Devils on the Darling Downs - the Tooth Mark Record

Volume: 28Start Page: 299End Page: 32

A ziphodont crocodile from the late Pleistocene King Creek catchment, Darling Downs, Queensland

Volume: 56Start Page: 601End Page: 60

Morphological variation within an individual Pleistocene Diprotodon optatum Owen, 1838 (Diprotodontinae; Marsupialia): Implications for taxonomy within diprotodontoids

A comprehensive understanding of morphological and morphometrical variation for systematically important characters is a prerequisite for reliable taxonomic analyses of extinct morphospecies. However, perception of such variation is commonly limited due to a paucity of fossil material that forms the basis of such analyses. Here we report a new record of Pleistocene Diprotodon optatum Owen, 1838 (Diprotodontoidea) represented by near-complete upper tooth rows that exhibit a high degree of individual variation within systematically important upper premolars. The individual possesses features (e.g. development of parastyle, anterocristae and anterior longitudinal groove) that are considered to be close to the polar extremes of premolar variation within the morphospecies, but occurring on either side of the palate. Although such morphologies were previously recognized on the basis of isolated specimens, they have never been observed as having occurred on either side of the tooth row within a single indvidual. The observation of such extreme variation in premolar form within a single individual means that although the diprotodontoid P3 may serve some systematic importance in distinguishing certain taxa, the weight placed upon perceived differences within any single character of the premolar must be gauged by an understanding of broader variation within the group

The diversity of Australian Mesozoic bennettitopsid reproductive organs

Several dispersed reproductive organs of bennettitopsid gymnosperms are described and illustrated from Triassic to Cretaceous strata of Australia: Williamsonia eskensis sp. nov. (Middle Triassic), Williamsonia ipsvicensis sp. nov. (Upper Triassic), Williamsonia durikaiensis sp. nov. (Lower Jurassic), Williamsonia sp. (Lower Jurassic), Williamsonia rugosa sp. nov. (Middle Jurassic), Williamsonia gracilis sp. nov. (Lower Cretaceous), Cycadolepis ferrugineus sp. nov. (Lower Jurassic), Cycadolepis sp. (Lower Cretaceous), and Fredlindia moretonensis Shirley 1898 comb. nov. (Upper Triassic). Among these, W. eskensis appears to represent the oldest bennettitalean reproductive structure yet identified. Although global floras expressed less provincialism during the Mesozoic and many genera are cosmopolitan, Australian bennettopsid species appear to have been endemic based on the morphological characters of the reproductive structures. Bennettopsids have a stratigraphic range of around 210 million years in Australia and are widely and abundantly represented by leaf fossils, but only around 20 specimens of reproductive structures, of which half are attributed to Fredlindia, have been recovered from that continent’s geological archive. The extremely low representation of reproductive organs vis-à-vis foliage is interpreted to reflect a combination of physical disintegration of the seed-bearing units while attached to the host axis and, potentially, extensive vegetative reproduction in bennettopsids growing at high southern latitudes during the Mesozoic.Other funding from:National Science Foundation (project #1636625)German Research Council (DFG KR2125/3)Friends of the Swedish Museum of Natural History (Riksmusei Vänner, Stockholm)SYNTHESYS (AT-TAF 467)</p