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Category : Cultural heritage monuments in Bredasdorp. Namespaces File Discussion. Harff, J. Lockley, M. In the footprints of our ancestors: an overview of the hominid track record. Ichnos 15 , — Bennett, M. Human Footprints: Fossilised Locomotion? Springer, Lategan, S. Viljoen, R. Tuttle, R. Footprint clues in hominid evolution and forensics: lessons and limitations. Jacobs, Z. Last interglacial age for aeolian and marine deposits and the Nahoon fossil human footprints, southeast coast of South Africa.
Roberts, D. Last interglacial hominid and associated vertebrate fossil trackways in coastal eolianites, South Africa. Dynamics of late Cenozoic aeolian deposition along the South African coast: a record of evolving climate and ecosystems Geological Society, London, Special Publications, Mountain, E.
Footprints in calcareous sandstone of Nahoon Point. Deacon, H. The dating of the Nahoon footprints. Last interglacial c. Berger, L. Dirks, P. Carr, A. The last interglacial sea-level high stand on the southern Cape coastline of South Africa. Bateman, M. The evolution of coastal barrier systems: a case study of the Middle-Late Pleistocene Wilderness barriers, South Africa. Musekiwa, C. An assessment of coastal vulnerability for the South African coast.
South African Journal of Geomatics 4 2 , — Malan, J. Lithostratigraphy of the Waenhuiskrans Formation Bredasdorp Group. Melting ice sheets , yr ago raised sea level by 13 m: past analogue for future trends. Earth Planet.
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The implications of being in an interglacial period in South Africa. GeoBulletin 59 2 , 30—35 Fleming, K. Refining the eustatic sea-level curve since the Last Glacial Maximum using far-and intermediate-field sites. Tinker, J. Mesozoic exhumation of the southern Cape, South Africa, quantified using apatite fission track thermochronology. Tectonophysics , 77—93 Billeaud, I. Impacts of late Holocene rapid climate changes as recorded in a macrotidal coastal setting Mont-Saint-Michel Bay, France.
Geology 37 11 , — Cowell, P. Carter, R. Tomazelli, L. Brooke, B. The distribution of carbonate eolianite.
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Murray-Wallace, C. Facies architecture of a last interglacial barrier: a model for Quaternary barrier development from the Coorong to Mount Gambier Coastal Plain, southeastern Australia. The marine geology of Mossel Bay Ph. Microfacies of carbonate rocks: analysis, interpretation and application.
Illenberger, W. The geomorphic evolution of the Wilderness dune cordons, South Africa.
Kruger, A. Climate of South Africa: Climate Regions. WS Flemming, B. Agulhas Bank Studies Report Fisher, E. Middle and Late Pleistocene paleoscape modeling along the southern coast of South Africa. Understanding Late Quaternary change at the land—ocean interface: a synthesis of the evolution of the Wilderness coastline, South Africa. Ramsay, P. Late Quaternary sea-level change in South Africa. Waelbroeck, C. Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records.
Compton, J. Holocene sea-level fluctuations inferred from the evolution of depositional environments of the southern Langebaan Lagoon salt marsh, South Africa. The Holocene 11 4 , — Morse, S. Holocene footprints in Namibia: the influence of substrate on footprint variability. Early hominin foot morphology based on 1. Hatala, K. Footprints reveal direct evidence of group behavior and locomotion in Homo erectus.
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Citton, P. Mietto, P. Palaeontology: human footprints in Pleistocene volcanic ash. Nature , Liutkus-Pierce, C. Radioisotopic age, formation, and preservation of Late Pleistocene human footprints at Engare Sero, Tanzania. Onac, B. Download references. The formal review of Dr. Neil Roach was much appreciated. Rudolf Hattingh assisted with the cave survey and provided valuable field assistance.
Caley Orr provided invaluable insights in his review. Douglas Jamieson, Lucia Jamieson, Dr. David Roberts, who discovered the Langebaan hominin tracksite, was an inspiration and a mentor regarding Pleistocene coastal trackways — he is sorely missed. Charles W. Correspondence to Charles W. Publisher's note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations. Reprints and Permissions. Helm, C. Sci Rep 8, Download citation.
Received : 15 November Accepted : 15 February Published : 28 February Quaternary Science Reviews South African Journal of Science By submitting a comment you agree to abide by our Terms and Community Guidelines.
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If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate. Advanced search. Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily. Skip to main content Thank you for visiting nature. Download PDF. Subjects Biogeochemistry Palaeontology. Abstract A Late Pleistocene hominin tracksite has been identified in coastal aeolianite rocks on the Cape south coast of South Africa, an area of great significance for the emergence of modern humans.
Introduction The Cape south coast of South Africa has one of the richest Middle Stone Age archaeological records in the world, and is of high importance to modern human origins. Tuttle 17 developed criteria for the identification of hominin tracks: the hallux big toe is aligned with the four lateral toes, which are short and straight the tip of the hallux is bulbous, not tapered the tips of the hallux and adjacent second and third toes do not project markedly beyond one another a prominent medial longitudinal arch is evident.
Figure 1. Full size image. Figure 2. Geological setting The Late Pleistocene tracks reported here occur in coastal aeolianites, or fossil dune systems, which extend intermittently along much of the South African coastline and are best exposed in embayments on or near the shoreline Methods Geological context was determined by standard field mapping of the exposure and outcrop.
Figure 3. Figure 4. Figure 5. Results The local geology is characterised by a steep coastal cliff, made up of moderately-bedded, consolidated aeolianite. Figure 6. Figure 7. Table 1 details of tracks on main track-bearing layer 01—31 and lower layer L01—L Full size table.