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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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ContributorsSchoenwetter, James (Author)
Created1999
Description
Sediment samples associated with a Mesolithic site on the shore of Tatton Mere contain pollen "downwashed" through the deposits since establishment of a soil on an aeolian dune that developed at the locale in Romano-British times. Application of the method suggested in Schoenwetter, 1990, "Method for the Application of Pollen

Sediment samples associated with a Mesolithic site on the shore of Tatton Mere contain pollen "downwashed" through the deposits since establishment of a soil on an aeolian dune that developed at the locale in Romano-British times. Application of the method suggested in Schoenwetter, 1990, "Method for the Application of Pollen Analysis in Landscape Archaeology," allows interpretation of the pollen sequence in terms of changes in local landuse. The result is wholly consistant with the sequence of landuses recorded for the locale since the 11th century. Rejected for European publication by reviewers.
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ContributorsSchoenwetter, James (Author)
Created1982
DescriptionReports successful extraction of pollen from Mesolithic archaeological site-context deposits at moor locations using swirl flotation technology. Integration with previously obtained pollen records from Central Pennines Mesolithic sites suggests alternative to conventional archaeological interpretation.
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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.