Abstract

This paper discusses the application of malacological identification of macrofossils in stone tools. A macroscopically distinct toolstone utilized by prehistoric peoples, reported widely in archaeological consulting literature across central and southern Alberta (Meyer et al. 2007; de Mille 2009; Bohach 2010; Porter 2014), features fossilized root traces and occasional large fossil shells. These fossils can be identified, and correlated with temporal and geologic formations indicative of the environments within which the taxa occurred. Artifacts with fossils morphologically coherent with Hydrobia, Lioplacodes, and Viviparus spp. are identified in stone artifacts analyzed in this paper. These taxa are consistent with depositional environments of Paleocene period Paskapoo Formation sedimentary rocks, particularly, as identified at the Blindman-Red Deer River confluence and Joffre roadcut paleontological localities (Hoffman and Stockey 2011). In this paper we explore how the identification of these fossils offer clues to the procurement areas which were sought out by prehistoric toolmakers. We do not suggest that all Red Deer Mudstone is from these localities, though the fossil molluscs presented so far do not refute this conclusion, but we do suggest that identifying large fossil shells can be a critical diagnostic tool for identifying the geologic origin of artifacts.

Highlights

  • Archaeological sourcing to preserve the integrity of artifacts for posterity or cultural significance, and maintain potential for museum display

  • This paper will present a case for the presence of macrofossils within stone tools from Central Alberta, and discuss the potential for their origin in that region’s Paskapoo Formation sedimentary rocks

  • The authors know of no published works that have provenanced archaeological material using the identification of large fossils within artifacts

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Summary

Identification of macrofossils within stone tools

This paper discusses the application of malacological identification of macrofossils in stone tools. Consultants (Bohach 2010; de Mille 2009; Meyer et al 2007; Porter 2014) have described a fine grained, dark red to tan mudstone, commonly with black patina and white macrofossil inclusions or ‘bog material’ as ‘Paskapoo Chert’ and ‘Red Deer Mudstone’ across central Alberta We have reviewed these descriptions, both in the literature and of artifacts discussed in this paper. The main exposures at the Blindman River locality are a bed of grey calcareous mudstone that is interpreted as a lacustrine deposit, and a mediumgrained sandstone that is interpreted as a fluvial channel deposit Both contain plant and mollusc fossils and, rarely, insect and vertebrate remains (Fox 1990; Taylor and Stockey 1984)

Fossiliferous Projectile Points
Paleontological Discussion
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