Abstract
The three Krakatau islands in Indonesia were completely denuded by the great eruption in 1883. One century after the eruption, the vegetation of Rakata on the one hand and of Panjang and Sertung on the other are quite different. Indigenous or exogenous Neonauclea seeds successfully formed Neonauclea forest on Rakata island but compltely failed to do so on Panjang and Sertung islands. The dispersal of seeds, soil conditions and volcanic activity of Anak Krakatau were all found to be contributing factors.
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