Aaron Camens

• BSc Hons, PHD
• Lecturer at Flinders University

Species of the kangaroo genus Protemnodon were common members of late Cenozoic communities across Australia and New Guinea until their extinction in the late Pleistocene. However, since the genus was first raised 150 years ago, it has proven difficult to diagnose, as have the species allocated to it. This is due primarily to the incompleteness of t...

Diprotodontians are the morphologically and ecologically most diverse order of marsupials. However, an approximately 30-million-year gap in the Australian terrestrial vertebrate fossil record means that the first half of diprotodontian evolution is unknown. Fossil taxa from immediately either side of this gap are therefore critical for reconstructi...

Diprotodontids were the largest marsupials to exist and an integral part of Australian terrestrial ecosystems until the last members of the group became extinct approximately 40 000 years ago. Despite the frequency with which diprotodontid remains are encountered, key aspects of their morphology, systematics, ecology and evolutionary history remain...

The late Oligocene taxa Marada arcanum and Mukupirna nambensis (Diprotodontia, Vombatiformes) are the only known representatives of the families Maradidae and Mukupirnidae, respectively. Mukupirna nambensis was described from a partial skeleton, including a cranium but no dentary, and reconstructed as the sister taxon to Vombatidae (wombats). By co...

The giant accipitrid Dynatoaetus gaffae gen. et sp. nov. is described from existing and newly collected material. Initial fossil remains were collected from Mairs Cave (Flinders Ranges, South Australia) in 1956 and 1969, and comprised a sternum, distal humerus and two ungual phalanges. A further 28 bones from this individual—including the neurocran...

The Ektopodontidae are an enigmatic group of phalangeroid marsupials known from the late Oligocene to the Early Pleistocene of Australia. Although represented to date only by isolated teeth and several partial dentaries and maxillae, their highly distinctive dental morphology has allowed three genera and nine species to be distinguished. Here, we d...

Vertebrate fossils showing pathological lesions are incredibly rare, and even more so is the identification of an ailment affecting multiple individuals in a population. However, the unique Lake Callabonna fossil deposit of South Australia has produced several such fossils from a single species of giant bird. Examination of the Lake Callabonna foss...

The Australian pre-Pleistocene fossil record of Accipitridae (eagles, hawks, old-world vultures) comprises one latest Oligocene or early Miocene and one middle Miocene species, each represented by partial bones. Globally, most fossil accipitrids are based on single bones. The recent discovery of an older and considerably more complete accipitrid fr...

The diverse living Australian lizard fauna contrasts greatly with their limited Oligo-Miocene fossil record. New Oligo-Miocene fossil vertebrates from the Namba Formation (south of Lake Frome, South Australia) were uncovered from multiple expeditions from 2007 to 2018. Abundant disarticulated material of small vertebrates was concentrated in shallo...

The tetrapod trace fossil record of Australia has, until recently, been poorly studied relative to records on other continents. In the last few decades, a series of studies have revealed that these traces are more common than was previously thought. They have provided fossil evidence of taxa for which no skeletal fossils are known and have been fou...

The extinct marsupial ‘lion’ Thylacoleo carnifex was Australia’s largest mammalian carnivore. Despite being the topic of more discussion than any other extinct Australian marsupial (excepting perhaps the Thylacine), basic aspects of its palaeobiology, including its locomotory repertoire, remain poorly understood. Recent discoveries allowed the firs...

Raw data related to all species studied in this manuscript. (XLSX)

The estimated period in which human colonization of Madagascar began has expanded recently to 5000–1000 y B.P., six times its range in 1990, prompting revised thinking about early migration sources, routes, maritime capability and environmental changes. Cited evidence of colonization age includes anthropogenic palaeoecological data 2500–2000 y B.P....

Research on sources of Madagascan IHCE estimates. (PDF)

Previous assessments of thermally transferred optically stimulated luminescence (TT-OSL) signal resetting in natural sedimentary settings have been based on relatively limited numbers of observations, and have been conducted primarily at the multi-grain scale of equivalent dose (De) analysis. In this study, we undertake a series of single-grain TT-...

It is rapidly becoming apparent that the Late Pleistocene vertebrate trace fossil record of southern Australia is much more comprehensive than previously understood, and complements the skeletal fossil record with regard to the distribution of taxa in coastal environments and the palaeobiology of both extinct and extant organisms. We surveyed the m...

The remarkable fauna of Australia evolved in isolation from other landmasses for millions of years, yet understanding the evolutionary history of endemic avian lineages on the continent is confounded by the ability of birds to disperse over geographical barriers even after vicariance events. The Plains-wanderer Pedionomus torquatus (Charadriiformes...

Understanding the evolution of Australia’s extinct marsupial megafauna has been hindered by a relatively incomplete fossil record and convergent or highly specialized morphology, which confound phylogenetic analyses. Further, the harsh Australian climate and early date of most megafaunal extinctions (39-52 ka) means that the vast majority of fossil...

The co-occurrence of vertebrate trace and body fossils within a single geological formation is rare and the probability of these parallel records being contemporaneous (i.e. on or near the same bedding plane) is extremely low. We report here a late Pleistocene locality from the Victorian Volcanic Plains in south-eastern Australia in which demonstra...

List of late Pleistocene vertebrate taxa recorded by various authors for south-eastern Australia. (DOCX)

Faunal list for the VVP skeletal deposits. A list of all identified taxa represented in the skeletal fossil deposits at the Victorian Volcanic Plains site. (DOCX)

List of the specimens catalogued from the VVP site (now housed in the MV collection). (XLSX)

The marsupial family Diprotodontidae (Diprotodontia, Vombatiformes) is a group of extinct large-bodied (60-2500 kg) wombat-like herbivores that were common and geographically widespread in Cenozoic fossil deposits of Australia and New Guinea. Typically they are regarded to be gregarious, terrestrial quadrupeds and have been likened in body form amo...

Nimbadon body weight estimates. (DOCX)

Description and comparison of Nimbadon lavarackorum appendicular skeleton. (DOCX)

Comparison of forelimb and hindlimb proportions of Nimbadon to a range of extant and extinct marsupials. All measurements (means in mm) taken from Finch and Freedman (1988, table 1) except those of Nimbadon. (DOCX)

Plot of forelimb vs hindlimb indices for Nimbadon and a range of marsupial taxa. (data from Table S1). (DOCX)

A diverse assemblage of late Pleistocene marsupial trackways on a lake bed in south-western Victoriaprovides the first information relating to the gaits and morphology of several megafaunal species, andrepresents the most speciose and best preserved megafaunal footprint site in Australia. The 60e110 kavolcaniclastic lacustrine sedimentary rocks pre...

The recent study of monotreme paleobiology and phylogeny by Phillips et al. (1) emphasized that the crown group Monotremata may have diverged relatively recently. However, they failed to discuss several aspects of the monotreme fossil record and functional morphology that may have a significant bearing on their conclusions.

The first Pliocene marsupial fossil trackways from Australia are described. The trackways, attributed to Euowenia grata (De Vis) (Diprotodontoidea, Marsupialia), occur in the middle Pliocene Tirari Formation, Warburton River, northern South Australia. The trackways were formed as the animals made their way across a soft claypan. Pad impressions, su...

The emerging molecular evolutionary tree for placental mammals differs greatly from morphological trees, leading to repeated suggestions that morphology is uninformative at this level. This view is here refuted empirically, using an extensive morphological and molecular dataset totalling 17 431 characters. When analysed alone, morphology indeed is...

Recovery of a specimen of Euowenia grata (De Vis, 1887) from mid Pliocene sediments of the Tirari Formation on the bank of the Warburton River in the Lake Eyre Basin provides the first recorded account of this species in South Australia. The specimen comprises a partial skull including left and right premaxillae, maxillae, and left zygomatic arch,...