2015
DOI: 10.1016/j.palaeo.2015.02.002
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Miocene–Pliocene vegetation change in south-western Africa (ODP Site 1081, offshore Namibia)

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Cited by 28 publications
(25 citation statements)
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“…Nevertheless, the two regions have different climates. The northern part of Namibia is a more mesic region and characterized by woodland vegetation (Hoetzel, Dupont, & Wefer, 2015;Simmons, Griffin, Griffin, Marais, & Kolberg, 1998;White, 1983), while central Namibia and the Karoo ecoregions (Succulent and Nama) of South Africa are semi-arid (Neumann & Bamford, 2015;Okitsu, 2005;Thuiller et al, 2006; Figure 2). The importance of region as a predictor of RF variation may be indicative of these environmental discontinuities.…”
Section: Discussionmentioning
confidence: 99%
“…Nevertheless, the two regions have different climates. The northern part of Namibia is a more mesic region and characterized by woodland vegetation (Hoetzel, Dupont, & Wefer, 2015;Simmons, Griffin, Griffin, Marais, & Kolberg, 1998;White, 1983), while central Namibia and the Karoo ecoregions (Succulent and Nama) of South Africa are semi-arid (Neumann & Bamford, 2015;Okitsu, 2005;Thuiller et al, 2006; Figure 2). The importance of region as a predictor of RF variation may be indicative of these environmental discontinuities.…”
Section: Discussionmentioning
confidence: 99%
“…The Plucheinae is most likely of southern African, specifically in the Namib region, origin (Figs b & ). The origin correlates in time with the start of the Miocene aridification of the general Namib area (Senut et al ., ; Hoetzel et al ., ) in connection with the formation of the Benguela Upwelling, following the formation of the ACC. Connections between the formation of the Benguela upwelling and radiation of species with presumed Namib origin have been previously hypothesized (e.g.…”
Section: Discussionmentioning
confidence: 99%
“…30, Figure 1) off the coast of Namibia, involving pollen, microscopic charcoal and the stable isotopic composition of plant waxes, draws the picture of a late Miocene-Pliocene (c. 9-3 Myr) spread of C 4 grasses, probably more pronounced in the central than in the southern Namib (Ségalen et al, 2006;Senut & Ségalen, 2014), in an environment of shrinking grasslands and expanding deserts (Hoetzel et al, 2013). Hoetzel et al (2015) distinguish three vegetation phases utilising ODP 1081: a wet phase during the Tortonian, a transitional Messinian period with a pronounced spread of grasses and a rather dry Pliocene period with desert plants. Another marine core close by (ODP 1082, no. 30, Figure 1) shows major vegetation changes 3,4-1,8 Myr but they also show developments in the eastern hinterland of the desert (Dupont, 2006).…”
Section: Desert Biomementioning
confidence: 89%
“…The scarcity of terrestrial Neogene sites in southern Africa makes the study of marine records invaluable as this allows, at least to a limited degree, an indication of the vegetation onshore (e.g. van Zinderen Bakker, 1984;Dupont et al, 2005;Udeze & Oboh-Ikuenobe, 2005;Hoetzel et al, 2015). Although direct palaeobotanical evidence in Neogene terrestrial sites is often lacking, geochemical approaches (e.g.…”
Section: Introductionmentioning
confidence: 99%