Bieszczady Earthworm Conference
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Nottingham Trent University Different Land Use Effect
NOTTINGHAM TRENT UNIVERSITY DIFFERENT LAND USE EFFECT ON EARTHWORMS AT SAFE PROJECT SITE IN SABAH, BORNEO by SRI VENKATESWARA RAO Dissertation submitted in partial fulfilment of the MSc. Endangered Species Recovery & Conservation 2013 Abstract Earthworms are a major component of the soil biota as ‘ecosystem engineers’ sensitive to disturbance and the impact of deforestation on earthworms remains as one the least studied subject in tropical Borneo whose rainforest is fast disappearing due to logging and intensive agriculture. As such, this study investigated the impact of land use disturbance on earthworms by comparing their abundance per m2 across forest modification gradient and measured changes in environmental variables across the gradient and their subsequent effect on earthworms. Old growth (OG2), secondary logged forest (B and F) and oil palm (OP2 and OP3) sites were surveyed in SAFE Project site in Sabah, Borneo. Transect and monolith digging methods were employed to sample earthworms from soil. At each monolith, environmental variables were measured to characterise each land use by canopy exposure, litter depth and forest quality and soil samples were taken to analyse soil properties. Earthworm abundance was highest in OG2 and decreased across the disturbance gradient and was significantly lower in OP2 indicating some level of tolerance between old growth and secondary forest system. However, functional group response and changes in functional group composition varied significantly between land uses and corresponded significantly to variation in environmental variables which also significantly differed between land uses. Changes in functional group response potentially show greater implication for soil function and the ecosystem services derived from the processes. -
Forest Structure and Land Use Change in the Bieszczady Mountains
Humboldt Universität zu Berlin Geographisches Institut Studienprojekt und Geländepraktikum Karpaten 2014 Veranstaltungsnummer 34042 Seminarleitung Tobias Kümmerle, Jan Knorn, Patrick Culbert Sommersemester 2014 Forest Structure and Land Use Change in the Bieszczady Mountains Projektarbeit als Modulabschlussprüfung (MAP) Abgabe 14. November 2014 Monobachelor Geographie, 6. Fachsemester Beifach Regionalstudien Asien/Afrika Studienprojekt und Geländepraktikum Karpaten 2014 – MAP Table of contents 1. Introduction ................................................................................................................................................ 4 2. Materials and Methods .............................................................................................................................. 5 2.1. Study area ........................................................................................................................................... 5 2.2. Forest classification ............................................................................................................................ 6 2.3. Sampling Design ................................................................................................................................. 6 2.4. Field Methods ..................................................................................................................................... 7 2.5. Data Analysis ..................................................................................................................................... -
Germania TEG1 8/2/2004 2:52 PM Page 16 TEG1 8/2/2004 2:52 PM Page 17
TEG1 8/2/2004 2:52 PM Page 15 Part I Germania TEG1 8/2/2004 2:52 PM Page 16 TEG1 8/2/2004 2:52 PM Page 17 1 Land and People The Land The heartland of the immense area of northern Europe occupied by the early Germanic peoples was the great expanse of lowland which extends from the Netherlands to western Russia. There are no heights here over 300 metres and most of the land rises no higher than 100 metres. But there is considerable variety in relief and soil conditions. Several areas, like the Lüneburg Heath and the hills of Schleswig-Holstein, are diverse in both relief and landscape. There was until recent times a good deal of marshy ground in the northern parts of the great plain, and a broad belt of coastal marshland girds it on its northern flank. Several major rivers drain the plain, the Ems, Weser and Elbe flowing into the North Sea, the Oder and the Vistula into the Baltic. Their broad valleys offered attrac- tive areas for early settlement, as well as corridors of communication from south to north. The surface deposits on the lowland largely result from successive periods of glaciation. A major influence on relief are the ground moraines, comprising a stiff boulder clay which produces gently undu- lating plains or a terrain of small, steep-sided hills and hollows, the latter often containing small lakes and marshes, as in the area around Berlin. Other features of the relief are the hills left behind by terminal glacial moraines, the sinuous lakes which are the remains of melt-water, and the embayments created by the sea intruding behind a moraine. -
The Transformation of the Natural Environment of The
/ !"# 27 THE TRANSFORMATION OF THE NATURAL ENVIRONMENT OF THE POLISH AND UKRAINIAN BIESZCZADY MOUNTAINS DUE TO TOURISM AND OTHER FORMS OF HUMAN PRESSURE Agnieszka Œwigost Institute of Urban Development, Krakow, Poland Abstract The area of Bieszczady Mountains is the cross-border zone characterized by a great diversity in both policies and a level of economic development between the Polish and Ukrainian part of the region. Therefore, it exhibits a significant variation in the degree, form and character of anthropopres- sure. The main aim of the study is to compare the intensity of transformation of Polish and Ukrainian parts of Bieszczady Mountains and indicate the anthropogenic conditions existing in both countries. Four villages of Bieszczady were analysed – Solina and Wetlina in Poland and Sianki and Volosjanka in Ukraine. The study, conducted using the point scoring evaluation method, showed large variations in the degree of anthropopressure in different localities. The area that has the lowest level of human impact is Po³onina Wetliñska while the largest one occurs in Solina. Wetlina, Sianki and Volosjanka have a similar level of transformation. Research areas located in the Polish part of Bieszczady are exposed to environmental changes primarily related to the development of tourism. In Ukraine, the pressure is observable due to unregulated water and sewage systems, a large accumulation of possessions with a traditional heating and highly developed railway network. Keywords: anthropopressure; tourism; Polish Bieszczady Mountains; Ukrainian Bieszczady Mountains Introduction rently, research in the field of anthropopressure includes also Contemporary transformations of the natural environment the less visible transformation of the environment caused for are the consequences of not only natural alterations but also instance by tourism development. -
POLAND: COUNTRY REPORT to the FAO INTERNATIONAL TECHNICAL CONFERENCE on PLANT GENETIC RESOURCES (Leipzig 1996)
POLAND: COUNTRY REPORT TO THE FAO INTERNATIONAL TECHNICAL CONFERENCE ON PLANT GENETIC RESOURCES (Leipzig 1996) Prepared by: Wieslaw Podyma Barbara Janik-Janiec Radzikow, June 1995 POLAND country report 2 Note by FAO This Country Report has been prepared by the national authorities in the context of the preparatory process for the FAO International Technical Conference on Plant Genetic Resources, Leipzig, Germany, 17-23 June 1996. The Report is being made available by FAO as requested by the International Technical Conference. However, the report is solely the responsibility of the national authorities. The information in this report has not been verified by FAO, and the opinions expressed do not necessarily represent the views or policy of FAO. The designations employed and the presentation of the material and maps in this document do not imply the expression of any option whatsoever on the part of the Food and Agriculture Organization of the United Nations concerning the legal status of any country, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. POLAND country report 3 Table of Contents CHAPTER 1 THE COUNTRY AND ITS AGRICULTURAL SECTOR 6 1.1 THE COUNTRY 6 1.2 AGRICULTURAL SECTOR IN POLAND 8 CHAPTER 2 INDIGENOUS PLANT GENETIC RESOURCES 12 2.1 FLORA OF POLAND 12 2.2 FOREST GENETIC RESOURCES 37 2.3 WILD AND CROPS-RELATED SPECIES 38 2.4 LANDRACES AND OLD CULTIVARS 40 CHAPTER 3 CONSERVATION ACTIVITIES 42 3.1 IN SITU PRESERVATION OF GENETIC RESOURCES 42 3.2 EX SITU COLLECTIONS 45 3.2.1 Sample -
Archaeological and Radiocarbon Dating of Alluvial Fans As an Indicator of Prehistoric Colonisation of the G£Ubczyce Plateau (Southwestern Poland)
GEOCHRONOMETRIA Vol. 23, pp 101-107, 2004 – Journal on Methods and Applications of Absolute Chronology ARCHAEOLOGICAL AND RADIOCARBON DATING OF ALLUVIAL FANS AS AN INDICATOR OF PREHISTORIC COLONISATION OF THE G£UBCZYCE PLATEAU (SOUTHWESTERN POLAND) EDYTA ZYGMUNT University of Silesia, Faculty of Earth Sciences, Department of Quaternary Palaeogeography and Palaeoecology, Bedzinska 60, 41-200 Sosnowiec, Poland (e-mail: [email protected]) Key wordswords: Abstract: The development of agriculture accelerated soil erosion processes and the deposi- LOESS G£UBCZYCE tion of erosion products in the form of alluvial fans at the mouths of dry or temporarily drained PLATEAU, PREHISTORIC valleys. The age of the alluvial fan in Borucin, in the Psina basin, has been established and the COLONISATION, FOREST stages of its formation have been reconstructed with the use of radiocarbon dating of the roof CLEARANCE, SOIL of peat underlying the mineral sediment of the fan. The fan started to form in the second part EROSION, ALLUVIAL of Suboreal period (3650 ± 70 BP). Maximum fan progradation occurred at the end of the FAN, ARCHAEOLOGICAL Period of Roman Influence when the area was settled by the agricultural Przeworsk cul- DATING, RADIOCARBON ture(1670 ± 70 BP). In the Early Middle Ages, silty clays eroded from cultivated slopes no DATING longer reached the outer fan zone, which points to a lower population density/less intensive agriculture in the area. The period of formation of the second fan under examination, located at the mouth of a side valley of the Odra, has been preliminarily determined on the basis of archaeological research. The progradation of this fan is probably related to the agricultural activity of the Lusitian Culture and forest clearances linked to the construction of a strong- hold (9th-7th century BC). -
PS T5 Druk Cyfrowy Ksiega 1.Indb 122 23.02.2017 11:25 C 3
PS T5_druk cyfrowy_ksiega 1.indb 122 23.02.2017 11:25 C 3 From a tribe to a state The archaeology of the early Middle Ages in the interior area between the Odra and Bug rivers – the so-called “tribal period” 124 Abstract 125 1. Introduction 130 2. The natural environment 132 3. The landscape of settlement 148 4. The economic landscape 153 5. The symbolic landscape 162 6. Conclusion 164 Bibliography PS T5_druk cyfrowy_ksiega 1.indb 123 23.02.2017 11:25 C 3 F©Ó° ¬ ѩ϶ª ÑÓ ¬ ²Ñ¬Ñª Abstract The present chapter is devoted to presenting the complexity of research issues related to the communities which inhabited Polish territory during the so-called tribal period (between the 7th and the middle of the 10th century AD). Despite long years of study, the most elementary questions remain unan- swered – as a result of the scarcity of material traces of the said communities and due to the changing nature of scholarly interest or the lack of enthusiasm for studying subjects beyond so-called tribal geography. The introduction presents the currently available data which may be used in the reconstruction of the natural en- vironment in the area in question, emphasizing the impact it may have had on the stability and structure of settlements. The following subchapter focuses on the forms of architec- ture and the often discussed issue of the possibly seasonal nature of the structures. A separate subsection discusses defensive structures which began to appear at the end of the period under analysis. It also takes note of the structural S³¬´Ó°Ï© MÓ;Ö¯ÏÓ®× dierences between the strongholds erected in south-eastern and in north-western regions of Polish territory, emphasiz- ing the ongoing discussion regarding the function of these structures, which indubitably went beyond strictly defensive purposes. -
Językowe Pogranicza Polszczyzny
Gwary Dziś – vol. 9 – 2017, s. 85–158 DOI 10.14746/gd.2017.9.7 ISSN 1898-9276 Leszek Bednarczuk Akademia Polonijna w Częstochowie [email protected]* Językowe pogranicza polszczyzny Abstrakt: WPROWADZENIE A. POGRANICZE PÓŁNOCNO-WSCHODNIE 0. UWAGI WSTĘPNE I. KALENDARIUM WIELKIEGO KSIĘSTWA LITEWSKIEGO (WKL) II. WSPÓLNOTA KOMUNIKATYWNA WKL III. JĘZYK LITEWSKI IV. JĘZYK BIAŁORUSKI V. PIŚMIENNICTWO POLSKIE NA ZIEMIACH WKL VI. CECHY WSPÓLNE PÓŁNOCNO-WSCHODNIEJ POLSZCZYZNY VII. ZRÓŻNICOWANIE TERYTORIALNE PÓŁNOCNO-WSCHODNIEJ POLSZCZYZNY 1.Wileńszczyzna, 2.Kowieńszczyzna, 3. Suwalszczyzna, 4. Podlasie – Grodzieńszczyzna, 5. Polesie, 6. Nowogródczyzna, 7. Mińsk – Bobrujsk, 8. Mohylew – Witebsk – Połock, 9. Smoleńsk, 10. Inflanty – Łotwa VIII.UWAGI KOŃCOWE B. POGRANICZE POŁUDNIOWO-WSCHODNIE 0. UWAGI WSTĘPNE I. KALENDARIUM KONTAKTÓW POLSKO-RUSKICH II. INNOWACJE JĘZYKA UKRAIŃSKIEGO 1.Nazwa Ukraina, Ukrainiec, 2. Związki językowe ukraińsko-białoruskie, 3. Dialekty ukraińskie a południowo-wschodnia polszczyzna III. PIŚMIENNICTWO POLSKIE NA ZIEMIACH RUSKICH RZECZYPOSPOLITEJ IV. CECHY WSPÓLNE POŁUDNIOWO-WSCHODNIEJ POLSZCZYZNY V. ZRÓŻNICOWANIE TERYTORIALNE POŁUDNIOWO-WSCHODNIEJ POLSZCZYZNY 1. Ruś Czerwona, 2. Wołyń, 3. Podole – Huculszczyzna, 4. Podnieprze, 5. Bukowina – Mołdawia VI. UWAGI KOŃCOWE C. POGRANICZE POŁUDNIOWE 0. UWGI WSTĘPNE I. DOLNY I GÓRNY ŚLĄSK II. CIESZYŃSKIE – JABŁONKOWSKIE – CZADECKIE III. MAŁOPOLSKA POŁUDNIOWA 1. Żywieckie – Orawa, 2. Podhale, 3. Spisz – Pieniny – Gorce, 4. Muszyna – Tylicz, 5. Sądecczyzna, * Na życzenie Autora podajemy adres mailowy Redakcji; podobnie na życzenie Autora abstrakt polski ma postać spisu treści. Redakcja uznała, że ułatwi to Czytelnikowi orientację w tym dość obszernym tekście. 86 LESZEK BEDNARCZUK 6. Podkarpacie IV. NAWIĄZANIA WSCHODNIOSŁOWACKIE V. UWAGI KOŃCOWE Bibliografia, Wykaz skrótów Słowa kluczowe: interferencja, kresy, pogranicza, peryferie, substrat Abstract: The border areas of the polish language. A. -
The Oksywie Culture on the Right-Bank Lower Vistula1
ISSN 1392-6748 The Oksywie Culture on the Right-Bank Lower Vistula1 Milena Teska The late 3rd and early 2nd centuries BC saw major research procedure adopted by the present author is cultural changes and transformations which brought best reflected in the arrangement of the monograph. about a change in the appearance of not only the lands Volume I comprises the textual body of the thesis, i.e. of modern Poland but also of the whole of central Eu- introductory remarks and the history and state of ar- rope. The changes were precipitated by the impact chaeological research on the right-bank lower Vistula coming from the societies of the La Tène culture that prior to 1945. grew in strength, both economically and politically Next, investigations carried out there after 1945 no doubt, at that time (Godłowski, 1977, s. 111–120; are discussed. The study includes a detailed catalogue Woźniak, 1970; 1986, s. 12–13). The arrival of goods of 44 sites (Fig.), forming the source basis of the the- of a Celtic character marks thus the inception of an sis. The catalogue presents artefacts from the 23 cem- intensive La Tène influence process – a far-reaching eteries (18 archival) and 21 settlements (8 archival) impact of Celt civilization – going far beyond the area of the Oksywie Culture. It also presents the sites that of their compact settlement. The impact, in combina- have been explored under the programme of the Ar- tion with the strong traditions of the local sub-stratum, chaeological Record of Poland (AZP) (7 in all) and the caused new cultural patterns, typical of the younger finds the context of which could not be determined. -
Pedigree of the Wilson Family N O P
Pedigree of the Wilson Family N O P Namur** . NOP-1 Pegonitissa . NOP-203 Namur** . NOP-6 Pelaez** . NOP-205 Nantes** . NOP-10 Pembridge . NOP-208 Naples** . NOP-13 Peninton . NOP-210 Naples*** . NOP-16 Penthievre**. NOP-212 Narbonne** . NOP-27 Peplesham . NOP-217 Navarre*** . NOP-30 Perche** . NOP-220 Navarre*** . NOP-40 Percy** . NOP-224 Neuchatel** . NOP-51 Percy** . NOP-236 Neufmarche** . NOP-55 Periton . NOP-244 Nevers**. NOP-66 Pershale . NOP-246 Nevil . NOP-68 Pettendorf* . NOP-248 Neville** . NOP-70 Peverel . NOP-251 Neville** . NOP-78 Peverel . NOP-253 Noel* . NOP-84 Peverel . NOP-255 Nordmark . NOP-89 Pichard . NOP-257 Normandy** . NOP-92 Picot . NOP-259 Northeim**. NOP-96 Picquigny . NOP-261 Northumberland/Northumbria** . NOP-100 Pierrepont . NOP-263 Norton . NOP-103 Pigot . NOP-266 Norwood** . NOP-105 Plaiz . NOP-268 Nottingham . NOP-112 Plantagenet*** . NOP-270 Noyers** . NOP-114 Plantagenet** . NOP-288 Nullenburg . NOP-117 Plessis . NOP-295 Nunwicke . NOP-119 Poland*** . NOP-297 Olafsdotter*** . NOP-121 Pole*** . NOP-356 Olofsdottir*** . NOP-142 Pollington . NOP-360 O’Neill*** . NOP-148 Polotsk** . NOP-363 Orleans*** . NOP-153 Ponthieu . NOP-366 Orreby . NOP-157 Porhoet** . NOP-368 Osborn . NOP-160 Port . NOP-372 Ostmark** . NOP-163 Port* . NOP-374 O’Toole*** . NOP-166 Portugal*** . NOP-376 Ovequiz . NOP-173 Poynings . NOP-387 Oviedo* . NOP-175 Prendergast** . NOP-390 Oxton . NOP-178 Prescott . NOP-394 Pamplona . NOP-180 Preuilly . NOP-396 Pantolph . NOP-183 Provence*** . NOP-398 Paris*** . NOP-185 Provence** . NOP-400 Paris** . NOP-187 Provence** . NOP-406 Pateshull . NOP-189 Purefoy/Purifoy . NOP-410 Paunton . NOP-191 Pusterthal . -
Ecological Functions of Earthworms in Soil
Ecological functions of earthworms in soil Walter S. Andriuzzi Thesis committee Promotors Prof. Dr L. Brussaard Professor of Soil Biology and Biological Soil Quality Wageningen University Prof. Dr T. Bolger Professor of Zoology University College Dublin, Republic of Ireland Co-promotors Dr O. Schmidt Senior Lecturer University College Dublin, Republic of Ireland Dr J.H. Faber Senior Researcher and Team leader Alterra Other members Prof. Dr W.H. van der Putten, Wageningen University Prof. Dr J. Filser, University of Bremen, Germany Dr V. Nuutinen, Agrifood Research Finland, Jokioinen, Finland Dr P. Murphy, University College Dublin, Republic of Ireland This research was conducted under the auspices of University College Dublin and the C. T. De Wit Graduate School for Production Ecology and Resource Conservation following a Co-Tutelle Agreement between University College Dublin and Wageningen University. Ecological functions of earthworms in soil Walter S. Andriuzzi Thesis submitted in fulfilment of the requirements for the degree of doctor at Wageningen University by the authority of the Rector Magnificus Prof. Dr A.P.J. Mol, in the presence of the Thesis Committee appointed by the Academic Board to be defended in public on Monday 31 August 2015 at 4 p.m. in the Aula. Walter S. Andriuzzi Ecological functions of earthworms in soil 154 pages. PhD thesis, Wageningen University, Wageningen, NL (2015) With references, with summary in English ISBN 978-94-6257-417-5 Abstract Earthworms are known to play an important role in soil structure and fertility, but there are still big knowledge gaps on the functional ecology of distinct earthworm species, on their own and in interaction with other species. -
The Settlements of the Przeworsk Culture in Hungary
ACTA ARCHAEOLOGICA CARPATHICA VOL. LIV (2019): 227–258 PL ISSN 0001-5229 DOI 10.4467/00015229AAC.19.013.11890 ESZTER SOÓS THE SETTLEMENTS OF THE PRZEWORSK CULTURE IN HUNGARY Abstract: In the last decade, the Hungarian research of settlements belonging to the Przeworsk culture, generally identified with the Germanic Vandals, yielded important new results. The aim of this paper is to summarize these latest results based on which it also discusses the extension of the settlement territory, the problems of relative chronology, the evolution of material culture as well as the relations of the above-mentioned Germanic ethnic group in the Roman Imperial Age1. Keywords: Przeworsk culture, Vandals, Roman imports, pottery, settlements, chronology, dating I. INTRODUCTION For a long time, remains of cremation burials were the only phenomena which Hungarian and international research brought into relation with the expansion of the Przeworsk culture in the Carpathian Basin (Bóna 1986, 63; Olędzki 1992; Godłowski 1993; Olędzki 1999; Olędzki 2001). Meanwhile, the identification of settlements encountered many difficulties. From the 1950s onwards, pottery finds recovered during probe excavations were related to certain ethnic groups based on their typology and decoration. As a result, hand-formed, coarse ware with plastic decoration was usually identified as Dacian, while most of the wheel-thrown pottery was defined as Celtic, and hand-formed fine polished ware as Germanic (Lamiová-Schmiedlová 1969; Végh 1964; 1985; 1989; 1999). Accordingly, a mixed Culture including Dacian, Celtic and Germanic ethnic elements was identified in the Early Roman Period (Lamiová-Schmiedlová 1969, 458-466; Olędzki 2014). From the 1960s, the idea of Illyrian, Celtic, Púchov and 1 The writing of this is paper was supported by the János Bolyai Researchers’ Grant of the Hungarian Academy of Sciences.