25.06.2013 Views

Walia Special Edition on the Bale Mountains (2011) - Zoologische ...

Walia Special Edition on the Bale Mountains (2011) - Zoologische ...

Walia Special Edition on the Bale Mountains (2011) - Zoologische ...

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

The aim of this study was to examine <strong>the</strong> soil, vegetati<strong>on</strong> and land use history in glades<br />

across <strong>the</strong> altitudinal gradient present in <strong>the</strong> Harenna to characterize <strong>the</strong>m by examining <strong>the</strong>ir soil<br />

properties, and comparing <strong>the</strong>se with soils in adjacent forest areas to investigate <strong>the</strong>ir origins.<br />

Methods<br />

Study site<br />

The Harenna forest (approximately, 39’- 40’ E, 6’- 7’ N) is located in <strong>the</strong> sou<strong>the</strong>rn part of <strong>the</strong><br />

<strong>Bale</strong> <strong>Mountains</strong> Nati<strong>on</strong>al Park (BMNP). The forest develops <strong>on</strong> an initially steep, <strong>the</strong>n gradual<br />

escarpment from ~3800 m a.s.l. to ~1600 m a.s.l.; <strong>the</strong> pr<strong>on</strong>ounced altitudinal gradient creates a<br />

variety of forest ecotypes (Hillman 1988; Niatu et al. 1989; Woldu et al. 1989).<br />

Mean annual rainfall at <strong>the</strong> sou<strong>the</strong>rn end of <strong>the</strong> forest (Delo Mena, ~1500 m a.s.l.) is 987 mm<br />

(Tesfaye et al. 2002) and reaches a maximum of 1145 mm in Koromi (3850 m a.s.l.) (Hillman 1988).<br />

There are typically eight rainy m<strong>on</strong>ths (March-October) and four dry m<strong>on</strong>ths (November-February)<br />

in a given year. The soils are derived from volcanic parent material, originating from Mesozoic<br />

erupti<strong>on</strong>s of Trappean lava giving trachitic, basaltic and riolitic bedrocks, toge<strong>the</strong>r with tuffs and<br />

agglomerates (Nigatu et al. 1989).<br />

Sampling design<br />

The study area was divided in to three sampling strata, located at different positi<strong>on</strong>s <strong>on</strong> <strong>the</strong><br />

toposequence, reflecting both altitudinal variati<strong>on</strong> and variati<strong>on</strong> of positi<strong>on</strong> al<strong>on</strong>g <strong>the</strong> directi<strong>on</strong> of<br />

groundwater movement (Fig. 1; 2400 m a.s.l., 1850 m a.s.l., 1750 m a.s.l.; hereafter S-2400, S-1850,<br />

S-1750). The horiz<strong>on</strong>tal distance between S-2400 and S-1850 was about 6 km; <strong>the</strong> distance between<br />

S-1850 and S-1750 was about 8 km. Three forest glades with adjacent forested areas, were chosen in<br />

each strata, selecti<strong>on</strong> was based <strong>on</strong> accessibility (Table 1). Positi<strong>on</strong> and altitude of <strong>the</strong> glades were<br />

recorded using a GPS and an altimeter, respectively. Adjacent forest sites were chosen randomly at<br />

a distance between 50 m and 100 m from <strong>the</strong> edge of <strong>the</strong> glade. Fieldwork was undertaken during<br />

<strong>the</strong> rainy seas<strong>on</strong> between begin of July and end of August 2006.<br />

<str<strong>on</strong>g>Walia</str<strong>on</strong>g>-<str<strong>on</strong>g>Special</str<strong>on</strong>g> <str<strong>on</strong>g>Editi<strong>on</strong></str<strong>on</strong>g> <strong>on</strong> <strong>the</strong> <strong>Bale</strong> <strong>Mountains</strong> 132

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!