ABSTRACT

 

The Lower Pleistocene fossil site of Swartkrans has been excavated periodically since 1948 by Robert Broom and John Robinson and, most recently, by C.K. Brain.  Brain’s last major effort ended more than fourteen years ago.  This cave site has yielded the single largest sample of the early hominid species Paranthropus robustus, and several specimens referred to as the human ancestor, Homo erectus.  The final seven year period of excavation, initiated in 1979, was conducted in a meticulous fashion, and has produced an abundance of carefully recorded geological, fossil, and artifact data.  More than 20,000 fossils, along with a number of bone and stone tools, were recovered from Members (strata) 1, 2, and 3 alone.  The excavation was carried out largely in 10 cm elevation increments with a metal grid erected over the site to allow more accurate provenancing.

Fossil remains and tools found at the site of Swartkrans have been attributed to a variety of taphonomic stimuli such as hominid activity, carnivore activity,  alluvial deposition and gravitation.  In fact, accumulations at this and other Plio-Pleistocene cave sites in South Africa have probably resulted from a combination of these factors.  This webpage presents information on a method developed to allow researchers to archive and visualize fossil, artifact, and geological data in their spatial contexts, and to further explore taphonomic factors responsible for such accumulations.

A 3D Geographic Information System (GIS) was built with data from a variety of sources: 1) a 1999 survey using a laser theodolite to record spatial coordinates for remaining geological features; 2) the digitization of CK Brain’s field diagrams from the final seven years of excavation to reconstruct the original geology of the site; and 3) a relational database including information on more than 20,000 vertebrate fossils (macrofauna) and artifacts from Members 1, 2, and 3.  This system allows the evaluation of artifact and fossil distributions, and the exploration of the taphonomic nature of the site taking into consideration its geological framework.  It also facilitates the process of bone refitting, and contributes to the development of a protocol for similar reconstructions at other South African fossil-bearing cave sites.

Mapping and 3D reconstruction of sites such as Swartkrans present challenges when using traditional GIS approaches because they cannot interpolate data from overhang features (there must be only one z-value for each x-y coordinate).  This study uses a new 3D approach combining Intergraph’s Voxel Analyst and Esri’s Arcview 3D Analyst to overcome this limitation.  Results present an accurate three-dimensional model of the site and its contents for data storage and analysis. 

 

HOME        GOALS         IMAGES        CONTACT        ACKNOWLEDGEMENTS