2. Conservation Objectives Jak Et Al[1]
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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. -
Survey Guide Notes 2017
COASTWATCH SURVEY GUIDE NOTES The Coastwatch Survey 2017 is taking place from the Black sea to the Baltic and the Mediterranean to the Atlantic. This is the 30th anniversary of the survey which was started on the island of Ireland in 1987 and went international in 1988. It involves walking a chosen survey unit of sea shore (500m) once around low tide, eyes peeled for lots of information set out in the survey questionnaire and noting down your observations. Water quality tests may be used. Individual snapshot surveys are combined like a jigsaw of our shore in autumn 2017. Much of this citizen science work can be compared with or used to augment official data to better monitor our shores and seas and take action where needed. A survey unit (s.u. for short) is a stretch of shore approx. 500 m long as measured along mean high tide mark. On the Coastwatch map online it’s any one of the blue or white sections you see along the coast. If you click on one the colour changes to red and the unique survey unit code pops up. Spring (extreme) high-tide HINTERLAND Normal high-tide (MHWM) SPLASH Normal low-tide (MLWM) ZONE INTERTIDAL The width covers the sea shore from start of hinterland (dry land) down to shallow water when the tide is out. The intertidal may be over a kilometre in tidal estuaries with sand and mudflats, or reduced to a narrow strip along steeply sloping shores. In spring tides on a full and new moon it is widest. -
Phylum MOLLUSCA
285 MOLLUSCA: SOLENOGASTRES-POLYPLACOPHORA Phylum MOLLUSCA Class SOLENOGASTRES Family Lepidomeniidae NEMATOMENIA BANYULENSIS (Pruvot, 1891, p. 715, as Dondersia) Occasionally on Lafoea dumosa (R.A.T., S.P., E.J.A.): at 4 positions S.W. of Eddystone, 42-49 fm., on Lafoea dumosa (Crawshay, 1912, p. 368): Eddystone, 29 fm., 1920 (R.W.): 7, 3, 1 and 1 in 4 hauls N.E. of Eddystone, 1948 (V.F.) Breeding: gonads ripe in Aug. (R.A.T.) Family Neomeniidae NEOMENIA CARINATA Tullberg, 1875, p. 1 One specimen Rame-Eddystone Grounds, 29.12.49 (V.F.) Family Proneomeniidae PRONEOMENIA AGLAOPHENIAE Kovalevsky and Marion [Pruvot, 1891, p. 720] Common on Thecocarpus myriophyllum, generally coiled around the base of the stem of the hydroid (S.P., E.J.A.): at 4 positions S.W. of Eddystone, 43-49 fm. (Crawshay, 1912, p. 367): S. of Rame Head, 27 fm., 1920 (R.W.): N. of Eddystone, 29.3.33 (A.J.S.) Class POLYPLACOPHORA (=LORICATA) Family Lepidopleuridae LEPIDOPLEURUS ASELLUS (Gmelin) [Forbes and Hanley, 1849, II, p. 407, as Chiton; Matthews, 1953, p. 246] Abundant, 15-30 fm., especially on muddy gravel (S.P.): at 9 positions S.W. of Eddystone, 40-43 fm. (Crawshay, 1912, p. 368, as Craspedochilus onyx) SALCOMBE. Common in dredge material (Allen and Todd, 1900, p. 210) LEPIDOPLEURUS, CANCELLATUS (Sowerby) [Forbes and Hanley, 1849, II, p. 410, as Chiton; Matthews. 1953, p. 246] Wembury West Reef, three specimens at E.L.W.S.T. by J. Brady, 28.3.56 (G.M.S.) Family Lepidochitonidae TONICELLA RUBRA (L.) [Forbes and Hanley, 1849, II, p. -
Appendix 1 : Marine Habitat Types Definitions. Update Of
Appendix 1 Marine Habitat types definitions. Update of “Interpretation Manual of European Union Habitats” COASTAL AND HALOPHYTIC HABITATS Open sea and tidal areas 1110 Sandbanks which are slightly covered by sea water all the time PAL.CLASS.: 11.125, 11.22, 11.31 1. Definition: Sandbanks are elevated, elongated, rounded or irregular topographic features, permanently submerged and predominantly surrounded by deeper water. They consist mainly of sandy sediments, but larger grain sizes, including boulders and cobbles, or smaller grain sizes including mud may also be present on a sandbank. Banks where sandy sediments occur in a layer over hard substrata are classed as sandbanks if the associated biota are dependent on the sand rather than on the underlying hard substrata. “Slightly covered by sea water all the time” means that above a sandbank the water depth is seldom more than 20 m below chart datum. Sandbanks can, however, extend beneath 20 m below chart datum. It can, therefore, be appropriate to include in designations such areas where they are part of the feature and host its biological assemblages. 2. Characteristic animal and plant species 2.1. Vegetation: North Atlantic including North Sea: Zostera sp., free living species of the Corallinaceae family. On many sandbanks macrophytes do not occur. Central Atlantic Islands (Macaronesian Islands): Cymodocea nodosa and Zostera noltii. On many sandbanks free living species of Corallinaceae are conspicuous elements of biotic assemblages, with relevant role as feeding and nursery grounds for invertebrates and fish. On many sandbanks macrophytes do not occur. Baltic Sea: Zostera sp., Potamogeton spp., Ruppia spp., Tolypella nidifica, Zannichellia spp., carophytes. -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
Steckbriefe Und Kartierhinweise Für FFH-Lebensraumtypen
Steckbriefe und Kartierhinweise für FFH-Lebensraumtypen 1. Fassung, Mai 2007 Landesamt für Natur und Umwelt des Landes Schleswig-Holstein LANU Schleswig-Holstein Steckbriefe und Kartierhinweise für FFH-Lebensraumtypen 1. Fassung Mai 2007 EU-Code 1140 Kurzbezeichnung Watten FFH-Richtlinie 1997 Vegetationsfreies Schlick-, Sand- und Mischwatt BFN 1998 Vegetationsfreies Schlick-, Sand- und Mischwatt Interpretation Manual Mudflats and sandflats not covered by seawater at low tide Sands and muds of the coasts of the oceans, their connected seas and as- sociated lagoons, not covered by sea water at low tide, devoid of vascular plants, usually coated by blue algae and diatoms. They are of particular importance as feeding grounds for wildfowl and waders. The diverse inter- tidal communities of invertebrates and algae that occupy them can be used to define subdivisions of 11.27, eelgrass communities that may be exposed for a few hours in the course of every tide have been listed under 11.3, brackish water vegetation of permanent pools by use of those of 11.4. Note: Eelgrass communities (11.3) are included in this habitat type. Beschreibung Sand- und Schlickflächen, die im Küsten- und Brackwasserbereich von Nord- und Ostsee und in angrenzenden Meeresarmen, Strandseen und Salzwiesen bei LAT / lowest astronomical tide (Tidewatten der Nord- see) oder mittlerem Witterungsverlauf (Windwatten der Ostsee) regel- mäßig trocken fallen. Typische Arten Höhere Pflanzen : Eleocharis parvula (Schlei), Oenanthe conioides (Elbe), Ruppia cirrhosa, Ruppia maritima, Zostera marina, Zostera noltii Algen : div. Blau- und Kieselalgen Außerdem Windwatten z. T. mit Armleuchteralgen (Characeae), anderen Makroalgen Typische Vegetation > Zosteretum noltii HARMSEN 1936 > Zosteretum marinae B ORGESEN ex VAN GOOR 1921 > Ruppion maritimae B R.-B L. -
Assess-Env0196
Advisory Committee on Fishery Management and ICES CM 1996/AssesslEnv:l Advisory Committee on the Marine Environment Ref.: G REPORT OF THE WORKING GROUP ON ECOSYSTEM EFFECTS OF FISHING ACTIVITIES ICES Headquarters 13-21 March 1996 This report is not to be quoted without prior consultation with the General Secretary. The document is a report of an expert group under the auspices of the International Council for the Exploration of the Sea and does not necessarily represent the views of the Council. International Council for the ExpJoration of the Sea ConseiJ International pour J'Exploration de la Mer Palregade 2-4 DK-1261 Copenhagen K Denmark TABLE OF CONTENTS Section Page OPENING OF THE MEETING 1 2 ADOPTION OF THE AGENDA 1 3 COMMUNITIES AND ASSEMBLAGES 1 3.1 Introduction : 1 3.2 Theory ofCommunity and Assemblage Dynamics 2 3.2.1 Review of literature in community ecology and community metrics 2 3.2.2 Theory of the effect offishing on size and diversity spectra 3 3.3 Intersessional Analyses of Species Diversity and Ordinations 4 3.3.1 Hypotheses and analysis framework 4 3.3.2 Surveys analysed 4 3.3.3 Results · 4 3.4 Data Analyses: North Sea as a Whole 5 3.4.1 Data sets , 5 3.4.2 Variables and data preparation steps 5 3.4.3 Statistical analyses 5 304.4 Annual size spectra of the North Sea numbers and diversity 6 3.4.5 Area;.effects on the annual size and diversity spectra 7 3.4.6 Trends over years in the size spectra of numbers and diversity ~ 8 3.4.7 Analysis of frequencies of species by abundance and biomass class 10 3.5 Contrasts Among Selected -
ICES Marine Science Symposia
ICES mar. Sei. Symp., 199: 189-199. 1995 Distribution and abundance of molluscs and decapod crustaceans in trawl samples from the Galician Shelf (NW Spain) A. C. Farina and F. J. Pereiro Farina, A. C., and Pereiro, F. J. 1995. Distribution and abundance of molluscs and decapod crustaceans in trawl samples from the Galician Shelf (NW Spain). - ICES mar. Sei. Symp., 199: 189-199. This study presents the community composition and structure of molluscs and decapod crustaceans from trawl samples taken on the Galician Shelf in Northwest Spain. Spatial and temporal distribution, as well as the biomass and density of the main species, are presented in relation to depth and substrate type. A. C. Farina: Instituto Espanol Oceanografia, Apdo 130, 15080 La Coruna, Spain. F. J. Pereiro: Instituto Espanol Oceanografia, Apdo 1552, 36280 Vigo, Spain [tel: (+34) 98120 53 62, fax: (+34) 981 229077], Introduction with recruitment to the area (in the autumn) and the spawning season of the majority of the demersal and Two main groups of invertebrates (crustaceans and mol benthic species (in the spring). A stratified sampling luscs) are caught when trawling for fish on the Galician design was used and selection of the trawls was random. Shelf, which lies off northwestern Spain, reaching a The area is divided into three geographic sectors (Mino depth of 500 m 30 km from the coast along its southern to Finisterre, Finisterre to Estaca, and Estaca to Riba- part and broadening to 65 km from the coast in the deo), and each sector is divided into two strata by depth northern part. -
Comparison of Some Interesting Molluscs, Trawled by the Belgian Fishery in the Bay of Biscay, with Similar Representatives from Adjacent Waters: Part III
Comparison of some interesting molluscs, trawled by the Belgian fishery in the Bay of Biscay, with similar representatives from adjacent waters: part III Frank Nolf 1 & Jean-Paul Kreps 2 1 Pr. Stefanieplein, 43/8 – B-8400 Oostende [email protected] 2 Rode Kruisstraat, 5 – B-8300 Knokke-Heist [email protected] Keywords: Bay of Biscay, W France, Belgian XLIV, Fig. 248; Pl. XLV, Figs 249-254), the North fishery, Mollusca, Gastropoda, Bivalvia. Sea (Pl. XLVI, Figs 255-257) and the English Channel south to the Bay of Biscay (Pl. XLIV, Abstract: In the third part of the report on the Figs 243-244) and Portugal (Pl. XLVI, Figs 260- molluscs collected by the Belgian fishery in the 261). Bay of Biscay during the last decade, the Specimens reported from the Mediterranean are remaining gastropods and a first series of erroneous identifications and have to be bivalves are briefly described, figured and attributed to Colus jeffreysianus (P. Fischer, compared with similar specimens from North 1868). The species lives on muddy and sandy Atlantic waters, the Mediterranean Sea or West bottoms, usually from 30 to 800 m deep. It is less Africa. common and lives deeper in the south of its range. Abbreviations: This is a rather variable species with respect to FN: private collection of Frank Nolf. its shell, especially in relation to the H.: height. breadth/height ratio, the size of the aperture and JPK: private collection of Jean-Paul Kreps. the length of the siphonal canal. This is probably JV: private collection of Johan Verstraeten. due to its occurrence in several different L.: length. -
Survey Guide Notes (2019)
COASTWATCH SURVEY GUIDE NOTES 2019 The Coastwatch Survey 2019 is taking place from the Baltic and the Mediterranean to the Atlantic. This is the 32nd anniversary of the survey which was started on the island of Ireland in 1987. It was tried internationally in 1988 and carried out as a first proper international survey in 1989. It involves walking a chosen survey unit of sea shore (500m) once around low tide, eyes peeled for lots of information set out in the survey questionnaire and noting down your observations. Water quality tests may be used. Individual snapshot surveys are then put together like a huge jigsaw of our shore. Much of this citizen science work can be compared with or used to augment official data to better monitor our shores and seas and take action where needed. A survey unit (s.u. for short) is a stretch of shore approx. 500 m long, as measured along mean high tide mark. On the Coastwatch map online it’s any one of the blue or white sections you see along the coast. If you click on one, the colour changes to turquoise and the unique survey unit code pops up. That is the code for your survey form question A1. Spring (extreme) high-tide HINTERLAND Normal high-tide (MHWM) SPLASH Normal low-tide (MLWM) ZONE INTERTIDAL The width covers the sea shore from Spring High Tide Mark (= start of hinterland) down to shallow water when the tide is fully out. The intertidal may be over a kilometre in estuaries with sand and mudflats, or reduced to a narrow strip along steeply sloping shores or a wall. -
Gebiedendocument Waddenzee
001_gebiedendocument_Waddenzee_maart 2007.doc Natura 2000 gebied 1 - Waddenzee (Zie leeswijzer) Kenschets Natura 2000 Landschap: Noordzee, Waddenzee en Delta Status: Habitatrichtlijn + Vogelrichtlijn Site code: NL1000001 + NL9801001 Beschermd natuurmonument: Waddenzee SN, Noord-Friesland buitendijks BN/SN, Kwelders noordkust Friesland BN, Neerlands Reid BN, Boschplaat SN, Kwelders noordkust Groningen BN, Dollard BN/SN, Schorren van Eendracht/Vlakte van Kerken BN Beheerder: Rijkswaterstaat, Defensie, Staatsbosbeheer, Groninger Landschap, It Fryske Gea, Landschap Noord-Holland, Natuurmonumenten Provincie: Groningen, Friesland, Noord-Holland Gemeente: Ameland; Anna Paulowna; De Marne; Delfzijl; Den Helder; Dongeradeel; Eemsmond; Ferweradiel; Franekeradeel; Harlingen; het Bildt; Reiderland; Schiermonnikoog; Terschelling; Texel; Vlieland; Winseradiel; Wieringen; Winsum Oppervlakte: 272.449 ha Gebiedsbeschrijving De Waddenzee bestaat uit een complex van diepe geulen en ondiep water met zand- en slibbanken waarvan grote delen bij eb droog vallen. Deze banken worden doorsneden door een fijn vertakt stelsel van geulen. Langs het vasteland en de eilanden liggen verspreid kweldergebieden, die door grote verschillen in vocht- en zoutgehalte bijdragen aan een zeer diverse flora en vegetatie. Enkele voorbeelden hiervan zijn de Boschplaat op Terschelling en Neerlands Reid op Ameland, waar op de overgang naar het duingebied bijzondere kweldervegetaties aanwezig zijn. Er is een nagenoeg ongestoorde hydrodynamiek en geomorfologie aanwezig, waarin natuurlijke -
Coastal Dynamics 2017 Paper No. 235 323 CONNECTING SUBTIDAL
Coastal Dynamics 2017 Paper No. 235 CONNECTING SUBTIDAL AND SUBAERIAL SAND TRANSPORT PATHWAYS IN THE TEXEL INLET SYSTEM 1 Kathelijne Wijnberg1, Ad van der Spek2, Filipe Galiforni Silva , Edwin Elias3, ,2 Mick van der Wegen4 , and Jill Slinger5 Abstract Potential transport pathways between the subtidal and subaerial part of tidal inlet systems are explored by means of a case study of Texel Inlet, The Netherlands. Based on a morphologic analysis of multi-annual, high-resolution bathymetric and topographic data sets we hypothesize that two mechanisms connect the subtidal and subaerial parts of the system. The first mechanism relates to deposition on the tip of the island occurring to a large extent below spring high tide level, providing a fresh sediment source available for aeolian transport during parts of the tidal cycle. The second mechanism relates to sand deposition on the wide sandflat above spring high tide level occurring during storm surge flooding. These deposits are then available for aeolian transport during regular water levels. Due to the dominant wind direction at Texel Island, this leads to extensive dune formation on the downwind end of the sandflat. Key words: morphodynamics, tidal inlet, coastal dunes, sandflat, sediment transport pathways 1. Introduction Tidal inlets are cross-roads for sediment exchange, not only between the open coast and the connected tidal basin but also between the submerged ebb-delta and emerging sand shoals that, once attached to the shore, may induce vertical build-up of the coast above storm surge levels through dune formation. Identifying and understanding the transport pathways of sediment from the subtidal domain onto the barrier island is highly relevant, as the elevation of a barrier island above storm surge water levels is one of the primary factors in barrier island geomorphologic response to storms (e.g.