Popular version of Bethsaida pollen research prepared for "Discovering Archaeology" prior to the date that journal ceased publication. Rejected by "Biblical Archaeology."
Documents related to pollen studies at the Llano Grande site, Jalisco, Mexico. The 2002 report on this research contains tables of pollen observed, but presents interpretations based on a preliminary assessment of site stratigraphy. The 2004 report was prepared after a more thorough final report from 2000 on site stratigraphy.
Culmination study of palynological research on samples collected in Mammoth Cave National Park (MCNP) initiated 1974, continued 1978. Reports Early Woodland archaeological-context recovery of maize and cucurbit pollen, summarizes overall research results and archaeological implications.
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.
Paper presented at the annual meetings of the Society for American Archeology, 1960. Illustration of five types of archaeologically relevant information from pollen study of site-context sediment samples: which sites do and do not yield pollen data; intra-site cross-dating of sample proveniences; information on cultivated plants; and relationships of cultural activities to environmental conditions.
Paper discusses pollen study of 115 samples from Wetherill Mesa.
Paper discusses the use of two flotation techniques to recover pollen from this site fails to produce satisfying results.
Paper presented at the annual meetings of the Society for American Archeology, 1958. Discusses assumptions and problems of: techniques for extracting and identifying pollen, pollen distributions and deposition, analysis and statistics. Concludes that pollen study alone is not too reliable a methodology for establishing the types or durations of prior climatic events but it is reliable for reconstructing their geographic distributions and hypotheses of the reasons for climatic change.