TL;DR: Waring et al. as discussed by the authors described a new Saurischian reptile which has its nearest known allies in the lower secondary rocks of Europe and the Trias of South Africa.
Abstract: In July 1879 the Geological Department of the British Museum obtained by purchase from Mr. E. Charlesworth some fossil bones, which were dispersed at the sale of the collection of Mr. S. L. Waring, F.G.S., of Norwood, then recently deceased. They are labelled, in a small, delicate handwriting, “‘Ply,’ 1844. Jn. Macgillivray, from the NE. coast of Australia.” I believe this to indicate that the specimens were collected by Mr. Macgillivray during the voyage of the ‘Fly,‘ from some locality which was then unnamed. The bones were placed in the Mammal Gallery, where they have since remained. They comprise a complete left tibia, a less perfect proximal end of the corresponding right tibia, a fragment which I regard as a portion of a fibula, attached to matrix, which besides other fragments of bone contains two laterally compressed claw-phalanges. There is necessarily no direct evidence of their geological age. But as they indicate a new Saurischian reptile, which has its nearest known allies in the lower Secondary rocks of Europe and the Trias of South Africa, it is not improbable that the animal belongs to the Lower Oolites or Trias. I have not noticed any reference to the specimens by Professor Jukes in the “ Voyage of the ‘Fly’” or in his other books and papers, or in the writings of Mr. Macgillivray. The left tibia (figs. 1, 2) is about 20 cm. in extreme lengthy with the usual sub-triangular flattened proximal articular surface. That surface is nearly 5 cm. deep
TL;DR: The only known specimen of the prosauropod Agrosaunls macgillivrayi Seeley, 1891 probably comes from the Late Triassic Durdham Down locality near Bristol, England as discussed by the authors.
Abstract: The holotype and only known specimen of the prosauropod Agrosaunls macgillivrayi Seeley, 1891 probably comes from the Late Triassic Durdham Down locality near Bristol, England. Originally it was reported as being from the northeast coast of Australia. Firsthand examination of the most plausible northeast Australian source for such a fossil, outcrops of the Jurassic Helby Beds exposed on the east coast of Cape York Peninsula, have demonstrated that the rock in that unit was quite unlike that associated with the holotype. Gross and trace element comparisons between possible fossil bone fragments from the Helby Beds and the holotype also showed them to be quite different. On the other hand, similar comparisons between the holotype and fossil bone from Durdham Down showed them to be quite comparable, as were the rocks and microvertebrates there and the ones associated with the holotype. Furthermore, A. macgillivrayi is probably a junior synonym of Tlzecodontosaurus antiquus Morris, 1843 from Durdham Down.