| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4458647 | Organisms Diversity & Evolution | 2009 | 17 Pages |
Cistaceae consist of eight genera and about 180 species. Some taxonomic limits and relationships within the family remain unresolved when relying exclusively on morphological data. In the present study, a phylogeny was reconstructed and divergence times were estimated for 47 species representing various groups in Cistaceae and using coding (rbcL) and spacer (trnL-trnF) sequences of plastid DNA. The firm set of morphological synapomorphies that indicates the monophyly of the family is supported by both Bayesian and parsimony analyses. Five major lineages can be distinguished within the Cistaceae: (1) an early-diverging lineage containing Fumana species; (2) the New World Lechea clade; (3) the Helianthemum s.l. clade, containing two sister groups, one of species from the New World (Crocanthemum, Hudsonia) and the other with species from the Old World (Helianthemum s. str.); (4) the Tuberaria clade; and (5) a cohesive complex consisting of Halimium and Cistus species. Evolutionary shifts in 12 key characters of Cistaceae are inferred based on the most plausible phylogenetic hypothesis. Reconstructing the evolution of ovule position supports anatropous ovules as the ancestral condition within the Cistaceae, which is currently found only in Fumana. The Cistus-Halimium assemblage is consistently obtained as a natural clade and further supported by a cytological synapomorphy (chromosome number n=9). Optimisation of ancestral distribution areas and estimates of divergence times reveal an early divergence (10.17–18.51 Ma) of the Mediterranean-European genera, which may be related to subtropical vegetation, as complemented by paleobotanical data. In addition, the occurrence of multiple, independent migration events from the Old World to America between the Middle Miocene (8.44–14.7 Ma; Lechea) and the Upper Miocene (5.15–9.20 Ma; Crocanthemum/Hudsonia), and to the Canary Islands in the Pleistocene is inferred. We argue that the Mediterranean basin has been the main centre of differentiation of Cistaceae.
