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Annelida, Amphinomidae) in the Mediterranean Sea with an Updated Revision of the Alien Mediterranean Amphinomids
A peer-reviewed open-access journal ZooKeys 337: 19–33 (2013)On the occurrence of the firewormEurythoe complanata complex... 19 doi: 10.3897/zookeys.337.5811 RESEARCH ARTICLE www.zookeys.org Launched to accelerate biodiversity research On the occurrence of the fireworm Eurythoe complanata complex (Annelida, Amphinomidae) in the Mediterranean Sea with an updated revision of the alien Mediterranean amphinomids Andrés Arias1, Rômulo Barroso2,3, Nuria Anadón1, Paulo C. Paiva4 1 Departamento de Biología de Organismos y Sistemas (Zoología), Universidad de Oviedo, Oviedo 33071, Spain 2 Pontifícia Universidade Católica do Rio de Janeiro , Rio de Janeiro, Brazil 3 Museu de Zoologia da Unicamp, Campinas, SP, Brazil 4 Departamento de Zoologia, Instituto de Biologia, Universidade Federal do Rio de Janeiro (UFRJ) , Rio de Janeiro, RJ, Brasil Corresponding author: Andrés Arias ([email protected]) Academic editor: C. Glasby | Received 17 June 2013 | Accepted 19 September 2013 | Published 30 September 2013 Citation: Arias A, Barroso R, Anadón N, Paiva PC (2013) On the occurrence of the fireworm Eurythoe complanata complex (Annelida, Amphinomidae) in the Mediterranean Sea with an updated revision of the alien Mediterranean amphinomids. ZooKeys 337: 19–33. doi: 10.3897/zookeys.337.5811 Abstract The presence of two species within the Eurythoe complanata complex in the Mediterranean Sea is reported, as well as their geographical distributions. One species, Eurythoe laevisetis, occurs in the eastern and cen- tral Mediterranean, likely constituting the first historical introduction to the Mediterranean Sea and the other, Eurythoe complanata, in both eastern and Levantine basins. Brief notes on their taxonomy are also provided and their potential pathways for introduction to the Mediterranean are discussed. -
SCAMIT Newsletter Vol. 1 No. 2 1982
TAXONOMIC INTERCAL1BRAT10N NEWSLETTER May, 1932 Number 2 Next Scheduled Meeting: June lA, 1982 at 9:30 a.m. Place: Marine Biological Consultants 9^7 Newhal1 Street Costa Mesa, California 92627 Topic Taxonomic Group: Amphinomidae, Euphrosinidae, Phyllodocidae MINUTES FROM MAY 17, 1982 Name Fourteen different names with accompanying acronyms were suggested. Because there were so many, it was decided to vote for a name by ballot and talley the results at the June meeting. One ballot is enclosed in this Newsletter. Please bring it to the next meeting or mail it to Ann Martin by June 11. Make additional copies of the ballot for each member of your Company. Dues Unfortunately dues are going to be ch-arged. The dues will help defray costs incurred for storing the reference collection, paper, postage, and other unforeseen expenses. Dues will be $5.00 per year beginning June, 1982. This amount will be adjusted after six months if it is insufficient. Dues will be collected at the June meeting. For those unable to attend the meeting, dues can be mailed to.Ann Martin and a receipt will be mailed back. Specimen Exchange. Several points concerning the specimen exchange were brought out that will help. - Participants should be responsible for getting their specimens to the meeting, either in person or by mail. - Mark the specimens sequentially to prevent mixing of different groups. - Bring the voucher specimens to meeting to check them with ones from the specimen exchange. - When deciding what species to select for the specimen exchange, first call Tony Phillips, (213) 322-3131 extension 269, and tell him what you plan to bring in. -
H1.1 Open Water
PAGE .............................................................. 392 ▼ H1.1 OPEN WATER The open-water offshore habitat covers an area of by which solar energy enters the marine ecosystem, Nova Scotia larger than the land mass, and includes similar to the layer of plants on land. The ocean H1.1 Open Water salt water in inlets, bays and estuaries. The water waters are distinctive in having fostered the origins and the organisms it supports are the primary means of life on the planet. Plate H1.1.1: Right Whale, north of Brier Island (Unit 912). Photo: BIOS Habitats Natural History of Nova Scotia, Volume I © Nova Scotia Museum of Natural History .............................................................. PAGE 393 ▼ FORMATION PLANTS Oceans are formed as part of major geological events. The plants of the open ocean are almost entirely Nova Scotia’s open-ocean habitats are part of the microscopic algae, collectively known as phyto- Atlantic Ocean, which opened during the Jurassic plankton. Many different species occur, including Period and has been in continuous existence ever representatives of the prochlorophytes (blue-green since. The quality and depth of the water column algae—evolutionary intermediates between bacteria have fluctuated in relation to post-glacial climatic and algae), diatoms, dinoflagellates, chrysomonads, conditions. cryptomonads, minute flagellates and unicellular reproductive stages of macroscopic algae. Phyto- H1.1 PHYSICAL ASPECTS plankton are often grouped in size classes: Open Water 1. Water conditions, such as salinity, temperature, macroplankton: 200–2000 micrometres, includes ice-formation, turbidity, light penetration, tides larger diatoms. and currents, are extremely variable in the microplankton: 20–200 micrometres, includes waters offshore. most diatoms. 2. Air-water interaction, surface-water turbulence nanoplankton: 2–20 micrometres, includes determines the level of wave and gas exchange. -
OREGON ESTUARINE INVERTEBRATES an Illustrated Guide to the Common and Important Invertebrate Animals
OREGON ESTUARINE INVERTEBRATES An Illustrated Guide to the Common and Important Invertebrate Animals By Paul Rudy, Jr. Lynn Hay Rudy Oregon Institute of Marine Biology University of Oregon Charleston, Oregon 97420 Contract No. 79-111 Project Officer Jay F. Watson U.S. Fish and Wildlife Service 500 N.E. Multnomah Street Portland, Oregon 97232 Performed for National Coastal Ecosystems Team Office of Biological Services Fish and Wildlife Service U.S. Department of Interior Washington, D.C. 20240 Table of Contents Introduction CNIDARIA Hydrozoa Aequorea aequorea ................................................................ 6 Obelia longissima .................................................................. 8 Polyorchis penicillatus 10 Tubularia crocea ................................................................. 12 Anthozoa Anthopleura artemisia ................................. 14 Anthopleura elegantissima .................................................. 16 Haliplanella luciae .................................................................. 18 Nematostella vectensis ......................................................... 20 Metridium senile .................................................................... 22 NEMERTEA Amphiporus imparispinosus ................................................ 24 Carinoma mutabilis ................................................................ 26 Cerebratulus californiensis .................................................. 28 Lineus ruber ......................................................................... -
(Polychaeta) Borings in Paraspirifer Bownockeri (Brachiopoda: Devonian)1
114 A. E. ANNALA AND L. A. KAPUSTKA Vol. 83 Copyright © 1983 Ohio Acad. Sci. 003O-O95O/83/0003-O114 $2.00/0 VERMIFORICHNUS (POLYCHAETA) BORINGS IN PARASPIRIFER BOWNOCKERI (BRACHIOPODA: DEVONIAN)1 R. D. HOARE and R. L. WALDEN, Department of Geology, Bowling Green State University, Bowling Green, OH 43403 ABSTRACT. Shells of Paraspirifer bownockeri (Stewart) from the Silica Formation, Middle Devonian of northwestern Ohio, commonly contain numerous borings of a polychaete worm forming the endolithic trace fossil Vermiforichnus clarki Cameron (1969a) which can be exposed by acidizing the specimens. The borings are most abundant on the brachial valve, and their surface openings tend to be concentrated along major growth lines thence extending dominantly in the general direction of the beaks of the valves. In- festations of the polychaete occurred at 2 different time intervals as indicated by the spac- ing of the borings on 2 major growth lines with renewed shell growth between them. Growth of the host was severely reduced immediately following the infestation and in some areas damage to the mantle caused deformation in the shell of the host. OHIO J. SCI. 83 (3): 114-119, 1983 INTRODUCTION (1932) by Hoare and Steller (1967) (fig. 1), Previous interpretations of the larger as boring sponges by Kesling and Chilman borings commonly seen in the brachiopod (1975) and as "Clionoides" sp. by Steller Paraspirifer bownockeri (Stewart) from the (1965), Kesling et al. (1980) and Sparks Silica Formation in northwestern Ohio et al. (1980). These interpretations were have been alluded to as sponge borings, based on the external configuration of the Clionoides thomasi Fenton and Fenton surface opening of the boring only. -
The Presence of Melinna Palmata (Annelida: Polychaeta) and Ensis
Cah. Biol. Mar. (2007) 48 : 391-401 The presence of Melinna palmata (Annelida: Polychaeta) and Ensis directus (Mollusca: Bivalvia) related to sedimentary changes in the Bay of Seine (English Channel, France) Jean-Claude DAUVIN1*, Thierry RUELLET1, Eric THIEBAUT2, Franck GENTIL2, Nicolas DESROY3, Anne-Laure JANSON4, Sylvain DUHAMEL5, Jérôme JOURDE5 and Serge SIMON5 (1) Station Marine de Wimereux, Université des Sciences et Technologies de Lille, FRE CNRS 2816 ELICO, B.P. 80, 62930 Wimereux, France. *Corresponding author: Fax: 33 3 21 99 29 01, E-mail: [email protected] (2) Université Pierre et Marie Curie-Paris 6, Station Biologique de Roscoff, UMR CNRS 7144, B.P. 74, 29682 Roscoff Cedex, France (3) Station IFREMER, 2 bis rue Saint-Georges, B.P. 46, 35042 Saint-Malo Cedex, France (4) Muséum National d’Histoire Naturelle, Département Milieux et Peuplements Aquatiques CNRS UMR 5178 BOME, 61 rue Buffon, 75005 Paris, France (5) Cellule du Suivi du Littoral Normand, 16 quai Casimir Delavigne, 76600 Le Havre, France Abstract: Since late 1990s the annelid polychaete Melinna palmata and the mollusc bivalve Ensis directus have been collected in the eastern part of the Bay of Seine (English Channel), indicating changes in the benthic communities. Melinna palmata was never collected prior to 2002, whereas it was reported in the muddy fine sands of the western part of the Channel, along the French (e.g. Bay of Cherbourg) and southern UK (e.g. Southampton Waters) coasts. Ensis directus was first reported in 1998 and now appears to be well implanted, given the abundant population collected in 2006. -
The Snodgrass Tapes Evolution of the Arthropods Robert Evans Snodgrass Page 1 Figure 1
The Snodgrass Tapes Evolution of the Arthropods The third of three lectures by the insect morphologist Robert Evans Snodgrass delivered to the Department of Entomology at the University of Maryland in 1960. Transcribed, assembled and annotated by Jeffrey W. Shultz Robert Evans Snodgrass Well, the subject today will be the evolution of the arthropods. But, of course, I'll have to admit to begin with that I don't really know the truth of the matter. So, judging from what facts you can get to together... I suppose at the present time that all .... evolution is accepted as a fact by all zoologists. And apparently the fundamentalists have given up trying to do anything about it. Yet it is a theory. And ... But it seems the idea of natural selection well- enough accounts for the physical evolution of animals; that is, certain genes produce the proper variations. But what bothers me about the ... about the evolution of the animals is how did the animal ever become such a com- plex assemblage of chemical substances. I've had a cold, but I guess I can talk through it. Every cell in the body, for example, has to have its own enzymes to do its work it's supposed to do. And all these activities have to be correlated and regulated by hormones, and hormones, again, are just chemical compounds. And, so, it seems to me that that's one of the problems of evolution yet is to find out how all of these chemical substances ever got together in the animal in the proper amount, in the proper places and [how they came] to do the things that they do do... -
Identification Guide to the Planktonic Polychaete Larvae Around the Island of Helgoland (German Bight)
HELGOL.~NDER MEERESUNTERSUCHUNGEN Helgol/inder Meeresunters. 48, 1-58 (1994) Identification guide to the planktonic polychaete larvae around the island of Helgoland (German Bight) S. Plate* & E. Husemann* * Biologische Anstalt Helgoland (Meeresstation); D-27483 Helgoland, Federal Republic of Germany ABSTRACT: The purpose of this work is to provide the means of identifying the planktonic larvae of the polychaete species appearing in the plankton around the island of Helgoland (North Sea). During a three-year survey in this area, the larvae of 54 species out of 24 families belonging to the orders Orbiniida, Spionida, Capitelhda, Phyllodocida, Oweniida, Terebelhda, Sabelhda and the former Archiannelida have been recorded. Illustrated keys to the families, genera and species are presented. To facilitate the identification, additional descriptions and information about the seasonal appearance of the species are given. INTRODUCTION More than 13 000 species of polychaetous annelids take part in the marine benthos communities worldwide. Their distribution, species composition and population density are monitored within various benthos surveys. For the North Sea, especially the German Bight and the Wadden Sea, much information about the benthic polychaete fauna is available (Caspers, 1950; Stripp, 1969; DSrjes, 1977; Rachor & Gerlach, 1978; Gillandt, 1979; Salzwedel et al., 1985; Rachor, 1990; Bosselmann, 1991; Kr6ncke, 1991). In contrast, the holoplanktonic polychaete species and the meroplanktonic polychaete larvae, which are only part of the plankton during a more or less expanded phase of their ontogenesis, have never received much attention. Meroplanktonic polychaete larvae are seldomly recorded during studies monitoring the North Sea plankton (Smidt, 1951; Giere, 1968; Fransz, 1981; Bosselmann, 1989; Belgrano et al., 1990). -
Oxygen, Ecology, and the Cambrian Radiation of Animals
Oxygen, Ecology, and the Cambrian Radiation of Animals The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Sperling, Erik A., Christina A. Frieder, Akkur V. Raman, Peter R. Girguis, Lisa A. Levin, and Andrew H. Knoll. 2013. Oxygen, Ecology, and the Cambrian Radiation of Animals. Proceedings of the National Academy of Sciences 110, no. 33: 13446–13451. Published Version doi:10.1073/pnas.1312778110 Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:12336338 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA Oxygen, ecology, and the Cambrian radiation of animals Erik A. Sperlinga,1, Christina A. Friederb, Akkur V. Ramanc, Peter R. Girguisd, Lisa A. Levinb, a,d, 2 Andrew H. Knoll Affiliations: a Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, 02138 b Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, 92093- 0218 c Marine Biological Laboratory, Department of Zoology, Andhra University, Waltair, Visakhapatnam – 530003 d Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, 02138 1 Correspondence to: [email protected] 2 Correspondence to: [email protected] PHYSICAL SCIENCES: Earth, Atmospheric and Planetary Sciences BIOLOGICAL SCIENCES: Evolution Abstract: 154 words Main Text: 2,746 words Number of Figures: 2 Number of Tables: 1 Running Title: Oxygen, ecology, and the Cambrian radiation Keywords: oxygen, ecology, predation, Cambrian radiation The Proterozoic-Cambrian transition records the appearance of essentially all animal body plans (phyla), yet to date no single hypothesis adequately explains both the timing of the event and the evident increase in diversity and disparity. -
Tropical Marine Invertebrates CAS BI 569 Phylum ANNELIDA by J
Tropical Marine Invertebrates CAS BI 569 Phylum ANNELIDA by J. R. Finnerty Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA “BILATERIA” (=TRIPLOBLASTICA) Bilateral symmetry (?) Mesoderm (triploblasty) Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA “COELOMATA” True coelom Coelomata gut cavity endoderm mesoderm coelom ectoderm [note: dorso-ventral inversion] Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA PROTOSTOMIA “first mouth” blastopore contributes to mouth ventral nerve cord The Blastopore ! Forms during gastrulation ectoderm blastocoel blastocoel endoderm gut blastoderm BLASTULA blastopore The Gut “internal, epithelium-lined cavity for the digestion and absorption of food sponges lack a gut simplest gut = blind sac (Cnidaria) blastopore gives rise to dual- function mouth/anus through-guts evolve later Protostome = blastopore contributes to the mouth Deuterostome = blastopore becomes the anus; mouth is a second opening Protostomy blastopore mouth anus Deuterostomy blastopore -
Polychaeta Lana Crumrine
Polychaeta Lana Crumrine Well over 200 species of the class Polychaeta are found in waters off the shores of the Pacific Northwest. Larval descriptions are not available for the majority of these species, though descriptions are available of the larvae for at least some species from most families. This chapter provides a dichotomous key to the polychaete larvae to the family level for those families with known or suspected pelagic larva. Descriptions have be $in gleaned from the literature from sites worldwide, and the keys are based on the assumption that developmental patterns are similar in different geographical locations. This is a large assumption; there are cases in which development varies with geography (e.g., Levin, 1984). Identifying polychaetes at the trochophore stage can be difficult, and culturing larvae to advanced stages is advised by several experts in the field (Bhaud and Cazaux, 1987; Plate and Husemann, 1994). Reproduction, Development, and Morphology Within the polychaetes, the patterns of reproduction and larval development are quite variable. Sexes are separate in most species, though hermaphroditism is not uncommon. Some groups undergo a process called epitoky at sexual maturation; benthic adults develop swimming structures, internal organs degenerate, and mating occurs between adults swimming in the water column. Descriptions of reproductive pattern, gamete formation, and spawning can be found in Strathmann (1987). Larval polychaetes generally develop through three stages: the trochophore, metatrochophore, and nectochaete stages. Trochophores are ciliated larvae (see Fig. 1).A band of cilia, the prototroch, is used for locomotion and sometimes feeding. Trochophore larvae are generally broad anteriorly and taper posteriorly. -
AMPHINOMIDAE (ANNELIDA: POLYCHAETA) from ROCAS ATOLL, NORTHEASTERN BRAZIL 1 (With 3 Figures)
Arquivos do Museu Nacional, Rio de Janeiro, v.65, n.3, p.357-362, jul./set.2007 ISSN 0365-4508 AMPHINOMIDAE (ANNELIDA: POLYCHAETA) FROM ROCAS ATOLL, NORTHEASTERN BRAZIL 1 (With 3 figures) RÔMULO BARROSO 2, 3 PAULO CESAR PAIVA 3 ABSTRACT: Three amphinomid species from Rocas Atoll - Northeastern Brazil are reported. The re-description of Eurythoe complanata , Hermodice carunculata and the description of L inopherus cf. canariensis is provided. Key words: Amphinomidae. Eurythoe . Hermodice . Linopherus . Rocas Atoll. RESUMO: Amphinomidae (Annelida: Polychaeta) do Atol das Rocas, nordeste do Brasil. Três espécies de anfinomídeos do Atol das Rocas, nordeste do Brasil foram identificados. São apresentadas redescrições das espécies: Eurythoe complanata, Hermodice carunculata e a descrição de Linopherus cf. canariensis. Palavras-chave: Amphinomidae. Eurythoe . Hermodice . Linopherus . Atol das Rocas. INTRODUCTION They possess an eversible pharynx, bearing neither jaws, teeth, nor papillae. The family Amphinomidae was proposed by Branchiae may be present on some, or on all Lamarck in 1818. Within this family, 19 genera notopodia, although they are typically absent on the and 130 species have been recognized (K UDENOV , first setiger. Branchiae shape includes dendritic, 1995). The amphinomids are commonly found in bipinate or palmate forms. shallow tropical and subtropical water; however All chaetae are calcified, and the notosetae include specimens have also been reported in abyssal bifurcate and “harpoon” setae and neurosetae may depths and polar regions (K UDENOV , 1993). include curved hooks, bifurcated setae, smooth or Members within this family normally have spurred spines and capillaries. elongated body, more or less sub-rectangular in Amphinomids together with the other members of cross-section, less commonly depressed and sub- the Order Amphinomida are unusual, compared to elliptic in outline.