1981
DOI: 10.1007/978-94-009-8629-9_49
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The Australian reptiles: origins, biogeography, distribution patterns and island evolution

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Cited by 69 publications
(81 citation statements)
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“…Thus, some of the terminal splits among elapids had already occurred by the Miocene. Considering that the split between hydrophiines and elapines represents the basal split within elapids, not a terminal split, then clearly the division between elapines and hydrophiines predates the Miocene and probably considerably so, an idea that has been suggested by other authors (e.g., Cogger and Heatwole, 1981;Cogger, 1984). We ascribe Schwaner et al's results to a rate slow-down in the evolution of elapid plasma transferrins.…”
Section: Figmentioning
confidence: 81%
“…Thus, some of the terminal splits among elapids had already occurred by the Miocene. Considering that the split between hydrophiines and elapines represents the basal split within elapids, not a terminal split, then clearly the division between elapines and hydrophiines predates the Miocene and probably considerably so, an idea that has been suggested by other authors (e.g., Cogger and Heatwole, 1981;Cogger, 1984). We ascribe Schwaner et al's results to a rate slow-down in the evolution of elapid plasma transferrins.…”
Section: Figmentioning
confidence: 81%
“…The D. tincta group as a whole has a 'Torresian' distribution (sensu Cogger and Heatwole 1981). This appears to be unique within the genus Delma, since other species groups recognized on morphological (Kluge 1974;Shea 1991) or molecular criteria _ (Jennings et al 2003) …”
Section: Biogeography Of the Delma Tincta Groupmentioning
confidence: 99%
“…The first hypothesis claims that climatic changes and the close proximity of the Australia-New Guinea plate to Laurasia during the Miocene would have allowed Laurasian groups to disperse to Australia or New Guinea and to occupy open niches not available in South East Asia (Cogger & Heatwole 1981). Alternatively, a Middle to Late Mesozoic (75-160 Myr ago) separation of these faunas by the breakup of Gondwanaland indicates that the primary diversification of major groups occurred among continental fragments moving in isolation across the Tethys Sea.…”
Section: Introductionmentioning
confidence: 99%