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ContributorsSchoenwetter, James (Author)
Created1964
Description

Draft of report published in A.H. Schroeder, 1965, Anthropological Papers of the Department of Anthropology, University of Utah, Misc. Coll. Papers 75; 10: 85-110. Pilot study of 3 pollen samples suggests pollen chronology developed for Northern Arizona and New Mexico portions of the Colorado Plateau not applicable to SE Utah.

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ContributorsSchoenwetter, James (Author)
Created1967
DescriptionPaper presented as an invited lecture to graduate students in Botany at Arizona State University. Discusses the history and outcomes of Quaternary pollen studies in the desert Southwest of the United States.
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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)
Created1964
Description

Unpublished report, 1964

Pilot study of 3 pollen samples allows vegetation pattern reconstruction for period of occupation and suggests successful maize farming required water control technology.

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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.