School of Chemistry (ETDs)

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Browsing School of Chemistry (ETDs) by Author "Dyubele, Viwe"

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    Geochemical Investigation Into Holocene Palaeoenvironmental Change Along The Southern Cape Coast, South Africa
    (University of the Witwatersrand, Johannesburg, 2023-06) Dyubele, Viwe; Quick, Lynne; Humphries, Marc
    Climatic conditions across southern Africa are affected by the complex interaction of different atmospheric and oceanic circulation systems, the understanding of which is important to predicting future climate change. Palaeoenvironmental reconstruction is an essential tool to understand long-term environmental change and the response of ecosystems to such changes. This study examines the geochemical composition of a sediment core (WR1-1) extracted from a freshwater wetland located near Plettenberg Bay on the southern Cape coast. The wetland is located ~4 m above present sea level and positioned ~500 m from the modern coast. Situated within the year-round rainfall zone, the site is influenced by tropical easterly flow and the southern westerlies. Elemental and stable isotope geochemistry are used to reconstruct the palaeoenvironmental change at the site over the last ~8000 cal yr BP. Variations in CaO/Al2O3, Sr/Al2O3 and δ13C indicate that marine conditions dominated from 7300 to 6400 cal yr BP. Marine influence at the site decreased dramatically from ~6300 cal yr BP, as the system transitioned to a freshwater back-barrier wetland. Enrichments in SiO2/Al2O3 and Zr/Al2O3 track changes in depositional energy and suggest that the period 3800 – 3200 cal yr BP was associated with increased aeolian activity. This is interpreted to reflect increased aridity and is consistent with geochemical and pollen records from nearby sites at Eilandvlei and Voëlvlei. This suggests that a shift to more arid conditions during this time was a broad feature of the climate in the year-round rainfall zone of South Africa. The timing of this event corresponds with a marked decrease in Antarctic sea ice and pronounced aridity along the east coast of South Africa, suggesting that mid to late Holocene aridity in the YRZ was likely driven by declines in moisture from both westerly and easterly wind systems.