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Recreational Boating As a Major Vector of Spread of Nonindigenous Species Around the Mediterranean Aylin Ulman
Recreational boating as a major vector of spread of nonindigenous species around the Mediterranean Aylin Ulman To cite this version: Aylin Ulman. Recreational boating as a major vector of spread of nonindigenous species around the Mediterranean. Ecosystems. Sorbonne Université, 2018. English. NNT : 2018SORUS222. tel- 02483397 HAL Id: tel-02483397 https://tel.archives-ouvertes.fr/tel-02483397 Submitted on 18 Feb 2020 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. Sorbonne Université Università di Pavia Ecole doctorale CNRS, Laboratoire d'Ecogeochimie des Environments Benthiques, LECOB, F-66650 Banyuls-sur-Mer, France Recreational boating as a major vector of spread of non- indigenous species around the Mediterranean La navigation de plaisance, vecteur majeur de la propagation d’espèces non-indigènes autour des marinas Méditerranéenne Par Aylin Ulman Thèse de doctorat de Philosophie Dirigée par Agnese Marchini et Jean-Marc Guarini Présentée et soutenue publiquement le 6 Avril, 2018 Devant un jury composé de : Anna Occhipinti (President, University -
BIOLOGICAL FEATURES on EPIBIOSIS of Amphibalanus Improvisus (CIRRIPEDIA) on Macrobrachium Acanthurus (DECAPODA)*
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Cadernos Espinosanos (E-Journal) BRAZILIAN JOURNAL OF OCEANOGRAPHY, 58(special issue IV SBO):15-22, 2010 BIOLOGICAL FEATURES ON EPIBIOSIS OF Amphibalanus improvisus (CIRRIPEDIA) ON Macrobrachium acanthurus (DECAPODA)* Cristiane Maria Rocha Farrapeira¹** and Tereza Cristina dos Santos Calado² 1Universidade Federal Rural de Pernambuco – UFRPE Departamento de Biologia (Rua Dom Manoel de Medeiros, s/nº, 52-171-900 Recife, PE, Brasil) 2Universidade Federal de Alagoas – UFAL Laboratório Integrado de Ciências do Mar e Naturais (Rua Aristeu de Andrade, 452, 57051-090 Maceió, AL, Brasil) **[email protected] A B S T R A C T This study aimed to describe the epibiosis of barnacles Amphibalanus improvisus on eight adult Macrobrachium acanthurus males from the Mundaú Lagoon, state of Alagoas, Brazil. The number of epibiont barnacles varied from 247 to 1,544 specimens per prawn; these were distributed predominantly on the cephalothorax and pereiopods, but also on the abdomen and other appendices. Although some were already reproducing, most barnacles had been recruited recently or were still sexually immature; this suggests recent host arrival in that estuarine environment. Despite the fact that other barnacles occur in this region, A. improvisus is the only species reported as an epibiont on Macrobrachium acanthurus; this was also the first record of epibiosis on this host . The occurrence of innumerable specimens in the pereiopods' articulations and the almost complete covering of the carapace of some prawns (which also increased their weight) suggest that A. improvisus is adapted to fixate this kind of biogenic substrate and that the relationship between the two species biologically damages the basibiont. -
Balanus Glandula Class: Multicrustacea, Hexanauplia, Thecostraca, Cirripedia
Phylum: Arthropoda, Crustacea Balanus glandula Class: Multicrustacea, Hexanauplia, Thecostraca, Cirripedia Order: Thoracica, Sessilia, Balanomorpha Acorn barnacle Family: Balanoidea, Balanidae, Balaninae Description (the plate overlapping plate edges) and radii Size: Up to 3 cm in diameter, but usually (the plate edge marked off from the parietes less than 1.5 cm (Ricketts and Calvin 1971; by a definite change in direction of growth Kozloff 1993). lines) (Fig. 3b) (Newman 2007). The plates Color: Shell usually white, often irregular themselves include the carina, the carinola- and color varies with state of erosion. Cirri teral plates and the compound rostrum (Fig. are black and white (see Plate 11, Kozloff 3). 1993). Opercular Valves: Valves consist of General Morphology: Members of the Cirri- two pairs of movable plates inside the wall, pedia, or barnacles, can be recognized by which close the aperture: the tergum and the their feathery thoracic limbs (called cirri) that scutum (Figs. 3a, 4, 5). are used for feeding. There are six pairs of Scuta: The scuta have pits on cirri in B. glandula (Fig. 1). Sessile barna- either side of a short adductor ridge (Fig. 5), cles are surrounded by a shell that is com- fine growth ridges, and a prominent articular posed of a flat basis attached to the sub- ridge. stratum, a wall formed by several articulated Terga: The terga are the upper, plates (six in Balanus species, Fig. 3) and smaller plate pair and each tergum has a movable opercular valves including terga short spur at its base (Fig. 4), deep crests for and scuta (Newman 2007) (Figs. -
Balanus Trigonus
Nauplius ORIGINAL ARTICLE THE JOURNAL OF THE Settlement of the barnacle Balanus trigonus BRAZILIAN CRUSTACEAN SOCIETY Darwin, 1854, on Panulirus gracilis Streets, 1871, in western Mexico e-ISSN 2358-2936 www.scielo.br/nau 1 orcid.org/0000-0001-9187-6080 www.crustacea.org.br Michel E. Hendrickx Evlin Ramírez-Félix2 orcid.org/0000-0002-5136-5283 1 Unidad académica Mazatlán, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México. A.P. 811, Mazatlán, Sinaloa, 82000, Mexico 2 Oficina de INAPESCA Mazatlán, Instituto Nacional de Pesca y Acuacultura. Sábalo- Cerritos s/n., Col. Estero El Yugo, Mazatlán, 82112, Sinaloa, Mexico. ZOOBANK http://zoobank.org/urn:lsid:zoobank.org:pub:74B93F4F-0E5E-4D69- A7F5-5F423DA3762E ABSTRACT A large number of specimens (2765) of the acorn barnacle Balanus trigonus Darwin, 1854, were observed on the spiny lobster Panulirus gracilis Streets, 1871, in western Mexico, including recently settled cypris (1019 individuals or 37%) and encrusted specimens (1746) of different sizes: <1.99 mm, 88%; 1.99 to 2.82 mm, 8%; >2.82 mm, 4%). Cypris settled predominantly on the carapace (67%), mostly on the gastric area (40%), on the left or right orbital areas (35%), on the head appendages, and on the pereiopods 1–3. Encrusting individuals were mostly small (84%); medium-sized specimens accounted for 11% and large for 5%. On the cephalothorax, most were observed in branchial (661) and orbital areas (240). Only 40–41 individuals were found on gastric and cardiac areas. Some individuals (246), mostly small (95%), were observed on the dorsal portion of somites. -
Origin of Chordates Part-I
ORIGIN OF CHORDATES Evolution of chordate was one of the most important event in the history of chordate as it was the beginning of evolution of more advanced chordates like bird and mammals. It is the story of origin from a primitive invertebrate like creatures to early chordates. Though first fossil of the first vertebrate the ostrachoderm was discovered from the Ordovician period but it might have originated in late Cambrian period. As early chordates were soft bodied, their fossil records are not preserved. Hence, to trace their ancestry, we have to find out the similarity among different deuterostomes to trace the origin of chordates. Some structural features shared by them such as bilateral symmetry, antero-posterior body axis, triploblastic coelomate condition, etc., may he because of their common ancestry. TIME OF ORIGIN: Late Cambrian period PLACE OF ORIGIN: Fresh water THEORIES OF INVERTEBRATE ANCESTRY OF CHORDATES Several theories have been put forwarded to explain the origin of chordates either directly from some invertebrate group or through the intervention of some protochordate. Almost every invertebrate phylum—Coelenterata, Nemertean, Phoronida, Annelids, Arthropods and Echinodermatashas been suggested. But these theories are far from being satisfactory and convincing and have only a historical value. Only the echinoderm theory has received some acceptance. DIVISION OF BILATERIA The Bilateria is divided into two major divisions (1) Protostomia and (2) Deuterostornia. This division is based on the differences in embryonic and larval developments. Protostomia includes from Annelida to Arthropoda while deuterostomia includes Echinodermata, Pogonophora and Chordate. DEUTEROSTOME LINE OF CHORDATE EVOLUTION Following common features of all Deuterostomes suggests strong evidence of a closer evolutionary relationship between the three principal deuterostome phyla – Echinodermata, Hemichordata and Chordata. -
The Barnacle Amphibalanus Improvisus (Darwin, 1854), and the Mitten Crab Eriocheir: One Invasive Species Getting Off on Another!
BioInvasions Records (2015) Volume 4, Issue 3: 205–209 Open Access doi: http://dx.doi.org/10.3391/bir.2015.4.3.09 © 2015 The Author(s). Journal compilation © 2015 REABIC Rapid Communication The barnacle Amphibalanus improvisus (Darwin, 1854), and the mitten crab Eriocheir: one invasive species getting off on another! Murtada D. Naser1,4, Philip S. Rainbow2, Paul F. Clark2*, Amaal Gh. Yasser1,4 and Diana S. Jones3 1Marine Biology Department, Marine Science Centre, University of Basrah, Basrah, Iraq 2Department of Life Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, England 3Western Australian Museum, 49 Kew Street, Welshpool, Western Australia, 6106 Australia 4Australian Rivers Institute, Griffith University, 170 Kessels Road, Nathan, Queensland, 4111 Australia E-mail: [email protected] (MDN), [email protected] (PSR), [email protected] (PFC), [email protected] (AGY), [email protected] (DSJ) *Corresponding author Received: 9 March 2015 / Accepted: 20 May 2015 / Published online: 16 June 2015 Handling editor: Vadim Panov Abstract The balanoid barnacle, Amphibalanus improvisus (Darwin, 1854), was found on the carapaces of two invasive species of mitten crabs: Eriocheir sinensis H. Milne Edwards, 1853 and E. hepuensis Dai, 1991. The first instance was from a female mitten crab captured from the River Thames estuary, Kent, England, where A. improvisus is common. However, the second record, on a Hepu mitten crab from Iraq is the first record of A. improvisus from the Persian Gulf. Key words: Eriocheir sinensis H. Milne Edwards, 1853, E. hepuensis Dai, 1991, invasive species, England, Iraq, barnacles, mitten crabs Introduction the eastern and western North Atlantic; Baltic Sea; west coast of Africa (to the Cape of Good “Hairy” (Southeast and East Asia) or “mitten” Hope); Mediterranean Sea; Black Sea; Caspian (Europe) crabs are currently assigned to Eriocheir Sea; Red Sea; Straits of Malacca; Singapore; De Haan, 1835 (Brachyura: Grapsoidea: Varunidae). -
Copper Tolerance of Amphibalanus Amphitrite As Observed in Central Florida
Copper Tolerance of Amphibalanus amphitrite as Observed in Central Florida by Hannah Grace Brinson Bachelor of Science Oceanography Florida Institute of Technology 2015 A thesis submitted to Department of Ocean Engineering and Sciences at Florida Institute of Technology in partial fulfillment of the requirements for the degree of: Master of Science in Biological Oceanography Melbourne, Florida December 2017 We the undersigned committee hereby approve the attached thesis, “Copper Tolerance of Amphibalanus amphitrite as observed in Central Florida,” by Hannah Grace Brinson. ________________________________ Emily Ralston, Ph.D. Research Assistant Professor of Ocean Engineering and Sciences; Department of Ocean Engineering and Sciences Major Advisor ________________________________ Geoffrey Swain, Ph.D. Professor of Oceanography and Ocean Engineering; Department of Ocean Engineering and Sciences ________________________________ Kevin B. Johnson, Ph.D. Chair of Ocean Sciences; Professor of Oceanography and Environmental Sciences; Department of Ocean Engineering and Sciences ________________________________ Richard Aronson, Ph.D. Department Head and Professor of Biological Sciences; Department of Biological Sciences ________________________________ Dr. Marco Carvalho Dean of College of Engineering and Computing Abstract Copper Tolerance of Amphibalanus amphitrite as observed in Central Florida by Hannah Grace Brinson Major Advisor: Emily Ralston, Ph.D. Copper tolerance in the invasive barnacle Amphibalanus amphitrite has been observed in Florida -
Year 2 Report
NORTH PACIFIC MARINE SCIENCE ORGANIZATION (PICES) PROJECT ON “EFFECTS OF MARINE DEBRIS CAUSED BY THE GREAT TSUNAMI OF 2011” Year 2 Final Report 1. PROJECT INFORMATION Title: PICES Tohoku coast field survey (fouling plate) – supplemental study for U.S. tsunami debris spp. list Award period July 15, 2015 – March 31, 2016 Amount of funding $ 68,965 CAD Report submission date December 12, 2015 Lead Author of Report* Hisatsugu Kato (JANUS), Michio Otani, Karin Baba (JANUS) Principal Investigator(s), Co-Principal Investigators and Recipient Organization(s): Dr. Hisatsugu Kato Karin Baba Japan NUS Co., LTD. Nishi-Shinjuku Kimuraya Building 5F, 7-5-25 Nishi-Shinjuku, Shinjuku-Ku, Tokyo 160-0023, Japan Phone: (81)-3-5925-6866 (direct) Email: [email protected] Dr. Michio Otani Rokujo Midori-machi 3-9-10, Nara City, Japan, 630-8045 Tel & Fax: 81-742-48-8552 2. EXECUTIVE SUMMARY Introduction During the Great East Japan Earthquake and tsunami in 2011, vast amount of debris got washed out from land and some became Japanese Tsunami Marine Debris (JTMD) and reached Hawaii and west coast of the U.S. and Canada with many coastal fouling organisms attached. It is uncertain amount and species of fouling organisms which were transferred from Japan to the U.S. and Canada. This research is the survey which is aimed to obtain a thorough collection of fouling organisms to morphologically and genetically complement the existing collection of JTMD species in Japan. 1 Materials and method The survey was conducted at several locations in the Tohoku coast. Fouling plates of 14 cm square were placed in 3 different locations; Miyako (Iwate prefecture), Kesennuma and Matsushima (Miyagi prefecture) in July or August, 2015 (Figure 1). -
ON the ECOLOGY of DEROCHEILOCARIS REMANEI DELAMARE and CHAPPUIS (CRUSTACEA, MYSTACOCARIDA) Bengt-Owe Jansson
ON THE ECOLOGY OF DEROCHEILOCARIS REMANEI DELAMARE AND CHAPPUIS (CRUSTACEA, MYSTACOCARIDA) Bengt-Owe Jansson To cite this version: Bengt-Owe Jansson. ON THE ECOLOGY OF DEROCHEILOCARIS REMANEI DELAMARE AND CHAPPUIS (CRUSTACEA, MYSTACOCARIDA). Vie et Milieu , Observatoire Océanologique - Lab- oratoire Arago, 1966, pp.143-186. hal-02946026 HAL Id: hal-02946026 https://hal.sorbonne-universite.fr/hal-02946026 Submitted on 22 Sep 2020 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. ON THE ECOLOGY OF DEROCHEILOCARIS REMANEI DELAMARE AND CHAPPUIS (CRUSTACEA, MYSTACOCARIDA) by Bengt-Owe JANSSON Askô Laboratory, Department of Zoology, University of Stockholm ABSTRACT The horizontal and vertical distribution of D. remanei has been investigated during April 1962 and May 1964 at Canet-Plage. The chief ecological factors have been studied, and tolérance and préférence experiments have been conducted. For this localy, salinity, température and turbulence are the chief parameters governing the distribution of D. remanei. INTRODUCTION Most of our présent knowledge of Mystacocarida is summarized by DELAMARE DEBOUTTEVILLE (1960). While two of the three hitherto known species — Derocheilocaris typicus Pennak & Zinn and D. remanei have been found in the littoral subsoil water the third, D. -
Remarkable Convergent Evolution in Specialized Parasitic Thecostraca (Crustacea)
Remarkable convergent evolution in specialized parasitic Thecostraca (Crustacea) Pérez-Losada, Marcos; Høeg, Jens Thorvald; Crandall, Keith A Published in: BMC Biology DOI: 10.1186/1741-7007-7-15 Publication date: 2009 Document version Publisher's PDF, also known as Version of record Citation for published version (APA): Pérez-Losada, M., Høeg, J. T., & Crandall, K. A. (2009). Remarkable convergent evolution in specialized parasitic Thecostraca (Crustacea). BMC Biology, 7(15), 1-12. https://doi.org/10.1186/1741-7007-7-15 Download date: 25. Sep. 2021 BMC Biology BioMed Central Research article Open Access Remarkable convergent evolution in specialized parasitic Thecostraca (Crustacea) Marcos Pérez-Losada*1, JensTHøeg2 and Keith A Crandall3 Address: 1CIBIO, Centro de Investigação em Biodiversidade e Recursos Genéticos, Universidade do Porto, Campus Agrário de Vairão, Portugal, 2Comparative Zoology, Department of Biology, University of Copenhagen, Copenhagen, Denmark and 3Department of Biology and Monte L Bean Life Science Museum, Brigham Young University, Provo, Utah, USA Email: Marcos Pérez-Losada* - [email protected]; Jens T Høeg - [email protected]; Keith A Crandall - [email protected] * Corresponding author Published: 17 April 2009 Received: 10 December 2008 Accepted: 17 April 2009 BMC Biology 2009, 7:15 doi:10.1186/1741-7007-7-15 This article is available from: http://www.biomedcentral.com/1741-7007/7/15 © 2009 Pérez-Losada et al; licensee BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. -
A Possible 150 Million Years Old Cirripede Crustacean Nauplius and the Phenomenon of Giant Larvae
Contributions to Zoology, 86 (3) 213-227 (2017) A possible 150 million years old cirripede crustacean nauplius and the phenomenon of giant larvae Christina Nagler1, 4, Jens T. Høeg2, Carolin Haug1, 3, Joachim T. Haug1, 3 1 Department of Biology, Ludwig-Maximilians-Universität München, Großhaderner Straße 2, 82152 Planegg- Martinsried, Germany 2 Department of Biology, University of Copenhagen, Universitetsparken 15, 2100 Copenhagen, Denmark 3 GeoBio-Center, Ludwig-Maximilians-Universität München, Richard-Wagner-Straße 10, 80333 Munich, Germany 4 E-mail: [email protected] Key words: nauplius, metamorphosis, palaeo-evo-devo, Cirripedia, Solnhofen lithographic limestones Abstract The possible function of giant larvae ................................ 222 Interpretation of the present case ....................................... 223 The larval phase of metazoans can be interpreted as a discrete Acknowledgements ....................................................................... 223 post-embryonic period. Larvae have been usually considered to References ...................................................................................... 223 be small, yet some metazoans possess unusually large larvae, or giant larvae. Here, we report a possible case of such a giant larva from the Upper Jurassic Solnhofen Lithographic limestones (150 Introduction million years old, southern Germany), most likely representing an immature cirripede crustacean (barnacles and their relatives). The single specimen was documented with up-to-date -
Articles (Newman and Unger, 2003; Rainbow, 1995; Cumulation in Shells
Biogeosciences, 18, 707–728, 2021 https://doi.org/10.5194/bg-18-707-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. The patterns of elemental concentration (Ca, Na, Sr, Mg, Mn, Ba, Cu, Pb, V, Y, U and Cd) in shells of invertebrates representing different CaCO3 polymorphs: a case study from the brackish Gulf of Gdansk´ (the Baltic Sea) Anna Piwoni-Piórewicz1, Stanislav Strekopytov2,a, Emma Humphreys-Williams2, and Piotr Kuklinski´ 1,3 1Institute of Oceanology, Polish Academy of Sciences, Sopot, 81-712, Poland 2Imaging and Analysis Centre, Natural History Museum, London, SW7 5BD, United Kingdom 3Department of Life Sciences, Natural History Museum, London, SW7 5BD, United Kingdom acurrent address: National Measurement Laboratory, LGC Limited, Teddington, TW11 0LY, United Kingdom Correspondence: Anna Piwoni-Piórewicz ([email protected]) Received: 10 September 2019 – Discussion started: 20 September 2019 Revised: 6 November 2020 – Accepted: 9 December 2020 – Published: 29 January 2021 Abstract. The shells of calcitic arthropod Amphibalanus 1 Introduction improvisus; aragonitic bivalves Cerastoderma glaucum, Limecola balthica, and Mya arenaria; and bimineralic bi- Marine invertebrates such as molluscs, brachiopods, corals, valve Mytilus trossulus were collected in the brackish waters echinoderms, bryozoans and some groups of protozoa of the southern Baltic Sea in order to study patterns of bulk (foraminifera) are able to form skeletons built of calcium car- elemental concentration (Ca, Na, Sr, Mg, Ba, Mn, Cu, Pb, V, bonate. The combination of inorganic CaCO3 crystals and or- Y, U and Cd) in shells composed of different crystal lattices ganic compounds with a characteristic and ordered structure, (calcite and aragonite).