Role of aeolian sediment accretion in the formation of heuweltjie earth mounds,western South Africa |
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| Authors: | Joseph R McAuliffe M Timm Hoffman Leslie D McFadden Matthew P King |
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| Affiliation: | 1. Desert Botanical Garden, Phoenix, Arizona, USA;2. Plant Conservation Unit, Biological Sciences Dept., University of Cape Town, Cape Town, Republic of South Africa;3. Dept of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico, USA;4. Dept of Geosciences, University of Arizona, Tucson, Arizona, USA |
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| Abstract: | The action of organisms in shaping landforms is increasingly recognized; the field of biogeomorphology and the conceptual framework of ecosystem engineering have arisen in response to the need for integrated studies of the interactions between biotic and abiotic components of landscapes. Pathways by which organisms influence landscape development may be complex. For example, primary change initiated by one biotic element may initiate a cascade of other changes that eventually produce a significant landscape modification. Mound‐like landforms in North America and southern Africa are widely cited examples of biogenic structures, yet there is considerable controversy regarding the processes responsible for their formation. Heuweltjies (Afrikaans for little hills) are circular mounds ranging from 10–30 m diameter and 0.5–2 m height and are widespread in western South Africa. Colonies of the termite (Microhodotermes viator) are typically associated with heuweltjies and some investigators have attributed heuweltjie formation to the direct action of termites in redistributing earthen materials. However, rather than being directly responsible in this way, termites simply create nutrient‐rich islands, which support denser vegetation, thereby inducing the localized accretion of aeolian sediments and upward growth of mounds. Contrasting soil features in heuweltjies in one locale indicate these processes have occurred throughout the late Quaternary. Geographic variation in sizes of mounds is explained in part by the local availability of sediments that can be mobilized and redistributed by the wind. Recognition of the operation of aeolian processes in the formation of heuweltjies has important implications for conservation. Any land use that diminishes the sediment‐trapping effect of vegetation on heuweltjies truncates the very process by which new aeolian materials can accrue and may promote irreversible erosion and landscape degradation. Copyright © 2014 John Wiley & Sons, Ltd. |
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| Keywords: | biogeomorphology calcic horizon ecosystem engineering Mima mound termites |
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