1978
DOI: 10.1007/978-94-009-9951-0_5
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Late Cretaceous and Tertiary vegetation history of Africa

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Cited by 317 publications
(319 citation statements)
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References 124 publications
(125 reference statements)
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“…These dates are contemporaneous with, or slightly earlier than, current fossil constraints on Oligocene mammal interchange between Eurasia and Africa (45). The establishment of currently disjunct oscine lineages in Asia and Africa was likely mediated by the presence of mesic forest throughout northern Africa and Eurasia before Miocene desertification (46), which generated disjunct patterns of distribution in many bird groups and other vertebrate lineages (47,48). More extensive sampling of passerine lineages will undoubtedly reveal additional unrecognized faunal connections between these regions, allowing more detailed evaluation of avian dispersal into Africa.…”
Section: Resultsmentioning
confidence: 94%
“…These dates are contemporaneous with, or slightly earlier than, current fossil constraints on Oligocene mammal interchange between Eurasia and Africa (45). The establishment of currently disjunct oscine lineages in Asia and Africa was likely mediated by the presence of mesic forest throughout northern Africa and Eurasia before Miocene desertification (46), which generated disjunct patterns of distribution in many bird groups and other vertebrate lineages (47,48). More extensive sampling of passerine lineages will undoubtedly reveal additional unrecognized faunal connections between these regions, allowing more detailed evaluation of avian dispersal into Africa.…”
Section: Resultsmentioning
confidence: 94%
“…Contemporary drier areas in the north and south of the African continent were linked in the past. For example, during a period of cooling in the middle Miocene 15.6-12.5 million years ago (Denton 1999), and during repeated interglacial periods of the Pleistocene epoch when forests in tropical Africa contracted considerably, forming refugia with a corresponding expansion of more xeric environments (Axelrod & Raven 1978;Denton 1999). The historical distribution of pycnostigmines, as did the rest of the fauna exposed to these changes (Grubb 1999;Grubb et al 1999;Vrba 1992), followed suite, experiencing phases of being alternately continuous and disjunct, culminating in the current phase of vicariance dictated by habitat and environment.…”
Section: Discussionmentioning
confidence: 99%
“…It is also interesting that the basal divergences within Nothophryne split the lineage at the edge of the distribution, at Taratibu, from all others. This might reflect a formerly more extensive distribution of subtropical forest across the region that became increasingly isolated and restricted to moist areas (i.e Afromontane and coastal forest) over time (Axelrod and Raven, 1978;Brenan, 1978). The biogeographic interpretations of these patterns merits further investigation, particularly if additional populations are discovered on other inselbergs.…”
Section: Phylogenymentioning
confidence: 99%