Abstract
AbstractAeolianites and cemented foreshore deposits on South Africa's Cape south coast have the capacity to record and preserve events that transpired on them when they were composed of unconsolidated sand. Thirty-five Pleistocene elephant tracksites have been identified along this coastline. This abundance of sites along what was the margin of the vast Palaeo-Agulhas Plain allows for an appreciation of the forms that elephant tracks and traces can take in the context of the global proboscidean track record. They point to a significant regional elephant presence from Marine Isotope Stage (MIS) 11 (~400 ka) through MIS 5 (~130–80 ka) to MIS 3 (~35 ka) and also indicate repeated use of certain dune areas. They buttress Holocene and historical evidence that elephants made use of open areas in the region, and that the remaining “Knysna elephants” retreated into dense afrotemperate forest for protection in recent centuries. Analogies can be drawn between Pleistocene elephant tracks and Mesozoic dinosaur tracks, and some of the Cape south coast elephant tracks are among the largest Cenozoic (and hence, Quaternary) tracks ever to be described. A newly identified tracksite in this area may provide the first reported evidence of elephant trunk-drag impressions.
Highlights
The Cape south coast of South Africa contains an array of Pleistocene tracks and trace fossils in aeolianites and cemented foreshore deposits (e.g., Helm et al, 2020a)
The strike of the bedding planes in this area varies from 293° to 330°, and dip measurements vary from 12° to 30°, indicating a succession of dune layers and a predominant wind direction at the time of deposition from the southwest
At one Pleistocene elephant tracksite, we identified probable elephant coprolites, which are the object of further analysis
Summary
The Cape south coast of South Africa contains an array of Pleistocene tracks and trace fossils in aeolianites (cemented dunes) and cemented foreshore deposits (e.g., Helm et al, 2020a). The capacity of these dune and beach surfaces to record events that transpired on them has been demonstrated, including the passage of humans (Helm et al, 2018a), other mammals (Helm et al, 2018b; Lockley et al, 2021), birds (Helm et al, 2017, 2020b), reptiles (Lockley et al, 2019; Helm et al, 2020c), and invertebrates (Helm et al, 2020a).
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