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

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Preliminary Results<br />

All <strong>the</strong> lakes and p<strong>on</strong>ds are situated well above <strong>the</strong> timber line, which is marked by Hagenia-<br />

Hypercicum (2800 – 3200 m in <strong>the</strong> southwest, and 3300 – 3500 m in <strong>the</strong> nor<strong>the</strong>ast expositi<strong>on</strong>).<br />

On mountains north of <strong>the</strong> <strong>Bale</strong> range, such as Mt. Bada (4139 m), Mt. Abuye Meda (4305 m),<br />

Mt. Choke (4070 m), Mt. Guna (4231 m), Abuna Josef (4190 m) and <strong>the</strong> Semien range (4548<br />

m), lakes are ei<strong>the</strong>r absent (Semien) or do not occur at altitudes above <strong>the</strong> timberline. Although<br />

Garba Guracha, which is located in a side valley of <strong>the</strong> Tog<strong>on</strong>a River, is <strong>the</strong> <strong>on</strong>ly typical morainic<br />

lake under investigati<strong>on</strong>, <strong>the</strong>re is no doubt that almost all of <strong>the</strong> lake and p<strong>on</strong>d basins have been<br />

influenced, if not formed, by glacial activity. Many basins have been completely filled up or filled to<br />

such a degree that <strong>on</strong>ly very shallow and temporal water bodies remain.<br />

A summary of selected physical and chemical data <strong>on</strong> <strong>the</strong> study sites is presented in Table<br />

1. In brief, our <strong>Bale</strong> Mts study sites are located between 3917 and 4141 m elevati<strong>on</strong>. They are all<br />

permanent (i.e. <strong>the</strong>y also hold water during <strong>the</strong> dry seas<strong>on</strong>), and fairly shallow (average water depth<br />

of 29,1 cm during <strong>the</strong> dry seas<strong>on</strong> and 51,4 cm during <strong>the</strong> wet seas<strong>on</strong> ), except for Garba Guracha<br />

which is distinctly deeper (5,2 m during <strong>the</strong> dry seas<strong>on</strong>, and 6,0 m during <strong>the</strong> wet seas<strong>on</strong>). High<br />

water marks al<strong>on</strong>g <strong>the</strong> shoreline and GPS mapping of wet and dry seas<strong>on</strong> shorelines indicate that<br />

water level can vary c<strong>on</strong>siderably between seas<strong>on</strong>s (up to 1m), especially in <strong>the</strong> larger lakes like<br />

Garba Guracha and Hara Laki (called Hora Org<strong>on</strong>a by Löffler 1978). Water bodies look visibly very<br />

different during wet and dry seas<strong>on</strong>. More specifically, macrophytes are far less comm<strong>on</strong> and water<br />

transparency is c<strong>on</strong>siderably lower during <strong>the</strong> dry seas<strong>on</strong> (often with large amounts of suspended<br />

sediments). This is presumably due to <strong>the</strong> combinati<strong>on</strong> of wind-driven sediment disturbance during<br />

<strong>the</strong> dry seas<strong>on</strong>, and <strong>the</strong> higher number of waterfowl during that time increasing nutrient c<strong>on</strong>tent and<br />

algal productivity. Several chemical parameters (such as total phosphorus,<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> 174

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