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Angelosaurus is an Extinction genus of herbivorous Caseidae that lived during the late Cisuralian (Kungurian) and early Guadalupian (Roadian) in what is now Texas and Oklahoma. Like other herbivorous caseids, it had a small head, large barrel-shaped body, long tail, and massive limbs. Angelosaurus differs from other caseids by the extreme massiveness of its bones, particularly those of the limbs, which show a strong development of ridges, processes, and rugosities for the attachment of and . Relative to its body size, the limbs of Angelosaurus were shorter and wider than those of other caseids. The ungual phalanges looked more like hooves than claws. The few known cranial elements show that the skull was short and more robust than that of the other representatives of the group. Angelosaurus is also distinguished by its bulbous Tooth with shorter and wider crowns than those of other caseids. Their morphology and the high rate of wear they exhibit suggests a diet quite different from that of other large herbivorous caseids, and must have been based on particularly tough . A study published in 2022 suggests that the genus may be Paraphyly, with Angelosaurus possibly only represented by its type species A. dolani.
A. dolani is characterized by a heavy and massive skeleton, with shorter and wider limbs than those of other caseids. The humerus is one of the most distinctive elements of the skeleton by its extremely massive proportions. There is virtually no Diaphysis, and the width of the proximal end is almost equal to the total length of the bone. The delto-pectoral crest is highly developed and bears a prominent, knotty and rough process for the insertion of part of the Pectoralis major. Along the anterior margin of the proximal part of the humerus there is a strong ridge for the insertion of the deltoid muscle. The radial condyle of the humerus lies far anteriorly on the ventral and distal surface, and its proportions suggest that the head of the radius was massive. The femur is very massive with a deep and heavy proximal end. The internal trochanter is exceptionally strong and has a rough surface. Characteristically, it extends very close to the proximal end of the intertrochanteric fossa (a large concave surface located on the ventral side of the proximal end of the femur and where the puboischiofemoralis externus muscle inserted). The fourth trochanter, on the other hand, is weak. The distal condyles of the femur are large but not strongly differentiated, probably due to the presence of a Cartilage cap. A strong ridge passes proximally from the intercondylar fossa along the dorsal margin of the femur and continues over the area where the femoro-tibial portion of the triceps surae muscle likely originated. Like the femur, the tibia and fibula are characterized by their ends formed of unfinished bone, suggesting the presence of a substantial cartilage cover. This peculiarity, which is usually a sign of skeletal immaturity, is surprising because the holotype of A. dolani belongs to an adult animal as indicated by the complete ossification of various other parts of the skeleton. On the left foot, relatively large compared to the size of the body, the tarsal bones were found articulated but the Metatarsal bones and Phalanx bone were somewhat disarticulated. So Olson and Beerbower had some difficulty in determining the phalangeal formula. After re-examining the material discovered, Olson later assessed the phalangeal formula of the foot to be 2-2-2-3-3. The ungual phalanges are distinguished from those of other caseids by being short, broad, and smooth, and resemble hooves rather than claws. Some elements of the right manus show that the phalanges were wide and short. The pelvis is characterized by a pubis and ischium forming a broad flattened plate, with a weak symphysis for most of its length. The ilium, short and broad, shows some indication of the dorsal elevation characteristic of caseids, but the apex appears incomplete, possibly cartilaginous. The acetabulum is proportionately very wide and deep. The sacrum is composed of three vertebrae, the first and the second being fused together. The distal ends of the three sacral ribs are fused to form a broad plate that fits over the ilium. The thoracic vertebrae have relatively long transverse processes and there appears to have been a small ventral facet, indicating that the ribs were double-headed. The neural spines, although poorly preserved, appear to have been rather short. Two fragments of the upper and lower jaws indicate that the skull was rather small in relation to the size of the body, as is the case in other derived caseids. The two fragments of dentary and maxilla bear a few teeth which, although broken, had an ovoid section and were quite spaced, indicating that their total number should be low.
This species is mainly characterized by the morphology of its femur. The location of the internal trochanter is very characteristic in being located near the distal end of the intertrochanteric fossa. While it is located near the middle or proximal part of this fossa in the other two species. This internal trochanter is apparently fused with the fourth trochanter. There is no Adduction ridge. The anterior (internal) distal condyle is small and is sharply separated from the posterior by a deep groove. Finally, the shaft of the femur is very short.
The holotype (FMNH UR 827) is composed of the pelvis, the right femur, 16 presacral vertebrae, five of which have their associated ribs, 3 sacral, and 4 caudals, two of which are associated with chevrons. Also known are two sacral vertebrae and 2 presacral vertebrae forming an articulated series (FMNH UR 828), the right side of a pelvis lacking most of the ischium (FMNH UR 844), a right pubis (FMNH UR 845), an interclavicle (FMNH UR 846), two anterior dorsal ribs (FMNH UR 847 and 850), two median dorsal ribs (FMNH UR 848 and 849), a posterior dorsal rib (FMNH UR 851), a cervical rib (FMNH UR 852), four anterior caudal vertebrae (FMNH UR 853), and a fragment of premaxilla with two teeth (FMNH UR 854).
Subsequent excavations in the Omega quarry have uncovered many additional bones, including several previously unknown skeletal elements. This additional material includes a partial skeleton composed of the sacrum, 4 sacral vertebrae, 3 presacral, 18 caudal, and toe bones (FMNH UR 904), a right scapulocoracoid and a right humerus (FMNH UR 907), 20 presacral vertebrae (FMNH UR 908), a left scapulocoracoid (FMNH UR 909), a poorly preserved tibia (FMNH UR 911, doubtfully attributed to this taxon), 4 bones of the toes (FMNH UR 914), 3 presacral vertebrae with ribs (FMNH UR 916), a large left femur (FMNH UR 917), a fragment of maxilla with 2 teeth (FMNH UR 926), a Neurocranium and part of the palate (FMNH UR 927), a large rib (FMNH UR 928), a Pterygoid bone (FMNH UR 931), an anterior dorsal rib (FMNH UR 932), a clavicle (FMNH UR 933), the third presacral rib (FMNH UR 940), an anterior dorsal rib (FMNH UR 941), an isolated tooth (FMNH UR 942), a pair of articulated Mandible having retained their tooth rows (FMNH UR 943), 2 median dorsal ribs (FM NH UR 944), several anterior dorsal ribs (FMNH UR 945), 20 caudal vertebrae with ribs on the most anterior (FMNH UR 971), a pubis (FMNH UR 978), ilia and ischia of juvenile individuals (FMNH UR 979), and a left and right pelvis (FMNH UR 980).
No complete skull of Angelosaurus has yet been discovered. The species A. romeri provides the best picture of the cranial morphology in this genus. The skull is represented by an incomplete premaxilla with two teeth, a fragment of maxilla with two teeth, a braincase, a pterygoid, and a pair of lower jaws bearing an almost complete dentition. All these elements are consistent with each other indicating a fairly short, robust and heavy skull, with strong short teeth. The morphology of the skull in lateral view is not well known, but the premaxilla shows that the Nostril were large, and the fragment of maxilla shows the existence of a large orbit. These two fragments suggest that the elements of the skull were quite massive compared to those of Cotylorhynchus of comparable size. The skull of A. romeri must have looked like a slightly more solid and robust version of the basic pattern of the other derived caseids. The lower jaws show that the dentary is short and heavy with a strong symphysis. There is a moderately strong and wide shelf at the ventral margin of the symphysis.
The teeth of A. romeri differs very clearly from that of other caseids by their bulbous morphology with very short and wide crowns. The knowledge of the upper dentition is limited to four teeth, two being carried by an incomplete premaxilla and two others coming from a fragment of maxilla. The first premaxillary tooth is very different from that of other caseids genera, in being thick at the base and tapering to a blunt termination of the crown. The second tooth is similar in shape, but much smaller. Neither have cusps. The two maxillary teeth have a general structure similar to that of other derived caseids by having a base with a circular section, followed at the mid-height of the tooth by an enlargement of the crown, which then ends in a Lip-lingual thinning giving to the upper end of the crown a spatulate morphology. However, they differ from those of other caseids in being shorter and blunter, the crown ending in a flattened edge bearing five small longitudinal cusps. The pair of lower jaws retains a much more complete dentition. The three anterior teeth are very distinctive. They are very short and blunt with a very broad middle part, and lack cusps. The more posterior teeth are short and resemble the upper ones quite closely. The five cusps on the flattened dorsal margin of the crowns are very distinct. There are 11 teeth on the right side and 12 on the left, counting as present those which are being replaced. Apparently 12 is the correct number, the lowest number of teeth among the caseids from North America. Only the Russia Ennatosaurus has less with only 10 teeth per half jaw. The anterior teeth of the mandibles of A. romeri are relatively worn. Some of the most posterior teeth are worn and some are not. The cusps disappear quickly with wear and the final stages produce a button-shaped crown whose surface is formed by the bulbous, rounded area of the central part of the tooth. The robustness of these teeth, coupled with the heavy wear they show, indicate that the diet of A. romeri must have included plants that are tougher than those on which most other herbivorous caseids fed.
The postcranial skeleton of A. romeri differs mainly from that of the other two species of the genus in characteristics of the pelvis, femur, and humerus. The humerus, although large and heavy with strongly developed ridges and processes, differs from that of A. dolani by its less massive proportions and the presence of a distinct though relatively short shaft. The pelvis is characterized by a pubis and an ischium forming a large, somewhat saddle-shaped plate with a strongly ossified median symphysis whereas it was cartilaginous in A. dolani. In the holotype, the sacrum has only three vertebrae with three associated sacral ribs. However, the paratype FMNH UR 904 has four sacral ribs indicating the presence of four vertebrae in the sacrum of this specimen. It is likely that four is the normal number of sacral vertebrae in this species, as the sacrum of the holotype is in fact incomplete. In the holotype of A. romeri, the three sacral vertebrae are fused while in A. dolani only the first two are fused. The sacral ribs are blade-shaped and are almost completely separated from each other at the joint with the ilium. At most, a slight fusion is observed between the second and the third sacral rib. The femur is relatively small and strongly ossified. It is characterized by the position of the internal trochanter, which is located approximately halfway between the proximal and distal limits of the intertrochanteric fossa. The fourth trochanter is well developed and rises slightly above the ridge of the adductor. The anterior distal condyle is shallow and flat and is well separated from the posterior condyle. The latter is larger and bears a well-defined surface for articulation with the fibula. The Popliteal fossa space is prominent.
With a stratigraphic position equivalent to the central part of the Flowerpot Formation, the Chickasha Formation contains the most recent Permian tetrapod fauna of North America, including A. romeri. On the basis of its faunal composition, a Middle Permian (= Guadalupian) age was assigned to it several times. This attribution is based mainly on the presence in the Chickasha fauna of the Parareptilia Macroleter that was previously known only from the Mezen assemblage in European Russia, which contains a clearly Guadalupian non fauna, and also the caseid Ennatosaurus. Another possible clue of a Guadalupian age is the presence in the Chickasha fauna of the largest known representative of the Varanopidae, Watongia, whose large dimensions would be the sign of a late increase in size in the evolution of this clade, which would have taken the place of top predator in the absence of Sphenacodontidae. However, the presence of the genus Macroleter in both Russia and Oklahoma does not guarantee that the Mezen assemblage and the Chickasha formation are (sub) contemporary because various Permian genera had a wide temporal distribution, such Dimetrodon and Diplocaulus. Another example, the varanopid Mesenosaurus, originally known from the Guadalupian assemblage of Mezen, is also represented by a distinct species in a locality from Oklahoma radiometrically dated to the mid-Lower Permian (Artinskian), an age difference of at least 20 million years with the Russian species. Thus, the age of the Chickasha Formation can hardly be estimated from its fauna. Other researchers assign it a Kungurian age. However, magnetostratigraphic data suggest that the Chickasha formation probably dates from the lower Roadian. This age is also consistent with the Stratigraphy position of the Chickasha Formation which occupies a slightly higher position than that of the San Angelo Formation dated to the Kungurian-Roadian boundary.
The San Angelo Formation is composed at its base of hard, green, gray and brown and fine conglomerates, all of them unfossiliferous. The central part of the formation consists mainly of red corresponding to and mud deposited on the coastal plains during periodic Flood. The mode of preservation of the type specimen of Angelosaurus dolani, with the posterior part of the skeleton articulated and the anterior part incomplete and dislocated, suggests that the animal was trapped in muddy sediment and then devoured by carnivores who dispersed the exposed parts. The caseid Caseoides is also present in this part of the formation. These red mudstones are interspersed with a thin level of green sandstone, sandy mudstones, and evaporites. These correspond to a minor and ephemeral encroachment of Estuary, , and very shallow on the terrestrial part of the delta. The upper part of the San Angelo Formation is characterized by the preponderance of coarse sediments such as sandstones and conglomerates, but also including at its base sandy mudstones and at its top pure red mudstones. According to Olson, these sediments were deposited by wider and more powerful than those in the central part of the formation. However, in Oklahoma, strata equivalent to the San Angelo Formation, which were also considered fluvio-deltaic and coastal deposits, have been reinterpreted as being of aeolian origin. The base of the upper San Angelo Formation is characterized by the absence of the genus Angelosaurus and the abundance of Cotylorhynchus hanckoki, which is associated, among others, with the caseid Caseopsis, the Sphenacodontidae Dimetrodon, and the Captorhinidae Rothiniscus, and Kahneria. At the top of the San Angelo Formation, red mudstones are again the dominant sedimentary facies. The genus Angelosaurus is again present (with the species A. greeni), accompanied by Caseoides cf. agilis, R. multidonta and K. seltina.
In Oklahoma, the Chickasha Formation corresponds to the central part of the Flowerpot Formation in which it is locally inserted. The sediments that compose it are varied and include red shales, sandstones, mudstones, conglomerates, and evaporites, deposited in and channels bordering the sea and coastal lagoons. In the Omega quarry, all the fossils come from sandstones, mudstones and hard, Silicon dioxide conglomerates, arranged in lenses. They correspond to deposits of an old channel about 1.50 m thick and 4.6 m wide where the skeletons of Angelosaurus romeri have accumulated, but also those of a second caseid, Cotylorhynchus bransoni, and those of the captorhinid Rothianiscus. Elsewhere in this formation are known the Xenacanthida Orthacanthus, the Nectridea Diplocaulus, the temnospondyle Dissorophidae Nooxobeia, the pareiasauromorpha Nycteroleteridae Macroleter, and the Varanopidae Varanodon and Watongia.
Below is the first caseid cladogram published by Maddin et al. in 2008.
Another phylogenetic analysis performed in 2012 by Benson identifies Angelosaurus romeri as the sister group of the three species of Cotylorhynchus.
Below is the caseasaurs cladogram released by Benson in 2012.
In 2015, Romano and Nicosia published the first Cladistics study including almost all caseids, except for very fragmentary taxa such as Alierasaurus and Angelosaurus greeni. In this analysis, Angelosaurus and Ennatosaurus form a clade and this clade is the sister group of a clade containing the genus Ruthenosaurus and the three species of Cotylorhynchus.
Below is the caseid cladogram published by Romano and Nicosia in 2015.
In 2020, two published by Berman and colleagues also recover Angelosaurus as one of the most derived caseids. In the first cladogram, Angelosaurus romeri together with the three species of Cotylorhynchus and Alierasaurus form an unresolved polytomy. In the second cladogram, A. romeri is the sister taxon of a clade containing Cotylorhynchus and Alierasaurus.
Below are the two caseids cladograms published by Berman and colleagues in 2020.
A phylogenetic analysis published in 2022 by Werneburg and colleagues suggests that the genera Angelosaurus and Cotylorhynchus may be Paraphyly, the taxa other than their type species possibly belonging to different genera.
Below is the cladogram published by Werneburg and colleagues in 2022.
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