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Where Were Australia's First European Residents Marooned in 1629?
The Landing Site Debate: Where Were Australia’s First European Residents Marooned in 1629? Rupert Gerritsen1 Introduction On 16 November 1629, following the Batavia Mutiny on the Abrolhos Islands, just off the central west coast of Western Australia, Commander Francisco Pelsaert marooned two of the mutineers on the adjacent mainland of Australia. Since 1959 there has been an ongoing debate as to where these two mutineers, Wouter Loos and Jan Pelgrom de Bye van Bemmel, were put ashore. Two contending sites have been proposed, the mouth of the Hutt River and a location 61 kilometres further north, Wittecarra Gully, with an array of evidence having been marshalled by the proponents of each of the sites to support their case. This is no trivial matter, as these two mutineers were in fact the first Europeans to take up permanent residence in Australia, 159 years before the First Fleet. It is therefore a question of some significance in Australian history. This paper will put forward the evidence and arguments for each site for consideration, endeavouring to fairly reflect the contending positions, so that others may judge for themselves which is correct. Background The story begins in the early hours of 4 June 1629, when the Dutch ship the Batavia with 320 people on board, struck Morning Reef in the Northern, or Wallabi Group, of the Abrolhos Islands, 90 kilometres west north west of Geraldton (1). Approximately 275 people survived the initial disaster, finding their way by various means to the nearest islands. But they were in dire straits, they had almost no food or water. -
A Brief Review of the Status of Seabirds at Long Island, Wallabi Group, Houtman Abrolhos
Humfrey Land Developments Avifauna Field Survey January 2006 Citation. This report may be quoted as: Surman, C.A. (2006). Field Survey of Avifauna at Long Island, Wallabi Group, Houtman Abrolhos, September and December 2005. Unpublished report prepared for MBS by Halfmoon Biosciences. 33 pp. Submitted on: 30 January 2006 Prepared by: Dr Chris Surman Halfmoon Biosciences 14 Snook Crescent Hilton, W.A. 6163 [email protected] ©Copyright 2006 Halfmoon Biosciences This document and information contained in it has been prepared by Halfmoon Biosciences under the terms and conditions of his contract with his client. The report is for the client’s use only and may not be used, exploited, copied, duplicated or reproduced in any form or medium whatsoever without the prior written permission of Halfmoon Biosciences or their client. Halfmoon Biosciences i Humfrey Land Developments Avifauna Field Survey January 2006 Table of Contents 1 Introduction................................................................................................................. 1 1.1 Nomenclature...................................................................................................... 2 2 Nesting Habitat ........................................................................................................... 3 2.1 Low Sand Dunes (plates 1-4).............................................................................. 3 2.2 Coral Ridges........................................................................................................ 3 2.3 Tidal -
Bulletin of the Geological Society of America Vol. 71. Pp. 1729-1754, 7 Figs. December 1960 Bermuda: a Partially Drowned, Late M
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 71. PP. 1729-1754, 7 FIGS. DECEMBER 1960 BERMUDA: A PARTIALLY DROWNED, LATE MATURE, PLEISTOCENE KARST BY J HARLEN BRETZ ABSTRACT During Pleistocene time, the Bermuda Islands repeatedly underwent partial inundation and re-emergence. The land areas were continuously attacked and reduced by rain and ground water but repeatedly renewed, during times of submergence, by deposition of marine limestone and by contemporaneous additions of shore-born and wind-transported carbonate sand, now eolianite. Soils formed under subaerial conditions are now buried be- neath later deposits and constitute important stratigraphic markers. The igneous founda- tion rock appears to have been exposed during some low marine stands, and the former shore lines seem to be recorded by submerged terraces. The major karst features are largely below sea level, and they must date from times of continental glaciations. Previous writers have assigned eolian accumulation to times of Pleistocene low sea level and soil-making to times of interglacial high sea. Both conclusions are held to be er- roneous. CONTENTS TEXT Figure Page Page Navy and Air Force modifications of the Introduction 1729 shore line 1730 Acknowledgments 1732 2. Bermuda Islands with the adjacent Dunes and eolianites 1732 banks 1733 Paleosols 1736 3. Diagram of section at Whalebone Bay, Ber- Caves 1741 muda Islands 1735 Origin of the interior basins 1744 4. Diagram to show contrast in soil record on Correlation of soil-making and dune-building uplands and lowlands, Bermuda with Pleistocene eustatism 1746 Islands 1736 Conclusion 1752 5. Diagram of Shore Hills type section, References cited 1754 Bermuda Islands 1737 6. -
SUSTAINABLE TOURISM for the HOUTMAN ABROLHOS ISLANDS Progress Update July 2020
SUSTAINABLE TOURISM FOR THE HOUTMAN ABROLHOS ISLANDS Progress update July 2020 On 6 October 2017, the Premier, Hon Mark McGowan Progress towards achieving the Government’s For more information about the IPT or the sustainable MLA, announced that the State Government’s vision sustainable tourism vision for the Abrolhos has tourism project, please visit the DBCA website at: for the Abrolhos Islands was to create a world-class included: dbca.wa.gov.au/houtman-abrolhos-islands-national-park tourism experience while maintaining world’s • Creation of the Houtman Abrolhos Islands National best-practice environmental management. Park (national park) Planning for the Abrolhos land and waters Following this, a whole-of-Government planning • Development of an interagency Strategic Direction The Houtman Abrolhos Islands Strategic Direction process commenced to develop the most appropriate 2020–24 2020–24 management framework for the marine and terrestrial • Development of a draft Visitor Master Plan for the The Strategic Direction outlines the State Government’s areas of the Abrolhos and an Interagency Project Team national park vision and goals for management of the Abrolhos (lands (IPT) was established to ensure the effective delivery of • Commencement of a management plan for the and waters) with interagency collaboration between the Government’s commitment. The membership of the national park DBCA, DPIRD and the Western Australian Museum as a IPT includes agencies with legislative responsibilities or • Planning for the development of visitor facilities key focus. Other agencies supporting the realisation of an interest in the management of the Abrolhos, including initially in the Wallabi group the vision for the Abrolhos include Tourism WA, City of the Department of Biodiversity, Conservation and Greater Geraldton, Abrolhos Islands Bodies Corporate, Attractions (DBCA), Department of Primary Industries • Licensing of commercial tour operators in the national Mid West Development Commission, Department of and Regional Development (DPIRD), Western Australian park. -
WA999 Wallabi Group
999 WA HOUTMAN ABROLHOS - WALLABI GROUP WALLABI - ABROLHOS HOUTMAN SEE RELATED PUBLICATIONS: Notice to Mariners (http://www.transport.wa.gov.au/imarine/coastaldata/), Symbols, Abbreviations DEPTHS IN METRES and Terms (INT 1), Tide Tables, Sailing Directions. For surveys beyond this chart refer to RAN Charts AUS 83 and AUS 751. E= 7 52 000 E= 7 60 000 E= 7 68 000 E= 7 76 000 34' 35' 36' 37' 38' 39' 113°40' E 41' 42' 43' 44' 45' 46' 47' 48' 49' 52 46 44 43 42 44 28° 13' 24" S 51 49 113° 40' E Zone of Confidence (ZOC) Diagram 28° 13' 24" S 28° 13' 24" S HOUTMAN ABROLHOS AUSTRALIA - WEST COAST 50 48 43 CHART LAYOUT WESTERN AUSTRALIA 113° 49' 48" E 14’ 14’ 113° 49' 48" E 46 46 113° 49' 48" E 52 HOUTMAN ABROLHOS C 46 WALLABI GROUP 41 36 SCALE 1 : 50 000 000 44 72 44 46 68 DEPTHS 41 N= 23 44 Depths are shown in metres and decimetres, reduced to Sounding Datum, which is 15’ 35 approximately lowest water level. 15’ 21 B HEIGHTS Heights are shown in metres. Underlined figures are drying heights above Sounding 11 30 13 Datum. Overhead clearance heights are above Highest Astronomical Tide. All other 000 16 8 8 2 29 heights are above Mean Higher High Water. 72 128 C 68 62 POSITIONS 24 6 41 N= 6 Positions on this chart are referenced to the Map Grid of Australia, Zone 50, 18 43 Wallabi Group WA 999 Side A based on the Geocentric Datum of Australia 1994 (GDA94). -
Abrolhos Painted Button-Quail (Turnix Varius Scintillans) Interim Recovery Plan
Abrolhos Painted Button-Quail (Turnix varius scintillans) Interim Recovery Plan Wildlife Management Program No. 63 Western Australia Department of Biodiversity, Conservation and Attractions May 2018 Wildlife Management Program No. 63 Abrolhos Painted Button-Quail (Turnix varius scintillans) Interim Recovery Plan Western Australia Department of Biodiversity, Conservation and Attractions Locked Bag 104, Bentley Delivery Centre, Western Australia 6983 Foreword Recovery plans are developed within the framework laid down in the Department of Biodiversity, Conservation and Attractions Corporate Policy Statement No. 35 (Parks and Wildlife, 2015b) and Corporate Guideline No. 36 (Parks and Wildlife, 2015a). Interim recovery plans outline the recovery actions that are needed to urgently address those threatening processes most affecting the ongoing survival of threatened taxa or ecological communities, and begin the recovery process. The attainment of objectives and the provision of funds necessary to implement actions are subject to budgetary and other constraints affecting the parties involved, as well as the need to address other priorities. This interim recovery plan was approved by the Department of Biodiversity, Conservation and Attractions, Western Australia. Approved interim recovery plans are subject to modification as dictated by new findings, changes in status of the taxon or ecological community, and the completion of recovery actions. Information in this interim recovery plan was accurate as of May 2018. Interim recovery plan preparation: -
Australia's First Criminal Prosecutions in 1629
Australia’s First Criminal Prosecutions in 1629 Rupert Gerritsen Batavia Online Publishing Australia’s First Criminal Prosecutions in 1629 Batavia Online Publishing Canberra, Australia http://rupertgerritsen.tripod.com Published by Batavia Online Publishing 2011 Copyright © Rupert Gerritsen National Library of Australia Cataloguing-in-Publication Data Author: Gerritsen, Rupert, 1953- Title: Australia’s First Criminal Prosecutions in 1629 ISBN: 978-0-9872141-2-6 (pbk.) Notes: Includes bibliographic references Subjects: Batavia (Ship) Prosecution--Western Australia--Houtman Abrolhos Island.s Mutiny--Western Australia--Houtman Abrolhos Islands--History. Houtman Abrolhos Islands (W.A.) --History. Dewey Number: 345.941025 CONTENTS Introduction 1 The Batavia Mutiny 1 The Judicial Context 5 Judicial Proceedings Following 7 The Mutiny The Trials 9 The Executions 11 Other Legal Proceedings and Issues - 12 Their Outcomes and Implications Bibliography 16 Notes 19 Australia’s First Criminal Prosecutions in 1629 Rupert Gerritsen Introduction The first criminal proceedings in Australian history are usually identified as being the prosecution of Samuel Barsley, or Barsby, Thomas Hill and William Cole in the newly-established colony of New South Wales on 11 February 1788. Barsley was accused of abusing Benjamin Cook, Drum-Major in the marines, and striking John West, a drummer in the marines. It was alleged Hill had stolen bread valued at twopence, while Cole was charged with stealing two deal planks valued at ten pence. The men appeared before the Court of Criminal Judicature, the bench being made up of Judge-Advocate Collins and a number of naval and military officers - Captains Hunter, Meredith and Shea, and Lieutenants Ball, Bradley and Creswell.1,2 However, the first criminal prosecutions to take place on what is now Australian soil actually occurred in more dramatic circumstances in 1629. -
Impact of Sea Level Rise on Coastal Natural Values in Tasmania
Impact of sea level rise on coastal natural values in Tasmania JUNE 2016 Department of Primary Industries, Parks, Water and Environment Acknowledgements Thanks to the support we received in particular from Clarissa Murphy who gave six months as a volunteer in the first phase of the sea level rise risk assessment work. We also had considerable technical input from a range of people on various aspects of the work, including Hans and Annie Wapstra, Richard Schahinger, Tim Rudman, John Church, and Anni McCuaig. We acknowledge the hard work over a number of years from the Sea Level Rise Impacts Working Group: Oberon Carter, Louise Gilfedder, Felicity Faulkner, Lynne Sparrow (DPIPWE), Eric Woehler (BirdLife Tasmania) and Chris Sharples (University of Tasmania). This report was compiled by Oberon Carter, Felicity Faulkner, Louise Gilfedder and Peter Voller from the Natural Values Conservation Branch. Citation DPIPWE (2016) Impact of sea level rise on coastal natural values in Tasmania. Natural and Cultural Heritage Division, Department of Primary Industries, Parks, Water and Environment, Hobart. www.dpipwe.tas.gov.au ISBN: 978-1-74380-009-6 Cover View to Mount Cameron West by Oberon Carter. Pied Oystercatcher by Mick Brown. The Pied Oystercatcher is considered to have a very high exposure to sea level rise under both a national assessment and Tasmanian assessment. Its preferred habitat is mudflats, sandbanks and sandy ocean beaches, all vulnerable to inundation and erosion. Round-leaved Pigface (Disphyma australe) in flower in saltmarsh at Lauderdale by Iona Mitchell. Three saltmarsh communities are associated with the coastal zone and are considered at risk from sea level rise. -
Herpetofauna Assessment of Long Island, Wallabi Group – 8 November 2005
Herpetofauna of Long Island, Houtman Abrolhos Herpetofauna Assessment of Long Island, Wallabi Group – 8 November 2005 Prepared for: MBS Environmental By: Dr R. A. How Western Australian Museum Locked Bag 49 Welshpool DC, WA 6986 Phone: (08) 9427 2738 Facsimile: (08) 9427 2882 November 2005 Report No: NTVBE/2005/MBS Western Australian Museum 1 Herpetofauna of Long Island, Houtman Abrolhos Introduction Long Island lies in the Wallabi Group of the Houtman Abrolhos and is roughly 11 ha in extent with a maximum elevation of 2 m. It is part of the Long Island chain in the centre of the Wallabi Group and is a composite island consisting of unconsolidated coral rubble and some smaller areas of sand. The vegetation and relationship to other islands has been well documented by Harvey et al. (2001). The reptiles of Houtman Abrolhos were first documented by Alexander (1922) and subsequently by numerous surveys of the islands by Storr and the Aquinas College, Perth, which were summarized and re-evaluated by Storr et al. (1983). More recently there has been extensive research on the reptiles of the Wallabi Islands and opportunistic examination of several islands in the Pelsaert Group that has been summarized by How et al. (2004). The Abrolhos islands are the type locality of six reptile taxa, Pogona minor minima, Heteronotia binoei, Christinus marmoratus, Strophurus spinigerus, Egernia stokesii stokesii and Eremiascincus richardsonii. This report examines the herpetofauna of Long Island, the site for a new nature-based resort development. Methods A search for herpetofauna on Long Island was undertaken on the 8th of November 2005, by four expert herpetologists. -
A Multi-Gene Region Targeted Capture Approach to Detect Plant DNA in Environmental Samples
bioRxiv preprint doi: https://doi.org/10.1101/2021.07.03.450983; this version posted July 26, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 A multi-gene region targeted capture approach to detect plant DNA in 2 environmental samples: A case study from coastal environments 3 Nicole R. Foster1*, Kor-jent van Dijk1, Ed Biffin2, Jennifer M. Young3, Vicki Thomson1, 4 Bronwyn M. Gillanders1, Alice Jones1,4, Michelle Waycott1,2 5 6 Abstract 7 Metabarcoding of plant DNA recovered from environmental samples, termed environmental DNA 8 (eDNA), has been used to detect invasive species, track biodiversity changes and reconstruct past 9 ecosystems. The P6 loop of the trnL intron is the most widely utilized gene region for metabarcoding 10 plants due to the short fragment length and subsequent ease of recovery from degraded DNA, which 11 is characteristic of environmental samples. However, the taxonomic resolution for this gene region is 12 limited, often precluding species level identification. Additionally, targeting gene regions using 13 universal primers can bias results as some taxa will amplify more effectively than others. To increase 14 the ability of DNA metabarcoding to better resolve flowering plant species (angiosperms) within 15 environmental samples, and reduce bias in amplification, we developed a multi-gene targeted capture 16 method that simultaneously targets 20 chloroplast gene regions in a single assay across all flowering 17 plant species. -
The Origin and Paleoclimatic Significance of Carbonate Sand Dunes Deposited on the California Channel Islands During the Last Glacial Period
Pages 3–14 in Damiani, C.C. and D.K. Garcelon (eds.). 2009. Proceedings of 3 the 7th California Islands Symposium. Institute for Wildlife Studies, Arcata, CA. THE ORIGIN AND PALEOCLIMATIC SIGNIFICANCE OF CARBONATE SAND DUNES DEPOSITED ON THE CALIFORNIA CHANNEL ISLANDS DURING THE LAST GLACIAL PERIOD DANIEL R. MUHS,1 GARY SKIPP,1 R. RANDALL SCHUMANN,1 DONALD L. JOHNSON,2 JOHN P. MCGEEHIN,3 JOSSH BEANN,1 JOSHUA FREEMAN,1 TIMOTHY A. PEARCE,4 1 AND ZACHARY MUHS ROWLAND 1U.S. Geological Survey, MS 980, Box 25046, Federal Center, Denver, CO 80225; [email protected] 2Department of Geography, University of Illinois, Urbana, IL 61801 3U.S. Geological Survey, MS 926A, National Center, Reston, VA 20192 4Section of Mollusks, Carnegie Museum of Natural History, 4400 Forbes Ave., Pittsburgh, PA 15213 Abstract—Most coastal sand dunes, including those on mainland California, have a mineralogy dominated by silicates (quartz and feldspar), delivered to beach sources from rivers. However, carbonate minerals (aragonite and calcite) from marine invertebrates dominate dunes on many tropical and subtropical islands. The Channel Islands of California are the northernmost localities in North America where carbonate-rich coastal dunes occur. Unlike the mainland, a lack of major river inputs of silicates to the island shelves and beaches keeps the carbonate mineral content high. The resulting distinctive white dunes are extensive on San Miguel, Santa Rosa, San Nicolas, and San Clemente islands. Beaches have limited extent on all four of these islands at present, and some dunes abut rocky shores with no sand sources at all. Thus, the origin of many of the dunes is related to the lowering of sea level to ~120 m below present during the last glacial period (~25,000 to 10,000 years ago), when broad insular shelves were subaerially exposed. -
Houtman Abrolhos Islands National Park Draft Management Plan 2021
Houtman Abrolhos Islands National Park draft management plan 2021 Department of Biodiversity, Conservation and Attractions Conservation and Parks Commission Department of Biodiversity, Conservation and Attractions 17 Dick Perry Avenue KENSINGTON WA 6151 Phone: (08) 9219 9000 Fax: (08) 9334 0498 dbca.wa.gov.au © State of Western Australia 2021 2021 This work is copyright. You may download, display, print and reproduce this material in unaltered form (retaining this notice) for your personal, non-commercial use or use within your organisation. Apart from any use as permitted under the Copyright Act 1968, all other rights are reserved. Requests and enquiries concerning reproduction and rights should be addressed to Department of Biodiversity, Conservation and Attractions (DBCA). ISBN 978-1-925978-16-2 (online) ISBN 978-1-925978-15-5 (print) This management plan was prepared by the Conservation and Parks Commission through the agency of the Department of Biodiversity, Conservation and Attractions. Questions regarding this management plan should be directed to: Aboriginal Engagement, Planning and Lands Branch Department of Biodiversity, Conservation and Attractions Locked Bag 104 Bentley Delivery Centre WA 6983 Phone: (08) 9219 9000 The recommended reference for this publication is: Department of Biodiversity, Conservation and Attractions (2021) Houtman Abrolhos Islands National Park draft management plan, 2021. Department of Biodiversity, Conservation and Attractions, Perth. This document is available in alternative formats on request. Front