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Статті в журналах з теми "Fossils Australia History"
Rix, Alan. "The Triassic insects of Denmark Hill, Ipswich, Southeast Queensland: the creation, use and dispersal of a collection." Memoirs of the Queensland Museum - Nature 62 (March 18, 2021): 217–42. http://dx.doi.org/10.17082/j.2204-1478.62.2021.2020-11.
Повний текст джерелаMcnamara, Kenneth, and Frances Dodds. "The Early History of Palaeontology in Western Australia: 1791-1899." Earth Sciences History 5, no. 1 (January 1, 1986): 24–38. http://dx.doi.org/10.17704/eshi.5.1.t85384660311h176.
Повний текст джерелаRetallack, G. J. "Precambrian life on land." Journal of Palaeosciences 63, no. (1-2) (December 31, 2014): 1–15. http://dx.doi.org/10.54991/jop.2014.289.
Повний текст джерелаPark, Travis, Erich M. G. Fitzgerald, Stephen J. Gallagher, Ellyn Tomkins, and Tony Allan. "New Miocene Fossils and the History of Penguins in Australia." PLOS ONE 11, no. 4 (April 26, 2016): e0153915. http://dx.doi.org/10.1371/journal.pone.0153915.
Повний текст джерелаConran, John G., Raymond J. Carpenter, and Gregory J. Jordan. "Early Eocene Ripogonum (Liliales: Ripogonaceae) leaf macrofossils from southern Australia." Australian Systematic Botany 22, no. 3 (2009): 219. http://dx.doi.org/10.1071/sb08050.
Повний текст джерелаCOOPER, BARRY J., and JAMES B. JAGO. "ROBERT BEDFORD (1874–1951), THE KYANCUTTA MUSEUM, AND A UNIQUE CONTRIBUTION TO INTERNATIONAL GEOLOGY." Earth Sciences History 37, no. 2 (January 1, 2018): 416–43. http://dx.doi.org/10.17704/1944-6178-37.2.416.
Повний текст джерелаPoropat, Stephen F., Matt A. White, Tim Ziegler, Adele H. Pentland, Samantha L. Rigby, Ruairidh J. Duncan, Trish Sloan, and David A. Elliott. "A diverse Late Cretaceous vertebrate tracksite from the Winton Formation of Queensland, Australia." PeerJ 9 (June 17, 2021): e11544. http://dx.doi.org/10.7717/peerj.11544.
Повний текст джерелаOsborne, R. "Red Earth and Bones: the History of Cave Sediment Studies in New South Wales, Australia." Earth Sciences History 10, no. 1 (January 1, 1991): 13–28. http://dx.doi.org/10.17704/eshi.10.1.e132047518j87216.
Повний текст джерелаBranagan, David. "The Desert Sandstone of Australia A Late Nineteenth-Century Enigma of Deposition, Fossils, and Weathering." Earth Sciences History 23, no. 2 (January 1, 2004): 208–56. http://dx.doi.org/10.17704/eshi.23.2.gj680520775h7m27.
Повний текст джерелаArchbold, N. "Nineteenth Century Views on the Australian Marine Permian." Earth Sciences History 5, no. 1 (January 1, 1986): 12–23. http://dx.doi.org/10.17704/eshi.5.1.au03316525485655.
Повний текст джерелаДисертації з теми "Fossils Australia History"
Gayler, Lucyna Maria. "A palaeoenvironmental history of the Paroo and Warrego Regions, Australia: a multi-proxy, multi-site approach." Thesis, 2008. http://hdl.handle.net/1959.13/33470.
Повний текст джерелаThe records of environmental change in Australia’s arid zone can be greatly enriched by employing a multi-proxy approach and landscape-scale analysis. This research uses these tools to construct a palaeoenvironmental history of the Paroo/Warrego Region. While the Region’s flow regimes and water balances are characterised by medium-term (decadal) variability (Young, 1999), its hydrological records are inadequately brief. Subsequently, land and water management decisions are based on short term data, risking irreversible damage, desertification or loss of diversity. A better understanding of this highly dynamic landscape can thus improve the land and resource management outcomes. While dating was constrained by a lack of funds, the Paroo/Warrego history reconstructed from fluvial and aeolian deposits correlated well with events recorded from other inland regions of the Australian continent. In summary, this new research provided evidence of high lake water levels prior to the Last Glacial. The extreme aridity at the onset of Last Glacial caused long term drying of the lakes and mobilisation of the red sand dunes. In latter stages of the glacial phase the aridity gave way to periodic fluctuations between flood and drought events that probably lasted until 16 000 - 14 000 BP. The new climatic regime resulted in formation of gypsum lunettes and later, following reduction in gypsum supply, clay lunettes. The orientation of red sand dunes and lunettes indicates a more northerly extent of the westerlies than in modern times. Around the late Pleistocene-early Holocene boundary the climate became more stable and wetter, but still somewhat drier than during the pre-Last Glacial lacustrine phase. As a result, the region’s lakes reverted to a permanent and semi-permanent status. A strong aridity signal, comparable to the semi-regular droughts of the Last Glacial, was recorded in the Paroo/Warrego lakes during the late 1890s-1940s period of below average rainfall. It was followed by 50 years of wetter conditions with two extremely wet phases in the 1950s and the 1970s. Finally, the most recent records suggest a new drying trend. The semi-arid vegetation appears to have adapted to climate variability, with herbs and grasses expanding with the onset of wet conditions before being replaced by Chenopodiaceae as the landscape started to dry. The fresher lake basins and water courses were likely to provide refuge during prolonged arid phases and dispersal foci during intervening wetter periods, thus enabling greater flexibility in response to changes and enhancing resilience. The European land use interfered with the natural cycles and balances, leading to decrease in ground cover, suppression of fire, increase in runoff and catchment erosion, acceleration of sediment accumulation rates in wetlands, resulting in decline of their water holding capacity, and expansion of woody vegetation. The research improved the processing protocols, reference databases, and transfer of methods to enable greater sample processing efficiency and improve results. The use of multiple proxies (including biotic and abiotic components) and sites, as well as different depositional features, provided access to a broader picture of environmental change than was previously possible. It also facilitated multi-scale resolution, allowing discrimination between localised responses of individual lakes and regional trends. The full value of this research will come from informing natural resource managers, whose actions will shape the future landscapes of the Paroo and Warrego Region.
Gayler, Lucyna Maria. "A palaeoenvironmental history of the Paroo and Warrego Regions, Australia: a multi-proxy, multi-site approach." 2008. http://hdl.handle.net/1959.13/33470.
Повний текст джерелаThe records of environmental change in Australia’s arid zone can be greatly enriched by employing a multi-proxy approach and landscape-scale analysis. This research uses these tools to construct a palaeoenvironmental history of the Paroo/Warrego Region. While the Region’s flow regimes and water balances are characterised by medium-term (decadal) variability (Young, 1999), its hydrological records are inadequately brief. Subsequently, land and water management decisions are based on short term data, risking irreversible damage, desertification or loss of diversity. A better understanding of this highly dynamic landscape can thus improve the land and resource management outcomes. While dating was constrained by a lack of funds, the Paroo/Warrego history reconstructed from fluvial and aeolian deposits correlated well with events recorded from other inland regions of the Australian continent. In summary, this new research provided evidence of high lake water levels prior to the Last Glacial. The extreme aridity at the onset of Last Glacial caused long term drying of the lakes and mobilisation of the red sand dunes. In latter stages of the glacial phase the aridity gave way to periodic fluctuations between flood and drought events that probably lasted until 16 000 - 14 000 BP. The new climatic regime resulted in formation of gypsum lunettes and later, following reduction in gypsum supply, clay lunettes. The orientation of red sand dunes and lunettes indicates a more northerly extent of the westerlies than in modern times. Around the late Pleistocene-early Holocene boundary the climate became more stable and wetter, but still somewhat drier than during the pre-Last Glacial lacustrine phase. As a result, the region’s lakes reverted to a permanent and semi-permanent status. A strong aridity signal, comparable to the semi-regular droughts of the Last Glacial, was recorded in the Paroo/Warrego lakes during the late 1890s-1940s period of below average rainfall. It was followed by 50 years of wetter conditions with two extremely wet phases in the 1950s and the 1970s. Finally, the most recent records suggest a new drying trend. The semi-arid vegetation appears to have adapted to climate variability, with herbs and grasses expanding with the onset of wet conditions before being replaced by Chenopodiaceae as the landscape started to dry. The fresher lake basins and water courses were likely to provide refuge during prolonged arid phases and dispersal foci during intervening wetter periods, thus enabling greater flexibility in response to changes and enhancing resilience. The European land use interfered with the natural cycles and balances, leading to decrease in ground cover, suppression of fire, increase in runoff and catchment erosion, acceleration of sediment accumulation rates in wetlands, resulting in decline of their water holding capacity, and expansion of woody vegetation. The research improved the processing protocols, reference databases, and transfer of methods to enable greater sample processing efficiency and improve results. The use of multiple proxies (including biotic and abiotic components) and sites, as well as different depositional features, provided access to a broader picture of environmental change than was previously possible. It also facilitated multi-scale resolution, allowing discrimination between localised responses of individual lakes and regional trends. The full value of this research will come from informing natural resource managers, whose actions will shape the future landscapes of the Paroo and Warrego Region.
Douglas, Kirsty. "Pictures of time beneath : science, landscape, heritage and the uses of the deep past in Australia, 1830-2003." Phd thesis, 2004. http://hdl.handle.net/1885/7498.
Повний текст джерелаIn 2010, material in this thesis was reworked and published as Pictures of time beneath: science, heritage and the uses of the deep past (CSIRO Publishing, Collingwood, Victoria): http://www.publish.csiro.au/pid/6342.htm.
Passlow, Victoria. "Late Quaternary history of the Southern Ocean offshore Southeastern Australia, based on deep-sea Ostracoda." Phd thesis, 1994. http://hdl.handle.net/1885/140921.
Повний текст джерелаShulmeister, James. "Late Quaternary and Holocene environmental history of Groote Eylandt, Northern Australia." Phd thesis, 1991. http://hdl.handle.net/1885/140901.
Повний текст джерелаGrindrod, John. "Holocene mangrove history of the South Alligator River estuary, Northern Territory, Australia." Phd thesis, 1988. http://hdl.handle.net/1885/140910.
Повний текст джерелаКниги з теми "Fossils Australia History"
Australia's fossil heritage: A catalogue of important Australian fossil sites. Collingwood, Vic: CSIRO Pub., 2012.
Знайти повний текст джерелаMcNamara, Ken. Prehistoric mammals of Western Australia. Welshpool DC, W.A: Western Australian Museum, 2010.
Знайти повний текст джерелаKear, Benjamin P., and Robert J. Hamilton-Bruce. Dinosaurs in Australia. CSIRO Publishing, 2011. http://dx.doi.org/10.1071/9780643101692.
Повний текст джерелаDigging Up Deep Time: Fossils, Dinosaurs and Megabeasts from Australia's Distant Past. Bond University Press, 2005.
Знайти повний текст джерелаAustralia's Fossil Heritage. CSIRO Publishing, 2012. http://dx.doi.org/10.1071/9780643101784.
Повний текст джерелаWilliams, Geoff. Invertebrate World of Australia's Subtropical Rainforests. CSIRO Publishing, 2020. http://dx.doi.org/10.1071/9781486312924.
Повний текст джерелаCook, Patricia, Philip Bock, Dennis Gordon, and Haylee Weaver, eds. Australian Bryozoa Volume 1. CSIRO Publishing, 2018. http://dx.doi.org/10.1071/9781486306800.
Повний текст джерелаJohansen, Bruce, and Adebowale Akande, eds. Nationalism: Past as Prologue. Nova Science Publishers, Inc., 2021. http://dx.doi.org/10.52305/aief3847.
Повний текст джерелаЧастини книг з теми "Fossils Australia History"
Hill, R. S. "The Australian fossil plant record: an introduction." In History of the Australian Vegetation: Cretaceous to Recent, 1–4. University of Adelaide Press, 2017. http://dx.doi.org/10.20851/australian-vegetation-01.
Повний текст джерелаRogers, John J. W., and M. Santosh. "Gondwana and Pangea." In Continents and Supercontinents. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780195165890.003.0010.
Повний текст джерелаCann, John, and Chantelle Lower. "Fossil Molluscs, Foraminifera, Ostracods and Oogonia Record a Coorong History." In Natural History of the Coorong, Lower Lakes, and Murray Mouth region (Yarluwar-Ruwe). Royal Society of South Australia. University of Adelaide Press, 2018. http://dx.doi.org/10.20851/natural-history-cllmm-2.5.
Повний текст джерелаТези доповідей конференцій з теми "Fossils Australia History"
Schenewerk, William Ernest. "Fuel-Cell and Electrolysis By-Product D2O Improves Third Way to Mitigate CO2." In ASME 2015 Nuclear Forum collocated with the ASME 2015 Power Conference, the ASME 2015 9th International Conference on Energy Sustainability, and the ASME 2015 13th International Conference on Fuel Cell Science, Engineering and Technology. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/nuclrf2015-49061.
Повний текст джерела