D2.1 Classification Map of Running Waters Considering Fish Community
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Guidance Document on the Strict Protection of Animal Species of Community Interest Under the Habitats Directive 92/43/EEC
Guidance document on the strict protection of animal species of Community interest under the Habitats Directive 92/43/EEC Final version, February 2007 1 TABLE OF CONTENTS FOREWORD 4 I. CONTEXT 6 I.1 Species conservation within a wider legal and political context 6 I.1.1 Political context 6 I.1.2 Legal context 7 I.2 Species conservation within the overall scheme of Directive 92/43/EEC 8 I.2.1 Primary aim of the Directive: the role of Article 2 8 I.2.2 Favourable conservation status 9 I.2.3 Species conservation instruments 11 I.2.3.a) The Annexes 13 I.2.3.b) The protection of animal species listed under both Annexes II and IV in Natura 2000 sites 15 I.2.4 Basic principles of species conservation 17 I.2.4.a) Good knowledge and surveillance of conservation status 17 I.2.4.b) Appropriate and effective character of measures taken 19 II. ARTICLE 12 23 II.1 General legal considerations 23 II.2 Requisite measures for a system of strict protection 26 II.2.1 Measures to establish and effectively implement a system of strict protection 26 II.2.2 Measures to ensure favourable conservation status 27 II.2.3 Measures regarding the situations described in Article 12 28 II.2.4 Provisions of Article 12(1)(a)-(d) in relation to ongoing activities 30 II.3 The specific protection provisions under Article 12 35 II.3.1 Deliberate capture or killing of specimens of Annex IV(a) species 35 II.3.2 Deliberate disturbance of Annex IV(a) species, particularly during periods of breeding, rearing, hibernation and migration 37 II.3.2.a) Disturbance 37 II.3.2.b) Periods -
Publis14-Mistea-007 {5E1DA239
Bayesian hierarchical model used to analyze regression between fish body size and scale size: application torare fish species Zingel asper Bénédicte Fontez Nguyen The, Laurent Cavalli To cite this version: Bénédicte Fontez Nguyen The, Laurent Cavalli. Bayesian hierarchical model used to analyze regression between fish body size and scale size: application to rare fish species Zingel asper. Knowledge and Management of Aquatic Ecosystems, EDP sciences/ONEMA, 2014, pp.10P1-10P8. 10.1051/kmae/2014008. hal-01499072 HAL Id: hal-01499072 https://hal.archives-ouvertes.fr/hal-01499072 Submitted on 30 Mar 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Knowledge and Management of Aquatic Ecosystems (2014) 413, 10 http://www.kmae-journal.org c ONEMA, 2014 DOI: 10.1051/kmae/2014008 Bayesian hierarchical model used to analyze regression between fish body size and scale size: application to rare fish species Zingel asper B. Fontez(1),(2), L. Cavalli(3), Received May 24, 2013 Revised February 20, 2014 Accepted February 21, 2014 ABSTRACT Key-words: Back-calculation allows to increase available data on fish growth. The ac- hierarchical curacy of back-calculation models is of paramount importance for growth Bayes model, analysis. -
A Systematic Nomenclature for Metamorphic Rocks
A systematic nomenclature for metamorphic rocks: 1. HOW TO NAME A METAMORPHIC ROCK Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: Web version 1/4/04. Rolf Schmid1, Douglas Fettes2, Ben Harte3, Eleutheria Davis4, Jacqueline Desmons5, Hans- Joachim Meyer-Marsilius† and Jaakko Siivola6 1 Institut für Mineralogie und Petrographie, ETH-Centre, CH-8092, Zürich, Switzerland, [email protected] 2 British Geological Survey, Murchison House, West Mains Road, Edinburgh, United Kingdom, [email protected] 3 Grant Institute of Geology, Edinburgh, United Kingdom, [email protected] 4 Patission 339A, 11144 Athens, Greece 5 3, rue de Houdemont 54500, Vandoeuvre-lès-Nancy, France, [email protected] 6 Tasakalliontie 12c, 02760 Espoo, Finland ABSTRACT The usage of some common terms in metamorphic petrology has developed differently in different countries and a range of specialised rock names have been applied locally. The Subcommission on the Systematics of Metamorphic Rocks (SCMR) aims to provide systematic schemes for terminology and rock definitions that are widely acceptable and suitable for international use. This first paper explains the basic classification scheme for common metamorphic rocks proposed by the SCMR, and lays out the general principles which were used by the SCMR when defining terms for metamorphic rocks, their features, conditions of formation and processes. Subsequent papers discuss and present more detailed terminology for particular metamorphic rock groups and processes. The SCMR recognises the very wide usage of some rock names (for example, amphibolite, marble, hornfels) and the existence of many name sets related to specific types of metamorphism (for example, high P/T rocks, migmatites, impactites). -
Geochemical Consideration of Some Granitoids Around Ojirami-Ogbo and Environs, Southwestern Nigeria
PRINT ISSN 1119-8362 Full-text Available Online at J. Appl. Sci. Environ. Manage. Electronic ISSN 1119-8362 https://www.ajol.info/index.php/jasem Vol. 23 (6) 1127-1131 June 2019 http://ww.bioline.org.br/ja Geochemical Consideration of some Granitoids around Ojirami-Ogbo and Environs, Southwestern Nigeria *1ODOKUMA-ALONGE, O; 2EGWUATU, PN; 3OKUNUWADJE, SE Department of Geology, Faculty of Physical Sciences, University of Benin, Benin City, Nigeria *Corresponding Author Email: [email protected] ABSTRACT: Five (5) granitoid samples from Ojirami-Ogbo and Environs in Akoko-Edo area of southwestern Nigeria were obtained with the aim of determining their geochemical properties using the XRF and Xrd techniques. Results from the analysis revealed the presence of SiO2 (51.41-64.84%), Al2O3 (21.37-36.25%), Fe2O3 (5.89-8.02%), MgO (0.98-2.11%), K2O (0.02-0.97%) and Na2O (0.04-0.08%) all in wt%. Using the Al2O3 and SiO2 saturation schemes in classifying igneous rocks, sample two, three, four and five gave Al2O3 wt% values of 33.30%, 32.00%, 23.20%, 21.37% greater than the molars proportions of (Al2O3/CaO+Na2O+K2O) with values 22.54, 30.06, 22.10 and 14.07, and are peraluminous rocks while sample one had 36.25% and 43.10, respectively and is considered to be metaluminous. The SiO2 composition of the rocks ranges from 51.41-66.40% hence reveals a mafic to intermediate composition. The main felsic minerals from XrD analysis revealed the presence of quartz, alkali and plagioclase feldspars. Using the QAP diagram, the rocks fall within the granitoidal class. -
Genetic Structure of Fragmented Populations of a Threatened Endemic Percid of the Rhoˆne River: Zingel Asper
Heredity (2004) 92, 329–334 & 2004 Nature Publishing Group All rights reserved 0018-067X/04 $25.00 www.nature.com/hdy Genetic structure of fragmented populations of a threatened endemic percid of the Rhoˆne river: Zingel asper J Laroche1,2 and JD Durand1,3 1Laboratoire d’Ecologie des Hydrosyste`mes Fluviaux, UMR CNRS 5023, Universite´ Claude Bernard, 43 bd du 11 Novembre 1918, 69622 Villeurbanne cedex, France; 2Laboratoire Ressources Halieutiques – Poissons Marins, Institut Universitaire Europe´en de la Mer, Place Nicolas Copernic, 29280, Plouzane´, France; 3IRD/Laboratoire Ge´nome, Populations, Interactions, UMR CNRS 5000, Universite´ Montpellier II, Station Me´diterrane´enne de l’Environnement Littoral 1, quai de la Daurade F-34200 Se`te, France Zingel asper is an endemic percid of the Rhoˆne basin equilibrium between mutation and drift. Thus, this population considered to be critically endangered. This species was shows an apparently better evolutionary potential for long- continuously distributed throughout the Rhoˆne in 1900, but term survival. Since 1930, a marked fragmentation of the today only occupies 17% of its initial area. In the present whole Rhoˆne system has appeared, related to the develop- study, five microsatellite loci were used to assess the level of ment of dams, and we assume that the significant genetic genetic variability within and among populations localized in differentiation detected between the populations could different sub-basins. Contrasting results were obtained for mainly reflect the impact of this fragmentation. -
Geochronological and Geochemical Constraints on the Origin of Clastic Meta-Sedimentary Rocks Associated with the Yuanjiacun BIF from the Lüliang Complex, North China
Lithos 212–215 (2015) 231–246 Contents lists available at ScienceDirect Lithos journal homepage: www.elsevier.com/locate/lithos Geochronological and geochemical constraints on the origin of clastic meta-sedimentary rocks associated with the Yuanjiacun BIF from the Lüliang Complex, North China Changle Wang a,b, Lianchang Zhang a,⁎,YanpeiDaia,b,CaiyunLanb,c a Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China b University of Chinese Academy of Sciences, Beijing 100049, China c Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangdong, Guangzhou 510640, China article info abstract Article history: The Lüliang Complex is situated in the central part of the western margin of the Trans-North China Orogen Received 6 May 2014 (TNCO) in the North China Craton (NCC), and consists of metamorphic volcanic and sedimentary rocks and Accepted 14 November 2014 granitoid intrusions. The Yuanjiacun Formation metasediments occupy roughly the lowest part of the Lüliang Available online 27 November 2014 Group and are mainly represented by well-bedded meta-pelites (chlorite schists and sericite–chlorite phyllites), banded iron formations (BIFs) and meta-arenites (sericite schists), which have undergone greenschist-facies Keywords: metamorphism. The youngest group of detrital zircons from the meta-arenite samples constrains their maximum Yuanjiacun Formation Lüliang Complex depositional age at ~2350 Ma. In combination with previous geochronological studies on meta-volcanic rocks in Trans-North China Orogen the overlying Jinzhouyu Formation, the depositional age of the Yuanjiacun Formation can be constrained Detrital zircon between 2350 and 2215 Ma. The metasediments have suffered varying degrees of source weathering, measured Geochemistry using widely employed weathering indices (e.g., CIA, CIW, PIA and Th/U ratios). -
Actualisation Des Connaissances Sur La Population D'aprons Du Rhône (Zingel Asper) Dans Le Doubs Franco-Suisse
Master Sciences de la Terre, de l'Eau et de l'Environnement Ingénierie des Hydrosystèmes et des Bassins Versants Parcours IMACOF Rapport de stage pour l'obtention de la 2ème année de Master Actualisation des connaissances sur la population d’aprons du Rhône (Zingel Asper) dans le Doubs franco-suisse - linéaire du futur Parc Naturel Régional transfrontalier - Propositions d’actions en faveur de l’espèce et de son milieu Florian BONNAIRE Septembre, 2012 Maître de stage : François BOINAY Organisme : Centre Nature Les Cerlatez Photo, 1ère de couverture : deux aprons vus le 13 août 2012 sur les gravières de Saint- Ursanne, dont le seul jeune individu observé au cours de cette campagne 2012. Photo prise par : Florian Bonnaire REMERCIEMENTS Nombreux sont ceux qui m’ont soutenu jusqu’à l’aboutissement de cette étude. Mes prochains remerciements iront donc à ces gens passionnants qui m’ont ouvert leurs portes et enrichi à leur manière cette belle aventure. Tout d’abord, mes remerciements vont à François Boinay, mon maître de stage mais aussi directeur du Centre Nature les Cerlatez. Merci pour m’avoir offert l’opportunité de faire ce stage passionnant au cœur des paysages grandioses de la vallée du Doubs franco-suisse. Merci pour ton aide précieuse mais aussi ton humour formidable que je n’oublierai pas. À Mickael Béjean, cet homme entièrement dévoué à l’apron sans qui cette étude n’aurait pas pris tout son sens. Merci pour tous ces conseils et partages d’expériences plus que bénéfiques, ainsi que pour ces quelques prospections nocturnes et subaquatiques. À Marianne Georget, animatrice du Plan National d’Action en faveur de l’apron du Rhône, pour m’avoir ouvert les portes des spécialistes, sans quoi le déroulement de ce stage n’aurait certainement pas pris cette dimension transfrontalière. -
Proterozoic Deformation in the Northwest of the Archean Yilgarn Craton, Western Australia Catherine V
Available online at www.sciencedirect.com Precambrian Research 162 (2008) 354–384 Proterozoic deformation in the northwest of the Archean Yilgarn Craton, Western Australia Catherine V. Spaggiari a,∗, Jo-Anne Wartho b,1, Simon A. Wilde b a Geological Survey of Western Australia, Department of Industry and Resources, 100 Plain Street, East Perth, Western Australia 6004, Australia b Department of Applied Geology, Curtin University, GPO Box U1987, Perth, Western Australia 6845, Australia Received 31 January 2007; received in revised form 19 September 2007; accepted 16 October 2007 Abstract The Narryer Terrane within the northwestern Yilgarn Craton contains the oldest crust in Australia. The Jack Hills greenstone belt is located within the southern part of the Narryer Terrane, and structures cutting it and surrounding rocks have been dated using the 40Ar/39Ar technique. The results show that east-trending, dextral, transpressive shearing was related to the 1830–1780 Ma Capricorn Orogeny, followed by further deformation and/or cooling between c. 1760 and 1740 Ma. These results confirm that major deformation has affected the northwestern part of the Yilgarn Craton in an intracratonic setting during the Proterozoic. Proterozoic structures have been interpreted to extend south beyond the Narryer Terrane into the northern part of the Youanmi Terrane (Murchison Domain), and include the Yalgar Fault, previously interpreted as the boundary between the Narryer and Youanmi Terranes. Terrane amalgamation pre-dated the emplacement of c. 2660 Ma granites in both terranes, and the current expression of the Yalgar Fault must represent a younger, reworked, post-amalgamation structure, possibly controlled by the tectonic boundary. However, new aeromagnetic and gravity imagery does not show the eastern part of the Yalgar Fault as a major structure. -
BCGS IC1997-03.Pdf
For information on the contents of this document contact: Ministry of Employment and Investment Energy and Minerals Division British Columbia Geological Survey Branch 5 - 1810 Blanshard Street PO Box 9320, Stn Prov Gov't Victoria, BC, V8W 9N3 Attn: W.J. McMillan, Manager, Map ing Section Fax: 250-952-0381 [mail: [email protected] or; B. Grant, Editor, GSB Fax: 250-952-0451 E-mail : [email protected]. bc.ca Canadian Cataloguing in Publication Data I Main entry under title: Specifications and guidelines for bedrock mapping in British Columbia Includes bibliographical references: p. ISBN 0-7726-2950-1 1. Geological mapping - British Columbia. 2. Geology, Structural - British Columbia. 3. Geology - Maps - Symbols. I. British Columbia. Geological Survey Branch. Victoria British Columbia May 1997 October, 1996 TaMb Off GmQmQs Introduction . 3 Fission Track Dating Technique . 36 Part 1: Fundamental Bedrock Mapping Concepts 5 Usual Application of Geochronology . 36 Part 2: Mapping and Field Survey Procedures. 7 Materials Suitable for Dating. 36 2-1 Overview. 7 Rubidium-strontium Dating . 38 2-2 Bedrock Field Survey Databases . 10 Uranium-Lead Dating . 3 8 2-3 Quality Control, Correlation, and Map Lead Isotope Analysis . 38 Reliability . 11 Fission Track Dating . 38 Part 3: Data Representation On Bedrock Maps 13 Analytical Procedure . 39 3-1 Title Block . 13 Quaternary Dating Methods . 39 3-2 Base Map Specifications . 15 Radiocarbon Dating . 39 3-3 Reliability Diagrams . 15 Potassium-Argon Dating of Quaternary 3-4 Legend . 16 Volcanic Rocks. 40 3-5 Map Attributes . 17 Fission Track Dating . 40 3-6 Symbols. 17 Sampling . 41 3-7 Map-unit Designations . -
Archean and Paleoproterozoic Geology of the Northwestern Split Lake Block, Superior Province, Manitoba (Parts of NTS 54D4, 5, 6 and 64A1) by R.P
GS-16 Archean and Paleoproterozoic geology of the northwestern Split Lake Block, Superior Province, Manitoba (parts of NTS 54D4, 5, 6 and 64A1) by R.P. Hartlaub1, C.O. Böhm, Y.D. Kuiper2, M.S. Bowerman1 and L.M. Heaman1 Hartlaub, R.P., Böhm, C.O., Kuiper, Y.D., Bowerman, M.S. and Heaman, L.M. 2004: Archean and Paleoproterozoic geology of the northwestern Split Lake Block, Superior Province, Manitoba (parts of NTS 54D4, 5, 6 and 64A1); in Report of Activities 2004, Manitoba Industry, Economic Development and Mines, Manitoba Geological Survey, p. 187–194. Summary The Split Lake Block is a shear zone–bounded lozenge of Archean and Paleoproterozoic rock that lies along the northwestern paleomargin of the Superior Province. The oldest units in the area include pelite, and mafic to ultramafic granulite that is interpreted to be supracrustal in origin. An igneous complex, composed of anorthosite, anorthositic gabbro, gabbro and mafic tonalite, has an unknown age relationship to these supracrustal rocks. Both the supracrustal rocks and the igneous complex occur as coherent bodies and as disrupted layers, rafts and xenoliths in younger granite, granodiorite and tonalite. The presence of granulite-facies mineral assemblages in Archean rocks indicates that the Split Lake Block was deeply buried during the Neoarchean. Local retrogression of the granulite-facies assemblages occurred during a later amphibolite-facies event. Overall, the lithological and metamorphic characteristics of the Split Lake Block are similar to those of the bounding Pikwitonei Granulite Domain. Additional isotopic study will be required, however, before a detailed chronological comparison is possible. A suite of weakly metamorphosed and variably deformed mafic dikes crosscuts the high-grade Archean rocks and constitutes at least 15% of the exposed outcrop in the Split Lake Block. -
Annex 1: Field Protocol
Annex 1: Field protocol Annex 1-Table 1: Fish data Fish data Date (dd/mm/yyyy) Site code Sampling method Site name Sampling location Name of watercourse Main river region XY co-ordinates GPS co-ordinates Longitude Transect length [m] Latitude Fished area [m2] Altitude[m] Wetted width [m] Fish data Fish species number of specimen number of specimen length ≤150 mm length >150 mm 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 Annex 1-Table 2: Abiotic and method data Reference fields Site code Date dd/mm/yyyy Site name Name of watercourse or River name River region XY co-ordinates or longitude, latitude GPS co-ordinates Altitude m Sampling location Main channel/Backwaters/Mixed Sampling method Boat/Wading Fished area m2 Wetted width m Abiotic variables Altitude m Lakes upstream affecting Yes / No the site Distance from source km Flow regime Permanent / Summer dry/Winter dry/Intermittent Geomophology Naturally constrained no modification/ Braided/Sinuous/Meand regular/Meand tortuous Former floodplain No/Small/Medium/Large/Some waterbodies remaining/ Water source type Glacial/Nival/Pluvial/Groundwater Former sediment size Organic/Silt/Sand/ Gravel-Pebble-Cobble/Boulder-Rock Upstream drainage area km2 Distance from source km River slope m/km (‰) Mean air temperature Celsius (°C) Annex 1-Table 3: Human impact data (optional) Site code hChemical data Name watercourse Oxygen (mg/l or % saturation) XYZ co-ordinates or X:……………………(N) Conductivity (mS/cm) longitude latitude altitude Y:……………………(E) Z :…………………….m -
The Nature of C. 2.0 Ga Crust Along the Southern Margin of the Gascoyne Complex by S
Geological Survey of Western Australia 1998–99 Annual Review The nature of c. 2.0 Ga crust along the southern margin of the Gascoyne Complex by S. Sheppard1, S. A. Occhipinti, I. M. Tyler, and D. R. Nelson Remapping of the ROBINSON RANGE* Abstract and GLENBURGH 1:250 000 map sheets in 1997 and 1998, as part of the The southern part of the Gascoyne Complex consists of foliated and Southern Gascoyne Complex Project, gneissic granites of the Dalgaringa Supersuite, as well as pelitic and combined with SHRIMP U–Pb zircon calc-silicate gneisses of the Camel Hills Metamorphics, the protoliths geochronology (Nelson, 1998, 1999), of which were deposited between c. 2025 and c. 1960 Ma. The confirms that rocks of the Yilgarn Dalgaringa Supersuite mainly consists of 2005–1975 Ma foliated and Craton are not present north of the gneissic tonalite, granodiorite, and monzogranite. SHRIMP U–Pb Errabiddy Shear Zone in the mapped dating has not yet found any trace of Archaean rocks of the Yilgarn area (Fig. 1). Instead, the crust along Craton in the southern Gascoyne Complex. The complex may have the southern margin of the Gascoyne formed as a convergent continental margin above a northwesterly Complex mainly, or entirely, formed dipping subduction zone before it was accreted to the Yilgarn between 2005 and 1975 Ma. Craton at c. 1960 Ma during the Glenburgh Orogeny. Furthermore, this crust was deformed and metamorphosed at KEYWORDS: Proterozoic, structural terranes, granite, medium to high grade up to 150 geochronology, Gascoyne Complex, Dalgaringa million years before collision of the Supersuite, Camel Hills Metamorphics, Glenburgh Yilgarn and Pilbara Cratons between Orogeny 1840 and 1800 Ma (Tyler et al., 1998; Occhipinti et al., 1998).