James Edge-Partington in Australia in 1897
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Half Year Report (Due 31 October Each Year)
Darwin Initiative for the Survival of Species Half Year Report (due 31 October each year) Project Ref. No. 13-012 Project Title Integrated River Basin Management in the Sepik River Country(ies) Papua New Guinea UK WWF-UK Organisation Collaborator(s) PNG Department of Environment and Conservation, Ambunti Local Level Government, Ambunti District Local Environment Foundation (ADLEF), and project area communities Report date 1 April - 30 September 2004 Report No. 1 (HYR 1/2/3/4) Project website http://www.wwfpacific.org.fj/wetsepik.htm 1. Outline progress over the last 6 months (April – September) against the agreed baseline timetable for the project (if your project has started less than 6 months ago, please report on the period since start up). Progress towards project milestones: i) Confirm partnership agreements (Q1): The confirmation of partnership agreements between various partners and stakeholders in the national and local level has shown positive affirmation of better working relations. WWF PNG established and maintained the collaboration between the PNG Department of Environment and Conservation and Ambunti District Local Environment Foundation (ADLEF). WWF also strengthened the partnership network with other NGO’s and government institutions such as the PNG Department of Agriculture and Livestock (DAL), provincial government, local level government, and most importantly the local communities. This has enabled the better communication and facilitation of community planning and awareness mechanisms for the indigenous communities. ii) Consultants and staff hired (Q1-2): A position description for the WWF PNG Freshwater Programme Manager was formulated A copy is attached (Attachment A). The position vacancy announcement for a Freshwater Programme Manager was advertised in the major PNG newspaper on 9 June. -
The Quest for Natural Biogeographic Regions
Chapter 3 Carving up Australasia: the quest for natural biogeographic regions Most systematists will squirm at inferences derived from a non-monophyletic or artificial taxon. The importance of monophyly is critical to understanding the natural world and drawing inferences about past processes and events. Since the early 19th century, plant and animal geographers have also been concerned about correctly identifying natural areas. Plant geographer and taxonomist Augustin de Candolle tried to propose natural laws when proposing natural areas and failed. Humboldt abandoned natural classification and assigned vegetable forms, thereby creating a useful classification, which was unfortunately artificial. For early 19th century Australasian biogeographers, the concept of cladistic biogeography and area monophyly was decades away, while the importance of finding natural areas was immediate. Natural areas allowed the biogeographer to make inferences about the biotic evolution of a region such as Australia or New Zealand. Discovering the relationships between natural areas would allow for better inferences about dispersal pathways and evolutionary connections between continental floras and faunas, rather than proposing ephemeral land-bridges or sunken continents. Still, after 150 years of searching, biogeographers puzzle over the natural regions of Australasia. Why natural regions? As in biological systematics, artificial taxa represent a pastiche of distantly related taxa (think of the term ‘insectivores’, which would include all insect eating animals, such as funnel-web spiders, bee-eaters and echidnas). Artificial taxa are more closely related to other taxa than they are to themselves. The same is true for biogeography – artificial areas, such as ‘Australia’, are composites that are more closely related to other areas than they are to themselves. -
Rare and Curious Specimens, an Illustrated
Having held the position in an acting capacity, Etheridge experienced no dif ficulty in assuming the full-time position of curator on 1 January 1895. He had, of course, to relinquish his half-time post in the Geological Survey but, as consulting palaeontologist to the Survey, he retained a foot in each camp and continued to publish under the aegis of both institutions. His scientific staff consisted of six men. Whitelegge was still active in his researches on marine invertebrates and was engaged in testing the efficiency of formalin as a preservative. North continued his studies on birds, but somewhat less actively since, to free Brazier for work on his long-delayed catalogue, he had been made responsible also for the ethnological, numismatic and historical collections. Conchology was now in the hands of Charles Hedley, first appointed in 1891 on a temporary basis to handle the routine matters of this department and to leave Brazier more time for his catalogue. Born in England, Hedley came to Australia at the age of twenty to seek relief from asthma and after a short period working on an oyster lease on Stradbroke Island, turned to fruit growing at Boyne Island. When a badly fractured left arm rendered him unfit for heavy work, he moved to Brisbane where, in 1889, he obtained a position on the staff of the Queensland Museum and developed an interest in shells. Finding that the collections and library of that insti tution were inadequate for his needs, he moved to Sydney and, within a few months, was recruited to the Museum at the age of thirty. -
Geomorphology and the Great Barrier Reef
Cambridge University Press 978-0-521-85302-6 - The Geomorphology of the Great Barrier Reef: Development, Diversity, and Change David Hopley, Scott G. Smithers and Kevin E. Parnell Excerpt More information 1 Geomorphology and the Great Barrier Reef 1.1 Introduction The Great Barrier Reef (GBR) is the largest coral reef system in the world. It extends from 248 300 S in the south to 98 300 S in the north, a distance of about 2300 km along the north-east shelf of Australia (Fig. 1.1). Accurate estimates of dimensions and other geographical data are available only for the Great Barrier Reef Marine Park (345 500 km2) or the Great Barrier Reef World Heritage Area (348 000 km2) which also includes islands excluded from the Park. Within this area are 2900 reefs occupying over 20 000 km2 or 9% of the 224 000 km2 shelf area (Hopley et al., 1989). However, this administrative area does not include the contiguous shelf of Torres Strait, data for which are more scant. The Strait is 150 km wide and east of the line of high islands, which link Australia to Papua New Guinea, the shelf has a width of over 200 km. Estimated total shelf area here is about 37 000 km2 and, relying on comparative data from the adjacent Great Barrier Reef Marine Park (which ends at 108 420 S) there may be a further 750 reefs and shoals with a total area of about 6000 km2. The GBR is also one of the best studied in the world. Although first described during James Cook’s voyage of exploration in 1770, because of science’s preoccupation with atolls, it did not become a major focus until after the establishment of the Great Barrier Reef Committee in 1922 and the ground-breaking year-long Royal Society Expedition to Low Isles near Cairns in 1928–29 (see below and Bowen and Bowen, 2002). -
0=AFRICAN Geosector
2= AUSTRALASIA geosector Observatoire Linguistique Linguasphere Observatory page 123 2=AUSTRALASIA geosector édition princeps foundation edition DU RÉPERTOIRE DE LA LINGUASPHÈRE 1999-2000 THE LINGUASPHERE REGISTER 1999-2000 publiée en ligne et mise à jour dès novembre 2012 published online & updated from November 2012 This geosector covers 223 sets of languages (1167 outer languages, composed of 2258 inner languages) spoken or formerly spoken by communities in Australasia in a geographic sequence from Maluku and the Lesser Sunda islands through New Guinea and its adjacent islands, and throughout the Australian mainland to Tasmania. They comprise all languages of Australasia (Oceania) not covered by phylosectors 3=Austronesian or 5=Indo-European. Zones 20= to 24= cover all so-called "Papuan" languages, spoken on Maluku and the Lesser Sunda islands and the New Guinea mainland, which have been previously treated within the "Trans-New Guinea" hypothesis: 20= ARAFURA geozone 21= MAMBERAMO geozone 22= MANDANGIC phylozone 23= OWALAMIC phylozone 24= TRANSIRIANIC phylozone Zones 25= to 27= cover all other so-called "Papuan" languages, on the New Guinea mainland, Bismarck archipelago, New Britain, New Ireland and Solomon islands, which have not been treated within the "Trans-New Guinea" hypothesis: 25= CENDRAWASIH geozone 26= SEPIK-VALLEY geozone 27= BISMARCK-SEA geozone Zones 28= to 29= cover all languages spoken traditionally across the Australian mainland, on the offshore Elcho, Howard, Crocodile and Torres Strait islands (excluding Darnley island), and formerly on the island of Tasmania. An "Australian" hypothesis covers all these languages, excluding the extinct and little known languages of Tasmania, comprising (1.) an area of more diffuse and complex relationships in the extreme north, covered here by geozone 28=, and (2.) a more closely related affinity (Pama+ Nyungan) throughout the rest of Australia, covered by 24 of the 25 sets of phylozone 29=. -
Porphyry Copper)
The Exploration of Potential Mineral Resources in Papua New Guinea Howard Lole Chief Inspector of Mines Papua New Guinea THIRD PECC MINERAL NETWORK MEETING MINING ECONOMY: DEVELOPMENT & ENVIRONMENTAL PROTECTION September 9-11, 2005 Jin Ci Hotel Taiyuan, Shanxi Province, China 0 TABLE OF CONTENT INTRODUCTION ......................................................................................................................... 2 FREIDA COPPER AND GOLD PROJECT ................................................................................. 3 WAFI GOLD COPPER DEPOSIT................................................................................................ 5 SIMUKU COPPER GOLD............................................................................................................ 7 MOUNT NAKRU GOLD COPPER ........................................................................................... 10 YANDERRA (PORPHYRY CU-MO)........................................................................................ 14 WOWO GAP (NICKEL LATERITE)......................................................................................... 15 PANGUNA (PORPHYRY COPPER)......................................................................................... 17 MOROBE BEACH SANDS’ CHROMITE ................................................................................ 17 COPPER SMELTING ................................................................................................................. 22 LIMESTONE .............................................................................................................................. -
The Biology and Geology of Tuvalu: an Annotated Bibliography
ISSN 1031-8062 ISBN 0 7305 5592 5 The Biology and Geology of Tuvalu: an Annotated Bibliography K. A. Rodgers and Carol' Cant.-11 Technical Reports of the Australian Museu~ Number-t TECHNICAL REPORTS OF THE AUSTRALIAN MUSEUM Director: Technical Reports of the Australian Museum is D.J.G . Griffin a series of occasional papers which publishes Editor: bibliographies, catalogues, surveys, and data bases in J.K. Lowry the fields of anthropology, geology and zoology. The journal is an adjunct to Records of the Australian Assistant Editor: J.E. Hanley Museum and the Supplement series which publish original research in natural history. It is designed for Associate Editors: the quick dissemination of information at a moderate Anthropology: cost. The information is relevant to Australia, the R.J. Lampert South-west Pacific and the Indian Ocean area. Invertebrates: Submitted manuscripts are reviewed by external W.B. Rudman referees. A reasonable number of copies are distributed to scholarly institutions in Australia and Geology: around the world. F.L. Sutherland Submitted manuscripts should be addressed to the Vertebrates: Editor, Australian Museum, P.O. Box A285, Sydney A.E . Greer South, N.S.W. 2000, Australia. Manuscripts should preferably be on 51;4 inch diskettes in DOS format and ©Copyright Australian Museum, 1988 should include an original and two copies. No part of this publication may be reproduced without permission of the Editor. Technical Reports are not available through subscription. New issues will be announced in the Produced by the Australian Museum Records. Orders should be addressed to the Assistant 15 September 1988 Editor (Community Relations), Australian Museum, $16.00 bought at the Australian Museum P.O. -
Transformations of the Meeting-House in Tuvalu
Transformations of the meeting-house in Tuvalu Michael Goldsmith My problem is this: the Tuvaluan meeting-house is displayed as a symbol of indigenous culture in many different contexts. It is therefore often assumed, by both outside commentators and Tuvaluans themselves, to be of long standing in the history of that culture. Yet the word maneapa, by which the meeting-house is generically known, is of Gilbertese origin.1 Moreover, the weight of evidence suggests that not only the word but probably even the type of building itself is a post-colonial borrowing or implantation. If, indeed, there were no maneapa as such in Tuvalu before British hegemony was es tablished, then questions arise as to what, if anything, existed in its place; why the maneapa was introduced or borrowed; why it has achieved its current importance and, further, why it has become a symbol of national identity. In this connection, the concept of “transformation” calls out for a strong measure of historical attention. Yet the meaning of history is not as self-evident as the traditional definitions imply, with their references to narrative, sequences of events and so on (Braudel 1980:27). Another avenue, almost a new orthodoxy, has been explored under the influence of structuralism. Bather than using sequences of events to explain structure, some anthropologists use the delineation of structure to explain events. While Lêvi-Strauss’ name is the most closely linked to this programme (1966-.passim), even historical materialists find it beguiling. Godelier, for example, reverses the con ventional Marxist understanding of history with his contention that it explains nothing but is the category which itself needs to be explained, once structure has been revealed (Godelier 1977:49). -
Renato Pacini, Starlight Musical's Orchestra Conductor for This Season, Is Appearing on the Fair Grounds Podium for the First Time
• 4 O I V STARLIGHT MUSICALS presents _%s VN / -^ INDIANAPOLIS THEATRE ASSOCIATION, INC. INDIANA STATE FAIR GROUNDS INDIANAPOLIS cat^ INDIANAPOLIS THEATRE ASSOCIATION, INC. CLAYPOOL HOTEL • TELEPHONE RILEY 5417 INDIANAPOLIS, IND. OFFICERS Summer, 1951 MELVIN T. ROSS President and Gen. Manager Mr. and Mrs. John Q. Public HENRY HOLT Anyplace, Indiana 1st Vice-President H. T. PRITCHARD Dear Mr. and Mrs. Public: 2nd Vice-President CHARLES HEDLEY This is in answer to your letters of last season—the thousands of letters which expressed your Vice-Pres. and Producer L. G. GORDNER enjoyment of the entertainment you saw here at the Fair Grounds. Recording Secretary WILLIAM J. SCHUMACHER Any innovation in the entertainment business, especially if it involves a series of attractions, Corresponding Secretary takes thought, perseverance, time and money to become sufficiently well-established to bring the J. S. ROGAN Treasurer attractions which you, the public, deserve. DIRECTORS This is our most ambitious season to date. We believe that in our series this year we have chosen the cream of the crop as far as musical attractions are concerned. And the widened scope Fred Ayres Donald R. Barneclo of our plans has been made possible by your increased enthusiasm and patronage — for which we Noble Biddinger thank you. •J. M. Bloch William H. Book Almost every city our size in the middle west has a series of summer attractions which has Cecil M. Byrne lived, and grown, because the public wanted it. We, too, shall continue to grow and prosper by Joseph E. Cain giving you the type and calibre of entertainment which has kept you coming back year after year. -
A Revision of the Australian Pinnidae
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Hedley, Charles, 1924. A revision of the Australian Pinnidae. Records of the Australian Museum 14(3): 141–153, plates xix–xxi. [26 June 1924]. doi:10.3853/j.0067-1975.14.1924.838 ISSN 0067-1975 Published by the Australian Museum, Sydney nature culture discover Australian Museum science is freely accessible online at http://publications.australianmuseum.net.au 6 College Street, Sydney NSW 2010, Australia A REVISION OF THE AUSTRALIAN PINNIDJE. By CHARLES HEDLEY. (Plates xix-xxi.) The Pinnidm are a small family of marine bivalves including many fossil and about fifty recent species which occur throughout the warmer seas of the world. Though thin and brittle these shells are notable for their length, being exceeded in this respect only by the Giant Clams. They live planted point downwards with the tips of the broad ends projecting above the surface of zostera flats. An ugly wound may be inflicted on the bare feet of those who tread on their sharp blades, from this the shells are called in Australia "Razorbacks." The doings of a commensal crab, Pinnotheres, frequently a guest in the Pinna mansion, is related by classic legends either as the behaviour of a rascal or of a grateful attendant. The first attempt at classification of the Pinnidm was by Chemnitz, who in 1785 drew attention to a feature separating various species of Pinna,. In some, for instance P. ineurv1ata., the apical muscle scar has a ridge running lengthwise down the centre; in others, as in P. atrata, this ridge is absent. Apparently prompted by this observa tion, Gray proposed' the genus Atrina for the second group, with P. -
Diastrophic Evolution of Western Papua and New Guinea
DIASTROPHIC EVOLUTION OF WESTERN PAPUA AND NEW GUINEA by JAN G. WITH, B.S., M.S. (The Pennsylvania State University) A thesis submitted in partial fulfillment of the requirements for the Degree of Doctor of Philosophy UNIVERSITY OF TASMANIA HOBART July 1964 This thesis contains no material which has been accepted for the award of any other degree or diploma in any university and to the best of my knowledge and belief contains no copy or paraphrase of material previously published or written by another person except where due reference is made in the text of the thesis. JAN G. SMITH University of Tasmania Hobart July 1964 CONTENTS Page LIST OF ILLUSTRATIONS • • • xi ABSTRACT 1 INTRODUCTION 3 Nature and purpose of study Location Method of study and presentation Previous work Acknowledgements 1 DIASTROPHIC FRAMEWORK OF WESTERN PAPUA AND NEW GUINEA 8 1.1 QUARTERNARY DIASTROPHISM 14 1.1.1 Morphology of Western Papua and New Guinea 14 Western cordilleran region Central cordilleran region Central foothills region Darai Hills Fly-Digoel shelf Oriomo Plateau Kukukuku lobe Sepik and Ramu-Markham depressions 1.1.2 Nature of Quaternary Sediments and Crustal Movements 20 Fly-Digoel shelf Delta embayment Western cordilleran region Central cordilleran region Central foothills Sepik and Ramu-Markham depressions 1.1.3 Volcanism.. *400000 26 1.2 PLIOCENE DIASTROPHISM 28 1.2.1 Pliocene Rocks 28 Digoel-Strickland basin Fly-Digoel shelf Purari basin CONTENTS Page 1 DIASTROPHIC FRAMEWORK OF WESTERN PAPUA AND NEW GUINEA (continued) 1.2.2 Framework of Pliocene Diastrophism. • •••••• 34 Digoel-Strickland basin Fly-Digoel platform Purari basin Continuity of the Pliocene exogeosyncline Darai swell 1.2.3 Chronology of Pliocene and Quaternary Movements 38 Central foothills and cordillera Western cordillera 1.3 UPPER MIOCENE DIASTROPHISM 43 1.3.1 Upper Miocene Rocks 43 Limestone facies Mudstone fades 1.3.2 Framework of Upper Miocene Diastrophism. -
INVERTEBRATE ZOOLOGY Crustacet 286 JANET HAIG Needed
keprinted from the "Proceedings of Symposium on Crustacea"—Part t A REVIEW ©F THE INDO-WEST PACIFIC SPECIES OF GENUS PACHYCHELES (PORCELLANIDAE, ANOMURA)* JPiSDrr JANET HAIG 1 | B R A R Y Allan Hancock Foundation, University of Southern California, Los i/yj&gK . ABSTRACT Parhvcheles is a well-defined genus in the Porcellanidae, occurring world-wide and with approximately snacks Tb date the Indo-West Pacific members of the genus have not been reviewed a* a whole. In thisaSthere is a total of 11 species: of these, two have recently been described and two more have not pievioSy been recognized as members of genus Pachycheles. INTRODUCTION PACHYCHELES Stimpson, 1858, is a well-defined genus in the Porcellanidae, occurring world-wide in ironical warm-temperate, and cold-temperate regions and with approximately 40 species. Most of them live intertidally or in shallow water, although occasional individuals ol a few species have been dredged in *fopths of 100 meters or more. Like most porcellanids they conceal themselves under stones, in tie cavities of sponges, or among algae; in tropical regions they frequently live in corals. Pachycheles belongs to that group of genera in which the basal antennal segment is short, not ritctiiriinf the movable segments from the orbit. The carapace is usually about as broad as long in malesand somewhat broader than long in females. Jhe.outer orbital angle is produced into a spine m some species but, except for spiniform tubercles.which may be developed along the lateral margins (1 condition occurring only in P. spinipes), there are no other spines on the carapace.