Galahadosuchus

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Galahadosuchus
Temporal range: Late Triassic Carnian–Rhaetian
Blocks A and B of NHMUK PV R 10002
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Pseudosuchia
Clade: Crocodylomorpha
Family: Saltoposuchidae
Genus: Galahadosuchus
Bodenham et al., 2026
Species:
G. jonesi
Binomial name
Galahadosuchus jonesi
Bodenham et al., 2026

Galahadosuchus is an extinct genus of saltoposuchid crocodylomorph from the Late Triassic fissure deposits of Cromhall Quarry in the United Kingdom. It is known from a partial postcranial skeleton including most of the hindlimbs, an almost complete forelimb and a series of tail vertebrae. Based on these remains Galahadosuchus was a gracile animal with long, slender limbs. Like many other early crocodylomorphs it is considered to have been a terrestrial quadruped, showing evidence of an erect, digitigrade stance and adaptations towards a cursorial lifestyle. Though very similar to the related Terrestrisuchus, some subtle anatomical differences might suggest that the two taxa differed slightly in their locomotion, with Galahadosuchus possibly having been a faster animal with more flexible hands. Only a single species has been described, Galahadosuchus jonesi.

Skeletal reconstruction and size comparison, showcasing the known elements of the holotype

The holotype specimen of Galahadosuchus, NHMUK PV R 10002, was recovered by Ron Croucher in 1969 from site 1 of the fissure deposits at Cromhall Quarry in Gloucestershire, southwest England. The specimen is preserved across two slabs and consists of a partially articulated postcranial skeleton including parts of the tail and hindlimbs, a nearly complete right forelimb, several isolated elements such as osteoderms, ribs and non-caudal vertebrae as well as the remains of a rhynchocephalian reptile. The Cromhall Quarry, also known as Slickstones Quarry, is one of several Late Triassic to Early Jurassic fissure fill deposits in the Bristol Channel area that have previously yielded crocodylomorph remains including those of the saltoposuchid Terrestrisuchus (from the Pant-y-Ffynnon Quarry). Many of these remains have at times either been compared to Terrestrisuchus or assigned to the genus wholesale, though later revisions showed them to frequently be too fragmentary for such specific referrals.[1] In one such case, then not mentioned by their inventory number, the specimen NHMUK PV R 10002 and some other disarticulated remains from other sites (numbered 1-5 and 7) in the Cromhall Quarry were referred to Terrestrisuchus by Fraser and colleagues in 2002,[2] who regarded them to represent two different morphs of the genus, both of which were deemed different from the type material from Pant-y-Ffynnon.[1]

While Fraser and colleagues did not describe the material nor provide a concrete reasoning for their assignments and distinctions,[2] a brief description of the material was published by R. C. Allen in a PhD thesis in 2010 partially agreeing with their assertion. In this thesis Allen argued that while NHMUK PV R 10002 was referrable to Terrestrisuchus gracilis, the remains from the other Cromhall Quarry sites held at the Virginia Museum of Natural History were not.[3] In 2023 and 2024, Spiekman and colleagues held that contrary to the works of Fraser et al. (2002) and Allen (2010), NHMUK PV R 10002 was not assignable to Terrestrisuchus, though the team deamed a full redescription to be beyond the scope of their work.[4][5]

The name Galahadosuchus derives from Sir Galahad of Arthurian legend and is a play on words. As explained by Bodenham and colleagues, Galahad is renowned for being upright in a moral sense in the myth, while Galahadosuchus is also upright, albeit in relation to its posture. The ending of the genus name "suchus" is derived from the Greek word for crocodile as frequently used in the scientific names of fossil pseudosuchians. The species name "jonesi" was chosen in honor of David Rhys Jones, a teacher at the Ysgol Uwchradd Aberteifi school in Wales, who was an inspirational figure to lead author Ewan H. Bodenham, supporting student′s pursuit of science.[1]

Description

Live reconstruction of Galahadosuchus jonesi.

Galahadosuchus was a digitigrade quadrupedal crocodylomorph with long and slender limbs. Among the distinguishing features of this genus are the relatively short and stout ulnare and radiale, the proximal carpal bones, who′s with exceeds a quarter of their maximum length. Typically, the proximal carpal bones of early crocodylomorphs are described as long and slender, one other exception being Trialestes, although in this form only the radiale is described as shortened. Each bone is at most only a tenth the length of their respective limb bone pairing in the forearm, i.e. radius plus humerus for the radiale and ulna plus humerus for the ulnare. Here the ratio is again comparable to what is seen in Trialestes and even Terrestrisuchus, albeit only applying to the ulnare. Like in Trialestes the radiale is also marked by a deep concavity located at the posterior end of the bone but stretching across the entirety of the shaft.[1]

As in most other early crocodylomorphs the back of Galahadosuchus was covered by what a double-row of paramedian osteoderms. The individual bony plates are elongated, 2.5 times longer than wide and therefore more elongated than in Saltoposuchus and Hesperosuchus (among others) but not as much as in Terrestrisuchus. However this information is limited to only a select few osteoderms and most of the armor of Galahadosuchus is unknown, which is significant since osteoderm proportions may vary in accordance with their position along the spinal collumn. Their shape is described as "leaf-shaped" or subrectangular, featuring a straight medial edge where each osteoderm meets its partner and a curved outer edge that flows into a spike-like process towards the front. The surface is ornamented by a pattern of shallow pits that surround a long keel that runs down the osteoderms midline. The sculpting is similar to Terrestrisuchus but markedly less developed than in other early crocodylomorphs. The underside of the osteoderms bears a groove stretching about a quarter of the length measured from the posterior end. This groove shows how the osteoderms articulated with each other, as the dorsal keel of the subsequent osteoderm slides into it to allow for an arrangement where each plate overlays the one behind it.[1]

Phylogeny

Paleobiology

References

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