Smithsonian at the Poles Contributions to International Polar Year Science
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788 RR MAKAROV & AI DANILOV (Eds.)
788 R. R. MAKAROV& A. I. DANILOV(eds.), Investigations of the Weddell Gyre. Oceanographic conditions and peculiarities of the development of plankton communities: 140-160 [in Rus- sian]. (VNIRO Publication, Moscow). MAKAROV,R. R. & L. L. MENSHENINA,1992. Larvae of euphausiids off Queen Maud Land. Polar Biology, 11: 515-523. MAKAROV,R. R., L. L. MENSHENINA& V. I. LATOGURSKY,1993. Fishery of Antarctic krill (Euphausia superba Dana) and problems of rational exploitation of its resources. Antarctica, 32: 111-124 [in Russian]. MAKAROV,R. R. & V. A. SPIRIDONOV,1993. Life cycle and distribution of Antarctic krill. Some results of studies and problems. In: N. M. VORONINA(ed.), Pelagic ecosystems of the Southern Ocean: 158-168 [in Russian]. (Nauka, Moscow). BATHMANN,U. V., R. R. MAKAROV,V. A. SPIRIDONOV& G. ROHARDT,1993. Winter distribution and overwintering strategies of the Antarctic copepod species Calanoides acutus, Rhincalanus gigas and Calanus propinquus (Crustacea, Calanoida) in the Weddell Sea. Polar Biology, 13: 333-346. APPLICATION OF ULTRASOUND TECHNOLOGY TO CRUSTACEAN PHYSIOLOGY; MONITORING CARDIAC AND SCAPHOGNATHITE RATES IN BRACHYURA BY PAUL A. HAEFNER, JR. Rochester Institute of Technology, Department of Biology, Rochester, New York 14623, U.S.A. Machines used in diagnostic radiology and cardiology have application to crus- tacean organ systems. Gribble & Reynolds (1993), and Gribble (1994) demon- strated the use of angiography to describe cardiovascular function in a crab. In January 1994, I made preliminary ultrasound scans of a live crayfish. Although sagittal and transverse series of images produced little resolution of internal or- gans, movements of the heart and scaphognathites were easily detected. This paper reveals the ability to monitor the activities of these organs in brachyuran crabs. -
Zootaxa,Crustacean Classification
Zootaxa 1668: 313–325 (2007) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2007 · Magnolia Press ISSN 1175-5334 (online edition) Crustacean classification: on-going controversies and unresolved problems* GEOFF A. BOXSHALL Department of Zoology, The Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom E-mail: [email protected] *In: Zhang, Z.-Q. & Shear, W.A. (Eds) (2007) Linnaeus Tercentenary: Progress in Invertebrate Taxonomy. Zootaxa, 1668, 1–766. Table of contents Abstract . 313 Introduction . 313 Treatment of parasitic Crustacea . 315 Affinities of the Remipedia . 316 Validity of the Entomostraca . 318 Exopodites and epipodites . 319 Using of larval characters in estimating phylogenetic relationships . 320 Fossils and the crustacean stem lineage . 321 Acknowledgements . 322 References . 322 Abstract The journey from Linnaeus’s original treatment to modern crustacean systematics is briefly characterised. Progress in our understanding of phylogenetic relationships within the Crustacea is linked to continuing discoveries of new taxa, to advances in theory and to improvements in methodology. Six themes are discussed that serve to illustrate some of the major on-going controversies and unresolved problems in the field as well as to illustrate changes that have taken place since the time of Linnaeus. These themes are: 1. the treatment of parasitic Crustacea, 2. the affinities of the Remipedia, 3. the validity of the Entomostraca, 4. exopodites and epipodites, 5. using larval characters in estimating phylogenetic rela- tionships, and 6. fossils and the crustacean stem-lineage. It is concluded that the development of the stem lineage concept for the Crustacea has been dominated by consideration of taxa known only from larval or immature stages. -
The Plankton Lifeform Extraction Tool: a Digital Tool to Increase The
Discussions https://doi.org/10.5194/essd-2021-171 Earth System Preprint. Discussion started: 21 July 2021 Science c Author(s) 2021. CC BY 4.0 License. Open Access Open Data The Plankton Lifeform Extraction Tool: A digital tool to increase the discoverability and usability of plankton time-series data Clare Ostle1*, Kevin Paxman1, Carolyn A. Graves2, Mathew Arnold1, Felipe Artigas3, Angus Atkinson4, Anaïs Aubert5, Malcolm Baptie6, Beth Bear7, Jacob Bedford8, Michael Best9, Eileen 5 Bresnan10, Rachel Brittain1, Derek Broughton1, Alexandre Budria5,11, Kathryn Cook12, Michelle Devlin7, George Graham1, Nick Halliday1, Pierre Hélaouët1, Marie Johansen13, David G. Johns1, Dan Lear1, Margarita Machairopoulou10, April McKinney14, Adam Mellor14, Alex Milligan7, Sophie Pitois7, Isabelle Rombouts5, Cordula Scherer15, Paul Tett16, Claire Widdicombe4, and Abigail McQuatters-Gollop8 1 10 The Marine Biological Association (MBA), The Laboratory, Citadel Hill, Plymouth, PL1 2PB, UK. 2 Centre for Environment Fisheries and Aquacu∑lture Science (Cefas), Weymouth, UK. 3 Université du Littoral Côte d’Opale, Université de Lille, CNRS UMR 8187 LOG, Laboratoire d’Océanologie et de Géosciences, Wimereux, France. 4 Plymouth Marine Laboratory, Prospect Place, Plymouth, PL1 3DH, UK. 5 15 Muséum National d’Histoire Naturelle (MNHN), CRESCO, 38 UMS Patrinat, Dinard, France. 6 Scottish Environment Protection Agency, Angus Smith Building, Maxim 6, Parklands Avenue, Eurocentral, Holytown, North Lanarkshire ML1 4WQ, UK. 7 Centre for Environment Fisheries and Aquaculture Science (Cefas), Lowestoft, UK. 8 Marine Conservation Research Group, University of Plymouth, Drake Circus, Plymouth, PL4 8AA, UK. 9 20 The Environment Agency, Kingfisher House, Goldhay Way, Peterborough, PE4 6HL, UK. 10 Marine Scotland Science, Marine Laboratory, 375 Victoria Road, Aberdeen, AB11 9DB, UK. -
GSA TODAY • Southeastern Section Meeting, P
Vol. 5, No. 1 January 1995 INSIDE • 1995 GeoVentures, p. 4 • Environmental Education, p. 9 GSA TODAY • Southeastern Section Meeting, p. 15 A Publication of the Geological Society of America • North-Central–South-Central Section Meeting, p. 18 Stability or Instability of Antarctic Ice Sheets During Warm Climates of the Pliocene? James P. Kennett Marine Science Institute and Department of Geological Sciences, University of California Santa Barbara, CA 93106 David A. Hodell Department of Geology, University of Florida, Gainesville, FL 32611 ABSTRACT to the south from warmer, less nutrient- rich Subantarctic surface water. Up- During the Pliocene between welling of deep water in the circum- ~5 and 3 Ma, polar ice sheets were Antarctic links the mean chemical restricted to Antarctica, and climate composition of ocean deep water with was at times significantly warmer the atmosphere through gas exchange than now. Debate on whether the (Toggweiler and Sarmiento, 1985). Antarctic ice sheets and climate sys- The evolution of the Antarctic cryo- tem withstood this warmth with sphere-ocean system has profoundly relatively little change (stability influenced global climate, sea-level his- hypothesis) or whether much of the tory, Earth’s heat budget, atmospheric ice sheet disappeared (deglaciation composition and circulation, thermo- hypothesis) is ongoing. Paleoclimatic haline circulation, and the develop- data from high-latitude deep-sea sed- ment of Antarctic biota. iments strongly support the stability Given current concern about possi- hypothesis. Oxygen isotopic data ble global greenhouse warming, under- indicate that average sea-surface standing the history of the Antarctic temperatures in the Southern Ocean ocean-cryosphere system is important could not have increased by more for assessing future response of the Figure 1. -
36. Comparison of Winter and Summer Growth Stages of the Diatom Eucampia Antarctica from the Kerguelen Plateau and South of the Antarctic Convergence Zone1
Barron, J., Larsen, B., et al., 1991 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 119 36. COMPARISON OF WINTER AND SUMMER GROWTH STAGES OF THE DIATOM EUCAMPIA ANTARCTICA FROM THE KERGUELEN PLATEAU AND SOUTH OF THE ANTARCTIC CONVERGENCE ZONE1 Greta A. Fryxell2 ABSTRACT On ODP Leg 119, specimens collected of Eucampia antarctica (Castracane) Mangin var. antarctica exhibited mor- phological and distribution patterns that contrasted with those of Eucampia antarctica var. recta (Mangin) G. Fryxell et Prasad. E. antarctica var. antarctica was found over the northern Kerguelen Plateau, north of the summer Antarctic Convergence Zone, in the subpolar plankton and in the sediments. E. antarctica var. recta was found close to the conti- nent in Prydz Bay. It was also collected near and under the ice in the northern Weddell Sea on a National Science Foun- dation Division of Polar Programs project (1983-1988). A key feature for distinguishing the two varieties in the field is the growth habit, with curvature in broad girdle view of the nominate, subpolar variety in both the winter stage and the more lightly silicified summer stage. A low ratio of terminal to intercalary valves results from the repeated division of the original doublets into chains of considerable length of the winter stage. Small spines around the elevations of one valve serve to clasp the sibling valve and maintain the chain formation. Cells of E. antarctica var. recta tend to be somewhat larger than E. antarctica var. antarctica, and they form chains that are straight in broad girdle view but slightly curved in narrow girdle view. -
Antarctic Primer
Antarctic Primer By Nigel Sitwell, Tom Ritchie & Gary Miller By Nigel Sitwell, Tom Ritchie & Gary Miller Designed by: Olivia Young, Aurora Expeditions October 2018 Cover image © I.Tortosa Morgan Suite 12, Level 2 35 Buckingham Street Surry Hills, Sydney NSW 2010, Australia To anyone who goes to the Antarctic, there is a tremendous appeal, an unparalleled combination of grandeur, beauty, vastness, loneliness, and malevolence —all of which sound terribly melodramatic — but which truly convey the actual feeling of Antarctica. Where else in the world are all of these descriptions really true? —Captain T.L.M. Sunter, ‘The Antarctic Century Newsletter ANTARCTIC PRIMER 2018 | 3 CONTENTS I. CONSERVING ANTARCTICA Guidance for Visitors to the Antarctic Antarctica’s Historic Heritage South Georgia Biosecurity II. THE PHYSICAL ENVIRONMENT Antarctica The Southern Ocean The Continent Climate Atmospheric Phenomena The Ozone Hole Climate Change Sea Ice The Antarctic Ice Cap Icebergs A Short Glossary of Ice Terms III. THE BIOLOGICAL ENVIRONMENT Life in Antarctica Adapting to the Cold The Kingdom of Krill IV. THE WILDLIFE Antarctic Squids Antarctic Fishes Antarctic Birds Antarctic Seals Antarctic Whales 4 AURORA EXPEDITIONS | Pioneering expedition travel to the heart of nature. CONTENTS V. EXPLORERS AND SCIENTISTS The Exploration of Antarctica The Antarctic Treaty VI. PLACES YOU MAY VISIT South Shetland Islands Antarctic Peninsula Weddell Sea South Orkney Islands South Georgia The Falkland Islands South Sandwich Islands The Historic Ross Sea Sector Commonwealth Bay VII. FURTHER READING VIII. WILDLIFE CHECKLISTS ANTARCTIC PRIMER 2018 | 5 Adélie penguins in the Antarctic Peninsula I. CONSERVING ANTARCTICA Antarctica is the largest wilderness area on earth, a place that must be preserved in its present, virtually pristine state. -
Kinematic and Dynamic Scaling of Copepod Swimming
fluids Review Kinematic and Dynamic Scaling of Copepod Swimming Leonid Svetlichny 1,* , Poul S. Larsen 2 and Thomas Kiørboe 3 1 I.I. Schmalhausen Institute of Zoology, National Academy of Sciences of Ukraine, Str. B. Khmelnytskogo, 15, 01030 Kyiv, Ukraine 2 DTU Mechanical Engineering, Fluid Mechanics, Technical University of Denmark, Building 403, DK-2800 Kgs. Lyngby, Denmark; [email protected] 3 Centre for Ocean Life, Danish Technical University, DTU Aqua, Building 202, DK-2800 Kgs. Lyngby, Denmark; [email protected] * Correspondence: [email protected] Received: 30 March 2020; Accepted: 6 May 2020; Published: 11 May 2020 Abstract: Calanoid copepods have two swimming gaits, namely cruise swimming that is propelled by the beating of the cephalic feeding appendages and short-lasting jumps that are propelled by the power strokes of the four or five pairs of thoracal swimming legs. The latter may be 100 times faster than the former, and the required forces and power production are consequently much larger. Here, we estimated the magnitude and size scaling of swimming speed, leg beat frequency, forces, power requirements, and energetics of these two propulsion modes. We used data from the literature together with new data to estimate forces by two different approaches in 37 species of calanoid copepods: the direct measurement of forces produced by copepods attached to a tensiometer and the indirect estimation of forces from swimming speed or acceleration in combination with experimentally estimated drag coefficients. Depending on the approach, we found that the propulsive forces, both for cruise swimming and escape jumps, scaled with prosome length (L) to a power between 2 and 3. -
Fatty Acid and Alcohol Composition of the Small Polar Copepods, Oithona and Oncaea : Indication on Feeding Modes
Polar Biol (2003) 26: 666–671 DOI 10.1007/s00300-003-0540-x ORIGINAL PAPER G. Kattner Æ C. Albers Æ M. Graeve S. B. Schnack-Schiel Fatty acid and alcohol composition of the small polar copepods, Oithona and Oncaea : indication on feeding modes Received: 2 April 2003 / Accepted: 28 July 2003 / Published online: 27 August 2003 Ó Springer-Verlag 2003 Abstract The fatty acid and alcohol compositions of the (Paffenho¨ fer 1993). They occur from the polar seas to Antarctic copepods Oithona similis, Oncaea curvata, tropical regions at both hemispheres. Species of both Oncaea antarctica and the Arctic Oncaea borealis were genera can reach high concentrations, exceeding 5,000 determined to provide the first data on their lipid bio- individuals m)3 (Dagg et al. 1980; Koga 1986; chemistry and to expand the present knowledge on their Paffenho¨ fer 1993; Metz 1996). The high abundance of feeding modes and life-cycle strategies. All these tiny these tiny species compensates for the low biomass and, species contained high amounts of wax esters (on average thus, the populations can reach biomass levels of the 51.4–86.3% of total lipid), except females of Oithona same order as dominant calanoid species (Metz 1996). In similis (15.2%). The fatty-acid composition was clearly the Southern Ocean, Oithonidae and Oncaeidae can dominated by 18:1(n-9), especially in the wax-ester-rich account for between 20 and 24% of the total copepod Oncaea curvata (79.7% of total fatty acids). In all species, biomass (Schnack-Schiel et al. 1998). 16:0 and the polyunsaturated fatty acids 20:5(n-3) and The epipelagic species, Oithona similis, has been de- 22:6(n-3), which are structural components of all mem- scribed as the most numerous and widely distributed branes, occurred in significant proportions. -
Ocean Deoxygenation and Copepods: Coping with Oxygen Minimum Zone Variability
Biogeosciences, 17, 2315–2339, 2020 https://doi.org/10.5194/bg-17-2315-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Ocean deoxygenation and copepods: coping with oxygen minimum zone variability Karen F. Wishner1, Brad Seibel2, and Dawn Outram1 1Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882, USA 2College of Marine Science, University of South Florida, St. Petersburg, FL 33701, USA Correspondence: Karen F. Wishner ([email protected]) Received: 27 September 2019 – Discussion started: 28 October 2019 Revised: 31 March 2020 – Accepted: 2 April 2020 – Published: 24 April 2020 Abstract. Increasing deoxygenation (loss of oxygen) of compression concept). These distribution depths changed by the ocean, including expansion of oxygen minimum zones tens to hundreds of meters depending on the species, oxygen (OMZs), is a potentially important consequence of global profile, and phenomenon. For example, at the lower oxycline, warming. We examined present-day variability of vertical the depth of maximum abundance for Lucicutia hulsemannae distributions of 23 calanoid copepod species in the East- shifted from ∼ 600 to ∼ 800 m, and the depth of diapause for ern Tropical North Pacific (ETNP) living in locations with Eucalanus inermis shifted from ∼ 500 to ∼ 775 m, in an ex- different water column oxygen profiles and OMZ inten- panded OMZ compared to a thinner OMZ, but remained at sity (lowest oxygen concentration and its vertical extent in similar low oxygen levels in -
Tesis Estructura Comunitaria De Copepodos .Pdf
Universidad de Concepción Dirección de Postgrado Facultad de Ciencias Naturales y Oceanográficas Programa de Magister en Ciencias mención Oceanografía Estructura comunitaria de copépodos pelágicos asociados a montes submarinos de la Dorsal Juan Fernández (32-34°S) en el Pacífico Sur Oriental Tesis para optar al grado de Magíster en Ciencias con mención en Oceanografía PAMELA ANDREA FIERRO GONZÁLEZ CONCEPCIÓN-CHILE 2019 Profesora Guía: Pamela Hidalgo Díaz Departamento de Oceanografía, Facultad de Ciencias Naturales y Oceanográficas Universidad de Concepción Profesor Co-guía: Rubén Escribano Departamento de Oceanografía, Facultad de Ciencias Naturales y Oceanográficas Universidad de Concepción La Tesis de “Magister en Ciencias con mención en Oceanografía” titulada “Estructura comunitaria de copépodos pelágicos asociados a montes submarinos de la Dorsal Juan Fernández (32-34°S) en el Pacífico sur oriental”, de la Srta. “PAMELA ANDREA FIERRO GONZÁLEZ” y realizada bajo la Facultad de Ciencias Naturales y Oceanográficas, Universidad de Concepción, ha sido aprobada por la siguiente Comisión de Evaluación: Dra. Pamela Hidalgo Díaz Profesora Guía Universidad de Concepción Dr. Rubén Escribano Profesor Co-Guía Universidad de Concepción Dr. Samuel Hormazábal Miembro de la Comisión Evaluadora Pontificia Universidad Católica de Valparaíso Dr. Fabián Tapia Director Programa de Magister en Oceanografía Universidad de Concepción ii A Juan Carlos y Sebastián iii AGRADECIMIENTOS Agradezco a quienes con su colaboración y apoyo hicieron posible el desarrollo y término de esta tesis. En primer lugar, agradezco a los miembros de mi comisión de tesis. A mi profesora guía, Dra. Pamela Hidalgo, por apoyarme y guiarme en este largo camino de formación académica, por su gran calidad humana, contención y apoyo personal. -
General Background
Guidelines for the Establishment of Environmental Quality Objectives and Targets in the Coastal Zone of the Western Indian Ocean (WIO) Region October 2009 WIO region: Environmental Quality Objectives and Targets October 2009 First published in Kenya in 2009 by the United Nations Environment Programme (UNEP)/Nairobi Convention Secretariat and the Council for Scientific and Industrial Research of South Africa (CSIR). Copyright © 2009, UNEP/Nairobi Convention Secretariat and CSIR. UNEP/GEF WIO-LaB Technical Report Series No. 2009/7 CSIR Report Number: CSIR/NRE/CO/ER/2009/0115/A Copyright notice: This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes without special permission from the copyright holder provided that acknowledgement of the source is made. UNEP/Nairobi Convention Secretariat and CSIR would appreciate receiving a copy of any publication that uses this publication as a source. No use of this publication may be made for resale or for any other commercial purpose without prior permission in writing from UNEP/Nairobi Convention Secretariat and CSIR. Disclaimer: The contents of this report do not necessarily reflect the views and policies of UNEP. The designations employed and the presentations do not imply of any opinion whatsoever on the part of the UNEP, or of any cooperating organization concerning the legal status of any country, territory, city or area, of its authorities, or of the delineation of its territories or boundaries. For additional information please contact: UNEP/Nairobi Convention Secretariat Council for Scientific and Industrial Research (CSIR) United Nations Environment Programme P O Box 17001, Durban, South Africa United Nations Avenue, Gigiri, Tel: +27 31 2422356 P.O Box 47074, Nairobi, Kenya Fax: +27 31 2612509 Tel: +254 20 7621250/7622025 E-mail: [email protected] E-mail: [email protected] Principal Authors: Susan Taljaard (CSIR, Stellenbosch), Steven Weerts (CSIR, Durban), Shamilla Pillay (CSIR, Durban) and Anisha Rajkumar (CSIR, Durban) Technical Editors: Dr. -
Molecular Species Delimitation and Biogeography of Canadian Marine Planktonic Crustaceans
Molecular Species Delimitation and Biogeography of Canadian Marine Planktonic Crustaceans by Robert George Young A Thesis presented to The University of Guelph In partial fulfilment of requirements for the degree of Doctor of Philosophy in Integrative Biology Guelph, Ontario, Canada © Robert George Young, March, 2016 ABSTRACT MOLECULAR SPECIES DELIMITATION AND BIOGEOGRAPHY OF CANADIAN MARINE PLANKTONIC CRUSTACEANS Robert George Young Advisors: University of Guelph, 2016 Dr. Sarah Adamowicz Dr. Cathryn Abbott Zooplankton are a major component of the marine environment in both diversity and biomass and are a crucial source of nutrients for organisms at higher trophic levels. Unfortunately, marine zooplankton biodiversity is not well known because of difficult morphological identifications and lack of taxonomic experts for many groups. In addition, the large taxonomic diversity present in plankton and low sampling coverage pose challenges in obtaining a better understanding of true zooplankton diversity. Molecular identification tools, like DNA barcoding, have been successfully used to identify marine planktonic specimens to a species. However, the behaviour of methods for specimen identification and species delimitation remain untested for taxonomically diverse and widely-distributed marine zooplanktonic groups. Using Canadian marine planktonic crustacean collections, I generated a multi-gene data set including COI-5P and 18S-V4 molecular markers of morphologically-identified Copepoda and Thecostraca (Multicrustacea: Hexanauplia) species. I used this data set to assess generalities in the genetic divergence patterns and to determine if a barcode gap exists separating interspecific and intraspecific molecular divergences, which can reliably delimit specimens into species. I then used this information to evaluate the North Pacific, Arctic, and North Atlantic biogeography of marine Calanoida (Hexanauplia: Copepoda) plankton.