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list of figures - Terry Sunderland

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Cameroon hinterland are well-known for their high levels <strong>of</strong> endemism and speciation<br />

(Cheek et al., 1992; Thomas, 1994; Cable and Cheek, 1998) and these forests are<br />

postulated to represent a Pleistocene refuge <strong>of</strong> some significance (Brenan, 1978;<br />

Hamilton, 1981; Pannel and White, 1988; White, 1993; Maley, 1996; Robbrecht,<br />

1996; Sosef, 1996; Morat and Lowry, 1997).<br />

Table 6. Floristic similarity between the sample sites (all species)<br />

Sorenson’s coefficient 8 Jaccard’s coefficient 9<br />

Mokoko Campo Takamanda<br />

Mokoko - 0.609 0.560<br />

Campo 0.757 - 0.818<br />

Takamanda 0.718 0.900 -<br />

3.6.2 Rattan diversity and similarity<br />

It is speculated that, to a certain degree, rattan diversity is positively correlated to<br />

overall species diversity (Dransfield, 1979; Dransfield, 1992b). The results <strong>of</strong> this<br />

study provide evidence to support this hypothesis. The Mokoko FR shows the greatest<br />

diversity <strong>of</strong> rattan species (Shannon-Weaver index H = 1.09) followed by the<br />

Takamanda FR (H = 1.01) and the Campo FR (H = 0.31). From these results, it is<br />

clear that there is a strong positive correlation between overall floristic diversity and<br />

rattan diversity (Pearsons correlation analysis r = 0.849, P < 0.01). In this respect, and<br />

in the African context, preliminary study <strong>of</strong> the rattan diversity <strong>of</strong> an area may indeed<br />

prove to be a reliable indicator <strong>of</strong> overall species diversity.<br />

In terms <strong>of</strong> floristic similarity, however, the affinities between the rattan flora are<br />

closer between Mokoko and Takamanda, and Mokoko and Campo, with very few<br />

species shared between Takamanda and Campo. This is in contrast to the similarities<br />

in the wider vegetation presented above. Although it is not clear why this might be the<br />

case, the evolutionary history <strong>of</strong> the palm flora in Africa (as discussed in Chapter 1)<br />

may account for these affinities. However, unlike the vegetation as a whole, the<br />

7 Shannon-Weaver Diversity Index: H = -xpi 1n pi where p is the proportion <strong>of</strong> a particular species in<br />

a sample which is multiplied by the natural logarithm <strong>of</strong> itself. H is derived by summing the product for<br />

all the species in a sample (Hayak and Buzas, 1997).<br />

8 Sorenson’s coefficient: CN = 2jN / (aN+bN), where aN is the number <strong>of</strong> individuals in site A, bN is the<br />

number <strong>of</strong> individuals in site B and jN is the sum <strong>of</strong> the lower <strong>of</strong> the two abundances <strong>of</strong> species which<br />

occur at the two sites (Hayak and Buzas, 1997).<br />

9 Jaccard’s coefficient: Cj = j / (a=b-j), where j is the number <strong>of</strong> species common to both sites, a is the<br />

number <strong>of</strong> species in site A, and b is the number <strong>of</strong> species in site B (Fowler et al., 1998).<br />

188

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