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Fisheries in the Southern Border Zone of Takamanda - Impact ...

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Vegetation Assessment<br />

Table 4. Similarity <strong>of</strong> <strong>Takamanda</strong> plots to o<strong>the</strong>r plots <strong>in</strong><br />

Cameroon.<br />

habitats, some taxa were recorded at every assessment<br />

site, rang<strong>in</strong>g from lowland forest to montane forest.<br />

These <strong>in</strong>clude Protomegabaria stapfiana, Santiria<br />

tremira, Hypnodaphnis zenkeri, Xylopia staudtii,<br />

Tabernaemontana crassa, Strombosia grandifolia,<br />

Strombosia pustulata, Strombosiopsis tetandra, and<br />

Treculia oboviodea.<br />

5.4 Floristic Aff<strong>in</strong>ities<br />

The Reserve encompasses a unique region that <strong>in</strong>cludes<br />

<strong>the</strong> full altitud<strong>in</strong>al vegetation range found <strong>in</strong> this part <strong>of</strong><br />

Cameroon. From our surveys, it is clear that vegetation <strong>of</strong><br />

<strong>the</strong> area is somewhat dist<strong>in</strong>ctive and concurs with studies<br />

from <strong>the</strong> Nigerian side <strong>of</strong> <strong>the</strong> border (Hall and Medler<br />

1975, Keay 1979). As evidence <strong>of</strong> this uniqueness, <strong>the</strong><br />

Number <strong>of</strong> trees per hectare<br />

<strong>Takamanda</strong>/<br />

Campo<br />

<strong>Takamanda</strong><br />

/ Ejagham<br />

Campo /<br />

Ejagham<br />

560<br />

540<br />

520<br />

500<br />

480<br />

460<br />

440<br />

420<br />

400<br />

Sorensen©s<br />

Coefficient<br />

Jaccard©s<br />

Coefficient<br />

0.277 0.161<br />

0.308 0.182<br />

0.491 0.325<br />

380<br />

0 200 400 600 800 1000 1200 1400<br />

Altitude (m)<br />

r2 = 0.618<br />

Figure 6. Relationship between altitude and tree density <strong>in</strong><br />

<strong>the</strong> biodiversity plots <strong>of</strong> <strong>Takamanda</strong> Forest Reserve,<br />

Camerooon.<br />

Caesalp<strong>in</strong>aceae are relatively poorly represented <strong>in</strong> TFR<br />

lowland forests, unlike <strong>the</strong> Ejagham and Korup forests to<br />

<strong>the</strong> south and <strong>the</strong> majority <strong>of</strong> forested areas <strong>in</strong> Southwest<br />

Prov<strong>in</strong>ce. Ra<strong>the</strong>r, TFR lowland forests possess a far<br />

richer tree flora than <strong>the</strong>se o<strong>the</strong>r forests. Indeed, diversity<br />

decreases significantly as one moves from <strong>Takamanda</strong><br />

(H′=4.61) to Ejagham (H′=3.69).<br />

This uniqueness is also evident when floristic<br />

similarities and evenness at TFR are compared to <strong>the</strong><br />

Ejagham forest, also <strong>in</strong> <strong>the</strong> Southwest Prov<strong>in</strong>ce, and <strong>the</strong><br />

Campo region <strong>in</strong> sou<strong>the</strong>rn Cameroon. It came as a<br />

surprise that <strong>the</strong> geographically disjunct<br />

Campo/Ejagham shared more species than<br />

<strong>Takamanda</strong>/Ejagham and <strong>Takamanda</strong>/Campo (Table 4).<br />

For <strong>the</strong> montane forest and high-altitude grassland,<br />

however, <strong>the</strong> floristic aff<strong>in</strong>ities are more complex,<br />

result<strong>in</strong>g from climatic change and phytogeographical<br />

variance. Hall (1981) suggests that <strong>the</strong> montane forest<br />

flora <strong>of</strong> <strong>the</strong> Obudu area represents “an impoverished<br />

variant <strong>of</strong> <strong>the</strong> flora <strong>of</strong> <strong>the</strong> lowland forest <strong>of</strong> <strong>the</strong> Oban<br />

hills,” a known Pleistocene refuge, with <strong>the</strong> addition <strong>of</strong><br />

an Afromontane element. The presence (if not<br />

dom<strong>in</strong>ance) <strong>of</strong> many lowland species <strong>in</strong> TFR montane<br />

forest, along with Afromontane taxa, supports this<br />

hypo<strong>the</strong>sis and suggests that:<br />

• The “montane” forest is <strong>in</strong>fluenced by<br />

anthropogenic <strong>in</strong>terventions such as burn<strong>in</strong>g <strong>of</strong> highaltitude<br />

grassland that is reduc<strong>in</strong>g its altitud<strong>in</strong>al<br />

extent and ability to regenerate; hence, <strong>the</strong> tree l<strong>in</strong>e is<br />

gradually reduc<strong>in</strong>g. This accounts for <strong>the</strong> significant<br />

numbers <strong>of</strong> lowland forest species <strong>in</strong> this forest<br />

formation.<br />

• At lower altitudes (

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