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Ecologia Mediterranea

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elong to two major geomorphological habitat<br />

types: small wadis that cut their way down<br />

djebel (mountain) slopes and large wadi beds<br />

in valleys at low altitude (800 to 1200 m).<br />

Climatic characteristics<br />

The Ahaggar is under the influence of two climatic<br />

regimes: a <strong>Mediterranea</strong>n regime from<br />

the north and a tropical one from the south.<br />

The climate of the study area is characterised<br />

by low and irregular rainfall (Daget & Djellouli<br />

1992). The mean annual rainfall calculated<br />

over a period of 63 years was 46.6 mm.<br />

The desertic character of the climate is clearly<br />

illustrated by the ombrothermic diagram (Figure<br />

2). Temperatures are characterised by very<br />

high daily thermal amplitude, frequently<br />

reaching 35 o C (Dubief 1959). The mean temperature<br />

of the hottest month does not exceed<br />

35 o C while mean minimum temperatures can<br />

be as low as – 5 o C in winter.<br />

Sampling strategy<br />

During the sampling period, between 1990<br />

and 1992, 190 relevés were recorded from the<br />

different plant communities of the Tamanrasset<br />

region applying the Braun-Blanquet<br />

method (Gehu & Rivas Martinez 1981). Sampling<br />

strategy was based on quadrats recorded<br />

on floristically and geomorphologically<br />

homogeneous sites (Benhouhou et al. 2003a).<br />

According to topography, quadrat surface has<br />

varied in previous studies in desertic regions<br />

between 100 m 2 and 1000 m 2 (Abd El-Ghani<br />

& Amer 2003; Ali et al. 2000; Benhouhou et<br />

al. 2003a; Bornkamm & Kehl 1990;<br />

Brinkmann et al. 2009; Fossati et al. 1998;<br />

Hegazy et al. 1998). For our sampling set, we<br />

chose to use a standard relevé size of 200 m 2<br />

as applied in the Ahaggar by Quézel (1954).<br />

Topography, soil texture and altitude were the<br />

main determinants for the choice of sampling<br />

sites: gravelly wadis, sandy wadis, smaller<br />

affluent wadis, outwash zones, mountain<br />

slopes with boulders and crevices. Our sampling<br />

sites are located north-east, north-west,<br />

south and south-west of Tamanrasset in the<br />

wadis of the following massifs: Ahléheg,<br />

Adrar Heggueghene, Ti-n-Tourdi, Tahelgha,<br />

Touf Admer and Alemeda (Figure 3).<br />

ecologia mediterranea – Vol. 38 (2) – 2012<br />

Data analyses<br />

Plant communities in the Tamanrasset region, Ahaggar, Algeria<br />

Figure 2 – Ombrothermic diagram of Bagnouls and Gaussen<br />

for the Tamanrasset station for the period 1970-2008.<br />

Numerical analysis applying ordination techniques<br />

to reduce the complex data set and<br />

seek major ecological gradients responsible<br />

for floristic variation is widely used in stud-<br />

Figure 3 – Main wadis, sampling sites and localisation of the six identified<br />

plant communities in the region of Tamanrasset.<br />

69

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