This thesis began as an investigation into evolution of the platypus family (Ornithorhynchidae, Monotremata), now known from both Australia and South America. The thesis broadened its scope with inclusion of non-ornithorhynchid Mesozoic monotremes from Lightning Ridge, NSW. This change in direction brought an unexpected result: a fossil mammal from Lightning Ridge investigated for this thesis (presumed to be monotreme: Flannery et al., 1995) appears to be a new and unique type of mammal. Specimens were procured through Queensland Museum (Riversleigh material); Australian Museum (Lightning Ridge material); and Museum of Victoria and the South Australian Museum (fossil ornithorhynchids). Specimens were examined under a light microscope and scanning electron microscope; specimens were photographed using light photography and a scanning electron microscope; and illustrations and reconstructions were done with a camera lucida microscope attachment and photographic references. Parsimony analysis utilised the computer programs PAUP and MacClade. Major conclusions: 1) analysis and reconstruction of the skull of the Miocene platypus Obdurodon dicksoni suggest this robust, large-billed platypus was a derived northern offshoot off the main line of ornithorhynchid evolution; 2) the well-preserved skull of Obdurodon dicksoni shows aspects of soft anatomy previously unknown for fossil ornithorhynchids; 3) two upper molars from Mammalon Hill (Etadunna Formation, late Oligocene, central Australia) represent a third species of Obdurodon; 4) the South American ornithorhynchid Monotrematum sudamericanum from the Paleocene of Argentina is very close in form to the Oligocene-Miocene Obdurodon species from Australia and should be considered congeneric; 5) a revised diagnosis of the lower jaw of the Early Cretaceous monotreme Steropodon galmani includes the presence of two previously undescribed archaic features: the probable presence of postdentary bones and a meckelian groove; 6) morphological evidence is presented supporting a separate family Steropodontidae; and 7) analysis of new fossil material for Kollikodon ritchiei suggests that this taxon is not a monotreme mammal as originally identified but is a basal mammal with close relationships to allotherian mammals (Morganucodonta; Haramiyida). Kollikodon is provisionally placed as basal allotherian mammal (Allotheria sensu Butler 2000) and is unique at the ordinal level, being neither haramiyid nor multituberculate. A new allotherian order ??? Kollikodonta ??? is proposed.

This thesis began as an investigation into evolution of the platypus family (Ornithorhynchidae, Monotremata), now known from both Australia and South America. The thesis broadened its scope with inclusion of non-ornithorhynchid Mesozoic monotremes from Lightning Ridge, NSW. This change in direction brought an unexpected result: a fossil mammal from Lightning Ridge investigated for this thesis (presumed to be monotreme: Flannery et al., 1995) appears to be a new and unique type of mammal. Specimens were procured through Queensland Museum (Riversleigh material); Australian Museum (Lightning Ridge material); and Museum of Victoria and the South Australian Museum (fossil ornithorhynchids). Specimens were examined under a light microscope and scanning electron microscope; specimens were photographed using light photography and a scanning electron microscope; and illustrations and reconstructions were done with a camera lucida microscope attachment and photographic references. Parsimony analysis utilised the computer programs PAUP and MacClade. Major conclusions: 1) analysis and reconstruction of the skull of the Miocene platypus Obdurodon dicksoni suggest this robust, large-billed platypus was a derived northern offshoot off the main line of ornithorhynchid evolution; 2) the well-preserved skull of Obdurodon dicksoni shows aspects of soft anatomy previously unknown for fossil ornithorhynchids; 3) two upper molars from Mammalon Hill (Etadunna Formation, late Oligocene, central Australia) represent a third species of Obdurodon; 4) the South American ornithorhynchid Monotrematum sudamericanum from the Paleocene of Argentina is very close in form to the Oligocene-Miocene Obdurodon species from Australia and should be considered congeneric; 5) a revised diagnosis of the lower jaw of the Early Cretaceous monotreme Steropodon galmani includes the presence of two previously undescribed archaic features: the probable presence of postdentary bones and a meckelian groove; 6) morphological evidence is presented supporting a separate family Steropodontidae; and 7) analysis of new fossil material for Kollikodon ritchiei suggests that this taxon is not a monotreme mammal as originally identified but is a basal mammal with close relationships to allotherian mammals (Morganucodonta; Haramiyida). Kollikodon is provisionally placed as basal allotherian mammal (Allotheria sensu Butler 2000) and is unique at the ordinal level, being neither haramiyid nor multituberculate. A new allotherian order ??? Kollikodonta ??? is proposed.

Extant monotremes have a combination of plesiomorphic and apomorphic characters that causes ambiguity about their basic anatomy and evolutionary history. The problem is compounded by the lack of extinct and extant specimens of monotremes available for study. Only five species of monotremes are currently recognized, and all are endangered. The most speciose subclade, the long-beaked echidna, Zaglossus, has few specimens archived in mammalogy collections relative to the platypus, Ornithorhynchus anatinus, and the short-beaked echidna, Tachyglossus aculeatus. As a result, researchers sample from Ornithorhynchus and Tachyglossus, excluding species of Zaglossus from analysis. An equally depauperate fossil record consisting primarily of fragmentary jaws and isolated molars over a broad temporal range (~125 Ma) has led to controversies surrounding the origin and evolution of Monotremata and its major subclades. As new fossils attributable to Monotremata have been discovered, they are placed in conflicting positions on either the crown or the stem. I used CT scans of skeletally immature and mature specimens of Zaglossus bruijni and Zaglossus bartoni, respectively, to describe the cranial osteology of Zaglossus in detail. New insights about the anatomy of Zaglossus were then utilized in a phylogenetic analysis. Zaglossus and the extinct echidna, Megalibgwilia were added to a previously published morphological character matrix, along with 42 new skeletal characters. For the first time, I illustrated the cranial anatomy of Zaglossus bruijnii and Zaglossus bartoni, and described the endocranial morphology and individual variation among the two species. I described patterns of ossification throughout ontogeny that may explain a preservation bias against echidnas. My phylogenetic analysis placed the Early Cretaceous monotremes either on the stem of Ornithorhynchidae or in the monotreme crown, supporting an Early Cretaceous divergence estimate between platypuses and echidnas. I provide the first phylogenetic definition and diagnosis of Monotremata, Ornithorhynchidae, and Tachyglossidae. Based on the distribution of characters of extant monotremes, the ancestral monotreme was likely a terrestrial, scratch-digger capable of electroreception. The ancestral population gave rise to the semi-aquatic platypuses and the large, terrestrial echidnas. Tachyglossus is the most derived of the extant echidnas; it is more appropriate to include Ornithorhynchus and Zaglossus in future phylogenetic analyses. / text