Bryozoan Schizoporella Errata: the Influence of Hydrodynamics and Associated Biota
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Bryozoan Studies 2019
BRYOZOAN STUDIES 2019 Edited by Patrick Wyse Jackson & Kamil Zágoršek Czech Geological Survey 1 BRYOZOAN STUDIES 2019 2 Dedication This volume is dedicated with deep gratitude to Paul Taylor. Throughout his career Paul has worked at the Natural History Museum, London which he joined soon after completing post-doctoral studies in Swansea which in turn followed his completion of a PhD in Durham. Paul’s research interests are polymatic within the sphere of bryozoology – he has studied fossil bryozoans from all of the geological periods, and modern bryozoans from all oceanic basins. His interests include taxonomy, biodiversity, skeletal structure, ecology, evolution, history to name a few subject areas; in fact there are probably none in bryozoology that have not been the subject of his many publications. His office in the Natural History Museum quickly became a magnet for visiting bryozoological colleagues whom he always welcomed: he has always been highly encouraging of the research efforts of others, quick to collaborate, and generous with advice and information. A long-standing member of the International Bryozoology Association, Paul presided over the conference held in Boone in 2007. 3 BRYOZOAN STUDIES 2019 Contents Kamil Zágoršek and Patrick N. Wyse Jackson Foreword ...................................................................................................................................................... 6 Caroline J. Buttler and Paul D. Taylor Review of symbioses between bryozoans and primary and secondary occupants of gastropod -
Growth Geometry and Measurement of Growth Rates in Marine Bryozoans: a Review
BRYOZOAN STUDIES 2019 Growth geometry and measurement of growth rates in marine bryozoans: a review Abigail M. Smith1* and Marcus M. Key, Jr.2 1 Department of Marine Science, University of Otago, P.O. Box 56, Dunedin 9054, New Zealand [*corresponding author: email: [email protected]] 2 Department of Earth Sciences, Dickinson College, P.O. Box 1773, Carlisle, PA 17013-2896, USA ABSTRACT measuring and reporting growth rate in bryozoans The relationship between age and size in colonial will ensure they are robust and comparable. marine organisms is problematic. While growth of individual units may be measured fairly easily, the growth of colonies can be variable, complex, and INTRODUCTION difficult to measure. We need this information in Bryozoans are lophophorate aquatic invertebrates order to manage and protect ecosystems, acquire which typically form colonies by iterative addition bioactive compounds, and understand the history of of modular clones (zooids). Freshwater species environmental change. Bryozoan colonial growth are uncalcified; the majority of marine species are forms, determined by the pattern of sequential calcified, so that there is an extensive fossil record of addition of zooids or modules, enhance feeding, marine bryozoan colonies. When calcified colonies colony integration, strength, and/or gamete/larval grow large, they can provide benthic structures dispersal. Colony age varies from three months to which enhance biodiversity by provision of sheltered 86 years. Growth and development, including both habitat. Agencies who wish to manage or protect addition of zooids and extrazooidal calcification, these productive habitats need to understand the can be linear, two-dimensional across an area, or longevity and stability of these structures. -
Sucesión De Amonitas Del Cretácico Superior (Cenomaniano – Coniaciano) De La Parte Más Alta De La Formación Hondita Y De L
Boletín de Geología Vol. 33, N° 1, enero-junio de 2011 SUCESIÓN DE AMONITAS DEL CRETÁCICO SUPERIOR (CENOMANIANO – CONIACIANO) DE LA PARTE MÁS ALTA DE LA FORMACIÓN HONDITA Y DE LA FORMACIÓN LOMA GORDA EN LA QUEBRADA BAMBUCÁ, AIPE - HUILA (COLOMBIA, S. A.) Pedro Patarroyo1 RESUMEN La sección de la quebrada Bambucá (Aipe - Huila) posee una buena exposición de los depósitos del Cretácico del Valle Superior del Magdalena. De la parte alta de la Formación Hondita se recolectaron Acanthoceras sp. y Rhynchostreon sp. del Cenomaniano superior. Dentro del segmento inferior de la Formación Loma Gorda se hallaron Choffaticeras (C.) cf. segne, Fagesia cf. catinus, Neoptychites cf. andinus, Mitonia gracilis, Morrowites sp., Nannovascoceras ? sp., Quitmaniceras ? sp., Benueites ? sp. junto con Mytiloides kossmati, M. goppelnensis y Anomia sp. del Turoniano inferior. Estratigráficamente arriba aparecen Paramammites ? sp., Hoplitoides sp. H. ingens, H. cf. lagiraldae, Codazziceras ospinae, Allocrioceras sp., que pueden estar representando entre el Turoniano inferior y medio. Para la parte alta de este segmento se encontraron Prionocycloceras sp. P. guayabanum, Reesidites subtuberculatum, Subprionotropis colombianus, Mytiloides scupini, Dydimotis sp., Gauthiericeras sp., Anagaudryceras ? sp., Eulophoceras jacobi, Paralenticeras sieversi, Hauericeras cf. madagascarensis, Peroniceras (P.) subtricarinatum, Forresteria (F.) sp., Barroisiceras cf. onilahyense, Ankinatsytes venezolanus que abarcan entre el Turoniano superior y el Coniaciano. Con base en la fauna colectada no es posible establecer los límites Cenomaniano/Turoniano y Turoniano/Coniaciano. Palabras clave: Amonitas, Cretácico superior, Valle Superior del Magdalena, Aipe-Huila-Colombia. UPPER CRETACEOUS AMMONITE SUCCESSION (CENOMANIAN – CONIACIAN) RELATED TO THE UPPER HONDITA AND LOMA GORDA FORMATIONS ALONG THE BAMBUCÁ CREEK, AIPE - HUILA (COLOMBIA, S.A.) ABSTRACT The Bambucá creek section (Aipe - Huila) shows a very good exposition of the Upper Magdalena Valley Cretaceous deposits. -
(Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean Region
European Journal of Taxonomy 536: 1–33 ISSN 2118-9773 https://doi.org/10.5852/ejt.2019.536 www.europeanjournaloftaxonomy.eu 2019 · Madurell T. et al. This work is licensed under a Creative Commons Attribution License (CC BY 4.0). Research article urn:lsid:zoobank.org:pub:EC4DDAED-11A3-45AB-B276-4ED9A301F9FE Revision of the Genus Schizoretepora (Bryozoa, Cheilostomatida) from the Atlantic-Mediterranean region Teresa MADURELL 1,*, Mary SPENCER JONES 2 & Mikel ZABALA 3 1 Institute of Marine Sciences (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalonia. 2 Department of Life Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK. 3 Department d’Ecologia, Universitat de Barcelona (UB), Diagonal 645, 08028 Barcelona, Catalonia. * Corresponding author: [email protected] 2 Email: [email protected] 3 Email: [email protected] 1 urn:lsid:zoobank.org:author:AB9762AB-55CD-4642-B411-BDBE45CA2082 2 urn:lsid:zoobank.org:author:0C8C2EBE-17E1-44DA-8FDB-DC35F615F95B 3 urn:lsid:zoobank.org:author:7E533CE7-92CA-4A17-8E41-5C37188D0CDA Abstract. We examined the type specimens and historical collections holding puzzling Atlantic and Mediterranean material belonging to the genus Schizoretepora Gregory, 1893. We performed a detailed study of the colonial characters and re-describe the resulting species and those that have rarely been found or have poor original descriptions. As a result of this revision, nine species are found in the northeast Atlantic and Mediterranean. Six of them are re-described and illustrated: S. aviculifera (Canu & Bassler, 1930), S. calveti d’Hondt, 1975, S. imperati (Busk, 1884), S. sp. nov.? (= S. -
Marlin Marine Information Network Information on the Species and Habitats Around the Coasts and Sea of the British Isles
MarLIN Marine Information Network Information on the species and habitats around the coasts and sea of the British Isles Hornwrack (Flustra foliacea) MarLIN – Marine Life Information Network Biology and Sensitivity Key Information Review Dr Harvey Tyler-Walters & Susie Ballerstedt 2007-09-11 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/species/detail/1609]. All terms and the MarESA methodology are outlined on the website (https://www.marlin.ac.uk) This review can be cited as: Tyler-Walters, H. & Ballerstedt, S., 2007. Flustra foliacea Hornwrack. 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/marlinsp.1609.2 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) Date: 2007-09-11 Hornwrack (Flustra foliacea) - Marine Life Information Network See online review for distribution map Flustra foliacea. Distribution data supplied by the Ocean Photographer: Keith Hiscock Biogeographic Information System (OBIS). -
First Occurrence of the Non-Native Bryozoan Schizoporella Japonica Ortmann (1890) in Western Europe
Zootaxa 3780 (3): 481–502 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2014 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3780.3.3 http://zoobank.org/urn:lsid:zoobank.org:pub:E8B88941-65A4-44F8-8D93-D2F7B541152D First occurrence of the non-native bryozoan Schizoporella japonica Ortmann (1890) in Western Europe JOHN S. RYLAND1,6, ROHAN HOLT2, JENNIFER LOXTON3,4,5, MARY E. SPENCER JONES4 & JOANNE S. PORTER3,4 1Department of Biosciences, Wallace Building, Swansea University, Swansea SA2 8PP, Wales UK. E-mail: [email protected] 2Natural Resources Wales, Maes Y Ffynnon, Bangor LL57 2DW, Wales UK 3School of Life Sciences, Centre for Marine Biodiversity and Biotechnology, Heriot-Watt University, James Muir Building, Gait 1, Edinburgh EH14 4AS, Scotland UK 4Department of Zoology, Natural History Museum, Cromwell Road, London SW7 5BD, England UK 5University Marine Biological Station Millport, Isle of Cumbrae KA28 0EG, Scotland UK 6Corresponding author Abstract Schizoporella japonica Ortmann was described from Japan but was subsequently introduced on Pacific oysters to the Pa- cific coast of North America, where it is now well established. In this paper we record it for the first time in European waters. The initial discovery was in a marina at Holyhead, North Wales, in July 2010 but S. japonica has since been ob- served abundantly in the Orkney Islands (from May 2011) and, subsequently, at other localities in northern Scotland. In- troduction seems most likely to have been on an ocean-going vessel. The British material is here fully described and illustrated with SEMs and colour photographs; some unusual characters are discussed. -
Upper Cretaceous (Maestrichtian) Mollusca from the Haustator Bilira Assemblage Zone in the East Gulf Coastal Plain
UNITED STATES DEPARTMENT OF INTERIOR GEOLOGICAL SURVEY Upper Cretaceous (Maestrichtian) Mollusca from the Haustator bilira Assemblage Zone in the East Gulf Coastal Plain Norman F. So hi 1 and Carl F. Koch2 Open File Feport 83-451 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial Standards and stratigraphic nomenclature. Pages are numbered one to four and seven to 239. 1. Washington D.C. 2. Old Dominion University Norfolk, Va, 1983 CONTENTS Page Introduction 1 Explanation 1 Explanation of Annotation 4 References 9 Molluscan Faunal Lists 11 ILLUSTRATIONS Figure 1 Map showing location of collections 2 Relationships of stratigraphic units within the Haustator bilira Assemblage Zone, East Gulf Coastal Plain TABLE Table 1 U.S. Geological Survey numbers of collections for each location Upper Cretaceous (Maestrichtian) Mollusca from the Haustator bilira Assemblage Zone in the East Gulf Coastal Plain INTRODUCTION The following report contains lists of the molluscan fauna from 189 collections made at 161 localities or different levels at a locality in the rocks of the Haustator bilira Assemblage Zone as exposed in western Georgia, Alabama, Mississippi, and Tennessee (Figure 1). This compilation forms the data base for a series of studies published, in press or in preparation (Buzas, £t_ al. , 1982; Koch and Sohl, in press). The Haustator bilira Assemblage Zone was proposed by Sohl (1977) and traced through Late Cretaceous rocks of the Atlantic and Gulf Coastal Plains from New Jersey to Texas (Owens, et_jil_., 1977; Sohl and Smith, 1980). The base of the zone occurs above the base of the foraminiferid Globotruncana gansseri subzone of Pessagno (1967) and includes all subsequent younger Cretaceous deposits on the Coastal Plains (Figure 2). -
Marine Bryozoans (Ectoprocta) of the Indian River Area (Florida)
MARINE BRYOZOANS (ECTOPROCTA) OF THE INDIAN RIVER AREA (FLORIDA) JUDITH E. WINSTON BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY VOLUME 173 : ARTICLE 2 NEW YORK : 1982 MARINE BRYOZOANS (ECTOPROCTA) OF THE INDIAN RIVER AREA (FLORIDA) JUDITH E. WINSTON Assistant Curator, Department of Invertebrates American Museum of Natural History BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY Volume 173, article 2, pages 99-176, figures 1-94, tables 1-10 Issued June 28, 1982 Price: $5.30 a copy Copyright © American Museum of Natural History 1982 ISSN 0003-0090 CONTENTS Abstract 102 Introduction 102 Materials and Methods 103 Systematic Accounts 106 Ctenostomata 106 Alcyonidium polyoum (Hassall), 1841 106 Alcyonidium polypylum Marcus, 1941 106 Nolella stipata Gosse, 1855 106 Anguinella palmata van Beneden, 1845 108 Victorella pavida Saville Kent, 1870 108 Sundanella sibogae (Harmer), 1915 108 Amathia alternata Lamouroux, 1816 108 Amathia distans Busk, 1886 110 Amathia vidovici (Heller), 1867 110 Bowerbankia gracilis Leidy, 1855 110 Bowerbankia imbricata (Adams), 1798 Ill Bowerbankia maxima, New Species Ill Zoobotryon verticillatum (Delle Chiaje), 1828 113 Valkeria atlantica (Busk), 1886 114 Aeverrillia armata (Verrill), 1873 114 Cheilostomata 114 Aetea truncata (Landsborough), 1852 114 Aetea sica (Couch), 1844 116 Conopeum tenuissimum (Canu), 1908 116 IConopeum seurati (Canu), 1908 117 Membranipora arborescens (Canu and Bassler), 1928 117 Membranipora savartii (Audouin), 1926 119 Membranipora tuberculata (Bosc), 1802 119 Membranipora tenella Hincks, -
Invertebrate ID Guide
11/13/13 1 This book is a compilation of identification resources for invertebrates found in stomach samples. By no means is it a complete list of all possible prey types. It is simply what has been found in past ChesMMAP and NEAMAP diet studies. A copy of this document is stored in both the ChesMMAP and NEAMAP lab network drives in a folder called ID Guides, along with other useful identification keys, articles, documents, and photos. If you want to see a larger version of any of the images in this document you can simply open the file and zoom in on the picture, or you can open the original file for the photo by navigating to the appropriate subfolder within the Fisheries Gut Lab folder. Other useful links for identification: Isopods http://www.19thcenturyscience.org/HMSC/HMSC-Reports/Zool-33/htm/doc.html http://www.19thcenturyscience.org/HMSC/HMSC-Reports/Zool-48/htm/doc.html Polychaetes http://web.vims.edu/bio/benthic/polychaete.html http://www.19thcenturyscience.org/HMSC/HMSC-Reports/Zool-34/htm/doc.html Cephalopods http://www.19thcenturyscience.org/HMSC/HMSC-Reports/Zool-44/htm/doc.html Amphipods http://www.19thcenturyscience.org/HMSC/HMSC-Reports/Zool-67/htm/doc.html Molluscs http://www.oceanica.cofc.edu/shellguide/ http://www.jaxshells.org/slife4.htm Bivalves http://www.jaxshells.org/atlanticb.htm Gastropods http://www.jaxshells.org/atlantic.htm Crustaceans http://www.jaxshells.org/slifex26.htm Echinoderms http://www.jaxshells.org/eich26.htm 2 PROTOZOA (FORAMINIFERA) ................................................................................................................................ 4 PORIFERA (SPONGES) ............................................................................................................................................... 4 CNIDARIA (JELLYFISHES, HYDROIDS, SEA ANEMONES) ............................................................................... 4 CTENOPHORA (COMB JELLIES)............................................................................................................................ -
Feeding Repellence in Antarctic Bryozoans
Naturwissenschaften (2013) 100:1069–1081 DOI 10.1007/s00114-013-1112-8 ORIGINAL PAPER Feeding repellence in Antarctic bryozoans Blanca Figuerola & Laura Núñez-Pons & Juan Moles & Conxita Avila Received: 3 September 2013 /Revised: 16 October 2013 /Accepted: 20 October 2013 /Published online: 13 November 2013 # Springer-Verlag Berlin Heidelberg 2013 Abstract The Antarctic sea star Odontaster validus and the an important role in Antarctic bryozoans as defenses against amphipod Cheirimedon femoratus are important predators in predators. benthic communities. Some bryozoans are part of the diet of the asteroid and represent both potential host biosubstrata and Keywords Odontaster validus . Cheirimedon femoratus . prey for this omnivorous lysianassid amphipod. In response to Chemical ecology . Chemical defense . Deception Island such ecological pressure, bryozoans are expected to develop strategies to deter potential predators, ranging from physical to chemical mechanisms. However, the chemical ecology of Introduction Antarctic bryozoans has been scarcely studied. In this study we evaluated the presence of defenses against predation in The continental shelf of the eastern Weddell Sea and other selected species of Antarctic bryozoans. The sympatric om- Antarctic regions are characterized by presence of diverse, nivorous consumers O. validus and C. femoratus were select- well-structured benthic communities, dominated by eurybath- ed to perform feeding assays with 16 ether extracts (EE) and ic suspension feeders such as sponges, gorgonians, bryozoans, 16 butanol extracts (BE) obtained from 16 samples that and ascidians (Dayton et al. 1974; Teixidó et al. 2002; belonged to 13 different bryozoan species. Most species (9) Figuerola et al. 2012a). The establishment of the Antarctic were active (12 EE and 1 BE) in sea star bioassays. -
En San Francisco, Cundinamarca (Colombia)
Boletín de Geología ISSN: 0120-0283 Vol. 38, N° 3, julio-septiembre de 2016 URL: boletindegeologia.uis.edu.co AMONOIDEOS Y OTROS MACROFÓSILES DEL LECTOESTRATOTIPO DE LA FORMACIÓN LA FRONTERA, TURONIANO INFERIOR - MEDIO (CRETÁCICO SUPERIOR) EN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA) Pedro Patarroyo1 DOI: http://dx.doi.org/10.18273/revbol.v38n3-2016003 Forma de citar: Patarroyo, P. 2016. Amonoideos y otros macrofósiles del lectoestratotipo de la Formación La Frontera, Turoniano inferior - medio (Cretácico Superior) en San Francisco, Cundinamarca (Colombia). Boletín de Geología, 38(3): 41-54. RESUMEN Una sucesión de cerca de 109 m de espesor del lectoestratotipo de la Formación La Frontera (Colombia) se describe junto con el contenido fósil de Wrightoceras munieri (Pervinquière, 1907), Vascoceras cf. constrictum (Renz and Álvarez, 1979), V. cf. venezolanum Renz, 1982, Kamerunoceras sp., K. cf. turoniense (d’Orbigny, 1850), Hoplitoides cf. lagiraldae Etayo-Serna, 1979, Codazziceras ospinae (Karsten, 1858), Coilopoceras cf. newelli (Benavides-Cáceres, 1956); bivalvos: Anomia colombiana Villamil, 1996, e inocerámidos; y decápodos y plantas (troncos). Estos ejemplares incluidos dentro de la sucesión de la Formación La Frontera, en su mayoría, representan el Turoniano inferior - medio. La existencia de depósitos del Cenomaniano más alto hacia la base de la Formación La Frontera no se puede demostrar en este trabajo. Palabras clave: Formación La Frontera, Lectoestratotipo, Amonoideos, Turoniano, San Francisco-Cundinamarca AMMONITES AND OTHER MACROFOSSILS FROM THE LECTOSTRATOTYPE OF LA FRONTERA FORMATION, LOWER - MIDDLE TURONIAN (UPPER CRETACEOUS) IN SAN FRANCISCO, CUNDINAMARCA (COLOMBIA) ABSTRACT A succession of about 109 m thick of the La Frontera Formation lectostratotype (Colombia) is described as well as the fossils Wrightoceras munieri (Pervinquière, 1907), Vascoceras cf. -
Check List 8(1): 181-183, 2012 © 2012 Check List and Authors Chec List ISSN 1809-127X (Available at Journal of Species Lists and Distribution
Check List 8(1): 181-183, 2012 © 2012 Check List and Authors Chec List ISSN 1809-127X (available at www.checklist.org.br) Journal of species lists and distribution N Bryozoa, Cheilostomata: First records of two invasive species in Australia and the northerly range extension for a third ISTRIBUTIO D Kevin J. Tilbrook RAPHIC G Museum of Tropical Queensland, 70–102 Flinders Street, Townsville, QLD 4810, Australia. EO E-mail: [email protected] G N O OTES N Abstract: Biofouling of international marine vessels is one of the most important mechanisms for the transfer of non- native-invasive species around the world. Bryozoan species are some of the commonest of these marine biofouling organisms found worldwide. Whilst some efforts have been made to document the bryozoan species in Australian ports, these surveys are very limited in number, poorly resolved and lack repetition. This paper records two invasive bryozoan species new to Australian waters (Hippoporina indica and Biflustra grandicella), and a northerly range extension of a known invasive bryozoan (Zoobotryon verticillatum). Bryozoans are a phylum of sessile, colonial suspension- Zealand (Gordon et al. 2008), the Gulf of Mexico, and the feeders found throughout the world in both marine and Atlantic coast of the USA (McCann et al freshwater environments. Bryozoan species are some Hippoporina indica of the commonest marine fouling organisms found Marina, Brisbane (27°27’20” S; 153°11’24”. 2007). E In) Australia,in March worldwide, yet their distribution is not well known, 2010 on settlement was plates first attachednoticed into Manlypontoons, Harbour and generally through a lack of interest in the group and the marina pylons; it was noted as very common that austral fauna of the Queensland coast and the Great Barrier Reef Brisbane its peak growing period is between February (GBR)perception in particular, that their is probablytaxonomy one is difficult.of the richest The bryozoanand most andsummer-autumn May when it can(Dustin occupy Marshall up to 30%pers.