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Neogene to quaternary foraminifera from the western margin of southern Africa
The western margin of southern Africa underwent major palaeoceanographic changes since the initiation of the Benguela Upwelling System during the Neogene. Microfossils in marine sediments provide key proxies in our understanding of how the margin evolved. Fossil shells (tests) of foraminifera (singl...
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| Language: | English |
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Department of Geological Sciences
2019
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