Desert Roadside Vegetation in Eastern Egypt and Environmental Determinants for Its Distribution
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PHYTOLOGIA BALCANICA 19 (2): 233 – 242, Sofia, 2013 233 Desert roadside vegetation in eastern Egypt and environmental determinants for its distribution Monier M. Abd El-Ghani1, Fawzy M. Salama2 and Noha A. El-Tayeh3 1 Botany Department, Faculty of Science, Cairo University, Egypt 2 Botany Department, Faculty of Science, Assiut University, Egypt, e-mail: [email protected] (corresponding author) 3 Botany Department, Faculty of Science (Qena), South Valley University, Egypt Received: September 24, 2012 ▷ Accepted: June 18, 2013 Abstract. The purpose of this study was to describe the flora and vegetation at Qift-Qusier roadsides in the central part of the Eastern Desert of Egypt, and to relate floristic composition to edaphic conditions. A total of 61 species (28 annuals and 33 perennials) belonging to 50 genera and 27 families were recorded. On the basis of their presence values, classification of the 61 species recorded in 43 stands by cluster analysis yielded six vegetation groups. The results of CCA ordination indicated that the soil organic matter, Na, K, Ca, and pH were the most important factors for distribution of the vegetation pattern along the road verges in the study area. The DCA and CCA results suggested a strong correlation between vegetation and the measured soil parameters. Key words: arid environments, Egypt, flora, multivariate analysis, roadside vegetation, soil-vegetation relationship IIntroductionntroduction The plant communities of roadside vegetation are influenced not only by anthropogenic factors but al- The Eastern Desert of Egypt extends between the Nile so by geographical differentiation, physiography and Valley and the Red Sea. It is traversed by numerous topography (Ullmann & al. 1990). The advantage of canyon-like depressions (wadis) running to the Red roadsides for study of species and vegetation perfor- Sea or to the Nile Valley and the Red Sea coast. The mance along environmental gradients is widely rec- Qift-Qusier road connects Qift city on the Nile Valley ognized (Ullmann & Heindl 1989; Wilson & al. 1992). with the city of Qusier on the Red Sea coast. Such studies are well-documented in North Ameri- Road construction exercises a major anthropogen- ca (Lausi & Nimis 1985), Europe (Stottele & Schmidt ic impact on the composition of the flora and vege- 1988; Heindl & Ullmann 1991), North Africa (Sharaf tation (Sharaf El-Din & Shaltout 1985; Holzapfel & El-Din & Shaltout 1985; Shaltout & Sharaf El Din 1988; Schmidt 1990). Construction and use of highways, Abd El-Ghani 1998, 2000), Saudi Arabia (Batanouny tracks, railways, and airports involves many chang- 1979; Fayed & Zayed 1989; Abd El-Ghani 1996), the es; some of them direct and others indirect. Direct in- Judean Desert (Holzapfel & Schmidt 1990), and in fluences include destruction of the existing habitats New Zealand (Ullmann & al. 1995). and provision of new ones with special characteristics. In Egypt, desert highways and agricultural roads These are more or less continuous stretches of open that traverse the cultivated areas are adequately inter- habitats covering hundreds of miles and forming an connected. Generally, the present road network totals extensive network, with opportunities for rapid colo- 41.300 km, of which 19.6 % are in the Sinai Peninsula, nization and spread. followed by those in the Nile Delta (18.7 %) and Nile 234 El- Ghany M. & al. • Roadside vegetation in central Eastern Desert, Egypt Valley (15.7 %), while the lowest percentage (8 %) is in and wadi deposits), Pliocene deposits (including la- the Western and Eastern Deserts of the country (Abd custrine sediments representing the Durri Formation El-Ghani & El-Sawaf 2005). which is composed of marlstone and mudstone), an The purpose of this study is to describe the road- Upper Cretaceous/Lower Tertiary succession tilted side flora and vegetation of Qift-Qusier road in the towards the Nile Valley (West), basement complexes central part of the Eastern Desert of Egypt, and to re- (representing the Red Sea Mountain Chain and com- late floristic composition to soil properties. posed of igneous and metamorphic rocks). Detailed elogical and geomorphological features are described MMaterialaterial andand methodsmethods by Ismaiel & al. (2012). The stands of the present study were chosen when- ever some considerable vegetation cover was encoun- Qift-Qusier road extends for about 180 km from Qift tered. The stands were studied twice: in September city in the west, along the Nile Valley, to Qusier city 2010 (at the end of the hottest season) and in March in the east at the Red Sea coast (Fig. 1). The road 2011 (at the end of the coldest season). Multivariate crosses several wadis that run from the higher Red analysis was applied to analyse the vegetation of the Sea Zountain Chain to the west (Nile Valley) and to stands. Forty-three stands were found satisfactory to the east (Red Sea coast). The margin of the moun- represent the roadside vegetation and were geo-refer- tain chain has a strongly marked north-northwest- enced by GPS technique. Sixty-one plant species were ern orientation. Elevation of the Red Sea Mountain collected, identified and deposited at the Her barium Chain in the study area ranges from 500 m to 600 m, of the Botany Department, Assiut University. Dupli- in contrast to the elevation of sedimentary rocks ar- cates were checked for identification and also depos- ea at both sides of the mountain chain (to the west ited at the Cairo University Herbarium. The record- and east of it), which ranges from 0 m to 200 m (Said ed species were classified according to their life forms 1962) . (Raunkiaer 1937; Hassib 1951). The number of spe- According to Abu Al-Izz (1971), the exposed sedi- cies within each life form was expressed as percent- ments and rocks along this road from west (Qift city) age of the total number of species in the study area. to east (Qusier city) are Quaternary sediments (in- Taxonomic nomenclature followed Täckholm (1974); cluding the Nile deposits, alluvial sands and gravels Cope & Hosni (1991); El Hadidi & Fayed (1995) and Fig. 1. Location map of Qift -Qusier road in the Eastern Desert of Egypt; the stands are given by their numbers. Phytol. Balcan. 19(2) • Sofia • 2013 235 Boulos (1995, 1999, 2000, 2002). Analysis of phyto- RResultsesults geographical ranges was carried out according to Zo- hary (1966, 1972), Abd El-Ghani (1981 & 1985) and FFloristicloristic analysisanalysis andand biologicalbiological sspectrumpectrum Hassan (1987). Three soil samples were collected from each stud- A total of 61 species (28 annuals and 33 perennials) ied stand and then pooled together to form one com- belonging to 50 genera and 27 families were recorded. posite sample. Soil texture was determined by the hy- The largest families were Fabaceae (8), Zygophyllaceae drometer method, and organic matter content was (7), Asteraceae, Brassicaceae and Poaceae (6 for each), estimated by drying and then ignition at 600 °C for Asclepiadaceae and Resedaceae (3 for each), Amaran- 3h (Sparks & al. 1996). Soil reaction (pH) and electric thaceae and Cleomaceae (2 for each). They constituted conductivity were evaluated in 1:5 soil-water extract, about 70.5 % of the recorded species, and represent- using a glass electrode pH-meter and electric conduc- ed most of the floristic structure in the Eastern De- tivity meter, respectively. Estimation of chlorides was sert of Egypt (Abd El-Ghani 1998; Salama & al. 2012). carried out by titration methods (Hazen 1989), sul- Eighteen families were represented by only one spe- phates were determined turbidimetrically, according cies. Fagonia was the largest genus represented by four to Verma & al. (1977). Calcium and magnesium were species (Table 1). determined by Upadhyay & Sharma (2005) method, while flame photometer technique was applied for de- Table 1. Floristic composition, presence value (P %), life forms (L.F), and chorology of the recorded species in the studied area. termination of sodium and potassium (Jackson 1962). Per = Perennials, Ann = Annuals, Ph = Phanerophytes, H = Available phosphorus was gauged calorimetrically, as Hemicryptophyte, Ch = Chemaephytes, Th = Theophytes, Cr = Cryptophytes, G = Geophytes, SA = Saharo-Arabian, SZ = Sudano- described by Watanabe & Olsen (1965). Zambezian, IT = Irano-Turanian, ME = Mediterranean, PAL = Classification and ordination methods were ap- Palaeotropical, PAN = Pantropical, COSM = Cosmopolitan. plied as multivariate analysis techniques. Cluster anal- Species Duration Chorology L.F P% ysis was used to classify the floristic data matrix of Amaranthaceae 43 stands and 61 species, with the help of Commu- Aerva javanica (Burm. f.) Juss. Per SA+SZ Ch 9.30 nity Analysis Package (CAP) version 1.2 (Henderson ex Schult. Amaranthus graecizans L. Per ME+IT Ch 2.33 & Seaby, 1999), using squared Euclidean distance dis- Asclepiadaceae similarity matrix with minimum variance as agglom- Calotropis procera (Aiton) W.T. Per SA+SZ Ph 6.98 eration criterion (Orloci 1978). Computer program Aiton CANOCO 4.5 (Ter Braak 2003) was used for all ordi- Leptadenia pyrotechnica Per SA+SZ Ph 4.65 (Forssk.) Decne. nation analyses; whereas computer program SPSS 10.0 Pergularia tomentosa L. Per SA+SZ Ch 4.65 (SPSS 1999) was used for all statistical treatments. De- Asteraceae trended Correspondence Analysis (DCA) was applied Cotula cinerea Delile Ann SA Th 9.30 to check the magnitude of change in species compo- Ifloga spicata (Forssk.) Sch. Bip. Ann SA Th 2.33 sition along the first axis. The default settings of Ca- Launaea cassiniana Ann SA Th 9.30 nonical Correspondence Analysis (CCA) were used to L. nudicaulis (L.) Hook. f. Per SA+IT H 2.33 relate directly the vegetation data to the correspond- Pulicaria incisa (Lam.) DC. Ann SA H 16.28 ing measured soil parameters (Ter Braak 2003). Elec- P. undulata (L.) C. A. Mey Per SA H 41.86 tric conductivity and magnesium were excluded from Boraginaceae the analysis as high inflation factors. Therefore, CCA Trichodesma africanum (L.) R.Br. Ann SA+SZ Ch 27.91 Brassicaceae was performed with 12 soil variables: coarse sand, Diplotaxis acris (Forssk.) Boiss.