THE ECOLOGICAL VALUES of the WESTERN MAINE MOUNTAINS By
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' Committee on Environment and Natural
’ PO Box 164 - Greenville Junction, ME 04442 Testimony Before the Committee on Environment and Natural Resources on LD 901, HP 0629 An Act to Amend the Laws Governing the Determination of a Wind Energy Development's Efiect on the Scenic Character of Maine’s Special Places March 23, 2017 Senator Saviello, Representative Tucker, Distinguished Members of the Committee: My name is Christopher King, I live in Greenville, and I am Secretary of the Moosehead Region Futures Committee (MRFC), a Maine non-profit corporation, which has been active in shaping the Moosehead Lake Region's future development for more than a decade. I wish to testify in favor of LD 901, and to urge the Committee to adopt certain amendments to this bill. Specifically, the MRFC requests that the Committee amend LD 901, by adding to the language proposed in Section 3 (35-A MRSA §3452, sub-§4), paragraph B, the following subparagraphs: {Q} Big Moose Mountain in Piscataquis County; and ('7) Mount Kineo in Piscataquis County. MRFC TESTIMONY ow LD 901 BEFORE ENR COMMIITEE - 3/23/2017 - PAGE 1 OF 3 The purpose of LD 901 is to extend the protections granted by the Legislature in 35-A MRSA §3452 to Maine’s scenic resources of state or national significance (SRSNS), defined with precision in 35-A MRSA §3451 (9), to certain SRSNSs which are situated between 8 and 15 miles from a proposed wind energy development’s generating facilities. Currently, the Department of Environmental Protection “shall consider insignificant the effects of portions of [a wind energy] development’s generating facilities located more than 8 miles...from a [SRSNS].” 35-A MRSA §3452 (3). -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
Reduced Net Methane Emissions Due to Microbial Methane Oxidation in a Warmer Arctic
LETTERS https://doi.org/10.1038/s41558-020-0734-z Reduced net methane emissions due to microbial methane oxidation in a warmer Arctic Youmi Oh 1, Qianlai Zhuang 1,2,3 ✉ , Licheng Liu1, Lisa R. Welp 1,2, Maggie C. Y. Lau4,9, Tullis C. Onstott4, David Medvigy 5, Lori Bruhwiler6, Edward J. Dlugokencky6, Gustaf Hugelius 7, Ludovica D’Imperio8 and Bo Elberling 8 Methane emissions from organic-rich soils in the Arctic have bacteria (methanotrophs) and the remainder is mostly emitted into been extensively studied due to their potential to increase the atmosphere (Fig. 1a). The methanotrophs in these wet organic the atmospheric methane burden as permafrost thaws1–3. soils may be low-affinity methanotrophs (LAMs) that require However, this methane source might have been overestimated >600 ppm of methane (by moles) for their growth and mainte- without considering high-affinity methanotrophs (HAMs; nance23. But in dry mineral soils, the dominant methanotrophs are methane-oxidizing bacteria) recently identified in Arctic min- high-affinity methanotrophs (HAMs), which can survive and grow 4–7 eral soils . Herein we find that integrating the dynamics of at a level of atmospheric methane abundance ([CH4]atm) of about HAMs and methanogens into a biogeochemistry model8–10 1.8 ppm (Fig. 1b)24. that includes permafrost soil organic carbon dynamics3 leads Quantification of the previously underestimated HAM-driven −1 to the upland methane sink doubling (~5.5 Tg CH4 yr ) north of methane sink is needed to improve our understanding of Arctic 50 °N in simulations from 2000–2016. The increase is equiva- methane budgets. -
Évolution Spatio-Temporelle Du Pergélisol Alpin Marginal Au Mont Jacques-Cartier, Massif Des Chic-Chocs, Gaspésie (Qc)
Université de Montréal Évolution spatio-temporelle du pergélisol alpin marginal au mont Jacques-Cartier, massif des Chic-Chocs, Gaspésie (Qc) par Gautier DAVESNE Département de Géographie Faculté des arts et sciences Mémoire présenté à la Faculté des arts et des sciences en vue de l’obtention du grade de maîtrise en géographie Août 2015 © Gautier Davesne, 2015 ii Université de Montréal Faculté des études supérieures et postdoctorales Ce mémoire intitulé : Évolution spatio-temporelle du pergélisol alpin marginal au mont Jacques-Cartier, massif des Chic- Chocs, Gaspésie (Qc) Présenté par : Gautier Davesne a été évalué par un jury composé des personnes suivantes : François Cavayas, président rapporteur Daniel Fortier, directeur de recherche James Gray, membre du jury iii iv Résumé L’objectif de ce mémoire est d’acquérir une connaissance détaillée sur l’évolution spatiale de la température de surface du sol (GST) au mont Jacques-Cartier et sur la réponse thermique de son îlot de pergélisol alpin aux changements climatiques passés et futurs. L’étude est basée sur un ensemble de mesures de température (GST, sous-sol) et de neige, ainsi que des modèles spatiaux de distribution potentielle de la GST et des simulations numériques du régime thermique du sol. Les résultats montrent que la distribution de la GST sur le plateau est principalement corrélée avec la répartition du couvert nival. Au-dessus de la limite de la végétation, le plateau est caractérisé par un couvert de neige peu épais et discontinu en hiver en raison de la topographie du site et l’action des forts vents. La GST est alors couplée avec les températures de l’air amenant des conditions froides en surface. -
Taiga Plains
ECOLOGICAL REGIONS OF THE NORTHWEST TERRITORIES Taiga Plains Ecosystem Classification Group Department of Environment and Natural Resources Government of the Northwest Territories Revised 2009 ECOLOGICAL REGIONS OF THE NORTHWEST TERRITORIES TAIGA PLAINS This report may be cited as: Ecosystem Classification Group. 2007 (rev. 2009). Ecological Regions of the Northwest Territories – Taiga Plains. Department of Environment and Natural Resources, Government of the Northwest Territories, Yellowknife, NT, Canada. viii + 173 pp. + folded insert map. ISBN 0-7708-0161-7 Web Site: http://www.enr.gov.nt.ca/index.html For more information contact: Department of Environment and Natural Resources P.O. Box 1320 Yellowknife, NT X1A 2L9 Phone: (867) 920-8064 Fax: (867) 873-0293 About the cover: The small photographs in the inset boxes are enlarged with captions on pages 22 (Taiga Plains High Subarctic (HS) Ecoregion), 52 (Taiga Plains Low Subarctic (LS) Ecoregion), 82 (Taiga Plains High Boreal (HB) Ecoregion), and 96 (Taiga Plains Mid-Boreal (MB) Ecoregion). Aerial photographs: Dave Downing (Timberline Natural Resource Group). Ground photographs and photograph of cloudberry: Bob Decker (Government of the Northwest Territories). Other plant photographs: Christian Bucher. Members of the Ecosystem Classification Group Dave Downing Ecologist, Timberline Natural Resource Group, Edmonton, Alberta. Bob Decker Forest Ecologist, Forest Management Division, Department of Environment and Natural Resources, Government of the Northwest Territories, Hay River, Northwest Territories. Bas Oosenbrug Habitat Conservation Biologist, Wildlife Division, Department of Environment and Natural Resources, Government of the Northwest Territories, Yellowknife, Northwest Territories. Charles Tarnocai Research Scientist, Agriculture and Agri-Food Canada, Ottawa, Ontario. Tom Chowns Environmental Consultant, Powassan, Ontario. Chris Hampel Geographic Information System Specialist/Resource Analyst, Timberline Natural Resource Group, Edmonton, Alberta. -
Alpine Tundra
National Park Rocky Mountain Colorado National Park Service U.S. Department of the Interior Alpine Tundra WHAT IS ALPINE TUNDRA? Where mountaintops rise Arctic tundra occurs around like islands above a sea of the north pole. Alpine tundra trees lies the world of the crowns mountains that alpine tundra. John Muir reach above treeline. called it "a land of deso ...a world by itself lation covered with beautiful Rocky Mountain National in the sky. light." Yet this light shines Park is recognized world on a tapestry of living detail. wide as a Biosphere Reserve —Enos Mills Tundra lands too cold for because of the beauty and trees support over 200 kinds research value of its alpine of plants, as well as animals wild lands. Alpine tundra is from bighorn to butterflies. a sensitive indicator of such climatic changes as global Tundra is a Russian word for warming and acid rain. Over "land of no trees." 1/3 of the park is tundra. HOW FRAGILE IS IT? For 25 years after Trail That is why busy stops Ridge Road opened in 1932, along Trail Ridge Road are people had free run on the marked as Tundra Protection tundra. Repeated trampling Areas where no walking off damaged popular places. the trail is allowed. Some of these areas, fenced Elsewhere, walking on the off in 1959 for study, show tundra is permitted. But almost no sign of recovery walk with care! Step lightly, today. High winds and long without scuffing the winters make new growth surface. Step on rocks slow. Trampled places may when you can. -
Franklin County by Foot and Paddle Doug Dunlap
Franklin County by Foot and Paddle Doug Dunlap Progress Report September 15, 2020 For walks and hikes; and travel by kayak and canoe, August 31-September 15, 2020 Discoveries: The United Way and the 2-1-1 phone number, Six Months into the Pandemic Over the past two weeks I have learned much about 2-1-1, a major, indispensable service to people of Franklin County, and throughout Maine, led by the United Way. The United Way of the Tri-Valley continues to serve as a vital safety net for Franklin County residents. The 2-1-1 project is an indispensable service. This is a 24/7 service, staffed by call specialists who take calls from people seeking help of many kinds: food, clothing, shelter, heat; access to mental health services, help with caring for a sick or incapacitated family member, financial burdens of many kinds. United Ways throughout Maine fund this service, in cooperation with the State of Maine. There is always someone to take the call, always available to help guide the calling person to someone who may speak to the very specific need expressed. 2-1-1 was available prior to the COVID-19 pandemic, and widely used by thousands of callers each year. I am informed by United Way leadership that in 2020, Maine 2-1- 1 has received 36,000 pandemic related calls since the month of March. That amounts to 6000 calls per month for six months, an average of 200 calls per day. That is an astonishing figure. It costs money to provide the service. -
R E V I E W a Joint Publication of the Margaret Chase Smith Policy Center and the Margaret Chase Smith Library Maine Policy R E V I E W
Winter 2007 · Vol. 16, No. 2· $14 MAINE POLICY REVIEW A Joint Publication of the Margaret Chase Smith Policy Center and the Margaret Chase Smith Library MAINE POLICY REVIEW View current & previous issues of MPR at: www.umaine.edu/mcsc/mpr.htm Volume 16, Number 2 · MAINE POLICY REVIEW · 1 EDITORIAL BOARD & STAFF PUBLISHERS EdITORIAL BOARD MARGARET CHASE SMITH POLICY CENTER ROBIN ALDEN DON NICOLL Glenn Beamer, Director Stonington, ME Nicoll & Associates SANdfORD BLITZ CHRISTOPHER “KIT” ST. JOHN MARGARET CHASE SMITH LIBRARY EMESBEE Associates Maine Center for Economic Policy Greg Gallant, Director DAVID BOULTER VAUGHN STINSON The Legislative Council, Maine State Legislature Maine Tourism Association EDITORIAL STAFF BRUCE CLARY MIKE TRAINOR Edmund S. Muskie School of Public Service, USM Eaton, Peabody, Bradford & Veague EdITOR Kathryn Hunt NANCY GRAPE JERRY WHALEN Margaret Chase Smith Policy Center Maine Sunday Telegram Eastern Maine Healthcare MANAGING EdITOR WALTER HARRIS WENDY WOLF Ann Acheson College of Education, UM Maine Health Access Foundation Margaret Chase Smith Policy Center JAMES HENDERSON ASSISTANT MANAGING EdITOR Maine State Archives Barbara Harrity LLOYD IRLAND Margaret Chase Smith Policy Center The Irland Group PRODUCTION MEREDITH JONES Beth Goodnight Maine Commmunity Foundation Goodnight Design MARGE KILKELLY CIRCULATION Council of State Governments Serena Bemis-Goodall Margaret Chase Smith Policy Center JULIUS KREVANS WEB SITE MAINTENANCE Bar Harbor, ME Sharon LaBrie LAURIE LACHANCE Margaret Chase Smith Policy Center Maine Development Foundation DEVELOpmENT CHRIS LOckwOOD Eva McLaughlin Maine Municipal Association Margaret Chase Smith Policy Center Ed McLAUGHLIN COVER ILLUSTRATION Maine Economic Research Institute Robert Shetterly PETER MILLS PRINTING Wright & Mills J. S. McCarthy Printers Maine Policy Review (ISSN 1064-2587) publishes independent analyses of public policy issues revelant to Maine. -
The Exchange of Carbon Dioxide Between Wet Arctic Tundra and the Atmosphere at the Lena River Delta, Northern Siberia
Biogeosciences, 4, 869–890, 2007 www.biogeosciences.net/4/869/2007/ Biogeosciences © Author(s) 2007. This work is licensed under a Creative Commons License. The exchange of carbon dioxide between wet arctic tundra and the atmosphere at the Lena River Delta, Northern Siberia L. Kutzbach1,*, C. Wille1,*, and E.-M. Pfeiffer2 1Alfred Wegener Institute for Polar and Marine Research, Research Unit Potsdam, Telegrafenberg A43, 14473 Potsdam, Germany 2University of Hamburg, Institute of Soil Science, Allende-Platz 2, 20146 Hamburg, Germany *now at Ernst Moritz Arndt University Greifswald, Institute for Botany and Landscape Ecology, Grimmer Straße 88, 17487 Greifswald, Germany Received: 23 May 2007 – Published in Biogeosciences Discuss.: 25 June 2007 Revised: 1 October 2007 – Accepted: 8 October 2007 – Published: 18 October 2007 Abstract. The exchange fluxes of carbon dioxide between piration continued at substantial rates during autumn when wet arctic polygonal tundra and the atmosphere were inves- photosynthesis had ceased and the soils were still largely un- tigated by the micrometeorological eddy covariance method. frozen. The temporal variability of the ecosystem respiration The investigation site was situated in the centre of the Lena during summer was best explained by an exponential func- River Delta in Northern Siberia (72◦220 N, 126◦300 E). The tion with surface temperature, and not soil temperature, as study region is characterized by a polar and distinctly con- the independent variable. This was explained by the ma- tinental climate, very cold and ice-rich permafrost and its jor role of the plant respiration within the CO2 balance of position at the interface between the Eurasian continent and the tundra ecosystem. -
Alpine Soils on Mount Mansfield, Vermont
Alpine Soils on Mount Mansfi eld, Vermont, USA: Pedology, History, and Intraregional Comparison Jeffrey S. Munroe* The highest summits in the northeastern United States rise above the tree line and support Geology Dep. unique islands of alpine tundra. Little is known about the properties and history of these soils Middlebury College and it is unclear how soils compare between the separate, isolated alpine areas. As a step toward Middlebury, VT 05753 addressing this oversight, the physical and chemical properties of alpine soils were investigated on Mt. Mansfi eld, the highest mountain in Vermont. Soil thickness was determined through probing, while profi le development and horizon properties were investigated in 31 excava- tions. Soil covers ∼85% of the study area, with profi les averaging 18 cm thick (maximum of 58 cm). Most profi les demonstrate a variation on the sequence Oi, Oa and/or A, Bw or Bs (rare), AC, and Cr horizons. The Oa horizons contain signifi cantly more C, Ca, K, and Mg than A horizons, and have higher cation exchange capacity and base saturation, and lower pH values. Almost one-third of the profi les were classifi ed as Histosols, while nearly twice as many were classifi ed as Entisols. Only two profi les contained cambic horizons and were classifi ed as Inceptisols. Histosols contained signifi cantly more K and organic matter than Entisols. A buried Sphagnum layer, radiocarbon dated to approximately 1000 yr ago, suggests a wetter climate at that time. Mount Mansfi eld soils are generally thinner than those described from nearby alpine environments and contain more organic matter with higher C/N ratios. -
High Peaks Region Recreation Plan
High Peaks Region Recreation Plan An overview and analysis of the recreation, possibilities, and issues facing the High Peaks Region of Maine Chris Colin, Jacob Deslauriers, Dr. Chris Beach Fall 2008 Maine Appalachian Trail Land Trust – High Peaks Initiative: The Maine Appalachian Trail Land Trust (MATLT) was formed in June 2002 by a group of Mainers dedicated to the preservation of the natural qualities of the lands surrounding the Appalachian Trail in Maine. Following its campaign to acquire Mount Abraham and a portion of Saddleback Mountain, MATLT is embarking on a new initiative to research and document the ecological qualities of the entire Western Maine High Peaks Region. The MATLT website describes the region as follows: “The Western Maine High Peaks Region is the 203,400 acres roughly bounded by the communities of Rangeley, Phillips, Kingfield and Stratton. In this region, there are about 21,000 acres above 2700 feet. It is one of only three areas in Maine where the mountains rise above 4000 feet. The other two are the Mahoosuc Range and Baxter Park. Eight (8) of the fourteen (14) highest mountains in Maine are in this region (Sugarloaf, Crocker, South Crocker, Saddleback, Abraham, The Horn, Spaulding and Redington Peak.) These are all above 4000 feet. If one adds the Bigelow Range, across Route 27/16 from Sugarloaf, the region hosts ten (10) of the highest mountains (Avery Peak and West Peak added)). This area is comparable in size to Baxter Park but has 40% more area above 2700 feet.” Table of Contents I. Introduction ............................................................................................................................................... 1 A. Purpose and Need for High Peaks Area Recreation Plan .................................................................... -
Waterville Caniba Naturals
in Maine June 6, 2018 Special Advertising Supplement Kennebec Journal Morning Sentinel 2 Wednesday, June 6, 2018 _______________________________________________________Advertising Supplement • Kennebec Journal • Morning Sentinel INDEX OF ADVERTISERS AUTOMOTIVE CANNABIS CONNECTION St. Joseph Maronite Catholic Columbia Classic Cars...................13 Cannabis Connection Directories 70-71 Church ..........................................65 Skowhegan & Waterville Caniba Naturals ..............................70 St. Mary............................................65 Tire Center ....................................26 Cannabis Healing Center, The .......70 St. Michael Parish ...........................65 Father Jimmy’s ...............................70 Sugarloaf Christian Ministry ..........65 ANIMALS & Harry Brown’s Farm .......................70 Summer Worship Directory ...........65 PETS Homegrown Healthcare Union Church of Belgrade Lakes Paws and Claws........................19, 57 Apothecary & Learning Center ...71 United Methodist Church ............65 Companion Animal Clinic ..............57 Integr8 Health..................................70 Unity United Methodist Church .....65 Hometown Veterinary Care ............57 Limited Edition Farm, LLC - Vassalboro United Methodist Kennebec Veterinary Care .............57 Medical Marijuana........................71 Church ..........................................65 Veterinary and Kennel Directory ..... 57 Maja’s ...............................................71 Waterville First Baptist Church