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Vol. 32 – 2006 - Ecologia Mediterranea

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disturbance degree on Noy-Meir types? (iii)<br />

What is the impact of seasonal drought and<br />

disturbance degree on the CSR species strategies<br />

(Grime types)?<br />

Material and Methods<br />

Studied zone<br />

El Ouara communal rangelands<br />

El Ouara region is a part of Presaharian<br />

Tunisia following Floret and Pontanier’s definition<br />

(1982); this region corresponds<br />

roughly to the Tunisian part of the lower arid<br />

zone of North-Africa, comprised between the<br />

isohyets of 100 and 200 mm of annual rainfall<br />

(Figure 1). Rainfall pattern and temperature<br />

regime are <strong>Mediterranea</strong>n. The rainfall<br />

(256 mm) recorded in Sidi Toui National Park<br />

during the studied period (from fall 2003 to<br />

spring 2004) exceeds the annual averages of<br />

the region (100 mm). The unique land use of<br />

the area is rangeland. Topographically, this<br />

region is mainly composed of vast encrusted<br />

glacis with a thin sandy top layer (CNEA<br />

1991). The vegetation, essentially constituted<br />

of dwarf shrub steppe with perennial grasses,<br />

covers about 12%, 23% and 37% during a dry,<br />

medium and rainy year, respectively. Potential<br />

productivity, which varies with dominant<br />

plant species, is between 15 and 60 UF ha -1<br />

ecologia mediterranea <strong>–</strong> <strong>Vol</strong>. <strong>32</strong> <strong>–</strong> <strong>2006</strong><br />

A preliminary overview of the effects of seasonal drought and animal pressure around watering points<br />

on plant species using adaptative strategy analyses in the Tunisian arid zone<br />

an -1 (CNEA 1991) with 1UF: the equivalent<br />

of the energy produced by 1 kg of barley.<br />

Watering points<br />

Three watering points situated in El Ouara<br />

communal rangeland were retained for this<br />

study. These wells differ by the duration of<br />

exploitation, their geographical locations, the<br />

nature of surrounding vegetation and the grazing<br />

pressures. The first watering point (well<br />

1, exploited for 150 years) is located in the<br />

North of the studied zone, the second (well 2,<br />

exploited for 100 years) and the third (well 3,<br />

exploited for 5 years) are located in the south<br />

of Sidi Toui National Park. Well 1 is located<br />

on a stony soil with truncated top layer and<br />

surfacing rock due to erosion with plants,<br />

such as Anthyllis sericea Lag. subsp. henoniana<br />

(Coss.) Maire and Gymnocarpos decander<br />

Forssk. The east of this watering point is<br />

occupied by Stipagrostis pungens (Desf.) de<br />

Winter and Hammada schmittiana (Pomel)<br />

Iljin. Wells 2 and 3 are located on a sandy<br />

substratum with plants, such as S. pungens<br />

and H. schmittiana. A. sericea is absent there<br />

because of soil characteristics.<br />

Data collection<br />

Four transects were laid out in the four cardinal<br />

directions and sampling points were<br />

located at 250 m, 500 m, 1 km and 2 km from<br />

each watering point (Figure 1). The choice of<br />

Figure 1 <strong>–</strong> Location of the three studied watering points (W1 = Well 1; W2 = Well 2; W3 = Well 3),<br />

Sidi Toui National Park and the sampling design around them.<br />

300 mm<br />

200 mm<br />

100 mm<br />

100 mm<br />

W1<br />

Sidi Toui<br />

W2<br />

W3<br />

200 mm<br />

0 50 100 Km 0 30 60 Km 0 1 2 Km<br />

W<br />

41

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