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The aim of this paper is to discuss conceptual and methodological issues related with the archaeological study of lithic landscapes and exemplify the approach with a case study (artifact distribution data from east-central Argentina). A lithic landscape-understood as the co-occurrence, in a given geographic space, of different structural units each one composed by a raw material source and the complete set of unmodified and human-modified pieces of rock extracted from that source and then transported, used, and discarded across the landscape ( i.e., a scatter area)-can be modeled using kriging, a geostatistical interpolation tool useful for integrating scattered information into coherent spatial models. The case study allows for the examination and discussion of, on one hand, the relationships between the type and location of the sources and the size and shape of the respective scatter areas and, on the other, the reciprocal relationships between different raw materials and sources. It is concluded that a proper description of the spatial structure of a lithic landscape is the needed baseline from which to evaluate different explanatory models. Such models should take into account different sets of initial conditions and generative mechanisms, in order to cope with the pervasive problem of equifinality. [ABSTRACT FROM AUTHOR]

Zooarchaeological analyses have suggested a possible case of late Holocene resource depression in California tule elk ( Cervus elaphus nannodes). We develop and conduct a preliminary independent test of this here based on trends in genetic diversity derived from ancient DNA extracted from archaeological elk bone. Mitochondrial DNA sequence data from 24 tule elk temporally dispersed across the late Holocene deposits of the Emeryville Shellmound, California, provide provisional support for a decline in genetic diversity and a population bottleneck beginning about 1600 B.P. Final confirmation of this pattern must await complete replication of the sequences. Stable isotope analyses of the elk bone provide a record of change in the terrestrial environment across the period of deposition and no suggestion that climate change may have played a role in an elk population decline. The analysis has implications for our understanding of change in human behavior and biology during late Holocene of central California, the methodology of resource depression analyses, and the conservation biology of tule elk. [ABSTRACT FROM AUTHOR]