Spawning and Larval Development of the Black Turban Snail Tegula Funebralis (Prosobranchia: Trochidae)
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GASTROPOD CARE SOP# = Moll3 PURPOSE: to Describe Methods Of
GASTROPOD CARE SOP# = Moll3 PURPOSE: To describe methods of care for gastropods. POLICY: To provide optimum care for all animals. RESPONSIBILITY: Collector and user of the animals. If these are not the same person, the user takes over responsibility of the animals as soon as the animals have arrived on station. IDENTIFICATION: Common Name Scientific Name Identifying Characteristics Blue topsnail Calliostoma - Whorls are sculptured spirally with alternating ligatum light ridges and pinkish-brown furrows - Height reaches a little more than 2cm and is a bit greater than the width -There is no opening in the base of the shell near its center (umbilicus) Purple-ringed Calliostoma - Alternating whorls of orange and fluorescent topsnail annulatum purple make for spectacular colouration - The apex is sharply pointed - The foot is bright orange - They are often found amongst hydroids which are one of their food sources - These snails are up to 4cm across Leafy Ceratostoma - Spiral ridges on shell hornmouth foliatum - Three lengthwise frills - Frills vary, but are generally discontinuous and look unfinished - They reach a length of about 8cm Rough keyhole Diodora aspera - Likely to be found in the intertidal region limpet - Have a single apical aperture to allow water to exit - Reach a length of about 5 cm Limpet Lottia sp - This genus covers quite a few species of limpets, at least 4 of them are commonly found near BMSC - Different Lottia species vary greatly in appearance - See Eugene N. Kozloff’s book, “Seashore Life of the Northern Pacific Coast” for in depth descriptions of individual species Limpet Tectura sp. - This genus covers quite a few species of limpets, at least 6 of them are commonly found near BMSC - Different Tectura species vary greatly in appearance - See Eugene N. -
Paleoenvironmental Interpretation of Late Glacial and Post
PALEOENVIRONMENTAL INTERPRETATION OF LATE GLACIAL AND POST- GLACIAL FOSSIL MARINE MOLLUSCS, EUREKA SOUND, CANADIAN ARCTIC ARCHIPELAGO A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geography University of Saskatchewan Saskatoon By Shanshan Cai © Copyright Shanshan Cai, April 2006. All rights reserved. i PERMISSION TO USE In presenting this thesis in partial fulfillment of the requirements for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Geography University of Saskatchewan Saskatoon, Saskatchewan S7N 5A5 i ABSTRACT A total of 5065 specimens (5018 valves of bivalve and 47 gastropod shells) have been identified and classified into 27 species from 55 samples collected from raised glaciomarine and estuarine sediments, and glacial tills. -
Biodiversity Journal, 2021, 12 (1): 225–228
Biodiversity Journal, 2021, 12 (1): 225–228 https://doi.org/10.31396/Biodiv.Jour.2021.12.4.225.228 First record of Calliostoma lusitanicum F. Nordsieck et García- Talavera, 1979 (Gastropoda Calliostomatiidae) in the Mediter- ranean Sea and remarks on C. alexandrinum Pallary, 1912 Andrea Nappo1*, Daniel Pellegrini2 & Attilio Pagli3 1Via S’Arrulloni 25, 09045 Quartu Sant’Elena, Cagliari, Italy; e-mail: [email protected] 2Via Colle Morello 2, 00038 Valmontone, Roma, Italy; e-mail: [email protected] 3Via Valdorme 55, 50053 Empoli, Firenze, Italy; e-mail: [email protected] *Corresponding author ABSTRACT In this work is reported for the first time the presence of Calliostoma lusitanicum F. Nordsieck et García-Talavera, 1979 (Gastropoda Calliostomatiidae) in the Mediterranean Sea. Present sightings widen the known distribution of this species, found in the Madeira Archipelago and Canary Islands. The relationship between C. lusitanicum and C. alexandrinum Pallary, 1912 is discussed. KEY WORDS Calliostoma lusitanicum; Calliostomatiidae; Mollusca; Mediterranean Sea. Received 08.11.2020; accepted 26.02.2021; published online 15.03.2021 INTRODUCTION as shell height. Photos are obtained with a Nikon D90 and processed with Adobe Photoshop CC®. According to WoRMS (accessed on ABBREVIATIONS AND ACRONYMS. The 14.10.2020), 291 re cent species are currently placed following abbreviations and acronyms are used: in the genus Calliostoma Swainson, 1840 (Gas- AN: Andrea Nappo collection (Quartu Sant’Elena, tropoda Calliostomatiidae) with a worldwide distri- Cagliari, Italy); AP: Attilio Pagli collection (Em- bution. In the Medi terranean Sea, according to the poli, Firenze, Italy); DP: Daniel Pellegrini collec- systematic list of the SIM (Italian Society of Mala- tion (Valmontone, Roma, Italy); MNHN: Muséum cology) (accessed 14.10.2020), 11 species are pres- National d’Histoire Naturelle (Paris, France); SIM: ent. -
WMSDB - Worldwide Mollusc Species Data Base
WMSDB - Worldwide Mollusc Species Data Base Family: TURBINIDAE Author: Claudio Galli - [email protected] (updated 07/set/2015) Class: GASTROPODA --- Clade: VETIGASTROPODA-TROCHOIDEA ------ Family: TURBINIDAE Rafinesque, 1815 (Sea) - Alphabetic order - when first name is in bold the species has images Taxa=681, Genus=26, Subgenus=17, Species=203, Subspecies=23, Synonyms=411, Images=168 abyssorum , Bolma henica abyssorum M.M. Schepman, 1908 aculeata , Guildfordia aculeata S. Kosuge, 1979 aculeatus , Turbo aculeatus T. Allan, 1818 - syn of: Epitonium muricatum (A. Risso, 1826) acutangulus, Turbo acutangulus C. Linnaeus, 1758 acutus , Turbo acutus E. Donovan, 1804 - syn of: Turbonilla acuta (E. Donovan, 1804) aegyptius , Turbo aegyptius J.F. Gmelin, 1791 - syn of: Rubritrochus declivis (P. Forsskål in C. Niebuhr, 1775) aereus , Turbo aereus J. Adams, 1797 - syn of: Rissoa parva (E.M. Da Costa, 1778) aethiops , Turbo aethiops J.F. Gmelin, 1791 - syn of: Diloma aethiops (J.F. Gmelin, 1791) agonistes , Turbo agonistes W.H. Dall & W.H. Ochsner, 1928 - syn of: Turbo scitulus (W.H. Dall, 1919) albidus , Turbo albidus F. Kanmacher, 1798 - syn of: Graphis albida (F. Kanmacher, 1798) albocinctus , Turbo albocinctus J.H.F. Link, 1807 - syn of: Littorina saxatilis (A.G. Olivi, 1792) albofasciatus , Turbo albofasciatus L. Bozzetti, 1994 albofasciatus , Marmarostoma albofasciatus L. Bozzetti, 1994 - syn of: Turbo albofasciatus L. Bozzetti, 1994 albulus , Turbo albulus O. Fabricius, 1780 - syn of: Menestho albula (O. Fabricius, 1780) albus , Turbo albus J. Adams, 1797 - syn of: Rissoa parva (E.M. Da Costa, 1778) albus, Turbo albus T. Pennant, 1777 amabilis , Turbo amabilis H. Ozaki, 1954 - syn of: Bolma guttata (A. Adams, 1863) americanum , Lithopoma americanum (J.F. -
Phylum MOLLUSCA
285 MOLLUSCA: SOLENOGASTRES-POLYPLACOPHORA Phylum MOLLUSCA Class SOLENOGASTRES Family Lepidomeniidae NEMATOMENIA BANYULENSIS (Pruvot, 1891, p. 715, as Dondersia) Occasionally on Lafoea dumosa (R.A.T., S.P., E.J.A.): at 4 positions S.W. of Eddystone, 42-49 fm., on Lafoea dumosa (Crawshay, 1912, p. 368): Eddystone, 29 fm., 1920 (R.W.): 7, 3, 1 and 1 in 4 hauls N.E. of Eddystone, 1948 (V.F.) Breeding: gonads ripe in Aug. (R.A.T.) Family Neomeniidae NEOMENIA CARINATA Tullberg, 1875, p. 1 One specimen Rame-Eddystone Grounds, 29.12.49 (V.F.) Family Proneomeniidae PRONEOMENIA AGLAOPHENIAE Kovalevsky and Marion [Pruvot, 1891, p. 720] Common on Thecocarpus myriophyllum, generally coiled around the base of the stem of the hydroid (S.P., E.J.A.): at 4 positions S.W. of Eddystone, 43-49 fm. (Crawshay, 1912, p. 367): S. of Rame Head, 27 fm., 1920 (R.W.): N. of Eddystone, 29.3.33 (A.J.S.) Class POLYPLACOPHORA (=LORICATA) Family Lepidopleuridae LEPIDOPLEURUS ASELLUS (Gmelin) [Forbes and Hanley, 1849, II, p. 407, as Chiton; Matthews, 1953, p. 246] Abundant, 15-30 fm., especially on muddy gravel (S.P.): at 9 positions S.W. of Eddystone, 40-43 fm. (Crawshay, 1912, p. 368, as Craspedochilus onyx) SALCOMBE. Common in dredge material (Allen and Todd, 1900, p. 210) LEPIDOPLEURUS, CANCELLATUS (Sowerby) [Forbes and Hanley, 1849, II, p. 410, as Chiton; Matthews. 1953, p. 246] Wembury West Reef, three specimens at E.L.W.S.T. by J. Brady, 28.3.56 (G.M.S.) Family Lepidochitonidae TONICELLA RUBRA (L.) [Forbes and Hanley, 1849, II, p. -
Diet Composition of Cod (Gadus Morhua): Small-Scale Differences in a Sub-Arctic Fjord
Diet composition of cod (Gadus morhua): small-scale differences in a sub-arctic fjord Enoksen, Siri Elise BI309F MSc IN MARINE ECOLOGY Faculty for Biosciences and Aquaculture May 2015 Acknowledgements The presented thesis is the final part of a two-year Master of Science program at the Faculty of Biosciences and Aquaculture, University of Nordland, Bodø, Norway. I owe my supervisor Associate Professor Henning Reiss eternal gratitude for his patience and all the help with sampling, species determination and writing of this thesis. Without his expertise and guidance, this master thesis would not have been possible. A special thanks to Bjørn Tore Zahl at Saltstraumen Brygge, Geir Jøran Nyheim at Saltstraumen camping, Lill-Anita Stenersen at Kafe Kjelen, Fauske Båtforening and Saltdal Båtforening for helping during sampling, Coop Extra Bygg Fauske for sponsoring sheds for collecting stations, and to all anglers who handed inn samples. This project would not have been possible without their help. I would like to thank Professor Truls Moum, Martina Kopp, Vigdis Edvardsen, Tor Erik Jørgensen and Teshome Tilahun Bizuayehu for help and guidance during DNA barcoding analysis. I thank Nina Tande Hansen and Bibbi Myrvoll at Karrieresenteret Indre Salten for believing in me and convincing me that I was capable of studying at university level. This thesis would not have been possible without their guidance. I would also like to thank my family for their patience during the five years of fulfilling my Master. i Table of contents Acknowledgements ......................................................................................................................... -
Mollusks of Manuel Antonio National Park, Pacific Costa Rica
Rev. Biol. Trop. 49. Supl. 2: 25-36, 2001 www.rbt.ac.cr, www.ucr.ac.cr Mollusks of Manuel Antonio National Park, Pacific Costa Rica Samuel Willis 1 and Jorge Cortés 2-3 1140 East Middle Street, Gettysburg, Pennsylvania 17325, USA. 2Centro de Investigación en Ciencias del Mar y Limnología (CIMAR), Universidad de Costa Rica, 2060 San José, Costa Rica. FAX: (506) 207-3280. E-mail: [email protected] 3Escuela de Biología, Universidad de Costa Rica, 2060 San José, Costa Rica. (Received 14-VII-2000. Corrected 23-III-2001. Accepted 11-V-2001) Abstract: The mollusks in Manuel Antonio National Park on the central section of the Pacific coast of Costa Rica were studied along thirty-six transects done perpendicular to the shore, and by random sampling of subtidal environments, beaches and mangrove forest. Seventy-four species of mollusks belonging to three classes and 40 families were found: 63 gastropods, 9 bivalves and 2 chitons, during this study in 1995. Of these, 16 species were found only as empty shells (11) or inhabited by hermit crabs (5). Forty-eight species were found at only one locality. Half the species were found at one site, Puerto Escondido. The most diverse habitat was the low rocky intertidal zone. Nodilittorina modesta was present in 34 transects and Nerita scabricosta in 30. Nodilittorina aspera had the highest density of mollusks in the transects. Only four transects did not clustered into the four main groups. The species composition of one cluster of transects is associated with a boulder substrate, while another cluster of transects associates with site. -
Erminlo Caprotti F) L Avole Propriamente Nei Vasti Ammassi Di
\ \ Erminlo Caprotti MOLLUSCHI DEL TABIANIANO (PLIOCENE INFERIORE) DELLA VAL D'ARDA. LORO CONNESSIONI TEMPORALI E SPAZIALI. Gebun und GÈb, Èir cwias Mc.r. - F'n we.-hselnd W€hén Èin slUhcnd t2ben: So schatf ich .m sausendeù WcE sruhl de. z.n Und{i.ke dér Gonhéir lebendig.s (W. C@thé, Faust, I, Nacht) A) Introduzione B) Composizione della fauna e comparazioni - Le associazioni , dominanti C) Origine e divenire D) Descrizioni paleontologiche E) Nota bibliografica F) l avole A) INTRODUZIONE Questo lavoro studia i molluschi reperiti dall'Autore con sue per- sonali ricerche nel Tabianiano (Pliocene inferiore) della Val d'Arda, in provincia di Piacenza. La ricerca e la raccolta del materiale è stata ef- fettuata sulla riva destra dell'Arda nei pressi di Lugagnano, e Piir propriamente nei vasti ammassi di argille azzure che si stendono dall'Arda verso il paese di Vernasca (Foglio I.G.M. n. 72 II N.E.). In particolare le due zone di raccolta, oggetto di questo studio, sono topograficamente racchiuse tm quota 208 (Case Micelli presso la riva destra dell'Arda) e quota 300 circa. Si tratta di un grande ammasso di argille azzurre, situato ad Est ed a Sud-Est della fornace per late- rizi di Lugagnano. Topograficamente sovrapposte a queste argille si trovano sabbie basali del Pliocene inferiore variate con intercalazioni marmose, sab- bie medie e grossolane, marne grigio chiare, sabbie argillo§e, argille marmoso-sabbiose. Da esse non sono stati prelevati che scarsi fram_ menti di molluschi e pertanto queste non fanno oggetto di questo Iavoro. Queste sabbie sooo stratigraficamente sottoposte alle argille prese qui in esame, mentre dal punto di vista topografico esse si e' stcndono fin quasi al paese di Veanasca. -
554 Journal of Paleontology, V. 66, No. 4, 1992 Figure 9
554 JOURNAL OF PALEONTOLOGY, V. 66, NO. 4, 1992 FIGURE 9—Crepidula adunca encrusting living Calliostoma ligatum, Friday Harbor, Washington, shell height of C. ligatum, 21.0 mm, UCMP Type No. 39688. 1, two C. adunca conforming to upper whorls of C. ligatum; 2, C. adunca permanent scar on last whorl of hermitted C. ligatum, shell height, 22.0 mm, UCMP Type No. 39689. 1979). Other species also compete for, or inhabit, gastropod (Hyden and Forest, 1980). However, the shell-encrusting and shells (McLean, 1983; Vermeij, 1987; Walker, 1990). Because boring organisms that occur with hermit crabs have a long fossil empty shells may be rare, post-Triassic gastropod fossil assem- record, dating from the middle Jurassic. Determining the extent blages have most likely been taphonomically affected by sec- of hermitted shells in fossil assemblages should be the first line ondary occupants of shells. Because hermit crab modification of inquiry before paleoecological or evolutionary assessments of gastropod assemblages is great, Shimoyama et al. (1979) sug- are made. gested that the bivalve fossil record provided a more accurate Pagurized shells can be recognized by the settlement of bionts paleoecological record than gastropod assemblages. However, in specific locations on fossil shells (Palmer and Hancock, 1973; gastropod fossil assemblages provide valuable paleoecological Walker, 1988b, 1989, this paper). Recent and fossil biont pat- information for the history of the hermit crab. terns appear to be conservative from the Oligocene to the pres- Hermit crab body fossils are rare. Therefore, it is important ent. That is, taphonomically preserved biont patterns (e.g., east to study their other fossil record: that of the epi- and endobionts Gulf Coast examples) are similar to Recent pagurized shells. -
The Biology of Seashores - Image Bank Guide All Images and Text ©2006 Biomedia ASSOCIATES
The Biology of Seashores - Image Bank Guide All Images And Text ©2006 BioMEDIA ASSOCIATES Shore Types Low tide, sandy beach, clam diggers. Knowing the Low tide, rocky shore, sandstone shelves ,The time and extent of low tides is important for people amount of beach exposed at low tide depends both on who collect intertidal organisms for food. the level the tide will reach, and on the gradient of the beach. Low tide, Salt Point, CA, mixed sandstone and hard Low tide, granite boulders, The geology of intertidal rock boulders. A rocky beach at low tide. Rocks in the areas varies widely. Here, vertical faces of exposure background are about 15 ft. (4 meters) high. are mixed with gentle slopes, providing much variation in rocky intertidal habitat. Split frame, showing low tide and high tide from same view, Salt Point, California. Identical views Low tide, muddy bay, Bodega Bay, California. of a rocky intertidal area at a moderate low tide (left) Bays protected from winds, currents, and waves tend and moderate high tide (right). Tidal variation between to be shallow and muddy as sediments from rivers these two times was about 9 feet (2.7 m). accumulate in the basin. The receding tide leaves mudflats. High tide, Salt Point, mixed sandstone and hard rock boulders. Same beach as previous two slides, Low tide, muddy bay. In some bays, low tides expose note the absence of exposed algae on the rocks. vast areas of mudflats. The sea may recede several kilometers from the shoreline of high tide Tides Low tide, sandy beach. -
The Foocal Pellets of the Trochidoo
[ 235 ] The Foocal Pellets of the Trochidoo. By Hilary B. Moore, B.Se., Zoologist at the Marine Station, Port Erin, I.a.M. With 12 Figures in the Text. FlECALPELLETSof the following species are described :- Gibbula cineraria (Linn.). G. umbilicalis (Da Costa). G. tumida (Montagu). G. magus (Linn.). Oantharus (Jujubinus) clelandi (Wood). Oalliostomazizyphinum (Linn.). Of the various molluscan frecalpellets so far described, none have shown a very high degree either of internal differentiation, or of external sculp- turing. In the latter respect the most complicated are perhaps those of the Nuculidre (Moore, 1) and the Pectinidre (Moore,2). In neither of these groups is there any trace of internal localisation of different types of material, but in the Mytilidre (Moore, 2) there is, in some species, a sorting of the finer material to the lateral regions of the frecal ribbon, and of the courser material to the centre. There is not however any clear-cut line of demarcation between the two regions. In the present group there is, in all the species described except Oalliostomazizyphinum, a localisation of the constituent materials accord- ing to their grade into certain definite regions of the pellet; and there is further, in all except Calliostoma, a very complex system of surface sculpturing. The pellets of Gibbula umbilicalis and G. cineraria may frequently be seen on the shore, where their peculiar shape makes them easily recognis- able. Moorhouse (3), speaking of Trochus niloticus from Low Isles, on the Great Barrier Reef, says: "Feeding appears to proceed at every opportunity, so that the amount of frecal matter deposited is very great. -
Marine Ecology Progress Series 615:31
Vol. 615: 31–49, 2019 MARINE ECOLOGY PROGRESS SERIES Published April 18 https://doi.org/10.3354/meps12923 Mar Ecol Prog Ser OPENPEN ACCESSCCESS Food sources of macrozoobenthos in an Arctic kelp belt: trophic relationships revealed by stable isotope and fatty acid analyses M. Paar1,5,*, B. Lebreton2, M. Graeve3, M. Greenacre4, R. Asmus1, H. Asmus1 1Wattenmeerstation Sylt, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Hafenstraße 43, 25992 List/Sylt, Germany 2UMR 7266 Littoral, Environment and Societies, Institut du littoral et de l’environnement, CNRS-University of La Rochelle, 2 rue Olympes de Gouges, 17000 La Rochelle, France 3Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Am Handelshafen 12, 27570 Bremerhaven, Germany 4Department of Economics and Business, Universitat Pompeu Fabra and Barcelona Graduate School of Economics, Ramon Trias Fargas, 25-27, 08005 Barcelona, Spain 5Present address: Biologische Station Hiddensee, Universität Greifswald, Biologenweg 15, 18565 Kloster, Germany ABSTRACT: Arctic kelp belts, made of large perennial macroalgae of the order Laminariales, are expanding because of rising temperatures and reduced sea ice cover of coastal waters. In summer 2013, the trophic relationships within a kelp belt food web in Kongsfjorden (Spitsbergen) were determined using fatty acid and stable isotope analyses. Low relative proportions of Phaeophyta fatty acid trophic markers (i.e. 20:4(n-6), 18:3(n-3) and 18:2(n-6)) in consumers (3.3−8.9%), as well as low 20:4(n-6)/20:5(n-3) ratios (<0.1−0.6), indicated that Phaeophyta were poorly used by macro- zoobenthos as a food source, either fresh or as detritus.