the Royal Society B: Biological Sciences. 278 (1725): 3731–3737. doi:10.1098/rspb.2011.0439. ISSN 0962-8452. PMC 3203498. PMID 21525061.
- Ezcurra, Martín D. (2016-04-28). "The phylogenetic relationships of basal archosauromorphs, with an emphasis on the systematics of proterosuchian archosauriforms". PeerJ. 4: e1778. doi:10.7717/peerj.1778. ISSN 2167-8359. PMC 4860341. PMID 27162705.
- Bever, G. S.; Lyson, Tyler R.; Field, Daniel J. & Bhullar, Bhart-Anjan S. (2015). "Evolutionary origin of the turtle skull". Nature. 525 (7568): 239–242. doi:10.1038/nature14900.
- Schoch, Rainer R. & Sues, Hans-Dieter (2018). "Osteology of the Middle Triassic stem-turtle Pappochelys rosinae and the early evolution of the turtle skeleton". Journal of Systematic Palaeontology. 16 (11): 927–965. doi:10.1080/14772019.2017.1354936.
