National and Landscape Parks, Nature Reserves
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Arts in Wild Felid Conservation Programmes in Poland and in the World
J Vet Res 63, 457-464, 2019 DOI:10.2478/jvetres-2019-0043 REVIEW ARTICLE ARTs in wild felid conservation programmes in Poland and in the world Joanna Kochan1, Wojciech Niżański2, Nei Moreira3, Zalmir Silvino Cubas4, Agnieszka Nowak1, Sylwia Prochowska2, Agnieszka Partyka2, Wiesława Młodawska1, Józef Skotnicki5 1Institute of Veterinary Science, University of Agriculture in Kraków, 30-059 Kraków, Poland 2Department of Reproduction and Clinic of Farm Animals, Wrocław University of Environmental and Life Sciences, 50-366 Wrocław, Poland 3Federal University of Paraná, Palotina, PR 85950-000, Brazil 4ITAIPU Binacional, Refúgio Biológico Bela Vista, Foz do Iguaçu, PR 85856-970, Brazil 5City Zoological Park and Garden in Kraków Charitable Foundation, 30-232 Kraków, Poland [email protected] Received: January 11, 2019 Accepted: July 2, 2019 Abstract With the exception of the domestic cat, all felid species (Felidae) are currently threatened with extinction in their natural habitat. To develop effective and optimal wild cat conservation programmes with assisted reproductive technology (ART) it is necessary to combine advances from different disciplines of science, starting from the biology of the species, through research into the population and habitat, assisted reproductive technologies, establishment of gene banks, developing bioinformatic systems, and ending with biodiversity and endangered species management. In the last few years knowledge of felid reproduction has expanded considerably thanks to comparative studies utilising the domestic cat as a research model for endangered wild cats. Basic reproductive techniques utilised in both domestic cat breeding and rescuing wild felid populations that are threatened with extinction include semen collection and cryopreservation, artificial insemination, oocyte collection, in vitro maturation, in vitro fertilisation, somatic cloning, and embryo transfer. -
The Šariš Transitional Zone, Revealing Interactions Between Pieniny
Swiss Journal of Geosciences (2018) 111:245–267 https://doi.org/10.1007/s00015-017-0297-9 (0123456789().,-volV)(0123456789().,-volV) The Sˇarisˇ Transitional Zone, revealing interactions between Pieniny Klippen Belt, Outer Carpathians and European platform Edyta Jurewicz1 Received: 4 January 2017 / Accepted: 21 December 2017 / Published online: 16 January 2018 Ó The Author(s) 2018. This article is an open access publication Abstract The Pieniny Klippen Belt (PKB) is a narrow structure delineating the boundary between the Central and Outer Carpathians. It is built of nappes stacked during the Cretaceous and Paleocene and then re-folded in the Miocene during the formation of the Outer Carpathian overthrusts. The internal structure of the PKB at the Polish/Slovakian border first formed during northward nappe thrusting processes, which were most intense at the turn of the Cretaceous to the Paleocene. A secondary factor is the change in strike of the PKB turning from W–E to WNW–ESE, associated with dextral strike-slip faulting in the Carpathian basement (North-European Platform). These NNW-SSE oriented strike-slip fault zones, broadly parallel to the Teisseyre-Tornquist Zone, are responsible for the segmentation of the down-going plate, which influenced the sub- duction and collision between the North-European Platform and the Central Carpathian Block. Among them, the most important role was played by the Krako´w—Myszko´w Fault Zone separating the Małopolska and Upper Silesian blocks in the Carpathian foreland. Shifts and interactions between the neighboring Pieniny and Outer Carpathian basins—during contemporaneous sedimentation and deformation—resulted in a difficult-to-define, transitional zone. -
Bulletin (Pdf)
VI International Pontecorvo Neutrino Physics School First (and Last) Bulletin of VI International Pontecorvo Neutrino Physics School (February 2015) The VI Pontecorvo Neutrino Physics School is organized by Joint Institute for Nuclear Research (Dubna, Russia), Comenius University (Bratislava, Slovakia), Czech Technical University (Prague, Czech Republic), and Charles University (Prague, Czech Republic). Organizing Committee: Chairman: V.A. Matveev (JINR), Scientific program: S.M. Bilenky (JINR), Vice-chairmen: I. Štekl (CTU Prague), F. Šimkovic (Comenius U.), A.G. Olshevskiy (JINR), Members: V.A. Bednyakov (JINR), R. Leitner (Charles U. Prague), V.B. Brudanin (JINR), E. Kolganova (JINR), Secretaries: O. Matyuukhina (JINR), D. Štefánik (Comenius U.) Logo of the school was prepared by Mikhail Bilenky (Vancouver). Welcome The VI Pontecorvo Neutrino Physics School will be held in Grand Hotel Bellevue, on foot of the beautiful High Tatra Mountains, Slovakia within a period August 27 – September 4, 2015. The program of the School will cover modern topics of neutrino physics including neutrino experiments, phenomenology and theory: Theory of neutrino mixing and masses Solar, atmospheric, reactor and geo neutrino experiments Direct neutrino mass measurements Neutrinoless double-beeta decay (theory and experiment) Sterile neutrinos Dark matter Leptogenesis and Baryoogenesis Neutrino cosmology and astronomy Statistics for nuclear and particle physics General information The VI International Pontecorvo Neutrino Physics School to be held in Grand Hotel Bellevue, High Taatra Mountains, Slovakia, August 27 - September 4, 2015, continues the tradition of Pontecorvo Neutrino Physics Schools, which were held in Dubna and Alushta in 1998, 2003, 2007, 2010 and 2012. The information about previous editions of the Pontecorvo Neutrino Physics Schools is available at webpage http://pontecorvosch.jinr.ru. -
Geodynamical Studies of the Pieniny Klippen Belt in 1994 – 2011
Geophysical Research Abstracts Vol. 14, EGU2012-2528, 2012 EGU General Assembly 2012 © Author(s) 2012 Geodynamical studies of the Pieniny Klippen Belt in 1994 – 2011 J Walo, A. Pachuta, D. Próchniewicz, T. Olszak, R. Szpunar, and M. Barlik Faculty of Geodesy and Cartography, Warsaw University of Technology, Poland ([email protected]) The Pieniny Klippen Belt (PKB), which is situated in Southern Poland, is one of the main fault zones on the boundary of the outer and inner Carpathians. The geodynamical investigations which have been carried out since 1960s indicate that PKB demonstrates neo-tectonic activity. In 1994, the GPS measurements were included in the horizontal network and this epoch was used as a reference epoch for the further studies. In 1995-2001, when the measurements were interrupted, the Dunajec river dam and the water reservoirs in Czorsztyn and Sromowce Wyzne˙ have been built. This has created a new aspect in investigations related to the effect of tectonic movements on the dam. Taking that into account, the study was revived and the geodynamical investigations, which contain GPS, relative gravimetric and leveling observations, have been carried out annually, at the beginning of September, from 2001. In 2008, also the absolute gravity measurements (using FG-5 gravimeter) at three stations located in PKB and adjacent geological structures were included in the study. In this paper the result of horizontal displacement in the PKB area obtained from GPS measurement as well as gravity changes obtained from relative and absolute measurements in 1994-2011 period are presented and yields linear trend of horizontal displacement in north-east direction less than 1 mm/year.. -
Early Stages of Structural Evolution of the Carpathian Klippen Belt (Slovakian Pieniny Sector)
Mineralia Slovaca, 44 (2012), 1 – 16 Web ISSN 1338-3523, ISSN 0369-2086 Early stages of structural evolution of the Carpathian Klippen Belt (Slovakian Pieniny sector) DUšan Plašienka Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University, Mlynská dolina, SK-842 5 Bratislava, Slovak Republic; [email protected] Abstract The Pieniny Klippen Belt (PKB) is a distinctive, suture-like tectonic zone that separates the External Carpathian Tertiary accretionary wedge (Flysch Belt) and the Cretaceous thrust stack of the Central Western Carpathians. Whereas the lithostratigraphy of various PKB units is fairly well-known, its tectonic evolution and development of the peculiar “klippen tectonic style” is a subject of very different opinions. We present structural data from the Pieniny sector of the PKB in NE Slovakia, which indicate that: ) distinction should be made between the “blocky” klippen and the “ribbon” klippen, since locally considerable reorientation of the original attitudes of structural elements is presumed for the former ones; 2) bedding poles of the “ribbon” klippen (Jurassic to Neocomian limestones and radiolarites) plot in a girdle in NWN–SES to N–S direction, while those of the klippen matrix (mid-Cretaceous to Lower Eocene marlstones, shales and sandstones) are shifted clockwise; 3) occasionally, the bedding-perpendicular cleavage and buckle folds record an early layer-parallel shortening, which are clearly older than brittle transpression-related faults and fractures – therefore they are interpreted as initial detachment and thrusting deformation elements that are likely related to the nappe-forming processes in the PKB; 4) fold axes, β-intersections of mesoscopic fold limb pairs, as well as a part of the bedding/ cleavage intersections are all oriented in the SW–NE direction (mean 55°), i.e. -
Traditional Rural Małopolska
Traditional Rural Małopolska Catalogue TRADITIONAL RURAL MAŁOPOLSKA Małopolska is a region with a rich historical and cultural, extraordinary natural and landscape values and traditional hospitality famous well out of Poland. The uniqueness and multiculturalism affirm the exceptional qualities of the region. The still vibrant folk culture is the strongest expression of the diversity of Małopolska, where each part has its own specific costumes, dialect, customs and traditions. The same folk culture also manifests itself in the architecture, rural buildings, interior design, farm equipment and regional dishes and products. The publication ‘Traditional Rural Małopolska’, which includes offers from 13 farms and agritourism facilities, is an invitation to come to the Małopolska countryside and learn about the most beautiful folk traditions and rituals that have been cultivated in Małopolska for centuries. Hosts of the facilities are enthusiastic, exceptional and open-minded people, who know and nurture the history and traditions of their ‘Little Homelands’, willingly spend their time with their guests, showing them local monuments, folklore and customs. We look forward to seeing you! FARMS PARTICIPATING IN THE PROGRAMME “TRADITIONAL RURAL MAŁOPOLSKA” 1 ”PSZCZÓŁKI” – Niezwojowice .................................................................................................................................................... 6-7 2 ”GOŚCINA u BABCI” – Zalipie ...................................................................................................................................................... -
XVIII INTERNATIONAL MYELOMA WORKSHOP KRAKÓW 2021, POLAND (Proposed Term 14 – 19.09.2021)
APPLICATION FOR ORGANIZATION OF: XVIII INTERNATIONAL MYELOMA WORKSHOP KRAKÓW 2021, POLAND (proposed term 14 – 19.09.2021) Local Congress Organizers MD PhD, Prof. Aleksander B. Skotnicki Head of the Chair and Departament of Hematology Jagiellonian University Collegium Medicum MD PhD, Assoc. Prof . Artur Jurczyszyn Ms. Agnieszka Grzesiak President of the Myeloma Treatment Fundation Centre JORDAN Congress Bureau Chairman of the Krakow Branch Polish Society of Haematology and Blood Transfusion Address: 22/2 Sobieskiego St, 31-136 Krakow Jagiellonian University Medical College Department of Hematology (PCO Professional Congress Organiser) Address: 17, Kopernika St, 31-501 Krakow Address: 22/2 Sobieskiego St, 31-136 Krakow T: + 48 601 53 90 77 T: + 48 341 46 40 , e-mail: [email protected] e-mail: [email protected], http://szpiczak.org/en/ http://kongres.jordan.pl/en International Myeloma Workshop 2021 1 Table of Contents: Kraków 2021 ? Yes, of course ! …………………………..pages 3-4 Traveling to Cracow…………………………..………………..page 5 Scientific Committee and Partners………………………pages 6-7 Congress Venue ICE …………………………………………….page 8 Hotels in Krakow …………………………………………………pages 9-10 Opening and Closing Ceremony…………………………..page 11 Exhibition Space ………………………………………………… pages 12-13 Welcome Reception…………………………………………… page 14 Gala Dinner……………………………………………………….. .pages 15-17 Social Programme……………………………………………….pages 18-22 General Information about Poland…………………….pages 23-25 International Myeloma Workshop 2021 2 Kraków 2021 ? Yes, of course ! KRAKÓW is the second largest and one of the oldest cities in Poland situated on the Vistula river in the south of Poland. For many years Krakow was the royal capital of Poland until 17 th c. Krakow - an architectural pearl amongst Polish cities on the UNESCO World Cultural Heritage list with its architectural complex of the Old City which has survived unchanged since the Middle Age It is still the city where, like ages ago, one can walk along the Royal Route , starting from the city gates and arriving at the Royal Castle Hill . -
E X C U R S I O N I a (19. IX. 1963) the Excursion Was Devoted to The
GUIDE TO THE GEOLOGICAL EXCURSIONS OF THE XXXVI ANNUAL MEETING OF THE GEOLOGICAL SOCIETY OF POLAND, PIEN17NY MOUNTAINS, 1963 by Krzysztof Birkenmajer, Kazimierz Bogacz, Stefan Kozłowski and Stanisław Węcławik Excursion I A (19. IX. 1963) The excursion was devoted to the hydrogeological, geochemical and balneotechnical (as well as balneotherapeutical) problems of mineral waters of Szczawnica. Excursion IB (19. IX. 1963) During the excursion were shown outcrops of andesite dykes of Mt. Bryjarka at Szczawnica, as well as Quaternary terraces of the Grajcarek stream valley. Excursion IC (19. IX. 1963) The members of the excursion visited a clay pit at Krościenko, which exposes Pliocene clays and’ gravels with abundant and well preserved plant remains (references: Szafer 1946-7, 1950, 1954; K l i m a s ze w- s k i 1948; Birkenma j e r 1954a, 1958a). Excursions II A (20. IX) and III A (21. IX. 1963) The programme of the excursions included outcrops of the Podhale — 413 — Palaeogene (flysch) near the southern contact of the Pieniny Klippen Belt at Szaflary, stratigraphy and tectonics of the Pieniny-, Branisko-, and Czorsztyn Series, as well as the problem of the relation of the Upper Senonian Mantle (Jarmuta Beds) to the Klippen Series between the villa ge Szaflary and the Szaflary quarry. Later on, at Krempachy, has been demonstrated a section of the Pieniny Klippen Belt including strongly disturbed tectonically klippes of the Czorsztyn Series, as well as Dogger-, Middle and Upper Cretaceous members of the northern zone of the Klippen Belt, referred now to the Magura Series. Similar problems were also discussed at Dursztyn, where -the excursion had finished. -
Neotectonics of the Polish Carpathians in the Light of Geomorphic Studies: a State of the Art
Acta Geodyn. Geomater., Vol. 6, No. 3 (155), 291-308, 2009 NEOTECTONICS OF THE POLISH CARPATHIANS IN THE LIGHT OF GEOMORPHIC STUDIES: A STATE OF THE ART Witold ZUCHIEWICZ Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, A. Mickiewicza 30, 30-059 Kraków, Poland *Corresponding author‘s e-mail: [email protected] (Received January 2009, accepted March 2009) ABSTRACT Neotectonics of the Carpathians used to be studied extensively, particular attention being paid to the effects of large-scale domal uplifts and open folding above marginal zones of thrusts and imbricated map-scale folds, and rarely to the characteristics of young faulting. Neotectonic faults tend to be associated with the margins of the Orava-Nowy Targ Basin, superposed on the boundary between the Inner and Outer Western Carpathians, as well as with some regions within the Outer Carpathians. The size of Quaternary tilting of the Tatra Mts. on the sub-Tatric fault were estimated at 100 to 300 m, and recent vertical crustal movements of this area detected by repeated precise levelling are in the range of 0.4-1.0 mm/yr in rate. Minor vertical block movements of oscillatory character (0.5-1 mm/yr) were detected along faults cutting the Pieniny Klippen Belt owing to repeated geodetic measurements performed on the Pieniny geodynamic test area. In the western part of the Western Outer Carpathians, middle and late Pleistocene reactivation of early Neogene thrust surfaces was suggested. Differentiated mobility of reactivated as normal Miocene faults (oriented (N-S to NNW-SSE and NNE-SSW) in the medial portion of the Dunajec River drainage basin appears to be indicated by the results of long-profile analyses of deformed straths, usually of early and middle Pleistocene age. -
The Species Composition on Agricultural Terraces in Nw Part of Slovakia
Ekológia (Bratislava) Vol. 33, No. 4, p. 307–320, 2014 doi:10.2478/eko-2014-0029 THE SPECIES COMPOSITION ON AGRICULTURAL TERRACES IN NW PART OF SLOVAKIA IVA MACHOVÁ, KAREL KUBÁT Jan Evangelista Purkyně University in Ústí nad Labem, Faculty of Environment, Králova výšina 7, 400 96 Ústí nad Labem, Czech Republic; e-mail: [email protected] Jan Evangelista Purkyně University in Ústí nad Labem, Faculty of Science, Za Válcovnou 8, 400 96 Ústí nad Labem, Czech Republic; e-mail: [email protected] Abstract Machová I., Kubát K.: The species composition on agricultural terraces in NW part of Slovakia. Ekológia (Bratislava), Vol. 33, No. 4, p. 307–320, 2014. The article contributes to a deeper understanding of agricultural terraces in NW Slovakia. The agri- cultural terraces found in 12 mountain ranges were characterised in detail on 32 localities. The slope parts of the studied terraces are on average only 2.3 m wide and current and former agricultural areas between them are on average 11 m wide. Furthermore, seventy phytosociological relevés were made on the terraces. Overall, 360 species of vascular plants were found in the relevés, 66 of which appeared regularly. The localities were evaluated by DCA analysis. The main factor influencing the species com- position appears to be the geological composition of the bedrock and, probably, the altitude as well. High coverage of the herb layer (median value 95%), low coverage of the shrub layer (median value 5%) and the absence or a very low coverage of the tree layer is typical for these terraces. Key words: NW Slovakia, agricultural terraces, vascular plants species, properties of the terraces. -
Green Bond Report on the Use of Proceeds Green Bond Report On The Use Of Proceeds
GREEN BOND REPORT ON THE USE OF PROCEEDS Poland’s 8-year EUR Green Bond maturing on August 7, 2026 February 2019 Contents Introduction Green Bond details Use of Proceeds Use of Proceeds in detail COP24 in Katowice Erratum to the Green Bond Report on the Use of Proceeds published in December 2017 2 Introduction In December 2016, the Republic of Poland issued its inaugural Green Bond, which, at the same time, was the first sovereign Green Bond in the history. That successful transaction was aimed at financing or refinancing environmen- tal expenditures and hence, fighting the climate change. Many times the Ministry of Finance’s officials stated that Poland wanted to be a repeat issuer on this innovative market. It stressed that it wanted to be an inherent part of a broader pro-environmental community. In response to that, in February 2018, Poland decided to issue Green Bonds for the second time. This time bigger transaction translated into even higher value of green projects to be financed. This report provides details for the Use of Proceeds of the second issuance. It also contains estimation of CO2 avoided as a result of expenditures on Renewa- ble Energy Sector from both Green Bond issues (issued in December 2016 and February 2018). PIOTR NOWAK, UNDERSECRETARY OF STATE, MINISTRY OF FINANCE ”After launching the first issue we focused on allocation of proceeds, but, as time went by, we started to think about the second issue of that type. For sure, we didn’t and still don’t want to be only an occasional issuer on this important market. -
Environmental Protection of the Gorce Mountains by The
ENVIRONMENTAL PROTECTION OF THE AND GORCE MOUNTAINS BY THE USE OF GEOTHERMAL ENERGY KRZAN National Park Zakopane. POLAND SOKOLOWSKI Polish Academy of Science Mineral and Energy Economy Research Centre, POLAND Key words: Doublet, Ecology, Air pollution, Defoliatian Tatra are an important center of popular and winter sports. The TNP research station coordinates 100 scientific programs annually, and the naturc museum presents natural values of the park. 1992 Tatra Park Poland one of most polluted countries. This became a MAB Biosphere et 1993). also applies to that of high touristic Podhale basin, where geothermal waters have Pieniny National Park discovered, is national parks. A large The total area of the park is 2328 of which 25% are scale ecological degradation is observed due to atmospheric pol- strictly nature reservation. 'The highest peak, lution some of which is due t o emissions from lo- crowns) is 982 Park is covered cal sources. Geothermal water fur and farmland. climatic zones encompass a moderately in settlements (Zakopane, Nowy Biaty Dunajec, w a r m zone cool zone There etc.) can beneficially influence state of are species of vascular planrs with many endemics and rare health of population and the environment in national parks l'he whole area is located in a low mountain forcst aonc, as well as area's numerous nature reservations. with a forest dominant. The very the park contains 45 specics of t70 species of birds, and numerous fauna Pieniny National is also an historical site. Tourist totaling 28 NATIONAL PARKS Canyon boat, well as many other tourist facilities make the park The southern part of Poland is a very popular lor visitors.