Samples of paleosols from locality AL-333, known for numerous specimens of Australopithecus afarensis, were analyzed in order to reconstruct the original soils and environment of burial of the associated fossil hominids. The bones were found in swale-like features, within the calcareous and coarse-grained basal portion of a paleosol. This is more like an assemblage of bones buried during a single depositional episode, such as a flood, than an assemblage accumulated on a soil over a long period of time by carnivores or other means of death. What killed the hominids remains unclear, but considering the association of originally disarticulated bones of such hydraulically distinct types as phalanges and maxillae, it is very likely that they died and partially rotted at or very near this site. The paleosols at AL-333, here named the Fo and Go clay paleosols, have calcareous rhizoconcretions, granular surface horizons, prismatic peds, and shallow calcareous nodules and stringers like soils now supporting grassy woodland in semiarid regions. Although this group of hominids was buried in streamside gallery woodland, there is evidence from Laetoli, Tanzania, that A. afarensis ventured out into open wooded grassland as well. Evidence for this should be sought from other paleosols at Hadar.
An attempt to replicate results of a previous dietary trace-element study of northwestern Alaska (Connor and Slaughter 1984) was made with human- and animal-bone samples from the Naknek region, southwest Alaska. Trace elements of special interest are strontium and zinc because of previously postulated relation of abundances of these elements to marine and terrestrial dietary foci in human remains from archaeological sites (i.e., Nelson et al. 1986; Schoeninger and Peebles 1981). Related objectives were to develop evidence supporting Harritt's (1988) proposal for the existence of separate late prehistoric inland and coastal social and territorial entities in the region, which would be reflected as a dichotomy of trace levels in human bone; differences in abundances of strontium and zinc trace elements in bones representing each group should reflect diets based on either terrestrial fauna and plants or largely of marine sea mammals and shellfish. We find that there are no characteristic trace-element patterns for differentiating historic and late prehistoric coastal or interior inhabitants of the Alaska Peninsula, in spite of historic and archaeological evidence that indicates that such patterns should be present. This lack of patterning is traced to an erroneous assumption made initially by the present authors, and by Connor and Slaughter (1984): Because 99 percent of all digested Sr is deposited in the skeleton of vertebrates (including marine), there is no direct correlation between Sr content of human bones and the proportion of sea-mammal or teleost consumption in the prehistoric human diet.
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