Its wide geographic range make it the one of the only Turonianmosasaurs with a transatlantic range.[8]
Description
Angolasaurus was a small mosasaur, with a skull length estimated at 40 centimetres (1.3 ft),[12] suggesting a possible total length of about 4 meters (13 feet) based on the ratio provided by Russell (1967).[13] It shared much of a body plan with its relative Platecarpus, but with a slightly longer skull relative to body length.[6] Its skull housed 11 maxillary teeth, 4 premaxillary teeth, and 12 dentary teeth. The phylogenetic relationship of Angolasaurus indicates that individuals of this genus possessed a tail fluke, more forward-lying nostrils,[14] and keeled scales for hydrodynamic efficiency.[15]
Due to declining sea temperatures in the area that Angolasaurus inhabited, as well as the later Bientiaba locality, it has been hypothesized that it and the other mosasaurs inhabiting its region may have had an increased coverage of dark patterning on its dorsal surface to aid in thermoregulation.[16]
History of discovery
First named in 1964 by Miguel Telles Antunes on the basis of a partial skull and skeleton, Angolasaurus was reassigned in 1994 to the genus Platecarpus.[6] This placement was subsequently struck down in studies in 2005, which nested it within the plioplatecarpinae.[7] Fieldwork between 2005 and 2009 recovered at least two new Angolasaurus skeletons. One new skull as well as the type skull were CT scanned to reveal intricate details of the interior braincase that allowed for a more concrete placement within the plioplatecarpinae.[8] The most recent major phylogenetic analysis conducted on the mosasauridae placed Angolasaurus as basal to the clade composed of the russellosaurine subfamilies Tylosaurinae and Plioplatecarpinae, and part of neither.[17]
In 2007, two individuals from the Eagle Ford Formation of Texas were described as belonging to the genus Angolasaurus, one of which preserved part of the hyoid apparatus. The same abstract assigned two teeth previously assigned to Platecarpus to Angolasaurus. These teeth came from the Sergipe Basin of Brazil, and are virtually indistinguishable from those found in the holotype of Angolasaurus bocagei. These discoveries made Angolasaurus the first known Turonianmosasaur genus with a transatlantic distribution.[8]
Paleoecology
Angola
Angolasaurusbocagei, recovered only from the Itombe Formation, shared its habitat with the tylosaurine species Tylosaurus (formerly Mosasaurus) iembeensis and the durophagous shallow-water turtleAngolachelys. Indeterminate halisaurine and plesiosaur remains have also been recovered from this region. Terrestrial fauna consisted solely of the sauropod Angolatitan.[18]
^ abcdLingham-Soliar, T. (1994). "The mosasaur "Angolasaurus" bocagei (Reptilia: Mosasauridae) from the Turonian of Angola re-interpreted as the earliest member of the genus Platecarpus". Paläontologische Zeitschrift. 68 (1–2). doi:10.1007/bf02989445. S2CID128963124.
^ abcdPolcyn, M.; Lindgren, J.; Bell, G.L. Jr. (2007). "The possible occurrence of Angolasaurus in the Turonian of North and South America". In Everhart, M.J. (ed.). Abstract Booklet of the Second Mosasaur Meeting(PDF). Hays, Kansas. p. 21.{{cite book}}: CS1 maint: location missing publisher (link)
^Lingham-Soliar, Theagarten (1991). "Mosasaurs from the upper Cretaceous of Niger". Palaeontology. 34: 653–670.
^Moody, R. T. J and Suttcliffe, P. T. C. (1991). The Cretaceous deposits of the Iullemmeden Basin of Niger, central West Africa. Cretaceous Research 12:137-157
^Konishi, Takuya; Caldwell, Michaell (2011). "Two new plioplatecarpine (Squamata, Mosasauridae) genera from the Upper Cretaceous of North America, and a global phylogenetic analysis of plioplatecarpines". Journal of Vertebrate Paleontology. 31 (4): 754–783. Bibcode:2011JVPal..31..754K. doi:10.1080/02724634.2011.579023. S2CID85972311.
^Bardet, Nathalie (2008). "The Cenomanian-Turonian (late Cretaceous) radiation of marine squamates (Reptilia): the role of the Mediterranean Tethys". Bulletin de la Société Géologique de France. 179 (6): 605–623. doi:10.2113/gssgfbull.179.6.605.