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Статті в журналах з теми "Willandra Lakes"

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Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 29 січня 2023

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1

Johnston, Harvey, and Peter Clark. "Willandra Lakes Archaeological Investigations 1968-98." Archaeology in Oceania 33, no. 3 (October 1998): 105–19. http://dx.doi.org/10.1002/j.1834-4453.1998.tb00413.x.

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2

Hiscock, Peter, and Harry Allen. "Assemblage variability in the Willandra Lakes." Archaeology in Oceania 35, no. 3 (October 2000): 97–103. http://dx.doi.org/10.1002/j.1834-4453.2000.tb00462.x.

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3

Bowler, J. M. "Willandra Lakes revisited: environmental framework for human occupation." Archaeology in Oceania 33, no. 3 (October 1998): 120–55. http://dx.doi.org/10.1002/j.1834-4453.1998.tb00414.x.

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4

Allen, Harry. "Reinterpreting the 1969-1972 Willandra Lakes archaeological surveys." Archaeology in Oceania 33, no. 3 (October 1998): 207–20. http://dx.doi.org/10.1002/j.1834-4453.1998.tb00419.x.

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5

Webb, Steve, Matthew L. Cupper, and Richard Robins. "Pleistocene human footprints from the Willandra Lakes, southeastern Australia." Journal of Human Evolution 50, no. 4 (April 2006): 405–13. http://dx.doi.org/10.1016/j.jhevol.2005.10.002.

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6

Gillespie, Richard. "Alternative timescales: a critical review of Willandra Lakes dating." Archaeology in Oceania 33, no. 3 (October 1998): 169–82. http://dx.doi.org/10.1002/j.1834-4453.1998.tb00416.x.

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7

Smith, Mike. "How the Desert got a Past: A History of Quaternary Research in Australia’s Deserts." Historical Records of Australian Science 25, no. 2 (2014): 172. http://dx.doi.org/10.1071/hr14012.

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Анотація:

This paper examines how the past of desert landscapes has been interpreted since European explorers and scientists first encountered them. It charts the research that created the conceptual space within which archaeologists and Quaternarists now work. Studies from the 1840s–1960s created the notion of a ‘Great Australian Arid Period'. The 1960s studies of Lake Mungo and the Willandra Lakes by Jim Bowler revealed the cyclical nature of palaeolakes, that changed with climate changes in the Pleistocene, and the complexity of desert pasts. SLEADS and other researchers in the 1980s used thermoluminescence techniques that showed further complexities in desert lands beyond the Willandra particularly through new studies in the Strzelecki and Simpson Dunefields, Lake Eyre, Lake Woods and Lake Gregory. Australian deserts are varied and have very different histories. Far from ‘timeless lands', they have carried detailed information about long-term climate changes on continental scales.

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8

Hope, Jeannette. "A Regional Environmental Plan for the Willandra Lakes World Heritage Region." Australian Archaeology 20, no. 1 (June 1, 1985): 32–37. http://dx.doi.org/10.1080/03122417.1985.12092983.

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9

Durband, Arthur C. "Is there Evidence for Artificial Cranial Deformation at the Willandra Lakes?" Australian Archaeology 73, no. 1 (December 1, 2011): 62–64. http://dx.doi.org/10.1080/03122417.2011.11961925.

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10

Webb, Steve. "Further research of the Willandra Lakes fossil footprint site, southeastern Australia." Journal of Human Evolution 52, no. 6 (June 2007): 711–15. http://dx.doi.org/10.1016/j.jhevol.2007.02.001.

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11

MILNE, A. K., and A. L. O'NEILL. "Mapping and monitoring land cover in the Willandra Lakes World Heritage Region." International Journal of Remote Sensing 11, no. 11 (November 1990): 2035–49. http://dx.doi.org/10.1080/01431169008955159.

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12

ALLEN, HARRY, and SIMON HOLDAWAY. "The archaeology of Mungo and the Willandra Lakes: looking back, looking forward." Archaeology in Oceania 44, no. 2 (July 2009): 96–106. http://dx.doi.org/10.1002/j.1834-4453.2009.tb00052.x.

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13

Heupink, Tim H., Sankar Subramanian, Joanne L. Wright, Phillip Endicott, Michael Carrington Westaway, Leon Huynen, Walther Parson, Craig D. Millar, Eske Willerslev, and David M. Lambert. "Ancient mtDNA sequences from the First Australians revisited." Proceedings of the National Academy of Sciences 113, no. 25 (June 6, 2016): 6892–97. http://dx.doi.org/10.1073/pnas.1521066113.

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Анотація:

The publication in 2001 by Adcock et al. [Adcock GJ, et al. (2001) Proc Natl Acad Sci USA 98(2):537–542] in PNAS reported the recovery of short mtDNA sequences from ancient Australians, including the 42,000-y-old Mungo Man [Willandra Lakes Hominid (WLH3)]. This landmark study in human ancient DNA suggested that an early modern human mitochondrial lineage emerged in Asia and that the theory of modern human origins could no longer be considered solely through the lens of the “Out of Africa” model. To evaluate these claims, we used second generation DNA sequencing and capture methods as well as PCR-based and single-primer extension (SPEX) approaches to reexamine the same four Willandra Lakes and Kow Swamp 8 (KS8) remains studied in the work by Adcock et al. Two of the remains sampled contained no identifiable human DNA (WLH15 and WLH55), whereas the Mungo Man (WLH3) sample contained no Aboriginal Australian DNA. KS8 reveals human mitochondrial sequences that differ from the previously inferred sequence. Instead, we recover a total of five modern European contaminants from Mungo Man (WLH3). We show that the remaining sample (WLH4) contains ∼1.4% human DNA, from which we assembled two complete mitochondrial genomes. One of these was a previously unidentified Aboriginal Australian haplotype belonging to haplogroup S2 that we sequenced to a high coverage. The other was a contaminating modern European mitochondrial haplotype. Although none of the sequences that we recovered matched those reported by Adcock et al., except a contaminant, these findings show the feasibility of obtaining important information from ancient Aboriginal Australian remains.

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14

Allen, Harry, Simon Holdaway, Patricia Fanning, and Judith Littleton. "Footprints in the sand: appraising the archaeology of the Willandra Lakes, western New South Wales, Australia." Antiquity 82, no. 315 (March 1, 2008): 11–24. http://dx.doi.org/10.1017/s0003598x0009640x.

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Анотація:

Here is a paper of pivotal importance to all prehistorians attempting to reconstruct societies from assemblages of shells or stone artefacts in dispersed sites deposited over tens of thousands of years. The authors demonstrate the perilous connections between the distribution and content of sites, their geomorphic formation process and the models used to analyse them. In particular they warn against extrapolating the enticing evidence from Pleistocene Willandra into behavioural patterns by drawing on the models presented by nineteenth-century anthropologists. They propose new strategies at once more revealing and more ethical.

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15

Fitzsimmons, Kathryn E., Caroline Spry, and Nicola Stern. "Holocene and recent aeolian reactivation of the Willandra Lakes lunettes, semi-arid southeastern Australia." Holocene 29, no. 4 (January 29, 2019): 606–21. http://dx.doi.org/10.1177/0959683618824790.

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The Willandra Lakes in semi-arid southeastern Australia provide some of the most continuous combined palaeoenvironmental and archaeological records on the continent. These are best preserved within the transverse shoreline (lunette) dunes on their downwind margins. Following final lake retreat c. 15 ka avulsion of the dominant fluvial inflow eastwards, the Willandra lunettes periodically reactivated, experiencing erosion, aeolian redeposition and alluvial sheetwash. These reworked sedimentary archives reflect regional climatic conditions rather than those of the entire catchment. Yet the focus of most study in the region to date has remained on the late Pleistocene. The general paucity of Holocene data has contributed to a perception that people largely abandoned the area in favour of the perennial Murray and Darling Rivers to the south and west. Our study reconstructs past geomorphological conditions and patterns of human mobility in adjacent Lakes Mungo and Durthong over the last c. 15 ka subsequent to final lake retreat, including the most recent 150 years since Europeans established pastoralism in the region. Our data show that Indigenous people did not abandon the area as previously assumed, but developed effective strategies for responding to the changed environmental conditions. Final lake retreat transitioned into a phase of aeolian accumulation c. 15–12 ka, indicating locally dry conditions. Subsequent aeolian reactivation peaked during arid phases experiencing less rainfall in the early Holocene and twice in the most recent 1000 years prior to European settlement in the area. Alluvial sheetwash was deposited onto lake floors during the mid-Holocene, and again in the early decades of European settlement. Aeolian reactivation, likely driven by European pastoral activities, increases in the most recent 150 years. Our study underscores the necessity of integrating geomorphological and archaeological investigations over landscape scales in order to optimise our understanding of interactions between people and their environment through time.

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16

Schmidt, Patrick, and Peter Hiscock. "The antiquity of Australian silcrete heat treatment: Lake Mungo and the Willandra Lakes." Journal of Human Evolution 142 (May 2020): 102744. http://dx.doi.org/10.1016/j.jhevol.2020.102744.

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17

Gillespie, Richard. "Burnt and Unburnt Carbon: Dating Charcoal and Burnt Bone from the Willandra Lakes, Australia." Radiocarbon 39, no. 3 (1997): 239–50. http://dx.doi.org/10.1017/s0033822200053236.

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A new analysis of previous results on conflicts between shell and charcoal dates and on burnt human bones, with new data presented here, suggests that alternative interpretations are possible for the archaeology and environmental history of the Willandra Lakes region. Black sediment samples from archaeological sites at Lake Outer Arumpo exhibit wide variation in burnt and unburnt carbon content; high humic acid concentrations in midden layers and in one group of hearth/ovens are absent in another, older, group of hearth/ovens. There are no acceptable results on charcoal from hearth/ovens older than ca. 31 ka bp, and no evidence that these samples are associated with numerous midden shell dates at 34–37 ka bp. Similar logic applied to humic-free residue dates on burnt human bones places five gracile skeletons (including Mungo 1) as post–Last Glacial Maximum.

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18

Fitzsimmons, Kathryn E., Nicola Stern, and Colin V. Murray-Wallace. "Depositional history and archaeology of the central Lake Mungo lunette, Willandra Lakes, southeast Australia." Journal of Archaeological Science 41 (January 2014): 349–64. http://dx.doi.org/10.1016/j.jas.2013.08.004.

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19

Grün, Rainer, Nigel Spooner, John Magee, Alan Thorne, John Simpson, Ge Yan, and Graham Mortimer. "Stratigraphy and chronology of the WLH 50 human remains, Willandra Lakes World Heritage Area, Australia." Journal of Human Evolution 60, no. 5 (May 2011): 597–604. http://dx.doi.org/10.1016/j.jhevol.2010.12.001.

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20

Tidemann, C. R. "A survey of the mammal fauna of the Willandra Lakes World Heritage region, New South Wales." Australian Zoologist 24, no. 4 (September 1988): 197–204. http://dx.doi.org/10.7882/az.1988.002.

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21

Long, Kelsie, David Heslop, and Eelco J. Rohling. "Quantitative assessment of the oxygen isotope composition of fish otoliths from Lake Mungo, Australia." Quaternary Research 102 (February 1, 2021): 234–46. http://dx.doi.org/10.1017/qua.2020.121.

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AbstractThe Willandra Lakes region is a series of once interconnected and now-dry lake basins in the arid zone of southeastern Australia. It is a UNESCO World Heritage Site of cultural, archaeological, and geological significance, preserving records of Aboriginal occupation and environmental change stretching back to at least 50 ka. Linking the archaeology with the commensurate palaeoenvironmental information is complicated by the millennial time spans represented by the past hydrological record preserved in the sediment vs. the subdecadal evidence of each archaeological site. Oxygen isotope records across annual growth rings of fish otoliths (ear stones) can elucidate flooding and drying regimes on subannual scales. Otoliths from hearth sites (fireplaces) link lake hydrology with people eating fish on the lakeshore. Oxygen isotopic trends in hearth otoliths from the last glacial maximum (LGM) were previously interpreted in terms of high evaporation under dry conditions. However, this ignored hydrology-driven changes in water δ18O. Here, a mass balance model is constructed to test the effect lake desiccation has on water δ18O and how this compares with the LGM otolith records. Based on this modelling, we suggest that Lake Mungo otolith signatures are better explained by evaporation acting on full lakes rather than by lake drying.

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22

Westaway, Michael C., Jon Olley, and Rainer Grün. "At least 17,000 years of coexistence: Modern humans and megafauna at the Willandra Lakes, South-Eastern Australia." Quaternary Science Reviews 157 (February 2017): 206–11. http://dx.doi.org/10.1016/j.quascirev.2016.11.031.

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23

CONSTANTINIDIS, DORA. "GIS for managing the analysis and protection of archaeological remains in the Willandra Lakes World Heritage Area." Archaeology in Oceania 44, no. 2 (July 2009): 112–18. http://dx.doi.org/10.1002/j.1834-4453.2009.tb00054.x.

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24

O'Neill, A. L. "Land system mapping using landsat multispectral scanner imagery in the Willandra lakes region of western New South Wales." Australian Geographer 20, no. 1 (May 1989): 26–36. http://dx.doi.org/10.1080/00049188908702972.

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25

Thomas, Katherine. "Exploratory GIS: Modelling Past Land Use and Occupancy with Functional Connectivity, Willandra Lakes Region World Heritage Area, NSW, Australia." Journal of Computer Applications in Archaeology 5, no. 1 (2022): 188–214. http://dx.doi.org/10.5334/jcaa.98.

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26

DURBAND, ARTHUR, DORA CONSTANTINIDIS, and DANIEL RAYNER. "25 Years of World Heritage status for Willandra Lakes: Papers from the ‘Legacy of an Ice Age’ commemorative conference (2006)." Archaeology in Oceania 44, no. 2 (July 2009): 74. http://dx.doi.org/10.1002/j.1834-4453.2009.tb00048.x.

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27

Fitzsimmons, Kathryn. "Change through time in the Willandra Lakes World Heritage Area: Linking human response to environmental change in the semi-arid zone." Quaternary International 279-280 (November 2012): 146. http://dx.doi.org/10.1016/j.quaint.2012.08.121.

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28

Hill, Ethan C., and Arthur C. Durband. "Mobility and subsistence at the Willandra Lakes: A comparative analysis of femoral cross-sectional properties in the Lake Mungo 3 skeleton." Journal of Human Evolution 73 (August 2014): 103–6. http://dx.doi.org/10.1016/j.jhevol.2014.05.014.

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29

Kurpiel, Rebekah, Robyn Pickering, Roland Maas, and Nicola Stern. "Lead (Pb) isotope signatures for silcrete sources from the Willandra Lakes region, Australia: A pilot study of a new method for provenancing silcrete artefacts." Journal of Archaeological Science: Reports 23 (February 2019): 62–71. http://dx.doi.org/10.1016/j.jasrep.2018.10.031.

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30

Wood, Bernard. "Peter Brown. Coobool Creek: a morphological and metrical analysis of the crania, mandibles and dentitions of a prehistoric Australian human population. Terra Australis 13. xxii + 205 pages, 8 plates, 71 figures, 75 tables. 1989. Canberra (ACT): Department of Prehistory, Research School of Pacific Studies, Australian National University; ISBN 0-7315-0742-8 paperback Aus$29.50 (+ Aus$8 surface mail). - S. G. Webb. The Willandra Lakes hominids. x + 194 pages, 122 plates, 13 figures. 1989. Canberra (ACT): Department of Prehistory, Research School of Pacific Studies, Australian National University: ISBN 0-7315-0802-5 paperback Aus$29.50 (+ Aus$8 surface mail)." Antiquity 65, no. 246 (March 1991): 156–58. http://dx.doi.org/10.1017/s0003598x00079473.

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31

Macgregor, Colin. "Preserving the Ancient Human Trackways Site in the Willandra Lakes World Heritage Area." Studies in Conservation, March 17, 2022, 1–6. http://dx.doi.org/10.1080/00393630.2022.2050616.

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32

Fitzsimmons, Kathryn E., and Sergey S. Gromov. "Northward expansion of the westerlies over glacial southeastern Australia: evidence from semi-arid lunette dunes, temperate basalt plains, and wind modelling." Frontiers in Earth Science 10 (July 26, 2022). http://dx.doi.org/10.3389/feart.2022.921264.

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Анотація:

It has long been hypothesized that the last glacial maximum (LGM) oversaw cold, arid, windy climates across southern Australia, and that these were driven by intensification and northward expansion of mid-latitude westerly circulation. Moreover, it was recently suggested that Australia experienced an extended LGM which began several millennia before the global peak. Aeolian sedimentary deposits provide key evidence for these hypotheses, and climate modelling an alternative means to test them. As yet, however, combined approaches to reconstructing glacial environments on the continent are scarce. Here we provide new evidence for westerly wind regimes across glacial southeastern Australia. We confirm active transverse lunette deposition at c. 29 ka and c. 23–19 ka in the semi-arid Willandra Lakes, and identify aeolian sand incursions to Spring Creek on the temperate Western Victorian Volcanic Plains from c. 29 ka. The Spring Creek deposits contain a surprising quantity of sand-sized quartz given the basalt setting, which we propose to be allochthonous and likely transported some distance. The site lies more than 50 km east and south of dunefields which were active at the same time and may have contributed sediment via long distance transport. We investigate the hypothesis for northward glacial expansion of westerly winds by combining our sediment records with aeolian particle transport simulations. We find that LGM near-surface winds were dominated by stronger, more focussed westerly air flow across southeastern Australia, compared with presently more diffuse wind regimes. Our results suggest stronger potential for LGM eastward distal sand transport onto the basalt plains, coeval with enhanced aeolian activity in the semi-arid Australian dunefields. Our combined reconstruction of aeolian deposition and trajectory modelling confirms the extended LGM hypothesis and indicates a northward migration of westerly winds over southeastern Australia during this period.

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