Antarctic Ocean Legacy: a Vision for Circumpolar Protection Executive Summary
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The Kerguelen Plateau: Marine Ecosystem + Fisheries
THE KERGUELEN PLATEAU: MARINE ECOSYSTEM + FISHERIES Proceedings of the Second Symposium Kerguelen plateau Marine Ecosystems & Fisheries • SYMPOSIUM 2017 heardisland.antarctica.gov.au/research/kerguelen-plateau-symposium Important readjustments in the biomass and distribution of groundfish species in the northern part of the Kerguelen Plateau and Skiff Bank Guy Duhamel1, Clara Péron1, Romain Sinègre1, Charlotte Chazeau1, Nicolas Gasco1, Mélyne Hautecœur1, Alexis Martin1, Isabelle Durand2 and Romain Causse1 1 Muséum national d’Histoire naturelle, Département Adaptations du vivant, UMR 7208 BOREA (MNHN, CNRS, IRD, Sorbonne Université, UCB, UA), CP 26, 43 rue Cuvier, 75231 Paris cedex 05, France 2 Muséum national d’Histoire naturelle, Département Origines et Evolution, UMR 7159 LOCEAN (Sorbonne Université, IRD, CNRS, MNHN), CP 26, 43 rue Cuvier, 75231 Paris cedex 05, France Corresponding author: [email protected] Abstract The recent changes in the conservation status (establishment and extension of a marine reserve) and the long history of fishing in the Kerguelen Islands exclusive economic zone (EEZ) (Indian sector of the Southern Ocean) justified undertaking a fish biomass evaluation. This study analysed four groundfish biomass surveys (POKER 1–4) conducted from 2006 to 2017 across depths ranging from 100 to 1 000 m. Forty demersal species were recorded in total and density distributions of twenty presented. However, only seven species account for the majority of the biomass (96%). Total biomass was 250 000 tonnes during the first three surveys (POKER 1–3), and 400 000 tonnes for POKER 4 due to a high catch of marbled notothen (Notothenia rossii) and mackerel icefish (Champsocephalus gunnari) (accounting for 44% and 17% of the 400 000 tonnes biomass respectively). -
The Antarctic Coastal Current in the Bellingshausen Sea
The Cryosphere, 15, 4179–4199, 2021 https://doi.org/10.5194/tc-15-4179-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. The Antarctic Coastal Current in the Bellingshausen Sea Ryan Schubert1, Andrew F. Thompson3, Kevin Speer1, Lena Schulze Chretien4, and Yana Bebieva1,2 1Geophysical Fluid Dynamics Institute, Florida State University, Tallahassee, Florida 32306, USA 2Department of Scientific Computing, Florida State University, Tallahassee, Florida 32306, USA 3Environmental Science and Engineering, California Institute of Technology, Pasadena, CA 91125, USA 4Department of Biology and Marine Science, Marine Science Research Institute, Jacksonville University, Jacksonville, Florida, USA Correspondence: Ryan Schubert ([email protected]) Received: 4 February 2021 – Discussion started: 19 February 2021 Revised: 20 July 2021 – Accepted: 21 July 2021 – Published: 1 September 2021 Abstract. The ice shelves of the West Antarctic Ice Sheet 1 Introduction experience basal melting induced by underlying warm, salty Circumpolar Deep Water. Basal meltwater, along with runoff from ice sheets, supplies fresh buoyant water to a circula- The Antarctic continental slope in West Antarctica, spanning tion feature near the coast, the Antarctic Coastal Current the West Antarctic Peninsula (WAP) to the western Amund- (AACC). The formation, structure, and coherence of the sen Sea, is characterized by a shoaling of the subsurface tem- AACC has been well documented along the West Antarc- perature maximum, which allows warm, salty Circumpolar tic Peninsula (WAP). Observations from instrumented seals Deep Water (CDW) greater access to the continental shelf. collected in the Bellingshausen Sea offer extensive hydro- This leads to an increase in the oceanic heat content over the graphic coverage throughout the year, providing evidence of shelf in this region compared to other Antarctic shelf seas the continuation of the westward flowing AACC from the (Schmidtko et al., 2014). -
Advance and Unedited Reporting Material for the Resumed Review
Advance and unedited reporting material for the resumed Review Conference on the Agreement for the Implementation of the Provisions of the United Nations Convention on the Law of the Sea of 10 December 1982 relating to the Conservation and Management of Straddling Fish Stocks and Highly Migratory Fish Stocks (New York, 23-27 May 2016) (English only) Summary The present report has been prepared in response to the request made to the Secretary-General, in paragraph 41 of General Assembly resolution 69/109, to submit to the resumed Review Conference on the Agreement for the Implementation of the Provisions of the United Nations Convention on the Law of the Sea of 10 December 1982 relating to the Conservation and Management of Straddling Fish Stocks and Highly Migratory Fish Stocks (the Agreement) an updated comprehensive report, prepared in cooperation with the Food and Agriculture Organization of the United Nations (FAO), to assist the Conference in discharging its mandate under article 36, paragraph 2, of the Agreement. It is also based on information provided by States and regional fisheries management organizations and arrangements and other related bodies, in response to a questionnaire circulated in March 2015. The report provides an update of information contained in the reports of the Secretary-General to the Review Conference in 20061 and 2010. 2 1 A/CONF.210/2006/1. 2 A/CONF.210/2010/1. Contents Page Abbreviations .............................................................. I. Introduction................................................................ II. Overview of the status and trends of straddling fish stocks and highly migratory fish stocks, discrete high seas stocks and non-target, associated and dependent species ........................ -
Variations in the Diet Composition and Feeding Intensity of Mackerel Icefish Champsocephalus Gunnariat South Georgia (Antarctic)
MARINE ECOLOGY PROGRESS SERIES Published May 12 Mar. Ecol. Prog. Ser. Variations in the diet composition and feeding intensity of mackerel icefish Champsocephalus gunnari at South Georgia (Antarctic) K.-H. Kock l, S. Wilhelms 2, I. Everson3, J. Groger 'Institut fiir Seefischerei, Bundesforschungsanstalt fur Fischerei, Palmaille 9, D-22767 Hamburg, Germany 'Deutsches Ozeanographisches Datenzentrum, Bundesamt fiir Seeschiffahrt und Hydrographie, Bernhard-Nocht StraOe, D-20359 Hamburg, Germany 3British Antarctic Survey, High Cross Madingley Road, Cambridge CB3 OET. United Kingdom 41nstitut fur Ostseefischerei, Bundesforschungsanstalt fiir Fischerei, An der Jlgerbak 2, D-18069 Rostock, Germany ABSTRACT. The diet composition and feeding intensity of mackerel icefish Champsocephalus gunnari around Shag Rocks and the mainland of South Georgia was analyzed from ca 8700 stomachs collected in January/February 1985, January/February 1991 and January 1992. Main prey items were krill Euphausia superba, the amphipod hyperiid Themisto gaudrchaudii, mysids (primarily Antarctomysis maxima), and in 1985 also Thysanoessa species The proportion of krill and 7: gaudichaudii in the diet varied considerably among the 3 years, whereas the proportion of mysids in the diet rema~nedfairly constant. Krill appears to be the preferred food. In years of krill shortage, such as in 1991, krill was replaced by 7: gaudichaudii. The occurrence of krill in the diet in 1991 was among the lowest within a 28 yr period of investigation. Variation in food composition among sampling sites was high. This high variat~onappears to be primarily associated with differences in prey availability, but much less with prey size selectivity. Feeding intensity varied considerably among seasons. It was highest in 1992. -
Federal Register/Vol. 86, No. 147/Wednesday, August 4, 2021
Federal Register / Vol. 86, No. 147 / Wednesday, August 4, 2021 / Proposed Rules 41917 Bureau at (202) 418–0530 (VOICE), (202) Community Channel No. (1) Electronically: Go to the Federal 418–0432 (TTY). eRulemaking Portal: http:// This document does not contain www.regulations.gov. In the Search box, information collection requirements ***** enter FWS–HQ–ES–2021–0043, which subject to the Paperwork Reduction Act is the docket number for this of 1995, Public Law 104–13. In addition, NEVADA rulemaking. Then, click on the Search therefore, it does not contain any button. On the resulting page, in the proposed information collection burden ***** Search panel on the left side of the ‘‘for small business concerns with fewer Henderson ............................ 24 screen, under the Document Type than 25 employees,’’ pursuant to the heading, check the Proposed Rule box to Small Business Paperwork Relief Act of ***** locate this document. You may submit 2002, Public Law 107–198, see 44 U.S.C. a comment by clicking on ‘‘Comment.’’ 3506(c)(4). Provisions of the Regulatory [FR Doc. 2021–16589 Filed 8–3–21; 8:45 am] (2) By hard copy: Submit by U.S. mail Flexibility Act of 1980, 5 U.S.C. 601– BILLING CODE 6712–01–P to: Public Comments Processing, Attn: 612, do not apply to this proceeding. FWS–HQ–ES–2021–0043, U.S. Fish and Members of the public should note Wildlife Service, MS: PRB/3W, 5275 that all ex parte contacts are prohibited DEPARTMENT OF THE INTERIOR Leesburg Pike, Falls Church, VA 22041– from the time a Notice of Proposed 3803. -
Age-Length Composition of Mackerel Icefish (Champsocephalus Gunnari, Perciformes, Notothenioidei, Channichthyidae) from Different Parts of the South Georgia Shelf
CCAMLR Scieilce, Vol. 8 (2001): 133-146 AGE-LENGTH COMPOSITION OF MACKEREL ICEFISH (CHAMPSOCEPHALUS GUNNARI, PERCIFORMES, NOTOTHENIOIDEI, CHANNICHTHYIDAE) FROM DIFFERENT PARTS OF THE SOUTH GEORGIA SHELF G.A. Frolkina AtlantNIRO 5 Dmitry Donskoy Street Kaliningrad 236000, Russia Email - atlantQbaltnet.ru Abstract Biostatistical data obtained by Soviet research and commercial vessels from 1970 to 1991 have been used to determine tlne age-length composition of mackerel icefish (Chnnzpsoceplzalus g~~izllnrl)from different parts of the South Georgia area. An analysis of the spatial distribution of C. giirzrznri size and age groups over the eastern, northern, western and soutlnern parts of tlne shelf, and near Shag Rocks, revealed a similar age-leingtl~composition for young fish inhabiting areas to the west of the island and near Shag Rocks. Differences were observed between those t~7ogroups and the easterin group. The larger number of mature fish in the west is related to the migration of maturing individuals from the eastern and western parts of the area. It is implied that part of tlne western group migrates towards Shag Rocks at the age of 2-3 years. It has been found that, by number, recruits represent the largest part of tlne population, whether a fishery is operating or not. As a result of this, as well as the species' ability to live not only in off- bottom, but also in pelagic waters, an earlier age of sexual maturity compared to other nototheniids, and favourable oceanographic conditions, the C. g~lrliznrl stock could potentially recover quickly from declines in stock size and inay become abundant in the area, as has bee11 demonstrated on several occasions in the 1970s and 1980s. -
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. -
A GUIDE to IDENTIFICATION of FISHES CAUGHT ALONG with the ANTARCTIC KRILL Author(S) 1) Iwami, T
Document No. [ to be completed by the Secretariat ] WG-EMM-07/32 Date submitted [ to be completed by the Secretariat ] 1 July 2007 Language [ to be completed by the Secretariat ] Original: English Agenda Agenda Item No(s): 4.3 Title A GUIDE TO IDENTIFICATION OF FISHES CAUGHT ALONG WITH THE ANTARCTIC KRILL Author(s) 1) Iwami, T. and 2) M. Naganobu Affiliation(s) 1) Laboratory of Biology, Tokyo Kasei Gakuin University 2) National Research Institute of Far Seas Fisheries Published or accepted for publication elsewhere? Yes No x If published, give details ABSTRACT A field key to early life stages of Antarctic fish caught along with the Antarctic krill is produced. The key includes 8 families and 28 species mainly from the Atlantic sector of the Southern Ocean and uses distinguished characters which permit rapid field identification. In some cases, however, it is impossible to discriminate among species of the same family by remarkable characters. A species key is not shown for such resemble species and a brief summary of the main morphological features of species and genera is provided. SUMMARY OF FINDINGS AS RELATED TO NOMINATED AGENDA ITEMS Agenda Item Finding 4.3 We are producing a practical field key to juvenile fish caught along with the Antarctic Scientific krill. To our knowledge more than 40 species of fish have been found as by-catch. Observation However, the number of dominant fish species found in the krill catch never exceeds 20 species. An useful and practical identification key to these dominant species maybe facilitate the quantitative assessment of fish in the krill catch. -
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. -
Variability in Cenozoic Sedimentation Along the Continental Rise of the Bellingshausen Sea, West Antarctica ⁎ Carsten Scheuer A, , Karsten Gohl A, Robert D
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Electronic Publication Information Center Marine Geology 227 (2006) 279–298 www.elsevier.com/locate/margeo Variability in Cenozoic sedimentation along the continental rise of the Bellingshausen Sea, West Antarctica ⁎ Carsten Scheuer a, , Karsten Gohl a, Robert D. Larter b, Michele Rebesco c, Gleb Udintsev d a Alfred Wegener Institute for Polar and Marine Research (AWI), Postfach 120161, D-27515, Bremerhaven, Germany b British Antarctic Survey (BAS), High Cross, Madingley Road, Cambridge CB3 OET, UK c Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS), Borgo Grotta Gigante 42/C, 34010 Sconico (TS), Italy d Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 19, Kosygin Str, 117975 Moscow, Russia Received 29 September 2004; received in revised form 16 December 2005; accepted 21 December 2005 Abstract Seismic reflection profiles, bathymetric and magnetic data collected along and across the continental margin of the Bellingshausen Sea provide new constraints and interpretations of the oceanic basement structure and Cenozoic glacial history of West Antarctica. Evidence for tectonic boundaries that lie perpendicular to the margin has been identified on the basis of one previously unpublished along-slope multichannel seismic reflection profile. By combining several magnetic data sets, we determined basement ages and verified the positions of possible fracture zones, enabling us to improve previous tectonic and stratigraphic models. We establish three main sediment units on the basis of one seismic along-slope profile and by correlation to the continental shelf via one cross-slope profile. We interpret a lowermost unit, Be3 (older then 9.6 Ma), as representing a long period of slow accumulation of mainly turbiditic sediments. -
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. -
Ice Core Records of 20Th Century Sea Ice Decline in the Bellingshausen Sea, Geophysical Research Letters, Submitted
R. Röthlisberger and N. Abram Abram, N., McConnell, J.R., Thomas, E.R., Mulvaney, R. and Aristarain, A.J., 2008: Ice core records of 20th century sea ice decline in the Bellingshausen Sea, Geophysical Research Letters, submitted. Abram, N., Mulvaney, R., Wolff, E.W. and Mudelsee, M., 2007: Ice core records as sea ice proxies: an evaluation from the Weddell Sea region of Antarctica, Journal of Geophysical Research, 112: D15101, doi:15110.11029/12006JD008139. Castebrunet, H., Genthon, C. and Martinerie, P., 2006: Sulfur cycle at Last Glacial Maximum: Model results versus Antarctic ice core data, Geophysical Research Letters, 33: L22711, doi:10.1029/2006GL027681. Crosta, X., Sturm, A., Armand, L. and Pichon, J.J., 2004: Late Quaternary sea ice history in the Indian sector of the Southern Ocean as recorded by diatom assemblages, Marine Micropaleontology, 50: 209-223. Curran, M.A.J. and Jones, G.B., 2000: Dimethyl sulfide in the Southern Ocean: Seasonality and flux, Journal of Geophysical Research, 105: 20451-20459. Curran, M.A.J., van Ommen, T.D., Morgan, V.I., Phillips, K.L. and Palmer, A.S., 2003: Ice core evidence for Antarctic sea ice decline since the 1950s, Science, 302: 1203-1206. Foster, A.F.M., Curran, M.A.J., Smith, B.T., van Ommen, T.D. and Morgan, V.I., 2006: Covariation of sea ice and methanesulphonic acid in Wilhelm II Land, East Antarctica, Annals of Glaciology, 44: 429-432. Fundel, F., Fischer, H., Weller, R., Traufetter, F., Oerter, H. and Miller, H., 2006: Influence of large-scale teleconnection patterns on methane sulfonate ice core records in Dronning Maud Land, Journal of Geophysical Research, 111: (D04103), doi:10.1029/2005JD005872.