Open AccessHistorical biogeography of Androcymbium Willd. (Colchicaceae) in Africa: evidence from cpDNA RFLPs
Author(s) -
CAUJAPÉCASTELLS JULI,
JANSEN ROBERT K.,
MEMBRIVES NÚRIA,
PEDROLAMONFORT JOAN,
MONTSERRAT JOSEP M.,
ARDANUY AMPARO
Publication year - 2001
Publication title -
botanical journal of the linnean society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.872
H-Index - 68
eISSN - 1095-8339
pISSN - 0024-4074
DOI - 10.1111/j.1095-8339.2001.tb00581.x
Subject(s) - aridification , biogeography , biological dispersal , ecology , range (aeronautics) , genus , phylogeography , woodland , pleistocene , biology , mediterranean climate , geography , arid , paleontology , phylogenetics , population , biochemistry , materials science , demography , sociology , gene , composite material
The cpDNA restriction variation in 39 populations representing a geographical sampling of 18 species of Androcymbium in southwestern and northern Africa was examined to assess the historical biogeography of the genus. The cpDNA phylogeny indicates that the disjunction between South and North Africa is best explained by the dispersal of southern African ancestors into North Africa. Divergence time estimates suggest that the geographic range of the genus may have extended considerably north (perhaps to Tanzania and Kenya) prior to the global desiccation of Africa in the Miocene. Further expansion of the genus northward was probably stalled until climatic changes in the late Miocene brought about the gradual replacement of a subtropical woodland savanna with the arid landscape that gave rise to the Sahara. Aridification of the northern quarter of the continent provided the ecological conditions for fostering the expansion of Androcymbium along the Mediterranean fringe (probably east to west) and its introduction into the Canary Islands. Unlike their South African congeners, the northern species have experienced expansions, fragmentations, and local extinctions in response to the severe climatic shifts in this area during the Pliocene‐Pleistocene. According to our divergence time estimates, the arid track may have already existed as a continuous area connecting southern and northern Africa in the late Miocene.