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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. -
Propuesta De Áreas Marinas De Importancia Ecológica : Islas Canarias
Islas Canarias PROPUESTA DE ÁREAS MARINAS DE IMPORTANCIA ECOLÓGICA Plaza de España - Leganitos, 47 1350 Connecticut Ave., NW, 5th Floor Av. Condell 520, 28013 Madrid (España) Washington D.C., 20036 (USA) Providencia, Santiago (Chile) Tel.: + 34 911 440 880 Tel.: + 1 (202) 833 3900 CP 7500875 Islas Canarias Fax: + 34 911 440 890 Fax: + 1 (202) 833 2070 Tel.: + 56 2 925 5600 [email protected] [email protected] Fax: + 56 2 925 5610 www.oceana.org [email protected] 175 South Franklin Street - Suite 418 Rue Montoyer, 39 Juneau, Alaska 99801 (USA) 1000 Bruselas (Bélgica) Tel.: + 1 (907) 586 40 50 Tel.: + 32 (0) 2 513 22 42 Fax: + 1(907) 586 49 44 Fax: + 32 (0) 2 513 22 46 [email protected] [email protected] PROPUESTA DE ÁREAS MARINAS IMPORTANCIA ECOLÓGICA PROPUESTA DE ÁREAS MARINAS DE IMPORTANCIA ECOLÓGICA Islas Canarias índice 1 INTRODUCCIÓN ___________________________________________________________________ 004 Características oceánicas Características geológicas Áreas Marinas Protegidas 2 METODOLOGÍA ____________________________________________________________________ 020 3 RESULTADOS POR ZONAS _________________________________________________________ 026 Lanzarote ________________________________________________________________________ 028 Cagafrecho La Isleta Isla de La Graciosa e Islotes del Norte de Lanzarote Cuevas submarinas Estrecho de la Bocayna Fuerteventura ____________________________________________________________________ 050 Isla de Lobos Jandía Oeste de la isla: Pájara y Betancuria Banco de Amanay y Banquete Gran -
Islas Canarias
Islas Canarias PROPUESTA DE ÁREAS MARINAS DE IMPORTANCIA ECOLÓGICA Plaza de España - Leganitos, 47 1350 Connecticut Ave., NW, 5th Floor Av. Condell 520, 28013 Madrid (España) Washington D.C., 20036 (USA) Providencia, Santiago (Chile) Tel.: + 34 911 440 880 Tel.: + 1 (202) 833 3900 CP 7500875 Islas Canarias Fax: + 34 911 440 890 Fax: + 1 (202) 833 2070 Tel.: + 56 2 925 5600 [email protected] [email protected] Fax: + 56 2 925 5610 www.oceana.org [email protected] 175 South Franklin Street - Suite 418 Rue Montoyer, 39 Juneau, Alaska 99801 (USA) 1000 Bruselas (Bélgica) Tel.: + 1 (907) 586 40 50 Tel.: + 32 (0) 2 513 22 42 Fax: + 1(907) 586 49 44 Fax: + 32 (0) 2 513 22 46 [email protected] [email protected] PROPUESTA DE ÁREAS MARINAS IMPORTANCIA ECOLÓGICA PROPUESTA DE ÁREAS MARINAS DE IMPORTANCIA ECOLÓGICA Islas Canarias índice 1 INTRODUCCIÓN ___________________________________________________________________ 004 Características oceánicas Características geológicas Áreas Marinas Protegidas 2 METODOLOGÍA ____________________________________________________________________ 020 3 RESULTADOS POR ZONAS _________________________________________________________ 026 Lanzarote ________________________________________________________________________ 028 Cagafrecho La Isleta Isla de La Graciosa e Islotes del Norte de Lanzarote Cuevas submarinas Estrecho de la Bocayna Fuerteventura ____________________________________________________________________ 050 Isla de Lobos Jandía Oeste de la isla: Pájara y Betancuria Banco de Amanay y Banquete Gran -
Biogeography of the Recent Brachiopods O
ISSN 0031-0301, Paleontological Journal, 2008, Vol. 42, No. 8, pp. 830–858. © Pleiades Publishing, Ltd., 2008. Biogeography of the Recent Brachiopods O. N. Zezina Shirshov Institute of Oceanology, Russian Academy of Sciences, Nakhimovskii pr. 36, Moscow, 117997 Russia e-mail: [email protected] Received July 3, 2007 Abstract—The vertical, latitudinal, and circumcontinental zonality of the distribution of the species, genera, and families of recent brachiopods is considered. The distortions of the latitudinal and meridional symmetry of the biogeographic structure of the ocean are analyzed in view of the patterns of the global circulation of the surface and intermediate waters. Thus ancient faunas may be reconstructed based on data on the structural char- acteristics of the taxocene of recent brachiopods. The features of the paedomorphic evolution of brachiopods from the different families in extreme habitats (interstitial, underwater caverns, submarine rises, abyssal depths, hydrothermal areas, and margins of habitats) are discussed. The biogeographic structure of bottom dwellers is shown to simplify with depth as well as with simplification of the hydrological structure of the ocean. The important role of the bathyal oceanic zone (slopes of continents, islands, submarine mountains, ridges, and rises) in the preservation of faunal relicts is shown. The historical change from brachiopods to bivalves that occurred from the Paleozoic to the Mesozoic and Cenozoic is shown to have resulted not from competitive exclusion, but from complex and global changes in the plankton composition, which were unfavorable for artic- ulate brachiopods, which had already developed specialized feeding habits, feeding on food that led to the pro- duction of almost no metabolic waste products; they had even partly lost their alimentary canal. -
Neuromuscular Development in Novocrania Anomala: Evidence for the Presence of Serotonin and a Spiralian-Like Apical Organ in Lecithotrophic Brachiopod Larvae
Neuromuscular development in Novocrania anomala: evidence for the presence of serotonin and a spiralian-like apical organ in lecithotrophic brachiopod larvae Altenburger, Andreas; Wanninger, Andreas Wilhelm Georg Published in: Evolution & Development DOI: 10.1111/j.1525-142X.2009.00387.x Publication date: 2010 Document version Early version, also known as pre-print Citation for published version (APA): Altenburger, A., & Wanninger, A. W. G. (2010). Neuromuscular development in Novocrania anomala: evidence for the presence of serotonin and a spiralian-like apical organ in lecithotrophic brachiopod larvae. Evolution & Development, 12(1), 16-24. https://doi.org/10.1111/j.1525-142X.2009.00387.x Download date: 30. Sep. 2021 Neuromuscular development in Novocrania anomala: evidence for the presence of serotonin and a spiralian-like apical organ in lecithotrophic brachiopod larvae Andreas Altenburger, Andreas Wanninger* University of Copenhagen, Deptartment of Biology, Research Group for Comparative Zoology, Universitetsparken 15, DK-2100 Copenhagen Ø, Denmark *corresponding author. E-mail: [email protected] Phone: +45-35321240 Fax: +45-35321200 Running Title: Brachiopod neuromuscular development Word count: 3975 1 ABSTRACT The phylogenetic position of Brachiopoda remains unsettled, and only few recent data on brachiopod organogenesis are currently available. In order to contribute to questions concerning brachiopod ontogeny and evolution we investigated nervous and muscle system development in the craniiform (inarticulate) brachiopod Novocrania anomala. Larvae of this species are lecithotrophic and have a bilobed body with three pairs of dorsal setal bundles which emerge from the posterior lobe. Fully developed larvae exhibit a network of setae pouch muscles as well as medioventral longitudinal and transversal muscles. After settlement, the anterior and posterior adductor muscles and delicate mantle retractor muscles start to form. -
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MarLIN Marine Information Network Information on the species and habitats around the coasts and sea of the British Isles Novocrania anomala and Protanthea simplex on very wave-sheltered circalittoral rock MarLIN – Marine Life Information Network Marine Evidence–based Sensitivity Assessment (MarESA) Review John Readman 2018-02-16 A report from: The Marine Life Information Network, Marine Biological Association of the United Kingdom. Please note. This MarESA report is a dated version of the online review. Please refer to the website for the most up-to-date version [https://www.marlin.ac.uk/habitats/detail/1162]. All terms and the MarESA methodology are outlined on the website (https://www.marlin.ac.uk) This review can be cited as: Readman, J.A.J., 2018. [Novocrania anomala] and [Protanthea simplex] on very wave-sheltered circalittoral rock. In Tyler-Walters H. and Hiscock K. (eds) Marine Life Information Network: Biology and Sensitivity Key Information Reviews, [on-line]. Plymouth: Marine Biological Association of the United Kingdom. DOI https://dx.doi.org/10.17031/marlinhab.1162.1 The information (TEXT ONLY) provided by the Marine Life Information Network (MarLIN) is licensed under a Creative Commons Attribution-Non-Commercial-Share Alike 2.0 UK: England & Wales License. Note that images and other media featured on this page are each governed by their own terms and conditions and they may or may not be available for reuse. Permissions beyond the scope of this license are available here. Based on a work at www.marlin.ac.uk (page left blank) -
Uu.Diva-Portal.Org
http://uu.diva-portal.org This is an author produced version of a paper published in Lethaia (Blackwell Publishing). This paper has been peer-reviewed but does not include the final publisher proof-corrections or journal pagination. Citation for the published paper: Popov, Leonid E.; Bassett, Michael G.; Holmer, Lars E.; Skovsted, Christian B.; Zuykov, Michael A. "Earliest ontogeny of Early Palaeozoic Craniiformea: implications for brachiopod phylogeny" Lethaia, 2010, Vol. 43, Issue 3, pp. 323-333 URL: http://dx.doi.org/10.1111/j.1502-3931.2009.00197.x The definitive version is available at http://wileyonlinelibrary.com. Access to the definitive version may require subscription. 1 Earliest ontogeny of Early Palaeozoic Craniiformea: implications for brachiopod phylogeny LEONID E. POPOV, MICHAEL G. BASSETT, LARS E. HOLMER, CHRISTIAN B. SKOVSTED & MICHAEL ZUYKOV Leonid E. Popov, Michael G. Bassett, Lars E. Holmer, Christian B. Skovsted & Michael Zuykov. 2009 ## ##: Earliest ontogeny of Early Palaeozoic Craniiformea: implications for brachiopod phylogeny. Lethaia, Vol. ##, pp. ###-###. Well preserved specimens of the Early Palaeozoic craniiform brachiopods Orthisocrania and Craniops retain clear evidence of a lecithotrophic larval stage, indicating the loss of planktotrophy early in their phylogeny. The size of the earliest mineralised dorsal shell was less than 100μm across, and the well preserved shell structure in these fossil craniiforms allows their earliest ontogeny to be compared directly with that of living Novocrania, in which the first mineralised dorsal shell (metamorphic shell) is secreted only after settlement of the lecithotrophic larvae. Immediately outside this earliest shell (early post-metamorphic or brephic shell) and in the rest of the dorsal valve the primary layer in both fossil and living craniiforms has characteristic radially arranged laths, which are invariably lacking in the earliest dorsal shell. -
Metamorphosis in Craniiformea Revisited Novocrania Anomala Shows Delayed Development of the Ventral Valve Altenburger, Andreas; Wanninger, Andreas; Holmer, Lars E
Metamorphosis in Craniiformea revisited Novocrania anomala shows delayed development of the ventral valve Altenburger, Andreas; Wanninger, Andreas; Holmer, Lars E. Published in: Zoomorphology DOI: 10.1007/s00435-013-0194-3 Publication date: 2013 Document version Early version, also known as pre-print Citation for published version (APA): Altenburger, A., Wanninger, A., & Holmer, L. E. (2013). Metamorphosis in Craniiformea revisited: Novocrania anomala shows delayed development of the ventral valve. Zoomorphology, 132(4), 379-387. https://doi.org/10.1007/s00435-013-0194-3 Download date: 02. Oct. 2021 *Manuscript Click here to download Manuscript: 130422 Metamorphosis in Novocrania.docx Click here to view linked References 1 Metamorphosis in Craniiformea revisited – Novocrania anomala shows delayed 1 2 development of the ventral valve 3 4 5 6 7 Running title: Metamorphosis in Novocrania 8 9 10 11 12 Andreas Altenburger, Andreas Wanninger, Lars E. Holmer 13 14 15 16 Authors’ names and addresses 17 18 19 Andreas Altenburger, University of Copenhagen, Natural History Museum of 20 21 Denmark – Zoological Museum, Universitetsparken 15, DK-2100 Copenhagen, 22 23 24 Denmark, [email protected], phone: +45 35321114 25 26 Andreas Wanninger, University of Vienna, Dept. of Integrative Zoology, Althanstr. 27 28 29 14, AUT-1090 Vienna, Austria 30 31 Lars E. Holmer, Uppsala University, Department of Earth Sciences, Palaeobiology, 32 33 SE-752 36 Uppsala, Sweden 34 35 36 37 38 Abstract 39 40 41 We revisited the brachiopod fold hypothesis and investigated metamorphosis in the 42 43 craniiform brachiopod Novocrania anomala. Larval development is lecithotrophic 44 45 46 and the dorsal (brachial) valve is secreted by dorsal epithelia. -
Proceedings of the 2Nd Mediterranean Symposium on the Conservation of Dark Habitats
PROCEEDINGS OF THE 2nd MEDITERRANEAN SYMPOSIUM ON THE CONSERVATION OF DARK HABITATS ANTALYA, TURKEY, 16 JANUARY 2019 Technical partner Financial support Legal notice: The designations employed and the presentation of the material in this document do not imply the expression of any opinion whatsoever on the part of the Specially Protected Areas Regional Activity Centre (SPA/RAC) and UN Environment/Mediterranean Action Plan (MAP) concerning the legal status of any State, Territory, city or area, or of its authorities, or concerning the delimitation of their frontiers or boundaries. Copyright: All property rights of texts and content of different types of this publication belong to SPA/RAC. Reproduction of these texts and contents, in whole or in part, and in any form, is prohibited without prior written permission from SPA/RAC, except for educational and other non-commercial purposes, provided that the source is fully acknowledged. © 2018 - United Nations Environment Programme Mediterranean Action Plan Specially Protected Areas Regional Activity Centre (SPA/RAC) Boulevard du Leader Yasser Arafat B.P. 337 1080 Tunis Cedex - Tunisia. E-mail : [email protected] For bibliographic purposes, this document may be cited as: UNEP/MAP – SPA/RAC, 2019. Proceedings of the 2nd Mediterranean Symposium on the conservation of Dark Habitats (Antalya, Turkey, 17 January 2019). LANGAR H., OUERGHI A., edits, SPA/RAC publi., Tunis, 76 p. ISBN 978-9938-9574-6-4 With the financial support of MAVA foundation through the MedKeyHabitats II project. Available at: -
Neuromuscular Development in Novocrania Anomala: Evidence for the Presence of Serotonin and a Spiralian-Like Apical Organ in Lecithotrophic Brachiopod Larvae
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Copenhagen University Research Information System Neuromuscular development in Novocrania anomala: evidence for the presence of serotonin and a spiralian-like apical organ in lecithotrophic brachiopod larvae Altenburger, Andreas; Wanninger, Andreas Wilhelm Georg Published in: Evolution & Development DOI: 10.1111/j.1525-142X.2009.00387.x Publication date: 2010 Document version Early version, also known as pre-print Citation for published version (APA): Altenburger, A., & Wanninger, A. W. G. (2010). Neuromuscular development in Novocrania anomala: evidence for the presence of serotonin and a spiralian-like apical organ in lecithotrophic brachiopod larvae. Evolution & Development, 12(1), 16-24. https://doi.org/10.1111/j.1525-142X.2009.00387.x Download date: 07. apr.. 2020 Neuromuscular development in Novocrania anomala: evidence for the presence of serotonin and a spiralian-like apical organ in lecithotrophic brachiopod larvae Andreas Altenburger, Andreas Wanninger* University of Copenhagen, Deptartment of Biology, Research Group for Comparative Zoology, Universitetsparken 15, DK-2100 Copenhagen Ø, Denmark *corresponding author. E-mail: [email protected] Phone: +45-35321240 Fax: +45-35321200 Running Title: Brachiopod neuromuscular development Word count: 3975 1 ABSTRACT The phylogenetic position of Brachiopoda remains unsettled, and only few recent data on brachiopod organogenesis are currently available. In order to contribute to questions concerning brachiopod ontogeny and evolution we investigated nervous and muscle system development in the craniiform (inarticulate) brachiopod Novocrania anomala. Larvae of this species are lecithotrophic and have a bilobed body with three pairs of dorsal setal bundles which emerge from the posterior lobe. -
Crystallography of Craniid Brachiopods by Electron Backscatter
Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 98, 437–442, 2008 (for 2007) Crystallography of craniid brachiopods by electron backscatter diffraction (EBSD) Alberto Pe´rez-Huerta, Jennifer England and Maggie Cusack Department of Geographical and Earth Sciences, University of Glasgow, Glasgow G12 8QQ, UK E-mail: [email protected] ABSTRACT: Electron backscatter diffraction (EBSD) is used to determine the detailed crystallo- graphic orientation of calcite crystals of craniid brachiopods in the context of shell ultrastructure. Sections of shells of two Recent species, Novocrania anomala and Novocrania huttoni, are analysed to provide 3D crystallographic patterns at high spatial resolution. The c-axis of semi-nacre calcite crystals is oriented parallel to the laminae that define the ultrastructure of the secondary layer. This orientation differs from that of rhynchonelliform calcitic brachiopods where the c-axis is perpen- dicular to the length of morphological fibres and to the shell exterior. KEY WORDS: Brachiopoda, calcite, c-axis, Novocrania anomala, Novocrania huttoni, secondary layer, semi-nacre Williams & Wright (1970) conducted the most comprehensive groups, Craniiformea and Rhynchonelliformea, comprise taxa study in understanding the shell ultrastructure of craniid with calcite shells, but different ultrastructures that may reflect brachiopods. Since the publication of this pioneering work, a dissimilar specific biomineralisation processes. In Craniifor- few studies have dealt with this topic in the analysis of Recent mea, craniid brachiopods consist of shells with an outer species (e.g., Bassett 2000; Logan & Long 2001; Robinson & organic periostracum, a primary layer with acicular calcite and Lee 2007) and of fossil ones (e.g., Smirnova 1997; Halamski an innermost non-fibrous secondary layer of calcite semi-nacre 2004). -
New Records of Recent Brachiopods from the Eastern Mediterranean Sea
ALAN LOGAN, CARLO NIKE BIANCHI, CARLA MORRI, HELMUT ZIBROWIUS & GHAZI BITAR NEW RECORDS OF RECENT BRACHIOPODS FROM THE EASTERN MEDITERRANEAN SEA ESTRATTO dagli ANNALI del MUSEO CIVICO di STORIA NATURALE "G. DORIA' Vol. XCIV - 6 FEBBRAIO 2002 GENOVA ERREDI GRAFICHE EDITORIALI 2002 407 ALAN LOGAN (*), CARLO NIKE BIANCHI (**), CARLA MORRI (**), HELMUT ZIBROWIUS (***) & GHAZI BITAR (****) NEW RECORDS OF RECENT BRACHIOPODS FROM THE EASTERN MEDITERRANEAN SEA INTRODUCTION In a taxonomic guide to the Recent brachiopods of the Mediterra- nean Sea, LOGAN (1979) re-described and re-illustrated 11 species, all of which had been described and illustrated by DAVIDSON (1886-88) and others many years before. Later LOGAN & NOBLE (1983) described and figured six of these species from Malta. Subsequently BRUNTON (1989) identified specimens sent to him from Tel Aviv University and added Neocrania (now Novocrania, see LEE & BRUNTON, 2001) turbinata (Poli) to the list of extant Mediterranean brachiopods, separating this eastern Mediterranean form from the western Mediterranean and eastern Atlantic species Novocrania anomala (Müller). He also recognized Megerlia monstruosa (Scacchi), previously placed in the synonymy of Megerlia truncata (Linnaeus) by LOGAN (1979) and others, as a distinct species, and included M. echinata (Fischer & Oehlert) in its synonymy. In 1994 Logan (in LOGAN & ZIBROWIUS, 1994) described Tethyrhynchia mediterranea, a new species of rhynchonellid, from caves in southern France and Tunisia. Since then Gwynia capsula (Jeffreys), previously known only from the eastern Atlantic (LOGAN et al., 1997), has been identified from the Adriatic Sea by SIMON & WILLEMS (1999). Recently ---------- (*) Centre for Coastal Studies and Aquaculture, University of New Brunswick, Saint John, N.B.