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Articles 1 - 4 of 4
Full-Text Articles in Social and Behavioral Sciences
Climate-Induced Reaction Norms For Life-History Traits In Pythons, Beata Ujvari, Richard Shine, L Luiselli, Thomas R. Madsen
Climate-Induced Reaction Norms For Life-History Traits In Pythons, Beata Ujvari, Richard Shine, L Luiselli, Thomas R. Madsen
Faculty of Science - Papers (Archive)
Climate change modelers predict increasingly frequent ''extreme events,'' so it is critical to quantify whether organismal responses (such as reproductive output) measured over the range of usual climatic conditions can predict responses under more extreme conditions. In a 20-year field study on water pythons (Liasis fuscus), we quantified the effects of climatically driven annual variation in food supply on demographic traits of female pythons (feeding rate, body size, body mass, and reproductive output). Reaction norms linking food supply to feeding rates and residual body mass were broadly linear, whereas norms linking food supply to female body size became curvilinear when …
Structural History Of The Greenvale Province, North Queensland: Early Palaeozoic Extension And Convergence On The Pacific Margin Of Gondwana, Christopher L. Fergusson, R A Henderson, I. W. Withnall, C M Fanning
Structural History Of The Greenvale Province, North Queensland: Early Palaeozoic Extension And Convergence On The Pacific Margin Of Gondwana, Christopher L. Fergusson, R A Henderson, I. W. Withnall, C M Fanning
Faculty of Science - Papers (Archive)
The southeastern Georgetown Inlier (Greenvale Province) consists of Early Palaeozoic metamorphic rocks in fault contact along the Lynd Mylonite Zone with the Palaeoproterozoic to Mesoproterozoic craton of northeastern Australia. It has a central assemblage of metamorphosed silicic volcanic and sedimentary rocks considered equivalent to the Late Cambrian to Early Ordovician Seventy Mile Range Group that developed in an extensional backarc in the Charters Towers Province to the southeast. In the western part of the Greenvale Province the Oasis Metamorphics has a U-Pb zircon SHRIMP metamorphic age of 476 ± 5 Ma and is intruded by the granodioritic Lynwater Complex with …
Detrital Zircon Ages In Neoproterozoic To Ordovician Siliciclastic Rocks, Northeastern Australia: Implications For The Tectonic History Of The East Gondwana Continental Margin, Christopher L. Fergusson, Robert A. Henderson, C Mark Fanning, Ian W. Withnall
Detrital Zircon Ages In Neoproterozoic To Ordovician Siliciclastic Rocks, Northeastern Australia: Implications For The Tectonic History Of The East Gondwana Continental Margin, Christopher L. Fergusson, Robert A. Henderson, C Mark Fanning, Ian W. Withnall
Faculty of Science - Papers (Archive)
U–Pb detrital zircon ages in variably metamorphosed, dominantly fine-grained clastic successions are used in northeastern Australia to identify two major successions along the East Gondwana margin. The older succession is of probable Late Neoproterozoic age and is considered part of a passive margin associated with rifting at c. 600 Ma. Most detrital zircons have ages in the range 1000–1300 Ma and were probably derived from an extension of a Late Mesoproterozoic (1050–1200 Ma) orogenic belt from the central Australian Musgrave Complex located 1500 km to the west. No evidence has been found for 600–800 Ma rifting of a Rodinian supercontinent …
The History Of Aridity In Australia: Chronological Developments, Ed Rhodes, John Chappell, Toshiyuki Fujioka, Kat Fitzsimmons, John Magee, Max Aubert, Dolan Hewitt
The History Of Aridity In Australia: Chronological Developments, Ed Rhodes, John Chappell, Toshiyuki Fujioka, Kat Fitzsimmons, John Magee, Max Aubert, Dolan Hewitt
Faculty of Science - Papers (Archive)
Desert dune-fields are quintessential features of arid landscapes. During arid phases in the recent geological past, such as the global last glacial maximum (LGM) at around 20,000 years ago, many parts of Australia experienced significant sand movement, with sand migrating down-wind and forming linear dunes. Sand entrainment and deposition is controlled by vegetative surface stabilisation, wind speed and direction, which in turn are controlled by regional climate and local factors including ground-water levels. Climate also affects sand supply, through its effects on erosion in the source areas and transport to the dune-building areas.