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Interactions of Patagonian Toothfish Fisheries With
CCAMLR Science, Vol. 17 (2010): 179–195 INTERACTIONS OF PATAGONIAN TOOTHFISH FISHERIES WITH KILLER AND SPERM WHALES IN THE CROZET ISLANDS EXCLUSIVE ECONOMIC ZONE: AN ASSESSMENT OF DEPREDATION LEVELS AND INSIGHTS ON POSSIBLE MITIGATION STRATEGIES P. Tixier1, N. Gasco2, G. Duhamel2, M. Viviant1, M. Authier1 and C. Guinet1 1 Centre d’Etudes Biologiques de Chizé CNRS, UPR 1934 Villiers-en-Bois, 79360 France Email – [email protected] 2 MNHN Paris, 75005 France Abstract Within the Crozet Islands Exclusive Economic Zone (EEZ), the Patagonian toothfish (Dissostichus eleginoides) longline fishery is exposed to high levels of depredation by killer (Orcinus orca) and sperm whales (Physeter macrocephalus). From 2003 to 2008, sperm whales alone, killer whales alone, and the two species co-occurring were observed on 32.6%, 18.6% and 23.4% respectively of the 4 289 hauled lines. It was estimated that a total of 571 tonnes (€4.8 million) of Patagonian toothfish were lost due to depredation by killer whales and both killer and sperm whales. Killer whales were found to be responsible for the largest part of this loss (>75%), while sperm whales had a lower impact (>25%). Photo-identification data revealed 35 killer whales belonging to four different pods were involved in 81.3% of the interactions. Significant variations of interaction rates with killer whales were detected between vessels suggesting the influence of operational factors on depredation. When killer whales were absent at the beginning of the line hauling process, short lines (<5 000 m) provided higher yield and were significantly less impacted by depredation than longer lines. -
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 -
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Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Jean-Philippe Palasi Director for European policy Averting global biodiversity loss Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Can we avert global biodiversity loss ? That means addressing 5 direct causes: • Habitat destruction • Over exploitation • Pollution • Invasive species • Climate change Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Can we avert global biodiversity loss ? That means addressing 5 direct causes: • Habitat destruction • Over exploitation • Pollution • Invasive species • Climate change Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Can we avert global biodiversity loss ? That means addressing 5 direct causes: • Habitat destruction • Over exploitation • Pollution • Invasive species • Climate change And several root causes: • Demographic growth • Poverty • Poor governance, corruption and conflicts • Unsustainable economic models (production, Photo 1 consumption and supply chains) 4.2” x 10.31” • Lack of awareness & adequate accounting Position x: 8.74”, y: .18” Habitat destruction Climate change species confined to high altitude At 520 ppm (mid-century?) most of coral species in warm waters would scarcely support further growth. Increased droughts in the Amazon basin 2010 vegetation anomalies, Nasa Earth Observatory CC impact on species Chris Thomas (Leeds univ), Nature, 2004 « We predict, on the basis of mid-range climate-warming scenarios for 2050, that 15-37% of species (…) will be committed to exctinction » = 1 million terrestrial species by 2050 Mitigation is key: - Lower climate projections: ~18% - Mid-range: ~24% Photo 1 4.2” x 10.31” - Maximum: ~35% Position x: 8.74”, y: .18” Biodiversity loss …is a defining issues of our time …is closely linked to climate change …will carry on for decades, probably centuries …can be mitigated through profound changes in our economic and social systems Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” EU action for global biodiversity Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” EU action for global biodiversity 1. -
The Undiscovered Oil and Gas of Antarctica
DEPARTMENT OF THE INTERIOR U.S. Geological Survey The Undiscovered Oil and Gas of Antarctica by John Kingston^ OPEN-FILE REPORT 91-597 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. ^Santa Barbara, California CONTENTS Page Abstract ....................................................... 1 Introduction ................................................... 2 Size of area .............................................. 2 Premise and problems of petroleum recoverability .......... 2 Previous investigations and petroleum assessments ......... 2 Methods of assessment ..................................... 4 Regional geology and petroleum occurrence ...................... 6 Assessment by play analysis .................................... 13 Rifted continental margin provinces ....................... 13 General; the south Australia rifted margin analog .... 13 Antarctica-Australia rift province ................... 17 Antarctica-India rift province ....................... 20 Antarctica-Africa rift province ...................... 24 Antarctica-Falkland rift province .................... 24 Interior rift provinces ................................... 30 General .............................................. 30 Ross sea interior rift province ...................... 30 Weddell sea interior rift province .................. -
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. -
Investigation of Weather Anomalies in the Low-Latitude Islands of the Indian Ocean in 1991 Anne Réchou, S
Investigation of weather anomalies in the low-latitude islands of the Indian Ocean in 1991 Anne Réchou, S. Kirkwood To cite this version: Anne Réchou, S. Kirkwood. Investigation of weather anomalies in the low-latitude islands of the Indian Ocean in 1991. Annales Geophysicae, European Geosciences Union, 2015, pp.789-804. 10.5194/angeo- 33-789-2015. hal-01173951 HAL Id: hal-01173951 https://hal.archives-ouvertes.fr/hal-01173951 Submitted on 21 Oct 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Ann. Geophys., 33, 789–804, 2015 www.ann-geophys.net/33/789/2015/ doi:10.5194/angeo-33-789-2015 © Author(s) 2015. CC Attribution 3.0 License. Investigation of weather anomalies in the low-latitude islands of the Indian Ocean in 1991 A. Réchou1 and S. Kirkwood2 1Laboratoire de l’Atmosphère et des Cyclones, UMR8105, CNRS, Météo-France, Université de La Réunion, Réunion, France 2Swedish Institute of Space Physics, Box 812, 981 28 Kiruna, Sweden Correspondence to: A. Réchou ([email protected]) Received: 15 November 2014 – Revised: 13 April 2015 – Accepted: 10 June 2015 – Published: 02 July 2015 Abstract. Temperature, precipitation and sunshine duration should be more widespread, it seems unlikely that Pinatubo measurements at meteorological stations across the southern was the cause. -
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. -
Diffuse Spectral Reflectance-Derived Pliocene and Pleistocene Periodicity from Weddell Sea, Antarctica Sediment Cores
Wesleyan University The Honors College Diffuse Spectral Reflectance-derived Pliocene and Pleistocene Periodicity from Weddell Sea, Antarctica Sediment Cores by Tavo Tomás True-Alcalá Class of 2015 A thesis submitted to the faculty of Wesleyan University in partial fulfillment of the requirements for the Degree of Bachelor of Arts with Departmental Honors in Earth and Environmental Sciences Middletown, Connecticut April, 2015 Table of Contents List of Figures------------------------------------------------------------------------------IV Abstract----------------------------------------------------------------------------------------V Acknowledgements-----------------------------------------------------------------------VI 1. Introduction------------------------------------------------------------------------------1 1.1. Project Context-------------------------------------------------------------------------1 1.2. Antarctic Glacial History-------------------------------------------------------------5 1.3. Pliocene--------------------------------------------------------------------------------11 1.4. Pleistocene-----------------------------------------------------------------------------13 1.5. Weddell Sea---------------------------------------------------------------------------14 1.6. Site & Cores---------------------------------------------------------------------------19 1.7. Project Goals-------------------------------------------------------------------------22 2. Methodology----------------------------------------------------------------------------23 -
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 -
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). -
Article Size, 12 Nm Pore Size; YMC Collision Energy 15, 22.5, and 30; Isolation Window 1.0 M/Z)
Biogeosciences, 18, 3485–3504, 2021 https://doi.org/10.5194/bg-18-3485-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Archaeal intact polar lipids in polar waters: a comparison between the Amundsen and Scotia seas Charlotte L. Spencer-Jones1, Erin L. McClymont1, Nicole J. Bale2, Ellen C. Hopmans2, Stefan Schouten2,3, Juliane Müller4, E. Povl Abrahamsen5, Claire Allen5, Torsten Bickert6, Claus-Dieter Hillenbrand5, Elaine Mawbey5, Victoria Peck5, Aleksandra Svalova7, and James A. Smith5 1Department of Geography, Durham University, Lower Mountjoy, South Road, Durham, DH1 3LE, UK 2NIOZ Royal Netherlands Institute for Sea Research, Department of Marine Microbiology and Biogeochemistry, P.O. Box 59, 1790 AB Den Burg, Texel, the Netherlands 3Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands 4Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, 27568 Bremerhaven, Germany 5British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK 6MARUM – Center for Marine Environmental Sciences, University of Bremen, Leobener Str. 8, 28359, Bremen, Germany 7School of Natural and Environmental Sciences, Newcastle University, Newcastle-upon-Tyne, NE1 7RU, UK Correspondence: Charlotte L. Spencer-Jones ([email protected]) Received: 7 September 2020 – Discussion started: 5 November 2020 Revised: 3 March 2021 – Accepted: 23 March 2021 – Published: 11 June 2021 Abstract. The West Antarctic Ice Sheet (WAIS) is one of compassing the sub-Antarctic front through to the southern the largest potential sources of future sea-level rise, with boundary of the Antarctic Circumpolar Current. IPL-GDGTs glaciers draining the WAIS thinning at an accelerating rate with low cyclic diversity were detected throughout the water over the past 40 years. -
The EU and Its Overseas Entities Joining Forces on Biodiversity and Climate Change
BEST The EU and its overseas entities Joining forces on biodiversity and climate change Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Azores St-Martin Madeira St-Barth. Guadeloupe Canary islands Martinique French Guiana Reunion Outermost Regions (ORs) Azores Madeira French Guadeloupe Canary Guiana Martinique islands Reunion Azores St-Martin Madeira St-Barth. Guadeloupe Canary islands Martinique French Guiana Reunion Outermost Regions (ORs) Azores St-Martin Madeira St-Barth. Guadeloupe Canary islands Martinique French Guiana Reunion Outermost Regions (ORs) Anguilla British Virgin Is. Turks & Caïcos Caïman Islands Montserrat Sint-Marteen Sint-Eustatius Greenland Saba St Pierre & Miquelon Azores Aruba Wallis Bonaire French & Futuna Caraçao Ascension Polynesia Mayotte BIOT (British Indian Ocean Ter.) St Helena Scattered New Islands Caledonia Pitcairn Tristan da Cunha Amsterdam St-Paul South Georgia Crozet Islands TAAF (Terres Australes et Antarctiques Françaises) Iles Sandwich Falklands Kerguelen (Islas Malvinas) BAT (British Antarctic Territory) Adélie Land Overseas Countries and Territories (OCTs) Anguilla The EU overseas dimension British Virgin Is. Turks & Caïcos Caïman Islands Montserrat Sint-Marteen Sint-Eustatius Greenland Saba St Pierre & Miquelon Azores St-Martin Madeira St-Barth. Guadeloupe Canary islands Martinique Aruba French Guiana Wallis Bonaire French & Futuna Caraçao Ascension Polynesia Mayotte BIOT (British Indian Ocean Ter.) St Helena Reunion Scattered New Islands Caledonia Pitcairn Tristan da Cunha Amsterdam St-Paul South Georgia Crozet Islands TAAF (Terres Australes et Antarctiques Françaises) Iles Sandwich Falklands Kerguelen (Islas Malvinas) BAT (British Antarctic Territory) Adélie Land ORs OCTs Anguilla The EU overseas dimension British Virgin Is. A major potential for cooperation on climate change and biodiversity Turks & Caïcos Caïman Islands Montserrat Sint-Marteen Sint-Eustatius Greenland Saba St Pierre & Miquelon Azores St-Martin Madeira St-Barth.