2021
DOI: 10.1111/jse.12747
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Ecological and geological processes impacting speciation modes drive the formation of wide‐range disjunctions within tribe Putorieae (Rubiaceae)

Abstract: Wide‐range geographically discontinuous distributions have long intrigued scientists. We explore the role of ecology, geology, and dispersal in the formation of these large‐scale disjunctions, using the angiosperm tribe Putorieae (Rubiaceae) as a case study. From DNA sequences of nuclear ITS and six plastid markers, we inferred a phylogeny with 65% of all known Putorieae species. Divergence times, ancestral ranges, and diversification rate shifts were then estimated using Bayesian inference. We further explore… Show more

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Cited by 13 publications
(14 citation statements)
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References 116 publications
(191 reference statements)
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“…The scenario described above supports the “climatic refugia” hypothesis, according to which the current disjunct distribution of Camptoloma across Africa is the result of fragmentation and extinction events associated to a historical aridification process (Sanmartín et al, 2010; Mairal et al, 2015a, 2017; Pokorny et al, 2015; Villaverde et al, 2018; Rincón‐Barrado et al, 2021). This scenario does not preclude the possibility of dispersal events.…”
Section: Discussionsupporting
confidence: 53%
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“…The scenario described above supports the “climatic refugia” hypothesis, according to which the current disjunct distribution of Camptoloma across Africa is the result of fragmentation and extinction events associated to a historical aridification process (Sanmartín et al, 2010; Mairal et al, 2015a, 2017; Pokorny et al, 2015; Villaverde et al, 2018; Rincón‐Barrado et al, 2021). This scenario does not preclude the possibility of dispersal events.…”
Section: Discussionsupporting
confidence: 53%
“…In many groups, the eastern/western disjunction across North Africa is estimated to be older than the eastern–southern African disjunction (Pokorny et al, 2015). This is explained by initial vicariance in the north (i.e., due to the Late Miocene formation of the Sahara Desert; Senut et al, 2009), followed by stepping‐stone dispersal from eastern to southern Africa along the temperate‐climate corridor formed by the uplift of the Eastern Arc Mountains in the Pliocene (Sepulchre et al, 2006; Mairal et al, 2015a; Rincón‐Barrado et al, 2021).…”
Section: Discussionmentioning
confidence: 99%
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