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OSL Dating of a Woodland Period Occupation at the Hare Hammock Ring and Mound Complex, Bay County, FloridaHodson, Alex 15 December 2015 (has links)
This study used OSL dating to examine the chronological relationship between
two adjacent archaeological sites at the Hare Hammock complex in northwest Florida.
High-resolution vertical sampling was performed at 10cm intervals in profiles, one
corresponding to a Swift Creek burial mound, and the other to a Weeden Island ring
midden. This was done in order to determine the timing of occupations at the sites and
look for patterns in radiation dosimetry. The Swift Creek mound was found to have a
mean OSL age of 1835 +/- 68 years, consistent with archaeological expectations of the
site and the accepted range of Swift Creek culture. The subsequent Weeden Island
occupation was also found to have OSL ages within expectations, with a mean age of
1049 +/- 43 years that overlies a single age of 1511 +/- 372 years, corresponding to the
Late and Early Weeden Island periods, respectively. The general coherence with
radiocarbon dates and ceramic chronologies affirms the veracity of these OSL ages,
which were obtained using a very recently developed dosimetric technique that applies
Al2O3:C cylinders as in-situ dosimeters. These dosimeters indicated that the sediments at
Hare Hammock contain significant heterogeneity in beta dose rates. This study finds that,
under these circumstances, the best age results are obtained when applying the refined
dosimetric technique which combines the beta dose rate from NAA/DNC and gamma
dose rate from Al2O3:C dosimetry. / Thesis / Master of Science (MSc)
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Searching for early archaeological sites along the central Oregon coast : a case study from Neptune State Park (35LA3), Lane County, Oregon /Jenevein, Steve. January 1900 (has links)
Thesis (M.A.I.S.)--Oregon State University, 2011. / Printout. Includes bibliographical references (leaves 137-149). Also available on the World Wide Web.
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Asturian of Cantabria: Early Holocene Hunter-Gatherers in Northern SpainClark, Geoffrey A. January 1983 (has links)
The Anthropological Papers of the University of Arizona is a peer-reviewed monograph series sponsored by the School of Anthropology. Established in 1959, the series publishes archaeological and ethnographic papers that use contemporary method and theory to investigate problems of anthropological importance in the southwestern United States, Mexico, and related areas.
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Subsistence, butchery, and commercialization in Knox County, TennesseeWindham, Rachel Jeannine, January 2003 (has links) (PDF)
Thesis (M.A.)--University of Tennessee, Knoxville, 2003. / Title from title page screen (viewed Mar. 29, 2004). Thesis advisor: Walter E. Klippel. Document formatted into pages (ix, 135 p. : ill. (some col.)). Vita. Includes bibliographical references (p. 115-127).
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The taphonomic history of the vertebrate faunal assemblage from British Camp, San Juan Islands, WashingtonPegg, Brian Peter, January 1999 (has links) (PDF)
Thesis (M.A.)--Simon Fraser University, 1999. / Includes bibliographical references (leaves 106-113).
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Resource depression and intensification during the late Holocene, San Francisco Bay : evidence from the Emeryville shellmound vertebrate fauna /Broughton, John Michael, January 1995 (has links)
Thesis (Ph. D.)--University of Washington, 1995. / Vita. Includes bibliographical references (leaves [279]-331).
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Of millingstones and molluscs the cultural ecology of early Holocene hunter-gatherers on the California coast /Erlandson, Jon. January 1900 (has links)
Thesis (Ph. D.)--University of California, Santa Barbara, 1988. / Typescript. Vita. Includes bibliographical references (leaves 411-440).
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Stable isotopes, marine paleoclimates, and human subsistence on California's Channel IslandsRobbins, John A. January 2007 (has links)
Thesis (M.S.)--Southern Methodist University, 2007. / Includes bibliographical references.
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Biological affinities of archaic period populations from west-central Kentucky and TennesseeHerrmann, Nicholas Paul. January 2002 (has links) (PDF)
Thesis (Ph. D.)--University of Tennessee, Knoxville, 2002. / Title from title page screen (viewed Feb. 27, 2003). Thesis advisor: Lyle W. Konigsberg. Document formatted into pages (xii, 208 p. : ill., maps (some col.)). Vita. Includes bibliographical references (p. 180-202).
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Domestic refuse and residential mound formation in La Mixtequilla, Veracruz, Mexico.Hall, Barbara Ann. January 1991 (has links)
The Mesoamerican residential mound is a basic unit of archaeological analysis. The way mounds form has implications for reconstructing past social organization. Studies of formation processes assume that characteristics of refuse are the result of depositional history. Tracing the history of archaeological deposits is the first step toward understanding the social and economic milieu of the prehistoric household. The traces of mound formation processes particularly are evident in ceramics. This study examines measures such as density, mean size, and variation in size and wear, to determine their utility in ascertaining depositional history, including discard practices, erosion, and trampling. The measures are tested with the Exploratory Data Analysis method using visual inspection of the data for patterns and examination of exceptional cases. Density by weight and mean sherd size were found to be particularly useful and simple measures for differentiating archaeological deposits. The characteristics of artifacts in a deposit provide the basis for reconstructing the formation of mounds. Earthen residential mounds like those of Veracruz are low and broad and usually lack imperishable construction materials. Unlike Maya housemounds, which often use fill for mound construction, earthen mound formation resembles (on a smaller scale) the formation of tells, the remains of ancient villages and towns in Western Asia. For both tells and earthen mounds, the erosion of houses forms the bulk of mound sediments. Residential mound growth is more by gradual accretion than by deliberate construction, and is due to six main formation processes. These are: (1) the erosion of wattle-and-daub construction material, which contribute to mound sediments; (2) the gradual accretion of sediments and artifacts; (3) horizontal erosion of daub and artifacts; (4) secondary refuse deposition; (5) the occasional use of fill to expand or level the mound; and (6) the development of a humic topsoil layer commonly damaged by plowing. Through refuse characteristics it is possible to reconstruct mound growth, use of space, and the location of structures and refuse dumps. These formation processes distinguish earthen mound development in many parts of Mesoamerica.
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