2011
DOI: 10.1111/j.1365-2699.2011.02598.x
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‘Out‐of‐Africa’ dispersal of tropical floras during the Miocene climatic optimum: evidence fromUvaria(Annonaceae)

Abstract: Aim African-Asian disjunctions are common in palaeotropical taxa, and are typically explained by reference to three competing hypotheses: (1) 'rafting' on the Indian tectonic plate, enabling Africa-to-Asia dispersal; (2) migration via Eocene boreotropical forests; and (3) transoceanic long-distance dispersal. These hypotheses are tested using Uvaria (Annonaceae), which is distributed in tropical regions of Africa, Asia and Australasia. Recent phylogenetic reconstructions of the genus show a clear correlation w… Show more

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Cited by 103 publications
(108 citation statements)
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“…Previous identification of fossils attributed to Macaranga and/or Mallotus found in present day northern temperate regions could also not be confirmed [24]. The presence of a fossil Macaranga [25] in the Horn of Africa, which resembles the extant Macaranga kilimandscharica [24], is consistent with the existence of a dispersal route for Macaranga from Asia via southwest Asia and the Arabian peninsula [15], [55] in the early to middle Miocene when the climate was warm and humid [56]. The connectivity between Africa and Asia was good [55], [57], especially because land bridges between Africa and Southwest Asia occurred in the same time span (Meswa Bridge ca.…”
Section: Discussionmentioning
confidence: 91%
“…Previous identification of fossils attributed to Macaranga and/or Mallotus found in present day northern temperate regions could also not be confirmed [24]. The presence of a fossil Macaranga [25] in the Horn of Africa, which resembles the extant Macaranga kilimandscharica [24], is consistent with the existence of a dispersal route for Macaranga from Asia via southwest Asia and the Arabian peninsula [15], [55] in the early to middle Miocene when the climate was warm and humid [56]. The connectivity between Africa and Asia was good [55], [57], especially because land bridges between Africa and Southwest Asia occurred in the same time span (Meswa Bridge ca.…”
Section: Discussionmentioning
confidence: 91%
“…16–18 Mya (Rögl, 1999; Harzhauser & Piller, 2007; Inwood et al, 2009). The Gomphotherium land bridge had major biogeographical implications, enabling faunal dispersal from Africa to Eurasia and vice versa (Tchernov, 1992; Wüster et al, 2007; Harzhauser et al, 2007; Pook et al, 2009; Zhou et al, 2012). The marine connection between the Mediterranean and Paratethys seas to the Indian Ocean, severing this land bridge, is hypothesized to have been re-established in the Middle Miocene, around 15–16 Mya (Rögl, 1999; Popov et al, 2004; Harzhauser & Piller, 2007).…”
Section: Discussionmentioning
confidence: 99%
“…This 54 island nation is home to at least 11,220 described species of vascu-55 lar plants, of which 82% are endemic, including five entire families 56 (Callmander et al, 2011). Many biogeographic studies have been 57 conducted on the Malagasy flora, with the large majority indicating 58 dispersal to Madagascar from Africa and Asia (e.g., Bartish et al, 59 2011;Zhou et al, 2012;Ali et al, 2013), followed by, in some cases, 60 dispersal from Madagascar to the nearby volcanic Comoro and 61 Mascarene islands (e.g., Janssen et al, 2008;Wikstrom et al, 62 2010; Buerki et al, 2013). But few Malagasy lineages have been 63 documented as dispersing broadly across the Indian Ocean, to 64 the Arabian Peninsula and Asia (Yuan et al, 2005;Bukontaite 65 et al, 2015).…”
mentioning
confidence: 99%