Monjurosuchidae

Choristodera (from the Greek χωριστός ''chōristos'' + δέρη ''dérē'', 'separated neck') is an extinct order of semiaquatic diapsid reptiles that ranged from the Middle Jurassic, or possibly Triassic, to the late Miocene (168 to 11.6 million years ago). Choristoderes are morphologically diverse, with the best known members being the crocodile-like neochoristoderes such as ''Champsosaurus''. Other choristoderans had lizard-like or long necked morphologies. Choristoderes appear to have been confined to the Northern Hemisphere, having been found in North America, Asia, and Europe, and possibly also North Africa. Choristoderes are generally thought to be derived neodiapsids that are close relatives or members of Sauria.

History of Discovery

Choristodera was erected in 1876, originally as a suborder of Rhynchocephalia by Edward Drinker Cope to contain ''Champsosaurus,'' which was described from Late Cretaceous strata of Montana by Cope in the same paper. A year later, in 1877, ''Simoedosaurus'' was described by Paul Gervais from Upper Paleocene deposits at Cernay, near Rheims, France. These remained the only recognised choristoderes for over a century, until new taxa were described in the late 20th century. Beginning in the late 1970s, additional taxa were described by Soviet-Mongolian teams from Lower Cretaceous sediments in Mongolia. In studies from 1989 to 1991, Susan E. Evans described new material of ''Cteniogenys'' from the Middle Jurassic of Britain. The genus had first been described by Charles W. Gilmore in 1928 from the Late Jurassic of the western United States, and had previously been enigmatic. The studies revealed it to be a small, lizard-like choristodere, different from the crocodile-like forms previously known.

Description

Choristoderes vary substantially in size, the smallest genera like ''Cteniogenys'' and ''Lazarussuchus'' had a length of only around , and the largest known choristoderan, '' Kosmodraco dakotensis'' is estimated to have had a total length of around . Neochoristoderes such as ''Champsosaurus'' are the best-known group of the Choristodera. They resembled modern crocodilians, especially gharials. The skull of these animals have a long, thin snout filled with small, sharp conical teeth. Other choristoderes are referred to collectively as "non-neochoristoderes", which are mostly small lizard-like forms, though ''Shokawa, Khurendukhosaurus'' and ''Hyphalosaurus'' possess long plesiosaur like necks. The grouping of "non-neochoristoderes" is paraphyletic (not containing all descendants of a common ancestor), as the lizard-like bodyform represents the ancestral morphology of the group.

Skeletal anatomy

According to Matsumoto and colleagues (2019), choristoderes are united by the presence of 9 synapomorphies (shared traits characteristic of the group), including a median contact of the elongated prefrontal bones of the skull separating the nasal bones from the frontal bones, the dorsal flange of the maxilla is inflected medially (toward the midline of the body), the parietal foramen are absent, the squamosal bones are expanded behind ( posterior to) the occipital condyle, the teeth are conical and sub-thecodont (located in shallow sockets), the dentaries are slender with elongated grooves running along the labial (outward facing) surface of the bone, additional sacral vertebrae are present, expanded "spine tables" are present on the vertebrae, and the surfaces of both ends of vertebral centra are flat (amphiplatyan). All known choristoderans possess or are inferred to possess a novel skull bone not found in other reptiles, referred to as the "neomorphic bone" or neomorph, which is a component of the dermatocranium. It has been suggested that the bone may be homologous to the staples of other reptiles. The neomorph likely developed from the incomplete fusion of ossification centers of another skull bone, possibly the parietal. The neomorph is small and probably played little structural role in primitive choristoderes, suggesting it originated via a non-adaptive neutral mutation. Ancestrally, the skull of choristoderes possess elongated upper and lower temporal fenestrae (openings of the skull behind the eye socket), these are greatly expanded in neochoristoderes, most extremely in ''Champsosaurus'', giving the skull a cordiform (heart shaped) appearance when viewed from above. In many "non-neochoristoderes" the lower temporal fenestrae are secondarily closed. Choristoderes possessed gastralia (rib-like bones situated in the abdomen) like tuatara and crocodilians.

Internal skull anatomy

The internal skull anatomy of choristoderes is only known for ''Champsosaurus.'' The braincase of ''Champsosaurus'' is poorly ossified at the front of the skull (anterior), but is well ossified in the rear (posterior) similar to other diapsids. The cranial endocast (space occupied by the brain in the cranial vault) is proportionally narrow in both lateral and dorsoventral axes, with an enlarged pineal body and olfactory bulbs. The optic lobes and flocculi are small in size, indicating only average vision ability at best. The olfactory chambers of the nasal passages and olfactory stalks of the braincase are reasonably large, indicating that ''Champsosaurus'' probably had good olfactory capabilities (sense of smell). The nasal passages lack bony turbinates. The semicircular canals of the inner ear are most similar to those of other aquatic reptiles. The expansion of the sacculus indicates that ''Champsosaurus'' likely had an increased sensitivity to low frequency sounds and vibrations.

Dentition

Most choristoderes have rather simple undifferentiated (homodont) teeth, with striated enamel covering the tooth crown but not the base. Neochoristoderes have teeth completely enveloped in striated enamel with an enamel infolding at the base, labiolingually compressed and hooked, the exception being '' Ikechosaurus'' which has still rather simple teeth aside from the start of an enamel infolding. Teeth implantation is subthecodont, with teeth being replaced by erosion of a pit in the lingual (side of the tooth facing the tongue) surface of the tooth base. There is some tooth differentiation among neochoristoderes, with the anterior teeth being sharper and more slender than posterior teeth. Choristoderes retain palatal teeth (teeth present on the bones of the roof of the mouth). Unlike most diapsid groups, where palatal teeth are reduced or lost completely, the palatal teeth in choristoderes are extensively developed indicating food manipulation in the mouth, probably in combination with the tongue. In most choristoderes, longitudinal rows of palatal teeth are present on the pterygoid, palatine and vomer, as well as a row on the pterygoid flange. In some neochoristoderes the palatal tooth rows are modified into tooth batteries on raised platforms. The morphology of the palatal teeth is identical to that of the marginal teeth of non-neochoristoderes, and the replacement of palatal teeth is nearly identical to the replacement of marginal teeth.

Skin

An exceptionally preserved specimen of ''Monjurosuchus'' preserves pleated skin, which indicates that in life it was probably thin and soft. The preserved scales are small and overlapping, and are smaller on the ventral underside of the body than the dorsal surface. A double row of larger ovoid scales runs along the dorsum (upper midline) of the body. The fossil also preserves webbed feet. ''Hyphalosaurus'' was covered mostly in small, irregularly patterned polygonal scales, though these varied across the body. The scales of the hind legs were smaller, finer and more irregular than those of the torso, while the scales of the tail were nearly square and arranged in more regular rows. In addition to the small scales, two rows of large, round scutes with shallow keels ran along the animals sides. One row ran directly along the flank, with the other either slightly higher or lower and composed of scutes only 1/4 the size of the flank scutes. The flank row of larger scutes extended all the way to the base of the tail, and remained uniform in size across the entire row. The tail itself has preserved soft tissue extending well beyond the margins of the skeleton. This, combined with the already flattened appearance of the tail vertebrae, suggests that a ridge of skin may have extended from the top and bottom of the tail creating a small fin. Webbed feet are also preserved. Skin impressions of ''Champsosaurus'' have also been reported, they consist of small (0.6-0.1 mm) pustulate and rhomboid scales, with the largest scales being located on the lateral sides of the body, decreasing in size dorsally, no osteoderms were present. The Menat specimen of ''Lazarussuchus'' preserves some remnants of soft tissue, but no scales, which shows that the hindfoot (pes) was not webbed, and a dark stained region with a crenellated edge is present above the caudal vertebrae of the tail, suggestive of a crest similar to those found in some living reptiles, like the tuatara, lizards and crocodiles.

Paleobiology

Choristoderes are exclusively found in freshwater deposits, often associated with turtles, fish, frogs, salamanders and crocodyliformes. They appear to have been almost exclusively found in warm temperate climates, with the range of neochoristoderes extending to the high Canadian Arctic during the Coniacian-Santonian stages of the Late Cretaceous (~89-83 Million years ago), a time of extreme warmth. Due to the morphological similarities between choristoderes and crocodyliformes, it has often been assumed that they existed in competition. However "non-neochoristoderes" were smaller than adult aquatic crocodyliformes and were more likely in competition with other taxa. For the more crocodile-like neochoristoderes, there appears to have been niche differentiation, with gharial-like neochoristoderans occurring in association with blunt snouted crocodyliformes, but not in association with narrow snouted forms.

Diet

Neochoristoderans are presumed to have been piscivorous. ''Champsosaurus'' in particular is thought to have fed like modern gharials, sweeping its head to the side to catch individual fish from shoals, while ''Simoedosaurus'' is thought to have been more generalist, being able to take both aquatic and terrestrial prey. ''Cteniogenys'' and ''Lazarussuchus'' have been suggested to have fed on invertebrates. Preserved gut contents of a ''Monjurosuchus'' specimen appear to show arthropod cuticle fragments. Another specimen of ''Monjurosuchus'' has been found with preserved skulls of seven juvenile individuals within the abdominal cavity. This has been proposed to represent evidence of cannibalism. However, this proposal has been criticised by other authors, who suggest it is more likely that they represent late-stage embryos. A specimen of ''Hyphalosaurus'' has been found with small rib bones in its abdominal cavity, suggesting that it took vertebrate prey at least on occasion.

Reproduction

A specimen of ''Hyphalosaurus'' has been found with 18 fully developed embryos within the mothers body, suggesting that they were viviparous, but another specimen shows that ''Hyphalosaurus'' also possessed soft shelled eggs, similar to those of lepidosaurs. A possible explanation for this is that ''Hyphalosaurus'' was ovoviviparous, with the thin shelled eggs hatching immediately after they were laid, presumably on land. In ''Champsosaurus'', it has been suggested that adult females could crawl ashore to lay eggs on land, with males and juveniles appearing to be incapable of doing so, based on the presumably sexually dimorphic fusion of the sacral vertebrae and possession of more robust limb bones in presumed females. A skeleton of ''Philydrosaurus'' has been found with associated post-hatchling stage juveniles, suggesting that they engaged in post-hatching parental care.

Tracks

Tracks from the Early Cretaceous (Albian) of South Korea, given the ichnotaxon name '' Novapes ulsanensis'' have been attributed to choristoderans, based on the similarity of the pentadactyl (five fingered) preserved tracks to the foot morphology of ''Monjurosuchus''. The tracks preserve traces of webbing between the digits. The authors of the study proposed based on the spacing of the prints, that choristoderans could " high walk" like modern crocodilians. Tracks attributed to neochoristoderans dubbed '' Champsosaurichnus parfeti'' have also been reported from the Late Cretaceous Laramie Formation of the United States, though only two prints are present and it is not possible to distinguish between a manus (forefoot) or pes (hindfoot).

Classification and phylogeny

Choristoderes are universally agreed to be members of Neodiapsida, but their exact placement in the clade is uncertain, due to their mix of primitive and derived features, and a long ghost lineage (absence of a fossil record) after their split from other reptiles. After initially being placed in Rhynchocephalia, Cope later suggested a placement in Lacertilla due to the shape of the cervical vertebrae. Louis Dollo in 1891 returned Choristodera to Rhynchocephalia, but in 1893 suggested a close relationship with ''Pareiasaurus''. Alfred Romer in publications in 1956 and 1968 placed Choristodera within the paraphyletic or polyphyletic grouping of "Eosuchia", describing them, as “an offshoot of the basic eosuchian stock”, a classification which was widely accepted. However, the use of computer based cladistics in the 1980s demonstrated the non-monophyly of "Eosuchia", making the classification of choristoderes again uncertain. Subsequent studies either suggested placement as archosauromorphs, lepidosauromorphs or members of Diapsida ''incertae sedis''. In a 2016 analysis of neodiapsid relationships by Martín Ezcurra they were recovered as members of the advanced neodiapsid group Sauria, in a polytomy with Lepidosauromorpha and Archosauromorpha, with being the earliest diverging members of either group also being plausible.

Historically, the internal phylogenetics of Choristodera were unclear, with the neochoristoderes being recovered as a well-supported clade, but the relationships of the "non-neochoristoderes" being poorly resolved. However, during the 2010s, the "non-neochoristoderes" from the Early Cretaceous of Asia (with the exception of ''Heishanosaurus'') alongside ''Lazarussuchus'' from the Cenozoic of Europe were recovered (with weak support) as belonging to a monophyletic clade, which were informally named the "Allochoristoderes" by Dong and colleagues in 2020, characterised by the shared trait of completely closed lower temporal fenestrae, with ''Cteniogenys'' from the Middle-Late Jurassic of Europe and North America being consistently recovered as the basalmost choristodere. The long necked "non-neochoristoderes" ''Shokawa'' and ''Hyphalosaurus'' have often been recovered as a clade, dubbed the Hyphalosauridae by Gao and Fox in 2005. The finding of more complete material of the previously fragmentary ''Khurendukhosaurus'' shows that it also has a long neck, and it has also been recovered as part of the clade.

Phylogeny from the analysis of Dong and colleagues (2020):

Evolutionary history

Choristoderes must have diverged from all other known reptile groups prior to the end of the Permian period, over 250 million years ago, based on their primitive phylogenetic position. In 2015, Rainer R. Schoch reported a new small (~ 20 cm long) diapsid from the Middle Triassic (Ladinian) Lower Keuper of Southern Germany, known from both cranial and postcranial material, which he claimed represented the oldest known choristodere. '' Pachystropheus'' from the Late Triassic (Rhaetian) of Britain has been suggested to be a choristodere, but cannot be referred in confidence to the group as it lacks cranial material, on which most diagnostic characters of Choristodera are based. The oldest unequivocal choristoderan is the small lizard-like ''Cteniogenys,'' the oldest known remains of which are known from the late Middle Jurassic (Bathonian ~168-166 million years ago) Forest Marble and Kilmaluag formations of Britain, with remains also known from the Upper Jurassic Alcobaça Formation of Portugal and the Morrison Formation of the United States, with broadly similar remains also known from the late Middle Jurassic (Callovian) Balabansai Formation of Kyrgyzstan in Central Asia, the Bathonian Itat Formation of western Siberia, as well as possibly the Bathonian aged Anoual Formation in Morocco, North Africa.

Choristoderes underwent a major evolutionary radiation in Asia during the Early Cretaceous, which represents the high point of choristoderan diversity, including the first records of the gharial-like Neochoristodera, which appear to have evolved in the regional absence of aquatic neosuchian crocodyliformes. A partial femur of an indeterminate choristodere is known from the Yellow Cat Member of the Cedar Mountain Formation in North America. They appear to be absent from the well sampled European localities of the Berriasian aged Purbeck Group, Great Britain and the Barremian aged La Huérguina Formation, Spain, though there is a record of a small ''Cteniogenys''-like taxon from
the Berriasian aged Angeac-Charente bonebed in France.Ronan Allain, Romain Vullo, Lee Rozada, Jérémy Anquetin, Renaud Bourgeais, et al.
Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary
Geodiversitas, Museum National d’Histoire Naturelle Paris, In press. ffhal-03264773f In the latter half of the Late Cretaceous (Campanian-Maastrichtian), the neochoristodere ''Champsosaurus'' is found in Utah, Wyoming, Montana, North Dakota, Alberta and Saskatchewan, which were along the western coast of the Western Interior Seaway on the island of Laramidia. Indeterminate remains of neochoristoderes are also known from the Canadian High Arctic, dating to the early Late Cretaceous (Coniacian–Turonian) and from the Navesink Formation of New Jersey from the latest Cretaceous (Maastrichtian), which formed the separate island of Appalachia. Vertebrae from the Cenomanian of Germany and the Campanian aged Grünbach Formation of Austria indicate the presence of choristoderes in Europe during this time period. The only record of choristoderes from Asia in the Late Cretaceous is a single vertebra from the Turonian of Japan. Fragmentary remains found in the Campanian aged Oldman and Dinosaur Park formations in Alberta, Canada, also possibly suggest the presence of small bodied "non-neochoristoderes" in North America during the Late Cretaceous.

''Champsosaurus'' survived the K-Pg extinction, and together with fellow neochoristodere ''Simoedosaurus'' are present in Europe, Asia and North America during the Paleocene, however they became extinct during the early Eocene. Their extinction coincides with major faunal turnover associated with elevated temperatures. Small bodied "non-neochoristoderes", which are absent from the fossil record after the Early Cretaceous (except for possible North American remains), reappear in the form of the lizard-like ''Lazarussuchus'' from the late Paleocene of France. The European endemic ''Lazarussuchus'' is the last known choristodere, surviving the extinction of neochoristoderes during the Eocene, with the youngest known remains being those of ''L. dvoraki'' from the Early Miocene of the Czech Republic and indeterminate remains of ''Lazarussuchus'' reported from the late Miocene (~11.6 million years ago) of southern Germany.

References

Further reading

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External links

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* — brief article on the fossil record of choristoderes

{{Taxonbar, from=Q133068

Prehistoric animal orders
Tetrapod orders
Callovian first appearances
Middle Jurassic taxonomic orders
Late Jurassic taxonomic orders
Early Cretaceous taxonomic orders
Late Cretaceous taxonomic orders
Paleocene taxonomic orders
Eocene taxonomic orders
Oligocene taxonomic orders
Miocene taxonomic orders
Aquitanian extinctions
Tertiary extinctions of vertebrate taxa
Taxa named by Edward Drinker Cope