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ContributorsSchoenwetter, James (Author)
Created1986
Description

Version of 1976 Marble Canyon report prepared for publication. Rejected by "Plateau."

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ContributorsSchoenwetter, James (Author)
Created1969
DescriptionAbstract of paper presented at the annual meetings off the Society for American Archeology, 1969. The antiquity of certain sites in north-central Wisconsin may be predicted by the character of associated forest vegetation. The data also justify paleoecological hypotheses relevant to culture historical reconstructions.
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ContributorsSchoenwetter, James (Author)
Created1970
DescriptionSet of studies and documents relevant to the Anasazi Origins archaeological project directed by Cynthia Irwin- Williams in central New Mexico 1965-1970. Pollen records of surface samples and rockshelter and dune sites representing whole of the Paleoindian
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ContributorsSchoenwetter, James (Author) / Da Costa, Veronica (Author)
Created1976
Description

Squash and possible maize pollen in sediment samples from checkdams suggests the features are prehistoric and were used for crop production. No evidence that local environment was different when the features were used.

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ContributorsSchoenwetter, James (Author)
Created1966
Description

Study of 30 surface and 18 archaeological-context pollen samples was undertaken to assess the potential for further archaeological palynology research. Surface sample analysis allows palynological recognition of eight habitat types ranging from dry and cold through wet and moist to dry and warm. Comparison of fossil and modern surface pollen

Study of 30 surface and 18 archaeological-context pollen samples was undertaken to assess the potential for further archaeological palynology research. Surface sample analysis allows palynological recognition of eight habitat types ranging from dry and cold through wet and moist to dry and warm. Comparison of fossil and modern surface pollen data suggests the character of paleoecological change sequences at 4 sites, a positive potential for inter-site and intra-site relative cross-dating, and a positive potential for inter-regional dating on paleoclimatic grounds.