II. On the affinities of thylacoleo

1883 ◽  
Vol 35 (224-226) ◽  
pp. 19-19

Since the communication of the paper “On Thylacoleo,” in the “Philosophical Transactions” for 1871, further explorations of the caves and breccia-fissures in Wellington Valley, New South Wales, have been made, by a grant for that purpose from the Legislature of the Colony, and carried out by E. B. Ramsay, Esq., F. L. S., Curator of the Museum of Natural History, Sydney. The present paper treats of the fossils contributing to the further restoration of the great carnivorous Marsupial ( Thylacoleo carnifex , Ow.). They exemplify the entire dentition in situ of the upper and lower jaws of a nature individual: the bones of the fore-limb, of which those of the antibrachium and the ungual phalanges are described, are compared with those of other Marsupials, and of placental, especially feline, Carnivora . An entire lower jaw with the articular condyles adds to the grounds for determination of the habits and affinities of the extinct Marsupial. Figures of these fossils of the natural size accompany the paper.

1872 ◽  
Vol 20 (130-138) ◽  
pp. 66-67

In this paper the author premises a reference to former ones on the Osteology of existing Marsupialia , in the * Transactions of the Zoological Society,’ and to his 'Catalogue of the Osteological Series in the Museum of the Royal College of Surgeons,’ in which are defined cranial characters serving to distinguish existing species of the genus , Geoffr.; and after showing, in subsequently received materials, the kind and extent of variety of such characters in the same species, he proceeds to apply the knowledge so gained to the determination of some fossil remains of species of Wombat, similar in size to the known existing kinds. The extinct Phascolomys Mitchelli , indicated by remains brought to England in 1835 by Sir Thomas Mitchell, C.B., the discoverer of the bone-caves of Wellington Valley, Australia, is determined by specimens subsequently obtained by Prof. Alex. M. Thomson and Gerard Krefft, Esq., from the same caves. A second species, distinguished by characters of the nasal bones, is called, after its discoverer, Phascolomys Krefftii . Modifications of the lacrymal, maxillary, and palatal bones in the existing kinds of Wombat are also applied to the determination of the fossils: specimens from the freshwater deposits of Queensland are thus shown to belong to the species, Phascolomys Mitchelli , originally founded on fossils from the breccia-caves of New South Wales. The author next proceeds to point out the characters of the mandible in existing Wombats available in the determination of extinct species of Phascolomys . On this basis he defines specimens which he provisionally refers to his Phascolomys Krefftii . He then points out the mandibular characters of Phascolomys Mitchelli , and shows that the existing Phascolomys latifrons was represented by mandibular fossils from the breccia-caves of Wellington Valley. Proceeding next to the description of fossil mandibular remains of the genus Phascolomys , from the freshwater deposits of Queensland, the author defines Phascolomys Thomsoni , Phase platyrhinus , and Phase, parvus . The latter, seemingly extinct, species is markedly inferior in size to any of the known existing species. An account of the extinct kinds of Wombat, exceeding in size the existing species, will be the subject of a succeeding communication. The present is illustrated by subjects occupying seven plates and eight woodcuts, all the figures being from nature and of the natural size.


1884 ◽  
Vol 175 ◽  
pp. 245-248 ◽  

The only known Mammals of Australia with rootless, ever-growing scalpriform incisors, in bodily size suitable for wielding those about to be described, are the Diprotodon , the Notherium , and the Phascolonus , all of which have become extinct. But the incisors of the known species of the above genera differ in shape from each other and, in a still more marked degree, from those of Sceparnodon ; nor do any such teeth from other and smaller Mammals match with the present Fossils. My first cognizance of this form of tooth was derived from casts, which were kindly transmitted to me in October, 1881, by Edward P. Ramsay, Esq., Curator of the Museum of Natural History, Sydney, New South Wales.


1956 ◽  
Vol 4 (2) ◽  
pp. 165 ◽  
Author(s):  
JW Evans

New species of Triassic Homoptera and Heteroptera from the Brookvale series of New South Wales and Mt. Crosby, Queensland, are described, one homopteron from the Upper Permian of Warner's Bay, N.S.W., and Homoptera previously recorded from Palaeozoic and Mesozoic strata in Australia and elsewhere are reviewed. New illustrations, made from type specimens, are given for some Australian species. Representatives of the family Scytinopteridae, previously known only from Permian strata, are recorded from the Triassic. Two forewings of uncertain affinities, but having venational features similar to hylicids, are ascribed to species in genera placed in a new family, the Hylicellidae. For leaf-hoppers which are regarded as transitional between the Palaeozoic and Mesozoic faunas, a new family, the Stenoviciidae, is proposed, and another new family, the Chiliocyclidae, is proposed for a group of Mesozoic leaf-hoppers of wide distribution. A forewing from the Triassic of Queensland is identified as that of a eurymelid and another as a cicadellid. The earliest undoubted cercopid, so far recorded, is described from the Triassic; a new family, the Eoscarterellidae, is defined to comprise insects of probable cercopoid affinities, and the family Dysmorphoptilidae is transferred to the Cercopoidea. As the genus Palaeontina Butler is considered not to be a homopteron, a new family name, the Cicadomorphidae, is proposed for large Homoptera with cicada-like wings, previously recorded only from the Jurassic of Europe and which formerly have been included in the family Palaeontinidae. A new genus and species belonging to the Cicadomorphidae is described from the Triassic of New South Wales. The relationships of a new family, the Cicadoprosbolidae, and of the Mesogereonidae are discussed and both are considered to be allied to the Cicadidae. Two new psylloids are described and also an aphid, the latter being the first representative of the Aphidoidea to be recorded from Triassic strata. No new fulgoroids are described but problems associated with the determination of fulgoroid venation are discussed. The genus Actinoscytim Tillyard is transferred from the Homoptera to the Heteroptera and together with three new genera ascribed to a new family, the Actinoscytinidae. The family Ipsviciidae, formerly regarded as belonging to the Homoptera is also removed to the Heteroptera. The family Dunstaniidae is reviewed in the light of a re-examination of type specimens. Fossil fragments, poorly-preserved specimens, and wings of uncertain position which have at some time been referred to the Homoptera, are listed, and some are discussed. Possible derivations and interrelationships of the various major groups of Homoptera are indicated by means of a chart.


1886 ◽  
Vol 40 (242-245) ◽  
pp. 315-316 ◽  

In a scientific survey by the Department of Mines, New South Wales, of Lord Howe’s Island, fossil remains were obtained which were transmitted to the British Museum of Natural History, and were confided to the author for determination and description. These fossils, referable to the extinct family of horned Saurians described in former volumes of the “Philosophical Transactions" under the generic name Megalania , form the subject of the present paper. They represent species smaller in size than Megalania prisca , Ow., and with other differential characters on which an allied genus Meiolania is founded.


1883 ◽  
Vol 174 ◽  
pp. 639-643 ◽  

Since the communication of the 1st February, 1883, “On the Affinities of Thylacoleo,” I have received, through the favour of the Trustees of the Museum of Natural History, Sydney, and the care of the accomplished keeper, E. P Ramsay, Esq., F. L. S., a second consignment of the palaeontological results of his exploration of the Breccia Caverns of Wellington Valley, New South Wales. Besides additional confirmation of the dental, mandibular, antibrachial, ungual, and other osteal characters of Thylacoleo , these accessory specimens afford further evidence of the carnivorous modifications of parts of the skeleton. Of these a well-marked one is yielded by the pelvis (Plate 46, fig. 1).


1937 ◽  
Vol 74 (4) ◽  
pp. 145-153 ◽  
Author(s):  
Dorothy Hill

In this paper is given a revision of all but one of the corals in the Rev. W. B. Clarke's first collection of fossils from New South Wales; the collection was placed by him in the Woodwardian Museum at Cambridge in 1844, and was described by M'Coy (1847). The types are still preserved at the Sedgwick Museum, Cambridge. A description is also given of the holotype of Amplexus arundinaceus Lonsdale, which was collected from New South Wales by Strzelecki in 1842, and is now in the British Museum (Natural History), London. The species are distributed as follows: 1? Permian, 1 Lower Carboniferous, 1 Devonian, and 1 Silurian or Lower Devonian.


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