Amphipod – Pteropod Associations in the Southern Ocean
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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. -
AMPHIPODA Sheet 103 SUB-ORDER: HYPERIIDEA Family: Hyperiidae (BY M
CONSEIL INTERNATIONAL POUR L’EXPLORATION DE LA MER Zooplankton AMPHIPODA Sheet 103 SUB-ORDER: HYPERIIDEA Family: Hyperiidae (BY M. J. DUNBAR) 1963 https://doi.org/10.17895/ices.pub.4917 -2- 1. Hyperia galba, 9;a, per. 1; b, per. 2. - 2. Hyperia medusarum, 9;a, per. 1 ; b, per. 2. - 3. Hyperoche rnedusarum, 8; a, per. 1 ; b, per. 2. - 4. Parathemisto abyssorum, Q; a, per. 3; b, uropods. - 5. Para- themisto gauchicaudi (“short-legged” form), 9; a, per. 3; b, uropods; c, per. 5. - 6. Parathemisto libellula, Q; a, per. 3; b, uropods; c, per. 5. - 7. Parathemisto gracilipes, (first antenna not drawn in full); a, per. 5; b, uropods 3. (Figures 7, 7a and 7b redrawn from HURLEY;Figure 6c original; remainder drawn from SARS.) The limbs of the peraeon, or peraeopods, are here numbered in series from 1 to 7, numbers 1 and 2 being also called “gnathopods”; “per.” = peraeopod. Only the species of the northern part of the North Atlantic are treated here; the Mediterranean species are omitted. The family is still in need of revision. Family Hyperiidae Key to the genera:- la. Per. 5-7 considerably longer than per. 3 and 4. ........................................................ Parathemisto Boeck lb. Per. 5 and 6 longer than 3 and 4; per. 7 much shorter than 5 and 6 ..................Hyperioides longipes Chevreux (not figured) lc. Per. 5-7 not longer than 3 and 4 ....................................................................................... 2 2a. Per. 1 and 2, the fixed finger (onjoint 5) of thechelanot shorter than the movable finger (joint 6). ...Hyperoche medusarum (Kroyer) (Fig. 3) 2b. Per. -
Coastal and Marine Ecological Classification Standard (2012)
FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ...................................................... -
And Hyperia Curticephala (Peracarida: Amphipoda) in Mejillones Bay, Northern Chile
Revista de Biología Marina y Oceanografía 45(1): 127-130, abril de 2010 Association between Chrysaora plocamia (Cnidaria, Scyphozoa) and Hyperia curticephala (Peracarida: Amphipoda) in Mejillones Bay, Northern Chile Asociación entre Chrysaora plocamia (Cnidaria, Scyphozoa) e Hyperia curticephala (Peracarida: Amphipoda) en Bahía de Mejillones, norte de Chile Marcelo E. Oliva1, Alexis Maffet1 and Jürgen Laudien2 1Instituto de Investigaciones Oceanológicas, Facultad de Recursos del Mar, Universidad de Antofagasta, P.O. Box 170, Antofagasta, Chile 2Alfred Wegener Institute for Polar and Marine Research, Am Alten Hafen 26, D-27568, Bremerhaven, Germany [email protected] Resumen.- Se registra Hyperia curticephala (Amphipoda) parasitoide como ha sido sugerido para asociaciones entre viviendo en asociación con Chrysaora plocamia (Scyphozoa). hypéridos y plancton gelatinoso. Este registro extiende la Cinco ejemplares de C. plocamia presentaron entre 39 y 328 distribución del anfípodo en aproximadamente 18° de latitud especímenes de H. curticephala. No hay evidencia estadística hacia el sur y corresponde al primer registro de un anfípodo de correlación entre diámetro de umbrela y número de asociado con medusas en Chile. anfípodos, gráficamente es evidente una tendencia positiva. H. Palabras clave: Anfípodos hipéridos, sistema de afloramiento curticephala debe considerarse microdepredador y no de la Corriente de Humboldt, microdepredador Introduction plocamia (Lesson, 1830), reaches comparatively high abundances in shallow waters during the warm season Zooplanktivores are an important link between primary (December-February) (pers. observ.). The record of the consumers and higher trophic levels (Thiel et al. 2007). associated hyperiid amphipod Hyperia curticephala Off Chile by far the best studied zooplankton taxa are Vinogradov & Semenova, 1985 is the first from the copepods, euphausids (e.g. -
Data Structure
Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference. -
Species Status Assessment Emperor Penguin (Aptenodytes Fosteri)
SPECIES STATUS ASSESSMENT EMPEROR PENGUIN (APTENODYTES FOSTERI) Emperor penguin chicks being socialized by male parents at Auster Rookery, 2008. Photo Credit: Gary Miller, Australian Antarctic Program. Version 1.0 December 2020 U.S. Fish and Wildlife Service, Ecological Services Program Branch of Delisting and Foreign Species Falls Church, Virginia Acknowledgements: EXECUTIVE SUMMARY Penguins are flightless birds that are highly adapted for the marine environment. The emperor penguin (Aptenodytes forsteri) is the tallest and heaviest of all living penguin species. Emperors are near the top of the Southern Ocean’s food chain and primarily consume Antarctic silverfish, Antarctic krill, and squid. They are excellent swimmers and can dive to great depths. The average life span of emperor penguin in the wild is 15 to 20 years. Emperor penguins currently breed at 61 colonies located around Antarctica, with the largest colonies in the Ross Sea and Weddell Sea. The total population size is estimated at approximately 270,000–280,000 breeding pairs or 625,000–650,000 total birds. Emperor penguin depends upon stable fast ice throughout their 8–9 month breeding season to complete the rearing of its single chick. They are the only warm-blooded Antarctic species that breeds during the austral winter and therefore uniquely adapted to its environment. Breeding colonies mainly occur on fast ice, close to the coast or closely offshore, and amongst closely packed grounded icebergs that prevent ice breaking out during the breeding season and provide shelter from the wind. Sea ice extent in the Southern Ocean has undergone considerable inter-annual variability over the last 40 years, although with much greater inter-annual variability in the five sectors than for the Southern Ocean as a whole. -
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. -
Multidecadal Warming and Density Loss in the Deep Weddell Sea, Antarctica
15 NOVEMBER 2020 S T R A S S E T A L . 9863 Multidecadal Warming and Density Loss in the Deep Weddell Sea, Antarctica VOLKER H. STRASS,GERD ROHARDT,TORSTEN KANZOW,MARIO HOPPEMA, AND OLAF BOEBEL Alfred-Wegener-Institut Helmholtz-Zentrum fur€ Polar- und Meeresforschung, Bremerhaven, Germany (Manuscript received 16 April 2020, in final form 10 August 2020) ABSTRACT: The World Ocean is estimated to store more than 90% of the excess energy resulting from man-made greenhouse gas–driven radiative forcing as heat. Uncertainties of this estimate are related to undersampling of the subpolar and polar regions and of the depths below 2000 m. Here we present measurements from the Weddell Sea that cover the whole water column down to the sea floor, taken by the same accurate method at locations revisited every few years since 1989. Our results show widespread warming with similar long-term temperature trends below 700-m depth at all sampling sites. The mean heating rate below 2000 m exceeds that of the global ocean by a factor of about 5. Salinity tends to increase—in contrast to other Southern Ocean regions—at most sites and depths below 700 m, but nowhere strongly enough to fully compensate for the warming effect on seawater density, which hence shows a general decrease. In the top 700 m neither temperature nor salinity shows clear trends. A closer look at the vertical distribution of changes along an ap- proximately zonal and a meridional section across the Weddell Gyre reveals that the strongest vertically coherent warming is observed at the flanks of the gyre over the deep continental slopes and at its northern edge where the gyre connects to the Antarctic Circumpolar Current (ACC). -
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. -
MOLLUSCA Nudibranchs, Pteropods, Gastropods, Bivalves, Chitons, Octopus
UNDERWATER FIELD GUIDE TO ROSS ISLAND & MCMURDO SOUND, ANTARCTICA: MOLLUSCA nudibranchs, pteropods, gastropods, bivalves, chitons, octopus Peter Brueggeman Photographs: Steve Alexander, Rod Budd/Antarctica New Zealand, Peter Brueggeman, Kirsten Carlson/National Science Foundation, Canadian Museum of Nature (Kathleen Conlan), Shawn Harper, Luke Hunt, Henry Kaiser, Mike Lucibella/National Science Foundation, Adam G Marsh, Jim Mastro, Bruce A Miller, Eva Philipp, Rob Robbins, Steve Rupp/National Science Foundation, Dirk Schories, M Dale Stokes, and Norbert Wu The National Science Foundation's Office of Polar Programs sponsored Norbert Wu on an Artist's and Writer's Grant project, in which Peter Brueggeman participated. One outcome from Wu's endeavor is this Field Guide, which builds upon principal photography by Norbert Wu, with photos from other photographers, who are credited on their photographs and above. This Field Guide is intended to facilitate underwater/topside field identification from visual characters. Organisms were identified from photographs with no specimen collection, and there can be some uncertainty in identifications solely from photographs. © 1998+; text © Peter Brueggeman; photographs © Steve Alexander, Rod Budd/Antarctica New Zealand Pictorial Collection 159687 & 159713, 2001-2002, Peter Brueggeman, Kirsten Carlson/National Science Foundation, Canadian Museum of Nature (Kathleen Conlan), Shawn Harper, Luke Hunt, Henry Kaiser, Mike Lucibella/National Science Foundation, Adam G Marsh, Jim Mastro, Bruce A Miller, Eva