|
''Plesiosuchus'' is an extinct genus of geosaurine metriorhynchid crocodyliform known from the Late Jurassic (late Kimmeridgian to early Tithonian stage) of Dorset, England and possibly also Spain. It contains a single species, ''Plesiosuchus manselii''. ==Discovery== The type and referred specimens of ''Plesiosuchus'' were discovered by John Clavell Mansel-Pleydell in the 1860s alongside the remains of several other large-bodied marine reptiles along the coast of Dorset. Mansel-Pleydell gave these remains to the British Museum (now in the Natural History Museum) in 1866. Part of the holotype of ''P. manselii'' (NHMUK PV OR40103a) was first described by John Hulke in 1869. He referred it to ''Steneosaurus rostro-minor'' Geoffroy (1825), alongside ''Dakosaurus maximus'' and other specimens. Initially, the skull (NHMUK PV OR40103) was believed to be pliosaurian; it was the preparator Mr Davies that suggested a crocodylian nature for the skull. In 1870, Hulke described the skull, which is preserved in two sections: the rostrum and the occiput. Hulke suggested that "this head and the lower jaw both belonged to one individual" as both the same dimensions and were discovered in close proximity in a reef exposed at low water in Kimmeridge Bay. Some material was destroyed due to pyrite decay while the isolated bone fragment referred to as the "upper maxilla" has never been figured and cannot be located. Richard Owen erected the genus ''Plesiosuchus'' for ''S. manselii'' in 1884 as he considered it to be more similar morphologically to extant crocodylians than to ''Steneosaurus''. Woodward (1885) referred the species to the genus ''Dakosaurus''. Lydekker (1888) synonymized ''P. manselii'' with ''Dakosaurus maximus'' while Fraas (1902) regarded the two species to be synonymous or closely related. Phylogenetic analyses of Young & Andrade (2009), Cau & Fanti (2011) and Young ''et al.'' (2011) support the hypothesis that the two are separate species of ''Dakosaurus''. Young ''et al.'' (2012) resurrected the genus name ''Plesiosuchus'' as their phylogenetic analysis found a paraphyletic ''Dakosaurus'' and suggested more basal position for ''P. manselii'' within Geosaurini than previously thought.〔 The holotype of ''Plesiosuchus'' includes, NHMUK PV OR40103, a broken and incomplete skull with a mandible and isolated postcranial remains (NHMUK PV OR40103a). The incomplete skull includes the snout and the occiput, lacking the occipital condyle, with fragments of the supratemporal arches and isolated right articular. NHMUK PV OR40103a includes the right mandibular ramus, some isolated teeth, a humerus, and numerous ribs and vertebrae that are partially or completely imbedded in matrix. Two further specimens may belong to the holotype: NHMUK PV OR40104 - an occipital condyle, and NHMUK PV OR40105 – carpal and tarsal bones. Both specimens were donated to the University of Toronto through Professor Ramsay Wright in 1900. From examining the register in the NHMUK Earth Sciences Department, it is possible both specimens were part of NHMUK PV OR40103, althouth neither specimen could be located at the Royal Ontario Museum. The holotype of ''Plesiosuchus'' represents a large individual. Althouth it is uncertain whether the holotype (and referred specimens) belong to adults or subadults as none of the vertebrae are well enough preserved to determine the nature of the neurocentral sutures, its total body length is estimated to be . It was collected from the late Kimmeridgian (''Aulacostephanus autissiodorensis'' Sub-Boreal ammonite Zone) Lower Kimmeridge Clay Formation of Kimmeridge Bay, Dorset. The specimen NHMUK PV OR40103b, a short series of cervicodorsal vertebrae preserved in matrix, is also a thalattosuchian due to its possession of several apomorphies of the group. However, it does not belong to the same individual as the holotype as the vertebrae are much smaller than those of NHMUK PV OR40103a, and the matrix is of a different composition. It is unclear whether it belongs to ''Plesiosuchus'' or another metriorhynchid, and therefore it is considered to be Thalattosuchia indeterminate.〔 NHMUK PV R1089, a mandible and a braincase with part of the supratemporal arches collected from the early Tithonian (''Pectinatites wheatleyensis'' Sub-Boreal ammonite Zone) Upper Kimmeridge Clay Formation, of Kimmeridge is also referred to ''Plesiosuchus''. It was also presented by Mansel-Pleydell in 1866, and as with the holotype, was initially considered to belong to a pliosaurid plesiosaur. It was originally described by Owen (1869) as a referred specimen to the species ''Pliosaurus trochanterius''. However, Owen never provided evidence for this referral and there were no overlapping elements between NHMUK PV R1089 and the holotype of ''P. trochanterius'' (thought to be an isolated femur but is actually a humerus that was collected from the early Tithonian of Shotover Hill, Oxfordshire, England). Later, both Eudes-Deslongchamps (1867–1869) and Woodward (1885) referred it to the metriorhynchid genus ''Metriorhynchus'' while Tarlo (1960) considered it to be crocodylian, and Buffetaut (1982) considered it to be a large metriorhynchid closely related to ''Dakosaurus''. Although both Lydekker (1888) and Vignaud (1995) referred the specimen to the teleosaurid species ''Machimosaurus mosae'', Young ''et al.'' (2012) showed that its distinct from ''Machimosaurus'' that possess external mandibular fenestrae and an anterior transverse expansion of the mandibular symphysis, whereas NHMUK PV R1089 lacks both features. Furthermore, both species of ''Machimosaurus'' lack the prearticular, which is present in NHMUK PV R1089. Additionally, NHMUK PV R1089 exhibits extreme reduction in dentition (13 dentary alveoli compared to 19–25 in ''Machimosaurus'') that is otherwise observed in geosaurine metriorhynchids. As the holotype of ''P. manselii'' and NHMUK PV R1089 share a cranial apomorphy and can both be excluded from other closely related geosaurines, Young ''et al.'' (2012) referred it to ''P. manselii''. NHMUK PV R1089 represents even larger individual than the holotype with long mandible, while the mandible of NHMUK PV OR40103a is approximately in length. Thus NHMUK PV R1089 has been estimated to have been about in length. This body length falls within the size range of the top predator of the Oxford Clay Sea, the pliosaurid ''Liopleurodon ferox''.〔 Two further specimens in the Museum of Jurassic Marine Life are referable to ''Plesiosuchus manselii'': K181, isolated teeth, partial maxilla?, partial left mandible, ribs, vertebrae, femur; and K434, right dentary. The isolated Spanish tooth crown (MUJA-1004) described by Ruiz-Omeñaca ''et al.'' (2010) as ''Dakosaurus'' sp. was referred to cf. ''Plesiosuchus manselii'' by Young ''et al.'' (2012) as it shares the enamel ornamentation pattern, denticles size and lack of wear observed on the teeth with the holotype of ''Plesiosuchus'' and can be distinguished from any other known geosaurine. It was collected from the Kimmeridgian-aged Tereñes Formation in La Griega Beach of Asturias, northern Spain.〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Plesiosuchus」の詳細全文を読む スポンサード リンク
|