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The Legacy of the German Language in Papua New Guinea T
Craig Alan Voll<er The legacy of the German language in Papua New Guinea t. lntroduction' German colonial rule in the western Pacific began formally in 1884 when unbe- known to them, people in north-eastern New Guinea (Ifuiser Wilhelmsland), the archipelago around the Bismarck Sea, and in the next year, almost ali of neigh- boring Micronesia were proclaimed to be under German "protection". This act changed ways of living that had existed for tens of thousands of years and laid the foundation for what eventually became the modern state of Papua New Guinea. This proclamation was made in German, a language that was then unknown to Melanesians and Micronesians. Today the German language is again mostly unknown to most Melanesians and only a few visible traces of any German colonial legacy remain. There are no old colonial buildings, no monuments outside of a few small and almost hidden cemeteries, and no German Clubs or public signs in German. In this century there has not even been a German embassy. But it is impossible to step out in New Ireland (the former "Neu-Mecklenburg"), for example, without being con- fronted by a twenty-first century reality that is in part a creation of German col- onial rule. Species that were introduced by the Germans stiil retain their German name, frorn clover,I(lee in both German and the local Nalik language to pineap- ples (GermanAnanas / Nalik ananas). The best rural road in the country the Bulominski Highway was started by and named after the last German governor of Neu-Mecklenburg and a mountain range is known as the Schleinitz Range. -
Los Cien Montes Más Prominentes Del Planeta D
LOS CIEN MONTES MÁS PROMINENTES DEL PLANETA D. Metzler, E. Jurgalski, J. de Ferranti, A. Maizlish Nº Nombre Alt. Prom. Situación Lat. Long. Collado de referencia Alt. Lat. Long. 1 MOUNT EVEREST 8848 8848 Nepal/Tibet (China) 27°59'18" 86°55'27" 0 2 ACONCAGUA 6962 6962 Argentina -32°39'12" -70°00'39" 0 3 DENALI / MOUNT McKINLEY 6194 6144 Alaska (USA) 63°04'12" -151°00'15" SSW of Rivas (Nicaragua) 50 11°23'03" -85°51'11" 4 KILIMANJARO (KIBO) 5895 5885 Tanzania -3°04'33" 37°21'06" near Suez Canal 10 30°33'21" 32°07'04" 5 COLON/BOLIVAR * 5775 5584 Colombia 10°50'21" -73°41'09" local 191 10°43'51" -72°57'37" 6 MOUNT LOGAN 5959 5250 Yukon (Canada) 60°34'00" -140°24’14“ Mentasta Pass 709 62°55'19" -143°40’08“ 7 PICO DE ORIZABA / CITLALTÉPETL 5636 4922 Mexico 19°01'48" -97°16'15" Champagne Pass 714 60°47'26" -136°25'15" 8 VINSON MASSIF 4892 4892 Antarctica -78°31’32“ -85°37’02“ 0 New Guinea (Indonesia, Irian 9 PUNCAK JAYA / CARSTENSZ PYRAMID 4884 4884 -4°03'48" 137°11'09" 0 Jaya) 10 EL'BRUS 5642 4741 Russia 43°21'12" 42°26'21" West Pakistan 901 26°33'39" 63°39'17" 11 MONT BLANC 4808 4695 France 45°49'57" 06°51'52" near Ozero Kubenskoye 113 60°42'12" c.37°07'46" 12 DAMAVAND 5610 4667 Iran 35°57'18" 52°06'36" South of Kaukasus 943 42°01'27" 43°29'54" 13 KLYUCHEVSKAYA 4750 4649 Kamchatka (Russia) 56°03'15" 160°38'27" 101 60°23'27" 163°53'09" 14 NANGA PARBAT 8125 4608 Pakistan 35°14'21" 74°35'27" Zoji La 3517 34°16'39" 75°28'16" 15 MAUNA KEA 4205 4205 Hawaii (USA) 19°49'14" -155°28’05“ 0 16 JENGISH CHOKUSU 7435 4144 Kyrghysztan/China 42°02'15" 80°07'30" -
Kosipe Revisited
Peat in the mountains of New Guinea G.S. Hope Department of Archaeology and Natural History, Australian National University, Canberra, Australia _______________________________________________________________________________________ SUMMARY Peatlands are common in montane areas above 1,000 m in New Guinea and become extensive above 3,000 m in the subalpine zone. In the montane mires, swamp forests and grass or sedge fens predominate on swampy valley bottoms. These mires may be 4–8 m in depth and up to 30,000 years in age. In Papua New Guinea (PNG) there is about 2,250 km2 of montane peatland, and Papua Province (the Indonesian western half of the island) probably contains much more. Above 3,000 m, peat soils form under blanket bog on slopes as well as on valley floors. Vegetation types include cushion bog, grass bog and sedge fen. Typical peat depths are 0.5‒1 m on slopes, but valley floors and hollows contain up to 10 m of peat. The estimated total extent of mountain peatland is 14,800 km2 with 5,965 km2 in PNG and about 8,800 km2 in Papua Province. The stratigraphy, age structure and vegetation histories of 45 peatland or organic limnic sites above 750 m have been investigated since 1965. These record major vegetation shifts at 28,000, 17,000‒14,000 and 9,000 years ago and a variable history of human disturbance from 14,000 years ago with extensive clearance by the mid- Holocene at some sites. While montane peatlands were important agricultural centres in the Holocene, the introduction of new dryland crops has resulted in the abandonment of some peatlands in the last few centuries. -
Balkan Vegetation
Plant Formations in the Balkan BioProvince Peter Martin Rhind Balkan Mixed Deciduous Forest These forests vary enormously but usually include a variety of oak species such as Quercus cerris, Q. frainetto, Q. robur and Q. sessiliflora, and other broadleaved species like Acer campestris, Carpinus betulus, Castanea sative, Juglans regia, Ostrya carpinifolia and Tilia tomentosa. Balkan Montane Forest Above about 1000 m beech Fagus sylvatica forests often predominate, but beyond 1500 m up to about 1800 m various conifer communities form the main forest types. However, in some cases conifer and beech communities merge and both reach the tree line. The most important associates of beech include Acer platanoides, Betula verrucosa, Corylus colurna, Picea abies, Pyrus aucuparia and Ulmus scabra, while the shrub layer often consists of Alnus viridis, Euonymous latifolius, Pinus montana and Ruscus hypoglossum. The ground layer is not usually well developed and many of the herbaceous species are of central European distribution including Arabis turrita, Asperula muscosa, Cardamine bulbifera, Limodorum abortivum, Orthilia seconda and Saxifraga rotundifolia. Of the conifer forests, Pinus nigra (black pine) often forms the dominant species particularly in Bulgaria, Serbia and in the Rhodope massif. Associated trees may include Taxus buccata and the endemic Abies bovisii-regis (Macedonian fir), while the shrub layer typically includes Daphne blagayana, Erica carnea and the endemic Bruckenthalia spiculifolia (Ericaceae). In some areas there is a conifer forest above the black pine zone from about 1300 m to 2400 m in which the endemic Pinus heldreichii (Bosnian pine) predominates. It is often rather open possibly as a consequence of repeated fires. -
Description of the Ecoregions of the United States
(iii) ~ Agrl~:::~~;~":,c ullur. Description of the ~:::;. Ecoregions of the ==-'Number 1391 United States •• .~ • /..';;\:?;;.. \ United State. (;lAn) Department of Description of the .~ Agriculture Forest Ecoregions of the Service October United States 1980 Compiled by Robert G. Bailey Formerly Regional geographer, Intermountain Region; currently geographer, Rocky Mountain Forest and Range Experiment Station Prepared in cooperation with U.S. Fish and Wildlife Service and originally published as an unnumbered publication by the Intermountain Region, USDA Forest Service, Ogden, Utah In April 1979, the Agency leaders of the Bureau of Land Manage ment, Forest Service, Fish and Wildlife Service, Geological Survey, and Soil Conservation Service endorsed the concept of a national classification system developed by the Resources Evaluation Tech niques Program at the Rocky Mountain Forest and Range Experiment Station, to be used for renewable resources evaluation. The classifica tion system consists of four components (vegetation, soil, landform, and water), a proposed procedure for integrating the components into ecological response units, and a programmed procedure for integrating the ecological response units into ecosystem associations. The classification system described here is the result of literature synthesis and limited field testing and evaluation. It presents one procedure for defining, describing, and displaying ecosystems with respect to geographical distribution. The system and others are undergoing rigorous evaluation to determine the most appropriate procedure for defining and describing ecosystem associations. Bailey, Robert G. 1980. Description of the ecoregions of the United States. U. S. Department of Agriculture, Miscellaneous Publication No. 1391, 77 pp. This publication briefly describes and illustrates the Nation's ecosystem regions as shown in the 1976 map, "Ecoregions of the United States." A copy of this map, described in the Introduction, can be found between the last page and the back cover of this publication. -
Altitudinal and Polar Treelines in the Northern Hemisphere – Causes and Response to Climate Change
Umbruch 79 (3) 05.08.2010 23:45 Uhr Seite 139 Polarforschung 79 (3), 139 – 153, 2009 (erschienen 2010 Altitudinal and Polar Treelines in the Northern Hemisphere – Causes and Response to Climate Change by Friedrich-Karl Holtmeier1* and Gabriele Broll2 Abstract: This paper provides an overview on the main treeline-controlling dem Vorrücken der Baumgrenze in größere, wesentlich windigere Höhen factors and on the regional variety as well as on heterogeneity and response to relativ zunehmen. Die Verlagerung der Baumgrenze in größere Höhen und changing environmental conditions of both altitudinal and northern treelines. weiter nach Norden wird zu grundlegenden Veränderungen der Landschaft in From a global viewpoint, treeline position can be attributed to heat deficiency. den Hochgebirgen und am Rande von Subarktis/Arktis führen, die auch wirt- At smaller scales however, treeline position, spatial pattern and dynamics schaftliche Folgen haben werden. depend on multiple and often elusive interactions due to many natural factors and human impact. After the end of the Little Ice Age climate warming initiated tree establishment within the treeline ecotone and beyond the upper INTRODUCTION and northern tree limit. Tree establishment peaked from the 1920s to the 1940s and resumed again in the 1970s. Regional and local variations occur. In most areas, tree recruitment has been most successful in the treeline ecotone Global warming since the end of the “Little Ice Age” (about while new trees are still sporadic in the adjacent alpine or northern tundra. 1900) is bringing about socio-economic changes, shrinking Lack of local seed sources has often delayed tree advance to higher elevation. -
Identification of Recent Factors That Affect the Formation of the Upper Tree Line in Eastern Serbia
Arch. Biol. Sci., Belgrade, 63 (3), 825-830, 2011 DOI:10.2298/ABS1103825D IDENTIFICATION OF RECENT FACTORS THAT AFFECT THE FORMATION OF THE UPPER TREE LINE IN EASTERN SERBIA V. DUCIĆ1, B. MILOVANOVIĆ2 and S. ĐURĐIĆ1 1 University of Belgrade, Faculty of Geography, 11000 Belgrade, Serbia 2Geographical Institute “Jovan Cvijić”, Serbian Academy of Sciences and Arts, 11000 Belgrade, Serbia Abstract - The recent climate changes, among others, have contributed to the change in elevation of the upper tree line in high mountainous areas. At the same time, direct anthropogenic impact on the fragile ecosystems of high mountains has also been significant. The aim of this paper is to determine the actual dynamics of the formation of upper tree line in eastern Serbia and to identify the recent factors which condition it. The results obtained show that preconditions have been accomplished for the upper tree line increase, but this has not completely been confirmed by previous field researches. Key words: Upper tree line, climate changes, temperature gradient, Mt. Stara Planina, anthropogenic influence, depopula- tion. UDC 574:551.583(497.11-11) INTRODUCTION the upper tree line in eastern Serbia and to identify some of the recent factors by which it is conditioned. In conditions when changes in abiotic and biotic en- The Stara Planina mountain, as the most prominent vironment are intense and diverse, the question aris- high-altitude zone of the region, was examined. The es as to the origin and magnitude of potential factors study assumes that changes in the high-altitude lim- that influence the location, i.e. changes in elevation of its of forest spreading occurs in response to changes the upper tree line. -
Papua New Guinea Highlands and Mt Wilhelm 1978 Part 1
PAPUA NEW GUINEA HIGHLANDS AND MT WILHELM 1978 PART 1 The predawn forest became alive with the melodic calls of unseen thrushes, and the piercing calls of distant parrots. The skies revealed the warmth of the morning dawn revealing thunderheads over the distant mountains that seemed to reach the melting stars as the night sky disappeared. I was 30 meters above the ground in a tree blind climbed before dawn. Swirling mists enshrouded the steep jungle canopy amidst a great diversity of forest trees. I was waiting for male lesser birds of paradise Paradisaea minor to come in to a tree lek next to the blind, where males compete for prominent perches and defend them from rivals. From these perch’s males display by clapping their wings and shaking their head. At sunrise, two male Lesser Birds-of-Paradise arrived, scuffled for the highest perch and called with a series of loud far-carrying cries that increase in intensity. They then displayed and bobbed their yellow-and-iridescent-green heads for attention, spreading their feathers wide and hopped about madly, singing a one-note tune. The birds then lowered their heads, continuing to display their billowing golden white plumage rising above their rust-red wings. A less dazzling female flew in and moved around between the males critically choosing one, mated, then flew off. I was privileged to have used a researcher study blind and see one of the most unique group of birds in the world endemic to Papua New Guinea and its nearby islands. Lesser bird of paradise lek near Mt Kaindi near Wau Ecology Institute Birds of paradise are in the crow family, with intelligent crow behavior, and with amazingly complex sexual mate behavior. -
The Climate of Mt Wilhelm RJ Hnatiuk JM B Smith D N Mcvean Mt Wilhelm Studies 2
Mt Wilhelm Studies 2 The Climate of Mt Wilhelm RJ Hnatiuk JM B Smith D N Mcvean Mt Wilhelm Studies 2 TheRJ Hnatiuk Climate JM B Smith of DMt N Mcvean Wilhelm Research School of Pacific Studies Department of Biogeography & Geomorphology Publication BG/4 The Australian National University, Canberra Printed and Published in Australia at The Australian National University 1976 National Library of Australia Card No. and I.S.B.N. 0 7081 1335 4 © 1976 Australian National University This Book is copyright. Apart from any fair dealing for the purpose of private study, research, criticism, or review, as permitted under the Copyright Act, no part may be reproduced by any process without written permission . Printed at: SOCPAC Printery The Research Schools of Social Science and Pacific Studies H.C. Coombs Building, ANU Distributed for the Department by: The Australian National University Press The Climate of Mt Wilhelm PREFACE In 1966, the Australian National University with assistance from the Bernice P. Bishop Museum, Hawaii, established a field station beside the lower Pindaunde Lake at an altitude of 3480 m on the south- east flank of Mt Wilhelm, the highest point in Papua New Guinea. The field station has been used by a number of workers in the natural sciences, many of whose publications are referred to later in this work. The present volume arises from observations made by three botanists and their collaborators when members of the Department of Biogeography and Geomorphology, during the course of their work on Mt Wilhelm while based on the ANU field station. It is the second in the Departmental series describing the environment and biota of the mountain, and will be followed by others dealing with different aspects of its natural history. -
C073p135.Pdf
Vol. 73: 135–150, 2017 CLIMATE RESEARCH Published August 21 https://doi.org/10.3354/cr01465 Clim Res Contribution to CR Special 34 ‘SENSFOR: Resilience in SENSitive mountain FORest ecosystems OPENPEN under environmental change’ ACCESSCCESS Drivers of treeline shift in different European mountains Pavel Cudlín1,*, Matija Klop<i<2, Roberto Tognetti3,4, Frantisek Máliˇs5,6, Concepción L. Alados7, Peter Bebi8, Karsten Grunewald9, Miglena Zhiyanski10, Vlatko Andonowski11, Nicola La Porta12, Svetla Bratanova-Doncheva13, Eli Kachaunova13, Magda Edwards-Jonášová1, Josep Maria Ninot14, Andreas Rigling15, Annika Hofgaard16, Tomáš Hlásny17, Petr Skalák1,18, Frans Emil Wielgolaski19 1Global Change Research Institute CAS, Academy of Sciences of the Czech Republic, Cˇ eské Bude˘jovice 370 05, Czech Republic 2University of Ljubljana, Biotechnical Faculty, Department of Forestry and Renewable Forest Resources, Slovenia 3Dipartimento di Bioscienze e Territorio, Iniversità degli Studio del Molise, Contrada Fonte Lappone, 86090 Pesche, Italy 4MOUNTFOR Project Centre, European Forest Institute, 38010 San Michele all Adige (Trento), Italy 5Technical University Zvolen, Faculty of Forestry, 960 53 Zvolen, Slovakia 6National Forest Centre, Forest Research Institute Zvolen, 960 92 Zvolen, Slovakia 7Pyrenean Institute of Ecology (CSIC), Apdo. 13034, 50080 Zaragoza, Spain 8WSL Institute for Snow and Avalanche Research SLF, 7260 Davos Dorf, Switzerland 9Leibniz Institute of Ecological Urban and Regional Development, 01217 Dresden, Germany 10Forest Research Institute, -
Age-Dependent Growth Responses to Climate from Trees in Himalayan Treeline
ISSN: 2705-4403 (Print) & 2705-4411 (Online) www.cdztu.edu.np/njz Vol. 4 | Issue 1| August 2020 Research Article https://doi.org/10.3126/njz.v4i1.30669 Age-dependent growth responses to climate from trees in Himalayan treeline Achyut Tiwari1* 1 Central Department of Botany, Institute of Science and Technology, Tribhuvan University, Kirtipur Kathmandu, Nepal * Correspondence: [email protected] Received: 19 July 2019 | Revised: 24 July 2020 | Accepted: 27 July 2020 Abstract Tree rings provide an important biological archive for climate history in relation to the physiological mechanism of tree growth. Higher elevation forests including treelines are reliable indicators of climatic changes, and tree growth at most elevational treelines are sensitive to temperature at moist regions, while it is sensitive to moisture in semi-arid regions. However, there has been very less pieces of evidence regarding the age-related growth sensitivity of high mountain tree species. This study identified the key difference on the growth response of younger (<30 years of age) and older (>30 years) Abeis spectabilis trees from treeline ecotone of the Trans-Himalayan region in central Nepal. The adult trees showed a stronger positive correlation with precipitation (moisture) over juveniles giving the evidence of higher demand of water for adult trees, particularly in early growth seasons (March to May). The relationship between tree ring width indices and mean temperature was also different in juveniles and adult individuals, indicating that the juveniles are more sensitive to temperature whereas the adults are more sensitive to moisture availability. It is emphasized that the age-dependent growth response to climate has to be considered while analyzing the growth-climate relationship of high mountain tree populations. -
The Polar Regions
TEACHING DOSSIER 1 ENGLISH, GEOGRAPHY, SCIENCE, ECONOMICS THE POLAR REGIONS ANTARCTIC, ARCTIC, GEOGRAPHY, CLIMATE, FAUNA, FLORA, CLIMATE CHANGE, THREATS, CONSERVATION NORTH POLE SOUTH POLE 2 dossier CZE N° 1 THEORY SECTION THE ARCTIC AND ANTARCTIC The Arctic and the Antarctic have a number of points in common: low temperatures, darkness that lasts for several weeks or months in winter, and magnificent expanses of ice... There are several different types of ice1, including sea ice, which is ice that contains salt, and ice caps and icebergs, which consist solely of freshwater ice. How- ever, once we get past these initial similarities, it doesn’t take long to realise that the Arctic and the Antarctic are two totally different regions. THE ARCTIC - Frozen ocean surrounded by land - North Pole: located approximately in the centre of the Arctic Ocean - Ocean covered to a large extent by permanent sea ice - Holds almost 10% of all the Earth’s continental ice (7% of the world’s reserves of freshwater) - Outer limit: place where the temperature never exceeds 10°C during the warmest month (July) - Area: 21 million km2 (14 million km2 of which is the Arctic Ocean) Ice drift Maximum extent of the sea ice in summer Maximum extent of the sea ice in winter Outer limit of the Arctic 10°C Figure 1: Outer limit of the Arctic and seasonal variation of the sea ice The Arctic Ocean is bordered by broad, shallow continental plates and consists of two main basins (4 km deep on average) separated by a range of underwater mountains: the Lomonosov Ridge, which joins the north of Greenland to the New Siberia Archipelago along a line that runs close to the North Pole.