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D 6785 (L) Diary of Gilbert Mcdougall Recording His Observations of the Flora and Fauna Around Yorke Peninsula from 2 January 1886 to 16 October 1887 with an Index
_______________________________________________________________________________________ D 6785 (L) Diary of Gilbert McDougall recording his observations of the flora and fauna around Yorke Peninsula from 2 January 1886 to 16 October 1887 with an index. Transcribed by Judy Fander, Volunteer at the State Library of South Australia, 2012. Dropped out of manuscript: two watercolour drawings of two different unnamed insects on small cards. Now housed separately with the diary. Also one small drawing of a seed found between p173 and 174. On the fly leaf: J C McDougall, c/o National Bank, Adelaide Natural History Notes. 1886 Edithburgh, Y.P. Jan.2. Hunting on the rocks down at Gottschalck’s Jetty, & found several varieties of Cominella,a number of which were feeding on a dead Chiton. Several Dromiae, strange brown hairy crabs having their backs covered by a closely-fitting but unattached zoophyte ore sponge; also a couple of Chitonellus Gunni ( ), a genus of Chitonidae in which the plates are very small & narrow & imbedded at intervals along the cartilaginous back of the mollusc. Received a letter from Pulleine to whom I had sent a specimen of the black-faced Artamus which was so abundant a couple of months ago. It is the Masked Wood Swallow (Artamus personatus), a species of periodical occurrence. I have 3 good skins, & 2 eggs. The nest is si placed in similar situations to those of A. sordidus & the construction is pretty much the same, loose twigs with no lining. The male bird has a rusty red breast & is very un- Page 3. Opposite page 4 Reference date Cyclodus gigas Jan 4. -
Late Cretaceous-Early Palaeogene Echinoderms and the K/T Boundary in the Southeast Netherlands and Northeast Belgium — Part 6: Conclusions
pp 507-580 15-01-2007 14:51 Pagina 505 Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 6: Conclusions John W.M. Jagt Jagt, J.W.M. Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 6: Conclusions. — Scripta Geol., 121: 505-577, 8 figs., 9 tables, Leiden, December 2000. John W.M. Jagt, Natuurhistorisch Museum Maastricht, Postbus 882, NL-6200 AW Maastricht, The Netherlands, E-mail: [email protected] Key words: Echinodermata, Late Cretaceous, Early Palaeogene, palaeobiology, K/T boundary, extinc- tion. The palaeobiology of echinoderms occurring in the Meerssen and Geulhem members is discussed and changes in diversity across the K/T boundary are documented. Using literature data on the ecology of extant faunas, the various echinoderm groups are considered. Naturally, such data can only be applied with due caution to fossil forms, whose skeletal morphology is often incompletely known. This holds especially true for asteroids, ophiuroids, and crinoids, which, upon death, rapidly disinte- grate into jumbles of dissociated ossicles. Bioturbation, scavenging, and current winnowing all con- tribute to blurring the picture still further. However, data on extant forms do allow a preliminary sub- division of fossil species into various ecological groups, which are discussed herein. Combining recently published data on K/T boundary sections in Jylland and Sjælland (Denmark) with the pic- ture drawn here for the Maastricht area results in the following best constrained scenario. The demise of the highly diverse latest Maastrichtian echinoderm faunas, typical of shallow-water settings with local palaeorelief and associated unconsolidated bottoms, was rapid, suggestive of a catastrophic event (e.g. -
Chapter 21. Fauna of Jetty Piles, Artificial Reefs and Biogenic Surfaces
Chapter 21. Fauna of jetties and artificial reefs CHAPTER 21. FAUNA OF JETTY PILES, ARTIFICIAL REEFS AND BIOGENIC SURFACES ALAN BUTLER C.S.I.R.O. Marine Research, Hobart, Tasmania 7001. Email: [email protected] Figure 1. Piling of Edithburgh jetty showing sponges, ascidians and bryozoans. (CAS) Introduction This chapter is not a comprehensive description or natural history of the fauna of all jetties, artificial reefs and biogenic surfaces in Gulf St Vincent (GSV) and its approaches. It is about studies done on certain jetties, etc., in the Gulf, using them as experimental systems to increase our understanding of the larger ecosystem of which they are a part. I think of the fauna attached to pilings, artificial reefs and biogenic surfaces as a window on that larger system. Pilings have been convenient places to do experiments and make repeated observations. It has to be remembered, however, that the organisms we are studying on such surfaces are part of larger populations. They have dispersive larvae which may travel short to long distances with the currents; they have predators that move about; the assemblage on one jetty is thus connected to assemblages on other jetties and reefs. We can learn a great deal by observations and experiments at the small scale, but ultimately it only makes sense if we can successfully ‘scale up’—understand these habitats in the context of the system in which they are embedded. I say more, at the end, about this ‘scaling up’. Also, the jetties etc. are artificial—a type of substratum that was not present during the millions of years of evolution of these organisms—and are, in various respects, different from their ‘natural’ habitats. -
(Echinodermata: Holothuroidea) from the Latest Cretaceous Of
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Universität München: Elektronischen Publikationen 285 Zitteliana 89 Short Communication First report of sea cucumbers (Echinodermata: Holothuroidea) from the latest Cretaceous of Paläontologie Bayerische Bavaria,GeoBio- Germany & Geobiologie Center Staatssammlung 1,2,3 LMU München für Paläontologie und Geologie LMUMike MünchenReich 1 n München, 01.07.2017 SNSB - Bayerische Staatssammlung für Paläontologie und Geologie, Richard-Wagner-Straße 10, 80333 Munich, Germany 2 n Manuscript received Ludwig-Maximilians-Universität München, Department für Geo- und Umweltwissenschaften, 30.12.2016; revision ac- Paläontologie und Geobiologie, Richard-Wagner-Straße 10, 80333 Munich, Germany 3 cepted 21.01.2017 GeoBio-Center der Ludwig-Maximilians-Universität München, Richard-Wagner-Straße 10, 80333 Munich, Germany n ISSN 0373-9627 E-mail: [email protected] n ISBN 978-3-946705-00-0 Zitteliana 89, 285–289. Key words: fossil Holothuroidea; Cretaceous; Maastrichtian; Bavaria; Germany Schüsselwörter: fossile Holothuroidea; Kreide; Maastrichtium; Bayern; Deutschland The Bavarian Gerhardtsreit Formation (‶Gerhardts- 1993; Smith 2004) due to different reasons (Reich reiter Mergel″ / ‶Gerhardtsreiter Schichten″; cf. 2013). There are nearly 1,700 valid extant sea cucum- Böhm 1891; Hagn 1960; Wagreich et al. 2004), also ber species (Smiley 1994; Kerr 2003; Paulay pers. known as Gerhartsreit Formation (‶Gerhartsreiter comm.) known worldwide. The fossil record (since Schichten″; Hagn et al. 1981, 1992; Schwarzhans the Middle Ordovician; Reich 1999, 2010), by con- 2010; Pollerspöck & Beaury 2014) or ‶Gerhards- trast, is discontinuous in time and recorded ranges reuter Schichten″ (Egger 1899; Hagn & Hölzl 1952; of species with around 1,000 reported forms (Reich de Klasz 1956; Herm 1979, 2000) is exposed in Up- 2013, 2014, 2015b) since the early 19th century. -
Great Barrier Reef Marine Park ZONING PLAN 2003
Great Barrier Reef Marine Park ZONING PLAN 2003 Great Barrier Reef Marine Park Zoning Plan 2003 Published by the Great Barrier Reef Marine Park Authority, May 2004 © Great Barrier Reef Marine Park Authority Great Barrier Reef Marine Park zoning plan 2003. ISBN 1 876945 38 9. 1. Zoning - Queensland - Great Barrier Reef Marine Park. 2. Great Barrier Reef Marine Park (Qld.). I. Great Barrier Reef Marine Park Authority. 333.916409943 2 - 68 Flinders Street John Gorton Building PO Box 1379 King Edward Terrace TOWNSVILLE QLD 4810 PARKES ACT 2600 Phone: (07) 4750 0700 PO Box 791 Facsimile: (07) 4772 6093 CANBERRA ACT 2601 Freecall: 1800 990 177 Email: [email protected] Phone: (02) 6274 1922 Facsimile: (02) 6274 1509 www.gbrmpa.gov.au Great Barrier Reef Marine Park Zoning Plan 2003 I, DAVID ALiSTAU~ KEMP, Minister for the Environment and Heritage, accept this Zoning Plan under subsecti on 32 (It) of the Greal Barrier Reef Marine Park Act 1975. Dated 2. ~ ~ 2003 , Minister for the Environment and eritage This page is intentionally blank. Contents Page Contents Preface 1 A Introduction 1 B The Amalgamated Great Barrier Reef Section 2 C The Great Barrier Reef Marine Park Zoning Plan 4 D Additional management provisions 6 E Zoning maps 7 Part 1 Preliminary 1.1 Name of Zoning Plan 11 1.2 Commencement 11 1.3 Application of Zoning Plan 11 1.4 Revocation of previous Zoning Plans 11 1.5 Interpretation — general 11 1.6 Interpretation — geographic coordinates etc 12 1.7 Application of Queensland, Commonwealth and international law 14 1.8 Lawful taking of -
An Illustrated Key to the Sea Cucumbers of the South Atlantic Bight
Prepared by the Southeastern Regional Taxonomic Center AAnn iilllluussttrraatteedd kkeeyy ttoo tthhee sseeaa ccuuccuummbbeerrss ooff tthhee SSoouutthh AAttllaannttiicc BBiigghhtt David L. Pawson and Doris J. Pawson Smithsonian Institution, PO Box 37012, MRC 163, Washington, DC 20013-7012 1 Table of Contents Introduction ..........................................................................................................................3 General Morphology (internal) ................................................................................3 General morphology (external) ................................................................................4 Preparation of ossicles .............................................................................................4 Checklist of South Atlantic Bight holothuroideans ............................................................5 Key to Orders of Holothuroidea known from the South Atlantic Bight ..............................6 Key to members of the Order Dendrochirotida known from the South Atlantic Bight .......9 Key to species of the Aspidochirotida known from the South Atlantic Bight...................28 Key to species of the Molpadiida known from the South Atlantic Bight ..........................34 Key to species of the Apodiida known from the South Atlantic Bight .............................35 This document was prepared by Rachael A. King and is only part of a more extensive study that is expected to be published in 2008. The research was conducted in part using funding -
(Echinodermata) Collected During the TALUD Cruises Off the Pacific Coast of Mexico, with the Description of Two New Species Revista Mexicana De Biodiversidad, Vol
Revista Mexicana de Biodiversidad ISSN: 1870-3453 [email protected] Universidad Nacional Autónoma de México México Massin, Claude; Hendrickx, Michel E. Deep-water Holothuroidea (Echinodermata) collected during the TALUD cruises off the Pacific coast of Mexico, with the description of two new species Revista Mexicana de Biodiversidad, vol. 82, núm. 2, junio, 2011, pp. 413-443 Universidad Nacional Autónoma de México Distrito Federal, México Available in: http://www.redalyc.org/articulo.oa?id=42521043005 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Biodiversidad 82: 413-443, 2011 Deep-water Holothuroidea (Echinodermata) collected during the TALUD cruises off the Pacific coast of Mexico, with the description of two new species Holothuroidea (Echinodermata) de mar profundo recolectadas durante las campañas TALUD frente a la costa del Pacífico mexicano, con la descripción de dos especies nuevas Claude Massin1 and Michel E. Hendrickx2* 1Department of Recent Invertebrates, Royal Belgian Institute of Natural Sciences, Rue Vautier 29, Brussels, B-1000, Belgium. 2Unidad Académica Mazatlán, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, PO Box 811, 82000 Mazatlán, Sinaloa, México. *Correspondent: [email protected] Abstract. Research cruises aboard the R/V “El Puma” were organized to collect deep-water benthic and pelagic specimens off the Pacific coast of Mexico. Seventy four specimens of Holothuroidea were collected off the Pacific coast of Mexico in depths of 377-2 200 m. -
Mapping and Distribution of Sabella Spallanzanii in Port Phillip Bay Final
Mapping and distribution of Sabellaspallanzanii in Port Phillip Bay Final Report to Fisheries Research and Development Corporation (FRDC Project 94/164) G..D. Parry, M.M. Lockett, D.P. Crookes, N. Coleman and M.A. Sinclair May 1996 Mapping and distribution of Sabellaspallanzanii in Port Phillip Bay Final Report to Fisheries Research and Development Corporation (FRDC Project 94/164) G.D. Parry1, M. Lockett1, D. P. Crookes1, N. Coleman1 and M. Sinclair2 May 1996 1Victorian Fisheries Research Institute Departmentof Conservation and Natural Resources PO Box 114, Queenscliff,Victoria 3225 2Departmentof Ecology and Evolutionary Biology Monash University Clayton Victoria 3068 Contents Page Technical and non-technical summary 2 Introduction 3 Background 3 Need 4 Objectives 4 Methods 5 Results 5 Benefits 5 Intellectual Property 6 Further Development 6 Staff 6 Final cost 7 Distribution 7 Acknow ledgments 8 References 8 Technical and Non-technical Summary • The sabellid polychaete Sabella spallanzanii, a native to the Mediterranean, established in Port Phillip Bay in the late 1980s. Initially it was found only in Corio Bay, but during the past fiveyears it has spread so that it now occurs throughout the western half of Port Phillip Bay. • Densities of Sabella in many parts of the bay remain low but densities are usually higher (up to 13/m2 ) in deeper water and they extend into shallower depths in calmer regions. • Sabella larvae probably require a 'hard' surface (shell fragment, rock, seaweed, mollusc or sea squirt) for initial attachment, but subsequently they may use their own tube as an anchor in soft sediment . • Changes to fish communities following the establishment of Sabella were analysed using multidimensional scaling and BACI (Before, After, Control, Impact) design analyses of variance. -
The Following Notice to Mariners Is
LOCAL NAVIGATION WARNING GIPPSLAND PORTS The following navigation warning is published for general information. AUSTRALIA - VICTORIA LNW NO.1 OF 2021 GIPPSLAND PORTS NAVIGATION ADVICE OCEAN ACCESS BAR CROSSINGS ARE DANGEROUS DATE: Tuesday 9th March 2021 PREVIOUS Local Navigation Warning No10 of 2018 is referred. NOTICE: DETAILS: A recent Marine Incident has occurred at McLoughlins Beach ocean access entrance highlighting the risks involved for vessel operators attempting to make passage through and across ocean entrance sand bars. Gippsland Ports is the Local Port Manager for 5 Local Ports; Each of the following ports is a recognised Bar Port. • Port of Corner Inlet and Port Albert • Port of Gippsland Lakes • Port of Anderson Inlet • Port of Snowy River (Marlo) • Port of Mallacoota Inlet. Only the Ports of Corner Inlet, Port Albert and the Gippsland Lakes (Lakes Entrance Bar) have recognised aids to navigation to guide the Mariner through and across their respective ocean entrance sand bars. The entrances to these ports remain open at all times, however sound local knowledge and favorable environmental conditions are required to make a safe passage. The Port of Snowy River (Marlo), Port of Mallacoota Inlet and Port of Anderson Inlet are dynamic in nature with ever changing channel configuration and depths. Ocean access can be closed off at Marlo and Mallacoota during times of drought. There are no aids to navigation to guide the mariner through and across their respective ocean entrance sand bars. Lake Tyers - Sydenham Inlet and Tamboon Inlet, all remain closed until sufficient back up of water creates an ocean access entrance. -
Cape Liptrap Coastal Park Visitor Guide
Cape Liptrap Coastal Park Visitor Guide Stretching along the coast from the sand barrier of Point Smythe, to the sheltered waters of Waratah Bay - Cape Liptrap Coastal Park has strikingly beautiful scenery. The coastal park transforms from being a peaceful coastal area to wild, windy and awe-inspiring in stormy weather. With Cambrian rocks and Recent sands, the occurrence of about 270 species of flowering plants including 27 orchids, as well as supporting threatened flora and fauna species – Cape Liptrap Coastal Park is a highly valuable area in Victoria’s parks and reserves network. Getting there Dogs Cape Liptrap Coastal Park is 4,175 ha in size and is situated 160 Dogs are permitted in the following areas of Cape Liptrap Coastal kilometres south east of Melbourne. Park: Things to see and do between Walkerville North and Walkerville South between Venus Bay Number 1 and Number 5 Beaches Walking between Waratah Bay township and Cooks Creek Dogs in the above areas are required to be on a lead at all times and Point Smythe Walk – 6km, 1 hour one way are prohibited from these areas between 9am – 6pm from 1st December until 31st March. These measures protect the Hooded Grade 3 Plovers; a ground nesting bird listed as Vulnerable. Dogs are This circuit takes you through thick coastal vegetation leading to the prohibited in all other areas of Cape Liptrap Coastal Park. beach at Point Smythe. The track is particularly sheltered on windy days. Horse Riding Horse riding is permitted within the park on the intertidal area of Bald Hills Wetland Walk – 750 metres, 15 minutes beach below the high-water mark, between the ocean outfall one way pipeline of Venus Bay and Arch Rock. -
Chapter 18. Razor Fish and Scallops
Chapter 18. Razorfish and scallops CHAPTER 18. RAZOR FISH AND SCALLOPS ALAN BUTLER CSIRO Marine and Atmospheric Research, Hobart, Tasmania 7001. Email: [email protected] Figure 1. Razorfish Pinna bicolor near seagrass, Posidonia sp. The individual in foreground shows some recent, rapid growth at the posterior margin of the shell and an epifauna mainly of serpulids but with a gastropod, a few bryozoans, and a small colony of a didemnid ascidian beginning to overgrow the bryozoans. The shell in the background is dead, may have been there for a decade, and has a well-developed epifauna, mainly of bryozoans with a couple of sponge colonies. Introduction This chapter outlines some ecological studies of bivalve molluscs in Gulf St Vincent (GSV) waters. It is eclectic, not attempting to cover all studies of bivalves, but mainly those of several large species—the ‘razor fish’ Pinna bicolor, and the scallops Mimachlamys asperrima and Equichlamys bifrons—which are conspicuous, and have proven instructive not only for understanding the ecology of these sorts of animals (sessile filter-feeders, with broadcast spawning, external fertilisation and a long larval period), but of the dynamics of the Gulf ecosystem and of the relationships between species. A vast amount has been written about the ecology of bivalves worldwide (e.g. Wilbur & Yonge 1964- 1966; Bayne 1976; Yonge & Thompson 1976; Purchon 1977; Wilbur 1983-1988; Suchanek 1985; Ludbrook & Gowlett-Holmes 1989; Beesley et al. 1998), and no attempt is made to summarise it here. 238 Chapter 18. Razorfish and scallops Razor fish ‘Razor fish’ are bivalve molluscs, not fish. -
16. Jetties, Shipwrecks and Other Artificial Reefs
Jetties, shipwrecks and other artificial reefs. Chapter 16 in: Baker, J.L. (2015) Marine Assets of Yorke Peninsula. Report for Natural Resources - Northern and Yorke / NY NRM Board, South Australia. 16. Jetties, Shipwrecks and Other Artificial Reefs Edithburgh Kleins Point © D. Kinasz © J. Zhang Asset Jetties, Shipwrecks and other Artificial Reefs Description Structures of wood, iron, steel, and other materials, throughout the NY NRM region, ranging from oceanographically exposed through to sheltered locations. Jetties and shipwrecks function as surfaces for attachment of marine plants and attached invertebrates; sheltering and feeding areas for fishes, sharks, rays and invertebrates; and as “fish-attracting” devices, periodically visited by schooling fishes which are attracted to vertical structure. Surrounding sea floor varies according to the location of the jetty or wreck, and includes reef, seagrass, sand, and rubble. There are also two purpose-built artificial reefs in the NY NRM region, constructed of tetrahedon module units, made up vehicle tyres. Main Species Sponges sponges (numerous species, in genera Dysidea, Euryspongia, Darwinella, Aplysilla, Dendrilla, Clathrina and many others) Ascidians / Sea Squirts Red-mouthed Ascidian, Obese Ascidian, and other solitary ascidians / sea squirts Brain Ascidian, and other colonial ascidians Spongy Compound, Leach’s Compound & other compound ascidians Corals gorgonian corals such as Mopsella zimmeri (on current-exposed jetties) soft corals, such as Carijoa (also Drifa sp. on current-exposed jetties) solitary coral Scolymia Bryozoans various species, including various species in Cellaporaria (such as Orange Plate Bryozoan and Nipple Bryozoan) and species in Triphyllozoon (Lace Bryozoans) Gastropod Shells Cowries, Cartrut shell, Triton shells Bivalve Shells Doughboy Scallop, Razorfish Shell, juvenile Native Oyster Jetties, shipwrecks and other artificial reefs.