Redondasaurus

''Redondasaurus'' is an extinct genus or subgenus of phytosaur from the Late Triassic (late Norian or Rhaetian) of the southwestern United States. It was named by Hunt & Lucas in 1993, and contains two species, ''R. gregorii'' and ''R. bermani''. It is the youngest and most evolutionarily-advanced of the phytosaurs.

Specimens

Original specimens (1939-1992)

OMNH 1250, the first ''Redondasaurus'' specimen to be discovered, was a slender skull found in 1939 by D.E. Savage. Savage discovered the skull in the Travesser Formation of New Mexico, and originally referred it to the genus ''Machaeroprosopus''. In 1947, another phytosaur skull ( YPM 3294) was discovered by E.H. Colbert and J.T. Gregory in the Redonda Formation of New Mexico. Colbert & Gregory (1947) were the first to recognize that both skulls may represent a new taxon. In addition, they proposed that the skulls represented the most derived phytosaur species in North America, due to their supratemporal fenestrae being hidden in dorsal view.A third skull (CM 69727) was discovered by D.S. Berman in the 1980s. It was recovered from the ''Coelophysis'' Quarry of Ghost Ranch near Abiquiu, New Mexico. The deposits of the ''Coelophysis'' Quarry have variably been referred to as the Rock Point Formation or the "siltstone member" of the Chinle Formation. Ballew (1989) referred the Ghost Ranch skull to ''Pseudopalatus'' (now ''Machaeroprosopus'') ''buceros''.

''Redondasaurus'' named (1993)

The genus ''Redondasaurus'' was named by A.P. Hunt and S.G. Lucas in 1993. The name ''Redondasaurus'' is derived from the Redonda Formation and the Greek word "''saurus''," meaning lizard. The Redonda Formation is named after Mesa Redonda near Tucumcari, New Mexico. The authors had previously mentioned the unnamed phytosaur species in a 1992 paper on "Triassic Stratigraphy and Paleontology" in New Mexico.Lucas, SPENCER G., and ADRIAN P. Hunt. "Triassic stratigraphy and paleontology, Chama basin and adjacent areas, north-central New Mexico." New Mexico Geological Society Guidebook 43 (1992): 151-167.

Hunt & Lucas (1993) named two new species for ''Redondasaurus''. ''Redondasaurus gregorii'' consisted of Colbert & Gregory's Redonda Formation skull (which was termed the holotype) and Savage's Travesser Formation skull. ''Redondasaurus bermani'' was based on Berman's Ghost Ranch skull.

Other specimens (1993–present)

Many additional specimens have been added to ''Redondasaurus'' apart from the three originally placed in the genus in 1993. The first report from outside New Mexico, a skull impression (MNA V3498) from the Wingate Sandstone of Utah, was initially described by Morales & Ash (1993). Several skulls from the Bull Canyon Formation of Texas were mentioned in a Master's thesis by Chavez (2010). A juvenile skull of ''R. gregorii'' ( NMMNH P-44920) was first mentioned by Rinehart et al. (2009) and fully described by Lucas et al. (2013). It was collected from the ''Coelophysis'' Quarry, a site which had previously only produced the holotype of ''R. bermani''. Heckert et al. (2001) identified a massive flattened skull (NMMNH P-31094) from the Redonda Formation.

All specimens referred to ''Redondasaurus'' were discussed and redescribed by Spielmann & Lucas (2012). Several of the fossils were newly reported. The two most well-preserved skulls are from the Redonda Formation (an adult, NMMNH P-4983, and a juvenile, NMMNH P-31095). The oldest ''Redondasaurus'' specimen is an incomplete skull (UCMP V78034/119436) from the Petrified Forest Member (Chinle Formation) of Rio Arriba County, New Mexico. The authors also described a plethora of phytosaur postcranial bones from the Redonda Formation. The large sample of approximately 13 ''Redondasaurus gregorii'' skulls have helped to reconstruct growth series and sexual dimorphism trends in the species.

Description

''Redondasaurus'', like other phytosaurs, had a very long snout. Known skull lengths range from in juveniles to in very large adults, suggesting total lengths up to . The teeth of ''Redondasaurus'' have a columnar enamel microstructure while lines of arrested growth are rare. These characteristics are shared with other phytosaurs from Western North America, contrasting with those from Eastern North America ("'' Rutiodon''").

Differences between species

''R. gregorii'' is distinguished by the lack of a rostral crest. Complete skulls of this species are uncommon, but some fragmentary narrow-snouted phytosaur specimens from the Redonda Formation may be part of the taxon.

''R. bermani'' is distinguished by the presence of a partial crest on the rostrum. Only one skull of this species has been found, but Hunt and Lucas postulate that "by analogy with other phytosaurs, it is likely that this crested species was sub-equal in abundance with 'R. gregorii''".

Diagnostic features

The diagnostic criteria given in 1993 for the new genus was as follows:

''"Phytosaurid that differs from other genera in possessing supratemporal fenestrae that are essentially concealed in dorsal view and whose anterior margin only slightly emarginates the skull roof and has wide squamosal-postorbital bars."''

Hunt and Lucas also extended Colbert and Gregory's analysis that ''Redondasaurus'' was the most derived North American phytosaurs, as:

''"Phytosaurs show an evolutionary trend to displace ventrally the posterior portion of the midline of the skull roof. ''Redondasaurus'' represents the most advanced development of this character."''

Additional diagnostic criteria were introduced in 2012 by J. Spielmann and S.G. Lucas. These include:

# Reduced antorbital fenestra
# A prominent pre-infratemporal shelf
# A septomaxilla forming the anterolateral half of the external naris
# Thickened rim of the orbit
# Inflated posterior part of nasal
# Thickened dorsal osteoderms

Classification

Historically, studies of ''Redondasaurus'' have been hampered by small number of specimens available, of which only four skulls were recognized in literature. Recently, several Norian-Rhaetian phytosaur skulls have been referred to ''Redondasaurus'', which has brought the number of recognized skulls to ten. These new specimens encompass a range of sizes from hatchlings to adults and possibly include the first evidence of sexual dimorphism in the taxon.

Sexual dimorphism within ''Redondasaurus'' was also recognized by J. Spielman and S.G. Lucas on May 11, 2012, at the 64th Annual Meeting of the Geological Society of America.

Validity

Disagreement on the validity of ''Redondasaurus'' emerged 1995, when Long and Murry did not accept it and referred to the specimen as '' Pseudopalatus pristinus'' instead. The reason for this may have been that the type specimen of ''Redondasaurus'' is missing the entire narial area, left side of its snout, the anterior two thirds of the right premaxilla, and most of its palate. In addition to this, the term used by Savage to describe the first specimen found in 1939, ''Machaeroprosopus'', continues to be used by some scholars in place of ''Redondasaurus'' as the genus name. Hungerbühler ''et al.'' argued in 2013 that ''Redondasaurus'' should be regarded as a junior synonym of ''Machaeroprosopus'' because:

# Upon a comparison of cranial characters, ''Machaeroprosopus lottorum'' is found to bridge the morphological gap between ''Redondasaurus'' and ''Machaeroprosopus'' in such a way that the distinction becomes arbitrary.
# According to cladistic analysis, it is unlikely that ''Redondasaurus'' is in a basal position compared to other North American pseudopalatine phytosaurs.
# For ''R. gregorii'' and ''R. bermani'' to be sister taxa, three additional steps would be necessary for forming a phylogenetic tree. This is the case even if the rostral crest, used by Lucas and Hunt to differentiate ''R. gregorii'' and ''R. bermani'', is ignored in the analysis.

Paleoecology

The Chinle Group, where a large portion of ''Redondasaurus'' skulls have been found, is composed of fluvial and lacustrine sediments. Accumulations of fossils in the Chinle Formation can be found in floodplains, bogs, ponds, and fluvial channels. Additional paleontological and sedimentary evidence support the hypothesis that the climate of the Chinle was strongly influenced by high levels of precipitation.

Most ''Redondasaurus'' fossils have been collected from north-central and eastern New Mexico, with a few other occurrences in Texas and Utah. The Chinle Group is particularly important to paleontologists interested in aetosaurs, as it has been critical in establishing their biochronology in the Late Triassic.

''Redondasaurus'' is important because it serves as an index species for the Apachean Land Vertebrate Faunachron (LVF). Indeed, it is considered a true index fossil because ''Redondasaurus'' is temporally restricted and easily identified. The biostratigraphic importance of the genus was reaffirmed when it was determined that the beginning of the Apachean was lower than previously concluded. Rather than at the base of the Redonda Formation, the Apachean appears high in the Bull Canyon Formation. Correlating the vertebrate stratigraphy of ''Redondasaurus'' has also allowed for the correlation of Redonda locally within the southwestern USA. Given the recent acquisition of additional diagnostic characteristics, and the increase in number of ''Redondasaurus'' skulls recognized in literature, it is likely that the use of the genus as an index fossil will expand to other deposits and even globally.

References

Further reading

* ''The Great Rift Valleys of Pangea in Eastern North America'' By Peter M. LeTourneau, Paul Eric Olsen. Published 2003, Columbia University Press.
* ''Palaeogeography, Palaeoclimatology, Palaeoecology'' By Elsevier Science (Firm). Published 1998, Elsevier. v. 143. Original from the University of California.

External links

''Redondasaurus''
at the Paleobiology Database

{{Taxonbar, from=Q596876

Phytosauria
Prehistoric reptile genera
Late Triassic reptiles of North America
Chinle fauna
Fossil taxa described in 1993