Protected Areas and World Heritage Programme

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Protected Areas Programme

COUNTRY EGYPT

NAME El Omayed Protected Area, OPA (Experimental Research Area)

MANAGEMENT CATEGORY I (Scientific reserve);
IX (Biosphere reserve)

BIOGEOGRAPHICAL PROVINCE 2.18.07 (Sahara)

GEOGRAPHICAL LOCATION The Omayed is situated in the Mediterranean coastal desert region of north western Egypt, 7km south of Omayed village and 80km west of Alexandria. 30°45'N, 29°12'E.

DATE AND HISTORY OF ESTABLISHMENT Accepted by Unesco as a Biosphere reserve in October 1981 after having been protected since 1974 by REMDENE. The Governor of Matrouh recognised and designated the site at the same time as the Biosphere designation. Official national recognition of the site was made under Law 102 of 1983 and was instituted by Prime Ministerial decree in July 1986 (Ghabbour, 1986).

AREA 1,000ha (100ha core area)

LAND TENURE State ownership (rented by REMDENE)

ALTITUDE Sea-level to 110m

PHYSICAL FEATURES The site is situated on the Mediterranean Sahara coast, extending inland along the Gebel Mariut-Khahm El-Eish Depression of the western desert. Geological formations are essentially Quaternary and Tertiary in origin. The coast consists of Holocene beach deposits and sand dune accumulations. The pink oolitic limestones are of Pliocene-Pleistocene origin. The topographic relief is characterised by Pleistocene fossil rich white limestones forming successive undulations running more or less parallel to the coast. These undulations are in the form of calcareous rocky ridges (ancient dunes) alternating with depressions and varying in height from 10 to 60m. Five main habitat types exist at Omayed and these include: a) coastal calcareous dunes; b) inland ridges with relict soils; c) saline marsh depressions; d) non-saline depressions; and also e) inland plateaux (Ayyad and Ghabbour, 1986). The soils are generally sandy with a high percentage of calcium carbonate (Abdel-Razik et al., 1984).

CLIMATE Mediterranean arid sub-saharan bioclimate with typical low annual rainfall figures of 150-200mm. Temperatures vary from 12.7°C in January to 25.5°C in August. The area is included in Emberger's Mediterranean isoclimatic zones and is arid with mild winters and warm summers. There is some humidity influence from the nearby Mediterranean sea (Le Houérou, 1981).

VEGETATION The flora is characterised by xerophytic steppic vegetation of the Saharan Mediterranean region (Quezel, 1978, quoted by Ayyad and Ghabbour, 1986). The typical associations consist of Thymelaea hirsutae with Noaea mucronata (wet variant dominated by Asphodelus microcarpus and dry variant by Achillea santolina) or Anabisis articulata with Suaeda pruionosa (El Ghonemy and Tadros, 1970; Ayyad and Ghabbour, 1986). Dune vegetation consists of Ammophila arenaria, Euphorbia paralias, Pancratium maritimum, Elymus fancrus, Crucianella maritima, Echinops spinosissimus and Thymelaea hursuta on young dunes, whilst there are communities of Crucianella maritima and Ononis vaginalis on the older dunes (Ayyad and Ghabbour, 1986). The inland siliceous sands are dominated by communities of Urginea maritima, Plantago albicans and P. squarrosa. The shallow soiled inland ridges are more often characterised by either Thymelaea spp. and Gymnocarpos decadrum communities or by associations of Plantago albicans and Asphodelus microcarpa. In these communities local variations result from humidity differences: a) low moisture rocky ecosystems- Thymus capitatus, Globularia arabica and Dactylis glomerata; b) deep soil ecosystems - Asphodelus microcarpus, Hernaria hemistemon, Plantago albicans and Salvia lanigera; c) intermediate habitats - Gymnocarpos decandrum, Anabasis articulata, Helianthemum lippii and Pituranthos tortuosus (Ayyad and Ghabbour, 1986). The halophilous vegetation, typical of saline and marsh habitats, is dominated by Salicornia fruticosa, Cressa cretica, Atriplex halimus, Juncus rigidus, Arthrocnemum glaucum and Limonium echioides. In relatively deep water and under higher salinity conditions are also Suaeda monoica, Zygophyllum album, Limoniastrum monopetalum, Aeluropus lagopoides, Salsola tetrandra and Frankenia revoluta. In areas with deep water and low salinity are communities of Atriplex halimus, Hammada scoparia and Anabasis articulata (Ayyad and Ghabbour, 1986). The inland plateau vegetation includes Artemisia monosperma and Hammmada elegans associations (calcareous soils), Anabasis articulata and Hammada scoparia (shallow degraded soils) and Suaeda pruinosa and Salsola tetrandra communities (saline soils) (Ayyad and Ghabbour, 1986; El Ghonemy and Tadros, 1970).

FAUNA The mammals at Omayed include dorcas gazelle Gazella dorcas, a number of gerbils Gerbillus spp., the east Mediterranean endemic mole-rat Spalax leucodon, the fennec Vulpes zerda, red fox Vulpes vulpes, hare Lepus capensis and the North African endemic fat sand rat Psammomys obesus. There are 50-70 bird species including kestrel Falco tinnunculus and quail Coturnix coturnix and between 7-13 reptile and amphibian species such as horned viper Cerastes cerastes and also the tortoise Testudo graeca. Common insects are represented by the families Terrebrionidae, Scarabaeidae and Carabidae. There are also records of sand roach Heterogamia syriaca, harvester ants Messor spp. and a localised protozoa Acanthamoeba (Ayyad and Ghabbour, 1986).

CULTURAL HERITAGE No information

LOCAL HUMAN POPULATION Rain fed fig farms are present in the reserve. There are some scattered settlements and semi-nomad communities which have traditional land-use and grazing rights over the area (Ayyad and Ghabbour, 1986).

VISITORS AND VISITOR FACILITIES No information

SCIENTIFIC RESEARCH AND FACILITIES This area is one of the principal sites of research projects of SAMDENE (1974-1979) and its successor REMDENE (1979-). Projects include studies on soil, climate, flora and fauna. There are also monitoring projects specialising in meteorology, soil physics and behaviour of grazing animals. Controlled experiments are carried out on grazing densities and pressures in 75ha of land (varying from 25 to 50% grazing concentrations). The facilities at Omayed include a research station along with climatic station and accommodation for scientists (Ayyad and Ghabbour, 1986).

CONSERVATION MANAGEMENT The site has been designated because of its important assemblages of desert fauna and flora and for its research potential. The fenced core area of 100ha has been completely protected from grazing since 1974, and shows signs of regeneration. Three other fenced areas totalling 75ha have a controlled maximum level of 50 per cent grazing by domestic livestock. A major proportion of the remaining area is under traditional pasture land-use. A detailed management plan has recently been drawn up to include the whole protected area (Ayyad and Ghabbour, 1986).

Specific legislation prohibits "any action that would endanger living species or destroy landscapes within the protected area". Currently the site is rented and protected by the REMDENE project (Regional Environmental Management of Mediterranean Ecosystems of Northern Egypt).

MANAGEMENT PROBLEMS The main problem encountered in Omayed is the conflict in land-use especially since the area has long been used for grazing and agriculture. Tourist villages are currently being built on the adjacent coast and so may cause additional pressure. Other threats to the fauna include quail hunting by local people (Ayyad and Ghabbour, 1986).

STAFF There are two wardens solely concerned with patrolling the reserve. There is a total of 100 staff at the Omayed station (60 involved in research). Members of the local community also assist in running the reserve and monitoring research experiments (Ayyad and Ghabbour, 1986).

BUDGET No information

LOCAL ADMINISTRATION
· REMDENE, PO Box 589, Alexandria
· Faculty of Science, Alexandria University, Moharram Bey, Alexandria.

REFERENCES
Abdel-Razik, M., Abdel-Aziz, M. and Ayyad, M. (1984). Environmental gradients and species distributions in a transect at Omayed, Egypt. Journal of Arid Environments, 7: 337-352
Ayyad, M.A. (1973). Vegetation and environment of the western Mediterranean coastal land of Egypt. I: The habitat of sand dunes. Journal of Ecology, 61: 509-523.
Ayyad, M.A. and Ghabbour, S.I. (1986). Omayed Biosphere Reserve: History and Future Prospects. Mediterranean Biosphere reserves workshop. Florac, France, 8-12 September, 1986.
El Ghonemy, A.A. and Tadros, T.M. (1970). Socio-ecological studies of the natural plant communities along a transect, 200km long, between Alexandria and Cairo. Bulletin of the Faculty of Sciences, University of Alexandria, 10: 392-407.
Ghabbour, S.I. (1986). Species richness of soil fauna as criteria for priority choices of protected areas. Mediterranean Biosphere reserves workshop. Florac, France, 8-12 September, 1986.
Le Houérou, H.N. (1981). The arid bioclimates in the Mediterranean isoclimatic zone. Ecologia Mediterranean, 8: 103-114.
MAB. (1981). Omayed experimental research area. Biosphere reserves. MAB project No 8. Report.
Osborn, D.J. and Helmy, I. (1980). The contemporary land mammals of Egypt (including Sinai). Field museum of natural history new series, No. 5
Ozenda P. (1958). Flore du Sahara, septentrional et central. CRNS, Paris.

DATE January 1988
0353V



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