The Cape element in the Afrotemperate flora: from Cape to Cairo?

• Published in: Proceedings of the Royal Society. B, Biological sciences Vol. 274; no. 1609; pp. 535 - 543
• Main Authors: Galley, Chloé, Bytebier, Benny, Bellstedt, Dirk U, Peter Linder, H
• Format: Journal Article
• Language: English
• Published: London The Royal Society 22.02.2007
• Subjects: Africa; Afromontane forests; Ancestral Character Reconstruction; Animal migration behavior; Bayes Theorem; Biodiversity; Biogeography; Biological taxonomies; Climate; Evolution; Flora; Genetic Speciation; Historical Biogeography; Magnoliopsida - classification; Magnoliopsida - physiology; Molecular Dating; Orchidaceae - classification; Orchidaceae - physiology; Phylogeny; Phytogeography; Plants; Poaceae - classification; Poaceae - physiology; Restionaceae; Speciation; Taxa; Tropical regions
• ISSN: 0962-8452; 1471-2954
• DOI: 10.1098/rspb.2006.0046

The build-up of biodiversity is the result of immigration and in situ speciation. We investigate these two processes for four lineages (Disa, Irideae p.p., the Pentaschistis clade and Restionaceae) that are widespread in the Afrotemperate flora. These four lineages may be representative of the numerous clades which are species rich in the Cape and also occur in the highlands of tropical Africa. It is as yet unclear in which direction the lineages spread. Three hypotheses have been proposed: (i) a tropical origin with a southward migration towards the Cape, (ii) a Cape origin with a northward migration into tropical Africa, and (iii) vicariance. None of these hypotheses has been thoroughly tested. We reconstruct the historical biogeography of the four lineages using likelihood optimization onto molecular phylogenies. We find that tropical taxa are nested within a predominantly Cape clade. There is unidirectional migration from the Cape into the Drakensberg and from there northwards into tropical Africa. The amount of in situ diversification differs between areas and clades. Dating estimates show that the migration into tropical East Africa has occurred in the last 17 Myr, consistent with the Mio-Pliocene formation of the mountains in this area.