Palaeoclimate Reconstruction Using Charcoal from a Mid-Holocene Stratum 4b, Wonderwerk Cave, South Africa

dc.contributor.authorHlophe, Busisiwe
dc.contributor.supervisorBamford, Marion
dc.date.accessioned2025-06-25T16:34:45Z
dc.date.issued2024-06-18
dc.departmentEvolutionary Studies Institute ESI
dc.descriptionA Dissertation submitted in fulfilment of the requirements for the degree of Master of Science, to the Faculty of Science, School of Geosciences, University of the Witwatersrand, Johannesburg, 2023.
dc.description.abstractCaves are often sources for palaeoenvironmental information in the dry interior regions of southern Africa. The Wonderwerk Cave, located in Northern Cape, is a national heritage site with a well-preserved, nearly complete record of the local Holocene LSA techno-complexes and past environmental indicators. Hence, it has the potential to provide valuable insights into past human behaviour as well as the local palaeoclimate and vegetation. This study examined wood charcoal from stratum 4b, Excavation 1 of the Wonderwerk Cave. The aim was to evaluate the taxonomic composition and the physiognomy of the charcoal to understand the environment around the cave 6.9-5.9 ka. The study also investigated the modern uses of the vegetation to infer how humans may have utilized the woody plants around them during that period. The results indicate the landscape cover included woody plants adapted to dry conditions and summer rainfall. However, the archaeological taxa identified also included two species that thrive in moist environments, Halleria lucida and Olinia ventosa, suggesting fluctuations in climate. The taxonomic composition also suggests an environment similar to the modern bushveld found near the cave. The low conductivity capacity as well as vulnerability and mesomorphy indices of the woods support the implication that the vegetation was adapted to low water availability or aridity. The cave's inhabitants likely used the identified plants for firewood, magical and medicinal purposes, and more between 6.9 and 5.9 ka.
dc.description.sponsorshipNational Research Foundation (NRF)
dc.description.sponsorshipDSI-NRF Centre of Excellence in Palaeosciences
dc.description.submitterMMM2025
dc.facultyFaculty of Science
dc.identifier0000-0002-4123-9435
dc.identifier.citationHlophe, Busisiwe. (2023). Palaeoclimate Reconstruction Using Charcoal from a Mid-Holocene Stratum 4b, Wonderwerk Cave, South Africa. [Master's dissertation, University of the Witwatersrand, Johannesburg]. WIReDSpace. https://hdl.handle.net/10539/45247
dc.identifier.urihttps://hdl.handle.net/10539/45247
dc.language.isoen
dc.publisherUniversity of the Witwatersrand, Johannesburg
dc.rights©2023 University of the Witwatersrand, Johannesburg. All rights reserved. The copyright in this work vests in the University of the Witwatersrand, Johannesburg. No part of this work may be reproduced or transmitted in any form or by any means, without the prior written permission of University of the Witwatersrand, Johannesburg.
dc.rights.holderUniversity of the Witwatersrand, Johannesburg
dc.schoolSchool of Geosciences
dc.subjectCharcoal analysis
dc.subjectPalaeovegetation
dc.subjectPalaeoclimate: Mid-Holocene
dc.subjectWonderwerk Cave
dc.subjectUCTD
dc.subject.primarysdgSDG-13: Climate action
dc.subject.secondarysdgSDG-4: Quality education
dc.titlePalaeoclimate Reconstruction Using Charcoal from a Mid-Holocene Stratum 4b, Wonderwerk Cave, South Africa
dc.typeDissertation

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