Reports on Pranburi Beach and Haad Pran:
The Great Western Rain Forests
Equatorial rain forests
consist of tall closely set trees whose crowns form a continuous canopy
of foliage and provide dense shade for the ground and lower layers.
Tree leaves are broad and evergreen and the crowns tend to form into
two or three layers, of which the highest layer consists of scattered
emergent crowns rising to 40 m. Typical of the equatorial rain forest
are lianas, thick woody vines supported by the trunks and branches
of the trees. Some are slender like ropes, others reach thicknesses
of 20 cm.
Epiphytes are numerous
using the trunk, branches or foliage of trees and lianas solely as
a means of physical support. They are of many plant classes and include
ferns, orchids, mosses and lichens. Some epiphytes are stranglers,
sending down their roots to the soil, eventually surrounding the tree
and ultimately replacing it.
An important characteristic
of the equatorial rain forest is the large number of trees that coexist.
As many as 3000 species may be found in 1 square kilometre. The floor
of the forest is usally so densely shaded that plant foliage is sparse
close to the ground and gives the forest an open aspect, making it
easy to traverse. The ground surface is covered only by a thin litter
of leaves. Rapid consumption of dead plant matter by bacterial action
results in the absence of humus in the soil.
Equatorial rain forests
are limited to the Amazon basin, the Congo lowland and the South East
Asian islands of Sumatra, Borneo and New Guinea.
From 10º latitude
North and South to the tropics of Cancer and Capricorn equatorial
rain forest is substituted by tropical rain forest along windward
coasts. Here we find a distinct annual precipitation and temperature
cycle, resulting in fewer species and lianas. Epiphytes are, however,
abundant due to continued exposure to humid air and cloudiness of
the coastal hills and mountain slopes. Tropical rain forest is typical
for the Carribian lands, the eastern coasts of Brazil and Madagascar
and the western coasts of India, Burma and Thailand.
Monsoon forests
present a more open tree growth than the equatorial and tropical rain
forests. Consequently, there is less competition among trees for light
but a greater development in the lower layers. Trees have massive
trunks with thick and rough bark reaching a height of only 35 m.
The most important feature
is the deciduousness of most of the tree species, with the
teakwood tree (Tectona grandis) being the most important one among
them. This is a response to a climate where a long rainy season alternates
with a dry and cool season. Typical monsoon forests cover inland Burma,
northern Thailand, Laos and Cambodia.
Where the forest
has been cleared by cutting and burning, the returning plant growth
is low and dense and may be described as jungle. It can consist of
a tangled growth of lianas, bamboo shrub, thorny palms and thickly
branching shrubs, constituing an impenetrable barrier to travel in
contrast to the open area of the rain forest.
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| Updated: 28
January, 2008
|