Phytosaur

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Phytosaurs
Temporal range: LadinianRhaetian, 242–201.4  Ma
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Possible Ghost lineage from the Middle Triassic, but see [1]
Redondasaurus bermani at CMNH 04 white background.jpg
Skeleton of Redondasaurus at the Carnegie Museum of Natural History
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Archosauromorpha
Clade: Archosauriformes
Clade: Eucrocopoda
Clade: Crurotarsi
Order: Phytosauria
von Meyer, 1861
Genera
Synonyms

Parasuchia Huxley, 1875

Phytosaurs (Φυτόσαυροι in greek, meaning 'plant lizard') are an extinct group of large, mostly semiaquatic Late Triassic archosauriform reptiles. Phytosaurs belong to the order Phytosauria. and are sometimes referred to as parasuchians. Phytosauria, Parasuchia, Parasuchidae, and Phytosauridae have often been considered equivalent groupings containing the same species. Some recent studies have offered a more nuanced approach, defining Parasuchidae and Phytosauridae as nested clades within Phytosauria as a whole. Phytosaurs were long-snouted and heavily armoured, bearing a remarkable resemblance to modern crocodilians in size, appearance, and lifestyle, as an example of convergence or parallel evolution

Contents

The name "phytosaur" means "plant lizard", as the first fossils of phytosaurs were mistakenly thought to belong to plant eaters. [2]

For many years, phytosaurs were considered to be the most basal group of Pseudosuchia (crocodile-line archosaurs), meaning that they were thought to be more closely related to the crocodilians than to birds (the other living group of archosaurs). Then some studies of the evolutionary relationships of early archosauriforms suggested that phytosaurs evolved before the split between crocodile- and bird-line archosaurs and are the sister taxon of Archosauria. The most recent study retains the former way of classifying phytosaurs as pseudosuchians. [3]

Phytosaurs had a nearly global distribution during the Triassic. Fossils have been recovered from Europe, North America, India, Morocco, Thailand, Brazil, Greenland [4] and Madagascar. Fossils attributed to phytosaurs have been found in Early Jurassic rocks, possibly extending their temporal range beyond the Triassic-Jurassic boundary. [5]

Description

Illustration of two Smilosuchus species, illustrating brachyrostral and dolichorostral snout types Smilosuchus-reconstructions-Jeff-Martz-600-px-tiny-Oct-2014-Tetrapod-Zoology.jpg
Illustration of two Smilosuchus species, illustrating brachyrostral and dolichorostral snout types

Phytosaurs are known from many different morphologies, specifically with vastly different skull forms. These changes relate to the feeding and habits of the animals, not completely evolutionary modifications. Dolichorostral ("long snouted") phytosaurs have a long, slender snout with many conical teeth that are homodont (all the same). These taxa were most likely piscivores that were well adapted to capture fast aquatic prey, but not terrestrial animals. Paleorhinus , Rutiodon and Mystriosuchus are dolichorostral phytosaurs, but do not form a distinct group of taxa (named Mystriosuchinae of Friedrich von Huene) as other morphotypes such as Pseudopalatus are more closely related to Mystriosuchus than it is to the other long-snouted taxa. Brachyrostral ("short snouted") forms are the opposite, having a massive, broad snout, and very strong skulls and jaws. They are heterodont, as the front teeth are prominent fangs, and the rear teeth are blade-like for slicing food into chunks that can be swallowed easily. Taxa like this, such as Nicrosaurus and Smilosuchus , were powerful taxa that fed on stronger prey, such as terrestrial animals that came to the water to drink. Altirostral ("high snouted") animals are intermediate between the two distinct types. They had heterodont dentition but not as extremely developed as the brachyrostral type. Pseudopalatus is an altirostral phytosaur, and was most likely a generalist feeder. Modern crocodilians exhibit a similar morphological diversity, for example the broad snouted altirostral alligator and the long snouted dolichorostral gavial. [6]

Various phytosaurs have crests and similar ornamentions in their snouts. Nicrosaurus has a ridge along the snout that would have supported a keratinous crest in life, while Mystriosuchus westphali has several bony crests. [6]

Differences from crocodiles

Despite their great similarities in appearance and lifestyle, there are still a number of minor differences that distinguish phytosaurs from true crocodiles. For one thing, the phytosaur ankle structure is much more primitive than that of any crocodile. Also, phytosaurs lack the bony secondary palate that enables crocodiles to breathe even when the mouth is full of water. However, it is possible that phytosaurs had a fleshy palate, as many Mesozoic crocodiles are presumed to have had. Phytosaurs were even better armoured than crocodiles, protected by heavy bony scutes (often found as fossils), and the belly reinforced with a dense arrangement of gastralia (abdominal ribs). Finally, and most noticeably, phytosaurs had nostrils placed near or above the level of the eyes, in contrast to crocodiles where the nostrils are near the end of the snout. This adaptation may have developed to allow them to breathe while the rest of the body was submerged.

Teeth

Unlike most crocodilians, phytosaurs have tooth serrations. [7]

In a 2001 study of the biomechanics of the dinosaur Albertosaurus 's teeth, William L. Abler also examined a phytosaur's teeth, finding that it had had serrations so fine that they resembled a crack in the tooth. [8] Albertosaurus had similarly crack-like serrations, but, at the base of each serration Abler discovered a round void, which would have functioned to distribute force over a larger surface area. [8] This void, termed an ampulla, would hinder the ability of the "crack" formed by the serration to propagate through the tooth. [8] The phytosaur was found to lack adaptations for preventing its dental "cracks" from propagating. [8] Abler examined another sort of prehistoric predator, Dimetrodon , and found that it also lacked adaptations for guarding against crack propagation. [8] Based on their teeth, most phytosaur genera are carnivorous, piscivorous, or a combination of the two. However, two taxa show slight adaptations towards hunting and consuming harder invertebrates. [9]

A study on phytosaur microwear patterns has found Mystriosuchus to line with soft invertebrate consumers, Nicrosaurus with hard invertebrate consumers and Smilosuchus and Machaeroprosopus with carnivores and piscivores. [10]

Locomotion and terrestriality

Phytosaurs have been traditionally held as rather "primitive" animals in regards to terrestrial locomotion, particularly in regards to archosaurs such as crocodilians, lacking the erect gait seen in these, other pseudosuchians, dinosaurs and pterosaurs. However, the Apatopus ichnofossil shows that the animals did in fact have an erect gait like their archosaur relatives. [11] [12]

Most phytosaurs are thought to be aquatic animals, and indeed most do show adaptations for such a lifestyle; swim tracks attributed to phytosaurs, for example, are known. [13] However, at least Nicrosaurus seems to have evolved towards a secondarily terrestrial lifestyle, developing longer limb bones, straighter femora and a deeper pelvis, and indeed occurs in terrestrial or marginal lacustrine settings. Combined with its deep upper jaw, it probably led a similar lifestyle to terrestrial predatory crocodylomorphs like sebecians. [14]

Inversely, some dolichorostral forms like Mystriosuchus have become further specialised to life in the water, and occurred in marine environments. [15] A skeleton of Mystriosuchus planirostris, found in a marine setting and with evidence of little post-mortem transportation – indicating that it died either at sea or in a freshwater environment nearby – shows that this animal had paddle-like limbs, less adapted for terrestrial locomotion than in most other phytosaurs. [16] Furthermore, the tail of Mystriosuchus was laterally compressed and could have been used in propulsion. [17]

Endocast studies

Scans on various phytosaur braincases suggest that these animals generally had long olfactory tracts, weakly demarcated cerebral regions, dorsoventrally short endosseous labyrinths and various sinuses, including large antorbital and dural venous ones; the general bauplan is vaguely similar to that of crocodilians, but differs significantly in the presence of multiple sinuses, smaller cerebral hemispheres and smaller endosseous labyrinths. The similarities are considered to be plesiomorphic in relation to the ancestral archosauriform design, lacking many features seen in avemetatarsalians, though convergence in terms of lifestyle might also play a role. [18]

Reproduction

No phytosaur eggs have been found so far. There are pits associated with footprints in the Chinle Formation, but these "nests" are apparently the result of sandstone weathering. [19] A recent study suggests they might have had parental care. [20]

History

When the first phytosaur fossils were found, it was not immediately obvious what kind of animal/species they were. The first phytosaur species known to science was named Phytosaurus cylindricodon – "plant lizard with cylindrical teeth" – by G. Jaeger in 1828 because he mistakenly believed that petrified mud fillings in the jaw were herbivore teeth. The specimen is too poor to be diagnostic, and this species name is no longer valid. The name of the group – Phytosauria – was coined by the German paleontologist Hermann von Meyer in 1861, on the basis of this first species.

The next species to be described was Belodon plieningeri by von Meyer in von Meyer and Plieninger 1844. The altogether more appropriate name Parasuchia ("alongside the crocodiles", as they resembled crocodiles to a great degree) was coined by Thomas Huxley in 1875 along with his discovery and naming of the Indian species Parasuchus hislopi (Chatterjee, 1978), on the basis of a partial snout. The specimen also is usually considered non-diagnostic, and the name Parasuchus replaced by Paleorhinus . Although the names Parasuchidae and Phytosauridae are variously still used by different specialists, "phytosaur" is the standard generic name for these animals, despite the fact that these animals have been clearly shown to be carnivorous.

Evolutionary history

Phytosaur skull Phytosaur skull.jpg
Phytosaur skull

Phytosaurs first appeared during the Carnian or Ladinian age, evolving from an unknown crurotarsan ancestor. There are no clear intermediate forms, as even the earliest known phytosaurs are highly specialized aquatic animals, unlike most contemporary archosauriforms that were terrestrial. However, a recent study has suggested that Diandongosuchus is a basal phytosaur. If this is the case, this taxon offers more of a bridge between phytosaurs and earlier Archosauriformes. [21]

The earliest phytosaurs are traditionally classified in the genus Paleorhinus , now thought to be polyphyletic. Parasuchus and related basal species were widely distributed, meaning that phytosaurs dispersed across Pangea early on and there were probably few geographical barriers for their distribution; only in the southernmost regions are they rare, possibly due to increased aridity. [22]

A somewhat more advanced and larger form, Angistorhinus appears at the same time or soon after. Later in the Carnian, both these animals were replaced by more specialised forms like Rutiodon , Leptosuchus , and the huge Smilosuchus (Lucas 1998). The Carnian-Norian extinction meant that these animals died off, and the Early Norian sees new genera like Nicrosaurus and Pseudopalatus, both of which belong to the most derived clade of phytosaurs, the Pseudopalatinae. Later in the middle Norian the advanced and specialised fish-eater Mystriosuchus appears. Fossil remains of this widespread animal is known from Germany, northern Italy, and Thailand. Finally the large Redondasaurus in southwest North America and the long-snouted (altirostral) Angistorhinopsis ruetimeyeri in Europe continued the group into the Rhaetian. Phytosaur footprints (the ichnotaxon Apatopus) are also known from the latest Rhaetian of the East Coast of USA (the Newark Supergroup) (Olsen et al. 2002). This indicates that phytosaurs continued as successful animals until the very end of the Triassic, when, along with many other large crurotarsan reptiles, they were killed off by the end Triassic extinction event, about 200 Ma ago.

There have been reports of phytosaur remains found in lowermost Jurassic rocks. Several teeth from Early Jurassic deposits in France have been identified as phytosaur teeth, but other studies argue they have either been misidentified or were reworked from Late Triassic into Early Jurassic deposits. In 1951, a partial upper jaw was discovered in the Early Jurassic Lower Lufeng Series in China and described as a new genus of phytosaur, Pachysuchus , but a study in 2012 reinterpreted the fossil as a sauropodomorph dinosaur. [23]

A fragment of a lower jaw from a longirostrine archosaur has been described from early Hettangian strata in the town of Watchet in Somerset, England. While teleosaurid thalattosuchians had similar longirostrine jaws to phytosaurs and were common in the Jurassic, they do not appear in the earliest Jurassic rocks. The mandible is more similar to those of known phytosaurs than to thalattosuchians, and likely belongs to a phytosaur closely related to the genus Mystriosuchus. The presence of phytosaurs in the earliest Jurassic may have prevented thalattosuchians from occupying similar ecological niches at that time. [24] However, more recent work suggests that the jaw fragment came from a pre-Hettangian rock unit, and is therefore Late Triassic in age. [23] Also, if the age of the Magnesian Conglomerate does extend into the Early Jurassic (Hettangian), then it is possible that Rileyasuchus survived into the Early Jurassic. [25]

Classification

Genera

GenusStatusAgeLocationUnitNotesImages

Angistorhinopsis

Junior synonym Junior synonym of Nicrosaurus

Angistorhinus

ValidLate Carnian

Flag of Morocco.svg  Morocco
Flag of the United States.svg  US

Argana Formation
Dockum Group
Popo Agie Formation

Angistorhinus grandis.jpg

Arganarhinus

ValidMiddle Carnian

Flag of Morocco.svg  Morocco

Argana Formation

Arribasuchus

Junior synonymJunior synonym of Machaeroprosopus

Belodon

Nomen dubium Middle Norian

Flag of Germany.svg  Germany
Flag of the United States.svg  US

Stubensandstein
Chinle Formation

Many remains have since been attributed to other animals or given their own genera Belodon.jpg

Brachysuchus

ValidCarnian

Flag of the United States.svg  US

"Pre-Tecovas Horizon" (Dockum Group)

Centemodon

Nomen dubiumNorian

Flag of the United States.svg  US

Cumnock Formation

Named from several teeth in 1856

Coburgosuchus

ValidNorian

Flag of Germany.svg  Germany

Colossosuchus ValidCarnian-NorianFlag of India.svg  India Tiki Formation

? Diandongosuchus

ValidLadinian

Flag of the People's Republic of China.svg  China

Falang Formation

Possible basalmost taxon. Diandongosuchus fuyuanensis.jpg

Ebrachosuchus

ValidLate Carnian

Flag of Germany.svg  Germany

Hassberge Formation

Francosuchus

Nomen dubiumLate Carnian

Flag of Germany.svg  Germany

Hassberge Formation

Leptosuchus

ValidCarnian

Flag of the United States.svg  US

Tecovas Formation and unknown formation (Dockum Group)

Machaeroprosopus

ValidCarnian-Norian

Flag of the United States.svg  US

Chinle Formation
Dockum Group

Rutiodon validus 21DB.jpg

Mesorhinosuchus

 ? ValidTriassic, ? early Olenekian

Flag of Germany.svg  Germany

? Middle Buntsandstein

Mystriosuchus

ValidMiddle Norian

Flag of Germany.svg  Germany

Stubensandstein

Nicrosaurus ValidLate Norian – Rhaetian

Flag of France.svg  France
Flag of Germany.svg  Germany

Arnstadt Formation
Upper Keuper

Nicrosaurus1Zittel.jpg

"Paleorhinus"

Junior synonym Late Carnian

Flag of Germany.svg  Germany
Flag of Poland.svg  Poland
Flag of the United States.svg  US

Hassberge Formation
Middle Keuper
Cooper Canyon Formation
Popo Agie Formation
Tecovas Formation

Polyphyletic.

Parasuchus

ValidLate Carnian – Early NorianFlag of India.svg  India

Lower Maleri Formation
Tiki Formation

Paleorhinus.jpg

Pravusuchus

ValidNorian

Flag of the United States.svg  US

Chinle Formation

Promystriosuchus

Valid

Protome

ValidNorian

Flag of the United States.svg  US

Chinle Formation

Protome batalaria.jpg

Pseudopalatus

Junior synonymJunior synonym of Machaeroprosopus

Redondasaurus

ValidNorian – Rhaetian

Flag of the United States.svg  US

Redonda Formation
Travesser Formation

Redondasaurus bermani at CMNH 04.jpg

Rutiodon

ValidCarnian

Flag of the United States.svg  US

Newark Supergroup

Rutiodon BW.jpg

Smilosuchus

ValidCarnian

Flag of the United States.svg  US

Chinle Formation

Smilosuchus adamanensis.jpg

Volcanosuchus

ValidCarnianFlag of India.svg  India Tiki Formation

Wannia

ValidCarnian-Norian

Flag of the United States.svg  US

Camp Springs Formation

Phylogeny

Phytosaurs are generally regarded as the most basal group of Crurotarsi, a clade of archosaurs that includes crocodilians and their extinct relatives. [26] [27] [28] Phytosaurs are often excluded from a clade called Suchia, which usually encompasses all other crurotarsans, including aetosaurs, rauisuchians, and crocodylomorphs. [28] Some studies have found polytomies between phytosaurs and other groups, like Ornithosuchidae and Suchia. In these cases, it is unclear whether phytosaurs are the most basal crurotarsans. [29] In one of the earliest studies of crurotarsan phylogeny, Sereno and Arcucci (1990) found Crurotarsi to be a monophyletic grouping consisting of phytosaurs, ornithosuchids, and the more derived suchians, but produced a trichotomy between the three groups in their tree. [30] In resolving this trichotomy, Parrish (1993) placed ornithosuchids, not phytosaurs, as the most basal crurotarsans. However, most other studies, such as Sereno (1991) and Benton et al. (2010), recover phytosaurs in a basalmost position among crurotarsans. [31] Below is a cladogram modified from Benton et al. (2010) showing the widely accepted phylogenetic relationships of phytosaurs: [28]

Archosauria  

Avemetatarsalia

  Crurotarsi  

Phytosauria

  Suchia  

Aetosauria

Crocodylomorpha

Ornithosuchidae

Rauisuchia

A phylogenetic analysis of early archosaurs by paleontologist Sterling Nesbitt (2011) found strong support for a sister taxon relationship between phytosaurs and Archosauria. [32] If this is the case, phytosaurs would be placed outside Pseudosuchia in a more basal position among archosauriforms. Phytosaurs would be considered closely related to the ancestors of both crocodilians and dinosaurs. Furthermore, the definition of the clade Crurotarsi would change, as it is often defined by the inclusion of phytosaurs. Thus, Crurotarsi would include phytosaurs and all other archosaurs —including dinosaurs— under this phylogeny. [33] Below is a cladogram showing the placement of phytosaurs from Nesbitt (2011): [32]

Archosauriformes  

Proterosuchus

Erythrosuchus

Vancleavea

  Proterochampsia  

Tropidosuchus

Chanaresuchus

Euparkeria

  Crurotarsi  
 Phytosauria 

Parasuchus

Leptosuchus

Pseudopalatus

  Archosauria  

Pseudosuchia

Avemetatarsalia

The phylogenetic analysis of Stocker (2010) placed Paleorhinus outside Phytosauridae as a basal phytosaur. Under this phylogeny, Phytosauridae and Phytosauria are not synonymous. Stocker also erected the clade Leptosuchomorpha for derived phytosaurs, including Leptosuchus and Smilosuchus. [34]

Ezcurra (2016) updated Nesbitt's analysis and found that Phytosauria was once again a group of basal pseudosuchian archosaurs. His study analyzed the ten phylogenetic traits which Nesbitt claimed were lacking in phytosaurs but not archosaurs, thus excluding phytosaurs from Pseudosuchia. Four of the traits (well-developed palatal processes of the maxilla which meet at the midline, an elongated cochlear recess, a tuber on the lateral side of the ulna, and a particular orientation of the calcaneal tuber) were confirmed to support Nesbitt's placement of Phytosauria. However, one of the ten traits was found in Euparkeria (an abducens nerve exit foramen only present in the prootic) and another was found in proterochampsians (a swollen biceps tubercule), so their lack in phytosaurs may be reversals rather than basal traits. Another one of the traits (an antorbital fossa contacting the horizontal process of the maxilla) was found in the basal phytosaur Parasuchus. One trait (short metacarpals compared to metatarsals) was difficult to analyze in any crurotarsan, and another (a medial tuber on the femur) was found in both proterochampsids and Parasuchus. One trait (a divided tibial facet of the astragalus) was also lacking in Marasuchus and Nundasuchus , and therefore had a variable existence in Archosauria. This reanalysis, along with the observance of many traits linking Phytosauria with pseudosuchians, concluded that it was more likely that phytosaurs were pseudosuchians than non-archosaur archosauriforms. The following cladogram is a simplified version the fourth strict reduced consensus tree of Ezcurra's third phylogenetic analyses within his study. This cladogram only shows taxa from the group Eucrocopoda. [35]

Eucrocopoda  

Dorosuchus

Euparkeria

Dongusuchus

Yarasuchus

  Proterochampsia  

Doswelliidae

Proterochampsidae

  Archosauria  

Ornithodira

  Pseudosuchia  
 Phytosauria 

Parasuchus hislopi

Parasuchus angustifrons

Nicrosaurus kapfii

Smilosuchus spp.

Nundasuchus

Ornithosuchidae

Suchia

Paleoecology

In the Late Triassic coprolite which could belong to a phytosaur, eggs of nematodes and probably protozoan cysts were found. [36]

Footnotes

  1. "Phytosauria: The phytosaurs". University of California Museum of Paleontology. Matt Wedel. Retrieved 20 June 2022.
  2. Colbert, Edwin H. (Edwin Harris); Knight, Charles Robert (1951). The dinosaur book: the ruling reptiles and their relatives. New York: McGraw-Hill. p. 152.
  3. Jones, Andrew S.; Butler, Richard J. (10 December 2018). "A new phylogenetic analysis of Phytosauria (Archosauria: Pseudosuchia) with the application of continuous and geometric morphometric character coding". PeerJ. 6: e5901. doi: 10.7717/peerj.5901 . PMC   6292387 . PMID   30581656.
  4. Mateus, O., Clemmensen L., Klein N., Wings O., Frobøse N., Milàn J., Adolfssen J., & Estrup E. (2014). The Late Triassic of Jameson Land revisited: new vertebrate findings and the first phytosaur from Greenland. Journal of Vertebrate Paleontology. Program and Abstracts, 2014, 182.
  5. Maisch, M.W.; Kapitzke, M. (2010). "A presumably marine phytosaur (Reptilia: Archosauria) from the pre-planorbis beds (Hettangian) of England". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 257 (3): 373–379. doi:10.1127/0077-7749/2010/0076.
  6. 1 2 Hungerbühler, A (2002). "The Late Triassic phytosaur Mystriosuchus westphali, with a revision of the genus". Palaeontology. 45 (2): 377–418. Bibcode:2002Palgy..45..377H. doi: 10.1111/1475-4983.00242 .
  7. Stocker, Michelle R.; Butler, Richard J. (2013). "Phytosauria". Geological Society, London, Special Publications. 379 (1): 91–117. Bibcode:2013GSLSP.379...91S. doi:10.1144/SP379.5. S2CID   219192243.
  8. 1 2 3 4 5 "Abstract," Abler (2001). Page 84.
  9. Bestwick, Jordan; Jones, Andrew S.; Purnell, Mark A.; Butler, Richard J. (2021). "Dietary constraints of phytosaurian reptiles revealed by dental microwear textural analysis". Palaeontology. 64 (1): 119–136. Bibcode:2021Palgy..64..119B. doi:10.1111/pala.12515. ISSN   0031-0239. S2CID   229504989.
  10. Bestwick, Jordan; Jones, Andrew S.; Purnell, Mark A.; Butler, Richard J. (2021). "Dietary constraints of phytosaurian reptiles revealed by dental microwear textural analysis". Palaeontology. 64 (1): 119–136. Bibcode:2021Palgy..64..119B. doi:10.1111/pala.12515. ISSN   0031-0239. S2CID   229504989.
  11. Padian, K., Li, C., & Pchelnikova, J. 2010. The trackmaker of (Late Triassic, North America): implications for the evolution of archosaur stance and gait. Palaeontology 53, 175–189.
  12. Klein, H. & Lucas, S. G. 2013. The Late Triassic tetrapod ichnotaxon Apatopus lineatus (Bock, 1952) and its distribution. Bulletin of the New Mexico Museum of Natural History 61, 313–324.
  13. Stocker, M. R. & Butler, R. J. 2013. Phytosauria. Geological Society, London, Special Publications 379, 91–117. Link is broken.
  14. Kimmig, J. 2013. Possible secondarily terrestrial lifestyle in the European phytosaur Nicrosaurus kapfii (Late Triassic, Norian): a preliminary study. Bulletin of the New Mexico Museum of Natural History and Science 61, 306–312.
  15. Butler, Richard J.; Jones, Andrew S.; Buffetaut, Eric; Mandl, Gerhard W.; Scheyer, Torsten M.; Schultz, Ortwin (2019). "Description and phylogenetic placement of a new marine species of phytosaur (Archosauriformes: Phytosauria) from the Late Triassic of Austria". Zoological Journal of the Linnean Society. 187: 198–228. doi: 10.1093/zoolinnean/zlz014 .
  16. Gozzi, E.; Renesto, S.A. (2003). "Complete specimen of Mystriosuchus (Reptilia, Phytosauria) from the Norian (Late Triassic) of Lombardy (Northern Italy)". Rivista Italiana di Paleontologia e Stratigrafia. 109 (3): 475–498.
  17. Renesto, S.A.; Lombardo, C. (1999). "Structure of the tail of a phytosaur (Reptilia, Archosauria) from the Norian (Late Triassic) of Lombardy (Northern Italy)". Nota Breve, Rivista Italiana di Paleontologia e Stratigrafia. 105 (1): 135–144.
  18. Lautenschlager, S. & Butler, R.J. Neural and endocranial anatomy of Triassic phytosaurian reptiles and convergence with fossil and modern crocodylians Article in PeerJ 4(7):e2251 · July 2016 doi : 10.7717/peerj.2251
  19. Anatomy, Phylogeny and Palaeobiology of Early Archosaurs and Their Kin Capa Sterling J. Nesbitt, Julia Brenda Desojo, Randall B. Irmis Geological Society of London, 2013 – 608 páginas
  20. Datta, Debajit; Mukherjee, Debarati; Ray, Sanghamitra (2019). "Taphonomic signatures of a new Upper Triassic phytosaur (Diapsida, Archosauria) bonebed from India: Aggregation of a juvenile-dominated paleocommunity". Journal of Vertebrate Paleontology. 39 (6): e1726361. Bibcode:2019JVPal..39E6361D. doi:10.1080/02724634.2019.1726361. S2CID   219087095.
  21. Michelle R. Stoker; Sterling J. Nesbitt; Li-Jun Zhao; Xiao-Chun Wu; Chun Li (2016). "Mosaic evolution in Phytosauria: the origin of long-snouted morphologies based on a complete skeleton of a phytosaur from the Middle Triassic of China". Society of Vertebrate Paleontology 76th Annual Meeting Program & Abstracts: 232.
  22. "Relationships of the Indian phytosaur Parasuchus hislopi Lydekker, 1885", Article · July 2015 DOI: 10.1002/spp2.1022
  23. 1 2 Paul M. Barrett and Xu Xing (2012). "The enigmatic reptile Pachysuchus imperfectus Young, 1951 from the Lower Lufeng Formation (Lower Jurassic) of Yunnan, China" (PDF). Vertebrata PalAsiatica. 50 (2): 151–159.
  24. Maisch and Kapitzke (2010).
  25. Hunt, A.P. (1994). Unpublished doctoral dissertation, discussed here
  26. Benton, M.J. (1999). "Scleromochlus taylori and the origin of dinosaurs and pterosaurs" (PDF). Philosophical Transactions of the Royal Society B: Biological Sciences. 354 (1388): 1423–1446. doi:10.1098/rstb.1999.0489. PMC   1692658 .
  27. Nesbitt, S.J. (2007). "The anatomy of Effigia okeeffeae (Archosauria, Suchia), theropod-like convergence, and the distribution of related taxa" (PDF). Bulletin of the American Museum of Natural History. 302: 1–84. doi:10.1206/0003-0090(2007)302[1:TAOEOA]2.0.CO;2. hdl:2246/5840. S2CID   55677195.
  28. 1 2 3 Brusatte, S.L.; Benton, M.J.; Desojo, J.B.; Langer, M.C. (2010). "The higher-level phylogeny of Archosauria (Tetrapoda: Diapsida)" (PDF). Journal of Systematic Palaeontology. 8 (1): 3–47. doi:10.1080/14772010903537732. hdl: 20.500.11820/24322ff3-e80e-45f2-8d53-d35fd104195c . S2CID   59148006.
  29. Gower, D.J.; Wilkinson, M. (1996). "Is there any consensus on basal archosaur phylogeny?". Proceedings of the Royal Society B: Biological Sciences. 263 (1375): 1399–1406. doi:10.1098/rspb.1996.0205. S2CID   86610229.
  30. Sereno, P.C.; Arcucci, A.B. (1990). "The monophyly of crurotarsal archosaurs and the origin of bird and crocodile ankle joints". Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen. 180: 21–52. doi:10.1127/njgpa/180/1990/21. S2CID   256805773.
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<span class="mw-page-title-main">Archosaur</span> Group of diapsids broadly classified as reptiles

Archosauria is a clade of diapsid sauropsid tetrapods, with birds and crocodilians being the only living representatives. Archosaurs are broadly classified as reptiles, in the cladistic sense of the term, which includes birds. Extinct archosaurs include non-avian dinosaurs, pterosaurs and extinct relatives of crocodilians. Modern paleontologists define Archosauria as a crown group that includes the most recent common ancestor of living birds and crocodilians, and all of its descendants. The base of Archosauria splits into two clades: Pseudosuchia, which includes crocodilians and their extinct relatives; and Avemetatarsalia, which includes birds and their extinct relatives.

<span class="mw-page-title-main">Crurotarsi</span> Clade of reptiles

Crurotarsi is a clade of archosauriform reptiles that includes crocodilians and stem-crocodilians and possibly bird-line archosaurs too if the extinct, crocodile-like phytosaurs are more distantly related to crocodiles than traditionally thought. Prior to 2011, the group had invariably included only archosaurs closer to crocodilians than to birds and other dinosaurs. An equivalent term for the crocodilian side of the archosaur family tree is Pseudosuchia. This traditional definition of Crurotarsi assumed that phytosaurs were crown-group archosaurs and more closely related to crocodilians than to birds. However, a 2011 study argued that the phytosaur lineage evolved prior to the split between birds and crocodilians. This would mean that phytosaurs were not true archosaurs, and therefore could not be considered representatives of croc-line archosaurs.

<span class="mw-page-title-main">Archosauriformes</span> Clade of reptiles

Archosauriformes is a clade of diapsid reptiles encompassing archosaurs and some of their close relatives. It was defined by Jacques Gauthier (1994) as the clade stemming from the last common ancestor of Proterosuchidae and Archosauria. Phil Senter (2005) defined it as the most exclusive clade containing Proterosuchus and Archosauria. Archosauriforms are a branch of archosauromorphs which originated in the Late Permian and persist to the present day as the two surviving archosaur groups: crocodilians and birds.

<span class="mw-page-title-main">Rauisuchia</span> Informal group of Triassic archosaurs with pillar-erect posture

"Rauisuchia" is a paraphyletic group of mostly large and carnivorous Triassic archosaurs. Rauisuchians are a category of archosaurs within a larger group called Pseudosuchia, which encompasses all archosaurs more closely related to crocodilians than to birds and other dinosaurs. First named in the 1940s, Rauisuchia was a name exclusive to Triassic archosaurs which were generally large, carnivorous, and quadrupedal with a pillar-erect hip posture, though exceptions exist for all of these traits. Rauisuchians, as a traditional taxonomic group, were considered distinct from other Triassic archosaur groups such as early dinosaurs, phytosaurs, aetosaurs, and crocodylomorphs.

<i>Euparkeria</i> Extinct genus of reptiles

Euparkeria is an extinct genus of archosauriform reptile from the Triassic of South Africa. Euparkeria is close to the ancestry of Archosauria, the reptile group that includes crocodilians, pterosaurs, and dinosaurs.

<span class="mw-page-title-main">Aetosaur</span> Extinct order of heavily armoured reptiles

Aetosaurs are heavily armored reptiles belonging to the extinct order Aetosauria. They were medium- to large-sized omnivorous or herbivorous pseudosuchians, part of the branch of archosaurs more closely related to crocodilians than to birds and other dinosaurs. All known aetosaurs are restricted to the Late Triassic, and in some strata from this time they are among the most abundant fossil vertebrates. They have small heads, upturned snouts, erect limbs, and a body ornamented with four rows of plate-like osteoderms. Aetosaur fossil remains are known from Europe, North and South America, parts of Africa, and India. Since their armoured plates are often preserved and are abundant in certain localities, aetosaurs serve as important Late Triassic tetrapod index fossils. Many aetosaurs had wide geographic ranges, but their stratigraphic ranges were relatively short. Therefore, the presence of particular aetosaurs can accurately date a site in which they are found.

<span class="mw-page-title-main">Pseudosuchia</span> Clade of reptiles

Pseudosuchia is one of two major divisions of Archosauria, including living crocodilians and all archosaurs more closely related to crocodilians than to birds. Pseudosuchians are also informally known as "crocodilian-line archosaurs". Despite Pseudosuchia meaning "false crocodiles", the name is a misnomer as true crocodilians are now defined as a subset of the group.

<span class="mw-page-title-main">Prestosuchidae</span> Extinct family of reptiles

Prestosuchidae is a polyphyletic grouping of carnivorous archosaurs that lived during the Triassic. They were large active terrestrial apex predators, ranging from around 2.5 to 7 metres in length. They succeeded the Erythrosuchidae as the largest archosaurs of their time. While resembling erythrosuchids in size and some features of the skull and skeleton, they were more advanced in their erect posture and crocodile-like ankle, indicating more efficient gait. "Prestosuchids" flourished throughout the whole of the middle, and the early part of the late Triassic, and fossils are so far known from Europe, India, Africa (Tanzania), Argentina, and Paleorrota in Brazil. However, for a long time experts disagree regarding the phylogenetic relationships of the group, what genera should be included, and whether indeed the "Prestosuchidae" constitute a distinct family.

<i>Parasuchus</i> Extinct genus of reptiles

Parasuchus is an extinct genus of basal phytosaur known from the Late Triassic of Andhra Pradesh and Madhya Pradesh, India. At its most restricted definition, Parasuchus contains a single species, Parasuchus hislopi. Parasuchus hislopi is one of several species belonging to a basal grade of phytosaurs, typified by the genus Paleorhinus. Historically, Paleorhinus has been known from better-described fossils, and many species have been lumped into that genus. Parasuchus hislopi, despite being described earlier than Paleorhinus, was considered an undiagnostic chimera until new neotype fossils were described in the late 1970s. Parasuchus hislopi and the two unambiguously valid species of Paleorhinus are all closely related; some authors have historically described them all under the species Paleorhinus, while others place the two Paleorhinus species into Parasuchus according to the principle of priority.

<i>Rutiodon</i> Extinct genus of reptiles

Rutiodon is an extinct genus of mystriosuchine phytosaurs from the Late Triassic of the eastern United States. The type species of Rutiodon, Rutiodon carolinensis, encompasses a large number of skulls and assorted postcranial fossils discovered in the Cumnock Formation of North Carolina. Fossils referable to the species are also known from Pennsylvania, New Jersey, and Virginia. Rutiodon carolinensis is the most well-described species of phytosaur in eastern North America, though its validity as a natural taxon has been questioned. Some paleontologists also recognize a larger and more robust species, Rutiodon manhattanensis, which is known from teeth and postcranial fossils from New Jersey and Pennsylvania.

<i>Terrestrisuchus</i> Genus of terrestrial crocodylomorph

Terrestrisuchus is an extinct genus of very small early crocodylomorph that was about 76 centimetres (30 in) long. Fossils have been found in Wales and Southern England and date from near the very end of the Late Triassic during the Rhaetian, and it is known by type and only known species T. gracilis. Terrestrisuchus was a long-legged, active predator that lived entirely on land, unlike modern crocodilians. It inhabited a chain of tropical, low-lying islands that made up southern Britain, along with similarly small-sized dinosaurs and abundant rhynchocephalians. Numerous fossils of Terrestrisuchus are known from fissures in limestone karst which made up the islands it lived on, which formed caverns and sinkholes that preserved the remains of Terrestrisuchus and other island-living reptiles.

<span class="mw-page-title-main">Ornithosuchidae</span> Extinct family of reptiles

Ornithosuchidae is an extinct family of pseudosuchian archosaurs from the Triassic period. Ornithosuchids were quadrupedal and facultatively bipedal, meaning that they had the ability to walk on two legs for short periods of time. They had distinctive, downturned snouts, unique, "crocodile-reversed" ankle bones, and several other features that distinguish them from other archosaurs. Ornithosuchids were geographically widespread during the Carnian and Norian stages of the Late Triassic with members known from Argentina, Brazil, and the United Kingdom. Four genera, comprising Ornithosuchus, Venaticosuchus, Dynamosuchus, and Riojasuchus are presently known. The family was first erected by German paleontologist Friedrich von Huene in 1908.

<i>Angistorhinus</i> Extinct genus of reptiles

Angistorhinus is an extinct genus of phytosaur known from the Late Triassic period of Texas and Wyoming, United States. It was first named by Mehl in 1913 and the type species is Angistorhinus grandis. Other species from Texas and Wyoming, A. alticephalus, A. gracilis and A. maximus, are cospecific with the type species. Angistorhinus is known from the holotype UC 631, partial skull and lower jaws recovered from the Popo Agie Formation, Chugwater Group, Wyoming and from the associated paratype UM 531, a partial skull, TMM 31098-1, skull and lower jaws and ROM 7977, partial skull and lower jaws, recovered from the 'Pre-Tecovas Horizon' in the Dockum Group, Texas. A possible second species, A. talainti is known from the Triassic of Morocco. In 1995, Long and Murry created the new combination, Angistorhinus megalodon by synonymy for Brachysuchus. Hungerbühler and Sues (2001) hypothesised that Angistorhinus is a junior synonym of Rutiodon. However, in 2010 Michelle R. Stocker retained the validity of Brachysuchus and of A. grandis.

Mystriosuchus is an extinct genus of phytosaur that lived in the Late Triassic in Europe and Greenland. It was first named by Eberhard Fraas in 1896, and includes four species: M. planirostris, M. westphali, M. steinbergeri, and M. alleroq.

<i>Smilosuchus</i> Extinct genus of reptiles

Smilosuchus is an extinct genus of leptosuchomorph parasuchid from the Late Triassic of North America.

<span class="mw-page-title-main">Suchia</span> Clade of reptiles

Suchia is a clade of archosaurs containing the majority of pseudosuchians. It was defined as the least inclusive clade containing Aetosaurus ferratus, Rauisuchus tiradentes, Prestosuchus chiniquensis, and Crocodylus niloticus by Nesbitt (2011). Generally the only pseudosuchian group which is omitted from Suchia is the family Ornithosuchidae, although at least one analysis classifies ornithosuchids as close relatives of erpetosuchids and aetosaurs. Phytosaurs are also excluded from Suchia, although it is not certain whether they qualify as pseudosuchians in the first place.

<span class="mw-page-title-main">Erpetosuchidae</span> Extinct family of reptiles

Erpetosuchidae is an extinct family of pseudosuchian archosaurs. Erpetosuchidae was named by D. M. S. Watson in 1917 to include Erpetosuchus. It includes the type species Erpetosuchus granti from the Late Triassic of Scotland, Erpetosuchus sp. from the Late Triassic of eastern United States and Parringtonia gracilis from the middle Middle Triassic of Tanzania; the group might also include Dyoplax arenaceus from the Late Triassic of Germany, Archeopelta arborensis and Pagosvenator candelariensis from Brazil and Tarjadia ruthae from Argentina.

<i>Diandongosuchus</i> Extinct genus of reptiles

Diandongosuchus is an extinct genus of archosauriform reptile, possibly a member of the Phytosauria, known from the Middle Triassic of China. The type species Diandongosuchus fuyuanensis was named in 2012 from the Zhuganpo Formation of Yunnan Province. It is a marine species that shows similarities with another Chinese Triassic species called Qianosuchus mixtus, although it has fewer adaptations toward marine life. It was originally classified as the basal-most member of the pseudosuchian clade Poposauroidea. However, a subsequent study conducted by Stocker et al. indicated it to be the basalmost known phytosaur instead.

Nundasuchus is an extinct genus of crurotarsan, possibly a suchian archosaur related to Paracrocodylomorpha. Remains of this genus are known from the Middle Triassic Manda beds of southwestern Tanzania. It contains a single species, Nundasuchus songeaensis, known from a single partially complete skeleton, including vertebrae, limb elements, osteoderms, and skull fragments.