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Статті в журналах з теми "Naracoorte Caves"

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Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 29 січня 2023

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1

Adetutu, Eric, Krystal Thorpe, Esmaeil Shahsavari, Steven Bourne, Xiangsheng Cao, Ramin Fard, Greg Kirby, and Andrew Ball. "Bacterial community survey of sediments at Naracoorte Caves, Australia." International Journal of Speleology 41, no. 2 (July 2012): 137–47. http://dx.doi.org/10.5038/1827-806x.41.2.2.

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2

Hamilton-Smith, Elery. "No ordinary man: Tenison Woods and the Naracoorte Caves." Alcheringa: An Australasian Journal of Palaeontology 31 (2006): 187–93. http://dx.doi.org/10.1080/03115510608619581.

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3

HAMILTON-SMITH, ELERY. "No ordinary man: Tenison Woods and the Naracoorte Caves." Alcheringa: An Australasian Journal of Palaeontology 30, sup1 (January 2006): 187–93. http://dx.doi.org/10.1080/03115510609506862.

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4

Forbes, M. S., and E. A. Bestland. "Origin of the sedimentary deposits of the Naracoorte Caves, South Australia." Geomorphology 86, no. 3-4 (May 2007): 369–92. http://dx.doi.org/10.1016/j.geomorph.2006.09.009.

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5

Macken, Amy C., and Elizabeth H. Reed. "Late Quaternary Small Mammal Faunas of the Naracoorte Caves World Heritage Area." Transactions of the Royal Society of South Australia 137, no. 1 (January 2013): 53–67. http://dx.doi.org/10.1080/3721426.2013.10887171.

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6

Gr�n, Rainer, Kevin Moriarty, and Rod Wells. "Electron spin resonance dating of the fossil deposits in the Naracoorte Caves, South Australia." Journal of Quaternary Science 16, no. 1 (January 2001): 49–59. http://dx.doi.org/10.1002/1099-1417(200101)16:1<49::aid-jqs570>3.0.co;2-#.

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7

Adetutu, Eric M., Krystal Thorpe, Steven Bourne, Xiangsheng Cao, Esmaeil Shahsavari, Greg Kirby, and Andrew S. Ball. "Phylogenetic diversity of fungal communities in areas accessible and not accessible to tourists in Naracoorte Caves." Mycologia 103, no. 5 (September 2011): 959–68. http://dx.doi.org/10.3852/10-256.

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8

Holz, Peter H., Phillip Clark, David J. McLelland, Linda F. Lumsden, and Jasmin Hufschmid. "Haematology of southern bent-winged bats (Miniopterus orianae bassanii) from the Naracoorte Caves National Park, South Australia." Comparative Clinical Pathology 29, no. 1 (August 21, 2019): 231–37. http://dx.doi.org/10.1007/s00580-019-03049-z.

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9

James, Jane A., and Carolyn N. Wild. "The Bigger They Are, the Harder They Fall! Sustainable Tourism Planning at Naracoorte Caves World Heritage Site, Australia." Journal of Heritage Tourism 2, no. 3 (January 2008): 196–210. http://dx.doi.org/10.2167/jht060.0.

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10

Bestland, Erick, та Jessica Rennie. "Stable isotope record (δ18O and δ13C) of a Naracoorte Caves speleothem from before and after the Last Interglacial". Alcheringa: An Australasian Journal of Palaeontology 31 (2006): 19–29. http://dx.doi.org/10.1080/03115510608619571.

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11

BESTLAND, ERICK A., та JESSICA RENNIE. "Stable isotope record (δ18O and δ13C) of a Naracoorte Caves speleothem from before and after the Last Interglacial". Alcheringa: An Australasian Journal of Palaeontology 30, sup1 (січень 2006): 19–29. http://dx.doi.org/10.1080/03115510609506852.

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12

Lewis, I. D. "South Australian geology and the State Heritage Register: an example of geoconservation of the Naracoorte Caves complex and karst environment." Australian Journal of Earth Sciences 66, no. 6 (June 16, 2019): 785–92. http://dx.doi.org/10.1080/08120099.2019.1608300.

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13

Grealy, Alicia, Amy Macken, Morten E. Allentoft, Nicolas J. Rawlence, Elizabeth Reed, and Michael Bunce. "An assessment of ancient DNA preservation in Holocene-Pleistocene fossil bone excavated from the world heritage Naracoorte Caves, South Australia." Journal of Quaternary Science 31, no. 1 (January 2016): 33–45. http://dx.doi.org/10.1002/jqs.2830.

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14

Macken, Amy C., Richard A. Staff, and Elizabeth H. Reed. "Bayesian age-depth modelling of Late Quaternary deposits from Wet and Blanche Caves, Naracoorte, South Australia: A framework for comparative faunal analyses." Quaternary Geochronology 17 (June 2013): 26–43. http://dx.doi.org/10.1016/j.quageo.2013.03.001.

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15

Piper, KJ. "An early Pleistocene record of a giant koala (Phascolarctidae: Marsupialia) from western Victoria." Australian Mammalogy 27, no. 2 (2005): 221. http://dx.doi.org/10.1071/am05221.

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Анотація:

THE pre Holocene-Late Pleistocene record of Phascolarctos in Australia is extremely meagre. There are at least two, possibly three extinct species of Phascolarctos in addition to the extant Phascolarctos cinereus (Black 1999). P. yorkensis (syn. Cundokoala yorkensis; Black and Archer 1997) is known from the Early Pliocene Curramulka Local Fauna, South Australia (SA), and the Late Pleistocene Wellington Caves Local Fauna, New South Wales (Archer et al. 1997; Pledge 1992). P. stirtoni occurs in the Late Pleistocene Cement Mills Local Fauna, Queensland, and is known only from a partial maxilla containing P3-M2 (Bartholomai 1968, 1977). Phascolarctos material from the mid- Pleistocene Victoria Fossil Cave and Spring Cave, Naracoorte, SA, have also been referred to P. cf. stirtoni but remain undescribed (Reed and Bourne 2000; Moriarty et al. 2000). P. maris is known from a single lower molar from the Early Pliocene Sunlands Local Fauna, SA (Pledge 1987). Black (1999) cast doubt on its validity, suggesting its features may fall within the intraspecific variation of P. stirtoni. If P. maris is referable to P. stirtoni it is another South Australian instance of this species, and extends its range back to the Early Pliocene. The new phascolarctid material documented here is from the early Pleistocene Nelson Bay Local Fauna, Portland, Victoria (141o 35? E; 38o 36? S). It is therefore an important additional southern occurrence of a species larger than the living P. cinereus, and is the only pre- Late Pleistocene record of the Phascolarctidae in Victoria.

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16

Deland, M. P. B., J. M. Accioly, K. J. Copping, J. F. Graham, S. J. Lee, P. McGilchrist, and W. S. Pitchford. "Divergent breeding values for fatness or residual feed intake in Angus cattle. 6. Dam-line impacts on steer carcass compliance." Animal Production Science 58, no. 1 (2018): 94. http://dx.doi.org/10.1071/an14594.

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Анотація:

The present study determined the impact of maternal genetics for estimated breeding values for rib fat (High-Fat, Low-Fat) or residual feed intake (RFI; High-RFI, Low-RFI) on the carcass compliance of Angus steer progeny when reared pre-weaning under High or Low-Nutrition and post-weaning under various finishing system (grazing versus short-term feedlot). The dams were joined to sires of similar genetic background (close to average estimated breeding values) and sires were rotated among all dam genotypes, with herds located at either Struan Research Centre, near Naracoorte in the south-east of South Australia, or Vasse Research Station, in the south-west of Western Australia. The breeding herd was part of the Beef CRC maternal productivity project and cows were managed under either High or Low-Nutrition, achieved by adjustments to stocking rate in rotational grazing systems and supplementary feeding, so as to maintain ~20% difference in cow liveweight. The steer progeny were weaned at ~7 months of age, with individuals from both pre-weaning nutritional treatments being treated the same from then on at each site. Steers from Struan Research Centre in South Australia born in 2008 and 2009 were sold and grown out on pasture on a local commercial property. Steer calves born in 2010 at Vasse remained on the station where they were backgrounded on hay, followed by a short period (111 days) total mixed ration containing 40% grain. In the first year, steers from Struan (n = 58) were slaughtered together at ~2 years of age, and in the second year (n = 85), consigned to six slaughter groups as their ultrasound-scanned subcutaneous P8 (rump) fat reached 7 mm and their liveweight exceeded 550 kg. Steers from Vasse (n = 101) were slaughtered at ~12 months of age, all on the same day. High-Fat-line dams produced steers with carcasses with greater P8 fat than did Low-Fat-line dams at both sites. At Struan, when the 2008-born steers were slaughtered together, more steers from Low-Fat dams failed to meet minimum fat specifications, than steers from High-Fat dams (28% vs 9% respectively). The steers born in 2009 at Struan all met processor fat specifications but steers from the Low-Fat dams took longer to reach the fat threshold, and so had greater carcass weight, but attracted more price penalties because of increased dentition. All steers from Vasse met minimum requirements for fat, with none penalised for dentition. Vasse steers from High- or Low-RFI dams performed in a manner similar to that from High- and Low-Fat dams, respectively, in that the High-RFI group produced fatter carcasses than did the Low-RFI group. Steers reared under low pre-weaning nutrition weighed less at weaning than did those on High-Nutrition, but had higher weight gains after weaning, although insufficient to result in the same carcass weight. The results showed that commercial cattle producers need to be aware of the balance and trade-off among fat breeding value, effect of pre-weaning nutrition and post-weaning growth required to ensure their cattle meet market specifications and to avoid price penalties.

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17

Weij, Rieneke, Jon D. Woodhead, J. M. Kale Sniderman, John C. Hellstrom, Elizabeth Reed, Steven Bourne, Russell N. Drysdale, and Timothy J. Pollard. "Cave opening and fossil accumulation in Naracoorte, Australia, through charcoal and pollen in dated speleothems." Communications Earth & Environment 3, no. 1 (September 26, 2022). http://dx.doi.org/10.1038/s43247-022-00538-y.

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Анотація:

AbstractCaves are important fossil repositories which provide records extending back over million-year timescales. While the physical processes of cave formation are well understood, the timing of initial cave development and opening—a more important parameter to studies of palaeontology, palaeoanthropology and archaeology—has proved more difficult to constrain. Here we investigate speleothems from the Naracoorte Cave Complex in southern Australia, with a rich record of Pleistocene vertebrate fossils (including extinct megafauna) and partly World Heritage-listed, using U-Th-Pb dating and analyses of their charcoal and pollen content. We find that, although speleothem formation began at least 1.34 million years ago, pollen and charcoal only began to be trapped within growing speleothems from 600,000 years ago. We interpret these two ages to represent the timing of initial cave development and the subsequent opening of the caves to the atmosphere respectively. These findings demonstrate the potential of U-Th-Pb dating combined with charcoal and pollen as proxies to assess the potential upper age limit of vertebrate fossil records found within caves.

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