Intertidal Marine Invertebrates Guild (Intertidal Foraging Habitat Guild for Shorebirds)
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Polychaetes Associated with a Tropical Ocean Outfall: Synthesis of a Biomonitoring Program Off O'ahu, Hawai'f
Polychaetes Associated with a Tropical Ocean Outfall: Synthesis ofa Biomonitoring Program off O'ahu, Hawai'F J. H. Bailey-Brock,2,3,4,5 B. Paavo,3,4 B. M. Barrett,3,4 and J. Dreyer3,4 Abstract: A comparison of benthic polychaete communities off the Sand Island Wastewater Outfall was undertaken to recognize organic enrichment indicator species for Hawaiian waters. Primary-treatment sewage is discharged off the south shore of O'ahu at 70 m depth. A historical data set spanning 9 yr for seven sites at 70 m and two recent studies at 20, 50, and 100 m depths were analyzed. Geochemical data did not support the assumption that the outfall is an im portant source of organic enrichment in nutrient-poor sandy sediments within oligotrophic tropical waters. Five polychaete species, however, appeared partic ularly sensitive, positively or negatively, to environmental conditions near the outfall. Neanthes arenaceodentata (Nereididae) and Ophryotrocha adherens (Dor villeidae) have been dominant at sites within the outfall's zone of initial dilution (ZID). Since 1993, N arenaceodentata has virtually disappeared, and 0. adherens concurrently became abundant and continued to flourish at ZID sites. Well known indicators within the Capitella capitata complex (Capitellidae) were pres ent at ZID and control (far field) sites though their ZID abundance was greater. Two sabellids, Euchone sp. Band Augeneriella dubia were inversely distributed, the smaller Euchone sp. B at far field sites and larger A. dubia within ZID sta tions. The former was most likely restricted to a greater proportion offine sed iment particles at two far field sites. -
Mapping and Distribution of Sabella Spallanzanii in Port Phillip Bay Final
Mapping and distribution of Sabellaspallanzanii in Port Phillip Bay Final Report to Fisheries Research and Development Corporation (FRDC Project 94/164) G..D. Parry, M.M. Lockett, D.P. Crookes, N. Coleman and M.A. Sinclair May 1996 Mapping and distribution of Sabellaspallanzanii in Port Phillip Bay Final Report to Fisheries Research and Development Corporation (FRDC Project 94/164) G.D. Parry1, M. Lockett1, D. P. Crookes1, N. Coleman1 and M. Sinclair2 May 1996 1Victorian Fisheries Research Institute Departmentof Conservation and Natural Resources PO Box 114, Queenscliff,Victoria 3225 2Departmentof Ecology and Evolutionary Biology Monash University Clayton Victoria 3068 Contents Page Technical and non-technical summary 2 Introduction 3 Background 3 Need 4 Objectives 4 Methods 5 Results 5 Benefits 5 Intellectual Property 6 Further Development 6 Staff 6 Final cost 7 Distribution 7 Acknow ledgments 8 References 8 Technical and Non-technical Summary • The sabellid polychaete Sabella spallanzanii, a native to the Mediterranean, established in Port Phillip Bay in the late 1980s. Initially it was found only in Corio Bay, but during the past fiveyears it has spread so that it now occurs throughout the western half of Port Phillip Bay. • Densities of Sabella in many parts of the bay remain low but densities are usually higher (up to 13/m2 ) in deeper water and they extend into shallower depths in calmer regions. • Sabella larvae probably require a 'hard' surface (shell fragment, rock, seaweed, mollusc or sea squirt) for initial attachment, but subsequently they may use their own tube as an anchor in soft sediment . • Changes to fish communities following the establishment of Sabella were analysed using multidimensional scaling and BACI (Before, After, Control, Impact) design analyses of variance. -
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. -
Molecular Phylogeny of the Family Capitellidae (Annelida)
Title Molecular Phylogeny of the Family Capitellidae (Annelida) Author(s) Tomioka, Shinri; Kakui, Keiichi; Kajihara, Hiroshi Zoological Science, 35(5), 436-445 Citation https://doi.org/10.2108/zs180009 Issue Date 2018-10 Doc URL http://hdl.handle.net/2115/75605 Type article File Information Zoological Science35-5_436‒445(2018).pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP ZOOLOGICAL436 SCIENCE 35: 436–445 (2018) S. Tomioka et al. © 2018 Zoological Society of Japan Molecular Phylogeny of the Family Capitellidae (Annelida) Shinri Tomioka1*, Keiichi Kakui2, and Hiroshi Kajihara2 1Rishiri Town Museum, Senhoshi, Rishiri Is., Hokkaido 097-0311, Japan 2Department of Biological Sciences, Faculty of Science, Hokkaido University, N10 W8, Sapporo, Hokkaido 060-0810, Japan Capitellids have emerged as monophyletic in most but not all recent molecular phylogenies, indi- cating that more extensive taxon sampling is necessary. In addition, monophyly of most or all capitellid genera was questionable, as some diagnostic characters vary ontogenetically within individuals. We tested the monophyly of Capitellidae and eight capitellid genera using phyloge- netic analyses of combined 18S, 28S, H3, and COI gene sequences from 36 putative capitellid spe- cies. In our trees, Capitellidae formed a monophyletic sister group to Echiura, and Capitella was also monophyletic, separated by a long branch from other capitellids. Well-supported clades each containing representatives of different genera, or containing a subset of species within a genus, indicated that Barantolla, Heteromastus, and Notomastus are likely not monophyletic. We mapped three morphological characters traditionally used to define capitellid genera (head width relative to width of first segment, number of thoracic segments, and number of segments with capillary chae- tae) onto our tree. -
King George Whiting (Sillaginodes Punctatus)
Parasites of King George whiting (Sillaginodes punctatus) Name: Echinocephalus sp. (larval stage), a nematode Microhabitat: Lives in the intestinal tract Appearance: Rows of spines around the head and a single hook on the tail Pathology: Unknown Curiosity: As Echinocephalus species mature they grow more rows of spines Name: Cardicola sp., digenean flukes commonly called ‘blood fluke’ Microhabitat: Lives in the circulatory system Appearance: Adult worms are ~2mm long Pathology: Unknown Curiosity: This is the first record of these worms from King George whiting and only 2 adults have been found in over 1000 specimens examined Name: A juvenile isopod from the family Gnathiidae Microhabitat: Attaches to the gills of hosts while feeding Appearance: Small, transparent body that becomes red when feeding on blood Pathology: Unknown Curiosity: Only the larval and juvenile stages are parasitic Name: Anaclavella sillaginoides, a parasitic copepod, or ‘sea-louse’ Microhabitat: Attach to the gill arch Appearance: Small, white, circular-shaped body with long trunk-like attachment; females have a pair of egg strings Pathology: Unknown Name: A juvenile acanthocephalan from the family Polymorphidae, commonly called spiny headed worms Microhabitat: Lives in the intestinal track Appearance: Small, neck and head covered in a number of spines (can be retracted inside the body) Pathology: Unknown Curiosity: The shape of the head (proboscis) and the number of spines does not change during development Name: Polylabris sillaginae, flatworm parasites commonly called ‘gill fluke’ Microhabitat: Lives on the gills and feed on blood Appearance: Small, brown coloured worm that has two rows of microscopic clamps Pathology: Unknown. Gill flukes have been associated with anaemia in other fish hosts Further contact: A research initiative supported by: Conditions of use: ----------------------------------------------------- ----------------------------------------------------- ----------------------------------------------------- Emma L. -
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 ......................................................................... -
Onychophorology, the Study of Velvet Worms
Uniciencia Vol. 35(1), pp. 210-230, January-June, 2021 DOI: http://dx.doi.org/10.15359/ru.35-1.13 www.revistas.una.ac.cr/uniciencia E-ISSN: 2215-3470 [email protected] CC: BY-NC-ND Onychophorology, the study of velvet worms, historical trends, landmarks, and researchers from 1826 to 2020 (a literature review) Onicoforología, el estudio de los gusanos de terciopelo, tendencias históricas, hitos e investigadores de 1826 a 2020 (Revisión de la Literatura) Onicoforologia, o estudo dos vermes aveludados, tendências históricas, marcos e pesquisadores de 1826 a 2020 (Revisão da Literatura) Julián Monge-Nájera1 Received: Mar/25/2020 • Accepted: May/18/2020 • Published: Jan/31/2021 Abstract Velvet worms, also known as peripatus or onychophorans, are a phylum of evolutionary importance that has survived all mass extinctions since the Cambrian period. They capture prey with an adhesive net that is formed in a fraction of a second. The first naturalist to formally describe them was Lansdown Guilding (1797-1831), a British priest from the Caribbean island of Saint Vincent. His life is as little known as the history of the field he initiated, Onychophorology. This is the first general history of Onychophorology, which has been divided into half-century periods. The beginning, 1826-1879, was characterized by studies from former students of famous naturalists like Cuvier and von Baer. This generation included Milne-Edwards and Blanchard, and studies were done mostly in France, Britain, and Germany. In the 1880-1929 period, research was concentrated on anatomy, behavior, biogeography, and ecology; and it is in this period when Bouvier published his mammoth monograph. -
(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). -
Phylum Onychophora
Lab exercise 6: Arthropoda General Zoology Laborarory . Matt Nelson phylum onychophora Velvet worms Once considered to represent a transitional form between annelids and arthropods, the Onychophora (velvet worms) are now generally considered to be sister to the Arthropoda, and are included in chordata the clade Panarthropoda. They are no hemichordata longer considered to be closely related to echinodermata the Annelida. Molecular evidence strongly deuterostomia supports the clade Panarthropoda, platyhelminthes indicating that those characteristics which the velvet worms share with segmented rotifera worms (e.g. unjointed limbs and acanthocephala metanephridia) must be plesiomorphies. lophotrochozoa nemertea mollusca Onychophorans share many annelida synapomorphies with arthropods. Like arthropods, velvet worms possess a chitinous bilateria protostomia exoskeleton that necessitates molting. The nemata ecdysozoa also possess a tracheal system similar to that nematomorpha of insects and myriapods. Onychophorans panarthropoda have an open circulatory system with tardigrada hemocoels and a ventral heart. As in arthropoda arthropods, the fluid-filled hemocoel is the onychophora main body cavity. However, unlike the arthropods, the hemocoel of onychophorans is used as a hydrostatic acoela skeleton. Onychophorans feed mostly on small invertebrates such as insects. These prey items are captured using a special “slime” which is secreted from large slime glands inside the body and expelled through two oral papillae on either side of the mouth. This slime is protein based, sticking to the cuticle of insects, but not to the cuticle of the velvet worm itself. Secreted as a liquid, the slime quickly becomes solid when exposed to air. Once a prey item is captured, an onychophoran feeds much like a spider.