Preservation and Paleoenvironmental Significance of a Footprinted Surface on the Sandai Plain, Lake Bogoria, Kenya Rift Valley
Authors: Scott, Jennifer1; Renaut, Robin1; Owen, R. Bernhart2
Source: Ichnos, Volume 15, Numbers 3-4, July 2008 , pp. 208-231(24)
Publisher: Taylor and Francis Ltd
Abstract:
An exhumed late Pleistocene land surface on the deltaic Sandai Plain north of Lake Bogoria, Kenya, preserves traces of bovids, suids, birds, and at least one hominid. The host sediments (Loboi Silts) are reddish brown, poorly bedded siltstones, mudstones and silty sandstones that were probably deposited in a shallow closed-basin lake. Most of the prints were impressed on exposed, moist lake-marginal mudflats. Print distribution is patchy due to a complex interaction between biogenic and sedimentological factors. The preservation of a single hominid track provides a fortuitous addition to the sparse hominid track record in East Africa. Field, petrographic, and mineralogical analyses of the fossil substrate were undertaken to determine how the footprinted surface was preserved. Comparison with modern lake-marginal processes suggests that the prints were initially stabilized by desiccation, soil-crusting, and organic films, followed by cementation of the surface sediments by calcite and analcime, with minor authigenic clay minerals and Fe-Mn-oxihydroxides. The zeolites formed by reaction of detrital silicates with saline, alkaline groundwater; calcite was precipitated from dilute runoff and fresher groundwaters. Cementation likely occurred during a prolonged period of relatively low, stable lake level. Following cementation, the surface was buried by Holocene lake sediments, then recently exhumed.Keywords: Paleoichnology; vertebrate tracks; hominids; Kenya Rift; taphonomy; diagenesis
Document Type: Research article
DOI: 10.1080/10420940802470573
Affiliations: 1: Department of Geological Sciences, University of Saskatchewan, Saskatoon, Canada 2: Department of Geography, Hong Kong Baptist University, Hong Kong, China

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