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Vegetation of Southeast Asia Studies of Forest Types 1963-1965

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A postscript treats with the future <strong>of</strong> the Tropical Rain forest.<br />

Included also are a long list cf references; an index <strong>of</strong> plant<br />

names; and a general index.<br />

. The types <strong>of</strong> vegetation <strong>of</strong> the humid tropics in relation to the<br />

soil. Proc. <strong>of</strong> the Abidjan Symposium U.N.E.S.C.O. pp. 15-23. 1961.<br />

This is a discussion <strong>of</strong>: 1) the principal types <strong>of</strong> vegetation in<br />

the plains and lower mountain regions <strong>of</strong> equatorial and subequatorial<br />

zones and in adjoining tropical axeas, and the soils in which they<br />

are to be found; 2) characteristics <strong>of</strong> soils in this climatic zone<br />

which influence the occurrence <strong>of</strong> vegetation, and the possible influence<br />

<strong>of</strong> the various types <strong>of</strong> vegetation on the soil; and 3) evaluation<br />

<strong>of</strong> the soil in bringing the land under c-xltivation.<br />

. Plant Life and Tropical Climate. Biometeordlogy. pp. 67-75.<br />

1962<br />

Ṫhe absence <strong>of</strong> a cold season results in plant activities in the<br />

tropics being limited by lack <strong>of</strong> water rather than by low temperatures.<br />

The distribution <strong>of</strong> natural vegetation types in the tropics<br />

is thus mainly determined by the seasonal distribution <strong>of</strong> rainfall.<br />

Th< effects <strong>of</strong> excessively high temperatures on plants growing in<br />

some tropical habitats has been little studied, but the survival <strong>of</strong><br />

some plant species in the same areas seems to be dependent on the<br />

coo.ling effect due to transpiration. Information on the growth<br />

rates <strong>of</strong> plants, apart from a few cultivated species, is surprisingly<br />

incomplete. Available data indicate that the very high rates<br />

among some species depend on the rapid development <strong>of</strong> new leaf area<br />

rather than on net assimilation rates being higher than those <strong>of</strong><br />

temperate plants. Scanty evidence suggest that the rate <strong>of</strong> organic<br />

production by tropical forests is not much higher than in temperate<br />

hardwood forests.<br />

In tropical countries, with little seasonal change, plants <strong>of</strong>ten<br />

show regular rhythms <strong>of</strong> flowering, leaf change, etc., but these may<br />

be out <strong>of</strong> phase with the climate. I^en where there are marked wet •<br />

and dry seasons, plants do not always behave in the way expected.<br />

For example, seme trees lose their leaves in the wet season, hut not<br />

in the dry period. Seasonal rhythm in plants seems to be partly<br />

dependent on internal physiological rhythm and not entirely on the<br />

external environment. Kven in latitudes where differences in daylength<br />

are very small, day-length may be an important factor in<br />

controlling flowering and other seasonal phenomena in plants.<br />

Literature cited contains twelve titles.<br />

., A=.G. Tanslqy and A.S. Watt. The recording <strong>of</strong> structure, liveform<br />

and flora <strong>of</strong> tropical forest communities as a basis for their<br />

classification. Imperial <strong>Forest</strong>ry Institute, University <strong>of</strong> Oxford,<br />

Institute Paper No. 19. pp. 3-19. 1939.<br />

This paper f trims a valuable supplement to Burtt Davy's Institute<br />

Paper No. 13, published in 1938. It embodies the opinion <strong>of</strong> a<br />

258

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