Sedimentary Processes During the Late Quaternary Across The

Total Page:16

File Type:pdf, Size:1020Kb

Sedimentary Processes During the Late Quaternary Across The YOF o z n ( Sedimentary processes during the Late Quaterîary across the Kimberley Shelf, Northwest Australia. Kriton Glenn B.Sc. with Honours in Geology 1997 Australian National University Thesis submitted for the degree of Doctor of Philosophy in Geology and Geophysics THE UNIVERSITY OF ADELAIDE Department of Geology and Geophysics February 2004 TABLE OF CONTENTS Table of contents ll Abstract. xi Certification... .. xiii Acknowledgments. xiv Dedication. XV List of Acronyms.. .... xvi Chapter 1. Introduction 1.1 Setting 1 1.2 The Sahul Shell . 1 1.3 Thesis aim... 8 1.4 Bathymetric nomenclature... 9 I .5 Large-scale bathyrnetric features. l0 1.6 Shelf terraces. 11 Chapter 2. Mapping...... .13 2.1.1 Previous Maritime Mapping History...... ..13 2.1.2 Marine geological mapping. ..11 2.7.3 Onshore geological mapping ...... .18 2.1.4 Industrial mapping t9 2.7.5 Mapping regional hydrocarbon seeps 27 2.1.6 Mapping the regional bathymetry.. 2l 2.2 Regional Structural Geology ...... 22 2.2.7 Margin Scale Basins. 22 2.2.2 Carbonate Reef Development.. ...... 24 2.2.3Tectonic setting: rates of subsidence.. 29 2.3 Oceanography.. .. 32 2.3. I Regional Oceanography. 32 2,3.2 Changes in Sea lævel. .........38 2.3.3 Oceanic Flow and Tectonics. ..........41 2.3.4 Tides .. ..........43 2.3.5 Sea surface currents. .......... 43 2.4 Climate. .. .......45 2.4.1 Climate Introduction. ..........45 11 2.4.2 Present Day Conditions ......, , 46 2.4.3 Cyclones... ...... ., ,49 2.4.4 Cyclone frequency. ,........49 2.4.5 Two examples of severe tropical cyclones 51 2.4.6 Atmospheric circulation 52 2.4.7 Climate change of the Late Pleistocene - Holocene 53 2.5 Water Balance Fluvial inputs. 58 2.5.1 Regional river flows. 58 2.5.2 Landsat Thermatic Mapper images. 60 2.6 Terrestrial inputs 64 2.6.1 Fluvial derived sediments. 64 2.6.2 Sediment Yield 66 2.7 Yegetation since the Last Glacial Maximum. 69 2.7.1 Changes in vegetation distribution 69 Chapter 3. Surface morphology and surficial sediments of the study area...J2 3.1 Surface Morphology...... ...12 3.2 Prcvious work. ,...76 3.3 Regional sediment facies of the Sahul Shelf. ,... 81 3.3.1 The shaved shelf. ....81 3.4 Sediments.... ...82 3.4.1 Setting: Energy levels. ....82 3 .4.2 Preservation of Skeletal Components . ....83 3.5 Introduction to the surficial sediments of this study 81 3.5.1 Methods; Laboratory Sampling Protocol..... 8l 3.5.1. 1 Digital Imagery. 81 3.5.1.2 Colour. 87 3.5.1.3 Sub-Sampling.... .......88 3.5.1.4. Sediment Description .......89 3.5.1.5 Microscopic Examination......, ,... .. 89 3.5.1.6 Recording observations.. ..... ...... .89 3.5.1.7 Descriptions...... ... ....90 3.4.1.8 Carbonate percentage analysis.. .......91 3.5.1.9 Grain size analysis..... ., ,... 92 3.5.1.10 Accelerator mass spectrometry dating 92 3.5.1.11 Carbon and oxygen isotope analysis...... 92 lll 3.6 Images and descriptions of the Kimberley Shelf surficial sediments...'94 3.7 Accelerator mass spectrometry dates. "" " "" 108 3.8 Terrestrial sediment contribution. ""'' 108 3.9 Results...... ....112 3.10 Sedimenttexture. ....:..' """"' 115 3.11 Total Organic Carbon. ' ' 116 Chapter 4 Sediment Core Observations and Supporting Data' .......t23 4.1 Introduction. ......123 4.2 Accelerator Mass Spectrometry Dating. ......123 4.2.1Method.... .. ...t23 4.2.2 Accelerator mass spectrometry results 4.3 Total Organic Carbon values of the sediment cores. 4.3.1 Method.... 4.3.2 T otal Organic Carbon Results. 4.4 Core Sediment Colour. 4.4.1 Method.... 4.4.2 Observations. 4.5 Core Sediment Character. 4.5.1 Methods... 4.5.2Wet sieve. 4.6 Sediment Summary...... 4.6.1 Summaly... 4.6.2 lnterpretation. 4.1 Core observations and supporting Data 4.7 .l Preface ... 4.7 .2 Core descriPtions...... 4.7.2.1 GravitY Core 001 4.1 .2.1.1 InterPretation... 4.7.2.2 GravitY Core 002 4.1.2.2.1 DescriPtion 4.7.2.3 GravitY Core 003 4.7 .2.3.1 InterPretation.. 4.1.2.4 GravitY Core 004. 4.7 .2.4.7 InterPretation .... 1V 4.7.2.5 Gravity Core 005 .....141 4.1 .2.5.1 Interpretation. ,....\47 4.7.2.6 Gravity Core 007. ..153 4.1 .2.6.7 Interpretation.... .. ... 153 4.7.2.7 Gravity Core 008. .....156 4.7 .2.7 .7 Interpretation.. .. ... 156 4.7.2.8 Gravity Core 10. ....158 4.1 .2.8.1 Interpretation.. ... 159 4.7.2.9 Gravity Core 015. .....r63 4.1 .2.9.1 Interpretation... .....164 Chapter 5 Bathyrnetric and Sub bottom profiles of the Kimberley Shelf. 166 5.1 Introduction. 166 r67 5.2 Bathymetry Methods... - 5.3 Bathymetric Results... .. 167 5.4 Sub-bottom Profiling Equipment and methods. t7t 5.5 General observations and Interpretation of the seismic sections. 176 5.5.1 Line 101... 176 5.5.2 Line207 '. 177 5.5.3 Line 301 ....:.. '.. 179 181 5.5.4 Line 401. 5.5.5 Seismic Summary ..... 782 5.6 The Kimberley Shelf-slope transect. 183 5.7 The Holocene inner shelf sedimentprism """"" 183 5.7 .l The near-shore area. r83 5.7.2 The 75 m-deep, mid-shelf terrace' 184 5.1.3 The 95 m-deep, outer mid-shelf terrace 184 186 5 .7 .3.1 Model for the Penguin Deeps barrier bar formation'''''''' " 5.7.4 The 112 m-deep outer shelf terrace. t87 5.8 Possible relict shorefaces. 188 5.8.1 Relict shoreface A. .... 188 5.8.2 Relict shoreface B. .... 189 5.9 Origins of Continental Shelf Terraces 191 5.9.1 The origins of a single, regional continental shelf surface.. 191 5.9.2 Continental margin terraces' r92 5.10 Evidence for recent glacio-eustasy... """""194 5.1 1 The terraces of the Sahul Shelf. " " " " " 195 5.11.1 The Sahul and Kimberley Shelf terraces. """"'195 5.11.2 A model for the submergent terraces on a subsiding shelf.. 198 5.11.3 Formation of a primary highstand platform. "' 198 5.11.4 Formation of succeeding regressive or lowstand platforms .. 199 5.1 1.5 Subaerial modification of pre-existing terraces ....... 200 5.11.6 Formation of subsequent highstand terrace. "' 200 5.17.7 Submarine modification of pre-existing terraces 201 5 . 1 1 . 8 The continuing cycle of terrace formation and modifi cation.2l2 5.12 Sea level at the Last Glacial Maximum (MIS 2). """'205 5.13 Discussion .........207 6 Summary. "209 7 Conclusions. ......214 References.. 216 List of figures Figure 1.1 Study Location .2 a Figure 1.2 Carbonate sediment on the Australian continental shelves... J Figure 1.3 The Sahul shelf, the range of bioherms on the shelf edge.... 6 7 Figure 1.4 Present day bathymelry.. Figure 2.1 Coronelli's 1696 map of the'Top End'Australia. """"'14 Figure 2.2The mapping the north of Australia, shoals and reeß' " " 14 Figure 2.3 Regional hydrocarbon exploration wells. ""' 20 Figure 2.4The Bonaparte and Browse Basins. .'.'."""" 22 Figure 2.5 The Bathymetric expression showing the major features. ....... ' 25 Figure 2.6 a,b,c. The model for the development of Bonaparte Shelf. ....... 26 Figure 2.7 Depo-centres and sediment pathways at times of lower SL.......29 Figure 2.8 Regional perspective of the Global Conveyor Belt.. ...... 32 Figure 2.9 The track of the Indonesian Throughflow.. ..... ... 33 Figure 2J0 and2.11. Regional Sea Surface Temperatures... 34 VI Figure 2.l2Themain Indonesian Throughflow gateways' ""' 35 Figure 2.13The Indonesian Throughflow Gateways... ''' "'"' 36 Figure 2.14 The main conduit between the islands of Sawu and Roti. .. .... 36 Figure 2.l5 Sea tævel change over the past 25000 years ' " " " ' 38 Figure2.16sealevelat -724m 70m andpresentday"' """" 40 Figure 2.77 Tectonic movements at 20 Ma moves to the north. ...... 4l Figure 2.18 Tectonics at 8 Ma. " " "" 42 Figure 2.19 Present day tectonics...' """"" 42 Figure 2.20Tidalregime of Troughton Island, Australia' """' 43 Figure 2.21 Prcvailing Surface Currents of the Bonaparte Shelf. ....44 Figure 2.22 Location map with Troughton Island andKupang..... .........45 Figure 2.23Rainfall of Troughton Island and Kupang (Indonesia).. ......46 Figure 2.24 Temperature of Troughton Island. """""' 41 Figure 2.25 The mean relative humidity, Troughton Island. ..... .. .. 48 Figure 2.26. MeanDaily Wind. ""' 48 Figure 2.27 Cyclone Thelma, category 5 over the Timor sea.. ......49 Figure 2.28. The occurrences of cyclones in the Australian region.......... 50 Figare 2.29 Tropical cyclone tracks in the Australian region, 1 970-80. 5 1 Figure 2.30 Trackof Tropical cyclone Thelma 6 - ll Dec 1 998. ...... .. 52 Figure 2.3l.Trackof tropical Cyclone Vance. ""'52 Figure 2.32Modernseasonalwindshifts. """""53 Figure 2.33TheTorres Strait, Australian. ''''''""' 54 Figure 2.34 Depositional settings, (a) At high SL and (b) at low SL.... ....56 Figure 2.35 Fluvial inputs to the study region...... " " ""' 59 Figure 2.36 Landsat TM, sediment plumes along the eastern Kimberley" ' 62 Figure 2.37 LandsatTMBand, I ..... ""'62 Figure 2.38 Landsat TM Band, 2...... ""'63 Figure 2.39 LandsatTMBand,3...... ""' 63 Figure 2.40 The Ord River Mouth. " " " " " 64 Figure 2.41 Onshore Geology of Northwest Australia ""65 Figve 2.42 The drainage basins and restricted lagoon during the LGM... 69 Figure 2.43 Yegetation during the LGM. " " " " "' 70 72 Figure 3. I . The regional bath¡rrnetry Australia's Northwest shelf Figure 3.2The seismic, gravity core and sediment sample sites.... .14 vlr Figure 3.3 Aplanviewof the'PenguinDeeps' """""75 Figure 3.4 The Penguin Fan. A, viewing from the west.- """"""75 B, Viewing from the east... """""15 Figure 3.5 Reefs, banks and shoals of the sahul shelf.
Recommended publications
  • Submarine Morphology of the Sahul Shelf, Northwestern Australia
    TJEERD H. VAN ANDEL JOHN J. VEEVERS SUBMARINE MORPHOLOGY OF THE SAHUL SHELF, NORTHWESTERN AUSTRALIA Abstract: The Sahul Shelf, located between north- of which it probably is the submerged extension. western Australia and the Timor Trough, consists This requires uplift, weathering, and denudation of a central basin surrounded by broad, shallow of the shelf in middle and late Tertiary. Subse- rises. Superimposed on the regional relief is a quently, the shelf was deformed to form the basin system of banks, terraces, and channels. The flat and rises. This deformation caused the original tops of banks and terraces form parts of several drainage to become antecedent. Lower surfaces regional, subhorizontal surfaces. The steplike to- were formed during Pleistocene low sea-level pography closely resembles the system of late stands. Cenozoic erosional surfaces on the adjacent land area with the shelf edge. The Sahul Rise sepa- Introduction rates the Bonaparte Depression from the Timor The Sahul Shelf, off the northwest coast of Trough. The basin is connected with deep Australia, is a very wide continental shelf water by a long, narrow valley with a maximum which derives its interest primarily from its depth of 200 m, Malita Shelf Valley. position between the continental mass of The shelf edge is represented by a gradual Australia and the island arches and geosynclines change in slope, usually marked by a low cliff of Indonesia. An early study, based on con- at 110-130 m. A second shelf edge at approxi- ventional nautical charts, was made by Fair- mately 550 m, reported by Fairbridge (1953), bridge (1953).
    [Show full text]
  • Predominant Colonization of Malesian Mountains by Australian Tree Lineages
    Received: 28 February 2019 | Revised: 30 September 2019 | Accepted: 7 October 2019 DOI: 10.1111/jbi.13747 RESEARCH PAPER Predominant colonization of Malesian mountains by Australian tree lineages Fabian Brambach1 | Christoph Leuschner1 | Aiyen Tjoa2 | Heike Culmsee1,3 1Plant Ecology and Ecosystems Research, University of Goettingen, Abstract Goettingen, Germany Aim: Massive biota mixing due to plate-tectonic movement has shaped the bioge- 2 Agriculture Faculty, Tadulako University, ography of Malesia and during the colonization process, Asian plant lineages have Palu, Indonesia 3DBU Natural Heritage, German Federal presumably been more successful than their Australian counterparts. We aim to gain Foundation for the Environment, Osnabrück, a deeper understanding of this colonization asymmetry and its underlying mecha- Germany nisms by analysing how species richness and abundance of Asian versus Australian Correspondence tree lineages in three Malesian subregions change along environmental gradients. Fabian Brambach, Biodiversity, Macroecology and Biogeography, Faculty We hypothesize that differing environmental histories of Asia and Australia, and their of Forest Sciences and Forest Ecology, relation to habitats in Malesia, have been important factors driving assembly pat- University of Goettingen, Buesgenweg 1, 37077 Goettingen, Germany. terns of the Malesian flora. Email: [email protected] Location: Malesia, particularly Sundaland, the Philippines and Wallacea. Funding information Taxon: Seed plants (trees). Deutsche Forschungsgemeinschaft,
    [Show full text]
  • Kimberley Marine Biota. History and Environment
    RECORDS OF THE WESTERN AUSTRALIAN MUSEUM 84 001–018 (2014) DOI: 10.18195/issn.0313-122x.84.2014.001-018 SUPPLEMENT Kimberley marine biota. History and environment Barry Wilson Research Associate, Department of Aquatic Zoology, Western Australian Museum, Locked Bag 49, Welshpool DC, Western Australia 6986, Australia. Email: [email protected] ABSTRACT – The remote tropical Kimberley region of Western Australia is introduced, its physical marine environment, habitats and classifi cation into bioregions are described, and its marine science history is summarised. An introduction to the ongoing Western Australian Museum marine biological survey program and its objectives are also provided. The geology, metocean conditions and climate of the region are summarised. A primary division of the Kimberley coastline is noted with a northern section dominated by Proterozoic meta-sedimentary and igneous rocks (Kimberley and Bonaparte Gulf Bioregions) and a southern section dominated by Mesozoic and Cainozoic sedimentary rocks (King Sound and Canning Bioregions). In the former section inner shelf seabed sediments overlying the inundated Yampi Plateau are principally of terrestrial origin while in the Canning Bioregion they are principally marine carbonates. On the middle and outer shelf (Oceanic Shoals and North West Shelf Bioregions) sediments are primarily marine carbonates. Along the shelf margin the water is clear and oligotrophic and subject to the Indonesian Through Flow current that originates in the western Pacifi c. The coastal zone is macrotidal, currents are predominantly tide driven and the coastal water is turbid and probably nutrient rich. These environmental differences and the different connectivity regimes account for distinctive offshore and coastal reef communities. KEYWORDS: marine flora, marine fauna, habitats, geology, ocean currents, climate, species distributions, biogeographic affi nities, IMCRA Bioregions, science history INTRODUCTION traditional lands in their care under the Healthy The Kimberley is the northernmost part Country program.
    [Show full text]
  • Surveys of the Sea Snakes and Sea Turtles on Reefs of the Sahul Shelf
    Surveys of the Sea Snakes and Sea Turtles on Reefs of the Sahul Shelf Monitoring Program for the Montara Well Release Timor Sea MONITORING STUDY S6 SEA SNAKES / TURTLES Dr Michael L Guinea School of Environment Faculty of Engineering, Health, Science and the Environment Charles Darwin University Darwin 0909 Northern Territory Draft Final Report 2012-2013 Acknowledgements: Two survey by teams of ten and eleven people respectively housed on one boat and operating out of three tenders for most of the daylight hours for 20 days and covering over 2500 km of ocean can only succeed with enthusiastic members, competent and obliging crew and good organisation. I am indebted to my team members whose names appear in the personnel list. I thank Drs Arne Rasmussen and Kate Sanders who gave their time and shared their knowledge and experiences. I thank the staff at Pearl Sea Coastal Cruises for their organisation and forethought. In particular I thank Alice Ralston who kept us on track and informed. The captains Ben and Jeff and Engineer Josh and the coxswains Riley, Cam, Blade and Brad; the Chef Stephen and hostesses Sunny and Ellen made the trips productive, safe and enjoyable. I thank the Department of Environment and Conservation WA for scientific permits to enter the reserves of Sandy Islet, Scott Reef and Browse Island. I am grateful to the staff at DSEWPaC, for facilitating and providing the permits to survey sea snakes and marine turtles at Ashmore Reef and Cartier Island. Activities were conducted under Animal Ethics Approval A11028 from Charles Darwin University. Olive Seasnake, Aipysurus laevis, on Seringapatam Reef.
    [Show full text]
  • The Discovery and Mapping of Australia's Coasts
    Paper 1 The Discovery and Mapping of Australia’s Coasts: the Contribution of the Dutch, French and British Explorer- Hydrographers Dorothy F. Prescott O.A.M [email protected] ABSTRACT This paper focuses on the mapping of Australia’s coasts resulting from the explorations of the Dutch, French and English hydrographers. It leaves untouched possible but unproven earlier voyages for which no incontrovertible evidence exists. Beginning with the voyage of the Dutch yacht, Duyfken, in 1605-6 it examines the planned voyages to the north coast and mentions the more numerous accidental landfalls on the west coast of the continent during the early decades of the 1600s. The voyages of Abel Tasman and Willem de Vlamingh end the period of successful Dutch visitations to Australian shores. Following James Cook’s discovery of the eastern seaboard and his charting of the east coast, further significant details to the charts were added by the later expeditions of Frenchmen, D’Entrecasteaux and Baudin, and the Englishmen, Bass and Flinders in 1798. Further work on the east coast was carried out by Flinders in 1799 and from 1801 to 1803 during his circumnavigation of the continent. The final work of completing the charting of the entire coastline was carried out by Phillip Parker King, John Clements Wickham and John Lort Stokes. It was Stokes who finally proved the death knell for the theory fondly entertained by the Admiralty of a great river flowing from the centre of the continent which would provide a highroad to the interior. Stokes would spend 6 years examining all possible river openings without the hoped- for result.
    [Show full text]
  • Adec Preview Generated PDF File
    Rec. West. Aust. M"... Suppl. No. 44.1993 Part 1 Historical background, description of the physical environments of Ashmore Reef and eartier Island and notes on exploited species P.F. Berry* Abstract Ashrnore Reef (12°17'S, 123°02'E) and nearby Cartier Island (l2°32'S, 123°33'E) are located on tl.e north-western extremity of the Sahul Shelf. They are approximately 350 km off the Kimberley coast of Australia and 145 km from Roti, Indonesia. The morphology and physical environments of the two reef systems are briefly described as a background to faunal inventories presented in Parts 2-7 ofthis publication. Ashrnore Reef (approximately 26 km long and 14 km wide) is similar in general shape and morphology to other shelf-edge atolls off the north-western coast of Australia, but because of the larger breaks in the reef there is no impounding of water in the lagoon on outgoing tides as at the Rowley Shoals and to a lesser extent, Scott Reef. There are three vegetated islets on Ashmore Reef. Cartier Island, an unvegetated sand cay, is surrounded by an oval-shaped reef platform approximately 4.5 km long by 2.3 km wide. Mean sea surface temperatures range from approximately 24°C in July and August to 30°C between January and March. Spring and neap tidal ranges (semi-diurnal) are 4.7 m and 2.8 m respectively. Observations on species exploited in the traditional Indonesian fishery are recorded. These suggest that composition and abundance of exploited species at Ashmore Reef and Cartier Island reflect a higher level of fishing effort there than at Scott Reef and Rowley Shoals.
    [Show full text]
  • Rainbowfishes (Melanotaenia: Melanotaeniidae) of the Aru Islands, Indonesia with Descriptions of Five New Species and Redescription of M
    aqua, International Journal of Ichthyology Rainbowfishes (Melanotaenia: Melanotaeniidae) of the Aru Islands, Indonesia with descriptions of five new species and redescription of M. patoti Weber and M. senckenbergianus Weber Gerald R. Allen1, Renny K. Hadiaty2, Peter J. Unmack3 and Mark V. Erdmann4,5 1) Western Australian Museum, Locked Bag 49, Welshpool DC, Perth, Western Australia 6986. E-mail: [email protected] 2) Museum Zoologicum Bogoriense (MZB), Division of Zoology, Research Centre for Biology, Indonesian Institute of Sciences (LIPI), Jalan Raya Bogor Km 46, Cibinong 16911, Indonesia. 3) Institute for Applied Ecology and Collaborative Research Network for Murray-Darling Basin Futures, University of Canberra, ACT 2601, Australia. 4) Conservation International Marine Program, Jl. Dr. Muwardi No. 17, Renon, Denpasar 80235, Bali, Indonesia. 5) California Academy of Sciences, Golden Gate Park, San Francisco, CA 94118, USA. Received: 02 November 2014 – Accepted: 08 March 2015 Abstract (14.1-75.6 mm SL) specimens respectively, collected at The Aru Archipelago is a relict of the former land bridge Kola, Kobroor, and Wokam islands. They comprise a connecting Australia and New Guinea and its freshwater close-knit group allied to the “Goldiei” group (along with Melanotaenia strongly reflect this past connection. Sea lev- M. senckenbergianus), but are differentiated on the basis of el changes over the past 2-3 million years have apparently live colour patterns and various genetic, morphometric, provided sufficient isolation for the radiation of a mini- and meristic features. species flock consisting of at least seven species. Melanotae- nia patoti and M. senckenbergianus were described from the Zusammenfassung islands by Weber in the early 1900s, but subsequently con- Das Aru-Archipel ist ein Überbleibsel der früheren Land- sidered as junior synonyms of the New Guinea mainland brücke zwischen Australien und Neuguinea, die Süßwasser- species M.
    [Show full text]
  • MASARYK UNIVERSITY BRNO Diploma Thesis
    MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský MASARYK UNIVERSITY BRNO FACULTY OF EDUCATION DEPARTMENT OF ENGLISH LANGUAGE AND LITERATURE Presentation Sentences in Wikipedia: FSP Analysis Diploma thesis Brno 2018 Supervisor: Author: doc. Mgr. Martin Adam, Ph.D. Bc. Lukáš Opavský Declaration I declare that I have worked on this thesis independently, using only the primary and secondary sources listed in the bibliography. I agree with the placing of this thesis in the library of the Faculty of Education at the Masaryk University and with the access for academic purposes. Brno, 30th March 2018 …………………………………………. Bc. Lukáš Opavský Acknowledgements I would like to thank my supervisor, doc. Mgr. Martin Adam, Ph.D. for his kind help and constant guidance throughout my work. Bc. Lukáš Opavský OPAVSKÝ, Lukáš. Presentation Sentences in Wikipedia: FSP Analysis; Diploma Thesis. Brno: Masaryk University, Faculty of Education, English Language and Literature Department, 2018. XX p. Supervisor: doc. Mgr. Martin Adam, Ph.D. Annotation The purpose of this thesis is an analysis of a corpus comprising of opening sentences of articles collected from the online encyclopaedia Wikipedia. Four different quality categories from Wikipedia were chosen, from the total amount of eight, to ensure gathering of a representative sample, for each category there are fifty sentences, the total amount of the sentences altogether is, therefore, two hundred. The sentences will be analysed according to the Firabsian theory of functional sentence perspective in order to discriminate differences both between the quality categories and also within the categories.
    [Show full text]
  • Environmental Health Australia
    Environmental Health The Journal of the Australian Institute of Environmental Health ...linking...linking thethe sciencescience andand practicepractice ofof EnvironmentalEnvironmental HealthHealth Environmental Health The Journal of the Australian Institute of Environmental Health ABN 58 000 031 998 Advisory Board Ms Jan Bowman, Department of Human Services, Victoria Professor Valerie A. Brown AO, University of Western Sydney Dr Nancy Cromar, Flinders University Associate Professor Heather Gardner Mr Murray McCafferty, Acting Company Secretary, Australian Institute of Environmental Health Mr John Murrihy, Bayside City Council, Victoria and Director, Australian Institute of Environmental Health Mr Ron Pickett, Curtin University Dr Eve Richards, TAFE Tasmania Dr Thomas Tenkate, Queensland Health Editor Associate Professor Heather Gardner Editorial Committee Dr Ross Bailie, Menzies School of Health Research Mr Dean Bertolatti, Curtin University of Technology Mr Peter Davey, Griffith University Ms Louise Dunn, Swinburne University of Technology Professor Christine Ewan, University of Wollongong Associate Professor Howard Fallowfield, Flinders University Ms Jane Heyworth, University of Western Australia Mr Stuart Heggie, Tropical Public Health Unit, Cairns Dr Deborah Hennessy, Developing Health Care, Kent, UK Professor Steve Hrudey, University of Alberta, Canada Professor Michael Jackson, University of Strathclyde, Scotland Mr Ross Jackson, Maddock Lonie & Chisholm, Melbourne Mr Steve Jeffes, TAFE Tasmania Mr Eric Johnson, Department of Health
    [Show full text]
  • Mineralization and Geology of the North Kimberley
    GEOLOGICAL SURVEY OF WESTERN AUSTRALIA REPORT 85 PLATE 1 è00 è25 128^30' è50 è75 129^00' å00 å25 127^30' å50 å75 128^00' ê00 REFERENCE ä25 126^30' ä50 ä75 127^00' 13^30' 126^00' ä00 13^30' q Quartz veins, of various ages; youngest post-dates Devonian q æåKk KEEP INLET FORMATION: deltaic sandstone, pebbly sandstone, mudstone, and minor coal æW Weaber Group: sandstone, limestone, and minor conglomerate, shale, and siltstone ðê00 ðê00 æL Langfield Group: sandstone, limestone, shale, and siltstone æåKk çma Limestone reef complexes; oolitic, cyanobacterial, and stromatolitic limestones, and debris flow deposits; BASIN Group Kulshill marginal slope and basin facies of Famennian reef carbonate; includes PIKER HILLS FORMATION and NORTHERN BONAPARTE T I M O R S E A VIRGIN HILLS FORMATION Branch Banks æW çg Boulder, cobble, and pebble conglomerate; includes BARRAMUNDI CONGLOMERATE and STONY CREEK CONGLOMERATE çN Ningbing Group: limestone reef complexes; cyanobacterial limestone, limestone breccia, shale, and sandstone East Holothuria Reef EARLY æL çC Cockatoo Group: sandstone, conglomerate, and limestone; minor dolomite and siltstone çM Mahony Group: quartz sandstone, pebbly sandstone, and pebble to boulder conglomerate CARBONIFEROUS êéc Carlton Group: shallow marine sandstone, siltstone, shale, and stromatolitic dolomite Otway Bank Stewart Islands êG Goose Hole Group: sandstone, limestone, stromatolitic limestone, siltstone, and mudstone çma çg çN çM Troughton Passage êa Vesicular, amygdaloidal, and porphyritic basalt, and conglomerate and sandstone;
    [Show full text]
  • Great Southern Land: the Maritime Exploration of Terra Australis
    GREAT SOUTHERN The Maritime Exploration of Terra Australis LAND Michael Pearson the australian government department of the environment and heritage, 2005 On the cover photo: Port Campbell, Vic. map: detail, Chart of Tasman’s photograph by John Baker discoveries in Tasmania. Department of the Environment From ‘Original Chart of the and Heritage Discovery of Tasmania’ by Isaac Gilsemans, Plate 97, volume 4, The anchors are from the from ‘Monumenta cartographica: Reproductions of unique and wreck of the ‘Marie Gabrielle’, rare maps, plans and views in a French built three-masted the actual size of the originals: barque of 250 tons built in accompanied by cartographical Nantes in 1864. She was monographs edited by Frederick driven ashore during a Casper Wieder, published y gale, on Wreck Beach near Martinus Nijhoff, the Hague, Moonlight Head on the 1925-1933. Victorian Coast at 1.00 am on National Library of Australia the morning of 25 November 1869, while carrying a cargo of tea from Foochow in China to Melbourne. © Commonwealth of Australia 2005 This work is copyright. Apart from any use as permitted under the Copyright Act 1968, no part may be reproduced by any process without prior written permission from the Commonwealth, available from the Department of the Environment and Heritage. Requests and inquiries concerning reproduction and rights should be addressed to: Assistant Secretary Heritage Assessment Branch Department of the Environment and Heritage GPO Box 787 Canberra ACT 2601 The views and opinions expressed in this publication are those of the author and do not necessarily reflect those of the Australian Government or the Minister for the Environment and Heritage.
    [Show full text]
  • 1. Thesis Topic
    1. Thesis Topic This thesis is an archaeological study focused on identifying the gender of the anthropomorphic motifs depicted in the rock art assemblage of the northwest Kimberley region of Australia. 1.1 Introduction – What is sex? What is gender? The terms ‘sex’ and ‘gender’ are often thought to be of the same essence. The purpose of this chapter is to make the difference between the two terms clear and to explain their respective significance to the study of rock art. In brief, ‘sex’ refers to the biological differences: physicality – hormonal profiles, chromosomes and their consequence for the human body i.e. internal and external sex organs and development of hair and muscle. In contrast, ‘gender’ describes the characteristics that a particular society or culture allocates as masculine or feminine, so while in every culture your sex as male or female is a biological fact, what your sex means in terms of your gender role as a ‘man’ or a ‘woman’ in society can be quite different cross culturally (Gross 1992:334-5). A ‘real man’ or ‘real woman’, therefore, requires male or female sex plus characteristics and behaviours ascribed by a particular culture as appropriate to those sexes. The resultant ‘gender roles’ have an effect on the individual’s societal position, their access to resources, their power of production and on their health (Hays-Gilpin 2009:336). Still, there is debate as to the worth of the term ‘gender’ when it is so closely related to the sex of an individual (Laqueur 1992). Nonetheless, it is clear that characteristics and behaviours of gender are ascribed dissimilarly across cultures to individuals physically marked as male, female and, more rarely to the intersexed.
    [Show full text]