Browsing by Author "Huber, James Kenneth"

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    A Late Holocene Vegetational Sequence from the Southeast Missouri Ozarks
    (1987-08) Huber, James Kenneth
    Palynological investigations of a peat deposit from a small sinkhole bog, Button bush Bog, and two archaeological sites, Round Spring Shelter, Round Spring Site 23SH19, and Gooseneck Site 23CT54 located in Shannon and Carter counties Missouri, provide a vegetational record for the last 3100 years in the southeast Ozarks. The Buttonbush Bog core has a basal radiocarbon date of 3130 ± 100 years B.P. Pollen spectra from the basal zone indicate a mixed oak forest with minor components of pine and hickory. Shortly thereafter, pine becomes more abundant, suggesting the presence of a pine-oak forest that has undergone very little change to the present. A small Ambrosia rise indicates land clearance and pioneer settlement about 165 years ago. The pollen sequence from Round Spring Shelter also suggests the presence of a pine-oak forest in the vicinity of Round Spring. However, the pollen spectra from Gooseneck Site 23CT54 indicate a mixed oak-hickory forest in the locality during the time of Indian occupation. Preliminary analysis of the fossil phytoliths from Gooseneck indicates that four grass subfamilies may have grown at the site.
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    Palynological Investigations Related to Archaeological Sites and the Expansion of Wild Rice (Zizania Aquatica L.) in Northeast Minnesota
    (2001-01) Huber, James Kenneth
    Four pollen sequences, from Big Rice, Cloquet, Gegoka, and East Bearskin lakes in northeast Minnesota indicate that postglacial vegetation progressed from tundra to a shrub parkland or forest-tundra to a conifer-hardwood forest to a mixed conifer-hardwood forest and to an uppermost ragweed zone that indicates Euro-American settlement and deforestation beginning about 1890. Based on the abundance of Gramineae pollen in the Big Rice Lake pollen sequence, wild rice (Zizania aquatica) is present in harvestable quantities approximately 1,600 years before its known use in a Laurel occupation at the Big Rice archaeological site. Pollen data from the uppermost sediment of Shannon Lake suggest that Gramineae abundance data may not indicate the presence of substantial wild rice beds in bays and shallows of lakes with large areas of deep open water. The Gramineae pollen profile from Gegoka Lake, which now supports wild rice over most of its surface, indicates that the current presence of wild rice in some lakes may be a relatively recent event. Nonsiliceous algae recovered in conjunction with pollen from Big Rice, Cloquet, Gegoka, and East Bearskin lakes indicate that each lake has undergone cycles of nutrient enrichment. Changing environmental or limnologic competition, or both, as well as competition by macrophytic vegetation, is indicated by oscillations in nonsiliceous algae abundance. Gramineae abundance data and Gramineae pollen grain size distribution data indicate that wild rice was probably present in harvestable quantities in northeast Minnesota in late Paleoindian times and has persisted up to the present. Gramineae pollen grain size distribution data was especially useful in identifying the probable presence of prehistoric wild rice in lakes that have Gramineae pollen profiles with low to moderate abundances. The advantages of using both palynological methods to determine prehistoric wild rice lakes is demonstrated by the Wild Rice Lake Reservoir pollen sequence. Preliminary data indicate a much greater association of Woodland sites and historic wild rice lakes than of Paleoindian/ Archaic sites and wild rice lakes. This suggests that wild rice became a more important food resource in the Woodland Period.