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EUROPE a Albania • National Historical Museum – Tirana, Albania
EUROPE A Albania • National Historical Museum – Tirana, Albania o The country's largest museum. It was opened on 28 October 1981 and is 27,000 square meters in size, while 18,000 square meters are available for expositions. The National Historical Museum includes the following pavilions: Pavilion of Antiquity, Pavilion of the Middle Ages, Pavilion of Renaissance, Pavilion of Independence, Pavilion of Iconography, Pavilion of the National Liberation Antifascist War, Pavilion of Communist Terror, and Pavilion of Mother Teresa. • Et'hem Bey Mosque – Tirana, Albania o The Et’hem Bey Mosque is located in the center of the Albanian capital Tirana. Construction was started in 1789 by Molla Bey and it was finished in 1823 by his son Ethem Pasha (Haxhi Ethem Bey), great- grandson of Sulejman Pasha. • Mount Dajt – Tirana, Albania o Its highest peak is at 1,613 m. In winter, the mountain is often covered with snow, and it is a popular retreat to the local population of Tirana that rarely sees snow falls. Its slopes have forests of pines, oak and beech. Dajti Mountain was declared a National Park in 1966, and has since 2006 an expanded area of about 29,384 ha. It is under the jurisdiction and administration of Tirana Forest Service Department. • Skanderbeg Square – Tirana, Albania o Skanderbeg Square is the main plaza of Tirana, Albania named in 1968 after the Albanian national hero Skanderbeg. A Skanderbeg Monument can be found in the plaza. • Skanderbeg Monument – Skanderberg Square, Tirana, Albania o The monument in memory of Skanderbeg was erected in Skanderbeg Square, Tirana. -
Freshwater Fishes and Lampreys of Greece
HELLENIC CENTRE FOR MARINE RESEARCH Monographs on Marine Sciences No. 8 Freshwater Fishes and Lampreys of Greece An Annotated Checklist Barbieri R., Zogaris S., Kalogianni E., Stoumboudi M. Th, Chatzinikolaou Y., Giakoumi S., Kapakos Y., Kommatas D., Koutsikos N., Tachos, V., Vardakas L. & Economou A.N. 2015 Freshwater Fishes and Lampreys of Greece An Annotated Checklist HELLENIC CENTRE FOR MARINE RESEARCH Monographs on Marine Sciences No. 8 Freshwater Fishes and Lampreys of Greece An Annotated Checklist Barbieri R., Zogaris S., Kalogianni E., Stoumboudi M. Th, Chatzinikolaou Y., Giakoumi S., Kapakos Y., Kommatas D., Koutsikos N., Tachos, V., Vardakas L. & Economou A.N. 2015 Monographs on Marine Sciences 8 Authors: Barbieri R., Zogaris S., Kalogianni E., Stoumboudi M.Th., Chatzinikolaou Y., Giakoumi S., Kapakos Y., Kommatas D., Koutsikos N., Tachos V., Vardakas L. & Economou A.N. Fish drawings: R. Barbieri English text editing: S. Zogaris, E. Kalogianni, E. Green Design and production: Aris Vidalis Scientific reviewers: Jörg Freyhof, Dimitra Bobori Acknowledgements We would like to thank the following people for significant assistance in the field, for providing unpublished information, and/or support during the preparation of this work: Apostolos Apostolou, Nicolas Bailly, Bill Beaumont, Dimitra Bobori, Giorgos Catsadorakis, Charalambos Daoulas, Elias Dimitriou, Panayiotis Dimopoulos, Uwe Dussling, Panos S. Economidis, Jörg Freyhof, Zbigniew Kaczkowski, Nektarios Kalaitzakis, Stephanos Kavadas, Maurice Kottelat, Emmanuil Koutrakis, David Koutsogianopoulos, Marcello Kovačić, Ioannis Leonardos, Danilo Mrdak, Theodoros Naziridis, Elena Oikonomou, Kostas G. Papakonstatinou, Ioannis Paschos, Kostas Perdikaris, Olga Petriki, Radek Šanda, Nikolaos Skoulikidis, Manos Sperelakis, Kostas Tsigenopoulos, Maarten Vanhove, Haris Vavalidis, Jasna Vukić , Brian Zimmerman and the HCMR library staff (Anavissos Attiki). -
Vegetation History and Palaeoclimate at Lake Dojran (FYROM
Clim. Past Discuss., https://doi.org/10.5194/cp-2017-114 Manuscript under review for journal Clim. Past Discussion started: 29 September 2017 c Author(s) 2017. CC BY 4.0 License. Vegetation history and palaeoclimate at Lake Dojran (FYROM/Greece) during the Late Glacial and Holocene Alessia Masi1, Alexander Francke2,3, Caterina Pepe1, Matthias Thienemann2, Bernd Wagner2, and Laura Sadori1 1Department of Environmental Biology, Sapienza University, Rome, Italy 2Institute of Geology and Mineralogy, University of Cologne, Cologne, Germany 3Wollongong Isotope Geochronology Laboratory, School of Earth and Environmental Sciences, University of Wollongong, Wollongong, Australia Correspondence to: Alessia Masi ([email protected]) Abstract. A new high-resolution pollen and NPPs (Non-Pollen Palynomorphs) analysis has been performed on the sediments of Lake Dojran, a transboundary lake located at the border between Greece and Former Yugoslavian Republic of Macedonia (FYROM). The sequence covers the last 12500 years and provides information on vegetational dynamics of the Late Glacial and Holocene for southern Balkans. A robust age-model, sedimentological, diatom, and biomarker analyses published previously 5 have been the base for a multi-perspective interpretation of the new palynological data. Pollen analysis revealed that the Late Glacial is characterized by steppic taxa with prevailing Amaranthaceae, Artemisia and Poaceae. The arboreal vegetation starts to rise after 11500 yr BP, taking a couple of millennia to be definitively attested. Holocene vegetation is characterized by the dominance of mesophilous plants. Quercus robur type and Pinus are the most abundant taxa followed by Quercus cerris type, Quercus ilex type and Ostrya/Carpinus orientalis. The first attestation of human presence can be presumed at 5000 yr BP for the 18 10 contemporary presence of cereals, Juglans and Rumex. -
Action for Culture in Mediterranean Wetlands Culture Action for Cover Page: Fishing at Orbetello Lagoon
Thymio Papayannis Med-INA Med-INA works closely with the following The Mediterranean Institute for Nature institutions: and Anthropos is a non-profit science and ñ Convention on Wetlands (Ramsar,1971) conservation organization established in ñ MedWet Initiative 2003,in Greece,with an international man- ñ IUCN / WCPA / CSVPA Task Force date. ñ European Landscape Convention Its mission is to contribute to a harmonious ñ UNESCO / World Heritage Convention Action for culture relationship between Anthropos (Man- ñThe Society for the Protection of Prespa kind) and Nature, by working on the interface between the two,particularly in Contacts: in Mediterranean wetlands the Mediterranean Region,through multi- Irini Lyratzaki disciplinary research,intergrated action and Med-INA Scientific Secretariat public awareness. 23 Voucourestiou Street, 10671 Athens, Greece Main activities T: +30 210 3600712 Med-INA’s main current activities include: F: +30 210 3629338 ñAnalyzing cultural activities in 21 Mediter- E: [email protected] ranean wetland sites and drawing con- clusions for the conservation jointly of natural and cultural values. ñDeveloping the guidance for the in- corporation of cultural values in the management of wetlands for the Ramsar Convention. ñAssisting the Society for the Protection of Prespa in establishing the Prespa Centre for Nature and Anthropos. ñWorking on the conservation of Mediter- ranean landscapes,focussing on island cultural landscapes, water related landscapes and the landscapes of Greece. ñEditing with Peter Howard the double issue of the International Journal of Heritage Studies on Nature as heritage (September 2007). ñCo-ordinating jointly with Silene (Catalonia, Spain) the Delos Initia- tive on sacred natural sites in devel- oped countries, in the framework of IUCN / WCPA and its Task Force on Cultural and Spiritual Values. -
Information Sheet on Ramsar Wetlands (Ris): Butrint (Albania)
Information Sheet on Ramsar Wetlands (Ris): Butrint (Albania) Information Sheet on Ramsar Wetlands (RIS) Categories approved by Recommendation 4.7, as amended by Resolution VIII.13 of the Conference of the Contracting Parties. 1. Name and address of the compiler of this form: Zamir Dedej FOR OFFICE USE ONLY. Director of Nature Protection Directorate DD MM YY Ministry of Environment Rr. Durresi, Nr. 27 Tirana – ALBANIA Tel: + 355 4 270624 Designation date Site Reference Number Fax: + 355 4 270 627 E-mail: [email protected] Taulant Bino Museum of Natural Sciences, Rr. e Kavajes 132, Tirana, Albania Tel/Fax : 00 355 42 29028 E-mail : [email protected] 2. Date this sheet was completed/updated: 20th of March 2003 3. Country: Albania 4. Name of the Ramsar site: Butrint 5. Map of site included: Refer to Annex III of the Explanatory Note and Guidelines, for detailed guidance on provision of suitable maps. a) hard copy (required for inclusion of site in the Ramsar List): yes -or- no b) digital (electronic) format (optional): yes -or- no 6. Geographical coordinates (latitude/longitude): 39º50’N/20º00E 7. General location: Butrint is located in the south west corner of Albania, some 8 km to the south of the town of Saranda (pop. est. 20,000). The area is part of Vlora district. The site borders with Greece in the south and the Ionian Sea in the west. Seven small villages occur within the area of the proposed RAMSAR site: Blerimasi (pop. est. 400), Pllaka (pop. est. 600) and Dritasi (pop. est. 300) situated in the northern part. -
Critical Ecosystem Partnership Fund
Critical Ecosystem Partnership Fund Call for Letters of Inquiry No. 2 LARGE GRANTS Investment in the Mediterranean Basin Biodiversity Hotspot 1. Opening Date: Monday 25 June 2018 2. Submission Deadline: Friday 14 September 2018 3. Budget and Timeframe The minimum budget per project is US$20,000 and the maximum budget per project is US$150,000. Projects are expected to start on 1st March 2019 at the earliest and must be completed by 30th May 2022. 4. General information The Critical Ecosystem Partnership Fund (CEPF) is a joint initiative of l’Agence Française de Développement, Conservation International, the European Union, the Global Environment Facility, the Government of Japan, the John D. and Catherine T. MacArthur Foundation, and the World Bank. A fundamental goal is to ensure civil society is engaged in biodiversity conservation. The Mediterranean Basin Hotspot is the second largest hotspot in the world and the largest of the world’s five Mediterranean-climate regions. CEPF’s niche for investment in the Mediterranean was formulated through a participatory process that engaged civil society, donor and governmental stakeholders throughout the region. The resulting Investment Strategy (2017- 2022) is documented within the ecosystem profile (PDF – 31 MB). This investment strategy comprises of a series of strategic directions, broken down into investment priorities outlining the types of activities that will be eligible for CEPF funding. CEPF is inviting proposals in the form of letters of inquiry (LOIs) for large grants from non- governmental organizations, community groups, private enterprises, universities and other civil society organizations. Applicants are advised to read this call for proposals document in full and submit LOIs under the scope of this call, as described in Section 6. -
Climate Interactions in the Central Mediterranean Region During The
Manuscript Click here to view linked References 1 Human – climate interactions in the central Mediterranean region 2 during the last millennia: The laminated record of Lake Butrint 3 (Albania) 4 1,2* 3 4 5 Mario Morellón , Flavio S. Anselmetti , Daniel Ariztegui , Brunhilda 5 6,7 8 6 9 6 Brushulli , Gaia Sinopoli , Bernd Wagner , Laura Sadori , Adrian Gilli , 5 7 Arben Pambuku 8 9 1 Instituto de Geociencias (CSIC, UCM),Calle José Antonio Nováis, 2, 3ª planta, 3b. 10 Facultad de Ciencias Geológicas, Univ. Complutense, 28040 Madrid, Spain. 11 2 Swiss Federal Institute of Aquatic Science and Technology, Eawag, Ueberlandstrasse 12 133, CH-8600 Dübendorf, Switzerland. 13 3 Institute of Geological Sciences and Oeschger Centre of Climate Change Research, 14 University of Bern, Baltzerstrasse 1, CH-3012 Bern, Switzerland. 15 4 Department of Earth Sciences, University of Geneva, Rue des Maraîchers 13, CH- 16 1205 Geneva, Switzerland. 17 5 Albanian Geological Survey, Rruga e Kavajes, Nr. 153. Tirana, Albania 18 6Dipartimento di Biologia Ambientale, Sapienza University of Rome, Italy 19 7Dipartimento di Scienze della Terra, Sapienza University of Rome, Italy 20 8 Department of Geology and Mineralogy, University of Cologne, Cologne, Germany 9 21 Geological Institute, ETH Zurich, Sonneggstrasse 5, CH-8092 Zurich, Switzerland 22 23 24 *Corresponding author. E-mail address: [email protected] 1 25 ABSTRACT 26 Lake Butrint (39°47 N, 20°1 E) is a ca. 21 m deep, coastal lagoon located in SW 27 Albania where finely-laminated sediments have been continuously deposited during the 28 last millennia. The multi-proxy analysis (sedimentology, high-resolution elemental 29 geochemistry and pollen) of a 12 m long sediment core, supported by seven AMS 30 radiocarbon dates and 137Cs dating, enable a precise reconstruction of the environmental 31 change that occurred in the central Mediterranean region during the last ~4.5 cal kyrs 32 BP. -
Battling Water: the Frontiers of Archaeological Excavations at Butrint (–)
The Annual of the British School at Athens, , page of © The Council, British School at Athens, doi:./S BATTLING WATER: THE FRONTIERS OF ARCHAEOLOGICAL EXCAVATIONS AT BUTRINT (–) by David R. Hernandez University of Notre Dame This article examines the impact of sea level (water table) on archaeological research at Butrint (Bouthrotos/Buthrotum) from to . Rising relative sea levels over the past three thousand years have shaped the actions not only of its ancient inhabitants but also of its modern archaeologists, conditioning archaeological objectives, fieldwork and the interpretation of the archaeological record. Butrint’s first archaeologist, Luigi M. Ugolini, considered groundwater to be a detriment to archaeological research at the site. Subsequent archaeologists have viewed it as the limit of excavation. Battling water at Butrint, archaeologists have shared a universal perception of groundwater as an enemy and thereby have overlooked one of Butrint’s most important areas of archaeological research – its wetland and wet-site archaeology. The Roman Forum Excavations (RFE) Project undertook the first wet-site excavations at Butrint, reaching depths of up to four metres below the water table in stratigraphic excavations in the ancient urban centre. The results demonstrate that the ancient urban centre formed much later than is presently thought: the lower city emerged as dryland in the second half of the second century BC. Relative sea levels have increased since antiquity at many coastal regions in the Mediterranean, often submerging archaeological sites either partially or completely. Butrint is a case study that shows how sea level is inextricably tied to archaeological practice and interpretation at this major ancient Mediterranean seaport. -
Vegetation, Climate and Environmental History of the Last 4500 Years At
HOL0010.1177/0959683614561891The HoloceneSadori et al. 561891research-article2014 Research paper The Holocene 2015, Vol. 25(3) 435 –444 Vegetation, climate and environmental © The Author(s) 2014 Reprints and permissions: sagepub.co.uk/journalsPermissions.nav history of the last 4500 years at lake DOI: 10.1177/0959683614561891 Shkodra (Albania/Montenegro) hol.sagepub.com Laura Sadori,1 Marco Giardini,1 Elsa Gliozzi,2 Ilaria Mazzini,3 Roberto Sulpizio,4 Aurelien van Welden5 and Giovanni Zanchetta6 Abstract Three parallel overlapping cores have been taken in the Albanian side of Lake Shkodra (Albania/Montenegro). The chronological frame of the record, spanning approximately the last 4500 years, has been assessed using four radiocarbon dates and four well-known tephra layers of Italian volcanoes. Multidisciplinary analyses turned out to be decisive to understand environmental, climatic changes and human impact. Here, we focus on palynology. The humidity at Shkodra was always enough to allow the developing of a luxuriant arboreal vegetation. The pollen percentage diagram does not record important changes in terrestrial plants percentages. Arboreal pollen (AP) shows only a rather slight decrease, with ‘natural forests’ replaced by intensive cultivation of chestnut and walnut in the last seven/eight centuries. The rather minimal changes in composition and dominance are because of the fact that the pollen rain comes from different vegetation belts, from the Mediterranean to the alpine one. Two major periods of humidity are found, one at the base of the pollen concentration and influx diagram, before 4100 yr BP, the other at 1300 yr BP. Minima in pollen influx and concentration occurred soon before 4000, at ca. -
The Proposed Ramsar Area Has a Surface of 13500 Ha (See Attached Map)
Ramsar Site: 1290 - Butrint Ramsar Information Sheet March 2003 Additional information Physical features of the site: The proposed Ramsar area has a surface of 13500 ha (see attached map). The territory comprises a wide variety of landscape features from mountain to plain and from freshwater marsh to saltwater lagoons and rocky coast. The main wetland area comprises Lake Butrint, Lake Bufi and the areas of the Vurgu plain in the north (including reed beds) and Vrina-Mursia plain in the south (including a shingle bank and temporary freshwater marsh). This part represents a tectonic graben of the plioquaternary, with descending movements still in progress. Riverbeds are shallow and wide. Table 2. Physical parameters of Lake Butrint Total water surface 1600 ha. Total water volume 211 x 106 m³ Greatest depth 21.5 m Mean depth 11 m North-south dimension 7.1 km East-west dimension 3.2 km Lake Butrint is surrounded by different ranges of mountains and hills: Mile mountain range to the east (845 m), Sotira to the west (240 m) and Stillo to the south (240 m). This higher terrain compliments the lower wetland areas by providing environmental corridors and areas were there is less human disturbance for wildlife. Physical features of the catchment area: The catchment area of the proposed Ramsar Site is extremely large (information not available for the surface of the catchment area) compared to the surface of the proposed site itself. It is similar to the one of the rivers pouring in the area, i.e., Bistrica, Kalasa and Pavllo. The upper part of the chatchment area of Bistrica and Kalasa is characterized by mountainous terrain, continues further down with hills and ends in Vurgu Plain. -
Tirana, Albania O the Country's Largest Museum. It Was Opened on 28
EUROPE A Albania National Historical Museum – Tirana, Albania o The country's largest museum. It was opened on 28 October 1981 and is 27,000 square meters in size, while 18,000 square meters are available for expositions. The National Historical Museum includes the following pavilions: Pavilion of Antiquity, Pavilion of the Middle Ages, Pavilion of Renaissance, Pavilion of Independence, Pavilion of Iconography, Pavilion of the National Liberation Antifascist War, Pavilion of Communist Terror, and Pavilion of Mother Teresa. Et'hem Bey Mosque – Tirana, Albania o The Et’hem Bey Mosque is located in the center of the Albanian capital Tirana. Construction was started in 1789 by Molla Bey and it was finished in 1823 by his son Ethem Pasha (Haxhi Ethem Bey), great- grandson of Sulejman Pasha. Mount Dajt – Tirana, Albania o Its highest peak is at 1,613 m. In winter, the mountain is often covered with snow, and it is a popular retreat to the local population of Tirana that rarely sees snow falls. Its slopes have forests of pines, oak and beech. Dajti Mountain was declared a National Park in 1966, and has since 2006 an expanded area of about 29,384 ha. It is under the jurisdiction and administration of Tirana Forest Service Department. Skanderbeg Square – Tirana, Albania o Skanderbeg Square is the main plaza of Tirana, Albania named in 1968 after the Albanian national hero Skanderbeg. A Skanderbeg Monument can be found in the plaza. Skanderbeg Monument – Skanderberg Square, Tirana, Albania o The monument in memory of Skanderbeg was erected in Skanderbeg Square, Tirana. -
Vegetation History and Palaeoclimate at Lake Dojran (FYROM/Greece)
Vegetation history and palaeoclimate at Lake Dojran (FYROM/Greece) during the Late Glacial and Holocene Alessia Masi1, Alexander Francke2,3, Caterina Pepe1, Matthias Thienemann2, Bernd Wagner2, and Laura Sadori1 1Department of Environmental Biology, Sapienza University, Rome, Italy 2Institute of Geology and Mineralogy, University of Cologne, Cologne, Germany 3Wollongong Isotope Geochronology Laboratory, School of Earth and Environmental Sciences, University of Wollongong, Wollongong, Australia Correspondence to: Alessia Masi ([email protected]) Abstract. A new high-resolution pollen and NPPs (Non-Pollen Palynomorphs) analysis has been performed on the sediments of Lake Dojran, a transboundary lake located at the border between Greece and Former Yugoslav Republic of Macedonia (FYROM). The sequence covers the last 12500 years and provides information on vegetational dynamics of the Late Glacial and Holocene for southern Balkans. A robust age-model, sedimentological, diatom, and biomarker analyses published previously 5 have been the base for a multi-perspective interpretation of the new palynological data. Pollen analysis revealed that the Late Glacial is characterized by steppic taxa with prevailing Amaranthaceae, Artemisia and Poaceae. The arboreal vegetation starts to rise after 11500 yr BP, taking a couple of millennia to be definitively attested. Holocene vegetation is characterized by the dominance of mesophilous plants. Quercus robur type and Pinus are the most abundant taxa followed by Quercus cerris type, Quercus ilex type and Ostrya/Carpinus orientalis. The first attestation of human presence can be presumed at 5000 yr 10 BP for the contemporary presence of cereals, Juglans and Rumex. A drop of both pollen concentration and influx together 18 with a δ Ocarb shift indicates increasing aridity and precedes clear and continuous human signs since 4000 yr BP.