Geografski Obrasci Genetičke I Morfološke Varijabilnosti Predstavnika Grupe Silene Saxifraga (Caryophyllaceae)

Total Page:16

File Type:pdf, Size:1020Kb

Geografski Obrasci Genetičke I Morfološke Varijabilnosti Predstavnika Grupe Silene Saxifraga (Caryophyllaceae) UNIVERZITET U BEOGRADU BIOLOŠKI FAKULTET Sanja Z. Đurović GEOGRAFSKI OBRASCI GENETIČKE I MORFOLOŠKE VARIJABILNOSTI PREDSTAVNIKA GRUPE SILENE SAXIFRAGA (CARYOPHYLLACEAE) doktorska disertacija Beograd, 2017 UNIVERSITY OF BELGRADE FACULTY OF BIOLOGY Sanja Z. Đurović GEOGRAPHICAL PATTERNS OF GENETIC AND MORPHOLOGICAL VARIABILITY OF THE TAXA BELONGING TO SILENE SAXIFRAGA GROUP (CARYOPHYLLACEAE) Doctoral Dissertation Belgrade, 2017 Mentori: dr Marjan Niketić naučni i muzejski savetnik, Prirodnjački muzej u Beogradu dr Gordana Tomović vanredni profesor, Univerzitet u Beogradu - Biološki fakultet Članovi komisije: dr Vladimir Stevanović redovni profesor u penziji, Univerzitet u Beogradu - Biološki fakultet, redovni član SANU dr Maja Lazarević docent, Univerzitet u Beogradu - Biološki fakultet dr Božo Frajman vanredni profesor, Univerzitet u Insbruku - Biološki fakultet Datum odbrane: _______________________ Izjave zahvalnosti Ova doktorska disertacija je realizovana u okviru projekta Ministarstva prosvete, nauke i tehnološkog razvoja Republike Srbije br. 173030 pod nazivom „Biodiverzitet biljnog sveta Srbije i Balkanskog poluostrva – procena, održivo korišćenje i zaštita“, na Katedri za ekologiju i geografiju biljaka Biološkog fakulteta Univerziteta u Beogradu. Molekularne analize su sprovedene u Institutu za Botaniku u Insbruku, u Austriji, a horološka istraživanja su u velikoj meri pomognuta SYNTHESYS stipendijama (AT-TAF-3503 i CZ-TAF-4439). Mnogi ljudi su me zadužili svojim savetima i pomoći tokom pripremanja ove teze i neću imenovati ni približno sve njih. Posebno se zahvaljujem mentorima dr Gordani Tomović i dr Marjanu Niketiću na ukazanoj šansi i poverenju, bez čijih ideja, znanja i iskustva ne bi bilo ove disertacije, ali i na velikoj pomoći prilikom terenskih istraživanja i na brojnim uspomenama sa zajedničkih putovanja, kao i na svim smernicama tokom izrade ove teze. Svojim učešćem u komisiji su mi veliku čast ukazali dr Vladimir Stevanović, dr Maja Lazarević i dr Božo Frajman, i zahvalna sam im na korisnim savetima, posebno tokom završnih faza izrade teze. Božo Frajman je ujedno i jedna od najzaslužnijih osoba zahvaljujući kojima su urađene molekularne analize i hvala mu na pruženoj prilici i uvek pozitivnom stavu tokom naše saradnje. Pored njega, mnogo su mi pomogli i dr Peter Schönswetter, Marianne Magauer i Daniela Pirkebner. Kustosi i botaničari koji su mi izašli u susret tokom poseta herbarskim zbirkama, a kojima sam veoma zahvalna, su: dr Snežana Vukojičić (BEOU), dr Zoltan Barina (BP), Otakar Šida (PR), Patrik Mráz (PRC), Dimitar Dimitrov (SO), Kiril Stoyanov (SOA), Chavdar Gusev i Svetlana Bancheva (SOM), dr Ernst Vitek (W), Walter Till (WU), dr Ivana Rešetnik i dr Antun Alegro (ZA, ZAHO). Snežana Vukojičić je bila mnogo više od jednog kustosa tokom posete zbirci. Njen vedri duh i veliko znanje su bili pokretačka snaga u mnogim trenucima. Neizmerno hvala na svim diskusijama i divnom društvu na terenskim istraživanjima. Zahvalna sam i brojnim profesorima i kolegama, koji su izvrsni učitelji, pomoć i inspiracija. Posebno hvala dr Dmitru Lakušiću, dr Jasmini Šinžar-Sekulić i dr Ljiljani Tomović, koji su nesebično podelili svoja znanja, koja su mi mnogo značila u izradi ove teze. Veoma sam zahvalna svojoj porodici i prijateljima, koji su ulepšali izradu ove teze svojom podrškom. Geografski obrasci genetičke i morfološke varijabilnosti predstavnika grupe Silene saxifraga (Caryophyllaceae) Sažetak Uzimajući u obzir prethodne klasifikacije i nejasne odnose između taksona u okviru ili dovođenih u vezu sa grupom Silene saxifraga, korišćene su nuklearne sekvence ITS, hloroplastne sekvence rps16 i polimorfizmi dužine umnoženih fragmenata (AFLP-ovi), za utvrđivanje filogenetičkih odnosa između ispitivanih taksona. Filogenetička analiza uzoraka 112 populacija, iz čitavog areala grupe, koji predstavljaju 33 taksona, je pokazala da su S. cephallenia, S. congesta, S. linoides, S. multicaulis, S. schwarzenbergeri i S. waldsteinii jasno izdiferencirane od ostalih analiziranih taksona, koji su formirali redefinisanu grupu S. saxifraga. Filogenetički odnosi u okviru ove grupe su slabo razjašnjeni i nisu u potpunosti u skladu sa aktuelnom taksonomijom. Na filogenetičkom stablu se uglavnom grupišu geografski bliske populacije, a ne one koje pripadaju istom taksonu, verovatno zato što je grupa nastala u skorije vreme, u pleistocenu, nakon čega je došlo do brze radijacije i ekspanzije areala. Redefinisanje taksona u okviru grupe S. saxifraga izvršeno je na osnovu multivarijantne analize morfometrijskih podataka i razlika u kvalitativnim karakterima. Analizirani su uzorci 122 populacije koje predstavljaju 22 taksona, uključujući S. linoides, S. multicaulis i S. waldsteinii. Izdvojeno je deset taksona u rangu vrste i osam podvrsta u okviru vrste S. saxifraga. Opisana je jedna nova vrsta (S. ancrae) i jedna nova podvrsta (S. saxifraga subsp. lurensis). Šest taksona je ušlo u novu kombinaciju, a od njih je pet dobilo i novi status. Ključ za identifikaciju taksona u okviru revidirane grupe S. saxifraga prate dopune originalnih opisa, kao i horološki podaci i karakteristike staništa. Centar genetičkog i taksonomskog diverziteta grupe se nalazi u južnim delovima Balkanskog poluostrva. Ključne reči: AFLP; Balkansko poluostrvo; diverzifikacija; filogeografija; horologija; ITS; morfometrija; Silene sect. Saxifragoideae; S. saxifraga grupa, taksonomija Naučna oblast: Biologija Uža naučna oblast: Ekologija, biogeografija i zaštita životne sredine UDK broj: [581.961+575.22]:582.661.51(497)(043.3) Geographical patterns of genetic and morphological variability of the taxa belonging to Silene saxifraga group (Caryophyllaceae) Abstract Considering previous classifications and unresolved relationships among taxa belonging to or hypothesized to be closely related to Silene saxifraga group, we used sequences of the nuclear ribosomal internal transcribed spacer (ITS), the plastid rps16 intron and amplified fragment length polymorphisms (AFLPs) to elucidate phylogenetic relationships, covering the section’s entire geographical range. Phylogenetic analyses of 112 populations belonging to 33 taxa showed that S. cephallenia, S. congesta, S. linoides, S. multicaulis, S. schwarzenbergeri and S. waldsteinii are clearly differentiated from all other taxa, which are included in the newly circumscribed S. saxifraga group. Unresolved phylogenetic relationships governed by geographic proximity rather than by taxonomic identity within S. saxifraga group are probably the result of recent rapid radiation and range expansion and/or local adaptation to divergent environments. Delimitation among taxa belonging to S. saxifraga group is discussed on the basis of multivariate analysis of morphometric data and differences in qualitative characters. Samples from 122 populations belonging to 22 taxa, including S. linoides, S. multicaulis and S. waldsteinii were analysed. Ten taxa are treated as species, with eight subspecies within S. saxifraga. One new species (S. ancrae) and one new subspecies (S. saxifraga subsp. lurensis) are desribed, whereas six taxa are given as new combination and five out of them as new status. Diagnostic key followed by addition to the original description of taxa belonging to revised S. saxifraga group is given, together with chorological data and habitat features. The southern part of the Balkan Peninsula is the centre of genetic and taxonomic diversity of the group. Key words: AFLP; Balkan Peninsula; chorology; diversification; ITS; phylogeography; morphometrics; Silene sect. Saxifragoideae; S. saxifraga group, taxonomy Scientific field: Biology Scientific subfield: Ecology, biogeography and environmental protection UDC number: [581.961+575.22]:582.661.51(497)(043.3) SADRŽAJ 1. UVOD ........................................................................................................................... 1 1.1. Istorijat klasifikacije tribusa Sileneae i roda Silene na osnovu morfologije i filogenetička istraživanja. ............................................................................................... 1 1.2. Filogeografska istraživanja južnoevropskih taksona. ................................................. 10 1.3. Karakteristike istraživanih taksona, koji su tokom istorije dovedeni u vezu sa grupom S. saxifraga. ..................................................................................................... 11 1.4. Pregled klasifikacije vrsta koje su tokom istorije dovedene u vezu sa grupom S. saxifraga. ....................................................................................................................... 45 2. CILJEVI RADA ......................................................................................................... 53 3. MATERIJAL I METODE .......................................................................................... 54 3.1. Molekularne analize ...................................................................................................... 54 3.1.1. Biljni materijal............................................................................................... 54 3.1.2. Rad u laboratoriji (ekstrakcija DNK, ITS, rps16, AFLP). ............................ 55 3.1.3. Analiza sekvenci. .......................................................................................... 57 3.1.4. Analiza polimorfizma dužine umnoženih fragmenata. ................................. 57 3.2. Morfometrijske analize ................................................................................................
Recommended publications
  • Moüjmtaiim Operations
    L f\f¿ áfó b^i,. ‘<& t¿ ytn) ¿L0d àw 1 /1 ^ / / /This publication contains copyright material. *FM 90-6 FieW Manual HEADQUARTERS No We DEPARTMENT OF THE ARMY Washington, DC, 30 June 1980 MOÜJMTAIIM OPERATIONS PREFACE he purpose of this rUanual is to describe how US Army forces fight in mountain regions. Conditions will be encountered in mountains that have a significant effect on. military operations. Mountain operations require, among other things^ special equipment, special training and acclimatization, and a high decree of self-discipline if operations are to succeed. Mountains of military significance are generally characterized by rugged compartmented terrain witn\steep slopes and few natural or manmade lines of communication. Weather in these mountains is seasonal and reaches across the entireSspectrum from extreme cold, with ice and snow in most regions during me winter, to extreme heat in some regions during the summer. AlthoughNthese extremes of weather are important planning considerations, the variability of weather over a short period of time—and from locality to locahty within the confines of a small area—also significantly influences tactical operations. Historically, the focal point of mountain operations has been the battle to control the heights. Changes in weaponry and equipment have not altered this fact. In all but the most extreme conditions of terrain and weather, infantry, with its light equipment and mobility, remains the basic maneuver force in the mountains. With proper equipment and training, it is ideally suited for fighting the close-in battfe commonly associated with mountain warfare. Mechanized infantry can\also enter the mountain battle, but it must be prepared to dismount and conduct operations on foot.
    [Show full text]
  • The Mountains of Crete
    208 THE MOUNTAINS OF CRETE THE MOUNTAINS OF CRETE BY L. H. HURST F he is not already aware of the fact, the visitor to Crete will at once perceive that it is a highly mountainous island. There are three groups whose summits exceed z,ooo m. In the west, the White Mountains rise behind Canea and fall steeply on the south to the Libyan sea. The area contains some twenty such summits and is by far the most important of the three. Mount Ida (in Greek, Psiloriti) rises in the centre of the island. In the east, the upland Lasithi plain is ringed by hills and mountains which reach their highest point in Mount Dikte to the south. With the possible exception of one particular face, the rock­ climber is unlikely to find anything to interest him in Crete. All the summits are easy and can be reached from various directions. But for the elderly mountaineer, whose more active days are behind him but who is still able to walk and to whom untravelled regions have an appeal, Crete may well be the answer. The mountains are best visited at the end of April or in early May, while some snow still remains to give them such beauty as they may claim and add to the interest of the ascents. Only a great enthusiast would wander amongst them in the months of summer when they have been stripped to their bare bones and their grey limestone faces blench and shimmer under a sun that is more African than European.
    [Show full text]
  • The Pirin Mountains, Bulgaria) in the Last Ten Years
    STUDIA GEOMORPHOLOGICA CARPATHO-BALCANICA VOL. XLV, 2011: 47–68 PL ISSN 0081-6434 EMIL GACHEV (BLAGOEVGRAD) INTER-ANNUAL SIZE VARIATIONS OF SNEZHNIKA GLACIERET (THE PIRIN MOUNTAINS, BULGARIA) IN THE LAST TEN YEARS Abstract: Glacierets, which are in fact embryonic forms of recent glaciation, can serve as important indicators of contemporary climate dynamics in areas where classical glaciers do not exist, such as the high mountains in Southeastern Europe. Two glacierets are located in Bulgaria’s Pirin Mountains: Snezhnika and Banski Suhodol. Snezhnika has been relatively well studied for the last 50 years, and in particular since 1994, when annual size measurements on a regular basis started. The present study focuses on the recent variations in the size of Snezhnika i.e. in the last ten years. Data about the area of the glacieret at the end of the ablation season (in autumn), which was obtained for each year by field measurements and analytical calculations, show that temperature can be considered as a major factor that drives glacieret fluctuations. At the current stage precipitation factor can not be evaluated properly due to the deficit of accurate climate information. Key words: the Pirin Mountains, glacierets, size variation, climate change, climatic factors INTRODUCTION Although small in size and volume, in many mountain areas glacierets are natu- ral features of sufficient value for studies of the dynamics of environmental proc- esses, climatic variations and change. Glacierets are small bodies of perennial ice, which are smaller than glaciers but bigger and more persistent than snow patches. Glacierets are typified by a density of close-to-bottom ice of about 0.6 to 0.8 g cm–3, presence of annual layers in the vertical cross-section, and long- term persistence — decades to centuries (G r u n e w a l d et al.
    [Show full text]
  • Monitoring Methodology and Protocols for 20 Habitats, 20 Species and 20 Birds
    1 Finnish Environment Institute SYKE, Finland Monitoring methodology and protocols for 20 habitats, 20 species and 20 birds Twinning Project MK 13 IPA EN 02 17 Strengthening the capacities for effective implementation of the acquis in the field of nature protection Report D 3.1. - 1. 7.11.2019 Funded by the European Union The Ministry of Environment and Physical Planning, Department of Nature, Republic of North Macedonia Metsähallitus (Parks and Wildlife Finland), Finland The State Service for Protected Areas (SSPA), Lithuania 2 This project is funded by the European Union This document has been produced with the financial support of the European Union. Its contents are the sole responsibility of the Twinning Project MK 13 IPA EN 02 17 and and do not necessarily reflect the views of the European Union 3 Table of Contents 1. Introduction .......................................................................................................................................................... 6 Summary 6 Overview 8 Establishment of Natura 2000 network and the process of site selection .............................................................. 9 Preparation of reference lists for the species and habitats ..................................................................................... 9 Needs for data .......................................................................................................................................................... 9 Protocols for the monitoring of birds ....................................................................................................................
    [Show full text]
  • About Bulgaria
    Source: Zone Bulgaria (http://en.zonebulgaria.com/) About Bulgaria General Information about Bulgaria Bulgaria is a country in Southeastern Europe and is situated on the Balkan Peninsula. To the north the country borders Rumania, to the east – the Black Sea, to the south – Turkey and Greece, and to the west – Yugoslavia and Macedonia. Bulgaria is a parliamentary republic with a National Assembly (One House Parliament) of 240 national representatives. The President is Head of State. Geography of Bulgaria The Republic of Bulgaria covers a territory of 110 993 square kilometres. The average altitude of the country is 470 metres above sea level. The Stara Planina Mountain occupies central position and serves as a natural dividing line from the west to the east. It is a 750 km long mountain range stretching from the Vrushka Chuka Pass to Cape Emine and is part of the Alpine-Himalayan mountain range. It reaches the Black Sea to the east and turns to the north along the Bulgarian-Yugoslavian border. A natural boundary with Romania is the Danube River, which is navigable all along for cargo and passenger vessels. The Black Sea is the natural eastern border of Bulgaria and its coastline is 378 km long. There are clearly cut bays, the biggest two being those of Varna and Bourgas. About 25% of the coastline are covered with sand and hosts our seaside resorts. The southern part of Bulgaria is mainly mountainous. The highest mountain is Rila with Mt. Moussala being the highest peak on the Balkan Peninsula (2925 m). The second highest and the mountain of most alpine character in Bulgaria is Pirin with its highest Mt.
    [Show full text]
  • Bonelli's Eagle and Bull Jumpers: Nature and Culture of Crete
    Crete April 2016 Bonelli’s Eagle and Bull Jumpers: Nature and Culture of Crete April 9 - 19, 2016 With Elissa Landre Photo of Chukar by Elissa Landre With a temperate climate, Crete is more pristine than the mainland Greece and has a culture all its own. Crete was once the center of the Minoan civilization (c. 2700–1420 BC), regarded as the earliest recorded civilization in Europe. In addition to birding, we will explore several famous archeological sites, including Knossos and ancient Phaistos, the most important centers of Minoan times. Crete’s landscape is very special: defined by high mountain ranges, deep valleys, fertile plateaus, and caves (including the mythological birthplace of the ancient Greek god, Zeus) Rivers have cut deep, exceptionally beautiful gorges that create a rich presence of geological wealth and have been explored for their aromatic and medicinal plants since Minoan times. Populations of choughs, Griffon Vultures, Lammergeiers, and swifts nest on the steep cliffs. A fantastic variety of birds and plants are found on Crete: not only its resident bird species, which are numerous and include rare and endangered birds, but also the migrants who stop over on Crete during their journeys to and from Africa and Europe. The isolation of Crete from mainland Europe, Asia, and Africa is reflected in the diversity of habitats, flora, and avifauna. The richness of the surroundings results in an impressive bird species list and often unexpected surprises. For example, last year a Blue- cheeked Bee-eater, usually only seen in northern Africa and the Middle East, was spotted. Join us for this unusual and very special trip.
    [Show full text]
  • Articles, Only Recently
    Nat. Hazards Earth Syst. Sci., 16, 2085–2106, 2016 www.nat-hazards-earth-syst-sci.net/16/2085/2016/ doi:10.5194/nhess-16-2085-2016 © Author(s) 2016. CC Attribution 3.0 License. Climate anomalies associated with the occurrence of rockfalls at high-elevation in the Italian Alps Roberta Paranunzio1, Francesco Laio1, Marta Chiarle2, Guido Nigrelli2, and Fausto Guzzetti3 1Department of Environment, Land and Infrastructure Engineering, Politecnico di Torino, Torino, Italy 2Research Institute for Geo-hydrological Protection, National Research Council (CNR IRPI), Torino, Italy 3Research Institute for Geo-hydrological Protection, National Research Council (CNR IRPI), Perugia, Italy Correspondence to: Roberta Paranunzio ([email protected]) Received: 29 March 2016 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 4 April 2016 Revised: 13 July 2016 – Accepted: 22 August 2016 – Published: 12 September 2016 Abstract. Climate change is seriously affecting the 1 Introduction cryosphere in terms, for example, of permafrost thaw, al- teration of rain=snow ratio, and glacier shrinkage. There is concern about the increasing number of rockfalls at high el- The recent decades have seen a pronounced warming in evation in the last decades. Nevertheless, the exact role of global climate, primarily at high elevations and high latitudes climate parameters in slope instability at high elevation has (Schär et al., 2004). Temperature across European Alps has ◦ not been fully explored yet. In this paper, we investigate 41 increased of about 1.4 K per century over the period 1906– rockfalls listed in different sources (newspapers, technical re- 2005, which is more than double the global average (Brunetti ports, and CNR IRPI archive) in the elevation range 1500– et al., 2009) and further increases are expected according to 4200 m a.s.l.
    [Show full text]
  • Greek Tourism 2009 the National Herald, September 26, 2009
    The National Herald a b September 26, 2009 www.thenationalherald.com 2 GREEK TOURISM 2009 THE NATIONAL HERALD, SEPTEMBER 26, 2009 RELIGIOUS TOURISM Discover The Other Face of Greece God. In the early 11th century the spring, a little way beyond, were Agios Nikolaos of Philanthropenoi. first anachorites living in the caves considered to be his sacred fount It is situated on the island of Lake in Meteora wanted to find a place (hagiasma). Pamvotis in Ioannina. It was found- to pray, to communicate with God Thessalonica: The city was ed at the end of the 13th c by the and devote to him. In the 14th cen- founded by Cassander in 315 B.C. Philanthropenoi, a noble Constan- tury, Athanassios the Meteorite and named after his wife, Thessa- tinople family. The church's fres- founded the Great Meteora. Since lonike, sister of Alexander the coes dated to the 16th c. are excel- then, and for more than 600 years, Great. Paul the Apostle reached the lent samples of post-Byzantine hundreds of monks and thousands city in autumn of 49 A.D. painting. Visitors should not miss in of believers have travelled to this Splendid Early Christian and the northern outer narthex the fa- holy site in order to pray. Byzantine Temples of very impor- mous fresco depicting the great The monks faced enormous tant historical value, such as the Greek philosophers and symboliz- problems due to the 400 meter Acheiropoietos (5th century A.D.) ing the union between the ancient height of the Holy Rocks. They built and the Church of the Holy Wisdom Greek spirit and Christianity.
    [Show full text]
  • Europa –Kontinent Der Berge Seite! Und Schauen Wir, Was Eu- Denn Die Grenze Zu Asien Ist Nicht Eindeutig Festgelegt
    BERGSTEIGEN EUROPAWEIT BERGSTEIGEN EUROPAWEIT Text: Joachim Burghardt assen wir die Alpen einmal bei- Europas – wenn man ihn denn als europäisch erachtet, Europa –Kontinent der Berge seite! Und schauen wir, was Eu- denn die Grenze zu Asien ist nicht eindeutig festgelegt. ropa an Bergen sonst noch zu Neben diesen großen Ketten und Massiven finden sich L bieten hat. Beim Blick auf die to- unzählige weitere Gebirge: die Gletscherberge Islands, pografische Karte fallen zuerst die gro- das französische Zentralmassiv, die schottischen High- Europa ist ein Kontinent der Berge – und ein Kontinent der Vielfalt. ßen Gebirgsketten ins Auge: im Westen lands und die deutschen Mittelgebirge, um nur wenige Große und kleine Gebirge, Gletscher- und Inselberge, Vulkane, Wald- die Pyrenäen. Im Norden das Skandina- zu nennen. vische Gebirge. Im Süden der Apennin. Bei genauerem Hinsehen treten aus den Gebirgen hügel und Meeresklippen laden ein zum Träumen, zum Entdecken und Im Südosten das verschlungene Ge- einzelne Berge und Gipfel hervor. Beginnend mit den birgsknäuel des Balkans, gebildet aus höchsten zunächst die Giganten des Kaukasus: Elbrus zum Besteigen. Bereit für eine Rundreise durch die Bergwelt Europas? Dinariden, Balkangebirge, Korab, Pindos (5642 m, je nach Definition der Kontinentgrenze höchs- und vielen weiteren gebirgigen Einhei- ter Berg Europas oder eben nicht), Dychtau (5203 m), Schchara ten. Schließlich im Osten der geschwun- (5201 m) und Kasbek (5047 m); unter den Viertausendern ist der spektaku- gene Karpatenbogen. Wenn der Blick lär aussehende Uschba (4737 m) wohl der prominenteste. Berge dieser Kra- noch ein gutes Stück weiter ostwärts genweite gibt es nur im Kaukasus und – auf Viertausender-Niveau – in den schweift, hinweg über das endlose russi- Alpen.
    [Show full text]
  • 2012 Update of the Scientific Data Underpinning the UNEP/CMS
    2012 Update of the scientific data underpinning the UNEP/CMS Memorandum of Understanding on the Conservation of Migratory Birds of Prey in Africa and Eurasia (Raptors MoU) BirdLife International October 2012 1 2012 Update of the scientific data underpinning the UNEP/CMS Memorandum of Understanding on the Conservation of Migratory Birds of Prey in Africa and Eurasia (Raptors MoU) October 2012 Prepared by Tris Allinson (Science & Information Management Officer, BirdLife International) Vicky Jones (Global Flyways Officer, BirdLife International) BirdLife International Wellbrook Court Girton Road Cambridge CB3 0NA UNITED KINGDOM T: +44 (0)1223 277 318 F: +44 (0)1223 277 200 E: birdlife @ birdlife.org Reviewed by Ibrahim Alhasani (Flyway Officer, Middle East, BirdLife International) Stuart Butchart (Global Research & Indicators Coordinator, BirdLife International) Lincoln Fishpool (Global IBA Coordinator, BirdLife International) Richard Grimmett (Director of Conservation, BirdLife International) Alison Stattersfield (Head of Science, BirdLife International) Nick P. Williams (Programme Officer Birds of Prey – Raptors, UNEP CMS) Additional contributions provided by Osama Alnouri (RFF Coordinator, Middle East, BirdLife International) Leon Bennun (Director of Science, Policy and Information Management, BirdLife International and CMS Appointed Councillor (Birds) Nicola J. Crockford (International Species Policy Officer, RSPB) George Eshiamwata (Flyway Officer, Africa, BirdLife International) Melanie Heath (Head of Policy, BirdLife International) Marcus Kohler (Senior Programme Manager, Flyways Programme, BirdLife International) Recommended citation: BirdLife International (2012) 2012 Update of the scientific data underpinning the UNEP/CMS Memorandum of Understanding on the Conservation of Migratory Birds of Prey in Africa and Eurasia (Raptors MoU). Cambridge, UK: BirdLife International. Cover image: Egyptian Vulture © Vladimir Melnik/Dreamstime.com 2 Contents 1.
    [Show full text]
  • “Samothraki Biosphere Reserve Nomination Form”
    “Samothraki Biosphere Reserve Nomination form” Final Official Document - Resubmission September 2013 UNESCO - Man and the Biosphere (MAB) Programme - Biosphere reserve nomination form - January 2013 1 BIOSPHERE RESERVE NOMINATION FORM [January 2013] INTRODUCTION Biosphere reserves are areas of terrestrial and coastal/marine ecosystems, or a combination thereof, which are internationally recognized within the framework of UNESCO's Programme on Man and the Biosphere (MAB) They are established to promote and demonstrate a balanced relationship between humans and the biosphere. Biosphere reserves are designated by the International Coordinating Council of the MAB Programme at the request of the State concerned. Individual biosphere reserves remain under the sovereign jurisdiction of the State where they are situated. Collectively, all biosphere reserves form a World Network in which participation by States is voluntary. The World Network is governed by the Statutory Framework adopted by the UNESCO General Conference in 1995 which presents the definition, objectives, criteria and the designation procedure for biosphere reserves. The actions recommended for the implementation of biosphere reserves are set out in the "Seville Strategy" and were further developed in the Madrid Action Plan (2008-2013). These documents should be used as basic references for the completion of this nomination form. The information presented on this nomination form will be used in a number of ways by UNESCO: (a) for examination of the site by the International Advisory Committee for Biosphere Reserves and by the Bureau of the MAB International Coordinating Council; (b) for use in a world-wide accessible information system, notably the UNESCO-MABnet and publications, facilitating communications and interaction amongst persons interested in biosphere reserves throughout the world.
    [Show full text]
  • Commission Implementing Decision of 16 November 2012 Adopting A
    26.1.2013 EN Official Journal of the European Union L 24/647 COMMISSION IMPLEMENTING DECISION of 16 November 2012 adopting a sixth updated list of sites of Community importance for the Mediterranean biogeographical region (notified under document C(2012) 8233) (2013/29/EU) THE EUROPEAN COMMISSION, (4) In the context of a dynamic adaptation of the Natura 2000 network, the lists of sites of Community importance are reviewed. An update of the list of sites Having regard to the Treaty on the Functioning of the European of Community importance for the Mediterranean biogeo­ Union, graphical region is therefore necessary. Having regard to Council Directive 92/43/EEC of 21 May 1992 on the conservation of natural habitats and of wild fauna and (5) On the one hand, the update of the list of sites of flora ( 1), and in particular the third subparagraph of Article 4(2) Community importance for the Mediterranean biogeo­ thereof, graphical region is necessary in order to include additional sites that have been proposed since 2010 by Whereas: Member States as sites of Community importance for the Mediterranean biogeographical region within the meaning of Article 1 of Directive 92/43/EEC. For these (1) The Mediterranean biogeographical region referred to in additional sites, the obligations resulting from Articles Article 1(c)(iii) of Directive 92/43/EEC comprises the 4(4) and 6(1) of Directive 92/43/EEC should apply as Union territories of Greece, Cyprus, in accordance with soon as possible and within six years at most from the Article 1 of Protocol No 10 of the 2003 Act of Acces­ adoption of this Decision.
    [Show full text]