Limmen Bight: Marine and Coastal Biodiversity Values
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GEOG 101 PLACE NAME LIST for EXAM THREE
GEOG 101 PLACE NAME LIST for EXAM THREE Each exam will have a place name location map section based on the list below, plus countries and political units. Consult the appropriate maps in the atlas and textbook to locate these places. The atlas has a detailed INDEX. Exam III will focus on place names from Asia and Oceania. This section of the exam will be in the form of a matching question. You will match the names to numbers on a map. ________________________________________________________________________________ I. CONTINENTS Australia Asia ________________________________________________________________________________ II. OCEANS Pacific Indian Arctic ________________________________________________________________________________ III. ASIA Seas/Gulfs/Bays/Lakes: Caspian Sea Sea of Japan Arabian Sea South China Sea Red Sea Aral Sea Lake Baikal East China Sea Bering Sea Persian Gulf Bay of Bengal Sea of Okhotsk ________________________________________________________________________________ Islands: New Guinea Taiwan Sri Lanka Singapore Maldives Sakhalin Sumatra Borneo Java Honshu Philippines Luzon Mindanao Cyprus Hokkaido ________________________________________________________________________________ Straits/Canals: Str. of Malacca Bosporas Dardanelles Suez Canal Str. of Hormuz ________________________________________________________________________________ Rivers: Huang Yangtze Tigris Euphrates Amur Ob Mekong Indus Ganges Brahmaputra Lena _______________________________________________________________________________ Mountains, Plateaus, -
Mcarthur Basin Geology and Mineral Resources of the Northern Territory
Geology and mineral resources of the Northern Territory Ahmad M and Munson TJ (compilers) Northern Territory Geological Survey Special Publication 5 Chapter 15: McArthur Basin BIBLIOGRAPHIC REFERENCE: Ahmad M, Dunster JN and Munson TJ, 2013. Chapter 15: McArthur Basin: in Ahmad M and Munson TJ (compilers). ‘Geology and mineral resources of the Northern Territory’. Northern Territory Geological Survey, Special Publication 5. Disclaimer While all care has been taken to ensure that information contained in this publication is true and correct at the time of publication, changes in circumstances after the time of publication may impact on the accuracy of its information. The Northern Territory of Australia gives no warranty or assurance, and makes no representation as to the accuracy of any information or advice contained in this publication, or that it is suitable for your intended use. You should not rely upon information in this publication for the purpose of making any serious business or investment decisions without obtaining independent and/or professional advice in relation to your particular situation. The Northern Territory of Australia disclaims any liability or responsibility or duty of care towards any person for loss or damage caused by any use of, or reliance on the information contained in this publication. McArthur Basin Current as of Dec 2010 Chapter 15: McARTHUR BASIN M Ahmad, JN Dunster and TJ Munson INTRODUCTION The basin has been modelled as several north-trending asymmetric rifts or grabens separated by northwest- The Palaeo- to Mesoproterozoic McArthur Basin is exposed trending faults and transverse ridges. Previous workers over an area of about 180 000 km2 in the northeastern NT. -
Natural Values and Resource Use in the Limmen Bight
NATURAL VALUES AND RESOURCE USE IN THE LIMMEN BIGHT REGION © Australian Marine Conservation Society, January 2019 Australian Marine Conservation Society Phone: +61 (07) 3846 6777 Freecall: 1800 066 299 Email: [email protected] PO Box 5815 West End QLD 4101 Keep Top End Coasts Healthy Alliance Keep Top End Coasts Healthy is an alliance of environment groups including the Australian Marine Conservation Society, the Pew Charitable Trusts and the Environment Centre of the Northern Territory. Authors: Chris Smyth and Joel Turner, Centre for Conservation Geography Printing: Printed on 100% recycled paper by IMAGE OFFSET, Darwin. Maps: Centre for Conservation Geography This report is an independent research paper prepared by the Centre for Conservation Geography commissioned by, and for the exclusive use of, the Keep Top End Coasts Healthy (KTECH) alliance. The report must only be used by KTECH, or with the explicit permission of KTECH. The matters covered in the report are those agreed to between KTECH and the authors. The report does not purport to consider exhaustively all values of the Limmen Bight region. The authors do not accept liability for any loss or damage, including without limitation, compensatory, direct, indirect, or consequential damages and claims of third parties that may be caused directly or indirectly through the use of, reliance upon or interpretation of the contents of the report. Cover photos: Main - Limmen River. Photo: David Hancock Inset (L-R): Green Turtle, Recreational fishing is an important leisure activity in -
Springs of the Mataranka Area 4
THE BIG PICTURE SPRINGS OF THE MATARANKA AREA 4. THE SWAMP Timor Sea A cavernous limestone aquifer extends The large swampy area located on the south side of across a large part of the Northern Territory the Roper River also owes it’s existence to a and into Queensland. The springs at The Mataranka area is notable for its many springs. geological structure that has caused the aquifer to DARWIN Mataranka are one of several outlet points for become shallower and to thin out towards the Roper the aquifer. Other big springs are found on 295000mE This map shows the location of the main springs and other groundwater discharge features. River (see the cross-section). This has resulted in a the Flora, Katherine and Daly Rivers and in broad area underlain by a shallow watertable and Queensland on the Lawn Hill Creek and It explains why the springs are there and describes some of their characteristics. zones of seepage. Extensive tufa deposits formed there because a ridge of bedrock located downstream Daly River Springs KATHERINE Gulf Gregory River. At Mataranka the water of originates from areas to the southeast as far of the seepage zone, ponded the water in a similar Flora River Springs MATARANKA Carpentaria away as the Barkly Tablelands and from the manner to the rock bars in streams as described in 300000mE northwest as far as the King River. Qa1 the note on tufa formation. The ridge formed a base for tufa to accumulate. Tufa dams merged and grew - Waterhouse Cmt over older ones, eventually forming a continuous sheet of limestone. -
Geog 120: World Geography American University of Phnom Penh
Geog 120: World Geography American University of Phnom Penh Map Quizzes: List of physical features 1. Africa Atlas Drakensberg Seas and Oceans Deserts Mediterranean Atlantic Kalahari Strait of Gibraltar Namib Suez Canal Sahara Mozambique Channel Ogaden Red Sea Libyan Gulf of Suez 2. Asia Lakes Lake Chad Seas and Oceans Lake Malawi (Nyasa) Lake Tanganyika Andaman Sea Lake Victoria Arabian Sea Lake Albert Aral Sea Lake Rudolph Arctic Ocean Atlantic Ocean Rivers Black Sea Caspian Sea Congo East China Sea Limpopo Indian Ocean Niger Inland Sea (also know as Setonaikai, Zambezi Japan) Nile Mediterranean Sea Orange Pacific Ocean Vaal Red Sea Sea of Japan Mountains Sea of Okhotsk 2 South China Sea Mountain Ranges Yellow Sea Caucuses Elburz Straits, Channels, Bays and Gulfs Himalayas Hindu Kush Bay of Bengal Ural Bosporus Zagros Dardanelles Gulf of Aden Gulf of Suez Deserts Gulf of Thailand Arabian Gulf of Tonkin Dasht-E-Kavir Persian Gulf Gobi Strait of Taiwan Negev Strait of Malacca Takla Makan Strait of Hormuz Strait of Sunda Suez Canal 3. The Americas Lakes Seas and Oceans Baykal Bering Tonle Sap Caribbean Sea Atlantic Ocean Pacific Ocean Rivers Straits, Channels, Bays and Gulfs Amur Brahmaputra Gulf of Mexico Chang Jiang Hudson Bay Euphrates Panama Canal Ganges Strait of Magellan Huang He (Yellow) Indus Lakes Irrawaddy Mekong Great Salt Tigris Great Lakes (Lakes Tonle Sap (River and Lake) Superior, Michigan, Huron, 3 Erie, and Ontario) 4. Australia and the Pacific Manitoba Titicaca Winnipeg Seas and Oceans Coral Sea Rivers Tasman Sea Pacific Ocean Amazon Indian Ocean Colorado Columbia Hudson Straits, Channels, Bays and Gulfs Mississippi Bass Strait Missouri Cook Strait Ohio Gulf of Carpentaria Orinoco Torres Strait Paraguay Plata Parana Rivers Rio Grande Darling St. -
A New Freshwater Catfish (Pisces: Ariidae) from Northern Australia
Rec. West. Aust. Mus. 1988,14(1): 73-89 A new freshwater catfish (Pisces: Ariidae) from northern Australia PatriciaJ. Kailola* and Bryan E. Pierce* Abstract A new species of fork-tailed catfish is described on the basis of 31 specimens collected in northern Australia between the Fitzroy River (Western Australia) and the Mitchell River (Queensland). Arius midgleyi sp. novo grows to at least 1.3 m TL and is distinguished from other Australo-Papuan ariids by a combination of charac ters including snout shape, barbel length, eye size, tooth arrangement and gill raker number and position. Comparison is made with other ariid species occurring in northern Australian rivers, including the morphologically similar A. leptaspis (Bleeker). Introduction The Timor Sea and Gulf of Carpentaria drainage systems (Lake 1971) approx imately represent the Leichhardtian zoogeographic region of Whitley (1947). The rainfall pattern in this region is dominated by the wet monsoon (occurring within the period November to April). Most rivers here traverse a flat coastal plain about 15 km wide before reaching the sea (Lake 1971). These rivers commonly possess wide flood plains and low gradients, often contracting to a chain of waterholes during the dry season; some (Gregory River; Fitzroy to Daly Rivers) have reaches of rapids or very deep gorges. The average annual discharge from this region is 69000 billion litres (Lake 1971), most of it occurring during the wet season. Five of Australia's 18 species of fork-tailed catfishes (Ariidae) are common in this northern region, yet were overlooked by Whitley (1947) and Iredale and Whitley (1938). The members of this family, which is distributed circumglobally in the tropics and subtropics, may inhabit the sea, rivers within tidal influence, or fresh waters. -
Demographic Trends and Likely Futures for Australia's Tropical Rivers
Demographic Trends and Likely Futures for Australia’s Tropical Rivers Prepared by Dean Carson, Andrew Taylor and Suzanne Campbell School for Social and Policy Research, Charles Darwin University October 2009 Disclaimer TRaCK has published the information contained in this publication to assist public knowledge and discussion and to help improve the sustainable management of Australia’s tropical rivers and coasts. Where technical information has been prepared by or contributed by authors external to TRaCK, readers should contact the author(s), and conduct their own enquiries, before making use of that information. No person should act on the contents of this publication whether as to matters of fact or opinion or other content, without first obtaining specific independent professional advice which confirms the information contained within this publication. While all reasonable efforts have been made to ensure that the information in this publication is correct, matters covered by the publication are subject to change. Charles Darwin University does not assume and hereby disclaims any express or implied liability whatsoever to any party for any loss or damage caused by errors or omissions, whether these errors or omissions result from negligence, accident or any other cause. Copyright This publication is copyright. Apart from any fair dealing for the purpose of private study, research, criticism or review as permitted under the Copyright Act, no part may be reproduced, by any process, without written permission from the publisher, Enquiries -
Testudines: Chelidae) of Australia, New Guinea and Indonesia
Zoological Journal of the Linnean Society, 2002, 134, 401–421. With 7 figures Electrophoretic delineation of species boundaries within the genus Chelodina (Testudines: Chelidae) of Australia, New Guinea and Indonesia ARTHUR GEORGES1*, MARK ADAMS2 and WILLIAM McCORD3 1Applied Ecology Research Group, University of Canberra, ACT 2601, Australia 2Evolutionary Biology Unit, South Australian Museum, North Terrace, Adelaide, SA 5001, Australia 3East Fishkill Animal Hospital, 285 Rt 82, Hopewell Junction NY 12533, USA Received February 2001; revised and accepted for publication June 2001 A total of 281 specimens of long-necked chelid turtles (Chelodina) were obtained from drainages of Australia, Papua New Guinea and the island of Roti in Indonesia. Ten diagnosable taxa were identified using allozyme profiles at 45 presumptive loci. Chelodina expansa, C. parkeri, C. rugosa and C. burrungandjii are in a Group A clade, C. longi- collis, C. novaeguineae, C. steindachneri, C. pritchardi and C. mccordi are in a Group B clade, and C. oblonga is in a monotypic Group C clade, with each clade thought to represent a distinct subgenus. Chelodina siebenrocki is syn- onymised with C. rugosa. An eleventh taxon, C. reimanni, could not be distinguished from C. novaeguineae on the basis of allozyme profiles, but it is morphologically distinct. Its status is therefore worthy of further investigation. Three instances of natural hybridization were detected. Chelodina rugosa and C. novaeguineae hybridize in the Gulf country of Queensland, with evidence of backcrossing to C. novaeguineae. Chelodina longicollis and C. novaeguineae hybridize in central coastal Queensland, and C. rugosa and C. burrungandjii hybridize along their zone of contact in the plateau escarpment streams and pools. -
Morning Glories" ^S'as* Over Northern Australia And
Interacting "Morning Glories" ^S'aS* over Northern Australia and Abstract some of the place names mentioned in the text is displayed in Fig. 1a; the remaining place names are It is just over 15 years since the first major expedition was indicated on Fig. 1b, which focuses on the Gulf of organized to investigate the "morning glory" phenomenon of north- Carpentaria region.) A photograph of a morning glory eastern Australia. The authors review briefly what has been learned roll cloud is shown in Fig. 2. The clouds are parallel to about the generation and evolution of morning glory disturbances during this time and present data for a particularly interesting event one another, often stretching for several hundred that occurred on 3 October 1991, a day on which two morning glory kilometers. The leading roll is usually smooth, whereas wave formations, one from the northeast and one from the south, were successive rolls are more ragged in texture reflecting detected. The morning glories were seen to interact over the Gulf of a higher degree of turbulence. As the name suggests, Carpentaria. Spectacular National Oceanic and Atmospheric Ad- ministration/Advanced Very High Resolution Radiometer satellite imagery together with comparatively good surface data are pre- sented for this event. Aspects of the interaction between the north- easterly and southerly morning glories are shown to be consistent with theoretical predictions concerning solitary wave interactions. 1. Introduction Solitary waves are isolated finite-amplitude waves of permanent form. Although their mathematical prop- erties have been studied for the past century and a half, only recently have they been viewed as funda- mentally important in the evolution of a wide variety of dynamical systems in the physical and biological sciences. -
Project 4.13 Assessing the Gulf of Carpentaria Mangrove Dieback
Project 4.13 Assessing the Gulf of Carpentaria Mangrove Dieback Project Summary In early 2016, extensive dieback of mangrove forests was recorded along the southern and western Gulf of Carpentaria coastline. Landsat analysis suggests that more than 8,000 hectares of mangrove forest suffered dieback over a relatively short and synchronous time period around November 2015 along a >2,000km wide front from Pormpuraaw in the east (Queensland) to Rose River in the west (Northern Territory). Initial field visits to a limited range of affected sites suggest that a relatively low percentage of trees have recovered and most are dying or dead. This is the largest event of natural dieback of mangroves ever recorded in the world. Problem Across the whole dieback area, there is not for any location, a current formal assessment of the condition of affected forests and what proportion are recovering. Of the affected forests, most are shoreline mangroves, whose death would leave the coastal shoreline exposed to erosion and storm surge effects which may cause even greater and more serious geomorphic and ecological disturbance to this coastline. Biodiversity is likely to have been significantly impacted. Recent field observations showed the epibiont communities that reside upon the trunks and aerial roots of the mangroves have been shed as these structures die and decay, and leaf litter supplies, an important source of food for fisheries production, has significantly decreased. How Research Addresses Problem This project will survey, describe and analyse the dieback across its range. Examination of the patterns of dieback will provide significant insights into the causative factors, what species are in what locations, and in what tidal elevations were species most impacted, and where it was most pronounced. -
Revisiting Inscriptions on the Investigator Tree on Sweers Island, Gulf of Carpentaria
REVISITING INSCRIPTIONS ON THE INVESTIGATOR TREE ON SWEERS ISLAND, GULF OF CARPENTARIA COLLINS, S. J.1, MATE, G.2,1 & ULM, S.1,3 The Investigator Tree, so named after Matthew Flinders’ ship HMS Investigator, is an inscribed tree currently on display in the Queensland Museum. Before being accessioned into the Queensland Museum’s collection in 1889, the Investigator Tree grew on the western shore of Sweers Island in the southern Gulf of Carpentaria. The tree’s “Investigator” inscription, attributed to Flinders (1802), provided the catalyst for future and varied forms of European inscription making on Sweers Island, including a contentious additional “Investigator” inscription on the Investigator Tree carved by Thomas Baines in 1856. Previous researchers have speculated that Baines’ second “Investigator” inscription has caused the faded original “Investigator” inscription to be misinterpreted as either a Chinese or Dutch inscription predating Flinders’ visit to Sweers Island. For the first time, this study undertakes a physical examination of all markings on the Investigator Tree, including a second portion of the tree located at the Queensland Museum since 2009. In com bination with a review of the archival and historical record, findings provide alternative interpretations regarding the (28) inscriptions to address outstanding questions. Archival documents demonstrate that there were at least three inscribed trees on Sweers Island. This paper also revisits the possibility of there once being preFlinders inscriptions on the Investigator -
Under the Fish and Fisheries Act
NORTHERN TERRITORY OF AUSTRALIA Regulations 1985, No. 39* Regulations under the Fish and Fisheries Act I, ERIC EUGENE JOHNSTON, the Administrator of the Northern Territory of Australia, acting with the advice of the Executive Council, hereby make the following Regulations under the Fish and Fisheries Act. Dated this twentieth day of December, 1985. E.E. JOHNSTON Administrator AMENDMENTS OF THE FISH AND FISHERIES REGULATIONS 1. PRINCIPAL REGULATIONS The Fish and Fisheries Regulations are in these Regulations referred to as the Principal Regulations. 2. REPEAL ~~D SUBSTITUTION (1) Regulations 4, 5, 6 and 7 are repealed and the following substituted: fI 4. AMATEUR GEAR fI (l) An amateur fisherman shall not use an item of fishing gear other than an item that is listed in the Table to this regulation, and the items that are listed in that Table are accordingly prescribed for the purposes of section 27(1)(a) of the Act. ,', Notified in the Northern Territorg Government Gazette on 20 December, 1985. G. L. DUFFIELD, Government Printer of the Northern Territory Price: $1.40 Fish and Fisheries Regulations "(2) An amateur fisherman shall not use more than 3 amateur's pots. Penalty: $1,000. "(3) Where an amateur fisherman establishes that - (a) he is a member of a fishing party; and (b) the number of amateur's pots being used by the members of the party does not exceed 3 times the number of fishermen in the party who are no younger than 8 years of age, he may, notwithstanding subregulation (2), use any number of the amateur's pots used by the fishing party up to the limit specified in paragraph (b).