Impact of Carnivore Ravaging on Zooarchaeological Measures of Element Abundance

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Abstract

Most zooarchaeologists estimate limb-bone abundance from limb ends. Researchers have provided detailed documentation of the preferential destruction by carnivores of limb ends (Binford 1981; Binford et al. 1988; Blumenschine 1988; Brain 1981; Marean et al. 1990; Orloff and Marean 1990; Sutcliffe 1970). Others have observed differences between limb abundances calculated on limb shafts vs. ends, suggesting shaft pieces may provide more accurate estimates of original element abundance in carnivore-ravaged assemblages (Bunn 1986; Bunn and Kroll 1986; Blumenschine 1988; Klein 1975; Marean et al. 1990; Orloff and Marean 1990). However, the exact quantitative effect of carnivore ravaging on measures of element abundance has never been investigated. We provide an experimental test of the accuracy of different bone portions for estimating the original element abundance after carnivore ravaging. Spotted hyenas were allowed to ravage 33 simulated archaeological sites of known element abundance. Estimates of abundance calculated on limb ends differ greatly from original bone abundance, and estimates based on proximal/distal-shaft pieces are also inaccurate. Estimates from middle-shaft fragments, however, are uniquely accurate. These experimental data mandate reanalysis of assemblages where limb frequencies were calculated from limb ends and carnivore ravaging is implicated, and experimentally vindicate observations originally provided by Klein (1975).

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Most cited references 14

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Taphonomic and ecologic information from bone weathering

Anna K. Behrensmeyer (1978)

Bones of recent mammals in the Amboseli Basin, southern Kenya, exhibit distinctive weathering characteristics that can be related to the time since death and to the local conditions of temperature, humidity and soil chemistry. A categorization of weathering characteristics into six stages, recognizable on descriptive criteria, provides a basis for investigation of weathering rates and processes. The time necessary to achieve each successive weathering stage has been calibrated using known-age carcasses. Most bones decompose beyond recognition in 10 to 15 yr. Bones of animals under 100 kg and juveniles appear to weather more rapidly than bones of large animals or adults. Small-scale rather than widespread environmental factors seem to have greatest influence on weathering characteristics and rates. Bone weathering is potentially valuable as evidence for the period of time represented in recent or fossil bone assemblages, including those on archeological sites, and may also be an important tool in censusing populations of animals in modern ecosystems.