Thesis (Ph.D.)--University of Western Australia, 2007.

Life history exist as a set of co-adapted traits designed to solve ecological problems, and theory predicts that in unpredictable environments, these are geared towards relatively slow growth and a long reproductive lifespan with relatively few offspring per reproductive event. However, recently the response of anurans to such conditions has been controversial and little empirical data are published on the response of Australian anurans living under such conditions. Limnodynastes Tasmaniensis is a medium sized endemic frog of the family Myobatrachidae that has an extensive range that encompasses every Australian state. Limited published data indicates that intra-population variation in reproductive parameters exist in this species and therefore it is an ideal model to test life history theory under Australian conditions. A population of the species was studied within remnant woodlands of North West Sydney, Australia. Many observations were made and the results shown in some detail. The data found does not completely conform with current theory developed largely for data collected in the northern hemisphere and highlights the need for further research into life history strategies of Australian anurans. / Doctor of Philosphy (PhD)

Thesis (PhD.) -- University of Western Sydney, 2002. / "A thesis submitted in fulfilment of the requirements for the degree of Doctor of Philosophy at the University of Western Sydney, Centre for Integrated Catchment Management". References : leaves 133 - 162.

Thesis (Ph.D.)--University of Melbourne, Dept. of Zoology, 2004. / Typescript (photocopy). Includes bibliographical references (leaves 261-298).

The phylogenetic relationships of Pseudophryne and the closely related monotypic Metacrinia are resolved with the use of morphological characters and comparison with representatives species of Crinia, Uperoleia, and Taudactylus as defined out-groups. Characters describing musculature are not sufficient to resolve the relationships, but do provide support when used in combination with osteological and external characteristics. When all data are considered, parsimony and maximum likelihood analyses yield the same hypothesis of relationships within Pseudophryne + Metacrinia. Thus, a monophyletic lineage of Pseudophryne + Metacrinia is supported by four synapomorphies: (1) the absence of toe fringes, (2) wide frontoparietal fontanelle, (3) m. abductor indicis longus arising from the humerus and radioulna, and (4) neopalatine in contact with the maxilla. The columella is shown as a relatively plastic characteristic, present ancestrally but lost in the common ancestor to Pseudophrye+Metacrinia and then reappearing within that taxon as well as one outgroup species (Crinia riparia). Analyses of size data reveal shape trends among the outgroup taxa that differ from the in-group of Pseudophryne and Metacrinia. Interpretations of shape differences are congruent with the placement of Uperoleia as more closely related to Pseudophrye. This study suggests support for re-synonymy of Metacrinia nichollsi with Pseudophryne, but formal change of status depends on access to more complete data.

[Truncated abstract] Southwestern Australia is a global biodiversity hotspot. The region contains a high number of endemic species, ranging from Gondwanan relicts to more recently evolved plant and animal species. Biogeographic models developed primarily for plants suggest a prominent role of Quaternary climatic fluctuations in the rampant speciation of endemic plants. Those models were not based on explicit spatial analysis of genetic structure, did not estimate divergence dates and may be a poor predictor of patterns in endemic vertebrates. Myobatrachid frogs have featured heavily in the limited investigations of the biogeography of the regions fauna. Myobatrachid frogs are diverse in southwestern Australia, and while we know they have speciated in situ, we know little about the temporal and spatial patterning of speciation events. In order to gain insight into the biogeographic history and potential speciation patterns of Myobatrachid frogs in the southwest I conducted a comparative phylogeography of four frog species spanning three life history strategies. I aimed to: 1) assess the biogeographic history of individual species, 2) determine where patterns of regional diversity exist using a comparative framework, 3) determine whether congruent patterns across species enable the development of explicit biogeographic hypotheses for frogs, and 4) compare patterns of diversity in plants with the models I developed for frogs. I conducted fine-scale intraspecific phylogeographies on four species. ... Geocrinia leai: deep divergences, coincident with late Miocene arid onset, divide this species into western and southeast coastal lineages, with a third only found within the Shannon-Gardner River catchments. Phylogeographic history within each lineage has been shaped by climatic fluctuations from the Pliocene through to the present. Arenophryne shows the first evidence of geological activity in speciation of a Shark Bay endemic. Divergence patterns between the High Rainfall and Southeast Coastal Provinces within C. georgiana are consistent with patterns between Litoria moorei and L. cyclorhynchus and plant biogeographic regions. Subdivision between drainage systems along the southern coast (in M. nichollsi, G. leai and the G. rosea species complex) reflect the relative importance of distinct catchments as refuges during arid maxima, similarly the northern Darling Escarpment is identified as a potential refugium (C. georgiana and G. leai). Divergences in Myobatrachid frogs are far older than those inferred for plants with the late Miocene apparently an important time for speciation of southwestern frogs. Speciation of Myobatrachids broadly relates to the onset of aridity in Australia in the late Miocene, with the exception of earlier/contemporaneous geological activity in Arenophryne. The origins of subsequent intraspecific phylogeographic structure are coincident with subsequent climatic fluctuations and correlated landscape evolution. Divergence within frogs in the forest system may be far older than the Pleistocene models developed for plants because of the heavy reliance on wet systems by relictual frog species persisting in the southwestern corner of Australia.