A Crassigyrinus-like jaw from the Tournaisian (Early Mississippian) of Scotland. (March 2017)

• Record Type: Journal Article
• Authors: Clack, Jennifer A.; Porro, Laura B.; Bennett, Carys E.
• Is Part Of: Earth and environmental science transactions of the Royal Society of Edinburgh. Volume 108:Number 1(2018)
• Page Start: 37
• Page End: 46
• Publication Date: 2017-03
• Subjects: Burnmouth, -- Borders region, -- Romer's Gap, -- tetrapod, -- TW:eed project; Earth sciences -- Periodicals; Earth sciences -- Scotland -- Periodicals; 550.5
• DOI: 10.1017/S1755691018000087
• Languages: English
• ISSNs: 1755-6910

Abstract

ABSTRACT: The early tetrapod Crassigyrinus scoticus was a large aquatic predator from the mid Carboniferous (late Viséan or early Serpukovian) of Scotland, around 330 My in age. There are five main specimens with cranial remains: an articulated skeleton; two incomplete skulls; and two lower jaws. Crassigyrinus retains several apparently primitive features of the palatal dentition and lower jaw, and its phylogenetic position is disputed. A partial lower jaw resembling that of Crassigyrinus was discovered at Burnmouth in the Borders region of Scotland. The horizon in which it was found is dated as late Tournaisian, CM palynozone, around 350 My in age. Though it lacks dentition, the jaw preserves much of the postsplenial, angular and surangular, whose appearance externally and internally is almost identical to that of C. scoticus . Internally, the jaw shows a similarly limited extent of the suturing between the splenial series and the prearticular, a primitive condition. Externally, the type and distribution of dermal ornamentation closely matches that of C. scoticus, as does the deeply excavated and marginally positioned lateral line groove. As well as external and internal features, all specimens of C. scoticus are of similar skull size, though the Burnmouth jaw is somewhat smaller. If correctly attributable to Crassigyrinus, this specimen extends the existence of the genus by approximately 20 million years towards the base of the Carboniferous.