The Upper Triassic of India preserves a rich record of phytosaurs, encompassing both early- and later-diverging parasuchids. We report here a new leptosuchomorph phytosaur from the Maleri Formation of Pranhita-Godavari basin. The new taxon, represented by an incomplete cranium, is characterised by a tripartite upper jaw dentition, narial crest, naris-antorbital fenestra overlap, partially depressed parietal–squamosal bar, dorsoventrally high posterior process of squamosal, posteroventrally directed opisthotic process, subsidiary opisthotic process of the squamosal, a pair of fossae on the parietal that meet along a raised median wall, and a deep pit on the parietal–supraoccipital shelf. Phylogenetic analysis places the new taxon, Primisuchus gen. et sp. nov., among the later-diverging leptosuchomorphs, as sister taxon to Mystriosuchini. This discovery represents the first definitive record of a non-Mystriosuchini leptosuchomorph from Gondwana, defining the lower boundary of the Upper Maleri–Lower Dharmaram Assemblage Eubiozone at the base of the Adamanian holochron. Biogeographic considerations suggest a Middle Triassic origin of Phytosauria with early parasuchids becoming cosmopolitan during the late Carnian, coincident with the terminal phase of the Carnian Pluvial Event. A climate-induced faunal turnover straddling the Carnian–Norian boundary led to the disappearance of non-leptosuchomorphs. The early Norian saw endemic radiations followed by renewed intercontinental dispersal of leptosuchomorphs during the middle–late Norian.
No takes yet. Share an insight, caveat, or question.
Datta et al. (2026) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: