The State of Lake Superior in 2000
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Atlas of the Copepods (Class Crustacea: Subclass Copepoda: Orders Calanoida, Cyclopoida, and Harpacticoida)
Taxonomic Atlas of the Copepods (Class Crustacea: Subclass Copepoda: Orders Calanoida, Cyclopoida, and Harpacticoida) Recorded at the Old Woman Creek National Estuarine Research Reserve and State Nature Preserve, Ohio by Jakob A. Boehler and Kenneth A. Krieger National Center for Water Quality Research Heidelberg University Tiffin, Ohio, USA 44883 August 2012 Atlas of the Copepods, (Class Crustacea: Subclass Copepoda) Recorded at the Old Woman Creek National Estuarine Research Reserve and State Nature Preserve, Ohio Acknowledgments The authors are grateful for the funding for this project provided by Dr. David Klarer, Old Woman Creek National Estuarine Research Reserve. We appreciate the critical reviews of a draft of this atlas provided by David Klarer and Dr. Janet Reid. This work was funded under contract to Heidelberg University by the Ohio Department of Natural Resources. This publication was supported in part by Grant Number H50/CCH524266 from the Centers for Disease Control and Prevention. Its contents are solely the responsibility of the authors and do not necessarily represent the official views of Centers for Disease Control and Prevention. The Old Woman Creek National Estuarine Research Reserve in Ohio is part of the National Estuarine Research Reserve System (NERRS), established by Section 315 of the Coastal Zone Management Act, as amended. Additional information about the system can be obtained from the Estuarine Reserves Division, Office of Ocean and Coastal Resource Management, National Oceanic and Atmospheric Administration, U.S. Department of Commerce, 1305 East West Highway – N/ORM5, Silver Spring, MD 20910. Financial support for this publication was provided by a grant under the Federal Coastal Zone Management Act, administered by the Office of Ocean and Coastal Resource Management, National Oceanic and Atmospheric Administration, Silver Spring, MD. -
Restoration of Woodland Caribou to the Lake Superior Region
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. National Park Service Publications and Papers National Park Service 1994 Restoration of Woodland Caribou to the Lake Superior Region Peter J. P. Gogan Yellowstone National Park Jean Fitts Cochrane USFWS, Anchorage, AL Follow this and additional works at: https://digitalcommons.unl.edu/natlpark Part of the Environmental Sciences Commons Gogan, Peter J. P. and Cochrane, Jean Fitts, "Restoration of Woodland Caribou to the Lake Superior Region" (1994). U.S. National Park Service Publications and Papers. 11. https://digitalcommons.unl.edu/natlpark/11 This Article is brought to you for free and open access by the National Park Service at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in U.S. National Park Service Publications and Papers by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 9 Restoration of woodland caribou to the Lake Superior region PETER J. P. GOGAN AND JEAN FITTS COCHRANE Introduction Woodland caribou (Rangifer tarandus caribou) historically occupied the boreal forest zone across the North American continent. The distribution and abun dance of the species has declined in the past century. In particular, it has been extirpated from much of the southern limits of its historical range on both sides of the boundary between Canada and the United States (Bergerud 1974). Translocation of animals from extant populations may be used to reestablish populations in portions of the species' former range. Recently, wildlife biolo gists in Ontario have translocated woodland caribou to a number of sites in or adjacent to Lake Superior. While it is too soon to evaluate their long-term suc cess, these restoration efforts do provide useful insights into factors likely to influence the outcome of woodland caribou translocations elsewhere. -
N Shore L. Superior: Geology, Scenery
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
Shipwreck Coast National Marine Sanctuary Proposal
Shipwreck Coast National Marine Sanctuary Nomination, Lake Superior, MI Shipwreck Coast National Marine Sanctuary Proposal Lake Superior, Michigan – 2017 1 12-1-2017 Shipwreck Coast National Marine Sanctuary Nomination, Lake Superior, MI Section I - Basics Nomination Title: Shipwreck Coast National Marine Sanctuary, Lake Superior, MI Nominator Name(s) and Affiliation(s): Darryl Ertel of the Whitefish Point Underwater Preserve (WPUP) one of the State of Michigan’s 13 designated underwater preserves, which operates under the authority of the Paradise Area Tourism Council a 501C3 not for profit organization, serves as the nominator on behalf of a truly grass roots group of supporting affiliate collaborators and supporters as presented under Consideration 7. Nomination Point of Contact - Name, Phone, Email, Address Darryl Ertel P.O. Box 318 Paradise, MI 49768 810-247-4583 [email protected] Section II - Introduction Narrative Description – a brief overview of the nomination This nomination area resides within the Michigan waters of Lake Superior described by noted Great Lakes shipwreck author, Frederick Stonehouse, in his book “Lake Superior’s Shipwreck Coast”. Stonehouse writes therein “If there is truly a graveyard of Lake Superior, it is the general area of Whitefish Point. More vessels have been lost there than any other part of the lake.” Stonehouse lists over 100 vessels lost between Grand Marais MI, west of Whitefish Point and Pt. Iroquois MI, southeast of Whitefish Point. Less than half of these shipwrecks have been found and documented to date. Several shipwrecks of historical significance have been found in amazingly well-preserved condition including the Comet, Cowle, Vienna, Osborn, and Mather as documented in GLSHS’ project report “The Art and Science of Mapping Lake Superior’s Shipwrecks: Ghosts of the Shipwreck Coast” 1. -
Seasonal Zooplankton Dynamics in Lake Michigan
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Publications, Agencies and Staff of the U.S. Department of Commerce U.S. Department of Commerce 2012 Seasonal zooplankton dynamics in Lake Michigan: Disentangling impacts of resource limitation, ecosystem engineering, and predation during a critical ecosystem transition Henry A. Vanderploeg National Oceanic and Atmospheric Administration, [email protected] Steven A. Pothoven Great Lakes Environmental Research Laboratory, [email protected] Gary L. Fahnenstiel Great Lakes Environmental Research Laboratory, [email protected] Joann F. Cavaletto National Oceanic and Atmospheric Administration, [email protected] James R. Liebig National Oceanic and Atmospheric Administration, [email protected] See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/usdeptcommercepub Part of the Environmental Sciences Commons Vanderploeg, Henry A.; Pothoven, Steven A.; Fahnenstiel, Gary L.; Cavaletto, Joann F.; Liebig, James R.; Stow, Craig A.; Nalepa, Thomas F.; Madenjian, Charles P.; and Bunnell, David B., "Seasonal zooplankton dynamics in Lake Michigan: Disentangling impacts of resource limitation, ecosystem engineering, and predation during a critical ecosystem transition" (2012). Publications, Agencies and Staff of the U.S. Department of Commerce. 406. https://digitalcommons.unl.edu/usdeptcommercepub/406 This Article is brought to you for free and open access by the U.S. Department of Commerce at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Publications, Agencies and Staff of the U.S. Department of Commerce by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors Henry A. Vanderploeg, Steven A. Pothoven, Gary L. Fahnenstiel, Joann F. -
Section 5.0 Existing Environment
SECTION 5.0 EXISTING ENVIRONMENT MARATHON PGM-CU PROJECT Environmental Impact Statement – Main Report 5.0 EXISTING ENVIRONMENT This section provides a summary of existing physical, biological and socio-environment baseline conditions as it relates to the proposed SCI Marathon PGM Copper Project. 5.1 Geology Detailed information regarding regional and deposit geology, host material geochemistry and seismicity are provided by EcoMetrix (2012b, 2012d, 2012e) and MICON (2010). The following sections provide a summary of this information. 5.1.1 Work Scope The geology within the study area is described in terms of the following components: geological components of the region and deposit; regional seismicity; mine material investigations; and, characterization of overburden, mine rock, and Type 1 (low-sulphur) and Type 2 (high- sulphur) process solids in terms of acid rock drainage and metal leaching potential. Predicted pit water quality post-mine closure and the filling of the pits is also described in this section. 5.1.2 Regional Geology The Marathon PGM-Cu deposit is hosted within the Eastern Gabbro Series of the Proterozoic Coldwell Complex, which intrudes and bisects the much older Archean Schreiber-Hemlo Greenstone Belt. The sub-circular complex has a diameter of 25 km and a surface area of 580 km2 and is the largest alkaline intrusive complex in North America (Walker et al., 1993a). The Coldwell Complex was emplaced as three nested intrusive centres (Centres I, II and III) (Mitchell and Platt, 1982) that were active during cauldron subsidence near where the northern end of the Thiel Fault intersected Archean rocks, on the north shore of Lake Superior (Figure 5.1-1). -
Molecular Species Delimitation and Biogeography of Canadian Marine Planktonic Crustaceans
Molecular Species Delimitation and Biogeography of Canadian Marine Planktonic Crustaceans by Robert George Young A Thesis presented to The University of Guelph In partial fulfilment of requirements for the degree of Doctor of Philosophy in Integrative Biology Guelph, Ontario, Canada © Robert George Young, March, 2016 ABSTRACT MOLECULAR SPECIES DELIMITATION AND BIOGEOGRAPHY OF CANADIAN MARINE PLANKTONIC CRUSTACEANS Robert George Young Advisors: University of Guelph, 2016 Dr. Sarah Adamowicz Dr. Cathryn Abbott Zooplankton are a major component of the marine environment in both diversity and biomass and are a crucial source of nutrients for organisms at higher trophic levels. Unfortunately, marine zooplankton biodiversity is not well known because of difficult morphological identifications and lack of taxonomic experts for many groups. In addition, the large taxonomic diversity present in plankton and low sampling coverage pose challenges in obtaining a better understanding of true zooplankton diversity. Molecular identification tools, like DNA barcoding, have been successfully used to identify marine planktonic specimens to a species. However, the behaviour of methods for specimen identification and species delimitation remain untested for taxonomically diverse and widely-distributed marine zooplanktonic groups. Using Canadian marine planktonic crustacean collections, I generated a multi-gene data set including COI-5P and 18S-V4 molecular markers of morphologically-identified Copepoda and Thecostraca (Multicrustacea: Hexanauplia) species. I used this data set to assess generalities in the genetic divergence patterns and to determine if a barcode gap exists separating interspecific and intraspecific molecular divergences, which can reliably delimit specimens into species. I then used this information to evaluate the North Pacific, Arctic, and North Atlantic biogeography of marine Calanoida (Hexanauplia: Copepoda) plankton. -
Lighthouses – Clippings
GREAT LAKES MARINE COLLECTION MILWAUKEE PUBLIC LIBRARY/WISCONSIN MARINE HISTORICAL SOCIETY MARINE SUBJECT FILES LIGHTHOUSE CLIPPINGS Current as of November 7, 2018 LIGHTHOUSE NAME – STATE - LAKE – FILE LOCATION Algoma Pierhead Light – Wisconsin – Lake Michigan - Algoma Alpena Light – Michigan – Lake Huron - Alpena Apostle Islands Lights – Wisconsin – Lake Superior - Apostle Islands Ashland Harbor Breakwater Light – Wisconsin – Lake Superior - Ashland Ashtabula Harbor Light – Ohio – Lake Erie - Ashtabula Badgeley Island – Ontario – Georgian Bay, Lake Huron – Badgeley Island Bailey’s Harbor Light – Wisconsin – Lake Michigan – Bailey’s Harbor, Door County Bailey’s Harbor Range Lights – Wisconsin – Lake Michigan – Bailey’s Harbor, Door County Bala Light – Ontario – Lake Muskoka – Muskoka Lakes Bar Point Shoal Light – Michigan – Lake Erie – Detroit River Baraga (Escanaba) (Sand Point) Light – Michigan – Lake Michigan – Sand Point Barber’s Point Light (Old) – New York – Lake Champlain – Barber’s Point Barcelona Light – New York – Lake Erie – Barcelona Lighthouse Battle Island Lightstation – Ontario – Lake Superior – Battle Island Light Beaver Head Light – Michigan – Lake Michigan – Beaver Island Beaver Island Harbor Light – Michigan – Lake Michigan – St. James (Beaver Island Harbor) Belle Isle Lighthouse – Michigan – Lake St. Clair – Belle Isle Bellevue Park Old Range Light – Michigan/Ontario – St. Mary’s River – Bellevue Park Bete Grise Light – Michigan – Lake Superior – Mendota (Bete Grise) Bete Grise Bay Light – Michigan – Lake Superior -
G-012011-1E Geological Precambrian Timeline Midwest
Copper Harbor Conglomerate Gunflint Formation: Breccia with white quartz Precambrian Geologic Events in the Mid-Continent of North America G-012011-1E 1 inch (Century Mine, Upper Peninsula MI) (Sibley Peninsula, Thunder Bay, ON) Compiled by: Steven D.J. Baumann, Alexandra B. Cory, Micaela M. Krol, Elisa J. Piispa Updated March 2013 Oldest known rock showing a dipole magnetic field: red dacite in Austrailia Paleomagnetic Line 3,800 3,700 3,600 3,500 3,400 3,300 3,200 3,100 3,000 2,900 2,800 2,700 2,600 2,500 2,400 2,300 2,200 2,100 2,000 1,900 1,800 1,700 1,600 1,500 1,400 1,300 1,200 1,100 1,000 900 800 700 600 500 Paleozoic Period Siderian Rhyacian Orosirian Statherian Calymmian Ectasian Stenian Tonian Cryogenian Ediacaran Eoarchean Paleoarchean Mesoarchean Neoarchean Era Paleoproterozoic Mesoproterozoic Neoproterozoic Eon Archean Proterozoic Pass Lake Kama Hill Sibley Group Sediments (Sibley Basin, Thunder Bay Area, ON) McGrath Gneiss McGrath Complex (EC MN) Metamorphic and cataclastic event Formation Formation Outan Island Formation Nipigon Formation Recent Era of Great Mid-continent Basin Formation (MI, IL, IA, IN, KY, MO) 2 inches Marshfield Archean Gneiss (C WI) Linwood Archean Migmatite (C WI) Sudbury Dike Swarm (SE ON) Quinnesec Formation Intrusions (NE WI) Quinnesec Formation Metamorphism (NE WI) Hatfield Gneiss (WC WI) Pre-Quinnesec Formations deposited (NE WI) Upper Rove Formation Baraboo Quartzite LEGEND (Sibley Peninsula, Thunder Bay, ON) Gray granodioritic phase Montevideo Gneiss (SW MN) Red granite phase Montevideo Gneiss -
North Lake Superior Métis
The Historical Roots of Métis Communities North of Lake Superior Gwynneth C. D. Jones Vancouver, B. C. 31 March 2015. Prepared for the Métis Nation of Ontario Table of Contents Introduction 3 Section I: The Early Fur Trade and Populations to 1821 The Fur Trade on Lakes Superior and Nipigon, 1600 – 1763 8 Post-Conquest Organization of the Fur Trade, 1761 – 1784 14 Nipigon, Michipicoten, Grand Portage, and Mixed-Ancestry Fur Trade Employees, 1789 - 1804 21 Grand Portage, Kaministiquia, and North West Company families, 1799 – 1805 29 Posts and Settlements, 1807 – 1817 33 Long Lake, 1815 – 1818 40 Michipicoten, 1817 – 1821 44 Fort William/Point Meuron, 1817 – 1821 49 The HBC, NWC and Mixed-Ancestry Populations to 1821 57 Fur Trade Culture to 1821 60 Section II: From the Merger to the Treaty: 1821 - 1850 After the Merger: Restructuring the Fur Trade and Associated Populations, 1821 - 1826 67 Fort William, 1823 - 1836 73 Nipigon, Pic, Long Lake and Michipicoten, 1823 - 1836 79 Families in the Lake Superior District, 1825 - 1835 81 Fur Trade People and Work, 1825 - 1841 85 "Half-breed Indians", 1823 - 1849 92 Fur Trade Culture, 1821 - 1850 95 Section III: The Robinson Treaties, 1850 Preparations for Treaty, 1845 - 1850 111 The Robinson Treaty and the Métis, 1850 - 1856 117 Fur Trade Culture on Lake Superior in the 1850s 128 After the Treaty, 1856 - 1859 138 2 Section IV: Persistence of Fur Trade Families on Lakes Superior and Nipigon, 1855 - 1901 Infrastructure Changes in the Lake Superior District, 1863 - 1921 158 Investigations into Robinson-Superior Treaty paylists, 1879 - 1899 160 The Dominion Census of 1901 169 Section V: The Twentieth Century Lake Nipigon Fisheries, 1884 - 1973 172 Métis Organizations in Lake Nipigon and Lake Superior, 1971 - 1973 180 Appendix: Maps and Illustrations Watercolour, “Miss Le Ronde, Hudson Bay Post, Lake Nipigon”, 1867?/1901 Map of Lake Nipigon in T. -
High Resolution Aeromagnetic Survey of Lake Superior
Eos, Vol. 72, No. 8, February 19, 1991 Eos, TRANSACTIONS, AMERICAN GEOPHYSICAL UNION VOLUME 72, NUMBER 8 FEBRUARY 19, 1991 PAGES 81-96 Lake Superior basin are part of the same sys tem. (See introduction to Wold and Hinze High Resolution [1982] for discussion.) Development of the MCR in the Lake Su perior region is attributed to extensive volca- Aeromagnetic Survey of nism and subsidence at approximately 1.1 b.y. [Palmer and Davis, 1987; Davis and Sutcliffe, 1985; Davis and Paces, 1990]. The Lake Superior MCR is a series of segmented grabens or—as suggested by Behrendt et al. [1988]— PAGES 81, 85-86 a series of juxtaposed half-grabens contain ing weakly deformed and metamorphosed D. J. Teskey, M. D. Thomas, R. A. Gibb, S. D. Dods, R. P. Kucks, sequences of sedimentary and volcanic V. W. Chandler, K. Fadaie, and J. D. Phillips rocks more than 30 km thick [Cannon et al., 1989]. In the west and central part of the lake, the Keweenaw fault (Figure 3) appears A 57,000 line kilometer, high-resolution Lake Superior area, a major objective of the to form a southern bounding-fault. The aeromagnetic survey was flown in 1987 as a program is to develop thermal, tectonic, and northern bounding-fault in the central por contribution to the Great Lakes International petrogenetic models for the evolution of the tion, the Isle Royale fault, continues to the Multidisciplinary Program on Crustal Evolu MCR and to evaluate these in the broader west, as indicated on this new aeromagnetic tion (GLIMPCE). Existing aeromagnetic data context of the tectonic evolution of the North map. -
Annual Report 2018–2019
Ecological Studies of Wolves on Isle Royale Annual Report 2018–2019 Sarah R. Hoy, Rolf O. Peterson, and John A. Vucetich School of Forest Resources and Environmental Science, Michigan Technological University Houghton, Michigan USA 49931-1295 March 31, 2019 During the past year, major support for these studies was received from the National Science Foundation (DEB-1453041), National Park Service (CESU Task Agreement No. P16AC000004), a McIntyre-Stennis Grant (USDA-Nifa #1004363), Rob- ert Bateman Endowment at the Michigan Tech Fund, James L. Bigley Revocable Trust, and Detroit Zoological Society. For the period, March 1, 2018 through February 28, 2019, additional contributions were received from the following organizations and individuals: Dianne W. Ashley, Karen A. Bacula, Dorthey L. Behrend, William and Merlene Black, Terri L. Bocklund, Jerry and Jennifer Boeckman, Ryan M. Bottorff, Joseph V. Brazie, Sheri A. Buller, David Carl, Violet Carl, Michael Casner, Jacqueline Chapin, Alex M. Christensen, Alison J. Clarke, Donald C. Close, Nicholas Conrardy, James Deignan, Detroit Zoological Society, Ronald and Barbara Eckoff, Mary C. Edgar, James Eder, Wendy Evans, Ronald L. Felzer, William and Shirley Ferguson, Gaylon and Sharon Ford, Larry Fuerst and Suzanne Scott, Marjorie H. Freeman, C. Michael and K. A. George, Charles and Barbara Grade, Edith N. Greene, Randolf A. Gschwind, John and Heidi Harland- er, Christine I. Hammond, Hal W. Hanson, Russ Harrison and Karen Fulcher, Carolyn Hefferman, John H. Heidtke, John Heneghan, Steve Hodges and Lori Checkley, Jeffrey Holden and Sandra Noll, Fred Hutchings, Robert and Sally Irmiger, Kellogg’s Corporation Citizenship Fund, Dr. Paul M. Kotila, Roddie Larsen, Dana and Donna Lowell, William and Nicole Maier, Michael J.