Abstract
SummaryThe summit flora of the table mountains of Venezuela would appear to be represented by a relatively small endemic generic element with an intermixture of nonendemic generic elements, originating and immigrating centripetally at different times and from different dispersals or origins (West Gondwanaland‐American, Australasian/Malaysian‐American, Australasia‐Antarctica‐American), the whole modified by evolution and differentiation on newly available areas of the table mountains during their erosional history and derivation from lowland peripheral sources during Pleistocene and post‐Pleistocene times.
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