A dissertation submitted to the Faculty of Science, University of the Witwatersrand, Johannesburg, in fulfilment of requirements for the degree of Master of Science. March 2016 / Coastal waterbodies along the east coast of southern Africa evolved from fluvial origins that were slowly
drowned by rising sea levels during the Holocene. The accumulation of sediment in these systems is
relatively undisturbed, providing ideal sites from which longer term observations of palaeo-climatic
variability over most of the Holocene period can be made. Lake St. Lucia, on the north coast of KwaZulu-
Natal, is the largest estuarine lagoon in Africa and is widely regarded as one of the most important shallow
water systems globally. Despite the importance of this system, little is currently know about the processes
driving the long-term evolution of the lake. This study aimed to reconstruct the hydrological changes
associated with the Holocene evolution of Lake St. Lucia using fossil diatoms. Analyses were performed on
two sediment cores from the North Lake (15.6 m) and False Bay (15.9 m) basins of Lake St. Lucia. Age
models, each based on eight radiocarbon dates, revealed continuous sedimentary records covering ~8300
cal. yr BP. A total of 150 samples were examined resulting in a total of 113 species recorded which were
used to infer changes in environmental conditions based on their reported ecological preferences. / GR 2016
| Identifer | oai:union.ndltd.org:netd.ac.za/oai:union.ndltd.org:wits/oai:wiredspace.wits.ac.za:10539/21289 |
| Date | January 2016 |
| Creators | Gomes, Megan |
| Source Sets | South African National ETD Portal |
| Language | English |
| Detected Language | English |
| Type | Thesis |
| Format | application/pdf |
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