[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
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
Climbers such as Haumania danckelmanniana and Ancistrophyllium secundijlorum are frequ<strong>en</strong>tly<br />
found. Treculia obovoides, Scorodophloeus z<strong>en</strong>keri, Baphia lepitobotryx, Garcinia lucida,<br />
Garcinia mannii, Mammea africana and Drypetes 'group I '. are <strong>the</strong> most common species <strong>of</strong> <strong>the</strong><br />
shrub layer. The herb layer is closed and may reach a height <strong>of</strong> one meter. This layer is dominated<br />
ei<strong>the</strong>r by seedlings <strong>of</strong> forest trees or by herbs. Diospyros hoyleana, Scaphopetalum thonneri,<br />
Halopegia spp, Mapania amplivaginata and Palisotha mannii are frequ<strong>en</strong>tly found.<br />
The forests <strong>of</strong> this type appear to be highly dynamic. Many traces <strong>of</strong> uprooted and brok<strong>en</strong> trees are<br />
found. The gaps thus created are <strong>of</strong>t<strong>en</strong> infested by climbers that may reach down to <strong>the</strong> herb layer.<br />
Pioneer species like Musanga cecropioides are found in <strong>the</strong> larger gaps. Possible explanations for<br />
<strong>the</strong> dynamic nature <strong>of</strong> this vegetation are exposure to wind and instable steep slopes, <strong>of</strong>t<strong>en</strong> with<br />
rock outcrops.<br />
The submontane forest <strong>of</strong> <strong>the</strong> Maran<strong>the</strong>s - Anisophyllea community covers major parts <strong>of</strong> <strong>the</strong><br />
Bingalanda mountain range in <strong>the</strong> sou<strong>the</strong>astern part <strong>of</strong> <strong>the</strong> TCP area. The predominating landforms<br />
are mountains and isolated hills. The soils <strong>of</strong> <strong>the</strong>se areas belong to <strong>the</strong> Nyangong type, i.e. very<br />
clayey soils with 40 to 80% clay in <strong>the</strong> B horizon.<br />
The structure <strong>of</strong> this forest type resembles 'cloud forests'. As <strong>the</strong> elevation surpasses <strong>the</strong> average<br />
height <strong>of</strong> <strong>the</strong> cloud layer, <strong>the</strong> vegetation is regularly <strong>en</strong>gulfed in mist and drizzle (Hommel, 1985).<br />
A characteristic growth form <strong>of</strong> such forests is beard moss. In <strong>the</strong> UNESCO classification <strong>of</strong><br />
vegetation (1981), this vegetation can be typified as Tropical ombrophilous submontane forest.<br />
'The distribution <strong>of</strong> this community coincides with <strong>the</strong> forest types n° 117, n° 233 and partly with<br />
n° 228 <strong>of</strong> <strong>the</strong> phytogeographic map <strong>of</strong> Letouzey (1985, see Figure 6.1). Structurally, it resembles<br />
Letouzey's Forets submontagnardes (nO 117) although species composition is distinctly differ<strong>en</strong>t.<br />
Quite a number <strong>of</strong> species characteristic for <strong>the</strong> Maran<strong>the</strong>s - Anisophyllea community are typical<br />
for Letouzey's Semi-deciduous forest with Sterculiaceae and Ulmaceae (nOS 160 and 161). Also<br />
many repres<strong>en</strong>tatives <strong>of</strong> <strong>the</strong> Atlantic Biafran forest with Caesalpiniaceae (n° 228) are found. The<br />
Maran<strong>the</strong>s - Anisophyllea community appar<strong>en</strong>tly is a transitional vegetation betwe<strong>en</strong> <strong>the</strong> moist<br />
Atlantic forest zone and <strong>the</strong> drier Guineo-Congolian semi-deciduous forest zone.<br />
Mbatchou (1995) studied <strong>the</strong> vegetation <strong>of</strong> <strong>the</strong> proposed Etinde Rainforest reserve on <strong>the</strong> slopes<br />
<strong>of</strong>Mt Cameroon (4095 m asl) in <strong>the</strong> South-West Province <strong>of</strong>Cameroon.<br />
The submontane forest described by Mbatchou is divided in closed canopy submontane forest,<br />
discontinuous canopy submontane forest and submontane scrub. It is found betwe<strong>en</strong> 800 and 1,700<br />
m as!.. The submontane forests appears to be <strong>the</strong> transition betwe<strong>en</strong> <strong>the</strong> lowland forest and <strong>the</strong><br />
lower montane forest, and <strong>the</strong> species composition is a mixture <strong>of</strong> Guineo-Congolian and<br />
afromontane species. In structure and floristic composition, <strong>the</strong> Maran<strong>the</strong>s-Anisophyllea<br />
community resembles <strong>the</strong> closed canopy submontane forest <strong>of</strong> Mount Cameroon, although it is<br />
found in <strong>the</strong> TCP research area at much lower altitudes. The 'telescope-effect', i.e. <strong>the</strong> vegetation<br />
<strong>of</strong> <strong>the</strong> highest summits in a giv<strong>en</strong> area more or less imitates <strong>the</strong> physiognomy and species<br />
composition <strong>of</strong> forest types g<strong>en</strong>erally bound to far higher altitudes elsewhere (Hommel, 1987),<br />
could possibly be an explanation for <strong>the</strong> differ<strong>en</strong>ce in altitude range.<br />
63