Cambial dormancy and annual rings in tropical trees are induced by ann
ually occurring dry periods or flooding, Growth periodicity is indicat
ed by the leaf fall behaviour and is connected with an annual periodic
ity of shoot elongation. Changes in stem diameter are measured with a
dendrometer or by measurable differences in the electrical resistance
of the cambium. Dendrochronological methods applied to carefully prepa
red samples can serve as proof of the annual periodicity of growth zon
es. For this purpose the following methods have been used: cambial wou
nding, radiocarbon dating, pointer year detection and regression analy
ses of ring width and climate data. Although X-ray densitometry and th
e analysis of stable isotopes in rings of tropical trees promise to pr
ovide interesting climatological information, the use of these methods
remains difficult.