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A Post-Glacial Pollen Sequence From Dark Canyon Cave, New Mexico (With W.H. Balgemann)

ContributorsSchoenwetter, James (Author) / Baglemann, Wilfred H. (Author)
Created1961
Description

Complacent pollen records associated with both extinct fauna and archaeological remains argues that Southwest has been semi-arid throughout Late- and Post-Pleistocene.

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Pollen Studies From Northeastern Colorado: Preliminary Report

ContributorsSchoenwetter, James (Author)
Created1965
Description

Surface samples and stratigraphic sample series from 3 archaeological occupation sites and 2 samples from a burial site were examined for pollen in hopes of establishing a pollen sequence and paleoenvironmental interpretations. Both objectives achieved. Discussions of absolute dates of Woodland and Upper Republican contexts in this area and cultural…

Surface samples and stratigraphic sample series from 3 archaeological occupation sites and 2 samples from a burial site were examined for pollen in hopes of establishing a pollen sequence and paleoenvironmental interpretations. Both objectives achieved. Discussions of absolute dates of Woodland and Upper Republican contexts in this area and cultural ecology are included.
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Archaeological Pollen Study of Two Dune Sites in New Mexico

ContributorsSchoenwetter, James (Author)
Created1976
Description
Study of the pollen of 4 surface and 41 stratigraphic and archaeological-context sediment samples was undertaken to provide independent evidence of the antiquity of sites LA 11828 and LA 11904, and of the hypothesis the two sites had the same cultural functions. The pollen record suggests the two sites differ…

Study of the pollen of 4 surface and 41 stratigraphic and archaeological-context sediment samples was undertaken to provide independent evidence of the antiquity of sites LA 11828 and LA 11904, and of the hypothesis the two sites had the same cultural functions. The pollen record suggests the two sites differ in antiquity: the occupation horizon samples from LA 11828 correspond to others that date to the Historic Period, while those from LA 11904 correspond to others that date 1800 - 300 B.C. Palynological differences that are probably indices of seasonality of occupation argue for the sites having different cultural functions.