Can Fishing in the Ross Sea Be Sustainable? Leo Salas, Ph.D

Total Page:16

File Type:pdf, Size:1020Kb

Can Fishing in the Ross Sea Be Sustainable? Leo Salas, Ph.D Can fishing in the Ross Sea be sustainable? Leo Salas, Ph.D. [email protected] Humans have removed 90% of Besides being the largest fish in feasible metrics to monitor the big fish from every ocean in Antarctic waters, toothfish is also include seal population numbers, the planet, except for the among the most energy-rich. breeding propensity, diving effort, Southern Ocean, especially the Because of these two factors, It and toothfish consumption rate. Ross Sea. But that may be has been suggested that toothfish changing. Since 2003, the largest may be critical for mass recovery Main Points (more than twice as big as the in mother seals. next species) fish in Antarctica is Weddell seals may not Using all the scientific evidence being removed from the Ross Sea. recover sufficiently from available, the team constructed a nursing their pups without That fish is the Antarctic toothfish, the largest and model to determine how much toothfish, usually sold as Chilean among the most energy- energy the seals must consume seabass. The fishery target is to dense fish in Antarctic waters. reduce the total number of adult during the recovery period to maintain population numbers. The toothfish fishery is toothfish by 50% over a 35 year likely already adversely That model was coupled with a period. affecting seal populations. simulation of prey consumption The fishery may be Is the fishery affecting the to establish the role of toothfish sustainable at lower Antarctic ecosystem? If so, how, in sustaining seal populations. extraction rates. Monitoring of seal and by how much? A team of The results show that some populations is important to researchers, led by Point Blue ensure this fishery is consumption of toothfish is Conservation Science, sought to sustainable. answer these questions by paramount for Weddell seals to maintain a stable population focusing on the potential impact numbers. There are substantial Salas, L., N. Nur, D. Ainley, J. of the fishery on a toothfish Burns, J. Rotella, and G. Ballard (in reasons to expect that Weddell press). Coping with the loss of predator, the Weddell seal. seal populations are already large, energy-dense prey: A potential bottleneck for Weddell Weddell seal mothers may lose as severely impacted by the fishery. Seals in the Ross Sea. Ecological much as 40% of their body mass Findings also suggest that the Applications. http://onlinelibrary.wiley.com/doi/10. while nursing their pups. To breed fishery may be sustainable at 1002/eap.1435/full again, they must recover this lower extraction rates. mass. How quickly they recover is This research highlights areas of also correlated with the chances their pup survives and reaches critical importance for further adulthood, all of which eventually study and monitoring to ensure that the fishery is managed affects seal population numbers. sustainably. Important and January 2017, Point Blue Conservation Science visit www.pointblue.org/publication-briefs .
Recommended publications
  • The Ross Sea Dipole - Temperature, Snow Accumulation and Sea Ice Variability in the Ross Sea Region, Antarctica, Over the Past 2,700 Years
    Clim. Past Discuss., https://doi.org/10.5194/cp-2017-95 Manuscript under review for journal Clim. Past Discussion started: 1 August 2017 c Author(s) 2017. CC BY 4.0 License. The Ross Sea Dipole - Temperature, Snow Accumulation and Sea Ice Variability in the Ross Sea Region, Antarctica, over the Past 2,700 Years 5 RICE Community (Nancy A.N. Bertler1,2, Howard Conway3, Dorthe Dahl-Jensen4, Daniel B. Emanuelsson1,2, Mai Winstrup4, Paul T. Vallelonga4, James E. Lee5, Ed J. Brook5, Jeffrey P. Severinghaus6, Taylor J. Fudge3, Elizabeth D. Keller2, W. Troy Baisden2, Richard C.A. Hindmarsh7, Peter D. Neff8, Thomas Blunier4, Ross Edwards9, Paul A. Mayewski10, Sepp Kipfstuhl11, Christo Buizert5, Silvia Canessa2, Ruzica Dadic1, Helle 10 A. Kjær4, Andrei Kurbatov10, Dongqi Zhang12,13, Ed D. Waddington3, Giovanni Baccolo14, Thomas Beers10, Hannah J. Brightley1,2, Lionel Carter1, David Clemens-Sewall15, Viorela G. Ciobanu4, Barbara Delmonte14, Lukas Eling1,2, Aja A. Ellis16, Shruthi Ganesh17, Nicholas R. Golledge1,2, Skylar Haines10, Michael Handley10, Robert L. Hawley15, Chad M. Hogan18, Katelyn M. Johnson1,2, Elena Korotkikh10, Daniel P. Lowry1, Darcy Mandeno1, Robert M. McKay1, James A. Menking5, Timothy R. Naish1, 15 Caroline Noerling11, Agathe Ollive19, Anaïs Orsi20, Bernadette C. Proemse18, Alexander R. Pyne1, Rebecca L. Pyne2, James Renwick1, Reed P. Scherer21, Stefanie Semper22, M. Simonsen4, Sharon B. Sneed10, Eric J., Steig3, Andrea Tuohy23, Abhijith Ulayottil Venugopal1,2, Fernando Valero-Delgado11, Janani Venkatesh17, Feitang Wang24, Shimeng
    [Show full text]
  • The Ross Sea: a Valuable Reference Area to Assess the Effects of Climate Change
    IP (number) Agenda Item: CEP 7e, ATCM 13 Presented by: ASOC Original: English The Ross Sea: A Valuable Reference Area to Assess the Effects of Climate Change 1 IP (number) Summary International Panel on Climate Change models predict that the Ross Sea will be the last portion of the Southern Ocean with sea ice year round. Currently, the Ross Sea ecosystem is considered to be relatively little affected by direct human-related impacts other than the past exploitation of marine mammals along its slope and the recent exploratory Antarctic toothfish fishery. The indirect human impacts of CO2 pollution on melting ice and ocean acidification have yet to be felt. The Ross Sea - with its several very long biotic and hydrographic data sets - constitutes an important reference area to gauge the ecosystem effects of climate change and distinguish those effects from the effects of current fisheries, tourism, and historic overexploitation and recovery or lack of recovery of some seal, whale, and fish populations elsewhere. This, in conjunction with a range of other scientific and biological reasons that has been laid out in prior ASOC papers, underpins why the Ross Sea should be included as a key component in the network of marine protected areas currently being considered for the Southern Ocean by the Commission for the Conservation of Antarctic Marine Living Resources (CCAMLR). 1. Introduction Over the past few years, ASOC has put forward a number of papers making the ‘science case’ for supporting full protection of the Ross Sea slope and shelf,1 in the context of establishing an important component of a representative network of MPAs in the Southern Ocean.2 This paper focuses on the climate reference zone potential of the Ross Sea.
    [Show full text]
  • S41467-018-05625-3.Pdf
    ARTICLE DOI: 10.1038/s41467-018-05625-3 OPEN Holocene reconfiguration and readvance of the East Antarctic Ice Sheet Sarah L. Greenwood 1, Lauren M. Simkins2,3, Anna Ruth W. Halberstadt 2,4, Lindsay O. Prothro2 & John B. Anderson2 How ice sheets respond to changes in their grounding line is important in understanding ice sheet vulnerability to climate and ocean changes. The interplay between regional grounding 1234567890():,; line change and potentially diverse ice flow behaviour of contributing catchments is relevant to an ice sheet’s stability and resilience to change. At the last glacial maximum, marine-based ice streams in the western Ross Sea were fed by numerous catchments draining the East Antarctic Ice Sheet. Here we present geomorphological and acoustic stratigraphic evidence of ice sheet reorganisation in the South Victoria Land (SVL) sector of the western Ross Sea. The opening of a grounding line embayment unzipped ice sheet sub-sectors, enabled an ice flow direction change and triggered enhanced flow from SVL outlet glaciers. These relatively small catchments behaved independently of regional grounding line retreat, instead driving an ice sheet readvance that delivered a significant volume of ice to the ocean and was sustained for centuries. 1 Department of Geological Sciences, Stockholm University, Stockholm 10691, Sweden. 2 Department of Earth, Environmental and Planetary Sciences, Rice University, Houston, TX 77005, USA. 3 Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA. 4 Department
    [Show full text]
  • Ice Production in Ross Ice Shelf Polynyas During 2017–2018 from Sentinel–1 SAR Images
    remote sensing Article Ice Production in Ross Ice Shelf Polynyas during 2017–2018 from Sentinel–1 SAR Images Liyun Dai 1,2, Hongjie Xie 2,3,* , Stephen F. Ackley 2,3 and Alberto M. Mestas-Nuñez 2,3 1 Key Laboratory of Remote Sensing of Gansu Province, Heihe Remote Sensing Experimental Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China; [email protected] 2 Laboratory for Remote Sensing and Geoinformatics, Department of Geological Sciences, University of Texas at San Antonio, San Antonio, TX 78249, USA; [email protected] (S.F.A.); [email protected] (A.M.M.-N.) 3 Center for Advanced Measurements in Extreme Environments, University of Texas at San Antonio, San Antonio, TX 78249, USA * Correspondence: [email protected]; Tel.: +1-210-4585445 Received: 21 April 2020; Accepted: 5 May 2020; Published: 7 May 2020 Abstract: High sea ice production (SIP) generates high-salinity water, thus, influencing the global thermohaline circulation. Estimation from passive microwave data and heat flux models have indicated that the Ross Ice Shelf polynya (RISP) may be the highest SIP region in the Southern Oceans. However, the coarse spatial resolution of passive microwave data limited the accuracy of these estimates. The Sentinel-1 Synthetic Aperture Radar dataset with high spatial and temporal resolution provides an unprecedented opportunity to more accurately distinguish both polynya area/extent and occurrence. In this study, the SIPs of RISP and McMurdo Sound polynya (MSP) from 1 March–30 November 2017 and 2018 are calculated based on Sentinel-1 SAR data (for area/extent) and AMSR2 data (for ice thickness).
    [Show full text]
  • A Balanced Model of the Food Web of the Ross Sea, Antarctica
    CCAMLR Science, Vol. 17 (2010): 1–31 A BALANCED MODEL OF THE FOOD WEB OF THE ROSS SEA, ANTARCTICA M.H. Pinkerton, J.M. Bradford-Grieve National Institute of Water and Atmospheric Research (NIWA) Ltd Private Bag 14901, Wellington 6241 New Zealand Email – [email protected] S.M. Hanchet NIWA Ltd PO Box 893, Nelson 7040 New Zealand Abstract A quantitative food web of the Ross Sea is presented here as a step towards investigating ecosystem effects of the fishery for Antarctic toothfishDissostichus ( mawsoni). The model consolidates quantitative information on trophic links across all the major biota of the Ross Sea and tests for data consistency. The model has 38 trophic groups and is balanced in terms of annual flows of organic carbon in an average recent year (1990–2000). The focus of the model is on the role of Antarctic toothfish in the food web which means that the model has greater taxonomic resolution towards the top of the food web than the base. A survey of the available literature and both published and unpublished data provided an initial set of parameters describing the annual average abundance, imports, exports, energetics (growth, reproduction, consumption) and trophic linkages (diets, key predators) for each model group. The relative level of uncertainty on these parameters was also estimated. This set of parameters was not self consistent, and a method is described to adjust the initial parameter set to give a balanced model, taking into account the estimates of parameter uncertainty and the large range of magnitude (>6 orders of magnitude) in trophic flows between groups.
    [Show full text]
  • Buenos Aires Or Santiago 
    ANTARCTICA NEW! ANTARCTICA + PATAGONIA, ARGENTINA TO SOUTH GEORGIA GO DEEP ABOARD OUR POLAR FLEET SOLAR ECLIPSE PATH IN 2021 PLUS FREE AIR 2021-2023 VOYAGES | EXPEDITIONS.COM Hanusse Bay, Antarctica 66.56° S, 67.29° W Realizing that out here in pure wildness, curiosity is mutual. That’s the exhilaration of discovery. TABLE OF CONTENTS 2 Going Where Awesome Is 4 The Perfect Platform 8 Freedom to Explore 10 Our Expedition Team 12 Undersea Discoveries 16 National Geographic Photographers 18 Antarctica: The White Continent 20 Itinerary: Journey to Antarctica 22 Itinerary: Antarctica & Patagonia: Legendary Ice & Epic Fjords NEW 26 Antarctica, South Georgia & the Falklands 28 Itinerary: South Georgia & the Falklands 30 Itinerary: Antarctica, South Georgia & the Falklands 32 Itinerary: Wild Coasts of Argentina, South Georgia & the Falklands NEW 34 Epic Antarctica: The Peninsula to the Ross Sea & Beyond 36 Itinerary: Epic Antarctica 38 Explore More: Optional Extensions 40 Life Aboard 42 Dining Aboard 44 National Geographic Explorer 46 National Geographic Endurance/National Geographic Resolution 48 Offers, Terms & Conditions ICE FEVER: IT’S A THING 2 GOING WHERE AWESOME IS EDIFYING. EXHILARATING. AND DEEPLY MOVING. The Antarctic ice sheet is the most distinctive feature of Earth as seen from space—every astronaut’s account mentions it. And the ice is what makes every Antarctic explorer vow to return. There’s a whole glossary of ice words to learn—macro-scale terms like fast ice, leads, and growlers, to more granular terms like brash and bergy The single best whale encounter bits. Ice is visually stunning, and nearly kaleidoscopic in I’ve ever had.
    [Show full text]
  • Chapter 34: Australia, Oceania, and Antarctica Today
    GeoJournal As you read this chapter, use your journal to log the key economic activities of Australia, Chapter Overview Visit the Glencoe World Oceania, and Antarctica. Note interesting Geography Web site at geography.glencoe.com details that illustrate the ways in which and click on Chapter Overviews—Chapter 34 to human activities and the region’s environ- preview information about the region today. ment are interrelated. Guide to Reading Living in Australia, Consider What You Know Oceania, and Environments in Australia, Oceania, and Antarctica range from tropical rain forests to icy wastelands. What Antarctica attractions or activities might draw people to visit or live in a region with such extreme differences in the physical environment? Reading Strategy A Geographic View Organizing Complete a web diagram similar to the one below by filling in Antarctic Diving the developing South Pacific countries that receive much-needed income There’s something special about from tourism. peering beneath the bottom of the world. When Antarctica’s summer diving season begins in September Developing Countries the sun has been largely absent for six months, and the water . has become as clear as any in the Read to Find Out world. Visibility is measured not in feet but in football fields. • How do people in Australia, New . Only here can you orbit an Zealand, and Oceania make their electric-blue iceberg while livings? being serenaded by the eerie View from under Antarctic ice • What role does trade play in trills of Weddell seals. the economies of South Pacific countries? —Norbert Wu, “Under Antarctic Ice,” National Geographic, February 1999 • What means of transportation and communications are used in the region? Terms to Know The wonders hidden under Antarctic ice are • station among the many attractions of Australia, Oceania, and Antarctica.
    [Show full text]
  • The Ross Sea, Antarctica: a Sylvia Earle Alliance Hope Spot Initiative Protecting Our Ocean – Introducing Hope Spots
    The Ross Sea, Antarctica: A Sylvia Earle Alliance Hope Spot Initiative Protecting Our Ocean – Introducing Hope Spots Currently about 1.2% of the world ocean is set aside for wildlife and their habitat, as compared to around 14% of Earth’s terrestrial surface. We must take action to increase substantially the level of ocean protection that experts consider necessary for healthier oceans and a more sustainable fisheries future. Hope Spots are ocean areas that are especially important for their wildlife and habitats, and merit urgent and effective protection. One of the most important Hope Spots is the Ross Sea in Antarctica. The Antarctic and Southern Ocean Coalition (ASOC) and the Last Ocean Project have been working to protect the Ross Sea for the past four years. They are now joining forces with Mission Blue partners including the Sylvia Earle Alliance, International Union for Conservation of Nature (IUCN) and its World Commission on Protected Areas (WCPA), and the National Geographic Society to secure Marine Protected Area status for the entire Ross Sea shelf and slope ecosystem and superadjacent waters – 647,194 km2, or about 2% of the Southern Ocean. Toothfish and Wedell Seal © Jessica Meir Other Images © John Weller I wish you would use all means at your disposal to ignite public support for a global network of marine protected areas, Hope Spots large enough to save and restore the ocean, the blue heart of the planet. — TED Wish of Dr. Sylvia A. Earle The Importance of the Ross Sea Key Species The Ross Sea is called “the last ocean” because it is widely Although the Ross Sea shelf and slope and superadjacent recognized as the only remaining large ocean region on Earth in waters comprise just 2% of the Southern Ocean, they are home which the ecosystem is structured by natural rather than human to an estimated: forces.
    [Show full text]
  • The Silica Cycle in the Antarctic Ocean: Is the Weddell Sea Atypical?
    MARINE ECOLOGY PROGRESS SERIES Vol. 96: 1-15, 1993 Published June 3 Mar. Ecol. Prog. Ser. The silica cycle in the Antarctic Ocean: is the Weddell Sea atypical? Aude Leynaert l, David M. ~elson~,Bernard Queguinerl, Paul ~reguer' 'URA CNRS 1513, Institut d'Etudes Marines, BP 452, F-29275 Brest Cedex, France 'College of Oceanography. Oregon State University, Corvallis, Oregon 97331-5503. USA ABSTRACT: The lowest biogenic silica production rates in the Southern Ocean (average of 2.59 mm01 Si m-2 d-l) have been recorded in an area of heavy ice cover along a transect through the Weddell Sea from Joinville Island to Cap Norvegia (November-December 1990). The associated biomass was also very low (concentrations 50.6 pm01 1-I for biogenic silica and S0.8 pg I-' for chlorophyll a).Based upon these direct measurements of biogenic silica production rates and other data available from the mar- ginal ice zone and open ocean areas, we estimated the annual production of biogenlc silica in the northern Weddell Sea to be 810 to 870 rnrnol m-2 yrrl. Thls leads to a revised estimate of the total annual biogenic sdxa production in the Southern Ocean of between 11 and 32 Tmol Si yr-l. Comparing our annual production estimate to previous estimates of vertical flux of opal in the Weddell Sea, we conclude that no more than 1% of the silica produced annually by phytoplankton in the upper water column reaches a depth of 800 m. This is consistent with the general distribution of high accumulation rates of opal in Southern Ocean sedirnents which evidence an unexplained gap in the Weddell Sea.
    [Show full text]
  • Oceanography of Antarctic Waters
    Antarctic Research Series Antarctic Oceanology I Vol. 15 OCEANOGRAPHY OF ANTARCTIC WATERS ARNOLD L. GORDON Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964 Abstract. The physical oceanography for the southwest Atlantic and Pacific sectors of antarctic waters is investigated with particular reference to the water structure and meridional circula­ tion. The cyclonic gyres of the Weddell Sea and area to the north and northeast of the Ross Sea are regions of intense deep water upwelling. Water at 400 meters within these gyres occurs at depths below 2000 meters before entering the gyral circulation. The northern boundary for the Weddell gyre is the Weddell-Scotia Confluence, and that for the gyre near the Ross Sea is the secondary polar front zone. The major region for production of Antarctic Bottom Water is the Weddell Sea, whereas minor sources are found in the Ross Sea region and perhaps in the Indian Ocean sector in the vicinity of the Amery Ice Shelf. The Ross Sea Shelf Water contains, in part, water related to a freezing process at the base of the Ross Ice Shelf. The mechanism may be of local importance in bottom water production. The salt balance within the Antarctic Surface Water indicates approximately 60 X 106 m3/sec of deep water upwells into the surface layer during the summer. This value is also found from Ekman divergence calculation. In winter, only one half of this value remains with the surface water; the other half sinks in the production of bottom water. An equal part of deep water is entrained by the sinking water, making the total southward migration of deep water 108 m3/sec during the winter.
    [Show full text]
  • THE Case for a Marine Reserve in the Ross Sea
    THE CASE FOR A MARINE RESERVE IN THE ROSS SEA The Ross Sea is among the most hauntingly beautiful and species- rich marine environments in the world. Covering 3.6 million square kilometres (1.9 million square miles) in a horseshoe-shaped embayment clinging to the Antarctic coast south of New Zealand, the region supports species that have thrived essentially as they have for millennia. At the urging of scientists and conservation leaders, 24 countries and the European Union are expected to decide whether to create permanent protections for the Ross Sea or leave it vulnerable to large-scale industrial fishing. COUNTDOWN TO CONSENSUS: CREATING ANTARcTIC MARINE RESERVES THE CASE FOR A MARINE RESERVE IN THE ROSS SEA Vital to species and science A 2011 study published in the journal The Ross Sea designation Biological Conservation called the Ross Sea must be permanent. “the least altered marine ecosystem on Earth,” with unusually large and closely interacting Instead of applying a sunset populations of several marine bird and mammal species. The study found that nine predators clause, The Pew Charitable in the region—including emperor and Adélie penguins, minke whales, crabeater seals, Trusts calls on CCAMLR to and snow petrels—use the entire continental agree on a standard review shelf and slope as a naturally choreographed behavioral opera that allows large populations clause for use on all future MPAs. of these species to coexist. CurrentRoss U.S.–N.Z.Sea Marine Ross Protection Sea Proposal Proposals and Historic and ToothfishAOA Proposed
    [Show full text]
  • Constraints on Soluble Aerosol Iron Flux to the Southern Ocean
    ARTICLE Received 17 Feb 2015 | Accepted 17 Jun 2015 | Published 23 Jul 2015 DOI: 10.1038/ncomms8850 OPEN Constraints on soluble aerosol iron flux to the Southern Ocean at the Last Glacial Maximum T.M. Conway1,2,w, E.W. Wolff1,2,R.Ro¨thlisberger2,w, R. Mulvaney2 & H.E. Elderfield1 Relief of iron (Fe) limitation in the Southern Ocean during ice ages, with potentially increased carbon storage in the ocean, has been invoked as one driver of glacial–interglacial atmospheric CO2 cycles. Ice and marine sediment records demonstrate that atmospheric dust supply to the oceans increased by up to an order of magnitude during glacial intervals. However, poor constraints on soluble atmospheric Fe fluxes to the oceans limit assessment of the role of Fe in glacial–interglacial change. Here, using novel techniques, we present esti- mates of water- and seawater-soluble Fe solubility in Last Glacial Maximum (LGM) atmo- spheric dust from the European Project for Ice Coring in Antarctica (EPICA) Dome C and Berkner Island ice cores. Fe solubility was very variable (1–42%) during the interval, and frequently higher than typically assumed by models. Soluble aerosol Fe fluxes to Dome C at the LGM (0.01–0.84 mg m À 2 per year) suggest that soluble Fe deposition to the Southern Ocean would have been Z10 Â modern deposition, rivalling upwelling supply. 1 Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK. 2 British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK. w Present addresses: Department of Earth Sciences, Institute for Geochemistry and Petrology, ETH Zu¨rich, 8092 Zu¨rich, Switzerland (T.M.C.); Federal Office for the Environment, Bern, Switzerland (R.R.).
    [Show full text]