Chapter 8 Aquatic Biodiversity Summary Key Questions and Concepts
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Bathyal Zones of the Mediterranean Continental Slope: an Attempt
Publ: Espec. but. Esp. Oceanogr. 23. 1997: 23-33 P UBUCACIONES ESPECIALES L"lSTlTUTO ESP.I\NOL DE O CEANOGRAFIA ISSN; 021-1-7378 . ISBN: 81 ~19 1 -O 299-5 Ib Ministerio de Agriculrura, Pesca yAlimentacion , L997 Bathyal zones of the Mediterranean continental slope: An attempt c. C. Emig Centre d'Ocean ologie de Marseille (UMR-CNRS 6540) , Station Mari ne d 'Endoum e, Rue de la Batterie-des-Lions. 13007 Marseille, France. Received Febru ary 1996. A ccepted August 1 99 6. ABSTRACT On the con tine ntal slop e, th e bathyal can be divided into two zones, the upper bathya l and the middle bath yal, at the shelf break, which represents th e boun dary betwe en the coastal shelf environment an d the deep realm , located at about 100-110 m dep th. T he upper bathyal, previ ously considered a transitional zone, is characterised by distin ct physical, geological an d biol ogi cal features. Its bath ymen-ic extension is directly related to slope physiography, and its lower boun dary ge ne rally corresponds to the mud line. T his belt is governe d by specific abiotic factors with stee p physical grad ients (e.g., hydro dynam ics, salin ity, oxygen , temperat ure , sedirnen ts}. Major change in tbe benthic fauna is associated with major ch ange in these abiotic factors. The three main biocoeno ses are dominated by suspen sion-feed ing species, which are exclusive to th e Mediterran ean upper bathyal. Dep ending on water parameters, the limit between th e phytal and aphyta l systems gene ra lly occurs with in th e upper bathyal. -
INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The
INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The Intertidal Zone is the narrow belt along the shoreline lying between the lowest and highest tide marks. The intertidal or littoral zone is subdivided broadly into four vertical zones based on the amount of time the zone is submerged. From highest to lowest, they are Supratidal or Spray Zone Upper Intertidal submergence time Middle Intertidal Littoral Zone influenced by tides Lower Intertidal Subtidal Sublittoral Zone permanently submerged The intertidal zone may also be subdivided on the basis of the vertical distribution of the species that dominate a particular zone. However, zone divisions should, in most cases, be regarded as approximate! No single system of subdivision gives perfectly consistent results everywhere. Please refer to the intertidal zonation scheme given in the attached table (last page). Zonal Distribution of organisms is controlled by PHYSICAL factors (which set the UPPER limit of each zone): 1) tidal range 2) wave exposure or the degree of sheltering from surf 3) type of substrate, e.g., sand, cobble, rock 4) relative time exposed to air (controls overheating, desiccation, and salinity changes). BIOLOGICAL factors (which set the LOWER limit of each zone): 1) predation 2) competition for space 3) adaptation to biological or physical factors of the environment Species dominance patterns change abruptly in response to physical and/or biological factors. For example, tide pools provide permanently submerged areas in higher tidal zones; overhangs provide shaded areas of lower temperature; protected crevices provide permanently moist areas. Such subhabitats within a zone can contain quite different organisms from those typical for the zone. -
Beach Nourishment: Massdep's Guide to Best Management Practices for Projects in Massachusetts
BBEACHEACH NNOURISHMEOURISHMENNTT MassDEP’sMassDEP’s GuideGuide toto BestBest ManagementManagement PracticesPractices forfor ProjectsProjects inin MassachusettsMassachusetts March 2007 acknowledgements LEAD AUTHORS: Rebecca Haney (Coastal Zone Management), Liz Kouloheras, (MassDEP), Vin Malkoski (Mass. Division of Marine Fisheries), Jim Mahala (MassDEP) and Yvonne Unger (MassDEP) CONTRIBUTORS: From MassDEP: Fred Civian, Jen D’Urso, Glenn Haas, Lealdon Langley, Hilary Schwarzenbach and Jim Sprague. From Coastal Zone Management: Bob Boeri, Mark Borrelli, David Janik, Julia Knisel and Wendolyn Quigley. Engineering consultants from Applied Coastal Research and Engineering Inc. also reviewed the document for technical accuracy. Lead Editor: David Noonan (MassDEP) Design and Layout: Sandra Rabb (MassDEP) Photography: Sandra Rabb (MassDEP) unless otherwise noted. Massachusetts Massachusetts Office Department of of Coastal Zone Environmental Protection Management 1 Winter Street 251 Causeway Street Boston, MA Boston, MA table of contents I. Glossary of Terms 1 II. Summary 3 II. Overview 6 • Purpose 6 • Beach Nourishment 6 • Specifications and Best Management Practices 7 • Permit Requirements and Timelines 8 III. Technical Attachments A. Beach Stability Determination 13 B. Receiving Beach Characterization 17 C. Source Material Characterization 21 D. Sample Problem: Beach and Borrow Site Sediment Analysis to Determine Stability of Nourishment Material for Shore Protection 22 E. Generic Beach Monitoring Plan 27 F. Sample Easement 29 G. References 31 GLOSSARY Accretion - the gradual addition of land by deposition of water-borne sediment. Beach Fill – also called “artificial nourishment”, “beach nourishment”, “replenishment”, and “restoration,” comprises the placement of sediment within the nearshore sediment transport system (see littoral zone). (paraphrased from Dean, 2002) Beach Profile – the cross-sectional shape of a beach plotted perpendicular to the shoreline. -
MARINE ENVIRONMENTS Teaching Module for Grades 6-12
MARINE ENVIRONMENTS Teaching Module for Grades 6-12 Dear Educator, We are pleased to present you with the first in a series of teaching and learning modules developed by the DEEPEND (Deep-Pelagic Nekton Dynamics) consortium and their consultants. DEEPEND is a research network focusing primarily on the pelagic zone of the Gulf of Mexico, therefore the majority of the lessons will be based around this topic. Whenever possible, the lessons will focus specifically on events of the Gulf of Mexico or work from the DEEPEND scientists. All modules in this series aim to engage students in grades 6 through 12 in STEM disciplines, while promoting student learning of the marine environment. We hope these lessons enable teachers to address student misconceptions and apprehensions regarding the unique organisms and properties of marine ecosystems. We intend for these modules to be a guide for teaching. Teachers are welcome to use the lessons in any order they wish, use just portions of lessons, and may modify the lessons as they wish. Furthermore, educators may share these lessons with other school districts and teachers; however, please do not receive monetary gain for lessons in any of the modules. Moreover, please provide credit to photographers and authors whenever possible. This first module focuses on the marine environment in general including biological, chemical, and physical properties of the water column. We have provided a variety of activities and extensions within this module such that lessons can easily be adapted for various grade and proficiency levels. Given that education reform strives to incorporate authentic science experiences, many of these lessons encourage exploration and experimentation to encourage students to think and act like a scientist. -
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. -
Lake Ecology
Fundamentals of Limnology Oxygen, Temperature and Lake Stratification Prereqs: Students should have reviewed the importance of Oxygen and Carbon Dioxide in Aquatic Systems Students should have reviewed the video tape on the calibration and use of a YSI oxygen meter. Students should have a basic knowledge of pH and how to use a pH meter. Safety: This module includes field work in boats on Raystown Lake. On average, there is a death due to drowning on Raystown Lake every two years due to careless boating activities. You will very strongly decrease the risk of accident when you obey the following rules: 1. All participants in this field exercise will wear Coast Guard certified PFDs. (No exceptions for teachers or staff). 2. There is no "horseplay" allowed on boats. This includes throwing objects, splashing others, rocking boats, erratic operation of boats or unnecessary navigational detours. 3. Obey all boating regulations, especially, no wake zone markers 4. No swimming from boats 5. Keep all hands and sampling equipment inside of boats while the boats are moving. 6. Whenever possible, hold sampling equipment inside of the boats rather than over the water. We have no desire to donate sampling gear to the bottom of the lake. 7. The program director has final say as to what is and is not appropriate safety behavior. Failure to comply with the safety guidelines and the program director's requests will result in expulsion from the program and loss of Field Station privileges. I. Introduction to Aquatic Environments Water covers 75% of the Earth's surface. We divide that water into three types based on the salinity, the concentration of dissolved salts in the water. -
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. -
Hydrodynamics and Morphodynamics in the Swash Zone: Hydralab Iii Large-Scale Experiments
UNIVERSITÀ DEGLI STUDI DI NAPOLI ―FEDERICO II‖ in consorzio con SECONDA UNIVERSITÀ DI NAPOLI UNIVERSITÀ ―PARTHENOPE‖ NAPOLI in convenzione con ISTITUTO PER L‘AMBIENTE MARINO COSTIERO – C.N.R. STAZIONE ZOOLOGICA ―ANTON DOHRN‖ Dottorato in Scienze ed Ingegneria del Mare XXIV ciclo Tesi di Dottorato HYDRODYNAMICS AND MORPHODYNAMICS IN THE SWASH ZONE: HYDRALAB III LARGE-SCALE EXPERIMENTS Relatore: Prof. Diego Vicinanza Co-relatore: Prof. Maurizio Brocchini Candidato: Ing. Pasquale Contestabile Il Coordinatore del Dottorato: Prof. Alberto Incoronato ANNO 2011 ABSTRACT The modelling of swash zone hydrodynamics and sediment transport and the resulting morphodynamics has been an area of very active research over the last decade. However, many details are still to be understood, whose knowledge will be greatly advanced by the collection of high quality data under controlled large-scale laboratory conditions. The advantage of using a large wave flume is that scale effects that affected previous laboratory experiments are minimized. In this work new large-scale laboratory data from two sets of experiments are presented. Physical model tests were performed in the large-scale wave flumes at the Grosser Wellen Kanal (GWK) in Hannover and at the Catalonia University of Technology (UPC) in Barcelona, within the Hydralab III program. The tests carried out at the GWK aimed at improving the knowledge of the hydrodynamic and morphodynamic behaviour of a beach containing a buried drainage system. Experiments were undertaken using a set of multiple drains, up to three working simultaneously, located within the beach and at variable distances from the shoreline. The experimental program was organized in series of tests with variable wave energy. -
Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun
OCEANOGRAPHY – Vol.II - Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun BIOLOGICAL OCEANOGRAPHY Legendre, Louis and Rassoulzadegan, Fereidoun Laboratoire d'Océanographie de Villefranche, France. Keywords: Algae, allochthonous nutrient, aphotic zone, autochthonous nutrient, Auxotrophs, bacteria, bacterioplankton, benthos, carbon dioxide, carnivory, chelator, chemoautotrophs, ciliates, coastal eutrophication, coccolithophores, convection, crustaceans, cyanobacteria, detritus, diatoms, dinoflagellates, disphotic zone, dissolved organic carbon (DOC), dissolved organic matter (DOM), ecosystem, eukaryotes, euphotic zone, eutrophic, excretion, exoenzymes, exudation, fecal pellet, femtoplankton, fish, fish lavae, flagellates, food web, foraminifers, fungi, harmful algal blooms (HABs), herbivorous food web, herbivory, heterotrophs, holoplankton, ichthyoplankton, irradiance, labile, large planktonic microphages, lysis, macroplankton, marine snow, megaplankton, meroplankton, mesoplankton, metazoan, metazooplankton, microbial food web, microbial loop, microheterotrophs, microplankton, mixotrophs, mollusks, multivorous food web, mutualism, mycoplankton, nanoplankton, nekton, net community production (NCP), neuston, new production, nutrient limitation, nutrient (macro-, micro-, inorganic, organic), oligotrophic, omnivory, osmotrophs, particulate organic carbon (POC), particulate organic matter (POM), pelagic, phagocytosis, phagotrophs, photoautotorphs, photosynthesis, phytoplankton, phytoplankton bloom, picoplankton, plankton, -
Translation 3204
4 of 6 I' rÉ:1°.r - - - Ï''.ec.n::::,- - — TRANSLATION 3204 and Van, else--- de ,-0,- SERIES NO(S) ^4p €'`°°'°^^`m`^' TRANSLATION 3204 5 of 6 serceaesoe^nee SERIES NO.(S) serv,- i°- I' ann., Canada ° '° TRANSLATION 3204 6 of 6 SERIES NO(S) • =,-""r I FISHERIES AND MARINE SERVICE ARCHIVE:3 Translation Series No. 3204 Multidisciplinary investigations of the continental slope in the Gulf of Alaska area by Z.A. Filatova (ed.) Original title: Kompleksnyye issledovaniya materikovogo sklona v raione Zaliva Alyaska From: Trudy Instituta okeanologii im. P.P. ShirshoV (Publications of the P.P. Shirshov Oceanpgraphy Institute), 91 : 1-260, 1973 Translated by the Translation Bureau(HGC) Multilingual Services Division Department of the Secretary of State of Canada Department of the Environment Fisheries and Marine Service Pacific Biological Station Nanaimo, B.C. 1974 ; 494 pages typescriPt "DEPARTMENT OF THE SECRETARY OF STATE SECRÉTARIAT D'ÉTAT TRANSLATION BUREAU BUREAU DES TRADUCTIONS MULTILINGUAL SERVICES DIVISION DES SERVICES DIVISION MULTILINGUES ceÔ 'TRANSLATED FROM - TRADUCTION DE INTO - EN Russian English Ain HOR - AUTEUR Z. A. Filatova (ed.) ri TL E IN ENGLISH - TITRE ANGLAIS Multidisciplinary investigations of the continental slope in the Gulf of Aâaska ares TI TLE IN FORE I GN LANGuAGE (TRANS LI TERA TE FOREIGN CHARACTERS) TITRE EN LANGUE ÉTRANGÈRE (TRANSCRIRE EN CARACTÈRES ROMAINS) Kompleksnyye issledovaniya materikovogo sklona v raione Zaliva Alyaska. REFERENCE IN FOREI GN LANGUAGE (NAME: OF BOOK OR PUBLICATION) IN FULL. TRANSLI TERATE FOREIGN CHARACTERS, RÉFÉRENCE EN LANGUE ÉTRANGÈRE (NOM DU LIVRE OU PUBLICATION), AU COMPLET, TRANSCRIRE EN CARACTÈRES ROMAINS. Trudy Instituta okeanologii im. P.P. -
The EUNIS Habitat Classification. ICES CM 2000/T:04
Theme Session on Classification and Mapping of Marine Habitats CM 2000/T:04 The EUNIS Habitat Classification SUMMARY The EUNIS habitat classification has been developed on behalf of the European Environment Agency to facilitate description of marine and terrestrial European habitats through the use of criteria for habitat identification. It is a broadly-based hierarchical classification which provides an easily understood common language for habitats. It builds on earlier initiatives (CORINE and Palaearctic habitat classifications) and incorporates existing classifications used by European marine Conventions and the EU-funded BioMar project with cross-references to these and other systems. It is recognised that detailed biotopes from some marine regions are poorly represented and that EUNIS will need to be expanded to cover this wider geographic area. Most of the additions will probably be made at hierarchical level 5 (where the distinct BioMar and Mediterranean units are now held). Changes and additions to the classification will only be made following detailed consultation with experts. A key to the habitat units at each of the first three levels is incorporated and the classification is linked to a parameter-based database to describe specific habitats. The present draft of the EUNIS habitat classification was completed in November 1999 and is expected to remain stable for a time to allow validation and testing through field trials and descriptive parameters to be compiled. Cynthia E. Davies and Dorian Moss: CEH Monks Wood, Abbots Ripton, Huntingdon, Cambridgeshire, PE28 2LS, UK Tel: +44 (0)1487 772400 Fax: +44 (0)1487 773467 email: [email protected], [email protected] INTRODUCTION The European Environment Agency (EEA) Topic Centre on Nature Conservation (ETC/NC) is developing a European Nature Information System, EUNIS, which has two main aims: to facilitate use of data by promoting harmonisation of terminology and definitions and to be a reservoir of information on European environmentally important matters. -
Patterns of Bathymetric Zonation of Bivalves in the Porcupine Seabight and Adjacent Abyssal Plain, NE Atlantic
ARTICLE IN PRESS Deep-Sea Research I 52 (2005) 15–31 www.elsevier.com/locate/dsr Patterns of bathymetric zonation of bivalves in the Porcupine Seabight and adjacent Abyssal plain, NE Atlantic Celia Olabarriaà Southampton Oceanography Centre, DEEPSEAS Benthic Biology Group, Empress Dock, Southampton SO14 3ZH, UK Received 23 April2004; received in revised form 21 September 2004; accepted 21 September 2004 Abstract Although the organization patterns of fauna in the deep sea have been broadly documented, most studies have focused on the megafauna. Bivalves represent about 10% of the deep-sea macrobenthic fauna, being the third taxon in abundance after polychaetes and peracarid crustaceans. This study, based on a large data set, examined the bathymetric distribution, patterns of zonation and diversity–depth trends of bivalves from the Porcupine Seabight and adjacent Abyssal Plain (NE Atlantic). A total of 131,334 individuals belonging to 76 species were collected between 500 and 4866 m. Most of the species showed broad depth ranges with some ranges extending over more than 3000 m. Furthermore, many species overlapped in their depth distributions. Patterns of zonation were not very strong and faunal change was gradual. Nevertheless, four bathymetric discontinuities, more or less clearly delimited, occurred at about 750, 1900, 2900 and 4100 m. These boundaries indicated five faunistic zones: (1) a zone above 750 m marking the change from shelf species to bathyal species; (2) a zone from 750 to 1900 m that corresponds to the upper and mid- bathyalzones taken together; (3) a lowerbathyalzone from 1900 to 2900 m; (4) a transition zone from 2900 to 4100 m where the bathyal fauna meets and overlaps with the abyssal fauna and (5) a truly abyssal zone from approximately 4100–4900 m (the lower depth limit of this study), characterized by the presence of abyssal species with restricted depth ranges and a few specimens of some bathyalspecies with very broad distributions.