The Relationship Between Barnacles and Green Sea Turtle Health
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Marine Invertebrate Field Guide
Marine Invertebrate Field Guide Contents ANEMONES ....................................................................................................................................................................................... 2 AGGREGATING ANEMONE (ANTHOPLEURA ELEGANTISSIMA) ............................................................................................................................... 2 BROODING ANEMONE (EPIACTIS PROLIFERA) ................................................................................................................................................... 2 CHRISTMAS ANEMONE (URTICINA CRASSICORNIS) ............................................................................................................................................ 3 PLUMOSE ANEMONE (METRIDIUM SENILE) ..................................................................................................................................................... 3 BARNACLES ....................................................................................................................................................................................... 4 ACORN BARNACLE (BALANUS GLANDULA) ....................................................................................................................................................... 4 HAYSTACK BARNACLE (SEMIBALANUS CARIOSUS) .............................................................................................................................................. 4 CHITONS ........................................................................................................................................................................................... -
Using Growth Rates to Estimate Age of the Sea Turtle Barnacle Chelonibia Testudinaria
Mar Biol (2017) 164:222 DOI 10.1007/s00227-017-3251-5 SHORT NOTE Using growth rates to estimate age of the sea turtle barnacle Chelonibia testudinaria Sophie A. Doell1 · Rod M. Connolly1 · Colin J. Limpus2 · Ryan M. Pearson1 · Jason P. van de Merwe1 Received: 4 May 2017 / Accepted: 20 October 2017 © Springer-Verlag GmbH Germany 2017 Abstract Epibionts can serve as valuable ecological indi- may live for up to 2 years, means that these barnacles may cators, providing information about the behaviour or health serve as interesting ecological indicators over this period. of the host. The use of epibionts as indicators is, however, In turn, this information may be used to better understand often limited by a lack of knowledge about the basic ecology the movement and habitat use of their sea turtle hosts, ulti- of these ‘hitchhikers’. This study investigated the growth mately improving conservation and management of these rates of a turtle barnacle, Chelonibia testudinaria, under threatened animals. natural conditions, and then used the resulting growth curve to estimate the barnacle’s age. Repeat morphomet- ric measurements (length and basal area) on 78 barnacles Introduction were taken, as host loggerhead turtles (Caretta caretta) laid successive clutches at Mon Repos, Australia, during the Sea turtles are known to host diverse communities of plants 2015/16 nesting season. Barnacles when frst encountered and invertebrate animals (Caine 1986; Kitsos et al. 2005; ranged in size from 3.7 to 62.9 mm, and were recaptured Robinson et al. 2017). Past analyses of the size, abundance, between 12 and 56 days later. -
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). -
Occurrence of Sea Spider Endeis Mollis Carpenter (Arthropoda: Pycnogonida) on the Test Panels Submerged in Gulf of Mannar, Southeast Coast of India
Arthropods, 2012, 1(2):73-78 Article Occurrence of sea spider Endeis mollis Carpenter (Arthropoda: Pycnogonida) on the test panels submerged in Gulf of Mannar, southeast coast of India S. Satheesh*, S. G. Wesley Department of Zoology, Scott Christian College (Autonomous), Nagercoil-629003, Tamil Nadu, India *Present address: Department of Marine Biology, Faculty of Marine Sciences, King Abdulaziz University, Post Box No. 80207, Jeddah-21589, Saudi Arabia E-mail: [email protected] Received 27 February 2012; Accepted 1 April 2012; Published online 5 June 2012 IAEES Abstract Sea spiders (Pycnogonids) are exclusively marine arthropods with worldwide distribution. Pycnogonida remains one of the poorly investigated groups encountered in fouling communities. In the present study, distribution pycnogonid species Endeis mollis associated with the fouling community developed on test panels submerged at Kudankulam coast, Gulf of Mannar was studied for a period of two years. Throughout the period of investigation, Endeis mollis was observed on the test panels. A maximum of 55 individuals per square dm was observed during pre-monsoon season and a minimum of 9 individuals per square dm during monsoon season. Results of this study on seasonal distribution are of considerable interest because so little has been documented on the ecology of Pycnogonids in India. Keywords arthropods; biofouling; fouling community; Pycnogonids; Kudankulam; Endeis mollis; biogeography. 1 Introduction Sea spiders or pycnogonids are distinct group of arthropods, exclusively found in the intertidal to abyssal depths in all the marine waters of the world (Arango, 2003; Carranza et al., 2007; Fornshell, 2012). They are commonly found as epibenthic community on other invertebrates, algae, corals etc (Child and Harbison, 1986). -
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. -
Battle of the Barnacles
Gary Skinner Battle of the barnacles Competition on the seashore The photograph on the centre pages shows a themselves, head down, on suitable rocks, build a rock wall on a British rocky shore. It is covered shell, poke their legs out of the top of it and start to filter feed! Barnacles like this are called acorn with various intertidal animals, mainly barnacles, and they occur in mind boggling numbers barnacles. Have a good look at the image; you on most rocky beaches around the world. should be able to see barnacles of two different species and, amongst them, and even sometimes in their old shells, other animals, mainly shelled ones called molluscs. This image can be used to go on a virtual tour of this part of the rocky shore, and to see – nearly first hand – some important principles of ecology. uch of the UK coastline is rocky, and the parts washed by the sea from high Children might be doing worse at school then they otherwise would to low tide are called rocky shores. The M © Christoph Corteau/naturepl.com region between the tides is the littoral zone, home because they can’t pay attention in class after eating the colourings. A British barnacle, Semibalanus balanoides, to many species of animals and algae (but no true reveals its legs when the tide comes in. plants). A day spent searching for living creatures on a rocky shore, it is claimed, can yield creatures from Box 1 over twenty different phyla (singular phylum; see What is a phylum? Box 1).