[en] Landscape Ecological Survey of the Bipindi-Akom II ... - ITTO
[en] Landscape Ecological Survey of the Bipindi-Akom II ... - ITTO
[en] Landscape Ecological Survey of the Bipindi-Akom II ... - ITTO
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types are defined by floristic composition and <strong>the</strong> (external) foliage coverage <strong>of</strong> <strong>the</strong> species.<br />
Interpretation <strong>of</strong> successional status, overall physiognomy and g<strong>en</strong>eral site descriptors descriptors reveals<br />
a strong correlation <strong>of</strong> <strong>the</strong> plant communities with altitude and disturbance. The The communities<br />
discerned are: submontane forest (altitude> 700 m asl), three types <strong>of</strong> lowland evergre<strong>en</strong> forest<br />
« 350 m asl; 350-500 m asl; 500-700 m asl), swamp forest, young secondary forest and thicket<br />
on rec<strong>en</strong>tly abandoned agricultural fields.<br />
The leg<strong>en</strong>d <strong>of</strong> <strong>the</strong> 1: 100,000 landscape ecological map is based on altitude, landform, soil and and<br />
vegetation, and has a hierarchical hierarchical structure. A total <strong>of</strong> 14 main mapping units has be<strong>en</strong><br />
discerned. These These 14 units have be<strong>en</strong> fur<strong>the</strong>r fur<strong>the</strong>r subdivided according to vegetation characteristics<br />
brought about by human human influ<strong>en</strong>ces (shifting (shifting cultivation) into 34 units. The landscape ecological ecological<br />
map pres<strong>en</strong>ts <strong>the</strong> landscape in in its complexity <strong>of</strong> landforms, soils and vegetation. Cross refer<strong>en</strong>ce<br />
<strong>of</strong> <strong>the</strong> inv<strong>en</strong>tory data reveals a strong strong relationship betwe<strong>en</strong> vegetation, altitude and soils. This<br />
supports <strong>the</strong> notion that natural vegetation can be se<strong>en</strong> as a response variable to to <strong>en</strong>vironm<strong>en</strong>tal<br />
factors such as climate and soil. Since vegetation proves to be correlated with altitude, which<br />
is assumed to be related to climatic factors, <strong>the</strong> latter has be<strong>en</strong> tak<strong>en</strong> as <strong>the</strong> highest <strong>en</strong>try <strong>of</strong> <strong>the</strong><br />
map' leg<strong>en</strong>d. On this basis, <strong>the</strong> TCP research area is divided into five ecological zones (A-E).<br />
The overall ori<strong>en</strong>tation <strong>of</strong> <strong>the</strong> ecological zones is NNE-SSW and follows <strong>the</strong> g<strong>en</strong>eral ori<strong>en</strong>tation<br />
<strong>of</strong> <strong>the</strong> geological structures in Southwest Cameroon. The landscape <strong>of</strong> <strong>the</strong> TCP research area<br />
changes changes considerably from from west to east. east. Altitude rises from approximately 40 40 to over 1000 m<br />
as!. asl. Dissected erosional plains, hilly and rolling uplands dominate <strong>the</strong> western part <strong>of</strong> <strong>the</strong> area<br />
whereas complexes <strong>of</strong> hills and mountains are found solely in <strong>the</strong> east. Going from west to east<br />
<strong>the</strong> soils change from Ebimimbang to Ebom and Nyangong <strong>the</strong>reby increasing in clay cont<strong>en</strong>t.<br />
Valley bottoms are found throughout <strong>the</strong> area but are more frequ<strong>en</strong>t and wider in <strong>the</strong> west. The<br />
natural vegetation changes from low altitude evergre<strong>en</strong> forest with many littoral species to a<br />
submontane vegetation with characteristics <strong>of</strong> cloud forest. Human activities have influ<strong>en</strong>ced<br />
this gradi<strong>en</strong>t by logging and and shifting shifting cultivation. Along Along <strong>the</strong> main access roads roads and in <strong>the</strong> <strong>the</strong> vicinity<br />
<strong>of</strong> villages mosaics are found <strong>of</strong> actual actual fields, thickets on rec<strong>en</strong>tly abandoned fields, young young<br />
secondary forest and residual patches <strong>of</strong> tropical moist forest.<br />
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