The Balkans and the Colonization of Europe
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Fresh- and Brackish-Water Cold-Tolerant Species of Southern Europe: Migrants from the Paratethys That Colonized the Arctic
water Review Fresh- and Brackish-Water Cold-Tolerant Species of Southern Europe: Migrants from the Paratethys That Colonized the Arctic Valentina S. Artamonova 1, Ivan N. Bolotov 2,3,4, Maxim V. Vinarski 4 and Alexander A. Makhrov 1,4,* 1 A. N. Severtzov Institute of Ecology and Evolution, Russian Academy of Sciences, 119071 Moscow, Russia; [email protected] 2 Laboratory of Molecular Ecology and Phylogenetics, Northern Arctic Federal University, 163002 Arkhangelsk, Russia; [email protected] 3 Federal Center for Integrated Arctic Research, Russian Academy of Sciences, 163000 Arkhangelsk, Russia 4 Laboratory of Macroecology & Biogeography of Invertebrates, Saint Petersburg State University, 199034 Saint Petersburg, Russia; [email protected] * Correspondence: [email protected] Abstract: Analysis of zoogeographic, paleogeographic, and molecular data has shown that the ancestors of many fresh- and brackish-water cold-tolerant hydrobionts of the Mediterranean region and the Danube River basin likely originated in East Asia or Central Asia. The fish genera Gasterosteus, Hucho, Oxynoemacheilus, Salmo, and Schizothorax are examples of these groups among vertebrates, and the genera Magnibursatus (Trematoda), Margaritifera, Potomida, Microcondylaea, Leguminaia, Unio (Mollusca), and Phagocata (Planaria), among invertebrates. There is reason to believe that their ancestors spread to Europe through the Paratethys (or the proto-Paratethys basin that preceded it), where intense speciation took place and new genera of aquatic organisms arose. Some of the forms that originated in the Paratethys colonized the Mediterranean, and overwhelming data indicate that Citation: Artamonova, V.S.; Bolotov, representatives of the genera Salmo, Caspiomyzon, and Ecrobia migrated during the Miocene from I.N.; Vinarski, M.V.; Makhrov, A.A. -
Past and Current Trends of Balkan Migrations
ESPACE, POPULATIONS, SOCIETES, 2004-3 pp. 519-531 Corrado BONIFAZI Istituto di Ricerche sulla Popolazione e le Politiche Marija MAMOLO Sociali IRPPS via Nizza, 128 Roma Italie [email protected] Past and Current Trends of Balkan Migrations INTRODUCTION There is hardly another region of the world aspects of the Balkans [Prévélakis, 1994], where the current situation of migrations is affecting their specific nature also with still considerably influenced by the past his- regard to migration. However, the migration tory as in the Balkans. Migrations have been outlook of the Balkans does not just involve a fundamental element in the history of the these flows, which in some respects tend to Balkans, accompanying its stormy events reflect the movements de l’histoire de [Her√ak and Mesi´c, 1990] and obviously longue durée, but it is rather much more continuing to do so, even at the start of the structured and complex. Focusing for the new millennium. For centuries, invasions, moment on the most recent period, together wars, military defeats and victories have with the forced migrations caused by the been a more or less direct cause of popula- ethnic conflicts in the former Yugoslavia tion movements, in a continuous and still and the ethnic migrations followed by the ongoing transformation of the distribution collapse of the regimes created by “real and the overlapping of religions, languages, socialism”, we find both forms of labour ethnic groups and cultures [Sardon, 2001]. migration and transit migration. Therefore, Since the arrival of the Slav populations in the Balkans are also characterised by many the 7th century, the Ottoman expansion, the of the typical elements of the current forms extension of the Hapsburg domain, the rise of mobility in Eastern and Central Europe and growth of national states, the two World [Okólski, 1998; Bonifazi, 2003]. -
The Europeans Shores of the Bosporus Anca Dan
The Europeans Shores of the Bosporus Anca Dan To cite this version: Anca Dan. The Europeans Shores of the Bosporus. I∆ΥMAMEIZOOΣ EΛΛHIΣMOΥ. Eγκυκλoπαιδϵια Mϵιζoνo& Eλληνισµoυ, K!νσταντινoυπoλη, 2008. hal-02435580 HAL Id: hal-02435580 https://hal.archives-ouvertes.fr/hal-02435580 Submitted on 15 Jan 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. IΔΡΥΜA ΜΕΙΖΟΝΟΣ ΕΛΛΗΝΙΣΜΟΥ Συγγραφή : Dan Anca (30/9/2008) Για παραπομπή : Dan Anca , "European shores of the Bosporus", 2008, Εγκυκλοπαίδεια Μείζονος Ελληνισμού, Κωνσταντινούπολη URL: <http://www.ehw.gr/l.aspx?id=10951> European shores of the Bosporus Περίληψη : The “Thracian”or “Mysian”Bosporus separates the continents of Europe and Asia and the waters of the Black Sea from the Sea of Marmara. Its names distinguish it from the ancient Cimmerian Bosporus (Βόσπορος Κιμμέριος), which separates the modern Black Sea (ancient Pontus Euxinus, Πόντος ὁ Εὔξεινος) from the modern Sea of Azov (ancient Palus Maeotis, Μαιῶτις λίμνη) and corresponds to the modern Russian Kertch. Άλλες Ονομασίες Thracian Bosporus; Mysian Bosporus; ancient Greek Βόσπορος Θρακικὸς; Latin Bosphorus Thracicus 1. Anthropogeography 1a. Geographical location Bosporus is generally considered as the narrowest natural strait continuously used for navigation since Antiquity. -
Modeling of the Turkish Strait System Using a High Resolution Unstructured Grid Ocean Circulation Model
Journal of Marine Science and Engineering Article Modeling of the Turkish Strait System Using a High Resolution Unstructured Grid Ocean Circulation Model Mehmet Ilicak 1,* , Ivan Federico 2 , Ivano Barletta 2,3 , Sabri Mutlu 4 , Haldun Karan 4 , Stefania Angela Ciliberti 2 , Emanuela Clementi 5 , Giovanni Coppini 2 and Nadia Pinardi 3 1 Eurasia Institute of Earth Sciences, Istanbul Technical University, Istanbul 34469, Turkey 2 Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici, Ocean Predictions and Applications Division, 73100 Lecce, Italy; [email protected] (I.F.); [email protected] (I.B.); [email protected] (S.A.C.); [email protected] (G.C.) 3 Department of Physics and Astronomy, Universita di Bologna Alma Mater Studiorum, 40126 Bologna, Italy; [email protected] 4 TUBITAK MRC Environment and Cleaner Production Institute, Kocaeli 41470, Turkey; [email protected] (S.M.); [email protected] (H.K.) 5 Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici, Ocean Modeling and Data Assimilation Division, 40126 Bologna, Italy; [email protected] * Correspondence: [email protected] Abstract: The Turkish Strait System, which is the only connection between the Black Sea and the Mediterranean Sea, is a challenging region for ocean circulation models due to topographic constraints and water mass structure. We present a newly developed high resolution unstructured finite element grid model to simulate the Turkish Strait System using realistic atmospheric forcing and lateral open boundary conditions. We find that the jet flowing from the Bosphorus Strait into the Marmara creates Citation: Ilicak, M.; Federico, I.; an anticyclonic circulation. The eddy kinetic energy field is high around the jets exiting from the Barletta, I.; Mutlu, S.; Karan, H.; Ciliberti, S.A.; Clementi, E.; Coppini, Bosphorus Strait, Dardanelles Strait, and also the leeward side of the islands in the Marmara Sea. -
Chapter 2 GEOGRAPHY of the BOSPORUS, SEA of MARMARA, and DARDANELLES and the SURROUNDING REGION
Table of Contents THE TURKISH STRAITS BOSPORUS - SEA OF MARMARA - DARDANELLES Chapter 1 INTRODUCTION Chapter 2 GEOGRAPHY OF THE BOSPORUS, SEA OF MARMARA, AND DARDANELLES AND THE SURROUNDING REGION Historical geography Economic geography Cultural geography Chapter 3 GEOLOGY Physiography Black sea Bosporus Submarine sills and canyons Golden horn Sea of Marmara Izmit Bay Cekmece Lakes Dardanelles Submarine sills and canyons Aegean Sea Izmir Bay Regional Lithology Structure Seismicity Marine Sediments Distribution of grain size Age Mineralogy Life Historical geology Chapter 4 CLIMATE Black Sea Sea of Marmara Aegean Sea Eastern Mediterranean Regional Contents (continued) Chapter 5 HYDROLOGY Precipitation Runoff Chapter 6 PHYSICAL OCEANOGRAPHY Western Black Sea Distribution of properties Sea level Surface currents Bosporus Distribution of properties Temperature Salinity Density Sea level Waves Tides Seiche Surface currents Normal Vortices Reversals Two-layer flow system Normal Effects upon sedimentation Internal waves Hydraulic geometry Stirring and mixing Golden Horn Distribution of properties Sea level Surface currents Two—layer flow system Sea of Marmara Distribution of properties Sea level Surface currents Two-layer flow system Contents (continued) Chapter 6 (concluded) Izmit Bay Distribution of properties Cekmece Lakes Distribution of properties Dardanelles Distribution of properties Surface currents Two-layer flow system Aegean (including Izmir Bay) Distribution of properties Sea level Surface currents Regional Chapter 7 CHEMICAL AND -
The Waterway of Hellespont and Bosporus: the Origin of the Names and Early Greek Haplology
The Waterway of Hellespont and Bosporus: the Origin of the Names and Early Greek Haplology Dedicated to Henry and Renee Kahane* DEMETRIUS J. GEORGACAS ABBREVIATIONS AND BIBLIOGRAPHY 1. A few abbreviations are listed: AJA = American Journal of Archaeology. AJP = American Journal of Philology (The Johns Hopkins Press, Baltimore, Md.). BB = Bezzenbergers Beitriige zur Kunde der indogermanischen Sprachen. BNF = Beitriige zur Namenforschung (Heidelberg). OGL = Oorpus Glossariorum Latinorum, ed. G. Goetz. 7 vols. Lipsiae, 1888-1903. Chantraine, Dict. etym. = P. Chantraine, Dictionnaire etymologique de la langue grecque. Histoire des mots. 2 vols: A-K. Paris, 1968, 1970. Eberts RLV = M. Ebert (ed.), Reallexikon der Vorgeschichte. 16 vols. Berlin, 1924-32. EBr = Encyclopaedia Britannica. 30 vols. Chicago, 1970. EEBE = 'E:rccr'YJel~ t:ET:ateeta~ Bv~avnvwv E:rcovowv (Athens). EEC/JE = 'E:rcuJT'YJfhOVtUn ' E:rccrrJel~ C/JtAOaocptufj~ EXOAfj~ EIsl = The Encyclopaedia of Islam (Leiden and London) 1 (1960)-. Frisk, GEJV = H. Frisk, Griechisches etymologisches Worterbuch. 2 vols. Heidelberg, 1954 to 1970. GEL = Liddell-Scott-Jones, A Greek-English Lexicon. Oxford, 1925-40. A Supplement, 1968. GaM = Geographi Graeci Minores, ed. C. Miiller. GLM = Geographi Latini Minores, ed. A. Riese. GR = Geographical Review (New York). GZ = Geographische Zeitschrift (Berlin). IF = Indogermanische Forschungen (Berlin). 10 = Inscriptiones Graecae (Berlin). LB = Linguistique Balkanique (Sofia). * A summary of this paper was read at the meeting of the Linguistic Circle of Manitoba and North Dakota on 24 October 1970. My thanks go to Prof. Edmund Berry of the Univ. of Manitoba for reading a draft of the present study and for stylistic and other suggestions, and to the Editor of Names, Dr. -
1 the Turks and Europe by Gaston Gaillard London: Thomas Murby & Co
THE TURKS AND EUROPE BY GASTON GAILLARD LONDON: THOMAS MURBY & CO. 1 FLEET LANE, E.C. 1921 1 vi CONTENTS PAGES VI. THE TREATY WITH TURKEY: Mustafa Kemal’s Protest—Protests of Ahmed Riza and Galib Kemaly— Protest of the Indian Caliphate Delegation—Survey of the Treaty—The Turkish Press and the Treaty—Jafar Tayar at Adrianople—Operations of the Government Forces against the Nationalists—French Armistice in Cilicia—Mustafa Kemal’s Operations—Greek Operations in Asia Minor— The Ottoman Delegation’s Observations at the Peace Conference—The Allies’ Answer—Greek Operations in Thrace—The Ottoman Government decides to sign the Treaty—Italo-Greek Incident, and Protests of Armenia, Yugo-Slavia, and King Hussein—Signature of the Treaty – 169—271 VII. THE DISMEMBERMENT OF THE OTTOMAN EMPIRE: 1. The Turco-Armenian Question - 274—304 2. The Pan-Turanian and Pan-Arabian Movements: Origin of Pan-Turanism—The Turks and the Arabs—The Hejaz—The Emir Feisal—The Question of Syria—French Operations in Syria— Restoration of Greater Lebanon—The Arabian World and the Caliphate—The Part played by Islam - 304—356 VIII. THE MOSLEMS OF THE FORMER RUSSIAN EMPIRE AND TURKEY: The Republic of Northern Caucasus—Georgia and Azerbaïjan—The Bolshevists in the Republics of Caucasus and of the Transcaspian Isthmus—Armenians and Moslems - 357—369 IX. TURKEY AND THE SLAVS: Slavs versus Turks—Constantinople and Russia - 370—408 2 THE TURKS AND EUROPE I THE TURKS The peoples who speak the various Turkish dialects and who bear the generic name of Turcomans, or Turco-Tatars, are distributed over huge territories occupying nearly half of Asia and an important part of Eastern Europe. -
Autumn Migration of Soaring Birds at Bosporus: 5 Validating a New Survey Station Design
View metadata,TBIS907236 citation and similar papers at core.ac.uk Techset Composition India (P) Ltd., Bangalore and Chennai, Indiabrought 4/2/2014 to you by CORE provided by University of Debrecen Electronic Archive Bird Study (2014), 1–7 http://dx.doi.org/10.1080/00063657.2014.907236 SHORT REPORT Autumn migration of soaring birds at Bosporus: 5 validating a new survey station design ATTILA FÜLÖP1,2*, ISTVÁN KOVÁCS1, EMANUEL BALTAG1,3, SZILÁRD J. DARÓCZI1, ANDREEA S. DEHELEAN1, LUCA A. DEHELEAN1, RÉKA B. KISS1, ISTVÁN S. KOMÁROMI1, HANA LATKOVÁ1, 10 TAMÁS MIHOLCSA1, ATTILA NAGY1, SZILÁRD Z. ÖLVEDI1, TAMÁS PAPP1, ATTILA K. SÁNDOR1, RÓBERT ZEITZ1 AND MÁRTON A. KELEMEN1 1‘Milvus Group’–Bird and Nature Protection Association, Crinului street 22, Târgu Mureş RO-540620, Romania; 2MTA-DE ‘Lendület’ Behavioural Ecology Research Group, Department of Evolutionary Zoology and Human Biology, University of Debrecen, Egyetem tér 1, Debrecen H-4032, Hungary; 3Department of Zoology, Faculty of 15 Biology, ‘Al. I. Cuza’ University, B-dul Carol I 20A, Iasi̦ RO-700505, Romania Capsule Using a new survey station network we report the highest number of migrating raptors and Black Storks ever recorded on Bosporus during the autumn migration period. Also, we show that migration occurs 20 with similar intensities over the full length of the strait, but individual migration patterns differ for some species at a local scale. 25 Migration is an annual seasonal movement between development of thermals and (2) natural barriers (e.g. regular breeding and wintering grounds, covering large seas, deserts, ice fields or mountains) can be avoided or geographical distances over continents, caused passed with minimum risk (Elkins 2004, Newton primarily by seasonal changes in food abundance 2008). -
FIGURE 8.1 I EUROPE Stretching from Iceland in the Atlantic to The
FIGURE 8.1 I EUROPE Stretching from Iceland in the Atlantic to the Black Sea, Europe includes 40 countries, ranging in size from large states, such as France and Germany, to the microstates of Liechtenstein, Andorra, San Marino, and Monaco. Currently the population of the region is about 531 mil- lion. Europe is highly urbanized and, for the most part, relatively wealthy, par- ticularly the western portion. However, economic and social differences between eastern and western Europe remain a problem. (left) Migration re- mains one of Europe’s most troublesome issues. While some immigrates will- ingly embrace European values and culture, others prefer to remain more distant by resisting cultural and political integration. In Britain, for example, there is ongoing debate about Muslim women wearing their traditional veils. (Dave Thompson/AP Wide World Photos) 8 Europe SETTING THE BOUNDARIES The European region is small compared to the United roots. The Greeks and Romans divided their worlds into problematic. Now some geography textbooks extend States. In fact, Europe from Iceland to the Black Sea the three continents of Europe, Asia, and Africa sepa- Europe to the border with Russia, which places the would fit easily into the eastern two-thirds of North rated by the Mediterranean Sea, the Red Sea, and the two countries of Ukraine and Belarus, former Soviet America. A more apt comparison would be Canada, Bosporus Strait. A northward extension of the Black Sea republics, in eastern Europe. Though an argument can as Europe, too, is a northern region. More than half was thought to separate Europe from Asia, and only in be made for that expanded definition of Europe, recent of Europe lies north of the 49th parallel, the line of the 16th century was this proven false. -
[Poster Başlığı] Lorem Ipsum Dolor Sit Amet, Consectetuer Adipiscing Elit
Teaching of the subject “density difference caused by salinity", one of the reasons that plays role in the occurrence of currents in straits, seas and oceans by the use of a teaching material Verim Gümüşsoy 1, 2 1 Poster B29, Abstract EGU2015-2437 Geography Teacher, Harmandere Vocational and Technical Anatolian High School, Pendik, Istanbul, Turkey ([email protected]) 2 Postgraduate Student, Department of Geography, Sakarya University, Serdivan, Sakarya, Turkey ([email protected]) CURRENTS IN STRAITS, SEAS AND OCEANS SUBSURFACE CURRENTS IN THE BOSPORUS CURRENT DEMONSTRATION • I get my students to carry out a small demonstration to help • Large masses of moving water in seas The Black Sea Black Sea them understand the occurrence of ocean currents and and oceans are called currents. currents in the seas and the Bosporus by the use of a material. • Fundamental reasons of currents are The Bosporus Marmara Sea steady winds that occur due to the Istanbul • We need very simple materials to carry out this Aegean global atmospheric system and the Marmara Sea Sea demonstration: An aquarium, a bowl, water, salt, dye and any density differences caused by different stick to mix. heat and salinity levels of water masses. • As Marmara Sea has higher salt amount than Black Sea, • Different feeding and there is a great density difference between these two seas. evaporation • Marmara Sea has a higher concentration of salt and characteristics of seas therefore a higher density than Black Sea. and oceans result in • The demonstration is carried out as follows: we put water, salt salinity and density • And this leads to occurrence of subsurface currents in the and dye in the bowl and mix it well. -
TURKEY Threats to the World Heritage in the Changing Metropolitan Areas of Istanbul
Turkey 175 TURKEY Threats to the World Heritage in the Changing Metropolitan Areas of Istanbul The Historic Areas of Istanbul on the Bosporus peninsula were in- scribed in 1985 in the World Heritage List, not including Galata and without a buffer zone to protect the surroundings. Risks for the historic urban topography of Istanbul, especially by a series of high- rise buildings threatening the historic urban silhouette, were already presented in Heritage at Risk 2006/2007 (see the visual impact as- sessment study by Astrid Debold-Kritter on pp. 159 –164). In the last years, dynamic development and transformation have changed the metropolitan areas with a new scale of building inter- ventions and private investments. Furthermore, the privatisation of urban areas and the development of high-rise buildings with large ground plans or in large clusters have dramatically increased. orld eritagea,,eerules and standards set upby arely knownconveyrthe ap- provedConflicts in managing the World Heritage areas of Istanbul Metropolis derive from changing the law relevant for the core area- sisthe . Conservation sites and areas of conservation were proposed in 1983. In 1985, the historic areas of Istanbul were inscribed on the basis of criteria 1 to 4. The four “core areas”, Archaeological Park, Süleymaniye conservation site, Zeyrek conservation site, and the Theodosian land walls were protected by Law 2863, which in Article I (4) gives a definition of “conservation” and of “areas of conservation”. Article II defines right and responsibility: “cultural and natural property cannot be acquired through possession”; article Fig. 1. Project for Diamond of Dubai, 2010, height 270 m, 53 floors, Hattat 17 states that “urban development plans for conservation” have to Holding Arch. -
Bianca Elliott Lesson Title WHAT to THINK ABOUT the BALKAN
Bianca Elliott Lesson Title WHAT TO THINK ABOUT THE BALKAN SITUATION IN THE 1800S AND 1900S Class and Grade level(s) High School World History Classes or Western Civilization Classes Goals and Objectives The student will be able to: • Read and view materials that provide multiple views of the Balkan situation in the 1800 and 1900 AD. • After reading the selections, students will determine the geographic relevance of the activi- ties that occurred in the Balkans and the political entities involved. • Students will then decide if geography played a critical part in the decision they made and the decisions made in the past. They will verify their answers. • Students will analyze the different forces pulling at and within the Balkans and determine if there were any other ways the end could have changed and how. Curriculum standards addressed: Geography: The student uses a working knowledge and understanding of the spatial organiza- tion of Earth’s surface and relationships between peoples and places and physical and human environments in order to explain the interactions that occur in Kansas, the United States, and in our world. Benchmark 1: Geographic Tools and Location: The student uses maps, graphic representations, tools, and technologies to locate, use, and present information about people, places, and environ- ments. The student: 1. (K) locates major political and physical features of Earth from memory and compares the rela- tive locations of those features. Locations will be included in indicator at each grade level (e.g., Beijing, English Channel, India, Iraq, Moscow, Sahara Desert, South Africa, Venezuela, Balkan Peninsula, Berlin, Black Sea, Bosporus Strait, Euphrates River, Geneva, Hong Kong, Israel, Libya, North Korea, Pakistan, Saudi Arabia, Singapore, South Korea, Suez Canal, Tigris River, Tokyo, Yangtze River).