Case 3211 CLIONIDAE D'orbigny, 1851
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Metabolic Response of Antarctic Pteropods (Mollusca: Gastropoda) to Food Deprivation and Regional Productivity
Vol. 441: 129–139, 2011 MARINE ECOLOGY PROGRESS SERIES Published November 15 doi: 10.3354/meps09358 Mar Ecol Prog Ser Metabolic response of Antarctic pteropods (Mollusca: Gastropoda) to food deprivation and regional productivity Amy E. Maas1,*, Leanne E. Elder1, Heidi M. Dierssen2, Brad A. Seibel1 1Department of Biological Sciences, University of Rhode Island, Kingston, Rhode Island 02881, USA 2Department of Marine Sciences, University of Connecticut, Groton, Connecticut 06340, USA ABSTRACT: Pteropods are an abundant group of pelagic gastropods that, although temporally and spatially patchy in the Southern Ocean, can play an important role in food webs and biochem- ical cycles. We found that the metabolic rate in Limacina helicina antarctica is depressed (~23%) at lower mean chlorophyll a (chl a) concentrations in the Ross Sea. To assess the specific impact of food deprivation on these animals, we quantified aerobic respiration and ammonia (NH3) produc- tion for 2 dominant Antarctic pteropods, L. helicina antarctica and Clione limacina antarctica. Pteropods collected from sites west of Ross Island, Antarctica were held in captivity for a period of 1 to 13 d to determine their metabolic response to laboratory-induced food deprivation. L. helicina antarctica reduced oxygen consumption by ~20% after 4 d in captivity. Ammonia excretion was not significantly affected, suggesting a greater reliance on protein as a substrate for cellular res- piration during starvation. The oxygen consumption rate of the gymnosome, C. li macina antarc- tica, was reduced by ~35% and NH3 excretion by ~55% after 4 d without prey. Our results indi- cate that there is a link between the large scale chl a concentrations of the Ross Sea and the baseline metabolic rate of pteropods which impacts these animals across multiple seasons. -
Life Cycle and Early Development of the Thecosomatous Pteropod Limacina Retroversa in the Gulf of Maine, Including the Effect of Elevated CO2 Levels
Life cycle and early development of the thecosomatous pteropod Limacina retroversa in the Gulf of Maine, including the effect of elevated CO2 levels Ali A. Thabetab, Amy E. Maasac*, Gareth L. Lawsona and Ann M. Tarranta a. Biology Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543 b. Zoology Dept., Faculty of Science, Al-Azhar University in Assiut, Assiut, Egypt. c. Bermuda Institute of Ocean Sciences, St. George’s GE01, Bermuda *Corresponding Author, equal contribution with lead author Email: [email protected] Phone: 441-297-1880 x131 Keywords: mollusc, ocean acidification, calcification, mortality, developmental delay Abstract Thecosome pteropods are pelagic molluscs with aragonitic shells. They are considered to be especially vulnerable among plankton to ocean acidification (OA), but to recognize changes due to anthropogenic forcing a baseline understanding of their life history is needed. In the present study, adult Limacina retroversa were collected on five cruises from multiple sites in the Gulf of Maine (between 42° 22.1’–42° 0.0’ N and 69° 42.6’–70° 15.4’ W; water depths of ca. 45–260 m) from October 2013−November 2014. They were maintained in the laboratory under continuous light at 8° C. There was evidence of year-round reproduction and an individual life span in the laboratory of 6 months. Eggs laid in captivity were observed throughout development. Hatching occurred after 3 days, the veliger stage was reached after 6−7 days, and metamorphosis to the juvenile stage was after ~ 1 month. Reproductive individuals were first observed after 3 months. Calcein staining of embryos revealed calcium storage beginning in the late gastrula stage. -
Validation of Holoplanktonic Molluscan Taxa from the Oligo- Miocene of the Maltese Archipelago, Introduced in Violation with ICZN Regulations
Cainozoic Research, 9(2), pp. 189-191, December 2012 ! ! ! Validation of holoplanktonic molluscan taxa from the Oligo- Miocene of the Maltese Archipelago, introduced in violation with ICZN regulations Arie W. Janssen Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, The Netherlands; currently: 12 Triq tal’Hamrija, Xewkija XWK 9033, Gozo, Malta; email: [email protected] Received 29 August 2012, accepted 6 September 2012 Five gymnosomatous molluscan taxa were recently introduced applying ‘open generic nomenclature’ by using the indication ‘Genus Clionidarum’ instead of a formal genus name and therefore violating ICZN art. 11.9.3 of the Code. Herein those taxa are validated by placing them in the type genus of the family Clionidae, followed by a question mark indicating here that they might as well belong to any other of the known (or as yet unknown) genera in the family Clionidae . Introduction Clionidarum’ as used in my paper indeed cannot be con- sidered to be an unambiguous genus name. In my study of Maltese fossil holoplanktonic molluscs I herewith validate the new names by combining them with (Janssen, 2012) a number of new species of gymnosoma- the unambiguous genus name Clione, followed by a ques- tous larval shells were introduced, more or less resembling tion mark, indicating here that those species might as well the few Recent larval shells known from this group of Gas- belong to any other known or unknown genus in the tropoda, but obviously (also considering their ages) repre- Clionidae. senting undescribed species. Recent Gymnosomata are RGM-registration numbers refer to the collections of Natu- shell-less in the adult stage, and their larval shell is shed at ralis Biodiversity Center, Palaeontology Department (Lei- metamorphosis from larva to adult. -
The 17Th International Colloquium on Amphipoda
Biodiversity Journal, 2017, 8 (2): 391–394 MONOGRAPH The 17th International Colloquium on Amphipoda Sabrina Lo Brutto1,2,*, Eugenia Schimmenti1 & Davide Iaciofano1 1Dept. STEBICEF, Section of Animal Biology, via Archirafi 18, Palermo, University of Palermo, Italy 2Museum of Zoology “Doderlein”, SIMUA, via Archirafi 16, University of Palermo, Italy *Corresponding author, email: [email protected] th th ABSTRACT The 17 International Colloquium on Amphipoda (17 ICA) has been organized by the University of Palermo (Sicily, Italy), and took place in Trapani, 4-7 September 2017. All the contributions have been published in the present monograph and include a wide range of topics. KEY WORDS International Colloquium on Amphipoda; ICA; Amphipoda. Received 30.04.2017; accepted 31.05.2017; printed 30.06.2017 Proceedings of the 17th International Colloquium on Amphipoda (17th ICA), September 4th-7th 2017, Trapani (Italy) The first International Colloquium on Amphi- Poland, Turkey, Norway, Brazil and Canada within poda was held in Verona in 1969, as a simple meet- the Scientific Committee: ing of specialists interested in the Systematics of Sabrina Lo Brutto (Coordinator) - University of Gammarus and Niphargus. Palermo, Italy Now, after 48 years, the Colloquium reached the Elvira De Matthaeis - University La Sapienza, 17th edition, held at the “Polo Territoriale della Italy Provincia di Trapani”, a site of the University of Felicita Scapini - University of Firenze, Italy Palermo, in Italy; and for the second time in Sicily Alberto Ugolini - University of Firenze, Italy (Lo Brutto et al., 2013). Maria Beatrice Scipione - Stazione Zoologica The Organizing and Scientific Committees were Anton Dohrn, Italy composed by people from different countries. -
An Overview of the Fossil Record of Pteropoda (Mollusca, Gastropoda, Heterobranchia)
Cainozoic Research, 17(1), pp. 3-10 June 2017 3 An overview of the fossil record of Pteropoda (Mollusca, Gastropoda, Heterobranchia) Arie W. Janssen1 & Katja T.C.A. Peijnenburg2, 3 1 Naturalis Biodiversity Center, Marine Biodiversity, Fossil Mollusca, P.O. Box 9517, 2300 RA Leiden, The Nether lands; [email protected] 2 Naturalis Biodiversity Center, Marine Biodiversity, P.O. Box 9517, 2300 RA Leiden, The Netherlands; Katja.Peijnen [email protected] 3 Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, P.O. Box 94248, 1090 GE Am sterdam, The Netherlands. Manuscript received 23 January 2017, revised version accepted 14 March 2017 Based on the literature and on a massive collection of material, the fossil record of the Pteropoda, an important group of heterobranch marine, holoplanktic gastropods occurring from the late Cretaceous onwards, is broadly outlined. The vertical distribution of genera is illustrated in a range chart. KEY WORDS: Pteropoda, Euthecosomata, Pseudothecosomata, Gymnosomata, fossil record Introduction Thecosomata Mesozoic Much current research focusses on holoplanktic gastro- pods, in particular on the shelled pteropods since they The sister group of pteropods is now considered to belong are proposed as potential bioindicators of the effects of to Anaspidea, a group of heterobranch gastropods, based ocean acidification e.g.( Bednaršek et al., 2016). This on molecular evidence (Klussmann-Kolb & Dinapoli, has also led to increased interest in delimiting spe- 2006; Zapata et al., 2014). The first known species of cies boundaries and distribution patterns of pteropods pteropods in the fossil record belong to the Limacinidae, (e.g. Maas et al., 2013; Burridge et al., 2015; 2016a) and are characterised by sinistrally coiled, aragonitic and resolving their evolutionary history using molecu- shells. -
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. -
Proposal for a Revised Classification of the Demospongiae (Porifera) Christine Morrow1 and Paco Cárdenas2,3*
Morrow and Cárdenas Frontiers in Zoology (2015) 12:7 DOI 10.1186/s12983-015-0099-8 DEBATE Open Access Proposal for a revised classification of the Demospongiae (Porifera) Christine Morrow1 and Paco Cárdenas2,3* Abstract Background: Demospongiae is the largest sponge class including 81% of all living sponges with nearly 7,000 species worldwide. Systema Porifera (2002) was the result of a large international collaboration to update the Demospongiae higher taxa classification, essentially based on morphological data. Since then, an increasing number of molecular phylogenetic studies have considerably shaken this taxonomic framework, with numerous polyphyletic groups revealed or confirmed and new clades discovered. And yet, despite a few taxonomical changes, the overall framework of the Systema Porifera classification still stands and is used as it is by the scientific community. This has led to a widening phylogeny/classification gap which creates biases and inconsistencies for the many end-users of this classification and ultimately impedes our understanding of today’s marine ecosystems and evolutionary processes. In an attempt to bridge this phylogeny/classification gap, we propose to officially revise the higher taxa Demospongiae classification. Discussion: We propose a revision of the Demospongiae higher taxa classification, essentially based on molecular data of the last ten years. We recommend the use of three subclasses: Verongimorpha, Keratosa and Heteroscleromorpha. We retain seven (Agelasida, Chondrosiida, Dendroceratida, Dictyoceratida, Haplosclerida, Poecilosclerida, Verongiida) of the 13 orders from Systema Porifera. We recommend the abandonment of five order names (Hadromerida, Halichondrida, Halisarcida, lithistids, Verticillitida) and resurrect or upgrade six order names (Axinellida, Merliida, Spongillida, Sphaerocladina, Suberitida, Tetractinellida). Finally, we create seven new orders (Bubarida, Desmacellida, Polymastiida, Scopalinida, Clionaida, Tethyida, Trachycladida). -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
Xoimi AMERICAN COXCIIOLOGY
S31ITnS0NIAN MISCEllANEOUS COLLECTIOXS. BIBLIOGIIAPHY XOimi AMERICAN COXCIIOLOGY TREVIOUS TO THE YEAR 18G0. PREPARED FOR THE SMITHSONIAN INSTITUTION BY . W. G. BINNEY. PART II. FOKEIGN AUTHORS. WASHINGTON: SMITHSONIAN INSTITUTION. JUNE, 1864. : ADYERTISEMENT, The first part of the Bibliography of American Conchology, prepared for the Smithsonian Institution by Mr. Binuey, was published in March, 1863, and embraced the references to de- scriptions of shells by American authors. The second part of the same work is herewith presented to the public, and relates to species of North American shells referred to by European authors. In foreign works binomial authors alone have been quoted, and no species mentioned which is not referred to North America or some specified locality of it. The third part (in an advanced stage of preparation) will in- clude the General Index of Authors, the Index of Generic and Specific names, and a History of American Conchology, together with any additional references belonging to Part I and II, that may be met with. JOSEPH HENRY, Secretary S. I. Washington, June, 1864. (" ) PHILADELPHIA COLLINS, PRINTER. CO]^TENTS. Advertisement ii 4 PART II.—FOREIGN AUTHORS. Titles of Works and Articles published by Foreign Authors . 1 Appendix II to Part I, Section A 271 Appendix III to Part I, Section C 281 287 Appendix IV .......... • Index of Authors in Part II 295 Errata ' 306 (iii ) PART II. FOEEIGN AUTHORS. ( V ) BIBLIOGRxVPHY NOETH AMERICAN CONCHOLOGY. PART II. Pllipps.—A Voyage towards the North Pole, &c. : by CON- STANTiNE John Phipps. Loudou, ITTJc. Pa. BIBLIOGRAPHY OF [part II. FaliricillS.—Fauna Grcenlandica—systematice sistens ani- malia GrcEulandite occidentalis liactenus iudagata, &c., secun dum proprias observatioues Othonis Fabricii. -
Distribution Patterns of Pelagic Gastropods at the Cape Verde Islands Holger Ossenbrügger
Distribution patterns of pelagic gastropods at the Cape Verde Islands Holger Ossenbrügger* Semester thesis 2010 *GEOMAR | Helmholtz Centre for Ocean Research Kiel Marine Ecology | Evolutionary Ecology of Marine Fishes Düsternbrooker Weg 20 | 24105 Kiel | Germany Contact: [email protected] Contents 1. Introduction . .2 1.1. Pteropods . 2 1.2. Heteropods . 3 1.3. Hydrography . 4 2. Material and Methods . 5 3. Results and Discussion . 7 3.1. Pteropods . 7 3.1.1. Species Composition . 7 3.1.2. Spatial Density Distribution near Senghor Seamount . .. 9 3.1.3. Diel Vertical Migration . 11 3.2. Heteropods . 17 3.2.1. Species Composition . .17 3.2.2. Spatial Density Distribution near Senghor Seamount . .17 3.2.3. Diel Vertical Migration . 18 4. Summary and directions for future research . 19 References . 20 Acknowledgements . 21 Attachment . .22 1. Introduction 1.1. Pteropods Pteropods belong to the phylum of the Mollusca. They are part of the class Gastropoda and located in the order Ophistobranchia. The pteropods are divided into the orders Thecosomata and Gymnosomata. They are small to medium sized animals, ranging from little more than 1mm for example in many members of the Genus Limacina to larger species such as Cymbulia peroni, which reaches a pseudoconch length of 65mm. The mostly shell bearing Thecosomata are known from about 74 recent species worldwide and are divided into five families. The Limacinidae are small gastropods with a sinistrally coiled shell; they can completely retract their body into the shell. Seven recent species of the genus Limacina are known. The Cavoliniidae is the largest of the thecosomate families with about 47 species with quite unusually formed shells. -
Canada's Arctic Marine Atlas
CANADA’S ARCTIC MARINE ATLAS This Atlas is funded in part by the Gordon and Betty Moore Foundation. I | Suggested Citation: Oceans North Conservation Society, World Wildlife Fund Canada, and Ducks Unlimited Canada. (2018). Canada’s Arctic Marine Atlas. Ottawa, Ontario: Oceans North Conservation Society. Cover image: Shaded Relief Map of Canada’s Arctic by Jeremy Davies Inside cover: Topographic relief of the Canadian Arctic This work is licensed under the Creative Commons Attribution-NonCommercial 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc/4.0 or send a letter to Creative Commons, PO Box 1866, Mountain View, CA 94042, USA. All photographs © by the photographers ISBN: 978-1-7752749-0-2 (print version) ISBN: 978-1-7752749-1-9 (digital version) Library and Archives Canada Printed in Canada, February 2018 100% Carbon Neutral Print by Hemlock Printers © 1986 Panda symbol WWF-World Wide Fund For Nature (also known as World Wildlife Fund). ® “WWF” is a WWF Registered Trademark. Background Image: Phytoplankton— The foundation of the oceanic food chain. (photo: NOAA MESA Project) BOTTOM OF THE FOOD WEB The diatom, Nitzschia frigida, is a common type of phytoplankton that lives in Arctic sea ice. PHYTOPLANKTON Natural history BOTTOM OF THE Introduction Cultural significance Marine phytoplankton are single-celled organisms that grow and develop in the upper water column of oceans and in polar FOOD WEB The species that make up the base of the marine food Seasonal blooms of phytoplankton serve to con- sea ice. Phytoplankton are responsible for primary productivity—using the energy of the sun and transforming it via pho- web and those that create important seafloor habitat centrate birds, fishes, and marine mammals in key areas, tosynthesis. -
Notes on the Systematics, Morphology and Biostratigraphy of Fossil Holoplanktonic Mollusca, 22 1
B76-Janssen-Grebnev:Basteria-2010 11/07/2012 19:23 Page 15 Notes on the systematics, morphology and biostratigraphy of fossil holoplanktonic Mollusca, 22 1. Further pelagic gastropods from Viti Levu, Fiji Archipelago Arie W. Janssen Netherlands Centre for Biodiversity Naturalis (Palaeontology Department), P.O. Box 9517, NL-2300 RA Leiden, The Netherlands; currently: 12, Triq tal’Hamrija, Xewkija XWK 9033, Gozo, Malta; [email protected] Andrew Grebneff † Formerly : University of Otago, Geology Department, Dunedin, New Zealand himself during holiday trips in 1995 and 1996, also from Viti Two localities in the island of Viti Levu, Fiji Archipelago, Levu, the largest island in the Fiji archipelago. Following an yielded together 28 species of Heteropoda (3 species) and initial evaluation of this material it remained unstudied, 15 Pteropoda (25 species). Two samples from Tabataba, NW however, for a long time . A first inspection acknowledged Viti Levu, indicate an age of late Miocene to early Pliocene. Andrew’s impression that part of the samples was younger Two samples from Waila, SE Viti Levu, signify an age of than the earlier described material and therefore worth Pliocene (Piacenzian) and closely resemble coeval assem - publishing. blages described from Pangasinan, Philippines. After the untimely death of Andrew Grebneff in July 2010 (see the website of the University of Otago, New Key words: Gastropoda, Pterotracheoidea, Limacinoidea, Zealand (http://www.otago.ac.nz/geology/news/files/ Cavolinioidea, Clionoidea, late Miocene, Pliocene, biostratigraphy, andrew_ grebneff.html) it was decided to restart the study Fiji archipelago. of those samples and publish the results with Andrew’s name added as a valuable co-author, as he not only collected the specimens but also participated in discussions on their Introduction taxonomy and age.