Different Feeding Strategies in Antarctic Scavenging Amphipods and Their
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
List of Place-Names in Antarctica Introduced by Poland in 1978-1990
POLISH POLAR RESEARCH 13 3-4 273-302 1992 List of place-names in Antarctica introduced by Poland in 1978-1990 The place-names listed here in alphabetical order, have been introduced to the areas of King George Island and parts of Nelson Island (West Antarctica), and the surroundings of A. B. Dobrowolski Station at Bunger Hills (East Antarctica) as the result of Polish activities in these regions during the period of 1977-1990. The place-names connected with the activities of the Polish H. Arctowski Station have been* published by Birkenmajer (1980, 1984) and Tokarski (1981). Some of them were used on the Polish maps: 1:50,000 Admiralty Bay and 1:5,000 Lions Rump. The sheet reference is to the maps 1:200,000 scale, British Antarctic Territory, South Shetland Islands, published in 1968: King George Island (sheet W 62 58) and Bridgeman Island (Sheet W 62 56). The place-names connected with the activities of the Polish A. B. Dobrowolski Station have been published by Battke (1985) and used on the map 1:5,000 Antarctic Territory — Bunger Oasis. Agat Point. 6211'30" S, 58'26" W (King George Island) Small basaltic promontory with numerous agates (hence the name), immediately north of Staszek Cove. Admiralty Bay. Sheet W 62 58. Polish name: Przylądek Agat (Birkenmajer, 1980) Ambona. 62"09'30" S, 58°29' W (King George Island) Small rock ledge, 85 m a. s. 1. {ambona, Pol. = pulpit), above Arctowski Station, Admiralty Bay, Sheet W 62 58 (Birkenmajer, 1980). Andrzej Ridge. 62"02' S, 58° 13' W (King George Island) Ridge in Rose Peak massif, Arctowski Mountains. -
The Antarctic Treaty
The Antarctic Treaty Measures adopted at the Thirty-ninth Consultative Meeting held at Santiago, Chile 23 May – 1 June 2016 Presented to Parliament by the Secretary of State for Foreign and Commonwealth Affairs by Command of Her Majesty November 2017 Cm 9542 © Crown copyright 2017 This publication is licensed under the terms of the Open Government Licence v3.0 except where otherwise stated. To view this licence, visit nationalarchives.gov.uk/doc/open-government-licence/version/3 Where we have identified any third party copyright information you will need to obtain permission from the copyright holders concerned. This publication is available at www.gov.uk/government/publications Any enquiries regarding this publication should be sent to us at Treaty Section, Foreign and Commonwealth Office, King Charles Street, London, SW1A 2AH ISBN 978-1-5286-0126-9 CCS1117441642 11/17 Printed on paper containing 75% recycled fibre content minimum Printed in the UK by the APS Group on behalf of the Controller of Her Majestyʼs Stationery Office MEASURES ADOPTED AT THE THIRTY-NINTH ANTARCTIC TREATY CONSULTATIVE MEETING Santiago, Chile 23 May – 1 June 2016 The Measures1 adopted at the Thirty-ninth Antarctic Treaty Consultative Meeting are reproduced below from the Final Report of the Meeting. In accordance with Article IX, paragraph 4, of the Antarctic Treaty, the Measures adopted at Consultative Meetings become effective upon approval by all Contracting Parties whose representatives were entitled to participate in the meeting at which they were adopted (i.e. all the Consultative Parties). The full text of the Final Report of the Meeting, including the Decisions and Resolutions adopted at that Meeting and colour copies of the maps found in this command paper, is available on the website of the Antarctic Treaty Secretariat at www.ats.aq/documents. -
Anatomy of a Glacial Meltwater Discharge Event in An
Downloaded from http://rsta.royalsocietypublishing.org/ on May 22, 2018 Anatomy of a glacial meltwater discharge event rsta.royalsocietypublishing.org in an Antarctic cove Michael P.Meredith1, Ulrike Falk2,3, Anna Valeria Research Bers3,†, Andreas Mackensen3, Irene R. Schloss4,5,6, 4 3 Cite this article: Meredith MP,Falk U, Bers Eduardo Ruiz Barlett , Kerstin Jerosch , Adrián Silva AV, Mackensen A, Schloss IR, Ruiz Barlett E, Busso7 and Doris Abele3 Jerosch K, Silva Busso A, Abele D. 2018 Anatomy of a glacial meltwater discharge 1British Antarctic Survey, High Cross, Madingley Road, Cambridge eventinanAntarcticcove.Phil.Trans.R.Soc.A CB3 0ET, UK 376: 20170163. 2University of Bremen, Bremen, Germany http://dx.doi.org/10.1098/rsta.2017.0163 3Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am alten Hafen 24/Am Handelshafen 12, Accepted: 19 January 2018 27570 Bremerhaven, Germany 4Instituto Antártico Argentino, Buenos Aires, Argentina One contribution of 14 to a theme issue ‘The 5Centro Austral de Investigaciones Científicas (CADIC, CONICET), marine system of the West Antarctic Ushuaia, Argentina Peninsula: status and strategy for progress in a 6Universidad Nacional de Tierra del Fuego, Ushuaia, Argentina region of rapid change’. 7University of Buenos Aires, 1053 Buenos Aires, Argentina Subject Areas: MPM, 0000-0002-7342-7756;KJ,0000-0003-0728-2154 geochemistry, atmospheric science, biogeochemistry, glaciology, oceanography, Glacial meltwater discharge from Antarctica is a meteorology key influence on the marine environment, impacting ocean circulation, sea level and productivity of Keywords: the pelagic and benthic ecosystems. The responses elicited depend strongly on the characteristics of the glacial discharge, Antarctica, geochemical meltwater releases, including timing, spatial structure tracers, stable isotopes and geochemical composition. -
The Genome Sequence of the Antarctic Bullhead Notothen Reveals
Shin et al. Genome Biology 2014, 15:468 http://genomebiology.com/2014/15/9/468 RESEARCH Open Access The genome sequence of the Antarctic bullhead notothen reveals evolutionary adaptations to a cold environment Seung Chul Shin1, Do Hwan Ahn1,2, Su Jin Kim3, Chul Woo Pyo4, Hyoungseok Lee1, Mi-Kyeong Kim1, Jungeun Lee1, Jong Eun Lee5, H William Detrich III6, John H Postlethwait7, David Edwards8,9, Sung Gu Lee1,2, Jun Hyuck Lee1,2 and Hyun Park1,2* Abstract Background: Antarctic fish have adapted to the freezing waters of the Southern Ocean. Representative adaptations to this harsh environment include a constitutive heat shock response and the evolution of an antifreeze protein in the blood. Despite their adaptations to the cold, genome-wide studies have not yet been performed on these fish due to the lack of a sequenced genome. Notothenia coriiceps, the Antarctic bullhead notothen, is an endemic teleost fish with a circumpolar distribution and makes a good model to understand the genomic adaptations to constant sub-zero temperatures. Results: We provide the draft genome sequence and annotation for N. coriiceps. Comparative genome-wide analysis with other fish genomes shows that mitochondrial proteins and hemoglobin evolved rapidly. Transcriptome analysis of thermal stress responses find alternative response mechanisms for evolution strategies in a cold environment. Loss of the phosphorylation-dependent sumoylation motif in heat shock factor 1 suggests that the heat shock response evolved into a simple and rapid phosphorylation-independent regulatory mechanism. Rapidly evolved hemoglobin and the induction of a heat shock response in the blood may support the efficient supply of oxygen to cold-adapted mitochondria. -
THE OFFICIAL Magazine of the OCEANOGRAPHY SOCIETY
OceThe Officiala MaganZineog of the Oceanographyra Spocietyhy CITATION Detrich, H.W. III, B.A. Buckley, D.F. Doolittle, C.D. Jones, and S.J. Lockhart. 2012. Sub-Antarctic and high Antarctic notothenioid fishes: Ecology and adaptational biology revealed by the ICEFISH 2004 cruise of RVIB Nathaniel B. Palmer. Oceanography 25(3):184–187, http://dx.doi.org/10.5670/oceanog.2012.93. DOI http://dx.doi.org/10.5670/oceanog.2012.93 COPYRIGHT This article has been published inOceanography , Volume 25, Number 3, a quarterly journal of The Oceanography Society. Copyright 2012 by The Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching and research. Republication, systematic reproduction, or collective redistribution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: [email protected] or The Oceanography Society, PO Box 1931, Rockville, MD 20849-1931, USA. downloaded from http://www.tos.org/oceanography Antarctic OceanographY in A Changing WorLD >> SIDEBAR Sub-Antarctic and High Antarctic Notothenioid Fishes: Ecology and Adaptational Biology Revealed by the ICEFISH 2004 Cruise of RVIB Nathaniel B. Palmer BY H. WILLiam Detrich III, BraDLEY A. BUCKLEY, DanieL F. DooLittLE, Christopher D. Jones, anD SUsanne J. LocKhart ABSTRACT. The goal of the ICEFISH 2004 cruise, which was conducted on board RVIB high- and sub-Antarctic notothenioid fishes Nathaniel B. Palmer and traversed the transitional zones linking the South Atlantic to the Southern as we transitioned between these distinct Ocean, was to compare the evolution, ecology, adaptational biology, community structure, and oceanographic regimes. -
Multi-Year Analysis of Distributed Glacier Mass Balance Modelling and Equilibrium Line Altitude on King George Island, Antarctic Peninsula
The Cryosphere, 12, 1211–1232, 2018 https://doi.org/10.5194/tc-12-1211-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Multi-year analysis of distributed glacier mass balance modelling and equilibrium line altitude on King George Island, Antarctic Peninsula Ulrike Falk1,2, Damián A. López2,3, and Adrián Silva-Busso4,5 1Climate Lab, Institute for Geography, Bremen University, Bremen, Germany 2Center for Remote Sensing of Land Surfaces (ZFL), Bonn University, Bonn, Germany 3Institute of Geology and Mineralogy, University Cologne, Cologne, Germany 4Faculty of Exact and Natural Sciences, University Buenos Aires, Buenos Aires, Argentina 5Instituto Nacional de Agua (INA), Ezeiza, Buenos Aires, Argentina Correspondence: Ulrike Falk ([email protected]) Received: 12 October 2017 – Discussion started: 1 December 2017 Revised: 15 March 2018 – Accepted: 19 March 2018 – Published: 10 April 2018 Abstract. The South Shetland Islands are located at the seen over the course of the 5-year model run period. The win- northern tip of the Antarctic Peninsula (AP). This region ter accumulation does not suffice to compensate for the high was subject to strong warming trends in the atmospheric sur- variability in summer ablation. The results are analysed to as- face layer. Surface air temperature increased about 3K in sess changes in meltwater input to the coastal waters, specific 50 years, concurrent with retreating glacier fronts, an in- glacier mass balance and the equilibrium line altitude (ELA). crease in melt areas, ice surface lowering and rapid break- The Fourcade Glacier catchment drains into Potter cove, has up and disintegration of ice shelves. -
Ecology and Adaptational Biology Revealed by the ICEFISH 2004 Cruise of RVIB Nathaniel B
Portland State University PDXScholar Biology Faculty Publications and Presentations Biology 9-2012 Sub-Antarctic and High Antarctic Notothenioid Fishes: Ecology and Adaptational Biology Revealed by the ICEFISH 2004 Cruise of RVIB Nathaniel B. Palmer H. William Detrich III Northeastern University Bradley A. Buckley Portland State University Daniel F. Doolittle Christopher D. Jones National Oceanic and Atmospheric Administration Susanne J. Lockhart Antarctic Ecosystem Research Division Follow this and additional works at: https://pdxscholar.library.pdx.edu/bio_fac Part of the Aquaculture and Fisheries Commons, and the Biology Commons Let us know how access to this document benefits ou.y Citation Details Detrich, H.W. III, B.A. Buckley, D.F. Doolittle, C.D. Jones, and S.J. Lockhart. 2012. Sub-Antarctic and high Antarctic notothenioid fishes: cologyE and adaptational biology revealed by the ICEFISH 2004 cruise of RVIB Nathaniel B. Palmer. Oceanography 25(3):184–187. This Article is brought to you for free and open access. It has been accepted for inclusion in Biology Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Antarctic OceanographY in A Changing WorLD >> SIDEBAR Sub-Antarctic and High Antarctic Notothenioid Fishes: Ecology and Adaptational Biology Revealed by the ICEFISH 2004 Cruise of RVIB Nathaniel B. Palmer BY H. WILLiam Detrich III, BraDLEY A. BUCKLEY, DanieL F. DooLittLE, Christopher D. Jones, anD SUsanne J. LocKhart ABSTRACT. The goal of the ICEFISH 2004 cruise, which was conducted on board RVIB high- and sub-Antarctic notothenioid fishes Nathaniel B. Palmer and traversed the transitional zones linking the South Atlantic to the Southern as we transitioned between these distinct Ocean, was to compare the evolution, ecology, adaptational biology, community structure, and oceanographic regimes. -
Winter Melt Conditions of the Inland Ice Cap on King George Island, Antarctic Peninsula
2015 Vol. 69 · No. 4 · 341–363 WINTER MELT CONDITIONS OF THE INLAND ICE CAP ON KING GEORGE ISLAND, ANTARCTIC PENINSULA ULRIKE FALK and HERNÁN SALA With 13 figures, 1 table and 2 photos Received 23 June 2015 · Accepted 26 November 2015 Summary: The South Shetland Islands are located at the northern tip of the Antarctic Peninsula (AP) which is among the fastest warming regions on Earth. Surface air temperature increases (~3 K in 50 years) are concurrent with retreating glacier fronts, an increase in melt areas, ice surface lowering and rapid break-up and disintegration of ice shelves. We have com- piled a unique meteorological dataset for the King George Island (KGI)/Isla 25 de Mayo, the largest of the South Shetland Islands. It comprises high-temporal resolution and spatially distributed observations of surface air temperature, wind direc- tions and wind velocities, glacier ice temperatures in profile with a fully equipped automatic weather station as well as snow accumulation and ablation measurements on the Warszawa Icefield, since November 2010 and ongoing. In combination with long-term synoptic datasets (40 and 10 years, respectively) and atmospheric circulation indices datasets, we have looked at changes in the climatological drivers of the glacial melt processes, and the sensitivity of the inland ice cap with regard to winter melting periods and pressure anomalies. The analysis has revealed a positive trend of 5 K over four decades in minimum surface air temperatures for winter months, clearly exceeding the published annual mean statistics, associated to a negative trend in mean monthly winter sea level pressure. -
Em Áreas Livres De Gelo Nas Ilhas Nelson E Rei George, Antártica Marítima
Revista Brasileira de Geomorfologia v. 22, nº 3 (2021) http://lsie.unb.br/ugb/ ISSN 2236-5664 http://dx.doi.org/10.20502/rbg.v22i3.1911 Artigo de Pesquisa Mudanças recentes (1988-2018) em áreas livres de gelo nas ilhas Nelson e Rei George, Antártica Marítima Recent changes (1988-2018) in ice-marginal environments of the King George and Nelson Island ice-free land areas, Maritime Antarctica Manoela Araujo Gonçalves de Oliveira(1), Kátia Kellem da Rosa(2), Carina Petsch(3), Rosemary Vieira(4), Felipe Casanova(5), Jefferson Cardia Simões (6) 1 Centro Polar e Climático, Programa de Pós-Graduação em Geografia - UFRGS, Porto Alegre, RS, Brasil. [email protected] ORCID: https://orcid.org/0000-0003-4661-7316 2 Departamento de Geografia, Centro Polar e Climático, Programa de Pós-Graduação em Geografia - UFRGS, Porto Alegre, RS, Brasil. [email protected] ORCID: https://orcid.org/0000-0003-0977-9658 3 Departamento de Geociências – UFSM, Santa Maria, RS, Brasil. Centro Polar e Climático, UFRGS, Porto Alegre, RS, Brasil. [email protected] ORCID: http://orcid.org/0000-0002-1079-0080 4 Laboratório de Processos Sedimentares e Ambientais, Depto de Geografia – UFF, Niterói, RJ, Brasil [email protected] ORCID: https://orcid.org/0000-0003-0312-2890 5 Centro Polar e Climático, UFRGS, Porto Alegre, RS, Brasil, [email protected] ORCID: https://orcid.org/0000-0002-3626-7853 6 Departamento de Geografia, Centro Polar e Climático, Programa de Pós-Graduação em Geografia - UFRGS, Porto Alegre, RS, Brasil. jefferson.simõ[email protected] ORCID: https://orcid.org/0000-0001-5555-3401 Recebido: 11/12/2020; Aceito: 17/05/2021; Publicado: 01/07/2021 Resumo: O objetivo deste trabalho é comparar as variações dos lagos e geleiras apresentadas por diferentes setores de áreas livres de gelo nas ilhas Rei George (IRG) e Nelson (IN) no período 1988-2018. -
Induction of Heat Shock Proteins in Cold- Adapted and Cold
CORE Metadata, citation and similar papers at core.ac.uk Provided by ScholarWorks@UA INDUCTION OF HEAT SHOCK PROTEINS IN COLD- ADAPTED AND COLD- ACCLIMATED FISHES By Laura Elizabeth Teigen Dr. Kristin O'Brien Advisory Committee Chair Dr. Diane Wagner Chair, Department of Biology and Wildlife APPROVED: ;t.-/ INDUCTION OF HEAT SHOCK PROTEINS IN COLD- ADAPTED AND COLD- ACCLIMATED FISHES A THESIS Presented to the Faculty of the University of Alaska Fairbanks in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE By Laura Elizabeth Teigen, B.A. Fairbanks, Alaska May 2014 v Abstract I examined the effects of oxidative stress and changes in temperature on heat shock protein (Hsp) levels in cold-adapted and cold-acclimated fishes. Adaptation of Antarctic notothenioids to cold temperature is correlated with high levels of Hsps, thought to minimize cold-induced protein denaturation. Hsp70 levels were measured in red- and white-blooded Antarctic notothenioid fishes exposed to their critical thermal maximum (CTMax), 4C warm acclimated, and notothenioids from different latitudes. I determined the effect of cold acclimation on Hsp levels and the role of sirtuins in regulating Hsp expression and changes in metabolism in threespine stickleback, Gasterosteus aculeatus, cold-acclimated to 8C. Levels of Hsps do not increase in Antarctic notothenioids exposed to their CTMax, and warm acclimation reduced levels of Hsp70. Hsp70 levels were higher in Antarctic notothenioids compared to a temperate notothenioid and higher in white-blooded notothenioids compared to red-blooded notothenioids, despite higher oxidative stress levels in red-blooded fish, suggesting Hsp70 does not mitigate oxidative stress. -
Mitochondrial Phylogeny of Trematomid Fishes (Nototheniidae, Perciformes) and the Evolution of Antarctic Fish
MOLECULAR PHYLOGENETICS AND EVOLUTION Vol. 5, No. 2, April, pp. 383±390, 1996 ARTICLE NO. 0033 Mitochondrial Phylogeny of Trematomid Fishes (Nototheniidae, Perciformes) and the Evolution of Antarctic Fish PETER A. RITCHIE,²,*,1,2 LUCA BARGELLONI,*,³ AXEL MEYER,*,§ JOHN A. TAYLOR,² JOHN A. MACDONALD,² AND DAVID M. LAMBERT²,2 ²School of Biological Sciences, University of Auckland, Private Bag 92019, Auckland, New Zealand; *Department of Ecology and Evolution and §Program in Genetics, State University of New York, Stony Brook, New York 11794-5245; and ³Dipartimento di Biologia, Universita di Padova, Via Trieste 75, 35121 Padua, Italy Received November 22, 1994; revised June 2, 1995 there is evidence that this may have occurred about The subfamily of ®shes Trematominae is endemic to 12±14 million years ago (MYA) (Eastman, 1993; the subzero waters of Antarctica and is part of the Bargelloni et al., 1994). larger notothenioid radiation. Partial mitochondrial There may have been a suite of factors which allowed sequences from the 12S and 16S ribosomal RNA (rRNA) the notothenioids, in particular, to evolve to such domi- genes and a phylogeny for 10 trematomid species are nance in the Southern Oceans. Several authors have presented. As has been previously suggested, two taxa, suggested that speciation within the group could have Trematomus scotti and T. newnesi, do not appear to be been the result of large-scale disruptions in the Antarc- part of the main trematomid radiation. The genus Pa- tic ecosystem during the Miocene (Clarke, 1983). The gothenia is nested within the genus Trematomus and isostatic pressure from the accumulation of ice during has evolved a unique cyropelagic existence, an associ- the early Miocene (25±15 MYA) left the continental ation with pack ice. -
Ensemble Modeling of Antarctic Macroalgal Habitats Exposed to Glacial Melt in a Polar Fjord
ORIGINAL RESEARCH published: 13 June 2019 doi: 10.3389/fevo.2019.00207 Ensemble Modeling of Antarctic Macroalgal Habitats Exposed to Glacial Melt in a Polar Fjord Kerstin Jerosch 1*, Frauke K. Scharf 1, Dolores Deregibus 2, Gabriela L. Campana 2,3, Katharina Zacher 1, Hendrik Pehlke 1, Ulrike Falk 4, H. Christian Hass 5, Maria L. Quartino 2,6 and Doris Abele 1 1 Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Functional Ecology, Bremerhaven, Germany, 2 Department of Coastal Biology, Argentinean Antarctic Institute, Buenos Aires, Argentina, 3 Department of Basic Sciences, National University of Luján, Luján, Argentina, 4 Department of Geography FB08, University of Bremen, Bremen, Germany, 5 Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Wadden Sea Research Station, List, Germany, 6 Museo Argentino de Ciencias Naturales Bernardino Rivadavia, Buenos Aires, Argentina Edited by: Bruno Danis, Macroalgae are the main primary producers in polar coastal regions and of major Free University of Brussels, Belgium importance for the associated heterotrophic communities. On King George Island/Isla Reviewed by: 25 de Mayo, West Antarctic Peninsula (WAP) several fjords undergo rapid glacial Charlene Guillaumot, Free University of Brussels, Belgium retreat in response to increasing atmospheric temperatures. Hence, extended meltwater Charles Amsler, plumes laden with suspended particulate matter (SPM) are generated that hamper College of Arts and Sciences, University of Alabama at Birmingham, primary production