SNH Commissioned Report 752: Basking Shark Satellite Tagging
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Marine Scotland Strategic Environment Assessment of Proposed Marine Protected Areas Environmental Report
Marine Scotland Strategic Environment Assessment of proposed Marine Protected Areas Environmental Report May 2019 Report prepared by: For: Non-Technical Summary Introduction The Scottish Government has made a long-term commitment to ensuring the sustainable management of the marine environment and to balancing the competing interests of use and protection of the sea. This includes the designation and management of new nature conservation sites, including Marine Protected Areas (MPAs). Scottish Natural Heritage has advised that four additional MPAs should be included in the MPA network (Figure NTS1). Marine Scotland is proposing that these four proposed MPAs (pMPAs) now be considered for designation to supplement existing protected areas and to create a wider network of MPAs. As part of the process to determine whether these four pMPAs should be designated, Marine Scotland is now inviting views on the findings of the Strategic Environmental Assessment). What is Strategic Environmental Assessment? This Environmental Report summarises the findings from the Strategic Environmental Assessment (SEA) of the designation of four additional pMPAs. An SEA of the pMPAs is required by the Environmental Assessment (Scotland) Act 2005 (‘the 2005 Act’). SEA identifies the likely significant environmental impacts of plans and policies, and proposed reasonable alternatives to them. SEA also identifies mitigation measures that are required to avoid or minimise any significant adverse effects and highlights opportunities for enhancements of beneficial effects. Taking place at an early stage in the plan or policy preparation process, it ensures that decision-making is informed by relevant environmental information. SEA provides opportunities for the public to consider this information and use it to inform their views on the draft plan or policy. -
2020 Cruise Directory Directory 2020 Cruise 2020 Cruise Directory M 18 C B Y 80 −−−−−−−−−−−−−−− 17 −−−−−−−−−−−−−−−
2020 MAIN Cover Artwork.qxp_Layout 1 07/03/2019 16:16 Page 1 2020 Hebridean Princess Cruise Calendar SPRING page CONTENTS March 2nd A Taste of the Lower Clyde 4 nights 22 European River Cruises on board MS Royal Crown 6th Firth of Clyde Explorer 4 nights 24 10th Historic Houses and Castles of the Clyde 7 nights 26 The Hebridean difference 3 Private charters 17 17th Inlets and Islands of Argyll 7 nights 28 24th Highland and Island Discovery 7 nights 30 Genuinely fully-inclusive cruising 4-5 Belmond Royal Scotsman 17 31st Flavours of the Hebrides 7 nights 32 Discovering more with Scottish islands A-Z 18-21 Hebridean’s exceptional crew 6-7 April 7th Easter Explorer 7 nights 34 Cruise itineraries 22-97 Life on board 8-9 14th Springtime Surprise 7 nights 36 Cabins 98-107 21st Idyllic Outer Isles 7 nights 38 Dining and cuisine 10-11 28th Footloose through the Inner Sound 7 nights 40 Smooth start to your cruise 108-109 2020 Cruise DireCTOrY Going ashore 12-13 On board A-Z 111 May 5th Glorious Gardens of the West Coast 7 nights 42 Themed cruises 14 12th Western Isles Panorama 7 nights 44 Highlands and islands of scotland What you need to know 112 Enriching guest speakers 15 19th St Kilda and the Outer Isles 7 nights 46 Orkney, Northern ireland, isle of Man and Norway Cabin facilities 113 26th Western Isles Wildlife 7 nights 48 Knowledgeable guides 15 Deck plans 114 SuMMER Partnerships 16 June 2nd St Kilda & Scotland’s Remote Archipelagos 7 nights 50 9th Heart of the Hebrides 7 nights 52 16th Footloose to the Outer Isles 7 nights 54 HEBRIDEAN -
Data Structure
Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference. -
Lamna Nasus) Inferred from a Data Mining in the Spanish Longline Fishery Targeting Swordfish (Xiphias Gladius) in the Atlantic for the 1987-2017 Period
SCRS/2020/073 Collect. Vol. Sci. Pap. ICCAT, 77(6): 89-117 (2020) SIZE AND AREA DISTRIBUTION OF PORBEAGLE (LAMNA NASUS) INFERRED FROM A DATA MINING IN THE SPANISH LONGLINE FISHERY TARGETING SWORDFISH (XIPHIAS GLADIUS) IN THE ATLANTIC FOR THE 1987-2017 PERIOD J. Mejuto1, A. Ramos-Cartelle1, B. García-Cortés1 and J. Fernández-Costa1 SUMMARY A total of 5,136 size observations of porbeagle were recovered for the period 1987-2017. The GLM results explained very moderately the variability of the sizes considering three main factors, suggesting minor but significant differences in some cases especially for the year factor and non-significant differences in other factors depending on the analysis. The greatest differences in the standardized mean length between some zones were caused by some large fish of unidentified sex. The standardized mean length data for the northern zones showed stability throughout the time series, very stable range of mean values and very few differences between sexes. The size distribution for northern areas indicated an FL-overall mean of 158 cm. The size showed a normal distribution confirming that a small fraction of individuals of this stock/s is available in the oceanic areas where the North Atlantic fleet is regularly fishing and the fishes are not fully recruited to those areas and / or this fishing gear up to 160 cm. The data suggests that some individuals could sporadically reach some intertropical areas of the eastern Atlantic. RÉSUMÉ Un total de 5.136 observations de taille de requins-taupes communs ont été récupérées pour la période 1987-2017. Les résultats du GLM expliquent très modérément la variabilité des tailles en tenant compte de trois facteurs principaux, ce qui suggère des différences mineures mais significatives dans certains cas, notamment pour le facteur année et des différences non significatives pour d'autres facteurs selon le type d’analyse. -
Electrosensory Pore Distribution and Feeding in the Basking Shark Cetorhinus Maximus (Lamniformes: Cetorhinidae)
Vol. 12: 33–36, 2011 AQUATIC BIOLOGY Published online March 3 doi: 10.3354/ab00328 Aquat Biol NOTE Electrosensory pore distribution and feeding in the basking shark Cetorhinus maximus (Lamniformes: Cetorhinidae) Ryan M. Kempster*, Shaun P. Collin The UWA Oceans Institute and the School of Animal Biology, The University of Western Australia, 35 Stirling Highway, Crawley, Western Australia 6009, Australia ABSTRACT: The basking shark Cetorhinus maximus is the second largest fish in the world, attaining lengths of up to 10 m. Very little is known of its sensory biology, particularly in relation to its feeding behaviour. We describe the abundance and distribution of ampullary pores over the head and pro- pose that both the spacing and orientation of electrosensory pores enables C. maximus to use passive electroreception to track the diel vertical migrations of zooplankton that enable the shark to meet the energetic costs of ram filter feeding. KEY WORDS: Ampullae of Lorenzini · Electroreception · Filter feeding · Basking shark Resale or republication not permitted without written consent of the publisher INTRODUCTION shark Rhincodon typus and the megamouth shark Megachasma pelagios, which can attain lengths of up Electroreception is an ancient sensory modality that to 14 and 6 m, respectively (Compagno 1984). These 3 has evolved independently across the animal kingdom filter-feeding sharks are among the largest living in multiple groups (Scheich et al. 1986, Collin & White- marine vertebrates (Compagno 1984) and yet they are head 2004). Repeated independent evolution of elec- all able to meet their energetic costs through the con- troreception emphasises the importance of this sense sumption of tiny zooplankton. -
A Large Explosive Silicic Eruption in the British Palaeogene Igneous Province.', ScientiC Reports., 9 (1)
Durham Research Online Deposited in DRO: 08 February 2019 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Troll, Valentin R. and Emeleus, C. Henry and Nicoll, Graeme R. and Mattsson, Tobias and Ellam, Robert M. and Donaldson, Colin H. and Harris, Chris (2019) 'A large explosive silicic eruption in the British Palaeogene Igneous Province.', Scientic reports., 9 (1). p. 494. Further information on publisher's website: https://doi.org/10.1038/s41598-018-35855-w Publisher's copyright statement: This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. -
Order LAMNIFORMES ODONTASPIDIDAE Sand Tiger Sharks Iagnostic Characters: Large Sharks
click for previous page Lamniformes: Odontaspididae 419 Order LAMNIFORMES ODONTASPIDIDAE Sand tiger sharks iagnostic characters: Large sharks. Head with 5 medium-sized gill slits, all in front of pectoral-fin bases, Dtheir upper ends not extending onto dorsal surface of head; eyes small or moderately large, with- out nictitating eyelids; no nasal barbels or nasoral grooves; snout conical or moderately depressed, not blade-like;mouth very long and angular, extending well behind eyes when jaws are not protruded;lower labial furrows present at mouth corners; anterior teeth enlarged, with long, narrow, sharp-edged but unserrated cusps and small basal cusplets (absent in young of at least 1 species), the upper anteriors separated from the laterals by a gap and tiny intermediate teeth; gill arches without rakers; spiracles present but very small. Two moderately large high dorsal fins, the first dorsal fin originating well in advance of the pelvic fins, the second dorsal fin as large as or somewhat smaller than the first dorsal fin;anal fin as large as second dorsal fin or slightly smaller; caudal fin short, asymmetrical, with a strong subterminal notch and a short but well marked ventral lobe. Caudal peduncle not depressed, without keels; a deep upper precaudal pit present but no lower pit. Intestinal valve of ring type, with turns closely packed like a stack of washers. Colour: grey or grey-brown to blackish above, blackish to light grey or white, with round or oval dark spots and blotches vari- ably present on 2 species. high dorsal fins upper precaudal eyes without pit present nictitating eyelids intestinal valve of ring type Habitat, biology, and fisheries: Wide-ranging, tropical to cool-temperate sharks, found inshore and down to moderate depths on the edge of the continental shelves and around some oceanic islands, and in the open ocean. -
The Denticle Surface of Thresher Shark Tails: Three-Dimensional Structure and Comparison to Other Pelagic Species
Received: 3 April 2020 Revised: 14 May 2020 Accepted: 21 May 2020 DOI: 10.1002/jmor.21222 RESEARCH ARTICLE The denticle surface of thresher shark tails: Three-dimensional structure and comparison to other pelagic species Meagan Popp1 | Connor F. White1 | Diego Bernal2 | Dylan K. Wainwright1 | George V. Lauder1 1Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Abstract Massachusetts Shark skin denticles (scales) are diverse in morphology both among species and 2 Department of Biology, University of across the body of single individuals, although the function of this diversity is poorly Massachusetts Dartmouth, Dartmouth, Massachusetts understood. The extremely elongate and highly flexible tail of thresher sharks pro- vides an opportunity to characterize gradients in denticle surface characteristics Correspondence George V. Lauder, Museum of Comparative along the length of the tail and assess correlations between denticle morphology and Zoology, 26 Oxford Street, Cambridge, MA tail kinematics. We measured denticle morphology on the caudal fin of three mature 02138. Email: [email protected] and two embryo common thresher sharks (Alopias vulpinus), and we compared thresher tail denticles to those of eleven other shark species. Using surface Funding information National Oceanic and Atmospheric profilometry, we quantified 3D-denticle patterning and texture along the tail of Administration, Grant/Award Number: threshers (27 regions in adults, and 16 regions in embryos). We report that tails of NA16NMF4270231; National Science Foundation, Grant/Award Numbers: IOS- thresher embryos have a membrane that covers the denticles and reduces surface 1354593, GRF DGE-1144152; Office of Naval roughness. In mature thresher tails, surfaces have an average roughness of 5.6 μm Research, Grant/Award Numbers: N00014-09-1-0352, N000141410533 which is smoother than some other pelagic shark species, but similar in roughness to blacktip, porbeagle, and bonnethead shark tails. -
Porbeagle Shark Lamna Nasus
Porbeagle Shark Lamna nasus Lateral View (♀) Ventral View (♀) COMMON NAMES APPEARANCE Porbeagle Shark, Atlantic Mackerel Shark, Blue Dog, Bottle-nosed • Heavily built but streamlined mackerel shark. Shark, Beaumaris Shark, Requin-Taupe Commun (Fr), Marrajo • Moderately long conical snout with a relatively large eyes. Sardinero (Es), Tiburón Sardinero (Es), Tintorera (Es). • Large first dorsal fin with a conspicuous white free rear tip. SYNONYMS • Second dorsal fin and anal fin equal-sized and set together. Squalus glaucus (Gunnerus, 1758), Squalus cornubicus (Gmelin, 1789), • Lunate caudal fin with strong keel and small secondary keel. Squalus pennanti (Walbaum, 1792), Lamna pennanti (Desvaux, 1851), Squalus monensis (Shaw, 1804), Squalus cornubiensis (Pennant, 1812), • Dorsally dark blue to grey with no patterning. Squalus selanonus (Walker, 1818), Selanonius walkeri (Fleming, 1828), • Ventrally white. Lamna punctata (Storer, 1839), Oxyrhina daekyi (Gill, 1862), Lamna • Maximum length of 365cm, though rarely to this size. NE MED ATL philippi (Perez Canto, 1886), Lamna whitleyi (Phillipps, 1935). DISTRIBUTION The Porbeagle Shark is a large, streamlined mackerel shark with a In the northern conical snout and powerful body. The first dorsal fin is large and hemisphere, the originates above or slightly behind the pectoral fins. It has a free rear Porbeagle Shark tip which is white. The second dorsal fin is tiny and is set above the occurs only in the anal fin, to which it is comparable in size. The caudal fin is strong and North Atlantic and lunate with a small terminal notch. The caudal keel is strong and, Mediterranean, uniquely for the northeast Atlantic, a smaller secondary caudal keel is whilst in the present. -
HEBRIDEAN MARINE MAMMAL ATLAS Part 1: Silurian, 15 Years of Marine Mammal Monitoring in the Hebrides 2 CONTENTS CONTENTS 3
HEBRIDEAN MARINE MAMMAL ATLAS Part 1: Silurian, 15 years of marine mammal monitoring in the Hebrides 2 CONTENTS CONTENTS 3 CONTENTS 1 2 3 4 5 6 INTRODUCTION SILURIAN HEBRIDES SPECIES FUTURE CONTRIBUTORS 4 8 22 26 56 58 Foreword About our Extraordinary Harbour Porpoise On the Horizon Acknowledgements Research Vessel Biodiversity 5 29 59 About Us 10 Minke Whale References Survey Protocol 5 33 A Message from 14 Basking Shark our Patron Data Review 37 6 Short-Beaked About the Atlas Common Dolphin 40 Bottlenose Dolphin 43 White-Beaked Dolphin 46 Risso’s Dolphin 49 Killer Whale (Orca) 53 Humpback Whale Suggested citation; Hebridean Whale and Dolphin Trust (2018). Hebridean Marine Mammal Atlas. Part 1: Silurian, 15 years of marine mammal monitoring in the Hebrides. A Hebridean Whale and Dolphin Trust Report (HWDT), Scotland, UK. 60 pp. Compiled by Dr Lauren Hartny-Mills, Science and Policy Manager, Hebridean Whale and Dolphin Trust 4 CONTENTS INTRODUCTION 5 FOREWORD INTRODUCTION About Us Established in 1994, the Hebridean Whale and Dolphin Based on the Isle of Mull, in the heart of the Trust (HWDT) is the trusted voice and leading source of Hebrides, HWDT is a registered charity that information for the conservation of Hebridean whales, has pioneered practical, locally based education dolphins and porpoises (cetaceans). and scientifically rigorous long-term monitoring programmes on cetaceans in the Hebrides. The Hebridean Marine Mammal Atlas is a showcase of We believe that evidence is the foundation of effective 15 years of citizen science and species monitoring in the conservation. Our research has critically advanced Hebrides. -
Deep Structure of the Foreland to the Caledonian Orogen, Nw Scotland: Results of the Birps Winch Profile
TECTONICS, VOL. 5, NO. 2, PAGES 171-194, APRIL 1986 DEEP STRUCTURE OF THE FORELAND TO THE CALEDONIAN OROGEN, NW SCOTLAND: RESULTS OF THE BIRPS WINCH PROFILE Jonathan A. Brewer Department of Earth Sciences, University of Cambridge, Cambridge, United Kingdom David K. Smythe British Geological Survey, Edinburgh, United Kingdom Abstract. The WINCH marine deep tal velocity for the Hebridean shelf of seismic reflection profile crosses the 6.4+0.1 km s-1. The eastward-dipping Fla- Hebridean shelf, the Proterozoic foreland nnan Thrust can be mapped into the upper to the Caledonian orogen, west of Scot- mantle on three lines from about 15 to land. The data quality is very good. The 45 km depth, well into the upper mantle. upper crust is largely devoid of coherent Neither the Flannan Thrust nor the Outer seismic reflections, although this may in Isles Thrust appear to pass straight thro- part be due to acquisition techniques ugh the reflective lower crust, suggesting being inappropriate for this problem. In that the lower crust is a region of high contrast, the middle and lower crust (10- strain. The Outer Hebrides is a positive 25 km depth) exhibits good reflections; block probably formed as an isostatic the mid crust contains reflectors which response to Mesozoic normal faulting which may be relics of early Palaeozoic, Caledo- reactivated the Outer Isles Thrust. nian (or earlier Grenvillian) eastward- INTRODUCTION dipping thrust zones, which pass into an acoustically strongly layered lower crust. The Western Isles-North Channel (WINCH) The Outer Isles Thrust is mapped from the surf ace to the mid crust, and tied into deep crustal seismic reflection profile was recorded for BIRPS (British Institut- its land outcrop on north Lewis. -
The Geochemical Associations of Metals and Organic
THE GEOCHEMICAL ASSOCIATIONS OF METALS AND ORGANIC MATTER IN WEST COAST SCOTTISH SEDIMENTS. by DAVID ODONNELL B.Sc. A Thesis Submitted For The Degree Of DOCTOR OF PHILOSOPHY At The University Of Edinburgh. December 1987. To My Father Terry O'Donnell Science, beauty, freedom, adventure, what more could you ask for in life?" Charles A Lindberg ABSTRACT. Thirteen sediment cores have been collected from a variety of sedimentary environments around the coast of Western Scotland ranging from terrestrially dominated fjords to more marine shelf areas. Eight of these cores have been examined in detail for the minor elements (Cu, Pb, Zn, Zr, Rb, Sc, Sr, Ba, Ni, Cr, Y), Rare Earth elements (La, Ce, Nd), organic components (C, N, S. I, Br,) and porewater components (S042 , alkalinity). In addition, some cores were analysed for 615N and also 137Cs (to estimate sediment accumulation rates). Study of the minor elements associated with the lithogenic fraction (Zr, Rb, Sc, Sr, Ba, Ni, Cr) has highlighted variations in sediment mineralogy and grain-size both spatially and temporally, showing that few of the sediments show steady state accumulation. Indeed, in one core an erosive event can be identified which has been calculated to have removed 18cm of sediment accumulation. In these sediments Ni and Cr have been shown to be associated with the detrital ferromagnesian fraction. Ni can therefore be used as an indicator of Iithogenic metal input. The distibution of the REE (La, Ce, Nd) show enrichments of La and Ce relative to V and mean shales in the more terrestrially dominated fjords suggesting a possible association with the iron oxide phase.