Fluvial Sediment Supply to the North-East Queensland Coast,Australia

Rivers play a dominant role in supplying sediment to the mainly siliceous sandy north-east Queensland coast. The interaction of geology and the seasonally wet tropical climate in the coastal catchments results under natural conditions in a high, but seasonally variable river discharge and sediment yield. These are examined in the sample catchments of the Barron, Mulgrave-Russell and Burdekin Rivers Peak sediment delivery occurs with major river floods produced by tropical cyclones. The initial erosive impact of these floods and subsequent constructional effects are examined along the Burdekin and Barron delta coasts. Human interference in the coastal catchments has caused increased sediment yield especially with extensive clearance of tropical rainforest and with some agricultural practices; but when dams and weirs trap sediment and sand is extracted from river beds a decrease occurs.     

Documenting and Analyzing Rock,Paintings from Torres Strait,NE Australia,with Digital Photography and Computer Image Enhancement

Abstract

The deterioration of rock-art over time is an important concern for indigenous communities, archaeologists, rock-art researchers, and cultural heritage managers. Computer enhancement has emerged as an important tool in viewing poorly visible rock paintings. While most studies regarding this technique explore the methods associated with computer enhancement there is little discussion of the results that can be generated beyond the recovery of images. This article presents results from the application of computer enhancement methods to rock paintings from the Torres Strait region in NE Queensland. The results obtained through the computer enhancement of deteriorated rock paintings are used to reveal degrees of preservation, interregional interaction, and previously undocumented spatial patterning across the strait.     

Wenlock brachiopods from Canberra,Australia

Twenty-four brachiopod species are described from a well-preserved shelly fauna in the Walker Volcanics, collected from the Molonglo valley west of Canberra. There are three inarticulates and twenty-one articulates, of which nine are new, three are closely compared with previously described species and twelve are under open nomenclature. New are Skenidioides thrinax, Salopina mediocostata, Aegiria (Epelidoaegiria subgen. nov.) chilidifera, Morinorhynchus oepiki, Australina (Australina) kausi, Coelospira cavata, Endospirifer anxius, Reticulariopsis silurica and Vadum (gen. nov.) coppinsense. The fauna is shown to be cosmopolitan in character and falls within the scope of Benthic Assemblages 3 to 5 of Boucot (1975). It is of Wenlock age.     

Kincentric Ecology,Species Maintenance and the Relational Power of Place in Northern Australia

This paper considers themes of species maintenance and place engagement in Yanyuwa country, northern Australia. It traces the complexity of interpretations and relational contexts involved in places that are commonly – and we argue – misleadingly, referred to as increase and magic sites. Examining one specific place, at which people carry out maintenance rituals, we explore the complex bonds that unite Yanyuwa with the geography that is the Ancestral Hill Kangaroo. Not content with the classificatory habit of declaring actions either increase oriented or hunting magic, this research more fully explicates the relational substance of places that play a key role in ecological health. This is achieved by asking how might the profundity of a place of relational importance, such as a maintenance site, be better understood and written of in ways that convey an Indigenous ontology and epistemology?     

An Independent Confirmation of the 4 ka Antiquity of a Beeswax Figure in Western Arnhem Land,Northern Australia

Critical to any chronology is reliability in the determination of age for a distinctive artefact that is related to other components in a series. Therefore, the independent testing and verification of the antiquity of an apparent anomalous measurement for an old beeswax figure in northern Australia is of fundamental interest in rock art studies. Replication of the radiocarbon dating process has confirmed that one exceptional figure in early X‐ray style at the Gunbilngmurrung site in western Arnhem Land is indeed c. 4–4.5 ka. The result also confirms the great antiquity of paintings over which the beeswax was applied.     

Hydrothermal fluid flow models of stratiform ore genesis in the McArthur Basin, Northern Territory, Australia

This paper explores the role of basin‐scale fluid migration in stratiform Pb–Zn ore formation in the southern McArthur Basin, Australia. Mathematical models are presented for coupled brine migration and heat transport in the basin. The models account for: (i) topographically driven flow (forced convection) during periods when parts of the McArthur Basin were subaerial and elevated above the central Batten Fault Zone; (ii) density‐driven flow (free convection) during periods when the basin was mostly submarine; and (iii) transient flows associated with fault rupture during periods of transpression. These hydrologic models help to compare and contrast a variety of hypotheses concerning deep fluid migration and the origin of base metal ores in the McArthur Basin. The numerical results exhibit a strong structural control on fluid flow caused by the north‐trending fault systems that characterize the Batten Fault Zone. As a result, fluids descend to depths of a few kilometers along the western side, migrate laterally to the east through the clastic and volcanic aquifers of the upper Tawallah and lowest McArthur Groups, and then ascend along the eastern side of the fault zone. This recharge–discharge pattern dominates all of the hydrogeologic models. The basin‐wide flow pattern suggests that Na–Ca–Cl brines acquired base metals in the deepest levels of the basin stratigraphy as the fluids migrated eastwards through the aquifer system. Upward flow was relatively rapid along the Emu Fault Zone, so much so that fluid temperatures likely approached 130°C in the muddy sediments near the sea floor due to upward flow and venting at the HYC (‘Here’s Your Chance'). Transient pulses of flow characterized periods of transpressional stress and subsequent faulting may have punctuated the basin history. Large‐scale free convection, however, characterized notably long periods of diagenesis and ore mineralization during the Proterozoic in the McArthur Basin.     

Microseismic Signal Spectra,Energy Characteristics,and Fractal Features Prior to Rock Burst: A Case Study from the Qianqiu Coal Mine,China

Microseismic (MS) technology has been widely adopted for monitoring coal and rock dynamic disasters. Insights into MS wave characteristics contribute to the accurate prediction of these disasters. In this study, MS wave characteristics were analysed from three aspects: the signal spectra, wavelet packet energy and fractal features. It is shown that prior to the rock burst, the MS wave main frequency decreased following a power law, the amplitude linearly increased, the wavelet packet energy tended to become concentrated on the low frequency bands, and the correlation dimension decreased. When the rock burst occurred, the MS wave main frequency, wavelet packet energy and correlation dimension declined to their lowest levels. Meanwhile, the amplitude rose to a maximum. Therefore, the MS wave characteristics in this study were found to effectively identify and extract precursor information of value for predicting rock dynamic disasters.     

Boats on Bark: an Analysis of Groote Eylandt Aboriginal Bark-Paintings featuring Macassan Praus from the 1948 Arnhem Land Expedition, Northern Territory, Australia

This paper examines a group of Aboriginal bark-paintings featuring Macassan prau s that were collected in 1948 during the American-Australian Scientific Expedition to Arnhem Land. These paintings were studied in an effort to understand issues related to Aboriginal and Macassan cross-cultural interaction, stylistic adaptation and change, and maritime technologies. Furthermore it is one example in which the collaborative efforts of maritime and Indigenous archaeologies can achieve a more holistic technological and stylistic cross-analysis of watercraft imagery.
© 2009 The Authors     

First fossil pollen record of the Northern Hemisphere species Aglaoreidia cyclops Erdtman, 1960 in Australia

Sánchez Botero, C.A., Oboh-Ikuenobe, F.E. & Macphail, M.K., 2013. First fossil pollen record of the Northern Hemisphere species Aglaoreidia cyclops Erdtman, 1960 in Australia. Alcheringa 37, 1–5. ISSN 0311-5518.

Aglaoreidia cyclops Erdtman, 1960 is a fossil pollen species associated with upper Eocene to lower Oligocene freshwater deposits in Europe and North America. Specimens preserved in upper Eocene lignites near Norseman, Western Australia, are the first record of this Northern Hemisphere species both in Australia and the Southern Hemisphere. This new report widens the biogeographic distribution originally considered for this species. The stratigraphical and environmental characteristics of A. cyclops also make it an excellent stratigraphic indicator of upper Eocene freshwater deposits in Western Australia.

Carlos A. Sánchez Botero [casmwc@mail.mst.edu], Francisca E. Oboh-Ikuenobe [ikuenobe@mst.edu] Department of Geological Sciences and Engineering, Missouri University of Science and Technology, 129 McNutt Hall, Rolla, MO 65409, USA; Mike Macphail [mike.macphail@anu.edu.au] Department of Archaeology and Natural History, College of Asia and the Pacific, Australian National University Canberra, ACT 0200, Australia. Received 12.10.2012; revised 6.3.2013; accepted 7.3.2013.     

The Food Remains from Casselden Place, Melbourne, Australia

This paper discusses the faunal, shell, and botanical remains from Casselden Place with the aim of investigating consumption and dietary patterns at the site during the nineteenth and early twentieth centuries. Each of the major food sources are discussed in detail with reference to historical records regarding the price of various supplies and their availability at the time.     

Becoming the State in Northern Australia: Urbanisation,Intra‐Indigenous Relatedness,and the State Effect

In Australia's Northern Territory, the Larrakia have been involved in a decades‐long effort to gain recognition as traditional owners through Land Rights and Native Title legislation. From one perspective, their claims have failed to achieve the entitlement and recognition grounded in these governmental regimes (Scambary 2007; Povinelli 2002). However, over the past decade the Larrakia Nation Aboriginal Corporation (LNAC) and the Larrakia Development Corporation (LDC) have emerged as locally powerful corporate bodies that pursue programs and exercise forms of power on behalf of the Larrakia that can be understood in terms of state and governmental practice. Through suburban development, a night patrol, educational and vocational training, a radio station, and through forms of policy research and statistical enumeration, the Larrakia nation have emerged in the eyes of many as a de facto Aboriginal ‘state’ in the Darwin region. This paper explores the intra‐Indigenous relations through which these practices have emerged, and analyses the extent to which the LNAC might be understood as a kind of ‘state’ within a state, responsible for world‐shaping activities of knowledge production, housing and health outreach, vocational training and education, and policing. Focussing on the forms of ‘stateness’ that accrue to the Larrakia Nation in Darwin through its policing, knowledge production, and outreach programs for Aboriginal campers, the article explores the differential articulation of Aboriginal groups with the state. It concludes by asking how such differences matter in contexts of planned urbanisation in the Northern Territory.     

Ordovician acritarchs from the Canning Basin,Western Australia

A left mandibular toothplate of a chimaeroid fish collected from the Toolebuc Formation (Early Cretaceous, Albian), central Queensland is described. Comparisons with other chimaeroid genera show the toothplate to be sufficiently distinct to warrant the erection of a new genus. Ptyktoptychion tayyo gen. et sp. nov. is distinguished by the size and shape of its three tritors, the form of the symphysial facet and the overall shape of the toothplate.     

Oligocene-Miocene calcareous nannofossils from the Torquay Basin,Victoria, Australia

Oligocene-Miocene rocks of the Torquay Basin contain at least 55 different species of calcareous nannofossils. These species allow zonation of an offshore subsurface section (Nerita No. 1 Well) and two onshore sections (near Torquay). The Angahook Formation and the base of the Jan Juc Formation in the Nerita No. 1 Well belong to Martini's (1971) NP 22 calcareous nannofossil Zone (early Oligocene). The NP 23 Zone could not be identified with certainty, but Zones NP 24/25 (late Oligocene) to NN 2 (early Miocene) were recognized in the Jan Juc Formation. The Oligocene-Miocene boundary is present between 122 m and 135 m below the sea floor at this site. The Puebla Formation, exposed at the sea floor, contains NN 5 spanning the early-middle Miocene boundary.

Onshore along the Torquay coast, NP 24/25 (late Oligocene) is present in the Angahook Formation; the Jan Juc Formation at Bird Rock also contains NP 24/25, except the uppermost 2.5 m which belongs to NN 1. The NN 2 Zone begins at the contact between the Jan Juc and Puebla Formations and continues upward for at least 3 m. After a covered interval, NN 4 was identified 10 m above the contact. The Oligocene-Miocene boundary is placed at the base of the hard band capping Bird Rock in the type section of the Jan Juc Formation.

Nannofossil assemblages in the Torquay sections suggest deposition in cool, shallow continental shelf waters. The assemblages in Nerita No. 1 Well also suggest cool shelf waters, although deeper than at Torquay.     

Soanian cores and core-tools from Toka,Northern India: Towards a new typo-technological organization

Since the initial ‘discovery’ and explanation of the Soanian industry by H. de Terra and T.T. Paterson in the 1930s, multiple interpretations have been offered by various investigators on its chronology, geographical distribution, relationship with the Acheulian, and technological progression. In most cases, the presence of explicit tool-types and the absence of Acheulian bifaces were the distinguishing features utilized to recognize the industry as well as delineate its technological development through time and space. However, in light of recent intra-regional geoarchaeological investigations and the analyses of a large surface assemblage by the author, the existing framework for Soanian typology is in need of judicious revision. In this paper, some of the methodological and interpretative problems are briefly discussed from a historical perspective and the technological organization of cores and core-based tools from Toka, a rich factory site, is described. Essentially, the Toka assemblage comprises a dynamic range of non-biface tool-types on quartzite, which possess varying patterns of core reduction techniques, edge retouch, and associated use-wear. The study also introduces a modified typological classification of specific chopper morphologies, which may be broadly applicable in global context.     

A post-contact Aboriginal mortuary tree from southwestern Victoria,Australia

Abstract

Here we document the investigation of the first Australian Aboriginal mortuary tree found since the early 20th century and the first studied by archaeologists and Aboriginal traditional owners. In 2001, a landowner discovered Aboriginal skeletal remains inside a fallen, dead tree while evaluating the tree’s potential as firewood, leading to the investigation of the site. The tree was located near Moyston, in southwestern Victoria, in traditional Djab Wurrung country and held the partial skeletons of three Aboriginal individuals—two adults and a child. Clay pipe-stem wear on several teeth belonging to the two adults indicates that these remains were broadly contemporaneous secondary placements from the early post-contact period (ca. a.d. 1835–1845). Along with five additional mortuary trees within 30 km of the Moyston tree, this practice constitutes a previously unknown traditional mortuary pattern and contributes to our understanding of the complex mortuary behavior of the Aboriginal people of southwestern Victoria.     

Middle Ordovician brachiopods from the Stairway Sandstone,Amadeus Basin,central Australia

Jakobsen, K.G., Brock, G.A, Nielsen, A.T., Topper, T.P. & Harper, D.A.T., 2013. Middle Ordovician brachiopods from the Stairway Sandstone, Amadeus Basin, central Australia. Alcheringa. ISSN 0311–5518.

Middle Ordovician brachiopod faunas from the Amadeus Basin, central Australia are poorly known. The Darriwilian Stairway Sandstone was sampled stratigraphically for macrofossils in order to provide new information on marine benthic diversity in this clastic-dominated, shallow-water palaeoenvironment along the margin of northeastern Gondwana. The brachiopods from the Stairway Sandstone are of low diversity and represent ca 9% of the entire shelly fauna. Five brachiopod taxa are described from the Stairway Sandstone; all are endemic to the Amadeus Basin at species level. Two new species, Amadeuphyla joanae gen. et sp. nov. and Paralenorthis luritjaorum sp. nov., are described. Unweighted cladistic analysis based on 20 characters places the new genus Amadeuphyla within the Taffinae.

Kristian G. Jakobsen [kgjakobsen@snm.ku.dk] Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen, Denmark & Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia. Glenn A. Brock [glenn.brock@mq.edu.au] Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia. Arne T. Nielsen [arnet@snm.ku.dk] Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen, Denmark. Timothy P. Topper [timothy.topper@snm.ku.dk] Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen, Denmark. David A. T. Harper [david.harper@durham.ac.uk] Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Copenhagen, Denmark & Department of Earth Sciences, Durham University, Durham, UK. Received 14.6.2013; revised 25.9.2013; accepted 8.10.2013.