South Baffin Caribou Fall Composition And
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Long-Term Landscape Evolution of Hall Peninsula, Baffin Island, Nunavut: Insights from Low-Temperature (U-Th)/ He Thermochronology C
Atlantic Geology Volume 49 .. 2013 24 Long-term landscape evolution of Hall Peninsula, Baffin Island, Nunavut: insights from low-temperature (U-Th)/ He thermochronology C. Gabriel Creason and John C. Gosse Department of Earth Sciences, Dalhousie University, Halifax, Nova Scotia B3H 1N5, Canada <[email protected]> The northern coast of Hall Peninsula, Baffin Island, comprises a portion of the eastern Canadian Arctic Rim, an extensive physiographic feature with high relief spanning from southeastern Ellesmere Island to northern Labrador. Much of the high relief (> 1000 m) on Hall Peninsula has been attributed to incision during rift-flank uplift associated with Baffin Island separating from Greenland; however, the mechanisms for maintaining this high relief are poorly understood. In the nearby Torngat Mountains to the south, geophysical and thermochronologic data indicate the presence of a crustal root that induced rapid rift flank uplift. Conversely, thermochronologic data from Cumberland Peninsula to the north does not support the presence of a crustal root, suggesting other mechanisms responsible for the generation of its high relief. In the summer of 2012, 50 low-temperature thermochronology (e.g., apatite and zircon (U-Th)/He) samples were collected along three strategically positioned transects to determine the regional cooling history of the rocks on Hall Peninsula. Spatial distributions of the cooling ages of samples from two horizontal transects, one oriented parallel and one perpendicular to the Baffin rift-margin, will provide insight to the role (if any) of pre-existing drainage systems in the development of the high relief on eastern Hall Peninsula. Data from a vertical transect will be used to determine the rate of exhumation, if it varied with time, and the total amount of rock exhumed. -
Origin, Burial and Preservation of Late Pleistocene-Age Glacier Ice in Arctic
Origin, burial and preservation of late Pleistocene-age glacier ice in Arctic permafrost (Bylot Island, NU, Canada) Stephanie Coulombe1 2 3, Daniel Fortier 2 3 5, Denis Lacelle4, Mikhail Kanevskiy5, Yuri Shur5 6 1Polar Knowledge Canada, Cambridge Bay, X0B 0C0, Canada 5 2Department of Geography, Université de Montréal, Montréal, H2V 2B8, Canada 3Centre for Northern Studies, Université Laval, Quebec City, G1V 0A6, Canada 4Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, K1N 6N5, Canada 5Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5910, USA 6Department of Civil and Environmental Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5960, USA 10 Correspondence to: Stephanie Coulombe ([email protected]) Over the past decades, observations of buried glacier ice exposed in coastal bluffs and headwalls of retrogressive thaw slumps of the Arctic indicate that considerable amounts of late Pleistocene glacier ice survived the deglaciation and are still preserved in permafrost. In exposures, relict glacier ice and intrasedimental ice often coexist and look alike but their genesis is strikingly different. This paper aims to present a detailed description and infer the origin of a massive ice body preserved in the permafrost 15 of Bylot Island (Nunavut). The massive ice exposure and core samples were described according to the cryostratigraphic approach, combining the analysis of permafrost cryofacies and cryostructures, ice crystallography, stable O-H isotopes and cation contents. The ice was clear to whitish in appearance with large crystals (cm) and small gas inclusions (mm) at crystal intersections, similar to observations of englacial ice facies commonly found on contemporary glaciers and ice sheets. -
Across Borders, for the Future: Torngat Mountains Caribou Herd Inuit
ACROSS BORDERS, FOR THE FUTURE: Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study Prepared for the Nunatsiavut Government and Makivik Corporation, Parks Canada, and the Torngat Wildlife and Plants Co-Management Board - June 2014 This report may be cited as: Wilson KS, MW Basterfeld, C Furgal, T Sheldon, E Allen, the Communities of Nain and Kangiqsualujjuaq, and the Co-operative Management Board for the Torngat Mountains National Park. (2014). Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study. Final Report to the Nunatsiavut Government, Makivik Corporation, Parks Canada, and the Torngat Wildlife and Plants Co-Management Board. Nain, NL. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise (except brief passages for purposes of review) without the prior permission of the authors. Inuit Knowledge is intellectual property. All Inuit Knowledge is protected by international intellectual property rights of Indigenous peoples. As such, participants of the Torngat Mountains Caribou Herd Inuit Knowledge, Culture, and Values Study reserve the right to use and make public parts of their Inuit Knowledge as they deem appropriate. Use of Inuit Knowledge by any party other than hunters and Elders of Nunavik and Nunatsiavut does not infer comprehensive understanding of the knowledge, nor does it infer implicit support for activities or projects in which this knowledge is used in print, visual, electronic, or other media. Cover photo provided by and used with permission from Rodd Laing. All other photos provided by the lead author. -
Caribou (Barren-Ground Population) Rangifer Tarandus
COSEWIC Assessment and Status Report on the Caribou Rangifer tarandus Barren-ground population in Canada THREATENED 2016 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. 2016. COSEWIC assessment and status report on the Caribou Rangifer tarandus, Barren-ground population, in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. xiii + 123 pp. (http://www.registrelep-sararegistry.gc.ca/default.asp?lang=en&n=24F7211B-1). Production note: COSEWIC would like to acknowledge Anne Gunn, Kim Poole, and Don Russell for writing the status report on Caribou (Rangifer tarandus), Barren-ground population, in Canada, prepared under contract with Environment Canada. This report was overseen and edited by Justina Ray, Co-chair of the COSEWIC Terrestrial Mammals Specialist Subcommittee, with the support of the members of the Terrestrial Mammals Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment and Climate Change Canada Ottawa, ON K1A 0H3 Tel.: 819-938-4125 Fax: 819-938-3984 E-mail: [email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur le Caribou (Rangifer tarandus), population de la toundra, au Canada. Cover illustration/photo: Caribou — Photo by A. Gunn. Her Majesty the Queen in Right of Canada, 2016. Catalogue No. CW69-14/746-2017E-PDF ISBN 978-0-660-07782-6 COSEWIC Assessment Summary Assessment Summary – November 2016 Common name Caribou - Barren-ground population Scientific name Rangifer tarandus Status Threatened Reason for designation Members of this population give birth on the open arctic tundra, and most subpopulations (herds) winter in vast subarctic forests. -
Tab 6 Estimating the Abundance Of
SUBMISSION TO THE NUNAVUT WILDLIFE MANAGEMENT BOARD FOR Information: X Decision: Issue: South Baffin Island Caribou Abundance Survey, 2012 and Proposed Management Recommendations Background: Caribou are a critical component of the boreal and arctic ecosystems. They are culturally significant to local communities and provide an important source of food. In some areas, there is still uncertainty on population trends because of the lack of scientific information due to difficult logistics and remoteness. This is particularly true for Baffin Island, where three sub-populations of Barrenground caribou (Rangifer tarandus groenlandicus) are hypothesized, though little is known about their abundance and trends over time (Ferguson and Gauthier 1992). In the past 60 years, only discrete portions of their range have been surveyed and no robust quantitative estimates at the sub-population level were ever derived. For over a decade Inuit from communities on northern Baffin Island, and more recently from across the entire island, have reported declines in caribou numbers, although no quantitative estimates are available. In total 10 communities, representing half of all Nunavummiut, traditionally or currently harvest Baffin Island caribou. At the same time, climate change, including increased arctic temperatures and precipitation, and anthropogenic activities connected to mineral exploration and mining are potentially negatively impacting caribou and their range. Due to the risk of these cumulative negative effects, and the importance of these caribou to communities, the Department of Environment undertook, in 2012, a quantitative caribou abundance aerial survey of South Baffin Island with the support of the NWMB and co- management partners. This area represents the most abundant area of caribou on Baffin Island. -
Paper 64-35 a Provisional Physiographic Map of Canada
PAPER 64-35 A PROVISIONAL PHYSIOGRAPHIC MAP OF CANADA (Report and Map 13-1964) H. S. Bostock Price, 75 cents 1964 GEOLOGICAL SURVEY OF CANADA PAPER 64-35 A PROVISIONAL PHYSIOGRAPHIC MAP OF CANADA H. S. Bostock DEPARTMENT OF MINES AND TECHNICAL SURVEYS - iii - CONTENTS Page Introduction.... • • . • • . • . • • . • • . • • • . • • . • • • . l Physiographic subdivisions of Canada. • • • . • • . • . • l Shield Region . • • • . • • . • • • . • • • • . • . • • • . • . 5 Bear Province . • . • . • . • • • • . • • • • • • • • . 6 Slave Province • • • . • • • . • . • • . • • . • . • . 7 Churchill Provinces . • • . • • . • . 7 We stern Churchill Province ••.....• , • . • • • . 7 Northern Churchill Province . • . • . • • . • . • • • 9 Eastern Churchill Province . • • • • . • • • • . l 0 Superior Province . • • . • . • • . • . • • . • 12 Southern Province . • • . • • • . • • . • • • . • 14 Grenville Province . • . • • . • • . • • • . • • . 14 Border Region • . • • . • . • . • . • • • . • • • . 15 Innuitian Province • . • . • • . • • • . • . • • . 16 Arctic Lowland Province . • • . • . • • . • • • . 17 Arctic Coastal Plain Province . • . • . • • . • • 18 Cordilleran Province . • • . • • • . • • . • l 8 Interior Plains Province . • . • • • • . • • . 18 Hudson Bay Province • • . • • • . • • • . • 21 St. Lawrence Province . • . • . • . • • • . • . • . • • • • 21 Appalachian Province . • • . • • . • • . • . • . • • • 22 References................. • • • . • • . • • . • . • • • • • • • • . • 22 Map 13-1964 Provisional physiographic map of Canada .....••....••....••.......••..• -
The Arctic and Taiga Ecozone of Canada
THE CANADIAN ATLAS ONLINE NUNAVUT – GRADE 6 The Arctic and Taiga Ecozone of Canada Lesson Overview Students explore the various sub regions of the Arctic and Taiga ecozone, identifying specific physical and human characteristics of each. Grade Level Junior high (Grades 7-9); could be modified for high school as an introduction to a more in depth lesson in General Science, Biology, Environmental Science or Northern Studies. Time Required 90 min. (plus extra time if extension activities are attempted) Curriculum Connection • Nunavut – Inuuqatigiit/Piniaqtavut Integrated Program • Gr. 7 LAND: Canada’s Natural Resources and Canadian Geography Units • Gr. 8 COMMUNITY: Circumpolar Peoples Now Unit • Gr. 9 COMMUNITY: Young Northerners & Choice of Lifestyle • LAND: Responsibilities on the Land Link to Canadian National Geography Standards Essential Elements #1 (Grades 6-8) - The World in Spatial Terms • Distribution of major human and physical features at country and global scales • Expanding mental maps Essential Elements #2 (Grades 6-8) - Places and Regions • Physical and human characteristics of places and regions in Canada and the world Essential Elements #3 (Grades 6-8) - Physical Systems • Ecozones (major ecological communities such as boreal forest, polar regions, grasslands, wetlands and desert) Essential Elements #4 (Grades 6-8) - Human Systems (brief coverage) • Population density, distribution and growth rates Geographic Skill #2 (Grades 6-8) - Acquiring Geographic Information • Use maps to collect and/or compile geographic information Geographic Skill# 3 (Grades 6-8) - Organizing Geographic Information • Prepare various forms of graphs, tables and charts to organize and display geographic information • Integrate various types of materials to organize geographic information The Canadian Atlas The main resource for this lesson is the printed version of The Canadian Atlas: Our Nation, Environment and People (2004), more specifically the thematic pages entitled, The Far North: Arctic and Taiga, pg. -
Ecozones of Canada
Unit 3 Part 1 Pgs. 100- 109 • An introduction to Ecozones • - 15 terrestrial , or land regions. • - 5 marine ,or ocean regions. 1 Activity 1.Look at the map on p. 100 of your text. (a)What is the name of the ecozone you live in? (b)What image comes to mind when you think about that ecozone? 2 Ecozones 3 1. Ecozones • Marine • Terrestrial – Pacific – Arctic Cordillera – Arctic Archipelago – Northern Arctic – Arctic Basin – Southern Arctic – Northwest Atlantic – Taiga Plains – Atlantic – Taiga Shield – Taiga Cordillera – Hudson Plains – Boreal Plains – Boreal Shield – Boreal Cordillera – Pacific Maritime – Montane Cordillera – Prairies – Atlantic Maritime – Mixedwood Plains 4 2. Glossary Terms • Define the 2 terms below using the glossary. • Ecozones • Biodiversity 5 3.What is an Ecozone? • Ecozones are multifactor regions that are based upon a combination of natural and human characteristics. 6 4.The Characteristics of an Ecozone pg.102 • Landscape – Geology – Landforms – Climate – Soil – Water • Natural Vegetation • Wildlife • People 7 5. People Affect Ecozones p.104 • People can affect nature in significant ways. • Human activity often accelerates the pace of change in the environment, which causes stress on the environment. This can lead to serious and sometimes irreversible damage • Examples of damage: – Smoggy air, polluted water, disappearing forests and animals, collapse of fisheries. 8 6. Biodiversity pg.105 • Ecozones vary in shape and size which leads to them varying in biodiversity. • - Biodiversity means that there is a large variety of living things contained in each ecozone. 9 • Complete Handout #1 10 7.Where we live - Glossary Words (p.106) • Use the glossary to define the following terms: • Habitat • Ecology • Terrestrial Ecozone • Marine Ecozone • Boundary • Transition Zone 11 • Ecozones are vast in size, and so contain many smaller ecosystems. -
Glaciers of Canada
Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE ARCTIC ISLANDS GLACIERS OF BAFFIN ISLAND By JOHN T. ANDREWS With sections on BARNES ICE CAP: GEOMORPHOLOGY AND THERMODYNAMICS By GERALD HOLDSWORTH LATE 20TH CENTURY CHANGE AT THE BARNES ICE CAP MARGIN By JOHN D. JACOBS SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The glaciers on Baffin Island are primarily ice caps or ice fields and associated valley outlet glaciers and include numerous small glaciers as well. The two largest ice caps, the Barnes Ice Cap (5,935 km2) and the Penny Ice Cap (5,960 km2) are thought to be the last remnants of the Laurentide Ice Sheet. Approximately 8 percent of Baffin Island is covered by glaciers (36,839 km2). Nearby Bylot Island is heavily glacierized; it has 4,859 km2 of its area covered by glaciers, about 45 percent of the island. The Barnes Ice Cap has been slowly shrinking; the recession could accelerate if significant regional warming were to take place CONTENTS Page Abstract ---------------------------------------------------------------------------- J165 Introduction----------------------------------------------------------------------- 165 FIGURE 1. Sketch map of Baffin Island and adjacent regions ------------- 166 TABLE 1. Selected climatic data for climatic regions on Baffin Island and environs ------------------------------------------------- 167 Distribution of Glaciers -------------------------------------------------------- -
Wp-Uploads.Cngo.Ca
Rift flank uplift and landscape evolution of Hall Peninsula, Baffin Island, Nunavut: an exhumation model based on low-temperature thermochronology C.G. Creason, Department of Earth Science, Dalhousie University, Halifax, Nova Scotia, [email protected] J.C. Gosse, Department of Earth Science, Dalhousie University, Halifax, Nova Scotia M.D. Young, Department of Earth Science, Dalhousie University, Halifax, Nova Scotia Creason C.G., Gosse, J.C. and Young, M.D. 2013: Rift flank uplift and landscape evolution of Hall Peninsula, Baffin Island, Nunavut: an exhumation model based on low-temperature thermochronology; in Summary of Activities 2012, Canada-Nunavut Geoscience Office, p. 75–84. Abstract This study is part of the Canada-Nunavut Geoscience Office’s Hall Peninsula Integrated Geoscience Program, a multiyear bedrock and surficial geology mapping program with associated thematic studies. Baffin Island is characterized by fault- line bounded physiographic provinces that reflect lithological and structural elements inherited over the past two billion years. The northern coast of the Hall Peninsula half-horst is a rugged highland that constitutes a portion of the eastern Arctic Rim, a mountain range extending from northern Labrador to southern Ellesmere Island. Although Quaternary ice sheet and alpine glacial erosion has increased the relief of the mountain range, it appears from thermochronology and marine stratig- raphy that much of the relief was generated by incision through isostatically and thermally uplifted lithosphere accompany- ing rifting from Greenland. In the past decade, offshore geophysical surveys have provided a firmer understanding of post- rift processes and the nature of the continental-ocean crust boundary in Baffin Bay and Davis Strait. -
Terrestrial Ecozones of Canada
Terrestrial Ecozones of Canada Ecological land classification is a process of delineating and classifying ecologically distinctive areas and classification areas of the earth's surface. Each area can be viewed as a discrete system which has resulted from interplay of geologic, landform, soil, vegetation, climatic, water and human factors which may be present. Canada is divided into 15 separate terrestrial ecozones. Ecozones are areas of the earth's surface representative of large and very generalized ecological units characterized by interactive and adjusting abiotic and biotic factors. Canada's national parks and national park reserves are currently represented in 14 of the 15 terrestrial ecozones. 1. Arctic Cordillera 2. Northern Arctic 3. Southern Arctic 4. Atlantic Maritime 5. Boreal Cordillera 6. Boreal Plains 7. Boreal Shield 8. Hudson Plains 9. Prairie 10. Mixedwood Plains 11. Montane Cordillera 12. Pacific Maritime 13. Taiga Cordillera 14. Taiga Plains 15. Taiga Shield Reference: Lands Directorate, Terrestrial Ecozones Of Canada, Ecological Land Classification No. 19, 1986, p. 26. Arctic Cordillera Ecozone The Arctic Cordillera contains the only major mountainous environment other than the Rocky Mountain system. It occupies eastern Baffin and Devon islands and most of Ellesmere and Bylot islands. The highest parts are strikingly crowned by ice caps and multiple glaciers. The climate is very cold and arid. Mean daily January temperatures range from -25.5ºC in the south to -35ºC in the north and mean daily July temperatures are about 5ºC. Precipitation amounts to 200 mm to 300 mm generally with higher totals on exposed eastern slopes and at lower latitudes. Vegetation at upper elevations is largely absent due to the permanent ice and snow. -
Decoupling Between Plant Productivity and Growing Season Length Under a Warming Climate in Canada’S Arctic
American Journal of Climate Change, 2016, 5, 344-359 Published Online September 2016 in SciRes. http://www.scirp.org/journal/ajcc http://dx.doi.org/10.4236/ajcc.2016.53026 Decoupling between Plant Productivity and Growing Season Length under a Warming Climate in Canada’s Arctic Wenjun Chen1, Paul Zorn2, Lori White3, Ian Olthof1, Yu Zhang1, Robert Fraser1, Sylvain Leblanc1 1Canada Centre for Remote Sensing, Natural Resources Canada, Ottawa, Canada 2Parks Canada Agency, Gatineau, Canada 3Wildlife Landscape Science Directorate, Environment Canada, Ottawa, Canada Received 9 May 2016; accepted 13 August 2016; published 16 August 2016 Copyright © 2016 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract Given the short duration of growing season in the Arctic, a strong correlation between plant prod- uctivity and growing season length (GSL) is conventionally assumed. Will this assumption hold true under a warming climate? In this study, we addressed the question by investigating the rela- tionship between net primary productivity of leaves (NPPleaf) and GSL for various tundra ecosys- tems. We quantified NPPleaf and GSL using long-term satellite data and field measurements. Our results indicated that the relationship was not significant (i.e., decoupled) for 44% to 64% of tun- dra classes in the southern Canadian Arctic, but significant for all classes in the northern Canadian Arctic. To better understand the causes of the decoupling, we further decomposed the relationship into two components: the correspondence of interannual variations and the agreement of long- term trends.