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list of figures - Terry Sunderland

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and observations have built upon Letouzey’s original classification (Gartlan, 1989;<br />

Thomas, 1994).<br />

Based on preliminary Mount Cameroon Project inventory results, Thomas (1994)<br />

suggests that the vegetation <strong>of</strong> Mokoko is comprised <strong>of</strong> two forest types that intergrade<br />

completely. To the south, where the rainfall is higher is what Letouzey (1985)<br />

described as Atlantic Biafran Forest with Caesalpiniaceae with Oubangia alata<br />

(Scytopetalaceae) and other coastal indicators such as Protomegabaria stapfiana<br />

(Euphorbiaceae), Dichostemma glaucescens (Euphorbiaceae), Octoknema affinis<br />

(Octoknemataceae), Tapura africana (Dichapetalaceae) and many members <strong>of</strong> the<br />

Olacaceae.<br />

Moving progressively northwards, the coastal forest grades into Atlantic Biafran<br />

forest with Caesalpiniaceae well represented by gregarious genera such as Didelotia,<br />

Hymenostegia afzelii, Microberlinia bisulcata, Monopetalanthus, Plagiosiphon and<br />

Tetraberlinia bifoliolata. The Myristicaceae are also an important component <strong>of</strong> this<br />

forest, represented in particular by Coelocaryon preussii, Scyphocephalium mannii<br />

and Staudtia stipitata. The narrow endemic Medusandra richardsiana<br />

(Medusandraceae) along with Oubangia alata (Scytopetalaceae) dominate the<br />

understorey along with Garcinia mannii (Guttiferae) and Lasianthera africana<br />

(Icacinaceae), the latter <strong>of</strong> which are both important NTFP resources. The genera Cola<br />

(Sterculiaceae) and Diospyros (Ebenaceae) are also important components <strong>of</strong> the<br />

lowland forests <strong>of</strong> northern Mokoko. Cable and Cheek (1998) suggest that the forest<br />

types found in the northern Mokoko area exhibits clear affinities with the southern<br />

Korup area and, to a lesser extent, to the forests immediately south <strong>of</strong> the Sanaga.<br />

The vegetation was also described by Gartlan (1989) as having certain semideciduous<br />

elements at its western edge. These latter elements originate from the rain<br />

shadow present to the north <strong>of</strong> Mount Cameroon which has species communities<br />

present more <strong>of</strong>ten associated to those <strong>of</strong> the drier, eastern parts <strong>of</strong> Cameroon such as<br />

Triplochiton (Sterculiaceae) Ceiba (Bombacaceae) and many other representatives <strong>of</strong><br />

the Meliaceae and Sterculiaceae. The presence <strong>of</strong> these species more commonly<br />

178

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