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Pulanesaura
''Pulanesaura'' is an extinct genus of basal sauropod known from the Early Jurassic (late Hettangian to Sinemurian) Upper Elliot Formation of the Free State, South Africa. It contains a single species, ''Pulanesaura eocollum'', known from partial remains of at least two subadult to adult individuals.
==Discovery and naming==
The remains of ''Pulanesaura'' were discovered in a small quarry in the farm Spion Kop 932 in the Senekal District of the Free State in 2004 by paleontologist Matthew Bonnan. The bones were excavated between 2004 and 2006, and studied by Blair McPhee as part of his dissertation since 2011. ''Pulanesaura'' was then described and named officially by Blair W. McPhee, Matthew F. Bonnan, Adam M. Yates, Johann Neveling and Jonah N. Choiniere in 2015 with the type species ''Pulanesaura eocollum''. The generic name is derived from the Sesoth word for "rain-maker/bringer", ''Pulane'', in reference to the heavy rain conditions under which the remains were collected, and the feminine form of the common dinosaur name suffix, ''saura'', meaning "lizard" in Latin. The specific name is derived from Greek ''eo'', meaning "dawn", and Latin ''collum'', meaning "neck", in reference to ''Pulanesaura'' being a very basal sauropod not yet showing the most archetypal trait of more advanced sauropods - their very long necks.〔
''Pulanesaura'' is known from partial remains of at least two subadult to adult individuals. The holotype, BP/1/6882, represents the front dorsal vertebra missing the tip of the neural spine. In addition the referred material consists of two isolated teeth, a middle cervical vertebra, five back vertebral arches, a single right dorsal rib, three tail vertebrae, a left clavicle, a distal right humerus, a left ulna, possibly the fourth right middle hand bone, three ischia, a left and a right shinbones, and two hindlimb first claws. The remains are considered to be conspecific with the holotype due to their close association (in an area of three to three and a half meters) in fine and stable sandstone, their consistent morphology, and the fact the same elements from different individuals show no conflict in traits. The remains were collected on the farm Spion Kop 932, in a quarry located just over a kilometer East-North East another dinosaur rich quarry in a higher stratigraphic position within the probably Sinemurian part of the upper Elliot Formation, that yielded the less advanced sauropodomorphs ''Aardonyx celestae'' and the much smaller ''Arcusaurus pereirabdalorum''.〔
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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