Dracaena Ombet-MAP-Egypt Project
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This Keyword List Contains Indian Ocean Place Names of Coral Reefs, Islands, Bays and Other Geographic Features in a Hierarchical Structure
CoRIS Place Keyword Thesaurus by Ocean - 8/9/2016 Indian Ocean This keyword list contains Indian Ocean place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. For example, the first name on the list - Bird Islet - is part of the Addu Atoll, which is in the Indian Ocean. The leading label - OCEAN BASIN - indicates this list is organized according to ocean, sea, and geographic names rather than country place names. The list is sorted alphabetically. The same names are available from “Place Keywords by Country/Territory - Indian Ocean” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. For example, the first place name “Bird Islet” has a unique identifier of “00S073E0013”. From that we see that Bird Islet is located at 00 degrees south (S) and 073 degrees east (E). It is place number 0013 at that latitude and longitude. (Note: some long lines wrapped, placing the unique identifier on the following line.) This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Indian Ocean OCEAN BASIN > Indian Ocean > Addu Atoll > Bird Islet (00S073E0013) OCEAN BASIN > Indian Ocean > Addu Atoll > Bushy Islet (00S073E0014) OCEAN BASIN > Indian Ocean > Addu Atoll > Fedu Island (00S073E0008) -
Vascular Plant Survey of Vwaza Marsh Wildlife Reserve, Malawi
YIKA-VWAZA TRUST RESEARCH STUDY REPORT N (2017/18) Vascular Plant Survey of Vwaza Marsh Wildlife Reserve, Malawi By Sopani Sichinga ([email protected]) September , 2019 ABSTRACT In 2018 – 19, a survey on vascular plants was conducted in Vwaza Marsh Wildlife Reserve. The reserve is located in the north-western Malawi, covering an area of about 986 km2. Based on this survey, a total of 461 species from 76 families were recorded (i.e. 454 Angiosperms and 7 Pteridophyta). Of the total species recorded, 19 are exotics (of which 4 are reported to be invasive) while 1 species is considered threatened. The most dominant families were Fabaceae (80 species representing 17. 4%), Poaceae (53 species representing 11.5%), Rubiaceae (27 species representing 5.9 %), and Euphorbiaceae (24 species representing 5.2%). The annotated checklist includes scientific names, habit, habitat types and IUCN Red List status and is presented in section 5. i ACKNOLEDGEMENTS First and foremost, let me thank the Nyika–Vwaza Trust (UK) for funding this work. Without their financial support, this work would have not been materialized. The Department of National Parks and Wildlife (DNPW) Malawi through its Regional Office (N) is also thanked for the logistical support and accommodation throughout the entire study. Special thanks are due to my supervisor - Mr. George Zwide Nxumayo for his invaluable guidance. Mr. Thom McShane should also be thanked in a special way for sharing me some information, and sending me some documents about Vwaza which have contributed a lot to the success of this work. I extend my sincere thanks to the Vwaza Research Unit team for their assistance, especially during the field work. -
Restoration and Conservation of Deteriorated Arid Land by a Native Thorny Shrub Lycium Shawii
Journal of Agricultural Science and Technology A 7 (2017) 100-106 doi: 10.17265/2161-6256/2017.02.004 D DAVID PUBLISHING Restoration and Conservation of Deteriorated Arid Land by a Native Thorny Shrub Lycium shawii Modi Mohammed Ahmed and Ali Mohammed Al-Dousari Crisis Decision Program, Environment and Life Science Research Center, Kuwait Institute for Scientific Research, P.O. Box 24885, Safat 13109, Kuwait Abstract: Land degradation is of great concern in the desert environment of Kuwait, as it has a negative impact on the natural resources. In response to this situation, Kuwait conserves their natural environment by setting aside areas of significant natural ecosystem, such as wild life center at the Liyah area. The area suffered during the past four decades from severe environmental pressures due to the excessive exploitation of natural resources of sand and gravel as well as overgrazing and military activities. Re-vegetation and restoration programs were applied in the degraded areas in Liyah in December 2003. A large variety of native plants were used for the restoration, however, in this research, only one native perennial drought resistant plant Lycium shawii (Awsaj) was highlighted. Tissue cultured thorny shrub planted at experimental site showed high adaptation on gravel hill side with harsh field condition. Their survival rate was 100% under drip irrigation only 10% was the mortality rate due to improper fixation of irrigation system. The average length of the main stem and the number of branches gradually increased by year from 42 cm with three branches in 2011 to 170 cm with seven branches in 2014. -
University of Cape Town
The copyright of this thesis vests in the author. No quotation from it or information derived from it is to be published without full acknowledgementTown of the source. The thesis is to be used for private study or non- commercial research purposes only. Cape Published by the University ofof Cape Town (UCT) in terms of the non-exclusive license granted to UCT by the author. University Some consequences of woody plant encroachment in a mesic South African savanna Emma Fiona Gray Town Cape of Submitted in fulfilment of the requirements for a Master of Science Degree Supervisor UniversityProfessor William Bond Botany Department University of Cape Town Rondebosch 7701 March 2011 Acknowledgements My most sincere thanks go to my supervisor, Professor William Bond. There is no doubt that without his guidance, belief and support over the last two years I would still be sitting in front of a blank screen. Thanks for the passion, the inspiration and all the amazing opportunities. Thanks to Ezemvelo KZN Wildlife for allowing me to conduct my research in their park. Particular thanks go to Dr Dave Druce, for welcoming me into his research centre and giving me the staff and freedom I needed during my fieldwork. I am also extremely grateful to Geoff Clinning for his patience and willingness to help with all my data and GIS needs. Thanks to the Zululand Tree Project for logistical support during my field work. To my field assistants, Njabulo, Bheki and Ncobile, for their uncomplaining hard work in the most trying conditions. Without them I would have no data. -
New Records of the Family Chalcididae (Hymenoptera: Chalcidoidea) from Egypt
Zootaxa 4410 (1): 136–146 ISSN 1175-5326 (print edition) http://www.mapress.com/j/zt/ Article ZOOTAXA Copyright © 2018 Magnolia Press ISSN 1175-5334 (online edition) https://doi.org/10.11646/zootaxa.4410.1.7 http://zoobank.org/urn:lsid:zoobank.org:pub:6431DC44-3F90-413E-976F-4B00CFA6CD2B New records of the family Chalcididae (Hymenoptera: Chalcidoidea) from Egypt MEDHAT I. ABUL-SOOD1 & NEVEEN S. GADALLAH2,3 1Zoology Department, Faculty of Science (Boys), Al-Azhar University, P.O. Box 11884, Nasr City, Cairo, Egypt. E-mail: [email protected] 2Entomology Department, Faculty of Science, Cairo University, Giza, Egypt 3Corresponding author. E-mail: [email protected] Abstract In the present study, a checklist of new records of the family Chalcididae of Egypt is presented based on a total of 180 specimens collected from 24 different Egyptian localities between June 2011 and October 2016, mostly by sweeping and Malaise traps. Nineteen species as well as the subfamily Epitraninae and the genera Bucekia Steffan, Epitranus Walker, Proconura Dodd, and Tanycoryphus Cameron, are newly recorded from Egypt. A single species previously placed in the genus Hockeria is transferred to Euchalcis Dufour as E. rufula (Nikol’skaya, 1960) comb. nov. Key words: Parasitic wasps, Chalcidinae, Dirhininae, Epitraninae, Haltichellinae, new records, new combination Introduction The Chalcididae (Hymenoptera: Chalcidoidea) is a medium-sized family represented by more than 1500 described species in 93 genera (Aguiar et al. 2013; Noyes 2017; Abul-Sood et al. 2018). A large number of described species are classified in the genus Brachymeria Westwood (about 21%), followed by Conura Spinola (20.3%) (Noyes 2017). -
Southern Egyptian Red Sea Bays, Offshore Reefs and Islands IMMA
Southern Egyptian Red Sea Bays, Offshore Reefs and Islands IMMA Summary The Egyptian Red Sea waters south of Marsa Alam encompass diverse marine habitats, including coastal bays, offshore reefs, and islands, supporting populations of nine marine mammal species. The northern parts of the area feature habitats used by Area Size resident dugong (Dugong dugon) and spinner 19,425 km2 dolphins (Stenella longirostris).¬† These populations have become the target of popular, intense, and in Qualifying Species and Criteria many cases, unregulated “swim-with” tourism operations that take place in their resting and calving areas. Conversely, the southern portion of the area is Dugong – Dugong dugon remote and less affected by coastal development Criteria A, B1 and tourism. Scientific research on marine mammals in this area commenced in the early 2000s and has Indian Ocean humpback dolphin – Sousa plumbea contributed significantly to the understanding of Criterion A spinner dolphin and dugong behaviour, as well as species occurrence, distribution and ecology in the Risso’s dolphin – Grampus griseus region. Criterion B1 Description Spinner dolphin – Stenella longirostris Criteria B1, C1 The IMMA is located in Egypt’s Red Sea Governorate, an administrative division of Egypt including most of Indo-Pacific bottlenose dolphin – Tursiops aduncus the Red Sea coastal area, from the Suez Canal to the Criterion B1 border with Sudan. It encompasses the entire Marsa Alam administrative region, which ranges from Port Ghalib in the north (25.6°N, 34.1°E) to Shalatin in the Common bottlenose dolphin – Tursiops truncatus south (23.5°N; 33.5°E), and includes a range of diverse Criterion B2 marine and terrestrial habitats. -
Arbor Day in South Africa Champion Trees Project How Can You Help To
What about planting a tree? Raise awareness of South Africa’s urban and rural greening initiatives. Trees and climate change Promoting better understanding of trees, particularly indigenous trees The idea for Arbor Day originally came and fruit trees. It is now well known that global climate is changing and that it is likely to from Nebraska. When visiting the state continue changing for many years to come. Climate change brings about today one would not find evidence that Highlight the important role trees play in sustainable development and unusual weather, droughts, floods, melting of the permanent ice of the the area was once a treeless plain. the livelihoods of people and their environment . north and south poles as well as rising ocean levels. All this is the result Yes it was a lack of trees there that led of air pollution caused by human activities. to the founding of Arbor Week Encourage communities to participate in various greening activities One of the main pollutants responsible for this phenomenon is the in the 1800s. within their own surroundings. greenhouse gas Carbon Dioxide (CO2). Greenhouse gasses have the ability to trap the sun’s heat in the atmosphere and so prevent the earth Arbor Day in South Africa Furthermore, the aim is to encourage people to plant trees at various from cooling down. This is referred to as the greenhouse effect, which is places so that they are not lost to us and future generations. Indigenous important for maintaining life on earth, but which is also very dangerous Historically, South Africa did not have a culture of tree planting and it was trees are a heritage to our society. -
Exhibition Cataloque --> Download
Les joyaux cachés de l'Egypte Le Centre Culturel Egyptien à Paris CCEP MAI 2018 Sherif Lotfy Je suis un ancien hôtelier, qui a choisi d’entrer dans le monde des entreprises et a commencé de diriger sa propre entreprise en 1993. En effet, mon intérêt pour la photographie n’a pas cessé de grandir jusqu’a qu’elle a construit une auto-expression complète. Mes photographies sont le reflet de ma vision du monde qui m’entoure, et comment je souhaite être une source d’inspiration ’aux autres à rêver librement. Malgré l’éloge qui m’est fait de façon régulière, je ne me considère pas comme un photographe, mais un rêveur qui traverse un chemin magnifique. I am an ex hotelier, who chose to go into entrepreneurship and had been running my own business since 1993. My love for photography has been growing for decades, building up a complete self-expression. My photographs express how I perceive the world around me, how I see it through my own eyes, and how I wish to inspire my fellow human beings to open the door and dream freely.. Despite the praise that I always receive, I do not consider myself a photographer ... rather a dreamer undergoing an amazingly beautiful path. Amr El Kady Hazem El Mihy Je suis un photographe libre, j’ai fait plusieurs exposition en Egypte Je suis un artiste et un photographe d’Alexandrie. En effet, j’ai et à l’étranger et j’ai participé avec d'autres photographes à de hérité cette passion de photographie de mon père et pour cela j’ai nombreuses autres expositions. -
Late Oligocene–Early Miocene Nukhul Sequence, Gulf of Suez and Red Sea
GeoArabia, 2012, v. 17, no. 1, p. 17-44 Gulf PetroLink, Bahrain Late Oligocene–Early Miocene Nukhul Sequence, Gulf of Suez and Red Sea Moujahed I. Al-Husseini ABSTRACT Egypt’s Late Oligocene–Early Miocene Nukhul Formation was deposited during the earliest geological evolution of the Gulf of Suez and Red Sea Rift System. In this paper the formation is cast as a depositional sequence based on published sections, and correlated across the Gulf of Suez and northern Red Sea. The resulting correlations indicate that deposition was initiated in local grabens by the oldest continental clastics of the lower member of the Nukhul Formation, the Shoab Ali Member. The member overlies the Suez Rift Unconformity, a term proposed for the entire Red Sea. Although this member can attain a thickness of ca. 1,000 ft (305 m) locally in grabens, it is generally absent over horsts. Sedimentary facies of the member are interpreted as indicating an initial alluvial-fluvial setting that evolved to an estuarine and coastal setting. The upper part of the Nukhul Formation records a regional shallow-marine transgression, which can be subdivided into three correlative Upper Nukhul members. These sediments are absent over the highest paleo-horsts, but reach up to 900 ft (275 m) in thickness in grabens. In the southern Gulf of Suez the Ghara Member represents the Upper Nukhul members. In places it consists of four cycles, each of which starts with an anhydrite bed and is overlain by deposits of mixed lithology (sandstone, marl, and limestone). The four cycles are interpreted as transgressive-regressive subsequences that can be correlated across ca. -
Geology, Geochemistry and Radioactivity of Granitic and Volcanic Rocks at Hadarba Area, South Eastern Desert, Egypt
International Research Journal of Geology and Mining (IRJGM) (2276-6618) Vol. 6(2) pp. 038 - 052, June, 2016 DOI: http://dx.doi.org/10.14303/irjgm.2016.106 Available online http://www.interesjournals.org/irjgm Copyright©2016 International Research Journals Full Length Research Paper Geology, Geochemistry and Radioactivity of Granitic and Volcanic Rocks at Hadarba Area, South Eastern Desert, Egypt Hassan A. A. Shahin*, Masoud S. Masoud and Moustafa M. Bayoumi Nuclear Materials Authority, P. O. Box 530, El-Maadi, Cairo, Egypt Corresponding author email address: [email protected] ABSTRACT The present work deals with geology, geochemistry, radioactivity and tectonic environment of the granitic and volcanic rocks at Hadarba area, South Eastern Desert of Egypt. The granitic rocks comprise tonalite-granodiorite and monzogranite, while volcanic rocks include rhyolite, rhyodacite anddacite. These rocks are characterized by high concentrations of SiO2, Na2O, Fe2O3, K2O, Zr, Nb and Y but low in MgO, CaO, Cr, Ni, Sr, Ga and V. Field studies indicate that Dokhan volcanics extrude both tonalite-granodiorite and monzogranite with sharp contact forming a thick successive sequence of laminated acid lava flows, crystal lapilli tuffs and agglomerates. They range in composition from rhyolite, rhyodacite to dacite. Shear zone comprise lines–arranged intrusions trending NE-SW direction were recorded north Gabal Hadarba and extends for about 2.3 km in length with a width reaches up to 10 meter. These lines–arranged intrusions include quartz vein, microgranite and basic dykes. These shear zones cut through monzogranite. Petrochemical studies and tectonic discrimination diagrams for the monzogranite reveal that it is classified as granite developed in the within-plate tectonic environment, while Dokhan volcanics are classified as rhyolite and dacite developed in the immature island arcs and active continental margin environments.Field radiometric measurements of these granitic and volcanic rocks reveal low uranium and thorium contents. -
Euclea Undulata Herba
EUCLEA UNDULATA HERBA Definition alternate, leathery-granular in texture, often rust-coloured when young due to the Euclea Undulata Herba consists of the fresh presence of red-brown glands, entire, or dried leaves of Euclea undulata Thunb. obovate to oblanceolate, with undulate var. myrtina (Burch.) Hiern and var. undulata margin; flowers (Dec-Apr) white to cream, (Ebenaceae). fragrant, borne in axillary racemes of 5-7 individuals, ovary scaly; fruit a globose Synonyms fleshy berry 4-6mm in diameter, red becoming purple or black when ripe. E. myrtina Burch. E. undulata Thunb. Vernacular names Ghwarrie (Afr.), guarri, umgwali (Xh.); mokoerekoere (Se.); gwanxe, inkunzane, umshekizane, umbophanyamazane (Z); ihlangula (Sd) Description1 Macroscopical Figure 2 – line drawing Figure 1 – Live plant Erect dense twiggy evergreen dioecious shrubs, 0.75-5m high, or trees to 7m high, stem or trunk 2-15 cm in diameter, bark grey scaly; branchlets much divided and densely covered with leaves; leaves subopposite to 1 De Winter, B. (1963). The genus Euclea. Flora of Southern Africa 26: 82-99. Microscopical Province to Komga in the Eastern Cape while var. myrtina (small leaved ghwarrie) is found in Namibia, the Northern Cape, Northwest and Northern Provinces, entering KwaZulu-Natal through Mpumalanga and Swaziland. Quality standards Identity tests Thin layer chromatography on silica gel using as solvent a mixture of toluene:diethyl ether:1.75M acetic acid (1:1:1). Reference compound cineole (0,1% in chloroform). Method according to Appendix 2a. Rf values -
Egyptian National Action Program to Combat Desertification
Arab Republic of Egypt UNCCD Desert Research Center Ministry of Agriculture & Land Reclamation Egyptian National Action Program To Combat Desertification June, 2005 UNCCD Egypt Office: Mail Address: 1 Mathaf El Mataria – P.O.Box: 11753 El Mataria, Cairo, Egypt Tel: (+202) 6332352 Fax: (+202) 6332352 e-mail : [email protected] Prof. Dr. Abdel Moneim Hegazi +202 0123701410 Dr. Ahmed Abdel Ati Ahmed +202 0105146438 ARAB REPUBLIC OF EGYPT Ministry of Agriculture and Land Reclamation Desert Research Center (DRC) Egyptian National Action Program To Combat Desertification Editorial Board Dr. A.M.Hegazi Dr. M.Y.Afifi Dr. M.A.EL Shorbagy Dr. A.A. Elwan Dr. S. El- Demerdashe June, 2005 Contents Subject Page Introduction ………………………………………………………………….. 1 PART I 1- Physiographic Setting …………………………………………………….. 4 1.1. Location ……………………………………………………………. 4 1.2. Climate ……...………………………………………….................... 5 1.2.1. Climatic regions…………………………………….................... 5 1.2.2. Basic climatic elements …………………………….................... 5 1.2.3. Agro-ecological zones………………………………………….. 7 1.3. Water resources ……………………………………………………... 9 1.4. Soil resources ……...……………………………………………….. 11 1.5. Flora , natural vegetation and rangeland resources…………………. 14 1.6 Wildlife ……………………………………………………………... 28 1.7. Aquatic wealth ……………………………………………………... 30 1.8. Renewable energy ………………………………………………….. 30 1.8. Human resources ……………………………………………………. 32 2.2. Agriculture ……………………………………………………………… 34 2.1. Land use pattern …………………………………………………….. 34 2.2. Agriculture production ………...……………………………………. 34 2.3. Livestock, Poultry and Fishing production …………………………. 39 2.3.1. Livestock production …………………………………………… 39 2.3.2. Poultry production ……………………………………………… 40 2.3.3. Fish production………………………………………………….. 41 PART II 3. Causes, Processes and Impact of Desertification…………………………. 43 3.1. Causes of desertification ……………………………………………….. 43 Subject Page 3.2. Desertification processes ………………………………………………… 44 3.2.1. Urbanization ……………………………………………………….. 44 3.2.2. Salinization………………………………………………………….