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Vegetation of Southeast Asia Studies of Forest Types 1963-1965

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Under natural conditions the boundaries between tropical forests<br />

and savannas depend, generally speaking, upon the humidity factor.<br />

An exact determination, however, <strong>of</strong> the amount <strong>of</strong> rain necessary for<br />

the existence <strong>of</strong> forests is very difficult. General considerations<br />

which lead to the establishment <strong>of</strong> rain factors, aridity coefficients,<br />

and climatic types <strong>of</strong> formulae do not include the important physio-<br />

Ipgical factors <strong>of</strong> plant transpiration or the existence <strong>of</strong> subterranean<br />

water reserves which may be stored at great depths in tropical<br />

soils.<br />

The data on water requirements <strong>of</strong> forests from classical plant<br />

ecology are based upon the assumption that the present distribution<br />

<strong>of</strong> tropical forests and savannas corresponds to the ecological conditions<br />

<strong>of</strong> their environment. 'It is known, especially from researches<br />

in central equatorial Africa, that great areas <strong>of</strong> savannas,<br />

now occupying deteriorated soils, were forested in former times.<br />

More reliable data are obtained from the direct determination<br />

<strong>of</strong> transpiration values, which are scarce because <strong>of</strong> difficulty to<br />

obtain, or from a computation based on the knowledge <strong>of</strong> the total<br />

precipitation and <strong>of</strong> drainage water <strong>of</strong> an entire river basin covered<br />

by equatorial forest.<br />

The practical importance <strong>of</strong> such data is emphasized. For example,<br />

it is possible to distinguish savannas which can be reclaimed.<br />

A consideration <strong>of</strong> all the facts involved indicates how this reclamation<br />

can best be done. It is clear that agricultural methods<br />

used in temperate regions are inappropriate when applied to tropical<br />

lowland soils. Such practices disturb the water balance <strong>of</strong> tropical<br />

soils, favor serious surface erosion, cause internal, leaching <strong>of</strong><br />

soils, and there is evidence that they produce an irreversible degradation<br />

<strong>of</strong> soil fertility.<br />

Raymond, M. Carices Indochinenses Necnon Siamenses. Memoires du Jordan<br />

Botanique de Montreal, No. 53. 125 pp. Montreal. Feb. 1959.<br />

ReinJeing, O.A., and G.W. Gross. The kao pan seedless Siamese pummelo<br />

and its culture. Philippine Journal Science. 19: 389-^37. 1921.<br />

Rich, R. W. Aerial photography as a means <strong>of</strong> measuring plant Tver<br />

and composition. In Techniques and Methods <strong>of</strong> Measuring Understory<br />

<strong>Vegetation</strong>. Proceedings <strong>of</strong> a Sympos.ium at Tifton, Georgia, pp.<br />

79-81. Oct. 1958.<br />

Richards, P.W. The Tropical Rain <strong>Forest</strong> - An ecological study. 5^0 pp.<br />

%3 text figs, and 15 places. Univ. Press, Cambridge. 1952.<br />

This is probably the most authoritative and comprehensive reference<br />

on this vast and complicated subject. It contains 17 chapters,<br />

divided into 6 parts. Part 1 - Treats with structure and<br />

•physiognomy <strong>of</strong> the Tropical Rain forest; Part 2 - The Environment;<br />

Part 3 - Floristic composition <strong>of</strong> Climax communities; Part 4 -<br />

Primary successions; Part 5 - Tropical Kain forest under limiting<br />

conditions; and Part 6 - -Man and the Tropical Rain forest.<br />

257

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