Lynx Reintroductions in Fragmented Landscapes of Germany: Projects with a Future Or Misunderstood Wildlife Conservation?
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Potential European Bison (Bison Bonasus) Habitat in Germany
PROJECT REPORT Potential European bison (Bison bonasus) habitat in Germany Tobias Kuemmerle Humboldt-University Berlin Benjamin Bleyhl Humboldt-University Berlin Wanda Olech University of Warsaw & European Bison Friends Society Kajetan Perzanowski Carpathian Wildlife Research Station MIZ, PAS & European Bison Friends Society 1 PROJECT REPORT CONTENTS CONTENTS ...............................................................................................................................................................2 INTRODUCTION .......................................................................................................................................................3 HISTORIC DISTRIBUTION OF EUROPEAN BISON IN EUROPE .....................................................................................4 EUROPEAN BISON HABITAT PREFERENCES ..............................................................................................................6 HABITAT USE OF CONTEMPORARY EUROPEAN BISON POPULATIONS .......................................................................................... 6 PALEO-ECOLOGICAL DATA ON EUROPEAN BISON HABITAT USE ............................................................................................... 10 MAPPING EUROPEAN BISON HABITAT IN GERMANY ............................................................................................ 10 APPROACH ................................................................................................................................................................. -
Offenbach, 30 January 2015 – Frequent Weather Systems Coming in from the West Brought Varied Weather to Germany in January 2015
The weather in Germany in January 2015 Year of record temperatures in 2014 followed by a much too warm January 2015 Offenbach, 30 January 2015 – Frequent weather systems coming in from the west brought varied weather to Germany in January 2015. Everything was included, from spring-like warmth with record temperatures and severe storms to brief wintry interludes. Overall, the month was very mild with high precipitation and little sunshine. This is what the initial analysis by the Deutscher Wetterdienst (DWD) of data from its around 2,000 weather stations shows. Periods of spring-like warmth with record temperatures Following on from the year of 2014, which was the warmest since records began, January 2015, too, saw a positive temperature anomaly. At 2.1 degrees Celsius (°C), the average temperature was 2.6 degrees higher than the international reference value for 1961 to 1990 of -0.5°C. Compared to the warmer period 1981 to 2010, the deviation was +1.7°C. The influence of high pressure prevailed at the start of the month, but brought weather with little cloud cover only to the south. This caused the temperature over the snow cover existing there to fall and give hard frosts. Leutkirch-Herlazhofen in the Württemberg part of the Allgäu recorded the lowest temperature in January with -15.2°C in the night to 1 January. After that, lively westerly winds, which generally brought very mild air masses, prevailed under the influence of low pressure during the first twenty days of the month. On 10 January, the storm depression ‘Felix’ brought spring-like warmth to Germany. -
Biodiversity of the Hercynian Mountains of Central Europe
Pirineos, 151-152: 83 a 99, JACA; 1998 BIODIVERSITY OF THE HERCYNIAN MOUNTAINS OF CENTRAL EUROPE JAN JENÍK Faculty of Science, Charles University, Benátská 2, CZ-12801 Praha 2, Czech Republic SUMMARY.- The vegetation of temperate Central Europe north of the Alps is mainly of low diversity broadleaf and conifer forest. The occurrence of three azonal habitat types: mires with their numerous microhabitats, the georelief of the karst and its deeply-cut river valleys, and ecological islands with a distinct vegetation near the treeline of the middle-mountains causes local areas of high diversity. These high species diversity spots are the result of an interplay between physical, biotic and historical factors. A model of an anemo-orographic system with its underlying factors is described to explain the high plant and animal diversity in the corries (glacial cirques) of the Hercynian mountains. RÉSUMÉ.-La végétation de l'Europe Centrale tempérée au nord des Alpes nous montre surtout des forêts à de feuillues et de connifères à faible diversité. Cependant, la présence de trois types d'habitats azonaux peut produire une haute diversité au niveau local: zones humides avec leur nombreux microhabitats, reliefs karstiques et leur profonds défilés fluviaux, et enfin des îles écologiques avec une végétation par ticulière situées près de la limite supérieure des arbres (treeline). Ces secteurs riches en espèces peuvent s'expliquer par l'interaction des facteurs physiques, biotiques et historiques. Dans ce domaine nous proposons un système anémo-orographique avec ses facteurs inféodés qui pourrait expliquer la haute diversité animale et végétale dans les cirques glaciaires des montagnes hercyniennes. -
Proxy Environmental Record from the Bohemian Forest, Czech Republic
bs_bs_banner The Lateglacial and Holocene in Central Europe: a multi-proxy environmental record from the Bohemian Forest, Czech Republic KLARA VOCADLOV A, LIBOR PETR, PAVLA ZA CKOV A, MAREK KRIZEK, LENKA KRIZOV A, SIMON M. HUTCHINSON AND MIROSLAV SOBR Vocadlova, K., Petr, L., Zackova, P., Krızek, M., Krızova, L., Hutchinson, S. M. & Sobr M.: The Lateglacial and Holocene in Central Europe: a multi-proxy environmental record from the Bohemian Forest, Czech Republic. Boreas. 10.1111/bor.12126. ISSN 0300-9483. The Hercynian mountain ranges were islands of mountain glaciation and alpine tundra in a Central European ice-free corridor during the Late Pleistocene. Today they are notable areas of glacial landforms, alpine-forest free areas, peatlands and woodlands. However, our knowledge of the Lateglacial and early Holocene environmental changes in this region is limited. We present a new multi-proxy reconstruction of a mid-altitude environment in the Bohemian Forest spanning this period. A core (5.2 m length) in the Cern e Lake cirque (1028 m a.s.l.) was sub- jected to lithological, geochemical, pollen and macrofossil analysis supplemented by two optically stimulated luminescence (OSL) and 10 AMS radiocarbon dates. We determined the impact of regional and supraregional cli- mate changes on the environment. The two most significant changes in sedimentation during the Lateglacial (17.6 and 15.8–15.5 cal. ka BP) were synchronous with regional glacial chronostratigraphy. Unlike Central European mountain ranges, in the Bohemian Forest the Younger Dryas was not coincident with glacier re-advance, but was a dry, cold episode with low lake levels, which prevailed until the early Preboreal. -
ICOMOS Advisory Process Was
Background A nomination under the title “Mining Cultural Landscape Erzgebirge/Krušnohoří Erzgebirge/Krušnohoří” was submitted by the States (Germany/Czechia) Parties in January 2014 for evaluation as a cultural landscape under criteria (i), (ii), (iii) and (iv). The No 1478 nomination dossier was withdrawn by the States Parties following the receipt of the interim report. At the request of the States Parties, an ICOMOS Advisory process was carried out in May-September 2016. Official name as proposed by the States Parties The previous nomination dossier consisted of a serial Erzgebirge/Krušnohoří Mining Region property of 85 components. ICOMOS noticed the different approaches used by both States Parties to identify the Location components and to determine their boundaries; in some Germany (DE), Free State of Saxony; Parts of the cases, an extreme atomization of heritage assets was administrative districts of Mittelsachsen, Erzgebirgskreis, noticed. This is a new, revised nomination that takes into Meißen, Sächsische Schweiz-Osterzgebirgeand Zwickau account the ICOMOS Advisory process recommendations. Czechia (CZ); Parts of the regions of Karlovy Vary (Karlovarskýkraj) and Ústí (Ústeckýkraj), districts of Consultations and technical evaluation mission Karlovy Vary, Teplice and Chomutov Desk reviews have been provided by ICOMOS International Scientific Committees, members and Brief description independent experts. Erzgebirge/Krušnohoří (Ore Mountains) is a mining region located in southeastern Germany (Saxony) and An ICOMOS technical evaluation mission visited the northwestern Czechia. The area, some 95 km long and property in June 2018. 45 km wide, is rich in a variety of metals, which gave place to mining practices from the Middle Ages onwards. In Additional information received by ICOMOS relation to those activities, mining towns were established, A letter was sent to the States Parties on 17 October 2018 together with water management systems, training requesting further information about development projects academies, factories and other structures. -
2.14 Mean Annual Climatic Water Balance
2.14 Mean Annual Climatic Water Balance The climatic water balance (CWB) is defined as the difference between precipitation depth Baltic Sea. The whole lowland regions of Mecklenburg-Vorpommern (Mecklenburg-Western and the depth of potential evapotranspiration at a given site during a certain time period. Pomerania), Brandenburg, Sachsen-Anhalt (Saxony-Anhalt), and Sachsen (Saxony) have negative summer half-year balances, with average values sometimes drastically below In general climatology, climate classifications are usually based on the weather elements “air - 100 mm. The highest deficits in the summer half-year show values below -300 mm. In sum- temperature” and “precipitation depth”, from which e. g. the description of the aridity of the mers with abundant rainfall, positive half-year balances may be recorded too, what was the climate is derived, the so-called aridity index. However, in the context of water-resources case in about one third of the years in the series 1961–1990. management and hydrology, the climatic water balance is better suitable for the hydroclimatic characterisation of sites, areas or periods, because the (hydro-)climatic conditions are The period with mean negative monthly balances in the inland lowlands lasts from April to described directly by means of the water-balance effective elements “precipitation” or “poten- September/October. The highest monthly balance deficits below -100 mm are recorded in the tial evapotranspiration” in the dimension “mm”. Dependent on whether precipitation depth or months from May to July. Negative monthly balances may occur throughout the year, potential evapotranspiration depth prevails in the considered period, the climatic water provided dry weather prevails. -
Sulphate Sorption Characteristics of the Bohemian Forest Soils
Silva Gabreta vol. 11 (1) p. 3–12 Vimperk, 2005 Sulphate sorption characteristics of the Bohemian Forest soils Jiří Kaňa* & Jiří Kopáček Faculty of Biological Sciences, University of South Bohemia, and Hydrobiological Institute, AS CR, Na Sádkách 7, CZ-37005 České Budějovice, Czech Republic *[email protected] Abstract Sulphate (SO4-S) sorption characteristics were determined in soils from catchments of three acidified mountain lakes, Plešné (PL), Čertovo (CT), and Černé (CN), situated in the Bohemian Forest. The SO4-S desorption ranged between 0.07–0.73, 0.21–0.68, and 0.39–0.82 mmol.kg–1 in the PL, CT, and CN catchments, respectively. SO4-S desorption was observed to be higher in horizon A than in mineral horizons below. The SO4-S represented only 3.4% of total S pool in the catchments and did not explain a relatively high rate of terrestrial leaching of sulphate over last 10 years. This disproportion suggests that the soil SO4-S pool is being replenished from internal soil processes from the pool of total S. Sulphate sorption maxima in soils in the catchments of the Bohemian Forest lakes varied between 1.5–11.7 mmol.kg–1, being highest in A-horizon and lowest in E-horizon. Key words: acidification, recovery, soil chemistry INTRODUCTION The chemistry (and, consequently, biology) of mountain lakes is determined by amount of precipitation and their composition, bedrock (PSENNER & CATALAN 1994), catchment soils and vegetation (e.g. BARON et al. 1994), and hydrology (WETZEL 2002). Soil sorption charac- teristics may significantly affect water composition, e.g. -
Vegetation of the Czech Republic: Diversity, Ecology, History and Dynamics
Preslia 84: 427–504, 2012 427 Vegetation of the Czech Republic: diversity, ecology, history and dynamics Vegetace České republiky: diverzita, ekologie, historie a dynamika Dedicated to the centenary of the Czech Botanical Society (1912–2012) Milan C h y t r ý Department of Botany and Zoology, Masaryk University, Kotlářská 2, CZ-611 37 Brno, Czech Republic, e-mail: [email protected] Chytrý M. (2012): Vegetation of the Czech Republic: diversity, ecology, history and dynamics. – Preslia 84: 427–504. This review summarizes basic information on the diversity of vegetation in the Czech Republic. It describes basic environmenal factors affecting vegetation, vegetation history since the last glacial, biomes occurring in the Czech Republic (zonal biomes of broad-leaved deciduous forest and forest- steppe, and azonal biomes of taiga and tundra), altitudinal zonation of vegetation and landscapes with an exceptionally high diversity of vegetation types (deep river valleys in the Bohemian Massif, karst areas, sandstone pseudokarst areas, solitary volcanic hills, glacial cirques, lowland riverine landscapes and serpentine areas). Vegetation types, delimited according to the monograph Vegeta- tion of the Czech Republic, are described with emphasis on their diversity, ecology, history and dynamics. K e y w o r d s: alpine, aquatic, central Europe, forest, grassland, phytosociology, plant communi- ties, ruderal, vegetation change, vegetation classification, vegetation history, weed, wetland Introduction The Czech Republic is a land-locked country in central Europe occupying an area of 78,867 km2. It is situated in the zone of temperate broad-leaved deciduous forest, which in the south-east borders on the forest-steppe zone. -
Benefits of Biodiversity Enrichment Due to Forest Conversion: Evidence from Two Choice Experiments in Germany
Benefits of Biodiversity Enrichment due to Forest Conversion: Evidence from two Choice Experiments in Germany Jürgen Meyerhoffa, Ulf Liebeb, Volkmar Hartje a a Institute for Landscape and Environmental Planning, Technische Universität Berlin b Universität Leipzig, Institute of Sociology Corresponding author: Jürgen Meyerhoff, Institute for Landscape and Environmental Planning, Technische Universität Berlin, EB 4-2, Strasse des 17. Juni 145, D – 10623 Berlin, Germany, [email protected] Abstract Forest biodiversity has recently received increasing attention because forest ecosystems are critically important habitats in terms of biological diversity. However, although many non-marketed non-timber products provided by forest ecosystems have been subject to non-market valuation studies, little is known about the economic value of forest biodiversity at present apart from the value of genetic information. This applies to both tropical and temperate forests. In order to determine the benefits from enriched forest biodiversity, we employed choice experiments in two regions in Lower Saxony, Germany. As they are attribute based, we expected to obtain more information about how people value changes in biodiversity compared to the contingent valuation but the choice experiments only provided limited information about this since we found no significant differences between several implicit prices. Calculating the welfare measures shows that including the alternative specific constant or not switches the measure from negative to positive and vice-versa. This is also the case when we exclude all the respondents who always chose the status quo option. JEL Classification: Q23; Q51; Q57 Keywords: Alternative specific constant, choice experiment, forest biodiversity, forest conversion, implicit price, welfare measure 1 Introduction Among the non-marketed non-timber products forests provide, biodiversity has recently received increasing attention. -
Late Cretaceous to Paleogene Exhumation in Central Europe – Localized Inversion Vs
https://doi.org/10.5194/se-2020-183 Preprint. Discussion started: 11 November 2020 c Author(s) 2020. CC BY 4.0 License. Late Cretaceous to Paleogene exhumation in Central Europe – localized inversion vs. large-scale domal uplift Hilmar von Eynatten1, Jonas Kley2, István Dunkl1, Veit-Enno Hoffmann1, Annemarie Simon1 1University of Göttingen, Geoscience Center, Department of Sedimentology and Environmental Geology, 5 Goldschmidtstrasse 3, 37077 Göttingen, Germany 2University of Göttingen, Geoscience Center, Department of Structural Geology and Geodynamics, Goldschmidtstrasse 3, 37077 Göttingen, Germany Correspondence to: Hilmar von Eynatten ([email protected]) Abstract. Large parts of Central Europe have experienced exhumation in Late Cretaceous to Paleogene time. Previous 10 studies mainly focused on thrusted basement uplifts to unravel magnitude, processes and timing of exhumation. This study provides, for the first time, a comprehensive thermochronological dataset from mostly Permo-Triassic strata exposed adjacent to and between the basement uplifts in central Germany, comprising an area of at least some 250-300 km across. Results of apatite fission track and (U-Th)/He analyses on >100 new samples reveal that (i) km-scale exhumation affected the entire region, (ii) thrusting of basement blocks like the Harz Mountains and the Thuringian Forest focused in the Late 15 Cretaceous (about 90-70 Ma) while superimposed domal uplift of central Germany is slightly younger (about 75-55 Ma), and (iii) large parts of the domal uplift experienced removal of 3 to 4 km of Mesozoic strata. Using spatial extent, magnitude and timing as constraints suggests that thrusting and crustal thickening alone can account for no more than half of the domal uplift. -
A New Basal Sphenacodontid Synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany
A new basal sphenacodontid synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany JÖRG FRÖBISCH, RAINER R. SCHOCH, JOHANNES MÜLLER, THOMAS SCHINDLER, and DIETER SCHWEISS Fröbisch, J., Schoch, R.R., Müller, J., Schindler, T., and Schweiss, D. 2011. A new basal sphenacodontid synapsid from the Late Carboniferous of the Saar−Nahe Basin, Germany. Acta Palaeontologica Polonica 56 (1): 113–120. A new basal sphenacodontid synapsid, represented by an anterior portion of a mandible, demonstrates for the first time the presence of amniotes in the largest European Permo−Carboniferous basin, the Saar−Nahe Basin. The new taxon, Cryptovenator hirschbergeri gen. et sp. nov., is autapomorphic in the extreme shortness and robustness of the lower jaw, with moderate heterodonty, including the absence of a greatly reduced first tooth and only a slight caniniform develop− ment of the second and third teeth. Cryptovenator shares with Dimetrodon, Sphenacodon, and Ctenospondylus, but nota− bly not with Secodontosaurus, enlarged canines and a characteristic teardrop outline of the marginal teeth in lateral view, possession of a deep symphyseal region, and a strongly concave dorsal margin of the dentary. The new find shows that sphenacodontids were present in the Saar−Nahe Basin by the latest Carboniferous, predating the record of sphenacodontid tracks from slightly younger sediments in this region. Key words: Synapsida, Sphenacodontidae, Carboniferous, Saar−Nahe Basin, Germany. Jörg Fröbisch [[email protected]], Department of Geology, The Field Museum, 1400 South Lake Shore Drive, Chicago, Illinois 60605, USA and [joerg.froebisch@mfn−berlin.de], Museum für Naturkunde Leibniz−Institut für Evolu− tions− und Biodiversitätsforschung an der Humboldt−Universität zu Berlin, Invalidenstr. -
Causes and Potential Solutions for Conflicts Between Protected Area Management and Local People in Germany
Causes and Potential Solutions for Conflicts between Protected Area Management and Local People in Germany Eick von Ruschkowski, Department of Environmental Planning, Leibniz University Han- nover, Herrenhäuser Strasse 2, 30419, Hannover, Germany; [email protected] hannover.de Introduction The designation of protected areas (e.g. national parks) often leads to conflicts between local communities and the area’s administration. This phenomenon exists worldwide (Pretty and Pimbert 1995) and is probably as old as the national park idea itself. These conflicts often affect both the protected areas and the local communities as strained relations bear the dan- ger of gridlock on park planning, conservation objectives or regional economic development. As national parks and surrounding communities are highly dependent on each other (Jarvis 2000), the task of managing stakeholder interests and potential use conflicts should be of high priority for park managers. National parks in Germany (as much of Central Europe’s protected areas) are often very vulnerable to such conflicts for a number of reasons. Their history is quite recent, with the oldest park having been established less than 40 years ago. On the other hand, the German landscape has been altered throughout many centuries, hence creating cultural landscapes, rather than unimpaired wilderness. Thus, the designation of national parks has caused con- flicts in the past, mainly along the lines of the continuation of traditional uses vs. future (non- )development, often additionally fuelled by management issues (local vs. state vs. federal). Additionally,a high population density puts protected areas more likely close to urban areas. Against this background, the management of stakeholder issues in order to increase support among local communities remains one of the most important sociological challenges for Ger- man park managers.