Teyujagua

Discovery and Naming

The holotype material, UNIPAMPA 653, was collected from an exposure in the Sanga do Cabral Formation in Southern Brazil, informally known as Bica São Tomé, located in the Paraná Basin. The locality is composed of five outcrops, with UNIPAMPA 653 being found roughly 5 metres (16 ft) above the base of outcrop 5, in a layer rich in calcareous concretions. The specimen was collected by a team from the Paleobiology Laboratory of the Universidade Federal do Pampa (Unipampa) at the beginning of 2015, and later described in a study co-authored by Dr. Felipe L. Pinheiro and others and published in Scientific Reports (Nature Publishing Group) in early 2016.

The skull was noted to be exceptionally well preserved, as many other fossils from the Sanga do Cabral Formation are typically more fragmented and poorly preserved, having been reworked from slightly older sediments amongst layers of conglomerates. In addition to its unusual completeness, the skull was also CT scanned to reveal further details of the fossil that were still hidden by the surrounding matrix, particularly areas of the left side of the skull, palatal and occipital regions.

The genus name Teyujagua is derived from Teyú Yaguá, one of seven legendary monsters that are a part of Guaraní mythology. The Guaraní people occupied a large territory in central east South America, including an area of Southern Brazil where the type locality of Teyujagua is located. Teyú Yaguá is often depicted as a huge lizard with either seven or one large dog-head. Pinheiro et al. named it for Teyú Yaguá with the intended literal translation of "fierce lizard", although "dog lizard" has been offered as the correct literal Guaraní translation. The specific name is derived from Greek paradoxa ("paradoxical", "unexpected"), referring to its unusual combination of ancestral and derived archosauriform characteristics.

Classification

In a phylogenetic analysis, Teyujagua was recovered as the sister taxon to Archosauriformes, in a more derived position than the Triassic Prolacerta. Pinheiro et al. performed the analysis using a novel data matrix assembled from two previous studies by Martin D. Ezcurra. Their analysis recovered two most parsimonious trees, both recovering a clade made up of Teyujagua and Archosauriformes. This clade is supported by five synapomorphies. The results of their analysis are reproduced and simplified below.

They also performed another analysis that included the enigmatic and poorly known Permian Eorasaurus, thought to be the oldest known archosauriform. The inclusion of Eorasaurus produced a broadly similar topology to the first analysis, with Teyujagua still occupying a sister position with Archosauriformes. However, it recovered Eorasaurus in an unresolved polytomy with Koilamasuchus, Fugusuchus, erythrosuchids and a clade composed of Euparkeriidae, Proterochampsia and Archosauria. This provides further support of archosauriform affinities for Eorasaurus, and so also supports the presence of archosauriform and archosauromorph ghost lineages extending back into the Permian period, at least into the middle Wuchiapingian of the late Permian. Under these results, Teyujagua would represent a relict taxon that survived the end-Permian extinction from a prior evolutionary history in the late Permian.

Evolutionary significance

Teyujagua provides a form of transitional morphology between Archosauriformes and other earlier archosauromorphs. Features previously considered unique to Archosauriformes, including the external mandibular fenestra and serrated teeth, are found in Teyujagua, and demonstrate that the key traits of Archosauriformes were acquired in a mosaic fashion, rather than evolving all at once. Furthermore, these features broadly relate to dietary adaptations, suggesting that archosauriform skulls were first being adapted for a predatory, hypercarnivorous lifestyle prior to the acquisition of features relating to pneumaticity (e.g. the antorbital fenestra and a closed temporal bar) that characterise later Archosauriformes.

Teyujagua also supports a two-phase radiation model of archosauriform evolution at the end of the Permian and into the Triassic. The first of these radiations occurred as a phylogenetic diversification during the Lopingian, possibly as a response to the end-Guadalupian extinction event, where archosauriforms evolved as disaster taxa to fill minor predatory roles in Permian ecosystems, alongside their archosauromorph relatives. The second radiation follows the end-Permian extinction, where archosauriforms increased in size, abundance and species richness, coming to occupy the dominant terrestrial roles in Triassic ecosystems. The presence of the archosauriform Eorasaurus and proterosuchid Archosaurus in the Late Permian supports the initial diversification model, and Teyujagua provides unique insight to the initial acquisition of traits in their early evolution in the Permian, as the skeletal records for Permian archosauriforms are rare and fragmentary.

Palaeoecology

The Sanga do Cabral Formation is interpreted as representing a broad, semiarid plain with localised shallow braided stream channels. The most common vertebrate fauna are the procolophonoid parareptiles, particularly the genus Procolophon, as well as the fragmentary remains of temnospondyl amphibians, including the rhytidosteid Sangaia and the capitosauroid Tomeia. Less common are the postcranial remains of other archosauromorphs, and possibly synapsids. The formation is roughly coeval with the Lystrosaurus Assemblage Zone in Karoo, South Africa, and shares a similar composition of Early Triassic fauna.

Teyujagua may have been a semi-aquatic ambush predator along the margins of lakes and streams, as suggested by the dorsally positioned nares, similar to some later Crocodyliformes. The serrated teeth and external mandibular fenestra imply the development of a hypercarnivorous lifestyle as in later Archosauriformes, although the limited binocular vision suggests it was a visually oriented terrestrial predator.