The Tautra Cold-Water Coral Reef

Total Page:16

File Type:pdf, Size:1020Kb

The Tautra Cold-Water Coral Reef The Tautra Cold-Water Coral Reef Mapping and describing the biodiversity of a cold-water coral reef ecosystem in the Trondheimsfjord by use of multi-beam echo sounding and video mounted on a remotely operated vehicle June Jakobsen Marine Coastal Development Submission date: May 2016 Supervisor: Geir Johnsen, IBI Co-supervisor: Svein Karlsen, Fylkesmannen i Nord-Trøndelag Martin Ludvigsen, IMT Torkild Bakken, NTNU, Vitenskapsmuseet Norwegian University of Science and Technology Department of Biology i Contents Acknowledgements ................................................................................................................................. iii List of Abbreviations: .............................................................................................................................. iv Abstract: ................................................................................................................................................... v Sammendrag ............................................................................................................................................ vi Introduction: ............................................................................................................................................ 1 Theory ..................................................................................................................................................... 2 The geology of the fjord ...................................................................................................................... 2 Current systems in the fjord ................................................................................................................ 3 Lophelia pertusa – an important part of marine habitats and ecology ................................................ 4 Early coral research of the fjord .......................................................................................................... 7 Johan Gunnerus. .............................................................................................................................. 7 Vilhelm Ferdinand Johan Storm ...................................................................................................... 9 Carl Frederik Lindeman Dons ....................................................................................................... 10 Common traditional benthic sampling methods in marine biology .................................................. 11 Dredges, sledges and trawls .......................................................................................................... 11 Grabs and boxcorers. ..................................................................................................................... 12 Seabed mapping ................................................................................................................................ 12 Multi-Beam Echo Sounding .......................................................................................................... 12 Optical sea floor mapping ............................................................................................................. 13 Material and methods ............................................................................................................................ 14 Research platforms ............................................................................................................................ 14 The Research Vessel Gunnerus ..................................................................................................... 14 Multi-beam echo sounder (MBES) ............................................................................................... 14 Remotely operated vehicle ............................................................................................................ 15 Video Camera ................................................................................................................................ 16 Transects ............................................................................................................................................ 16 The Beitstadfjord transect.............................................................................................................. 16 The Tautra sill transect .................................................................................................................. 18 Data processing and analysis for the Hoøyskjæret in Beitstadfjorden .............................................. 19 Data processing for the Tautra sill..................................................................................................... 19 Data analysis for the Tautra sill ..................................................................................................... 23 Results ................................................................................................................................................... 26 The Beitstadfjord – Hoøyskjæret....................................................................................................... 26 The Tautra cold-water coral reef. Mapping and describing the biodiversity of a cold-water coral reef ecosystem in the Trondheimsfjord by the use of multibeam echo sounder and video mounted on a remotely operated vehicle. MSc thesis by June Jakobsen, May 2016, NTNU ii Tautra sill: Total abundance of benthic organisms ............................................................................ 27 Equitability and Shannon’s diversity index ....................................................................................... 31 Tautra sill: The equitability (E) of Shannon diversity index, H’, and depth ..................................... 33 Tautra sill: Live Lophelia pertusa coverage in relation to depth ...................................................... 36 Tautra sill: Live coral coverage and E ............................................................................................... 40 Tautra sill: Live Lophelia pertusa coverage in relation to numbers of sponges ............................... 43 Shannon’s diversity index, H’. .......................................................................................................... 46 Fish associated with live coral cover ................................................................................................. 47 Live L. pertusa gradient .................................................................................................................... 48 Discussion: ............................................................................................................................................ 50 Live Lophelia pertusa coverage ........................................................................................................ 50 Bioturbation ....................................................................................................................................... 51 Biodiversity along the Tautra sill transect. ........................................................................................ 52 Sponges ............................................................................................................................................. 53 Fish .................................................................................................................................................... 54 Data acquisition/performing a survey ............................................................................................... 55 Beitstadfjord – Hoøyskjæret .............................................................................................................. 56 Analysing data ................................................................................................................................... 58 ROV movement and video and image analysis ................................................................................. 59 Concluding remarks .............................................................................................................................. 61 References: ............................................................................................................................................ 62 The Tautra cold-water coral reef. Mapping and describing the biodiversity of a cold-water coral reef ecosystem in the Trondheimsfjord by the use of multibeam echo sounder and video mounted on a remotely operated vehicle. MSc thesis by June Jakobsen, May 2016, NTNU iii Acknowledgements The work of this MSc thesis was carried out at Trondheim Biological Station (TBS), Department of Biology, NTNU, in cooperation with the County Governor of Nord-Trøndelag and NTNU Autonomous Underwater Robotics-lab in the time between August 2014 to June 2016. I would like to express my sincere and utmost gratitude to my supervisor Geir Johnsen for inspiring me to do better and to be creative. Without your enthusiasm for my project, this would never have been as fun and interesting as it truly has been. Thank you. My co-supervisor Torkild Bakken, thank you for your sound and grounded advice and for listening to my thoughts about the work. I am indebted to you for your valuable input to my work and to your positive feedback keeping me on track. To my supervisor Martin Ludvigsen and to Christian Malmquist. Thank you for helping me understand the technological side of seabed mapping. Thank you for
Recommended publications
  • Norway and Its Marine Areas - a Brief Description of the Sea Floor
    No.3 2003 IN FOCUS Norway and its marine areas - a brief description of the sea floor From the deep sea to the fjord floor Norwegian waters comprise widely differing environments - from the Bjørnøyrenna deep sea via the continental slope and continental shelf to the coastal zone with its strandflat, archipelagos and fjords.This constitutes a geologi- cal diversity that is unique in a European context. An exciting geological history lies Trænadjupet behind this diversity - a development that has taken place over more than 400 million years.The continents con- Vøringplatået sist of plates of solidified rock that float on partially molten rock, and these plates move relative to one another.Where they collide, the Earth's crust is folded and mountain chains are created.Where they drift apart, deep oceans form and new sea Storegga floor is created along rifts because molten rock (magma) streams up from below. A good example is the Mid-Atlantic Ridge, including Iceland, a which is a result of Greenland and n n e Europe drifting from each other at a r e rate of about 2 cm a year. k s r o The plates on which Norway and N Greenland rest collided more than 400 million years ago and formed mountain chains on either side of a Skagerrak shallow sea. Both Greenland and Norway are remnants of worn down mountain chains. Between these mountain chains, the shallow sea Figure 1.Norway and its neighbouring seas. gradually filled with sediments derived from the erosion of the chains.These sedi- ments became transformed into sandstones, shales and limestones and it is in these rocks we now find oil and gas on the Norwegian continental shelf.
    [Show full text]
  • Ritual Landscapes and Borders Within Rock Art Research Stebergløkken, Berge, Lindgaard and Vangen Stuedal (Eds)
    Stebergløkken, Berge, Lindgaard and Vangen Stuedal (eds) and Vangen Lindgaard Berge, Stebergløkken, Art Research within Rock and Borders Ritual Landscapes Ritual Landscapes and Ritual landscapes and borders are recurring themes running through Professor Kalle Sognnes' Borders within long research career. This anthology contains 13 articles written by colleagues from his broad network in appreciation of his many contributions to the field of rock art research. The contributions discuss many different kinds of borders: those between landscapes, cultures, Rock Art Research traditions, settlements, power relations, symbolism, research traditions, theory and methods. We are grateful to the Department of Historical studies, NTNU; the Faculty of Humanities; NTNU, Papers in Honour of The Royal Norwegian Society of Sciences and Letters and The Norwegian Archaeological Society (Norsk arkeologisk selskap) for funding this volume that will add new knowledge to the field and Professor Kalle Sognnes will be of importance to researchers and students of rock art in Scandinavia and abroad. edited by Heidrun Stebergløkken, Ragnhild Berge, Eva Lindgaard and Helle Vangen Stuedal Archaeopress Archaeology www.archaeopress.com Steberglokken cover.indd 1 03/09/2015 17:30:19 Ritual Landscapes and Borders within Rock Art Research Papers in Honour of Professor Kalle Sognnes edited by Heidrun Stebergløkken, Ragnhild Berge, Eva Lindgaard and Helle Vangen Stuedal Archaeopress Archaeology Archaeopress Publishing Ltd Gordon House 276 Banbury Road Oxford OX2 7ED www.archaeopress.com ISBN 9781784911584 ISBN 978 1 78491 159 1 (e-Pdf) © Archaeopress and the individual authors 2015 Cover image: Crossing borders. Leirfall in Stjørdal, central Norway. Photo: Helle Vangen Stuedal All rights reserved. No part of this book may be reproduced, or transmitted, in any form or by any means, electronic, mechanical, photocopying or otherwise, without the prior written permission of the copyright owners.
    [Show full text]
  • Guide to Trondheim
    ROOMVENT 2011 12th International Conference on Air Distribution in Rooms, Trondheim, Norway, June 19-22, 2011 GUIDE TO TRONDHEIM Issued: 15 April 2011 HOW TO GET TO TRONDHEIM You can reach Trondheim by air, rail or sea. By air The easiest way to travel to Trondheim will be by air. Trondheim Airport Værnes (TRD) is the local airport located about 30 kilometers to the north-east of the city center. The airport offers regular domestic flights to and from most major cities in Norway, as well as daily flights with service to a few European cities. Traveling non-stop to Trondheim Trondheim Airport Værnes (TRD) offers multiple daily flights with service to Copenhagen Airport Kastrup (CPH), Stockholm Airport Arlanda (ARN), Amsterdam Schiphol Airport (AMS), and London Stansted Airport (STN). Copenhagen is the Scandinavian hub for Star Alliance, (with partner airlines SAS, United, Lufthansa, Air Canada, Air New Zealand and some others), and offers excellent connections to most parts of the world. Amsterdam is the central European hub for the Skyteam Airline Alliance (with partner airlines KLM, Northwest, Continental and Air France), with even more connections to all parts of the world. Nonstop flights between London (UK) and Trondheim are offered by the Norwegian Airline norwegian.no. Traveling through Oslo Airport Gardermoen (OSL) Many international travelers to Trondheim go through Oslo Airport Gardermoen (OSL). Oslo Airport offers connections to most major cities in Europe, in particular with frequent flights to the important hubs Amsterdam Schiphol Airport (AMS), London Airports Gatwick and Heathrow (LGW, LHR), Copenhagen Airport (CPH), Frankfurt am Main (FRA) and Paris Airports de Gaulle (CDG) and Orly (ORY).
    [Show full text]
  • Norwegian Tbm Tunnelling Norwegian Tbm Tunnelling Publication No
    NORWEGIAN TBM TUNNELLING NORWEGIAN NORWEGIAN TBM TUNNELLING PUBLICATION NO. 11 PUBLICATION NORWEGIAN SOIL AND ROCK ENGINEERING ASSOCIATION PUBLICATION NO. 11 NORWEGIAN TBM TUNNELLING 30 YEARS of EXPERIENCE with TBMs in NORWEGIAN TUNNELLING 3 NORWEGIAN SOIL AND ROCK ENGINEERING ASSOCIATION INCORPORATING NORWEGIAN TUNNELLING SOCIETY NORWEGIAN GEOTECHNICAL SOCIETY NORWEGIAN ROCK MECHANICS GROUP REPRESENTS EXPERTISE IN • Hard Rock Tunnelling techniques • Rock blasting technology • Soft soil engineering • Marine and offshore geotechnology • Rock mechanics and engineering geology USED IN THE DESIGN AND CONSTRUCTION OF • Hydroelectric power development, including: - water conveying tunnels - unlined pressure shafts - subsurface power stations - lake taps - earth and rock fill dams • Transportation tunnels • Underground storage facilities • Heavy foundations on soft ground • Foundations of offshore constructions • Underground openings for public use SECRETARIAT: NORWEGIAN TUNNELLING SOCIETY NFF P. O. Box 2312, Solli N-0251 Oslo, Norway e-mail: [email protected] 4 NORWEGIAN TBM TUNNELLING 30 YEARS of EXPERIENCE with TBMs in NORWEGIAN TUNNELLING Publication No. 11 NORWEGIAN SOIL AND ROCK ENGINEERING ASSOCIATION NORWEGIAN TUNNELLING SOCIETY, NFF, 5 © NORWEGIAN TUNNELLING SOCIETY 1998 ISBN 82-991952-1-7 Picture credits: Cover page: Statkraft Anlegg AS Print: Hansen Grafiske, Oslo 6 CONTENTS Preface 9 1 Arnulf Hansen The History of TBM Tunnelling in Norway 11 2 O. T. Blindheim and Amund Bruland Boreability Testing 21 3 Amund Bruland Prediction Model for Performance and Costs 29 4 Odd Askilsrud Development of TBM Technology for Hard Rock Conditions 35 5 O. T. Blindheim Early TBM Projects 43 6 Thor Skjeggedal and Karl Gunnar Holter The VEAS Project - 40 km Tunnelling with Pregrouting 53 7 O. T. Blindheim, Erik Dahl Johansen and Arild Hegrenæs Bored Road Tunnels in Hard Rock 57 8 Jan Drake and Erik Dahl Johansen The Svartisen Hydroelectric Project - 70 kilometres of Hydro Tunnels 63 9 Arne Myrvang, O.
    [Show full text]
  • THE LIBERATION of OSLO and COPENHAGEN: a MIDSHIPMAN's MEMOIR C.B. Koester
    THE LIBERATION OF OSLO AND COPENHAGEN: A MIDSHIPMAN'S MEMOIR C.B. Koester Introduction I joined HMS Devonshire, a County-class cruiser in the Home Fleet, on 16 September 1944. For the next nine months we operated out of Scapa Flow, the naval base in the Orkneys north of Scotland which had been home to Jellicoe's Grand Fleet during World War I and harboured the main units of the Home Fleet throughout the second conflict. It was a bleak, uninviting collection of seventy-three islands—at low water—twenty-nine of them inhabited, mainly by fishermen and shepherds. Winters were generally miserable and the opportunities for recreation ashore limited. There was boat-pulling and sailing, weather permitting; an occasional game of field hockey on the naval sports ground; and perhaps a Saturday afternoon concert in the fleet canteen or a "tea dance" at the Wrennery. Otherwise, we entertained ourselves aboard: singsongs in the Gunroom; a Sunday night film in the Wardroom; deck hockey in the Dog Watches; and endless games of "liar's dice." Our operations at sea were more harrowing, but only marginally more exciting, consisting mainly of attacks on German shore installations on the Norwegian coast. We rarely saw the coastline, however, for the strikes were carried out by aircraft flying from the escort carriers in the task force. At the same time, we had to be prepared for whatever counterattack the Germans might mount, and until Tirpitz was finally disabled on 12 November 1944, such a riposte might have been severe. That and the ever-present threat of submarines notwithstanding, for most of us these operations involved a large measure of boredom and discomfort.
    [Show full text]
  • Local Controls on Sediment Accumulation and Distribution in a Fjord in the West Antarctic Peninsula: Implications for Palaeoenvironmental Interpretations Yuribia P
    RESEARCH/REVIEW ARTICLE Local controls on sediment accumulation and distribution in a fjord in the West Antarctic Peninsula: implications for palaeoenvironmental interpretations Yuribia P. Munoz & Julia S. Wellner Department of Earth and Atmospheric Sciences, University of Houston, 4800 Calhoun Road, Houston, TX 77204, USA Keywords Abstract Flandres Bay; Antarctic Peninsula; sediment We analyse surface sediment and its distribution in Flandres Bay, West Antarctic distribution; grain size. Peninsula, in order to understand modern day sediment dispersal patterns in Correspondence a fjord with retreating, tidewater glaciers. The surface sediment descriptions Yuribia P. Munoz, Department of Earth and of 41 cores are included in this study. The sediment facies described include Atmospheric Sciences, University of muddy diatomaceous ooze, diatomaceous mud, pebbly mud, sandy mud and Houston, 4800 Calhoun Road, Houston, mud, with scattered pebbles present in most samples. In contrast to a traditional TX 77204, USA. E-mail: [email protected] conceptual model of glacial sediment distribution in fjords, grain size in Flandres Bay generally coarsens from the inner to outer bay. The smallest grain size sediments were found in the bay head and are interpreted as fine-grained deposits resulting from meltwater plumes and sediment gravity flows occurring close to the glacier front. The middle of the bay is characterized by a high silt percentage, which correlates to diatom-rich sediments. Sediments in the outer bay have a high component of coarse material, which is interpreted as being the result of winnowing from currents moving from the Bellingshausen Sea into the Gerlache Strait. Palaeoenvironmental reconstructions of glacial environ- ments often use grain size as an indicator of proximity to the ice margin.
    [Show full text]
  • Geography Quiz: Landform Vocabulary
    Geography Quiz: Landform Vocabulary Directions: Read each description below and circle the correct vocabulary term. 1. A large group of islands 9. A high ridge dividing rivers that flow to a. climate opposite sides of the continent b. tributary a. continental divide c. archipelago b. delta c. plain 2. An arm of a lake extending into the land a. bay 10. A build-up of silt at the river mouth b. glacier a. bay c. fjord b. delta c. canal 3. A steep mountain standing alone a. plateau 11. A very dry place with little rain b. cape a. desert c. butte b. island c. rapids 4. An inland waterway made by people a. reef 12. A body of slow moving ice b. ocean a. slip and slide c. canal b. ice cube c. glacier 5. A deep valley with steep sides a. canyon 13. Part of the ocean that extends into the b. valley land c. island a. gulf b. bay 6. A point of land extending out from the c. plateau coast into the sea a. delta 14. A protected body of water b. cape a. harbor c. gulf b. bay c. inter-coastal waterway 7. A pattern of weather over a long time a. temperature 15. Land completely surrounded by water b. climate a. peninsula c. ice b. island c. valley 8. A huge area of land a. state 16. A narrow strip of land connecting two b. mass bodies of water c. continent a. continent b. cape c. isthmus © 2000 – 2008 Pearson Education, Inc. All Rights Reserved.
    [Show full text]
  • A Late Triassic Lake System in East Greenland: Facies, Depositional Cycles and Palaeoclimate
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Columbia University Academic Commons ELSEVIER Palaeogeography, Palaeoclimatology, Palaeoecology 140 (1998) 135±159 A Late Triassic lake system in East Greenland: facies, depositional cycles and palaeoclimate Lars B. Clemmensen a,Ł,DennisV.Kentb, Farish A. Jenkins, Jr. c a Geological Institute, University of Copenhagen, DK-1350 Copenhagen K, Denmark b Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA c Department of Organismic and Evolutionary Biology and Museum of Comparative Zoology, Harvard University, Cambridge, MA 02138, USA Received 24 May 1996; accepted 18 January 1997 Abstract The Upper Triassic Fleming Fjord Formation of the Jameson Land Basin in East Greenland contains a well-exposed succession, 200±300 m thick, of lake deposits. The Malmros Klint Member, 100±130 m thick, is composed of cyclically bedded intraformational conglomerates, red siltstones and ®ne-grained sandstones and disrupted dolomitic sediments (paleosols). The cyclicity is composite with cycles having mean thicknesses of (25), 5.9 and 1.6 m. The overlying Carlsberg Fjord beds of the érsted Dal Member, 80±115 m thick, are composed of structureless red mudstones rhythmically broken by thin greyish siltstones. This unit also has a composite cyclicity with cycles having mean thicknesses of 5.0 and 1.0 m. The uppermost Tait Bjerg Beds of the érsted Dal Member, 50±65 m thick, can be divided into two units. A lower unit is composed of cyclically bedded intraformational conglomerates or thin sandstones, red mudstones, greenish mudstones and yellowish marlstones. An upper unit is composed of relatively simple cycles of grey mudstones and yellowish marlstones.
    [Show full text]
  • Recent Ringing Recoveries
    RecentRinging Recoveries Data has been provided by the British Trust for Ornithology from whompermission should be sought before using these data in publications. SYMBOLS. Age is coded according to EURING,x = found dead XF fresh XL not recent, + = killed by man +F fresh +L not recent, S = sick, A = alive taken to captivity, R = control, RR = field record. OYSTERCATCHERH•ematopus ostra[.egus FR04593 6F 15.06.80 Bangor, Gwynedd 53 13'N 4 2'W x. Sandoy, Faeroes 61 50'N 6 48'W 01.01.89 SS12624 6 15.12.77 Leverton, Wash 53 0'N 0 9'E x Finnoy, Norway 59 10'N 5 50'E 01.07.89 FV97128 10 30.03.90 Loch Flemington, Highlands 57 32'N 3 58'W x Llanelli, Dyfed 51 40'N 4 10'W 10.02.91 SS77180 5 30.08.68 Snettisham, Wash 52 51'N 0 27'E R Friskhey, Wash 53 3'N 0 13'E 12.08.91 FC61060 1 17.06.91 Elvanfoot, Strathclyde 55 26'N 3 40'W SR St. Brevin les Pins, France 47 15'N 2 10'W 20.10.91 FC61060 1 17.06.91 Elvanfoot, Strathclyde +F Les Moutiers, France 47 4'N 2 2'W 19.12.9] FS15793 8 12.08.71 Snettisham, Wash +F Les Moutiers, France 26.12.91 SS75185 4 08.09.67 Snettisham, Wash XL Westerduinen, Netherlands 53 2'N 4 43'E 29.12.91 SS59586 4F 24.07.67 Snettisham, Wash R Dorum Sued, F.R.germany 53 43'N 8 30'E 02.02.92 FA06129 1 14.06.86 South Nesting, Shetland 60 16'N 1 10'W XF Carnforth, Morecambe Bay 54 6'N 2 48'W 16.02.92 FA06955 7 12.06.83 Llanfairfechan, Gwynedd 53 15'N 3 59'W X Trondheim Fjord, Norway 63 50'N 9 39'W 08.03.92 FR38814 6 06.06.82 Bamgor, Gwynedd X Cuppin, Orkney 59 3'N 3 12'W 09.03.92 FV81188 7 07.12.80 Bangor, Gwynedd XF Yesnaby, Orkney
    [Show full text]
  • Binkley Thesis Poster Revised
    Late Mesolithic Foodways in Arctica and Subarctic Coastal Zones: An Ethnoarchaeological Approach Megan Binkley, University of Wisconsin–Madison Preferred Resource Concentrations Across Accessibility Zones 1. Skerry Introduction 25 Peaks & Late Mesolithic hunter-gatherers on northern Mainland coastlines c. 8,300-6,000 cal BP relied on marine Zone 20 resources for survival. Associated site distribution ≤ 2 km inland patterns suggest that these populations may have preferred areas with concentrations of specific resources, but this hypothesis has not previously been 15 tested via studies of modern behavior. Through collaboration with modern Norwegian 2. Supralittoral 10 farmers practicing hunting and gathering, I create an Zone analogy between current populations and Late Splashed but not Mesolithic hunter-gatherers. Through this, I test inundated by tides whether modern subsistence practices support the idea 5 of a Mesolithic preference for flatter coastlines with concentrations of accessible resources. 0 Zone 1 Zone 2 Zone 3 Zone 4 Zone 5 # Resources - All # Resources - Preferred # Demographics 3. Eulittoral Zone High-to-low tide Implications zones • Shellfish and seaweeds were likely critical secondary resources in Mesolithic foodways PERMANENT WATER LINE • Shell middens may have reinforced exploitation routes on an ecological level Results • Juvenile hunter-gatherers may have made meaningful 4. Infralittoral My observations at HF1 and HF2 revealed: contributions to subsistence economies Non-Immersion • 32 ongoing exploitation sites Zone • 30 regularly targeted species Up to 0.5 m deep Pacific Oyster harvesting beds (HF1, photo by author). • 21 ‘preferred’ marine species, exploited daily • 6 discrete topographic zones throughout the fjord- Methods skerry landscape 5. Infralittoral I gathered data during two homestays with the • Pros and cons associated with each zone following sample populations across Norway: Because Zone 6 is not fully within the fjord-skerry Immersion Zone landscape, I excluded it from my final analysis.
    [Show full text]
  • Systems Description of Krogen
    Building with Nature: Systems Description of Krogen August 2018 Project Building with Nature (EU-InterReg) Start date 01.11.2016 End date 01.07.2020 Project manager (PM) Ane Høiberg Nielsen Project leader (PL) Anni Lassen Project staff (PS) Mie Thomsen, Sofie Kamille Astrup Time registering 35410206 Approved date 10.08.2018 Signature Report Systems Description of Krogen Author Mie Thomsen, Sofie Kamille Astrup, Anni Lassen Keyword Joint Agreement, Krogen, Coastal, protection, nourishment Distribution www.kyst.dk, www.northsearegion.eu/building-with-Nature/ Referred to as Kystdirektoratet, BWN Krogen, 2018 2 Building with Nature: Systems Description of Krogen Contents 1 Introduction 5 1.1 Building with Nature 5 1.2 The Joint Agreement (on the North Sea coast) 6 1.3 Safety Level of Joint Agreement from Lodbjerg to Nymindegab 7 2 The Area of Krogen 9 2.1 The Landscape at Krogen 10 2.2 Threats to the Krogen Area 12 2.3 Coastal Protection at Krogen 14 2.4 Effect of the Coastal Protection at Krogen 17 3 Source-Pathway-Receptor 18 Building with Nature: Systems Description of Krogen 3 4 Building with Nature: Systems Description of Krogen 1 Introduction 1.1 Building with Nature The objective of the Building with Nature EU-InterReg project is to improve coastal adaptability and resilience to climate change by means of natural measures. As part of this project the Danish Coastal Authority (DCA) carry out research into different aspects of using natural processes and materials in coastal laboratories on Danish coasts. Through the EU InterReg project “Building with nature” a better understanding of the interactions within the coastal system is sought.
    [Show full text]
  • Fjord Estuary Ecosystem, Kenai Fjords National Park
    National Park Service Park Science U.S. Department of the Interior Kenai Fjords National Park, Alaska Fjord Estuary Ecosystem The fjord estuary ecosystem is one of the richest assemblages of life on earth, but not one of the most well known. Found only in six locations around the planet (Chile, Norway, New Zealand, Alaska, Green­ land, and Antarctica), fjord estuaries require just the right combination of events for their construction. About 27-32,000 years ago, this precise mixture began in Alaska during the Wisconsin glacial period. Snow piling up for years and years, compressing into ice underneath its own weight, spread across the Kenai Peninsula as the Cordilleran ice sheet. Here in the Ke­ nai Fjords, ice covered the mountains and carved the McCarthy Glacier. USGS photograph by Bruce Molnia valleys. The ice etched out a landscape of U-shaped valleys with jagged ridges, known as arêtes, in be­ tween. Many of these valleys extended 600-1000 feet Keystone Species below what would become sea level once the warm­ In most ecosystems there is a “keystone species,” ing progressed. Once filled with seawater, these long one that has a role linking the whole ecosystem. deep arms of the sea are called fjords; other glacially The sea otter holds that role for the fjord estuary carved valleys were elevated on mountainsides and ecosystems of Alaska. Feeding on a variety of appear today as what we call “hanging valleys.” shellfish but always keeping the sea urchin popu- lation in check. Sea urchins have been known to About 10,000 years ago as the ice began to melt, the create “urchin barrens” eliminating giant stands valleys filled with seawater.
    [Show full text]