(TSFN): 0402917N-M AMENDED Research Report 2017 Gjoa Haven

Total Page:16

File Type:pdf, Size:1020Kb

(TSFN): 0402917N-M AMENDED Research Report 2017 Gjoa Haven Toward a Sustainable Fishery for Nunavummiut (TSFN): 0402917N-M AMENDED Research Report 2017 Gjoa Haven HTA and Queen’s University (Supervisor: Virginia K. Walker; M. Sc. Students: Erin Hamilton and Geraint Element; Queen’s University, Department of Biology, Kingston, ON, K7L 3N6) Assessment of Water Microbial Communities and Microplastics in the Canadian Arctic’s Lower Northwest Passage (Kitikmeot Region) Section 1: Collection of Surface Water for Fish Microbiome Study Background Information Both fish slime on the scales as well as the intestines is made up of cells associated with the fish immune system as well as the microbiota or beneficial microorganisms. The microorganisms including symbiotic bacteria contribute to the health of the fish and by extension, the health of fish stocks. It is thought that the microbiomes contribute to fish well-being either through competing with harmful bacteria and therefore excluding them, or through a more complex interaction with the host immune defense response. From an academic view, it is important to characterize the microbiomes of fish to infer the functions these microbes serve to increase understanding of fish immunity, but from a practical view, knowledge of the fish microbiomes and of the waters they live in, will provide insight into the impact of climate change on fish populations that are an important food source to communities in the Northwest Passage. Accompanied by community members from Gjoa Haven, a research team sampled fish and water from fresh and saltwater sites around King William Island, Nunavut (with separate fish sampling permits and animal care permits for this aspect of the work; see application material). Methods (a) Water Sampling: Fish caught by community members in commercial, subsistence and multimesh nets were quickly processed as has been described under other permit reports. Personnel designated for dissection (including trained community members) maintained aseptic technique by spraying down their gloves and all dissection equipment with 70% ethanol between samples (i.e mucosal skin scrape and intestinal samples). Slime samples were obtained by scraping the skin mucous from the left side above the lateral line of the fish (both Arctic char and whitefish, since these were of most interest to community members). Intestinal microbiomes were obtained by dissecting a portion of the intestine, just below the stomach. At each fish sampling site, field personnel filtered 3-4 L of water through nitrocellulose filters (0.22µm) in triplicate, and collected 50 mL of water from the photic zone, and then stored these samples in 50 mL falcon tubes at -20 °C for transport. Once returned to Queen’s University, the water sample filters were stored at -80 °C until microbial analysis by project collaborator Charles Greer (NRC). The small water samples (50 mL) were stored for future Chlorophyll a, bacterial abundance, Particulate Organic Carbon (POC), Dissolved Organic Carbon (DOC), Dissolved Nitrogen (DN, 2- 3- NO3 , NO2), Dissolved Phosphorus (DP, PO4 ), and salinity. (b) On-going Sequence Analysis of Microbiomes In addition to the analysis of water samples, next generation sequencing analysis for both intestinal and skin-associated microbiomes of Arctic char and whitefish are currently being processed. Up to 50 samples obtained from Arctic char and whitefish from a select number of sites within the Lower Northwest Passage, as identified by elders and fishers as of interest for subsistence or possible future commercial harvesting, will be compared. These sequences will then be compared to the water microbial analysis (see above) and allow 1 comparison between the internal and external microbial communities inherent to the fish as well as to their environment, and give insight to the overall health of the fish. Section 2: Collection of Microplastics for Contaminant Research Background Information Microplastics are part of human marine litter. The plastics are small, ranging in size between 5 mm – 0.3 mm and they are of concern since water organisms confuse them with food, eat them and then feel full. Microplastics have spread throughout the oceans of the world because of poor waste management and recycling practices. Some of these plastics float and are found in the top 0-20 m of the water column, called the photic zone. As indicated, they can influence the food chain because they are similar in size to nutritious phytoplankton, and in turn, zooplankton are likely to ingest microplastics, providing a pathway for other pollutants adsorbed to the plastics surface to bioaccumulate and biomagnify through the food-chain. This is similar to the manner that other toxins bioaccumulate in predators. It is important to assess the abundance of microplastics within the lower Northwest Passage to assist in determining the impacts of increased shipping traffic, exploration, and tourism in the Arctic. Since the human population of the Arctic is low, it is expected that microplastic pollution may also be low, but this depends on the additional effect of ocean currents. To assist in determining the origin of any microplastics found in the Canadian Arctic within this study, we are also assessing the microbial diversity of both the microplastics and the water column in which they are sampled. Biofilms can form and adhere to the surface of plastics, and it may be possible to determine whether the plastics have a different microbial population in comparison to the waters in which they are found. Methods Aboard the R/V Martin Bergmann (Arctic Research Foundation) samples were collected from Cambridge Bay, Western and Eastern Queen Maud Gulf, Simpson Strait, Gjoa Haven Bay, Rasmussen Basin, and Chantrey Inlet within the Kitikmeot region of Nunavut. Reduced water sampling consisted of a ~30 minute net tow, in which the cod-end of the net was retrieved and debris ranging between 0.3 mm-5.6 mm was collected and subsequently frozen at -20 °C. For microbial comparison, surface samples were collected using the ship's underway pump and 500-750 mL was then filtered through 45 mm 0.22 µm pore-sized Millipore GV filters, which were then frozen at -20 °C short-term, and at -80 °C long-term. In addition, triplicate bulk water samples were obtained from a 4L Niskin bottle consisting of 1 L each and taken at a depth of 10 m or 20 m, depending on bottom depth. In addition, water samples were collected similar to that described in Section 1, and the filters were transported to Queen's University for storage prior to processing by Dr. Charles Greer (NRC). All microplastic samples are to be analyzed at Queen’s University. Future Work In January 2018, microplastic samples will be counted and analyzed for microbial abundance. Any net tow and/or bulk microplastic will have their accompanying filtered water samples sent for sequencing to compare the microbial diversity present in each. Microplastics may act as vectors for pathogens in the marine environment, and this will be determined after sequencing. 2 Appendix Figures: Fig. 2. 1. A picture of the 5.6 mm sieve, also with the 0.3 mm sieve below with some debris caught on it. While processing cod-end samples from net tows, debris would sometimes get caught on the 5.6mm top sieve, and was discarded. Pictured above, a zooplankton animal was caught on the sieve. This zooplankton appears to have blue inclusions (see arrows) inside since the organism was rinsed thoroughly with filtered sea-water to remove anything sticking to it before this photo was taken, so it is possible that what is left has been ingested by the organism. 3 Table summaries for collection sites and each method used in 2017: Table summaries for water collection sites in 2017: Table 1.1: Summary of water collection sites for microbial analysis under TSFN fishing project (2017). Location Name (Site) GPS Coordinates Port Perry (TSFN 1) 69°33’ 28.76”N, 97°26’ 13.89”W Murchison River 1 (TSFN 8) 68° 34’ 1.20”N, 93° 22’ 37.40”W Murchison River 2 (TSFN 14) 68°25’ 35.50”N, 93°19’ 11.60”W Lady Franklin Lake (TSFN 15) 67°19’ 5.34”N, 96°46’ 11.04”W Back River 1 (TSFN 13) 66°57’ 30.70”N, 95°18’5.20”W Back River 2 (TSFN 18) 67° 9’ 17.35”N, 95° 21’ 21.41”W Table 2.1: Microplastic sampling information from the Side Net Tow procedure (2017). Location Name GPS Tow In GPS Tow Out Flowmeter Flowmeter Flowmeter Total In Out Difference time in water (min) Cambridge Bay 69°6’49.5”N, 69°6’49.5”N, 168240 187806 19566 18:05 (B1) 105°3’33.7”W 105°3’33.7”W Queen Maud 68°12’46.5”N, 68°13’38.45”N, 187830 229684 41854 30:18 West (Ellice River 103°57’51.1”W 103°57’51.135”W 1) Queen Maud East 68°10’44.5”N, 68°10’49.7”N, 229688 272100 42412 29:30 (QME) 100°17’14.5”W 100°14’57.1”W Simpson Strait 68°32’26.5”N, 68°32’22.9”N, 298072 363705 65633 31:48 (SS3) 97°27’43.7”W 97°25’52.7”W Gjoa Haven Bay 68°36’22.3”N, 68°37’41.2”N, 363734 416475 52741 28:52 95°53’29.7”W 95°52’49.1”W Chantrey Inlet 67°44’48.7”N, 67°45’13.2”N, 416515 468158 51643 32:31 (CI3) 95°48’1.3”W 95°47’1.3”W Rasmussen Basin 68°21’43.8”N, 68°22’44.4”N, 467173 513830 46657 31:25 (CI1) 95°13’23.6”W 95°14’2.1”W Table 2.2: Microbial surface sample locations to compliment the net tow microplastic data.
Recommended publications
  • Transits of the Northwest Passage to End of the 2019 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
    TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2019 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 12 December 2019 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 but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 314 complete maritime transits of the Northwest Passage have been made to the end of the 2019 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 (transits 149 and 167).
    [Show full text]
  • Ice Shelf Advance and Retreat Rates Along the Coast of Queen Maud Land, Antarctica K
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 106, NO. C4, PAGES 7097–7106, APRIL 15, 2001 Ice shelf advance and retreat rates along the coast of Queen Maud Land, Antarctica K. T. Kim,1 K. C. Jezek,2 and H. G. Sohn3 Byrd Polar Research Center, The Ohio State University, Columbus, Ohio Abstract. We mapped ice shelf margins along the Queen Maud Land coast, Antarctica, in a study of ice shelf margin variability over time. Our objective was to determine the behavior of ice shelves at similar latitudes but different longitudes relative to ice shelves that are dramatically retreating along the Antarctic Peninsula, possibly in response to changing global climate. We measured coastline positions from 1963 satellite reconnaissance photography and 1997 RADARSAT synthetic aperture radar image data for comparison with coastlines inferred by other researchers who used Landsat data from the mid-1970s. We show that these ice shelves lost ϳ6.8% of their total area between 1963 and 1997. Most of the areal reduction occurred between 1963 and the mid-1970s. Since then, ice margin positions have stabilized or even readvanced. We conclude that these ice shelves are in a near-equilibrium state with the coastal environment. 1. Introduction summer 0Њ isotherm [Tolstikov, 1966, p. 76; King and Turner, 1997, p. 141]. Following Mercer’s hypothesis, we might expect Ice shelves are vast slabs of glacier ice floating on the coastal these ice shelves to be relatively stable at the present time. ocean surrounding Antarctica. They are a continuation of the Following the approach of other investigators [Rott et al., ice sheet and form, in part, as glacier ice flowing from the 1996; Ferrigno et al., 1998; Skvarca et al., 1999], we compare the interior ice sheet spreads across the ocean surface and away position of ice shelf margins and grounding lines derived from from the coast.
    [Show full text]
  • Arctic Marine Transport Workshop 28-30 September 2004
    Arctic Marine Transport Workshop 28-30 September 2004 Institute of the North • U.S. Arctic Research Commission • International Arctic Science Committee Arctic Ocean Marine Routes This map is a general portrayal of the major Arctic marine routes shown from the perspective of Bering Strait looking northward. The official Northern Sea Route encompasses all routes across the Russian Arctic coastal seas from Kara Gate (at the southern tip of Novaya Zemlya) to Bering Strait. The Northwest Passage is the name given to the marine routes between the Atlantic and Pacific oceans along the northern coast of North America that span the straits and sounds of the Canadian Arctic Archipelago. Three historic polar voyages in the Central Arctic Ocean are indicated: the first surface shop voyage to the North Pole by the Soviet nuclear icebreaker Arktika in August 1977; the tourist voyage of the Soviet nuclear icebreaker Sovetsky Soyuz across the Arctic Ocean in August 1991; and, the historic scientific (Arctic) transect by the polar icebreakers Polar Sea (U.S.) and Louis S. St-Laurent (Canada) during July and August 1994. Shown is the ice edge for 16 September 2004 (near the minimum extent of Arctic sea ice for 2004) as determined by satellite passive microwave sensors. Noted are ice-free coastal seas along the entire Russian Arctic and a large, ice-free area that extends 300 nautical miles north of the Alaskan coast. The ice edge is also shown to have retreated to a position north of Svalbard. The front cover shows the summer minimum extent of Arctic sea ice on 16 September 2002.
    [Show full text]
  • Supplementary File For: Blix A.S. 2016. on Roald Amundsen's Scientific Achievements. Polar Research 35. Correspondence: AAB Bu
    Supplementary file for: Blix A.S. 2016. On Roald Amundsen’s scientific achievements. Polar Research 35. Correspondence: AAB Building, Institute of Arctic and Marine Biology, University of Tromsø, NO-9037 Tromsø, Norway. E-mail: [email protected] Selected publications from the Gjøa expedition not cited in the text Geelmuyden H. 1932. Astronomy. The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 6(2), 23-27. Graarud A. 1932. Meteorology. The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 6(3), 31-131. Graarud A. & Russeltvedt N. 1926. Die Erdmagnetischen Beobachtungen der Gjöa-Expedition 1903- 1906. (Geomagnetic observations of the Gjøa expedition, 1903-06.) The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 3(8), 3-14. Holtedahl O. 1912. On some Ordovician fossils from Boothia Felix and King William Land, collected during the Norwegian expedition of the Gjøa, Captain Amundsen, through the North- west Passage. Videnskapsselskapets Skrifter 1, Matematisk–Naturvidenskabelig Klasse 9. Kristiania (Oslo): Jacob Dybwad. Lind J. 1910. Fungi (Micromycetes) collected in Arctic North America (King William Land, King Point and Herschell Isl.) by the Gjöa expedition under Captain Roald Amundsen 1904-1906. Videnskabs-Selskabets Skrifter 1. Mathematisk–Naturvidenskabelig Klasse 9. Christiania (Oslo): Jacob Dybwad. Lynge B. 1921. Lichens from the Gjøa expedition. Videnskabs-Selskabets Skrifter 1. Mathematisk– Naturvidenskabelig Klasse 15. Christiania (Oslo): Jacob Dybwad. Ostenfeld C.H. 1910. Vascular plants collected in Arctic North America (King William Land, King Point and Herschell Isl.) by the Gjöa expedition under Captain Roald Amundsen 1904-1906.
    [Show full text]
  • 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’).
    [Show full text]
  • Who Discovered the Northwest Passage? Janice Cavell1
    ARCTIC VOL. 71, NO.3 (SEPTEMBER 2018) P.292 – 308 https://doi.org/10.14430/arctic4733 Who Discovered the Northwest Passage? Janice Cavell1 (Received 31 January 2018; accepted in revised form 1 May 2018) ABSTRACT. In 1855 a parliamentary committee concluded that Robert McClure deserved to be rewarded as the discoverer of a Northwest Passage. Since then, various writers have put forward rival claims on behalf of Sir John Franklin, John Rae, and Roald Amundsen. This article examines the process of 19th-century European exploration in the Arctic Archipelago, the definition of discovering a passage that prevailed at the time, and the arguments for and against the various contenders. It concludes that while no one explorer was “the” discoverer, McClure’s achievement deserves reconsideration. Key words: Northwest Passage; John Franklin; Robert McClure; John Rae; Roald Amundsen RÉSUMÉ. En 1855, un comité parlementaire a conclu que Robert McClure méritait de recevoir le titre de découvreur d’un passage du Nord-Ouest. Depuis lors, diverses personnes ont avancé des prétentions rivales à l’endroit de Sir John Franklin, de John Rae et de Roald Amundsen. Cet article se penche sur l’exploration européenne de l’archipel Arctique au XIXe siècle, sur la définition de la découverte d’un passage en vigueur à l’époque, de même que sur les arguments pour et contre les divers prétendants au titre. Nous concluons en affirmant que même si aucun des explorateurs n’a été « le » découvreur, les réalisations de Robert McClure méritent d’être considérées de nouveau. Mots clés : passage du Nord-Ouest; John Franklin; Robert McClure; John Rae; Roald Amundsen Traduit pour la revue Arctic par Nicole Giguère.
    [Show full text]
  • Searching for HMS Terror
    ARTICLE KNOWLEDGE GAINED IN THE SEARCH FOR FRANKLIN Searching for HMS Terror “We know where the target is not located” is the only guaranteed result of any search expedition. This statement does not make for exciting headlines, however, the value of knowledge gained during the search itself and its many benefits to a variety of end-users, cannot be easily dismissed. The 2015 Franklin Expedition search coordinated by Parks Canada was the continuing multi-year, multi-partner effort that saw the discovery of HMS Erebus in September of 2014. In this article we will discuss the knowledge gained and multiple uses of the data collected toward our conclusion of verifying where HMS Terror is not located. In 1845, Captain Sir John Franklin led an ill-fated expedition to find the final elusive link in the Northwest Passage through what is now the Canadian Arctic Archipelago. Supplied for three years, HMS Erebus (Figure 1) and HMS Terror sailed from England outfitted with innovative auxiliary steam engines, coal-fired heating systems, and all manner of internal and external hull reinforcement to better withstand the ice -- including bows sheathed in iron hull plating. Given the experience of Franklin, his hand-picked crew, and the well- equipped ships he commanded, few anticipated the tragedy and ensuing searches that continue to this day. Many motivating factors have contributed to the launch of the searches for the ‘Lost Expedition’. Initially it was a rescue mission, and then a recovery mission, when all hope for any survivors was lost. Modern day searches coordinated and funded by the Government of Canada are motivated not only by the important history the lost expedition represents, but the added substantiation to Canada’s sovereignty claim to the Arctic.
    [Show full text]
  • Sail from Dover DAY 9 | Romsdalsmuseet, One of Finnsnes / Senja Norway’S Largest Folk Museums
    Return address Hurtigruten Ltd, Unit 1a, Commonwealth Buildings, Woolwich Church Street, SE18 5NS <T><F><S> <COMPANY> <ADDR1> <ADDR2> <ADDR3> <ADDR4> <ADDR5> <ADDR6> <ADDR7> Cust. ref.:<ACCOUNT_ID> <TOWN> <COUNTY> <Job ref>/<Cell>/<Seq. No> <ZIP> <SSC>/<Bag ID>/<Bag no.>/<MS brake> Notifi cation: We use your information in accordance with our Privacy Policy, updated June 2019. Please see www.hurtigruten.co.uk/practical-information/statement-of-privacy/ New expedition cruises 2021 | 2022 SAIL from save up to 20%* DOVER British Isles | Norway’s Northern Lights | Norway’s Arctic sunshine & Fjords | southern Scandinavia MS MAUD welcome For 127 years, Hurtigruten have been With our unique Science Center pioneers in expedition cruising, from as the beating heart of the ship, the rugged coastline of Norway and our expedition team serve as hosts, the Arctic islands, to the remote lecturers, instructors, companions continent of Antarctica. Our mission and guides as they bring to life is to deliver authentic adventures for breath-taking destinations. the naturally curious. Your health and safety is our I am thrilled to present our series top priority, and we constantly of NEW expedition cruises update our protocols and safety from Dover for 2021/22. Start guidelines, in consultation with your holiday without the stress of the Norwegian Government and a crowded airport, as we embark with local health authorities. from the beautiful cruise terminal Please book with confidence, in Dover, to discover hand-picked and for the latest information, gems on expertly-planned itineraries visit our website. visiting the British Isles, southern We can’t wait to welcome you Scandinavia and the stunning onboard MS Maud.
    [Show full text]
  • Gjoa Haven © Nunavut Tourism
    NUNAVUT COASTAL RESOURCE INVENTORY ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut Ministère de l’Environnement Gjoa Haven © Nunavut Tourism ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut NUNAVUT COASTAL RESOURCE INVENTORY • Gjoa Haven INVENTORY RESOURCE COASTAL NUNAVUT Ministère de l’Environnement Nunavut Coastal Resource Inventory – Gjoa Haven 2011 Department of Environment Fisheries and Sealing Division Box 1000 Station 1310 Iqaluit, Nunavut, X0A 0H0 GJOA HAVEN Inventory deliverables include: EXECUTIVE SUMMARY • A final report summarizing all of the activities This report is derived from the Hamlet of Gjoa Haven undertaken as part of this project; and represents one component of the Nunavut Coastal Resource Inventory (NCRI). “Coastal inventory”, as used • Provision of the coastal resource inventory in a GIS here, refers to the collection of information on coastal database; resources and activities gained from community interviews, research, reports, maps, and other resources. This data is • Large-format resource inventory maps for the Hamlet presented in a series of maps. of Gjoa Haven, Nunavut; and Coastal resource inventories have been conducted in • Key recommendations on both the use of this study as many jurisdictions throughout Canada, notably along the well as future initiatives. Atlantic and Pacific coasts. These inventories have been used as a means of gathering reliable information on During the course of this project, Gjoa Haven was visited on coastal resources to facilitate their strategic assessment, two occasions:
    [Show full text]
  • Canada's Arctic Marine Atlas
    Lincoln Sea Hall Basin MARINE ATLAS ARCTIC CANADA’S GREENLAND Ellesmere Island Kane Basin Nares Strait N nd ansen Sou s d Axel n Sve Heiberg rdr a up Island l Ch ann North CANADA’S s el I Pea Water ry Ch a h nnel Massey t Sou Baffin e Amund nd ISR Boundary b Ringnes Bay Ellef Norwegian Coburg Island Grise Fiord a Ringnes Bay Island ARCTIC MARINE z Island EEZ Boundary Prince i Borden ARCTIC l Island Gustaf E Adolf Sea Maclea Jones n Str OCEAN n ait Sound ATLANTIC e Mackenzie Pe Ball nn antyn King Island y S e trait e S u trait it Devon Wel ATLAS Stra OCEAN Q Prince l Island Clyde River Queens in Bylot Patrick Hazen Byam gt Channel o Island Martin n Island Ch tr. Channel an Pond Inlet S Bathurst nel Qikiqtarjuaq liam A Island Eclipse ust Lancaster Sound in Cornwallis Sound Hecla Ch Fitzwil Island and an Griper nel ait Bay r Resolute t Melville Barrow Strait Arctic Bay S et P l Island r i Kel l n e c n e n Somerset Pangnirtung EEZ Boundary a R M'Clure Strait h Island e C g Baffin Island Brodeur y e r r n Peninsula t a P I Cumberland n Peel Sound l e Sound Viscount Stefansson t Melville Island Sound Prince Labrador of Wales Igloolik Prince Sea it Island Charles ra Hadley Bay Banks St s Island le a Island W Hall Beach f Beaufort o M'Clintock Gulf of Iqaluit e c n Frobisher Bay i Channel Resolution r Boothia Boothia Sea P Island Sachs Franklin Peninsula Committee Foxe Harbour Strait Bay Melville Peninsula Basin Kimmirut Taloyoak N UNAT Minto Inlet Victoria SIA VUT Makkovik Ulukhaktok Kugaaruk Foxe Island Hopedale Liverpool Amundsen Victoria King
    [Show full text]
  • Roald Amundsen and Robert Scott: Amundsen’S Earlier Voyages and Experience
    Roald Amundsen and Robert Scott: Amundsen’s earlier voyages and experience. • Roald Amundsen joined the Belgian Antarctic Expedition (1897–99) as first mate. • This expedition, led by Adrien de Gerlache using the ship the RV Belgica, became the first expedition to winter in Antarctica. Voyage in research vessel Belgica. • The Belgica, whether by mistake or design, became locked in the sea ice at 70°30′S off Alexander Island, west of the Antarctic Peninsula. • The crew endured a winter for which they were poorly prepared. • RV Belgica frozen in the ice, 1898. Gaining valuable experience. • By Amundsen's own estimation, the doctor for the expedition, the American Frederick Cook, probably saved the crew from scurvy by hunting for animals and feeding the crew fresh meat • In cases where citrus fruits are lacking, fresh meat from animals that make their own vitamin C (which most do) contains enough of the vitamin to prevent scurvy, and even partly treat it. • This was an important lesson for Amundsen's future expeditions. Frederick Cook с. 1906. Another successful voyage. • In 1903, Amundsen led the first expedition to successfully traverse Canada's Northwest Passage between the Atlantic and Pacific oceans. • He planned a small expedition of six men in a 45-ton fishing vessel, Gjøa, in order to have flexibility. Gjøa today. Sailing westward. • His ship had relatively shallow draft. This was important since the depth of the sea was about a metre in some places. • His technique was to use a small ship and hug the coast. Amundsen had the ship outfitted with a small gasoline engine.
    [Show full text]
  • Canada Topographical
    University of Waikato Library: Map Collection Canada: topographical maps 1: 250,000 The Map Collection of the University of Waikato Library contains a comprehensive collection of maps from around the world with detailed coverage of New Zealand and the Pacific : Editions are first unless stated. These maps are held in storage on Level 1 Please ask a librarian if you would like to use one: Coverage of Canadian Provinces Province Covered by sectors On pages Alberta 72-74 and 82-84 pp. 14, 16 British Columbia 82-83, 92-94, 102-104 and 114 pp. 16-20 Manitoba 52-54 and 62-64 pp. 10, 12 New Brunswick 21 and 22 p. 3 Newfoundland and Labrador 01-02, 11, 13-14 and 23-25) pp. 1-4 Northwest Territories 65-66, 75-79, 85-89, 95-99 and 105-107) pp. 12-21 Nova Scotia 11 and 20-210) pp. 2-3 Nunavut 15-16, 25-27, 29, 35-39, 45-49, 55-59, 65-69, 76-79, pp. 3-7, 9-13, 86-87, 120, 340 and 560 15, 21 Ontario 30-32, 40-44 and 52-54 pp. 5, 6, 8-10 Prince Edward Island 11 and 21 p. 2 Quebec 11-14, 21-25 and 31-35 pp. 2-7 Saskatchewan 62-63 and 72-74 pp. 12, 14 Yukon 95,105-106 and 115-117 pp. 18, 20-21 The sector numbers begin in the southeast of Canada: They proceed west and north. 001 Newfoundland 001K Trepassey 3rd ed. 1989 001L St: Lawrence 4th ed. 1989 001M Belleoram 3rd ed.
    [Show full text]