Phenotypic Variation Among Thick-Billed Murres from Colonies
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Department of Environment– Wildlife Division
Department of Environment– Wildlife Division Wildlife Research Section Department of Environment Box 209 Igloolik, NU X0A 0L0 Tel: (867) 934-2179 Fax: (867) 934-2190 Email: [email protected] Frequently Asked Questions Government of Nunavut 1. What is the role of the GN in issuing wildlife research permits? On June 1, 1999, Nunavut became Canada’s newest territory. Since its creation, interest in studying its natural resources has steadily risen. Human demands on animals and plants can leave them vulnerable, and wildlife research permits allow the Department to keep records of what, and how much research is going on in Nunavut, and to use this as a tool to assist in the conservation of its resources. The four primary purposes of research in Nunavut are: a. To help ensure that communities are informed of scientific research in and around their communities; b. To maintain a centralized knowledgebase of research activities in Nunavut; c. To ensure that there are no conflicting or competing research activities in Nunavut; and d. To ensure that wildlife research activities abide by various laws and regulations governing the treatment and management of wildlife and wildlife habitat in Nunavut. 2. How is this process supported by the Nunavut Land Claims Agreement? Conservation: Article 5.1.5 The principles of conservation are: a. the maintenance of the natural balance of ecological systems within the Nunavut Settlement Area; b. the protection of wildlife habitat; c. the maintenance of vital, healthy, wildlife populations capable of sustaining harvesting needs as defined in this article; and d. the restoration and revitalization of depleted populations of wildlife and wildlife habitat. -
15 Canadian High Arctic-North Greenland
15/18: LME FACTSHEET SERIES CANADIAN HIGH ARCTIC-NORTH GREENLAND LME tic LMEs Arc CANADIAN HIGH ARCTIC-NORTH GREENLAND LME MAP 18 of Central Map Arctic Ocean LME North Pole Ellesmere Island Iceland Greenland 15 "1 ARCTIC LMEs Large ! Marine Ecosystems (LMEs) are defined as regions of work of the ArcNc Council in developing and promoNng the ocean space of 200,000 km² or greater, that encompass Ecosystem Approach to management of the ArcNc marine coastal areas from river basins and estuaries to the outer environment. margins of a conNnental shelf or the seaward extent of a predominant coastal current. LMEs are defined by ecological Joint EA Expert group criteria, including bathymetry, hydrography, producNvity, and PAME established an Ecosystem Approach to Management tropically linked populaNons. PAME developed a map expert group in 2011 with the parNcipaNon of other ArcNc delineaNng 17 ArcNc Large Marine Ecosystems (ArcNc LME's) Council working groups (AMAP, CAFF and SDWG). This joint in the marine waters of the ArcNc and adjacent seas in 2006. Ecosystem Approach Expert Group (EA-EG) has developed a In a consultaNve process including agencies of ArcNc Council framework for EA implementaNon where the first step is member states and other ArcNc Council working groups, the idenNficaNon of the ecosystem to be managed. IdenNfying ArcNc LME map was revised in 2012 to include 18 ArcNc the ArcNc LMEs represents this first step. LMEs. This is the current map of ArcNc LMEs used in the This factsheet is one of 18 in a series of the ArcCc LMEs. OVERVIEW: CANADIAN HIGH ARCTIC-NORTH GREENLAND LME The Canadian High Arcc-North Greenland LME (CAA) consists of the northernmost and high arcc part of Canada along with the adjacent part of North Greenland. -
Abstracts Annual Scientific Meeting ᐊᕐᕌᒍᑕᒫᕐᓯᐅᑎᒥᒃ ᑲᑎᒪᓂᕐᒃ
Abstracts Annual Scientific Meeting ᐊᕐᕌᒍᑕᒫᕐᓯᐅᑎᒥᒃ ᑲᑎᒪᓂᕐᒃ 2016 Réunion scientifique annuelle 5-9/12/2016, Winnipeg, MB ASM2016 Conference Program Oral Presentation and Poster Abstracts ABSTRACTS FROBISHER BAY: A NATURAL LABORATORY complete habitat characterization. This recent sampling FOR THE STUDY OF ENVIRONMENTAL effort recorded heterogeneous substrates composed of CHANGE IN CANADIAN ARCTIC MARINE various proportions of boulder, cobbles, gravel, sand HABITATS. and mud forming a thin veneer over bedrock at water depths less than 200 metres. Grab samples confirm Aitken, Alec (1), B. Misiuk (2), E. Herder (2), E. the relative abundance of mollusks, ophiuroids and Edinger (2), R. Deering (2), T. Bell (2), D. Mate(3), C. tubiculous polychaetes as constituents of the infauna Campbell (4), L. Ham (5) and V.. Barrie (6) in the inner bay. Drop video images captured a diverse (1) University of Saskatchewan (Saskatoon, Canada); epifauna not previously described from the FRBC (2) Department of Geography, Memorial University of research. A variety of bryozoans, crinoid echinoderms, Newfoundland (St. John’s, NL, Canada); sponges and tunicates recorded in the images remain (3) Polar Knowledge Canada (Ottawa, Ontario, to be identified. Habitat characterization will allow us Canada); to quantify ecological change in benthic invertebrate (4) Marine Resources Geoscience, Geological Survey of species composition within the habitat types represented Canada (Dartmouth, NS, Canada); at selected sampling stations through time. Such long- (5) Canada-Nunavut Geoscience Office, Natural term studies are crucial for distinguishing directional Resources Canada (Iqaluit, NU, Canada); change in ecosystems. Marine Geological Hazards (6) Marine Geoscience, Geological Survey of Canada and Seabed Disturbance: Extensive multibeam (Sidney, BC, Canada) echosounding surveys have recorded more than 250 submarine slope failures in inner Frobisher Bay. -
Green Paper the Lancaster Sound Region
Green Paper The Lancaster Sound Region: 1980-2000 Issues and Options on the Use and Management of the Region Lancaster Sound Regional Study H.J. Dirschl Project Manager January 1982 =Published under the authority of the Hon. John C. Munro, P.C., M.P., Minister of Indian Affairs and Northern Development, Ottawa, 1981. 05-8297-020-EE-A1 Catalogue No. R72-164/ 1982E ISBN 0-662-11869 Cette publication peut aussi etre obtenue en francais. Preface In the quest for a "best plan" for Lancaster Sound criticisms. This feedback is discussed in detail in a and its abundant resources, this public discussion recently puolished report by the workshop chairman. paper seeks to stimulate a continued. wide-ranging, Professor Peter Jacobs, entitled People. Resources examination of the issues involved in the future use and the Environment: Perspectives on the Use and and management of this unique area of the Canadian Management of the Lancaster Sound Region. All the Arctic. input received during the public review phase has been taken into consideration in the preparation of the The green paper is the result of more than two years final green paper. of work by the Northern Affairs Program of the Department of Indian Affairs and Northern From the beginning of the study, it was expected that Development, in co-operation with the government of to arrive at an overall consensus of the optimum fu the Northwest Territories and the federal departments ture use and management of the Lancaster Sound of Energy, Mines and Resources, Environment. region would require intensive public discussion fol Fisheries and Oceans. -
Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait
Polarforschung 74 (1-3), 129 – 160, 2004 (erschienen 2006) In Search of the Wegener Fault: Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait by J. Christopher Harrison1 Abstract: A total of 28 geological-geophysical markers are identified that lich der Bache Peninsula und Linksseitenverschiebungen am Judge-Daly- relate to the question of strike slip motions along and bordering Nares Strait. Störungssystem (70 km) und schließlich die S-, später SW-gerichtete Eight of the twelve markers, located within the Phanerozoic orogen of Kompression des Sverdrup-Beckens (100 + 35 km). Die spätere Deformation Kennedy Channel – Robeson Channel region, permit between 65 and 75 km wird auf die Rotation (entgegen dem Uhrzeigersinn) und ausweichende West- of sinistral offset on the Judge Daly Fault System (JDFS). In contrast, eight of drift eines semi-rigiden nördlichen Ellesmere-Blocks während der Kollision nine markers located in Kane Basin, Smith Sound and northern Baffin Bay mit der Grönlandplatte zurückgeführt. indicate no lateral displacement at all. Especially convincing is evidence, presented by DAMASKE & OAKEY (2006), that at least one basic dyke of Neoproterozoic age extends across Smith Sound from Inglefield Land to inshore eastern Ellesmere Island without any recognizable strike slip offset. INTRODUCTION These results confirm that no major sinistral fault exists in southern Nares Strait. It is apparent to both earth scientists and the general public To account for the absence of a Wegener Fault in most parts of Nares Strait, that the shape of both coastlines and continental margins of the present paper would locate the late Paleocene-Eocene Greenland plate boundary on an interconnected system of faults that are 1) traced through western Greenland and eastern Arctic Canada provide for a Jones Sound in the south, 2) lie between the Eurekan Orogen and the Precam- satisfactory restoration of the opposing lands. -
Upper Ordovician Conodont Biostratigraphy and Revised Lithostratigraphy and Geological Map, Akpatok Island, Ungava Bay, Nunavut
Canadian Journal of Earth Sciences Upper Ordovician conodont biostratigraphy and revised lithostratigraphy and geological map, Akpatok Island, Ungava Bay, Nunavut Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0145.R1 Manuscript Type: Article Date Submitted by the Author: 08-Sep-2017 Complete List of Authors: Zhang, Shunxin; Canada-Nunavut Geoscience Office, Is the invited manuscript for Draft consideration in a Special N/A Issue? : Upper Ordovician, conodont biostratigraphy, geological map, Akpatok Keyword: Island, Ungava Bay https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 55 Canadian Journal of Earth Sciences 1 2 Upper Ordovician conodont biostratigraphy and revised lithostratigraphy 3 and geological map, Akpatok Island, Ungava Bay, Nunavut 4 5 6 7 Shunxin Zhang 8 9 10 11 Canada - Nunavut Geoscience Office, PO Box 2319, 1106 Inuksugait IV, 1 st floor, Iqaluit, 12 Nunavut X0A 0H0, Canada; [email protected] 13 Draft 14 15 16 17 Correspondence author: 18 Shunxin Zhang 19 PO Box 2319, 1106 Inuksugait IV, 1 st floor, Iqaluit, Nunavut X0A 0H0, Canada; 20 Phone: (867) 975-4579 21 Fax: (867) 979-0708 22 Email: [email protected] 23 24 25 ESS contribution number: 20160440 26 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 55 27 Upper Ordovician conodont biostratigraphy and revised lithostratigraphy 28 and geological map, Akpatok Island, Ungava Bay, Nunavut 29 Shunxin Zhang 30 31 Abstract 32 Stratigraphic units exposed on Akpatok Island, Ungava Bay, Nunavut, were previously 33 recognized as Boas River and Akpatok formations; their biostratigraphic ages and correlations, 34 in particular the stratigraphic position and age of the organic rich “Boas River” Formation, were 35 largely based on limited data. -
Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (marked ‘cp’). -
Atlantic Walrus Odobenus Rosmarus Rosmarus
COSEWIC Assessment and Update Status Report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada SPECIAL CONCERN 2006 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2006. COSEWIC assessment and update status report on the Atlantic walrus Odobenus rosmarus rosmarus in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. ix + 65 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous reports: COSEWIC 2000. COSEWIC assessment and status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 23 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Richard, P. 1987. COSEWIC status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-23 pp. Production note: COSEWIC would like to acknowledge D.B. Stewart for writing the status report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada, prepared under contract with Environment Canada, overseen and edited by Andrew Trites, Co-chair, COSEWIC Marine Mammals Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Évaluation et Rapport de situation du COSEPAC sur la situation du morse de l'Atlantique (Odobenus rosmarus rosmarus) au Canada – Mise à jour. -
Annual Report of the Eastern Artic Marine Investigations for 1949
C ONF IDENT IA L FISHERIES RESEARCH BOARD OF CANADA ANNUAL REPORT OF EASTERN ARCTIC FISHERIES INVESTIGATION FOR 1949 OTTAWA DECEMBER , 1949. Eastern Arctic Fisheries Inv'estigation, 1949, The Cruise of the "CALANUS", 1949. M. J.Dunbar I. Introduction and Summary. The terms of reference of these investetions are (1) to study the physical and biological oceanography of the eastern arctic and (2) to discover, if possible, marine resources which may be developed by and for the native population, Results obtained in Ungava bay during the 1949 season are listed in Dr. Dunbar's report, under these headings: (1) a. Sections were made from Burwell to Akpatok, from Akpatok to Payne bay, and from Akpatok to the mouth of the Koksoak river. Salinities, temperatures and oxygen concentrations were measured (the salinities not yet determined at time of writing). The sections were made in mid-July and one section, that from Payne bay to Akpatok, was repeated late in August in order to show the changes during the summer months* b, Echo-sounder tracks were recorded and kept from regions in Ungava bay where soundings are very incomplete, c. The study of the biology and distribution of the plankton, benthos and littoral fauna was continued, by the addition to the already large collections (from 1947 and 1948) of material from deeper water and from other areas than were possible to reach in the first two seasons. An effort was also made to collect micro-organisms by centrifuging methods. d. Experimental fishing for codfish, shark and flatfish, by hand line and by long lino trawl was continued. -
Hudson Strait-Ungava Bay Common Eider Surveys
Hudson Strait Common Eider and Polar Bear Surveys 2014 Field Season Report Project Overview Our ongoing research investigates the status of common eiders, red-throated loons and other ground nesting birds nesting on coastal islands in the Hudson Strait, Ungava Bay, and Foxe Basin marine regions of the eastern Canadian Arctic. There is considerable interest in the north relating to issues of human health and food security, as well as wildlife conservation and sustainable harvest. We are focusing on several emerging issues of significant ecological and conservation importance: 1. Quantifying the extent of polar bear predation on eider nests as sea ice diminishes. 2. Quantifying the spread and severity of avian cholera outbreaks among northern eider populations. 3. Quantifying the distribution and abundance of birds nesting on coastal islands in support of environmental sensitivity mapping and marine emergency response planning. Clockwise from top left: Adamie Mangiuk conducting surveys in Digges Sound, Nik Clyde measuring ponds on an eider colony, a Common Eider on her nest. 2014 Research Highlights Avian Cholera and Marine Birds Avian cholera is one of the most lethal diseases for birds in North America. Although it has circulated in southern Canada and the United States for many years, its emergence among eiders in the north is new. To better understand transmission dynamics and potential population level impacts for eiders we have undertaken sampling across the eastern Arctic. We are examining the geographic extent of the outbreaks, as well as the origins, virulence and evolution of the disease. Map of survey locations and the year in which they were completed. -
POLYNYAS in the CANADIAN ARCTIC Analysis of MODIS Sea Ice Temperature Data Between June 2002 and July 2013
Canatec Associates International Ltd. POLYNYAS IN THE CANADIAN ARCTIC Analysis of MODIS Sea Ice Temperature Data Between June 2002 and July 2013 David Currie 7/16/2014 Using daily sea ice temperature grids produced from MODIS optical satellite imagery, polynya occurrences in the Canadian Arctic and Northwest Greenland were mapped with a spatial resolution of one square kilometer and a temporal resolution of one week. The eleven year dataset was used to identify and measure locations with a high probability of open water occurrence. This approach appears to be most suitable for the spring months, when polynyas and shore leads represent the only open water in the region. An analysis of the results at several geographic scales reveals considerable yearly variation in polynya extents, although the relatively short period studied makes identifying trends rather difficult. Contents Introduction ................................................................................................................................................................ 3 Goals ............................................................................................................................................................................... 5 Source Data ................................................................................................................................................................. 6 MODIS Sea Ice Temperature Product MOD29/MYD29 ....................................................................... 6 Landsat Quicklook -
Uria Lomvia) and Black-Legged Kittiwakes (Rissa Tridactyla
A First Count of Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ) Breeding on Bylot Island ANTHONY J. G ASTON 1, 4 , MARC -A NDRÉ CYR 2, and KIERAN O’D ONOVAN 3 1Science and Technology Branch, Environment and Climate Change Canada, Carleton University, Ottawa, Ontario K1A 0H3 Canada 2Canadian Wildlife Service, Environment and Climate Change Canada, Place Vincent Massey, 351 St. Joseph Boulevard, Gatineau, Quebec K1A 0H3 Canada 3308a Klukshu Avenue, Whitehorse, Yukon Y1A 3Y1 Canada 4Corresponding author: [email protected] Gaston, Anthony J., Marc-André Cyr, and Kieran O’Donovan. 2017. A first count of Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ) breeding on Bylot Island. Canadian Field-Naturalist 131(1): 69 –74. https:// doi.org/10.22621/cfn.v 131i 1.1953 Bylot Island, part of Sirmilik National Park, supports two major breeding colonies of intermingled Thick-billed Murres ( Uria lomvia ) and Black-legged Kittiwakes ( Rissa tridactyla ): at Cape Hay near the northwest tip and at Cape Graham Moore at the opposite end of the island. Although the size of these colonies has been estimated previously, there is no information on how the estimates were made, except for Thick-billed Murres at Cape Hay in 1977, when the numbers were based on sampling only about 30% of the colony. In 2013, high-resolution digital photographs of the whole area of both colonies were taken in July, when most birds were probably incubating eggs. Individual birds were counted on the photographs, and the numbers were corrected for image quality and converted to numbers of breeding pairs based on correction factors from another High Arctic colony.