Invasive Alien Species
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Black Sea-Caspian Steppe: Natural Conditions 20 1.1 the Great Steppe
The Pechenegs: Nomads in the Political and Cultural Landscape of Medieval Europe East Central and Eastern Europe in the Middle Ages, 450–1450 General Editors Florin Curta and Dušan Zupka volume 74 The titles published in this series are listed at brill.com/ecee The Pechenegs: Nomads in the Political and Cultural Landscape of Medieval Europe By Aleksander Paroń Translated by Thomas Anessi LEIDEN | BOSTON This is an open access title distributed under the terms of the CC BY-NC-ND 4.0 license, which permits any non-commercial use, distribution, and reproduction in any medium, provided no alterations are made and the original author(s) and source are credited. Further information and the complete license text can be found at https://creativecommons.org/licenses/by-nc-nd/4.0/ The terms of the CC license apply only to the original material. The use of material from other sources (indicated by a reference) such as diagrams, illustrations, photos and text samples may require further permission from the respective copyright holder. Publication of the presented monograph has been subsidized by the Polish Ministry of Science and Higher Education within the National Programme for the Development of Humanities, Modul Universalia 2.1. Research grant no. 0046/NPRH/H21/84/2017. National Programme for the Development of Humanities Cover illustration: Pechenegs slaughter prince Sviatoslav Igorevich and his “Scythians”. The Madrid manuscript of the Synopsis of Histories by John Skylitzes. Miniature 445, 175r, top. From Wikimedia Commons, the free media repository. Proofreading by Philip E. Steele The Library of Congress Cataloging-in-Publication Data is available online at http://catalog.loc.gov LC record available at http://catalog.loc.gov/2021015848 Typeface for the Latin, Greek, and Cyrillic scripts: “Brill”. -
The North-Western Region of the Black Sea During the 6Th and Early 7Th Century Ad*
doi: 10.2143/AWE.7.0.2033257 AWE 7 (2008) 151-187 THE NORTH-WESTERN REGION OF THE BLACK SEA 151 THE NORTH-WESTERN REGION OF THE BLACK SEA DURING THE 6TH AND EARLY 7TH CENTURY AD* Florin CURTA Abstract Early Byzantine authors knew very little about the north-western region of the Black Sea. 6th- to 7th-century archaeological assemblages display a remarkable polarity of distribution. This has often been viewed as an indication of distinct ethnic groups (Slavs in the north and nomads in the south), but a closer examination of the archaeological record suggests a different interpretation. Burial assemblages in the steppe represent the funerary monuments of individuals of prominent status from communities living in settlements on the border between the steppe and the forest-steppe belts. ‘From the city of Cherson to the mouth of the Ister river, which is also called the Danube, is a journey of ten days, and barbarians hold that whole region’ (Procopius Wars 8. 5. 29). Procopius of Caesarea’s description of the Black Sea shore between the Crimea and the Danube delta, a part of his ‘account of the distribution of the peoples who live about the Euxine Sea’ (Wars 7. 1. 7), 1 underscores the limits of his knowledge. Because of barbarians holding that entire region, not much was known to him about what was going on north of the Danube delta and the region beyond that, because of barbarians holding that entire region.2 It is not at all clear just who were the barbarians controlling the north-western coast of the Black Sea, but those ‘still’ crossing the Danube during Procopius’ lifetime were the Cutrigurs, whom Procopius otherwise placed ‘on the western side of the Maeotic Lake’ (Wars 8. -
PRESERVING the DNIPRO RIVER Harmony, History and Rehabilitation PRESERVING the DNIPRO RIVER
PRESERVING THE DNIPRO RIVER harmony, history and rehabilitation PRESERVING THE DNIPRO RIVER harmony, history and rehabilitation International Dnipro Fund, Kiev, Ukraine, National Academy of Sciences of Ukraine, International Development Research Centre, Ottawa, Canada, National Research Institute of Environment and Resources of Ukraine PRESERVING THE DNIPRO RIVER harmony, history and rehabilitation Vasyl Yakovych Shevchuk Georgiy Oleksiyovich Bilyavsky Vasyl M ykolayovych Navrotsky Oleksandr Oleksandrovych Mazurkevich Library and Archives Canada Cataloguing in Publication Preserving the Dnipro River / V.Y. Schevchuk ... [et al.]. Includes bibliographical references and index. ISBN 0-88962-827-0 1. Water quality management--Dnieper River. 2. Dnieper River--Environmental conditions. I. Schevchuk, V. Y. QH77.U38P73 2004 333.91'62153'09477 C2004-906230-1 No part of this book may be reproduced or transmitted in any form, by any means, electronic or mechanical, including photocopying and recording, information storage and retrieval systems, without permission in writing from the publisher, except by a reviewer who may quote brief passages in a review. Publishing by Mosaic Press, offices and warehouse at 1252 Speers Rd., units 1 & 2, Oakville, On L6L 5N9, Canada and Mosaic Press, PMB 145, 4500 Witmer Industrial Estates, Niagara Falls, NY, 14305-1386, U.S.A. and International Development Research Centre PO Box 8500 Ottawa, ON K1G 3H9/Centre de recherches pour le développement international BP 8500 Ottawa, ON K1G 3H9 (pub@ idrc.ca / www.idrc.ca) -
Social Stratifi Cation of the Population of the Forest-Steppe Area Of
Sprawozdania Archeologiczne, 2017, 69, s. 133-183 SPRAWOZDANIA ARCHEOLOGICZNE 69, 2017 PL ISSN 0081-3834 DOI: 10.23858/SA69.2017.007 Marcin Burghardt* SOCIAL STRATIFICATION OF THE POPULATION OF THE FOREST-STEPPE AREA OF THE DNIEPERLAND IN THE EARLY SCYTHIAN PERIOD (VII – FIRST HALF OF VI CENT. BC) ABSTRACT Burghardt M. 2017. Social stratifi cation of the population of the forest-steppe area of the Dnieperland in the Early Scythian period (VII – fi rst half of VI cent. BC). Sprawozdania Archeologiczne 69, 133-183. The paper raises the question of the reconstruction of the social structure of the Early Scythian population of the forest-steppe area of the Dnieperland. In the course of analysis, it was established that the most important elements of funeral rites among the population related to this group, as well as based on ancient writers, are the size and the complexity of burial and mound construction, and the diversity of grave goods. The classifi cation of 197 burial complexes carried out in relation to the above-mentioned features, with the use of statistical inference methods, has led to separation of seven classes of graves, which may be combined within different social classes. The higher and the lower aristocracy, the ordinary population with the distinguishing class of warriors and the poorest population are numbered to these classes. The lowest place in the social hierarchy was represented by the people buried in the graves of representatives of upper classes. Key words: burials, social stratifi cation, Scythian archaeology, Early Scythian Culture, Early Iron Age, Forest- Steppe zone Received: 21.01.2017; Revised: 06.05.2017; Accepted: 12.06.2017 *Institute of Archaeology, Rzeszów University, Moniuszki st. -
The Morphological Characteristics of the Danube Ruffe, Gymnocephalus Baloni (Perciformes, Percidae), in the Upper Reaches of the Dnipro River, Ukraine
Vestnik zoologii, 51(1): 79–82, 2017 DOI 10.1515/vzoo-2017-0013 UDC 597.556.331.1:591.4(477) THE MORPHOLOGICAL CHARACTERISTICS OF THE DANUBE RUFFE, GYMNOCEPHALUS BALONI (PERCIFORMES, PERCIDAE), IN THE UPPER REACHES OF THE DNIPRO RIVER, UKRAINE A. O. Tsyba, S. V. Kokodiy Schmalhausen Institute of Zoology, NAS of Ukraine, vul. B. Khmelnytskogo, 15, Kyiv, 01030 Ukraine E-mail: [email protected]. 0955300107 Th e Morphological Characteristics of the Danube Ruff e, Gymnocephalus baloni (Perciformes, Percidae), in the Upper Reaches of the Dnipro River, Ukraine. Tsyba, A. O., Kokodiy, S. V. — In the upper reaches of the Dnipro it was found a Danube ruff e population. It diff ers from the population of the middle reaches of the Dnipro by a longer caudal peduncle. Th e Danube ruff e diff ers from sympatric populations of the common ruff e by 10 features. For a fast and precise identifi cation of these two species, it was proposed to use the height of the membrane between the fi rst and second rays of the anal fi n as a percentageto the length of the body. Key words: Pisces, Gymnocephalus baloni,Gymnocephalus cernuus, ruff e, morphology, Upper Dnipro. Introduction Th e Danube ruff e Gymnocephalus baloni Holciket Hensel, 1974 refers to the poorly studied species in Ukraine (Movchan, 2011) and is included in the Red Book of Ukraine under the “unrated” category (2009). Within Ukraine, it is known from the Lower Danube, the Middle Dnipro and its tributaries: Supij, Sula, Trubizh (Catalogue…, 2003). In the upper reaches of the Dnipro this species known only in its tributaries. -
Ukraine on the Implementation of the Convention on Biological Diversity
Sixth National Report of Ukraine on the Implementation of the Convention on Biological Diversity English version December, 2018 Kyiv – 2018 Contents Introduction .................................................................................................................................. 4 Acknowledgements........................................................................................................................ 4 Abbreviations ................................................................................................................................ 5 Section I. Information on the targets being pursued at the national level .................................. 7 National Target 1 (NT1). Increasing the level of public environmental consciousness ............................... 7 National Target 2 (NT 2). Improving the environmental situation and increasing the level of environmental security ......................................................................................................................... 8 National Target 3 (NT 3). Attaining the environmental conditions safe for human health ..........................10 National Target 4 (NT 4). Integrating the environmental policy and improving the integrated environmental management system ......................................................................................................... 11 National Target 5 (NT 5). Halting the loss of biological and landscape diversity and establishing the ecological network .........................................................................................................12 -
Steppe of Dnieper Ecological Corridor
Ukrainian Journal of Ecology Ukrainian Journal of Ecology, 2020, 10(2), 209-218, doi: 10.15421/2020_87 ORIGINAL ARTICLE UDC 502.13(282.247.32:23.071:477) A Study of the Emerald Network objects in Ukrainian Forest- Steppe of Dnieper Ecological Corridor І.V. Solomakha1, V.V. Konishchuk1, O.V. Mudrak*2, H.V. Mudrak3 1Institute of Agroecology and Environmental Management NAAS of Ukraine, 12 Metrolohichna St., Kyiv, 03143, Ukraine, 2 Vinnytsia Academy of Continuing Education, 13 Hrushevskyi St., Vinnytsia, 21050, Ukraine, 3Vinnytsia National Agrarian University, 3 Soniachna st., Vinnytsia, 21008, Ukraine *Corresponding author E-mail: [email protected] Received: 20.03.2020. Accepted: 21.04.2020 The national ecological network is being developed in Ukraine to create pan-European ecological network. The legislative framework is adopted, the network of nature reserve fund objects is expanded, and ecological corridors of national and regional significance are formed. The Dnieper Ecological Corridor is one of the largest ones in Ukraine and has trans-boundary significance. Thus, the priority task is to study flora, fauna, and natural habitats of the region in order to preserve and reproduce the rare components of biotic and landscape diversity. To fulfill these tasks, the Emerald Network was created. It includes territories of special nature conservation significance. The Emerald Network of Ukraine ensures conservation of the most valuable and typical components of landscape and biotic diversity, including habitats of rare and endangered animals and plants species. These areas include natural objects in the valley of the forest steppe part of Dnieper River basin, where there is a combination of reservoirs cascade with the remnants of the Dnieper flood plain and mouth areas. -
The Fluvial Archive of the Middle and Lower Dnieper (A Review)
Netherlands Journal of Geosciences / Geologie en Mijnbouw 81 (3-4): 339-355 (2002) The fluvial archive of the Middle and Lower Dnieper (a review) A.V. Matoshko1, P.F. Gozhik2 & A.S. Ivchenko3 1 Corresponding author, Institute of Geological Sciences, National Academy of Sciences of Ukraine, 55B Gonchara Street, 01054, Kiev. Ukraine. E-mail: [email protected] 2 P.F.Gozhik. Institute of Geological Sciences, National Academy of Sciences of Ukraine, 55B Gonchara Street, 01054, Kiev. Ukraine. E-mail: [email protected] 3 A.S.Ivchenko. Institute of Geography, National Academy of Sciences of Ukraine, 44, 3 Volodymyrska Street, 01034, Kiev. Ukraine. E-mail: [email protected] r ; Manuscript received: November 2000; accepted: January 2002 Abstract Information about the morphology and alluvial sediments of the Dnieper Valley is reviewed. The Dnieper Valley originated in the Late Miocene. The Middle Dnieper Valley is an intercontinental alluvial basin and the Lower Dnieper Valley is a shallow canyon that ends with a delta. Identification of the alluvial dynamic fades (channel, overbank, abandoned channel) is crucial for stratigraphical analysis. The dynamic fades form regular sequences - alluvial suites that combine into series. Individual suites and series are characterized by their mode of occurrence, fades composition, lithological features and expression in the modern landscape. Their stratigraphic position is established with reference to index beds and palaeontological, geochrono- logical and archaeological research, allowing them to be correlated along the valley. Correlation between different parts of the Dnieper system uses a combination of fades and geomorphological analyses, whereas correlation with other river systems makes use of mammalian and molluscan biostratigraphy. -
Climatic Changes in the Quaternary of Poland, Belarus and Ukraine
Geological Quarterly, 2004, 48 (2): 97–114 Main climatic changes in the Quaternary of Poland, Belarus and Ukraine Leszek LINDNER, Petro GOZHIK, Barbara MARCINIAK, Leszek MARKS and Yadviga YELOVICHEVA Lindner L., Gozhik P., Marciniak B., Marks L. and Yelovicheva Y. (2004) — Main climatic changes in the Quaternary of Poland, Belarus and Ukraine. Geol. Quart., 48 (2): 97–114. Warszawa. 26 units are described and correlated, representing the main climatic episodes during the Quaternary in Poland, Belarus and Ukraine. They comprise 13 cool and 13 warm intervals. The four oldest ones are Ró¿cian (Olkhovskian, Siver), Ponurzycian (Grushevskian, Beregovo), Otwockian (Vselubskian, Berezan) and Celestynovian (Yelenynskian, Kryzhaniv); these correspond to Praetiglian, Tiglian, Eburonian and Menapian, respectively of the Early Pleistocene in the Netherlands. In Poland this part of the Quaternary is named the Pre-Glacial or the Pre-Pleistocene. The Mid and Late Quaternary (the glacial epoch in Europe) comprises 11 glaciations or global coolings, namely the Narevian in Poland (Zhlobynskian, Ilyichivsk), the younger pre-Augustovian (Rogachevian 1/2, Shirokino 1/2), Augustovian 1/2 (Rogachevian 2/3, Shirokino 2/3), Nidanian (Narevian in Belarus, Pryazovsk), Sanian 1 (Servetskian, Sula), Ferdynandovian 1/2 (Belovezhian 1/2, Lubny 1/2), Sanian 2 (Berezinian, Tiligul), Liviecian (Orel), Krznanian (Dnieper 1), Odranian+Wartanian (Dnieperian+Sozhian, Dnieper 2 = Tyasmyn), Vistulian (Poozerian, Valday); and 10 interglacials or global warm- ings: early pre-Augustovian (Rogachevian 1, Shirokino 1), Augustovian 1 (Rogachevian 2, Shirokino 2), Augustovian 2 (Rogachevian 3, Shirokino 3), Ma³opolanian (Korchevian, Martonosha), Ferdynandovian 1 (Belovezhian 1, Lubny 1), Ferdynandovian 2 (Belovezhian 2, Lubny 2), Mazovian (Alexandrian, Zavadivka), Zbójnian (Smolenskian, Potagaylivka), Lubavian (Shklovian, Kaydaky), Eemian (Muravian, Pryluky) and Holocene. -
The Assessment Ofukrainian Riverbed Deformation
Sediment Transfer through the Fluvial System (Proceedings of a symposium held in Moscow, August 2004). IAHS Publ. 288, 2004 253 The assessment of Ukrainian riverbed deformation ALEXANDR G. OBODOVSKY Geographical Faculty, Kyiv National Taras Shevchenko University, Vladimirska St., 64 Kyiv-33, 01033, Ukraine [email protected] Abstract Two types of riverbed deformation (vertical and horizontal) were assessed for Ukrainian rivers. In zones of mixed forests and forest-steppe, vertical deforma tion was manifested in the form of a decrease in water levels, with associated washing out of the riverbed. For rivers of steppe zone and some rivers of forest steppe, vertical deformation was manifested in the accumulation of alluvium due to increasing water level. Freely meandering rivers are characterized by intensive hori zontal deformation in the zone of mixed forests. The least horizontal deformation is observed for in-cut riverbeds. Criteria are provided which allow for the assessment of both vertical and horizontal deformation types. Key words activity of rivers; criteria correction; riverbed deformation types; riverbed formation; Ukrainian rivers INTRODUCTION Riverbed deformation reflects space and time dynamics of riverbed processes. It is one of the components in the structure of hydroecological analysis (Obodovsky, 2001). River deforma tion varies in direction (vertical and horizontal) and rate as influenced by various human and natural factors. Riverbed deformation develops freely, if soil resistance towards washing out is not significant. It was observed that rivers with soil beds and banks are easily erodable. In the Ukraine, such rivers are located in the territory of Polessie, Pridneprovska (Dnipro) and Prichemomorska (Black Sea) lowlands. -
18165 Spatial Correlation Function of the Mean Annual Water Runoff of the River of Ukraine
18165 Spatial correlation function of the mean annual water runoff of the river of Ukraine *S. O. Moskalenko (Taras Shevchenko National University of Kyiv, Ukraine), L. V. Malytska (Ukrainian hydrometeorological institute, Kyiv, Ukraine) SUMMARY The purpose of the study is to calculate the spatial correlation function of the average annual water runoff for the territory of Ukraine according to the data on average annual water flow for medium and large river basins. The spatial correlation function is the coefficients of paired correlation between river water runoff depending on the distances between the centers of gravity of their river basins. Mathematical statistics, statistical analysis of the relationships between hydrological variables, and GIS technologies were used to construct the spatial correlation function. It is concluded that in the range of distances between the centers of gravity of river basins (from 88.6 to 1040 kilometers) there is a positive correlation between the runoff of the studied rivers (from -0.05 to 0.88). Correlation coefficients with increasing distance between river basin centers are killing. A satisfactory correlation (at = 0.60-0.70) between the average annual river water runoff for the plain territories of Ukraine has observed at a distance between the centers of the basins 180-300 km, for the mountain areas - at a distance of 20-80 km. Geoinformatics 2020 11-14 May 2020, Kyiv, Ukraine Introduction The solution of the problems of spatial interpolation of hydro-meteorological characteristics and optimization (rationalization) of a meteorological or hydrological observation network is based on the use of the spatial correlation function of an element of the investigated hydro-meteorological regime. -
Olexandr ZHYLKA*
ACTA ICHTHYOLOGICA ET PISCATORIA (2008) 38 (1): 45–46 DOI: 10.3750/AIP2008.38.1.07 BIOLOGICAL DATA ON THE DANUBE RUFFE, GYMNOCEPHALUS BALONI HOLČÍK ET HENSEL, 1974, IN THE DESNA RIVER, UKRAINE Olexandr ZHYLKA * Gogol State Nizhyn University, Department of Zoology, Nizhyn, Ukraine Zhylka O. 2008. Biological data on the Danube ruffe, Gymnocephalus baloni Holčík et Hensel, 1974, in the Desna River, Ukraine. Acta Ichthyol. Piscat. 38 (1): 45–46. Abstract. The Danube ruffe, Gymnocephalus baloni Holčík et Hensel, 1974, is a little-known species from the middle and lower Danube River. The relevant information on its habitat, maturity, fecundity, spawning season, maximum size and age, as well as its growth and length–weight relation are provided herewith from the Desna River, Ukraine. The estimation of fecundity ranged from 5072 to 15 730 eggs within the length range of 8.6 to 10.4 cm SL and the gonado-somatic index was 0.12–0.14 respectively. The length–weight relation was deter - mined as W = 0.0345SL 2.83 . Keywords: Danube ruffe, Desna River, Ukraine, length–weight relation, fecundity, gonado-somatic index The Danube ruffe, Gymnocephalus baloni is a little- In the Desna River, G. baloni inhabits relatively deep- known species described from the middle and lower water areas (2–5 m) of the littoral zone. Usually it occurs Danube River by Holčík et Hensel (1974). In Ukraine it near rocky shores with hollows, near submerged tree inhabits the Dnepr River and the middle and lower cours - boles and trunks. It prefers clay- or muddy bottom with es of its tributaries such as the Desna, the Trubizh, the some grass stem or tree rods on its surface.