NPWS Inishmore Island SAC (Site Code: 213) Conservation Objectives
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New Zealand Oceanographic Institute Memoir 100
ISSN 0083-7903, 100 (Print) ISSN 2538-1016; 100 (Online) , , II COVER PHOTO. Dictyodendrilla cf. cavernosa (Lendenfeld, 1883) (type species of Dictyodendri/la Bergquist, 1980) (see page 24), from NZOI Stn I827, near Rikoriko Cave entrance, Poor Knights Islands Marine Reserve. Photo: Ken Grange, NZOI. This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ NATIONAL INSTITUTE OF WATER AND ATMOSPHERIC RESEARCH The Marine Fauna of New Zealand: Index to the Fauna 2. Porifera by ELLIOT W. DAWSON N .Z. Oceanographic Institute, Wellington New Zealand Oceanographic Institute Memoir 100 1993 • This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ Cataloguing in publication DAWSON, E.W. The marine fauna of New Zealand: Index to the Fauna 2. Porifera / by Elliot W. Dawson - Wellington: New Zealand Oceanographic Institute, 1993. (New Zealand Oceanographic Institute memoir, ISSN 0083-7903, 100) ISBN 0-478-08310-6 I. Title II. Series UDC Series Editor Dennis P. Gordon Typeset by Rose-Marie C. Thompson NIWA Oceanographic (NZOI) National Institute of Water and Atmospheric Research Received for publication: 17 July 1991 © NIWA Copyright 1993 2 This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ CONTENTS Page ABSTRACT 5 INTRODUCTION 5 SCOPE AND ARRANGEMENT 7 SYSTEMATIC LIST 8 Class DEMOSPONGIAE 8 Subclass Homosclcromorpha .............................................................................................. -
Cape Wrath Survey
Cape Wrath Survey diver & guillemot May 2002 marbled swimming crab Summary Report velvet crab & gooseberry seasquirts brittlestars in pitted limestone tideswept kelp forest lemon sole Cape Wrath Survey North Coast As well as being a famous nautical Sites 9, 19, 20 and 21 on the north coast were swept by strong currents, and exposed to waves from landmark, Cape Wrath marks a northerly directions. Cuvie kelp forests grew in shallow water, with dense red algae (Delesseria geographical and biological sanguinea, Plocamium cartilagineum, Phycodrys rubens and Odonthalia dentata) on stipes and on boundary between the exposed, rocks beneath. At the extremely exposed offshore rock Duslic (Site 19), clumps of blue mussels current-swept north coast and grew on kelp stipes, and breadcrumb sponge was common wrapped around kelp stipes at several Pentland Firth, and the more gentle sites. In deeper water, animal turfs covered rocks. Dominant animals varied from site to site, but waters of the Minch. The survey colonial and small solitary seasquirts were particularly abundant. At An Garb Eilean (Site 9), a small covered 24 sites spread over a island used by the military for target practice, north-east facing rock slopes were covered with dense large area of this spectacular part oaten-pipe sea fir Tubularia indivisa, together with abundant elegant anemones on vertical faces. of north-west Scotland. Where rocks were scoured by nearby sand, bushy sea mats Securiflustra securifrons and Flustra foliacea were common, with featherstars and scattered jewel anemones on vertical faces. Cape Wrath Faraid Head Cape Wrath (Site 15) proved as spectacular underwater as above, with wave-battered slopes covered with cuvie kelp Rock and boulders at Sites 10 and 11, slightly sheltered (Laminaria hyperborea), and a dense short turf of animals from the main current by offshore rocks had little beneath the kelp and in deeper water. -
California's Coastal Sea Caves, NSS News, October 1998
California’s Coastal Sea Caves by Dave Bunnell Large chamber in Cave-in-Rock Cave, San Luis Obispo County elmets, lights, wetsuits, fins, face California, with its more accessible caves, are undoubtedly caves in Humboldt and Del masks and snorkels, vertical gear, has yielded as many again to the surveyor’s Norte counties, no survey work has been H and sea kayaks were not what I was tape and doubtless many more remain, undertaken there. I’ll begin with the southern used to packing for a cave trip until I especially in the remote northern counties. counties, for that was the original focus of moved to California. But after a couple of Much has been published over the years in sea cave survey. years of caving here, I realized that there were grotto and regional publications, but this is large numbers of caves here that had been the first time I’ve written an overall summary SAN DIEGO COUNTY largely ignored. After all, what caver wants of the Survey’s work on coastal caves. Perhaps the most famous of the sea caves to spend his weekends at the beach? on the California coast are the “seven caves” Systematic exploration and survey of GENERALITIES at La Jolla, formed in a 200’ high cliff of California’s many sea caves really began While not as large on average as the Cretaceous-age sandstone. A perennial when Carol Vesely and I chartered the island caves, the coastal caves are found in tourist favorite, La Jolla Cove and its cavey Southern California Sea Cave Survey in numerous host rocks that lend diverse cliffs are featured on dozens of old postcards. -
Beaches Unit (4.5 Pts) Section
T. James Noyes, El Camino College Beaches Unit (Topic 6A) – page 1 Name: Beaches Unit (4.5 pts) Section: Beaches and Shorelines are always changing Waves are slowly and inexorably altering the shoreline, breaking down material in some places and carrying it to other places. Each wave has a small effect, but waves keep coming minute after minute, day after day, year after year. Significant changes in the shoreline (tens of feet) can occur within a human lifetime. For example, old maps of Encinitas (located along the coastal cliffs by Interstate 5 on the way down to San Diego) show that it has lost about a city block of land to the sea in the last century. In some places along the coast of Alaska, the shoreline has eroded 900 meters in 50 years, an average of about 18 meters (60 feet) per year! Beach Sediments Beach sediments are composed of whatever sediments are available locally: sand, cobbles, gravel, coral fragments, shell fragments, and so on. (In fact, tiny plastic sediments are making up a larger and larger component of our beaches.) Beach sediments are characterized by (1) the kind of material that they are made out of, (2) their size, (3) their shape, and (4) their sorting. (Well sorted sediments all have about the same size and shape, while poorly sorted sediments are a jumbled mix of sediments with many different sizes and shapes. Lithogenous sediments (“rock sediments”) are produced from the weathering of the rock of the land. Rocks are broken down into pieces (sediments) by the physical impact of water, wind, and other rocks; by chemicals dissolved in water; and repeated heating and cooling. -
A New Species of the Calcareous Sponge Genus Leuclathrina (Calcarea: Calcinea: Clathrinida) from the Maldives
Zootaxa 4382 (1): 147–158 ISSN 1175-5326 (print edition) http://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2018 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4382.1.5 http://zoobank.org/urn:lsid:zoobank.org:pub:B222C2D8-82FB-414C-A88F-44A12A837A21 A new species of the calcareous sponge genus Leuclathrina (Calcarea: Calcinea: Clathrinida) from the Maldives OLIVER VOIGT1,5, BERNHARD RUTHENSTEINER2, LAURA LEIVA1, BENEDETTA FRADUSCO1 & GERT WÖRHEIDE1,3,4 1Department of Earth and Environmental Sciences, Palaeontology and Geobiology, Ludwig-Maximilians-Universität München, Rich- ard-Wagner-Str. 10, 80333 München, Germany 2 SNSB - Zoologische Staatssammlung München, Sektion Evertebrata varia, Münchhausenstr. 21, 81247 München, Germany 3 GeoBio-Center, Ludwig-Maximilians-Universität München, Richard-Wagner-Str. 10, 80333 München, Germany 4SNSB - Bayerische Staatssammlung für Paläontologie und Geologie, Richard-Wagner-Str. 10, 80333 München, Germany 5Corresponding author. E-mail: [email protected], Tel.: +49 (0) 89 2180 6635; Fax: +49 (0) 89 2180 6601 Abstract The diversity and phylogenetic relationships of calcareous sponges are still not completely understood. Recent integrative approaches combined analyses of DNA and morphological observations. Such studies resulted in severe taxonomic revi- sions within the subclass Calcinea and provided the foundation for a phylogenetically meaningful classification. However, several genera are missing from DNA phylogenies and their relationship to other Calcinea remain uncertain. One of these genera is Leuclathrina (family Leucaltidae). We here describe a new species from the Maldives, Leuclathrina translucida sp. nov., which is only the second species of the genus. Like the type species Leuclathrina asconoides, the new species has a leuconoid aquiferous system and lacks a specialized choanoskeleton. -
Adventure Sea Cave Kayak Tours on Santa Cruz Island at Scorpion Anchorage
ADVENTURE SEA CAVE KAYAK TOURS ON SANTA CRUZ ISLAND AT SCORPION ANCHORAGE THIS IS NOT A BOOKING CONFIRMATION. The information below is only for reference. Please make sure to reference your booking confirmation sent via email for exact times and locations. If you have any questions please contact the Channel Islands Adventure Company - we will be happy to help you. Paddling Time and Distance 2.5-3 miles, 2.5-3 hours of island kayaking Tour Level of Difficulty Beginner through advanced experience levels welcome. Children under 12 must ride in double kayak with a parent. Adventure Sea Cave Kayak Tour Itinerary Your morning will begin at the Island Packers ferry dock for check-in at either 7am or 8am, depending on which ferry departure time you select (8am departure or 9am departure). You’ll want to look for Channel Islands Adventure Company guides just outside of the Island Packers building. Your guide will have your tickets. Detailed driving directions will be sent upon booking in your confirmation email. The ferry ride is generally 1-1.5 hour(s) depending on wildlife sightings. You’ll then meet your guide(s) on the island at 10:30am.We provide a basic paddling instruction/safety talk and distribute all necessary gear before hitting the water around 11:15am. Afterward we begin the guided paddle along the coast in one direction, exploring the sea caves as you go. At some point you turn around and come back past the landing area and explore in the other direction. You’ll return to the beach around 2:00-2:30pm, and have until about 3:30–4:30pm (your ferry captain or guide will tell you your pick-up time) before leaving the island. -
Kelp Forest Monitoring Handbook — Volume 1: Sampling Protocol
KELP FOREST MONITORING HANDBOOK VOLUME 1: SAMPLING PROTOCOL CHANNEL ISLANDS NATIONAL PARK KELP FOREST MONITORING HANDBOOK VOLUME 1: SAMPLING PROTOCOL Channel Islands National Park Gary E. Davis David J. Kushner Jennifer M. Mondragon Jeff E. Mondragon Derek Lerma Daniel V. Richards National Park Service Channel Islands National Park 1901 Spinnaker Drive Ventura, California 93001 November 1997 TABLE OF CONTENTS INTRODUCTION .....................................................................................................1 MONITORING DESIGN CONSIDERATIONS ......................................................... Species Selection ...........................................................................................2 Site Selection .................................................................................................3 Sampling Technique Selection .......................................................................3 SAMPLING METHOD PROTOCOL......................................................................... General Information .......................................................................................8 1 m Quadrats ..................................................................................................9 5 m Quadrats ..................................................................................................11 Band Transects ...............................................................................................13 Random Point Contacts ..................................................................................15 -
Oce1001, Introduction to Oceanography, Fall, 2005
OCE1001, INTRODUCTION TO OCEANOGRAPHY, Fall, 2018 THIRD MID-TERM EXAMINATION Test No. 0001 Name: __________________________ READ THIS!!!! Put your name in the blank above. Read all questions carefully, and answer only the question which is asked. You may find the following equations useful: C = (gL/2) = 1.25 L (m/s) Where: C = speed of a wave and: g = gravity = 9.8 m/s2 C = (gD) = 3.1 D (m/s) L = wavelength of a wave C = 1.56 T (m/s) D = water depth C = L/T T = period of a wave PLEASE WRITE NEATLY. Matching: The Beaches Are Moving (8 pts) Do not put these on the scantron sheet. ____ neap ____ hook A. worldwide change in sea level. B. structure intended to widen a beach. ____ jetty ____ groin C. wall intended to keep a channel open. D. two high and two low tides per day. ____ eustatic E. current parallel to the shore caused by waves. ____ semidiurnal F. twice monthly tide that with a smaller than average range. ____ marine terrace G. bend in end of a spit caused by wave refraction. ____ longshore current H. region eroded flat by waves, elevated above sea level. ____ longitudinal I. disturbance of wave is parallel to wave movement Multiple Choice: (2 pts each) Put the answers to these questions on the scantron sheet. 1. In Figure 1, the features labeled 1, 2, 3, 4, and 5 are, respectively: a. spit, barrier island, baymouth bar, hook, tombolo. b. hook, spit, baymouth bar, barrier island, tombolo. c. tombolo, spit, baymouth bar, barrier island, hook. -
Cave and Karst Inventory and Analysis
Preliminary Report on the Caves and Karst of ROTA (LUTA), CNMI Thomas M. Keel1,2, John E. Mylroie1 & John W. Jenson2 i Technical Report No. 105 September 2004 Preliminary Report on the Caves and Karst of ROTA (LUTA), CNMI Thomas M. Keel1,2, John E. Mylroie1 & John W. Jenson2 1Department of Geosciences Mississippi State University Mississippi State, MS 39762 2Water and Environmental Research Institute of the Western Pacific University of Guam Mangilao, Guam 96923 Technical Report No. 105 Water & Environmental Research Institute of the Western Pacific University of Guam September, 2004 THE WATER RESOURCES RESEARCH INSTITUTE PROGRAM OF THE US GEOLOGICAL SURVEY, AWARD NO. 01HQGR0134, SUPPORTED THE WORK REPORTED HERE. THE CONTENT OF THIS REPORT DOES NOT NECESSARILY REFLECT THE VIEWS AND POLICIES OF THE DEPARTMENT OF THE INTERIOR, NOR DOES THE MENTION OF TRADE NAMES OR COMMERCIAL PRODUCTS CONSTITUTE THEIR ENDORSEMENT BY THE UNITED STATES GOVERNMENT. i ABSTRACT The island of Rota, Commonwealth of the Northern Mariana Islands, contains caves developed by most of the mechanisms previously documented for similar islands. Rota has a large number of flank margin caves, developed by mixing dissolution, under diffuse flow conditions, at the edge of the fresh water lens. Rota has a few caves developed along the contact with the underlying volcanic rock. Rota also has a few caves formed primarily by the physical erosion of ocean waves. Unlike the other islands in the Mariana Arc, Rota has a large number of mixing zone fracture caves. These mixing zone fracture caves apparently developed as fresh water discharging from the fractures mixesd with sea water to create zones of enhanced dissolution in each fracture. -
Apostle Islands National Lakeshore Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Apostle Islands National Lakeshore Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2015/972 ON THIS PAGE An opening in an ice-fringed sea cave reveals ice flows on Lake Superior. Photograph by Neil Howk (National Park Service) taken in winter 2008. ON THE COVER Wind and associated wave activity created a window in Devils Island Sandstone at Devils Island. Photograph by Trista L. Thornberry-Ehrlich (Colorado State University) taken in summer 2010. Apostle Islands National Lakeshore Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2015/972 Trista L. Thornberry-Ehrlich Colorado State University Research Associate National Park Service Geologic Resources Division Geologic Resources Inventory PO Box 25287 Denver, CO 80225 May 2015 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate comprehensive information and analysis about natural resources and related topics concerning lands managed by the National Park Service. The series supports the advancement of science, informed decision-making, and the achievement of the National Park Service mission. The series also provides a forum for presenting more lengthy results that may not be accepted by publications with page limitations. -
Geology of Saipan Mariana Islands Part 4
Geology of Saipan Mariana Islands Part 4. Submarine Topography and Shoal- Water Ecology GEOLOGICAL SURVEY PROFESSIONAL PAPER 280-K Geology of Saipan Mariana Islands Part 4. Submarine Topography and Shoal- Water Ecology By PRESTON E. CLOUD, Jr. GEOLOGICAL SURVEY PROFESSIONAL PAPER 280-K Description and interpretation of the submarine topography and of the sediments^ biotas^ and morphology of the reef complex adjacent to a geologically diverse tropical island UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. S EATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. GEOLOGICAL SURVEY PROFESSIONAL PAPER 280 Geology of Saipan, Mariana Islands Part 1. General Geology A. General Geology By PRESTON E. CLOUD, Jr., ROBERT GEORGE SCHMIDT, and HAROLD W. BURKE Part 2. Petrology and Soils B. Petrology of the Volcanic Rocks By ROBERT GEORGE SCHMIDT C. Petrography of the Limestones By J. HARLAN JOHNSON D. Soils By RALPH J. McCRACKEN Part 3. Paleontology E. Calcareous Algae By J. HARLAN JOHNSON F. Difcoaster and Some Related Microfossils By M. N. BRAMLETTE G. Eocene Radiolaria By WILLIAM RIEDEL H. Smaller Foraminifera By RUTH TODD I. Larger Foraminifera By W. STORRS COLE J. Echinoids By C. WYTHE COOKE Part 4. Submarine Topography and Shoal-Water Ecology K. Submarine Topography and Shoal-Water Ecology By PRESTON E. CLOUD, Jr. CONTENTS Page Page Abstract_________________________________________ 361 Shoal-water and shoreline ecology and sediments—Con. Introduction. ______________________________________ 362 Habitat descriptions—Con. Purpose and scope of the work_____________________ 362 Organic reefs and reef benches______________ 383 Field methods and acknowledgments-_______________ 362 Minor reef structures______________________ 384 Systematic identifications and other research aid____ 363 Biotope X. -
General Coastal Notes + Landforms! 1
General Coastal Notes + Landforms! 1 Types of Coastlines: Type Description Primary Coast which is essentially in the same condition when sea level stabilized Coastline after the last ice age, “younger”. They are created by erosion (the wearing away of soil or rock), deposition (the buildup of sediment or sand) or tectonic activity (changes in the structure of the rock and soil because of earthquakes). River deltas are an example of a primary coast. They form where a river deposits soil and other material as it enters the sea. Secondary Coastline shaped primarily by marine forces or marine organisms, and wave Coastline energy is the main agent shaping the coastline. Emergent Emergent coastlines are stretches along the coast that have been exposed by Coastline the sea due to a relative fall in sea levels. Submergent Submergent coastlines are stretches along the coast that have been Coastline inundated by the sea due to a relative rise in sea levels. Concordant A coastline consisting of bands of rock, which run parallel to the coast. Coastline Discordant A discordant coastline occurs where bands of differing rock type run Coastline perpendicular to the coast. Factors affecting Wave Energy: Factor: Description Wind Speed Wind speed will in turn affect wind energy, which determines the size of the waves. Higher wind speed = Higher wind energy = Larger waves Fetch Fetch is the distance of the ocean which the wind blows over, Longer distance = Larger waves Wind How long the wind has blown in the same direction (steady winds at slower Duration