Chapter 10. Species Recorded from Fouling
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Appendix to Taxonomic Revision of Leopold and Rudolf Blaschkas' Glass Models of Invertebrates 1888 Catalogue, with Correction
http://www.natsca.org Journal of Natural Science Collections Title: Appendix to Taxonomic revision of Leopold and Rudolf Blaschkas’ Glass Models of Invertebrates 1888 Catalogue, with correction of authorities Author(s): Callaghan, E., Egger, B., Doyle, H., & E. G. Reynaud Source: Callaghan, E., Egger, B., Doyle, H., & E. G. Reynaud. (2020). Appendix to Taxonomic revision of Leopold and Rudolf Blaschkas’ Glass Models of Invertebrates 1888 Catalogue, with correction of authorities. Journal of Natural Science Collections, Volume 7, . URL: http://www.natsca.org/article/2587 NatSCA supports open access publication as part of its mission is to promote and support natural science collections. NatSCA uses the Creative Commons Attribution License (CCAL) http://creativecommons.org/licenses/by/2.5/ for all works we publish. Under CCAL authors retain ownership of the copyright for their article, but authors allow anyone to download, reuse, reprint, modify, distribute, and/or copy articles in NatSCA publications, so long as the original authors and source are cited. TABLE 3 – Callaghan et al. WARD AUTHORITY TAXONOMY ORIGINAL SPECIES NAME REVISED SPECIES NAME REVISED AUTHORITY N° (Ward Catalogue 1888) Coelenterata Anthozoa Alcyonaria 1 Alcyonium digitatum Linnaeus, 1758 2 Alcyonium palmatum Pallas, 1766 3 Alcyonium stellatum Milne-Edwards [?] Sarcophyton stellatum Kükenthal, 1910 4 Anthelia glauca Savigny Lamarck, 1816 5 Corallium rubrum Lamarck Linnaeus, 1758 6 Gorgonia verrucosa Pallas, 1766 [?] Eunicella verrucosa 7 Kophobelemon (Umbellularia) stelliferum -
The Chiton Radula: a Unique Model for Biomineralization Studies
4 The Chiton Radula: A Unique Model for Biomineralization Studies Lesley R. Brooker1 and Jeremy A. Shaw2 1University of the Sunshine Coast 2Centre for Microscopy, Characterisation & Analysis University of Western Australia Australia 1. Introduction Over the course of evolution, a range of strategies have been developed by different organisms to produce unique materials and structures perfected for their specific function. This biological mastery of materials production has inspired the birth of the new discipline of biomaterials through biomimicry (Birchall, 1989). Chitons (Mollusca: Polyplacophora) are slow moving, bilaterally symmetrical and dorso- ventrally flattened molluscs that are commonly found on hard substrata in intertidal regions of coastlines around the world (Kaas & Jones, 1998). All species are characterized by a series of eight dorsal, articulating shell plates or valves, which may be embedded, to varying degrees, in a fleshy, muscular girdle (Kaas & Jones, 1998) (Figure 1). Approximately 750 living species are known, and while intertidal regions are home to the majority of chitons, a number of species can be found at depths of up to 8000m where they feed on detrital material (Kaas & Jones, 1998). Fig. 1. Photograph of the dorsal surface of the chiton Acanthopleura gaimardi, showing the eight overlapping aragonite plates surrounded by the fleshy girdle, which, in this species, is covered in small aragonite spines. Chitons feed by rasping macro- and micro-algae from the rocks on which they live through the use of a radula. The radula has been coined as a conveyor belt of continuously developing www.intechopen.com 66 Advanced Topics in Biomineralization teeth, replaced by new teeth as they are worn and lost. -
RED ALGAE · RHODOPHYTA Rhodophyta Are Cosmopolitan, Found from the Artic to the Tropics
RED ALGAE · RHODOPHYTA Rhodophyta are cosmopolitan, found from the artic to the tropics. Although they grow in both marine and fresh water, 98% of the 6,500 species of red algae are marine. Most of these species occur in the tropics and sub-tropics, though the greatest number of species is temperate. Along the California coast, the species of red algae far outnumber the species of green and brown algae. In temperate regions such as California, red algae are common in the intertidal zone. In the tropics, however, they are mostly subtidal, growing as epiphytes on seagrasses, within the crevices of rock and coral reefs, or occasionally on dead coral or sand. In some tropical waters, red algae can be found as deep as 200 meters. Because of their unique accessory pigments (phycobiliproteins), the red algae are able to harvest the blue light that reaches deeper waters. Red algae are important economically in many parts of the world. For example, in Japan, the cultivation of Pyropia is a multibillion-dollar industry, used for nori and other algal products. Rhodophyta also provide valuable “gums” or colloidal agents for industrial and food applications. Two extremely important phycocolloids are agar (and the derivative agarose) and carrageenan. The Rhodophyta are the only algae which have “pit plugs” between cells in multicellular thalli. Though their true function is debated, pit plugs are thought to provide stability to the thallus. Also, the red algae are unique in that they have no flagellated stages, which enhance reproduction in other algae. Instead, red algae has a complex life cycle, with three distinct stages. -
SNH Commissioned Report 765: Seagrass (Zostera) Beds in Orkney
Scottish Natural Heritage Commissioned Report No. 765 Seagrass (Zostera) beds in Orkney COMMISSIONED REPORT Commissioned Report No. 765 Seagrass (Zostera) beds in Orkney For further information on this report please contact: Kate Thompson Scottish Natural Heritage 54-56 Junction Road KIRKWALL Orkney KW15 1AW Telephone: 01856 875302 E-mail: [email protected] This report should be quoted as: Thomson, M. and Jackson, E, with Kakkonen, J. 2014. Seagrass (Zostera) beds in Orkney. Scottish Natural Heritage Commissioned Report No. 765. This report, or any part of it, should not be reproduced without the permission of Scottish Natural Heritage. This permission will not be withheld unreasonably. The views expressed by the author(s) of this report should not be taken as the views and policies of Scottish Natural Heritage. © Scottish Natural Heritage 2014. COMMISSIONED REPORT Summary Seagrass (Zostera) beds in Orkney Commissioned Report No. 765 Project No: 848 Contractors: Emma Jackson (The Marine Biological Association of the United Kingdom) and Malcolm Thomson (Sula Diving) Year of publication: 2014 Keywords Seagrass; Zostera marina; Orkney; predictive model; survey. Background Seagrasses (Zostera spp) are marine flowering plants that develop on sands and muds in sheltered intertidal and shallow subtidal areas. Seagrass beds are important marine habitats but are vulnerable to a range of human induced pressures. Their vulnerability and importance to habitat creation and ecological functioning is recognised in their inclusion on the recommended Priority Marine Features list for Scotland’s seas. Prior to this study, there were few confirmed records of Zostera in Orkney waters. This study combined a predictive modelling approach with boat-based surveys to enhance under- standing of seagrass distribution in Orkney and inform conservation management. -
(Cirripedia : Thoracica) Over the Body of a Sea Snake, Laticauda Title Semifasciata (Reinwardt), from the Kii Peninsula, Southwestern Japan
Distribution of Two Species of Conchoderma (Cirripedia : Thoracica) over the Body of a Sea Snake, Laticauda Title semifasciata (Reinwardt), from the Kii Peninsula, Southwestern Japan Yamato, Shigeyuki; Yusa, Yoichi; Tanase, Hidetomo; Tanase, Author(s) Hidetomo PUBLICATIONS OF THE SETO MARINE BIOLOGICAL Citation LABORATORY (1996), 37(3-6): 337-343 Issue Date 1996-12-25 URL http://hdl.handle.net/2433/176259 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University Pub!. Seto Mar. Bioi. Lab., 37(3/6): 337-343, 1996 337 Distribution of Two Species of Conchoderma (Cirripedia: Thoracica) over the Body of a Sea Snake, Laticauda semifasciata (Reinwardt), from the Kii Peninsula, Southwestern Japan SHIGEYUKI YAMATO, YOICHI YUSA and HIDETOMO TANASE Seto Marine Biological Laboratory, Kyoto University, Shirahama, Wakayama 649-22, Japan Abstract Two species of Conchoderma were found on a sea snake, Laticauda semifas ciata (Reinwardt), collected on the west coast of the Kii Peninsula. A total of 223 individuals of C. virgatum and 6 of C. hunteri in 19 clumps were attached to the snake's body. The barnacles ranged in size from 1.4 mm (cypris larvae) to 18.2 mm in capitulum length in C. virgatum, and from 10.7 to 14.4 mm in C. hunteri. The size of the smallest gravid individuals in both species was between 10 and 11 mm. The distribution of C. virgatum on the snake was non-random both longitudinally and dorso-ventrally, with more barnacles in the posterior region and on the ventral side of the snake, respectively. The proportion of gravid individuals increased towards the tail. -
Bulletin of the British Museum (Natural History)
Charixa Lang and Spinicharixa gen. nov., cheilostome bryozoans from the Lower Cretaceous P. D. Taylor Department of Palaeontology, British Museum (Natural History), Cromwell Road, London SW7 5BD Synopsis Seven species of non-ovicellate anascans with pluriserial to loosely multiserial colonies are described from the Barremian-Albian of Europe and Africa. The genus Charixa Lang is revised and the following species assigned: C. vennensis Lang from the U. Albian Cowstones of Dorset, C. Ihuydi (Pitt) from the U. Aptian Faringdon Sponge Gravel of Oxfordshire, C. cryptocauda sp. nov. from the Albian Mzinene Fm. of Zululand, C. lindiensis sp. nov. from the Aptian of Tanzania, and C.I sp. from the Barremian Makatini Fm. of Zululand. Spinicharixa gen. nov. is introduced for Charixa-\ike species with multiple spine bases. Two species are described: S. pitti sp. nov., the type species, probably from the Urgoniana Fm. (?Aptian) of Spain, and S. dimorpha from the M.-U. Albian Gault Clay of Kent. All previous records of L. Cretaceous cheilostomes are reviewed. Although attaining a wide geographical distribution, cheilostomes remained uncommon, morphologically conservative and of low species diversity until late Albian-early Cenomanian times. Introduction An outstanding event in the fossil history of the Bryozoa is the appearance, radiation and dominance achieved by the Cheilostomata during the latter part of the Mesozoic. Aspects of et al. this event have been discussed by several authors (e.g. Cheetham & Cook in Boardman 1983; Larwood 1979; Larwood & Taylor 1981; Schopf 1977; Taylor 1981o; Voigt 1981). Comparative morphology provides strong evidence for regarding living cheilostomes as the sister group of living ctenostome bryozoans (Cheetham & Cook in Boardman et al. -
Bryozoan Genera Fenestrulina and Microporella No Longer Confamilial; Multi-Gene Phylogeny Supports Separation
Zoological Journal of the Linnean Society, 2019, 186, 190–199. With 2 figures. Bryozoan genera Fenestrulina and Microporella no longer confamilial; multi-gene phylogeny supports separation RUSSELL J. S. ORR1*, ANDREA WAESCHENBACH2, EMILY L. G. ENEVOLDSEN3, Downloaded from https://academic.oup.com/zoolinnean/article/186/1/190/5096936 by guest on 29 September 2021 JEROEN P. BOEVE3, MARIANNE N. HAUGEN3, KJETIL L. VOJE3, JOANNE PORTER4, KAMIL ZÁGORŠEK5, ABIGAIL M. SMITH6, DENNIS P. GORDON7 and LEE HSIANG LIOW1,3 1Natural History Museum, University of Oslo, Oslo, Norway 2Department of Life Sciences, Natural History Museum, London, UK 3Centre for Ecological & Evolutionary Synthesis, Department of Biosciences, University of Oslo, Oslo, Norway 4Centre for Marine Biodiversity and Biotechnology, School of Life Sciences, Heriot Watt University, Edinburgh, UK 5Department of Geography, Technical University of Liberec, Czech Republic 6Department of Marine Science, University of Otago, Dunedin, New Zealand 7National Institute of Water and Atmospheric Research, Wellington, New Zealand Received 25 March 2018; revised 28 June 2018; accepted for publication 11 July 2018 Bryozoans are a moderately diverse, mostly marine phylum with a fossil record extending to the Early Ordovician. Compared to other phyla, little is known about their phylogenetic relationships at both lower and higher taxonomic levels. Hence, an effort is being made to elucidate their phylogenetic relationships. Here, we present newly sequenced nuclear and mitochondrial genes for 21 cheilostome bryozoans. Combining these data with existing orthologous molecular data, we focus on reconstructing the phylogenetic relationships of Fenestrulina and Microporella, two species-rich genera. They are currently placed in Microporellidae, defined by having a semicircular primary orifice and a proximal ascopore. -
Epibiotic Associates of Oceanic-Stage Loggerhead Turtles from the Southeastern North Atlantic
Acknowledgements We thank the biology students of the occasional leatherback nests in Brazil. Marine Turtle Federal University of Paraíba (Pablo Riul, Robson G. dos Newsletter 96:13-16. Santos, André S. dos Santos, Ana C. G. P. Falcão, Stenphenson Abrantes, MS Elaine Elloy), the marathon MARCOVALDI, M. Â. & G. G. MARCOVALDI. 1999. Marine runner José A. Nóbrega, and the journalist Germana turtles of Brazil: the history and structure of Projeto Bronzeado for the volunteer field work; the Fauna department TAMAR-IBAMA. Biological Conservation 91:35-41. of IBAMA/PB and Jeremy and Diana Jeffers for kindly MARCOVALDI, M.Â., C.F. VIEITAS & M.H. GODFREY. 1999. providing photos, and also Alice Grossman for providing Nesting and conservation management of hawksbill turtles the TAMAR protocols. The manuscript benefited from the (Eretmochelys imbricata) in northern Bahia, Brazil. comments of two referees. Chelonian Conservation and Biology 3:301-307. BARATA, P.C.R. & F.F.C. FABIANO. 2002. Evidence for SAMPAIO, C.L.S. 1999. Dermochelys coriacea (Leatherback leatherback sea turtle (Dermochelys coriacea) nesting in sea turtle), accidental capture. Herpetological Review Arraial do Cabo, state of Rio de Janeiro, and a review of 30:38-39. Epibiotic Associates of Oceanic-Stage Loggerhead Turtles from the Southeastern North Atlantic Michael G. Frick1, Arnold Ross2, Kristina L. Williams1, Alan B. Bolten3, Karen A. Bjorndal3 & Helen R. Martins4 1 Caretta Research Project, P.O. Box 9841, Savannah, Georgia 31412 USA. (E-mail: [email protected]) 2 Scripps Institution of Oceanography, Marine Biology Research Division, La Jolla, California 92093-0202, USA, (E-mail: [email protected]) 3 Archie Carr Center for Sea Turtle Research and Department of Zoology, University of Florida, P.O. -
Chitons (Mollusca: Polyplacophora) Known from Benthic Monitoring Programs in the Southern California Bight
ISSN 0738-9388 THE FESTIVUS A publication of the San Diego Shell Club Volume XLI Special Issue June 11, 2009 Chitons (Mollusca: Polyplacophora) Known from Benthic Monitoring Programs in the Southern California Bight Timothy D. Stebbins and Douglas J. Eernisse COVER PHOTO Live specimen of Lepidozona sp. C occurring on a piece of metal debris collected off San Diego, southern California at a depth of 90 m. Photo provided courtesy of R. Rowe. Vol. XLI(6): 2009 THE FESTIVUS Page 53 CHITONS (MOLLUSCA: POLYPLACOPHORA) KNOWN FROM BENTHIC MONITORING PROGRAMS IN THE SOUTHERN CALIFORNIA BIGHT TIMOTHY D. STEBBINS 1,* and DOUGLAS J. EERNISSE 2 1 City of San Diego Marine Biology Laboratory, Metropolitan Wastewater Department, San Diego, CA, USA 2 Department of Biological Science, California State University, Fullerton, CA, USA Abstract: About 36 species of chitons possibly occur at depths greater than 30 m along the continental shelf and slope of the Southern California Bight (SCB), although little is known about their distribution or ecology. Nineteen species are reported here based on chitons collected as part of long-term, local benthic monitoring programs or less frequent region-wide surveys of the entire SCB, and these show little overlap with species that occur at depths typically encountered by scuba divers. Most chitons were collected between 30-305 m depths, although records are included for a few from slightly shallower waters. Of the two extant chiton lineages, Lepidopleurida is represented by Leptochitonidae (2 genera, 3 species), while Chitonida is represented by Ischnochitonidae (2 genera, 6-9 species) and Mopaliidae (4 genera, 7 species). -
Chiton (Chiton) Articulatus (MOLLUSCA: POLYPLACOPHORA) DE LA COSTA ROCOSA DE PUERTO ÁNGEL, OAXACA, MÉXICO
INSTITUTO POLITECNICO NACIONAL CENTRO INTERDISCIPLINARIO DE CIENCIAS MARINAS MADURACIÓN GONÁDICA, CICLO REPRODUCTIVO Y TALLA DE MADUREZ SEXUAL DEL QUITÓN Chiton (Chiton) articulatus (MOLLUSCA: POLYPLACOPHORA) DE LA COSTA ROCOSA DE PUERTO ÁNGEL, OAXACA, MÉXICO TESIS QUE PARA OBTENER EL GRADO DE MAESTRÍA EN CIENCIAS EN MANEJO DE RECURSOS MARINOS PRESENTA QUETZALLI YASU ABADIA CHANONA LA PAZ, B.C.S., JULIO 2015 SIP-14 BIS INSTITUTO POLITÉCNICO NACIONAL SECRETARIA DE INVESTIGACIÓN Y POSGRADO ACTA DE REVISIÓN DE TESIS En la Ciudad de La Paz, B.CS,, siendo las i2:Q0 horas del día 18 del mes de Junio del 2015 se reunieron los miembros de la Comisión Revisora de Tesis designada por el Colegio de Profesores de Estudios de Posgrado e Investigación de CICIMAR para examinar la tesis titulada: "MADURACIÓN GONÁDICA, CICLO REPRODUCTIVO Y TALLA DE MADUREZ SEXUAL DEL QUITÓN Chiton (Chkorí) articulatus (Mollusca: Polyplacophora) DE LA COSTA ROCOSA DE PUERTO ÁNGEL, OAXACA, MÉXICO" Presentada por el alumno: ABADÍA CHANONA QUETZALLI YASU Apellido paterno materno nombre(s2 B 1 3 0 8 4 9 Con registro: Aspirante de: MAESTRÍA EN CIENCIAS EN MANEJO DE RECURSOS MARINOS Después de intercambiar opiniones los miembros de la Comisión manifestaron APROBAR LA DEFENSA DELA TESIS, en virtud de que satisface los requisitos señalados por las disposiciones reglamentarias vigentes. &BRIEL MORENO SANCHEZ INSTITUTO POLITÉCNICO NACIONAL SECRETAíRÍA DE INVESTIGACIÓN Y POSGRADO CARTA CESIÓN DE DERECHOS En la Ciudad de La Paz, B.C.S., el día 22 del mes lunio del año 2015 el (la) que suscribe BM. QUETZALLIYASÚABA alumno(a) del Programa de MAESTRÍA EN CIENCIAS EN MANEJO DE RECURSOS MARINOS con número de registro B130849 adscrito al CENTRO INTERDISCIPLINARIO DE CIENCIAS MARINAS manifiesta que es autor (a) intelectual del presente trabajo de tesis, bajo la dirección de: DR. -
The Timescale of Early Land Plant Evolution PNAS PLUS
The timescale of early land plant evolution PNAS PLUS Jennifer L. Morrisa,1, Mark N. Putticka,b,1, James W. Clarka, Dianne Edwardsc, Paul Kenrickb, Silvia Presseld, Charles H. Wellmane, Ziheng Yangf,g, Harald Schneidera,d,h,2, and Philip C. J. Donoghuea,2 aSchool of Earth Sciences, University of Bristol, Bristol BS8 1TQ, United Kingdom; bDepartment of Earth Sciences, Natural History Museum, London SW7 5BD, United Kingdom; cSchool of Earth and Ocean Sciences, Cardiff University, Cardiff CF10, United Kingdom; dDepartment of Life Sciences, Natural History Museum, London SW7 5BD, United Kingdom; eDepartment of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, United Kingdom; fDepartment of Genetics, Evolution and Environment, University College London, London WC1E 6BT, United Kingdom; gRadclie Institute for Advanced Studies, Harvard University, Cambridge, MA 02138; and hCenter of Integrative Conservation, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Yunnan 666303, China Edited by Peter R. Crane, Oak Spring Garden Foundation, Upperville, VA, and approved January 17, 2018 (received for review November 10, 2017) Establishing the timescale of early land plant evolution is essential recourse but to molecular clock methodology, employing the for testing hypotheses on the coevolution of land plants and known fossil record to calibrate and constrain molecular evolu- Earth’s System. The sparseness of early land plant megafossils and tion to time. Unfortunately, the relationships among the four stratigraphic controls on their distribution make the fossil record principal lineages of land plants, namely, hornworts, liverworts, an unreliable guide, leaving only the molecular clock. However, mosses, and tracheophytes, are unresolved, with almost every the application of molecular clock methodology is challenged by possible solution currently considered viable (14). -
Redalyc.Lista Sistemática De Los Moluscos Marinos Y Estuarinos Del
Comunicaciones de la Sociedad Malacológica del Uruguay ISSN: 0037-8607 [email protected] Sociedad Malacológica del Uruguay Uruguay Clavijo, Cristhian; Scarabino, Fabrizio; Rojas, Alejandra; Martínez, Sergio Lista sistemática de los moluscos marinos y estuarinos del cuaternario de Uruguay Comunicaciones de la Sociedad Malacológica del Uruguay, vol. 9, núm. 88, 2005, pp. 381-411 Sociedad Malacológica del Uruguay Montevideo, Uruguay Disponible en: http://www.redalyc.org/articulo.oa?id=52408804 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Comunicaciones de la Sociedad Malacológica del Uruguay ISSN 0037- 8607 9 (88): 381 – 411. 2005 LISTA SISTEMÁTICA DE LOS MOLUSCOS MARINOS Y ESTUARINOS DEL CUATERNARIO DE URUGUAY Cristhian Clavijo § , Fabrizio Scarabino § , Alejandra Rojas * & Sergio Martínez * R ESUMEN Hasta el momento han sido citadas 142 especies de moluscos marinos y estuarinos para el Cuaternario de Uruguay. Esta fauna está compuesta taxonómicamente de la siguiente forma: Polyplacophora (2 especies), Scaphopoda (1), Gastropoda (66) y Bivalvia (73). PALABRAS CLAVE: Holoceno, Pleistoceno, Polyplacophora, Scaphopoda, Gastropoda, Bivalvia, Atlántico Sudoccidental. A BSTRACT Systematic list of the marine and estuarine molluscs from the Quaternary of Uruguay. Until now 142 species of marine and estuarine molluscs have been recorded from the Quaternary of Uruguay. This fauna is taxonomically composed as follows: Polyplacophora (2 species), Scaphopoda (1), Gastropoda (66) and Bivalvia (73). KEY WORDS: Holocene, Pleistocene, Polyplacophora, Scaphopoda, Gastropoda, Bivalvia, Southwestern Atlantic. INTRODUCCIÓN pobremente estudiados, constituyendo un particular ejemplo de los desafíos a superar.