During the year 1902 I was occupied with a study of the algal flora in the hot-houses of the Royal Botanic Gardens at Kew, and certain observations made then seemed scarcely to support the prevalent view of the very close similarity between tropical and temperate algal vegetation. This stimulated me to undertake a personal investigation of some tropical algal flora, and Ceylon was chosen owing to the diversity of climatic conditions which it presents. My objects was rather to study the ecological and biological aspects of the algal vegetation than to make a systematic collection of materials for a flora, and I hope to be able to show that I have been in some measure successful. A careful analysis, as I think the subsequent pages of this paper will show, brings to light very considerable differences between algal growth in the tropics and in our parts, although a certain similarity between freshwater Algæ all over the surface of the earth (considerably greater than in the case of the terrestrial flora) is indisputable. It is, in fact, a natural consequence of the uniform character of the surrounding medium. The island of Ceylon is peculiarly favourable for a study of the influence of tropical temperature and moisture on the distribution of algal growth, since the rainfall varies considerably in different parts of the island, while the mountainous southern portion (attaining a height of 8000 feet and more) produces a very considerable range of temperature, from the intense heat of Colombo and other lowland places to the high-lying Nuwara Eliya, where, at certain times of the year, the thermometer falls to below freezing point at night. In fact, we have here confined in a narrow compass almost all the different possibilities that can be realised in the tropics. It may be well at this point to briefly outline the range of variation in this respect (see also the map). The low country, with it high tropical temperature, shows great diversity in the amount of rainfall; so that some localities are exceptionally wet ( e. g. , Kalutara, Labugama), others (under the prevalent tropical conditions) very dry ( e. g. , Hambantota, Vavoniya), whilst numerous intermediate conditions between the two extremes are found ( e. g. , at Colombo, Matara, etc.); the wettest place I visited was Labugama (166 inches). The amount of rainfall at Peradeniya is not much less than at Colombo, but the lower temperature, due to the higher altitude, has some influence on the algal vegetation. In travelling upward to Nuwara Eliya the gradual change of temperature is very perceptible; the climate in the uplands is indeed practically European, although not so cold in winter, and considerably hotter in the middle of a sunny day (mean annual temperature a little over 60° F). The rainfall, however, is heavy (about 90 inches), and that produces an abundant vegetation. If we further bear in mind that there is coastal and an inland region, we shall have roughly reviewed the diversity of climatic conditions obtaining in the island.
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