The isotopic labelling of carbon in tree-rings varies as a function of growth season temperature and relative humidity. The isotopic labelling of oxygen in tree-rings varies as a function of source-water isotopic composition and humidity-dependent evaporative enrichment of leaf water during the growth season. The season of carbon-isotope labelling was identified statistically as late-spring to early-fall (April to October) for temperatures and relative humidity with a three-year weighted (50-30-20) carry-over due mainly to stored photosynthates. The season of oxygen-isotope labelling was identified statistically as a combination of a winter (pDecember to March) source-water signal (temperature-dependent precipitation isotope composition) with a late-spring to early-fall (April to October) humidity signal (evaporative enrichment of leaf water). A two-year carry-over was attributed to the residence time of soil water, but no notable photosynthate carry-over was identified. Carbon- and oxygen- (mechanistic) isotope response surface models were then compared and contrasted to regression-based bivariate and univariate models. It was found that in most cases the isotope response surface models were the best means of predicting isotopic labelling when environmental data are known. The carbon-isotope response surface was used to reconstruct 50-years (AD 1900-1954) of relative humidity data by introducing measured carbon isotope values and instrumental growth season temperature. During the analysis of the oxygen-isotope response surface we found an isotope-temperature relation that appears to reflect circulation-dependent damping. To verify this we introduced scaled values of the North Pacific index as a proxy for this suppression. The coupling of the isotope response surfaces generated a humidity reconstruction that is also thought to be driven by atmospheric circulation. Our reconstruction shows that the fluctuations in temperature range have not exceeded the natural variability in the instrumental record of the 20th century; however, the atmospheric moisture (humidity) reconstruction predicts a directional drying trend in the Peace-Athabasca Delta that appears to reflect increasingly zonal circulation in western Canada over this period.

The isotopic labelling of carbon in tree-rings varies as a function of growth season temperature and relative humidity. The isotopic labelling of oxygen in tree-rings varies as a function of source-water isotopic composition and humidity-dependent evaporative enrichment of leaf water during the growth season. The season of carbon-isotope labelling was identified statistically as late-spring to early-fall (April to October) for temperatures and relative humidity with a three-year weighted (50-30-20) carry-over due mainly to stored photosynthates. The season of oxygen-isotope labelling was identified statistically as a combination of a winter (pDecember to March) source-water signal (temperature-dependent precipitation isotope composition) with a late-spring to early-fall (April to October) humidity signal (evaporative enrichment of leaf water). A two-year carry-over was attributed to the residence time of soil water, but no notable photosynthate carry-over was identified. Carbon- and oxygen- (mechanistic) isotope response surface models were then compared and contrasted to regression-based bivariate and univariate models. It was found that in most cases the isotope response surface models were the best means of predicting isotopic labelling when environmental data are known. The carbon-isotope response surface was used to reconstruct 50-years (AD 1900-1954) of relative humidity data by introducing measured carbon isotope values and instrumental growth season temperature. During the analysis of the oxygen-isotope response surface we found an isotope-temperature relation that appears to reflect circulation-dependent damping. To verify this we introduced scaled values of the North Pacific index as a proxy for this suppression. The coupling of the isotope response surfaces generated a humidity reconstruction that is also thought to be driven by atmospheric circulation. Our reconstruction shows that the fluctuations in temperature range have not exceeded the natural variability in the instrumental record of the 20th century; however, the atmospheric moisture (humidity) reconstruction predicts a directional drying trend in the Peace-Athabasca Delta that appears to reflect increasingly zonal circulation in western Canada over this period.

Thesis (M.S.)--Florida State University, 2004. / Advisor: Dr. Cheryl Ward, Florida State University, College of Arts and Sciences, Department of Anthropology. Title and description from dissertation home page (viewed June 16, 2004). Includes bibliographical references.

Thesis (D. Min.)--Southwestern Baptist Theological Seminary, 2003. / Includes abstract. Includes bibliographical references (leaves 213-227).

Thesis (Ph. D.)--University of Chicago, Dept. of Anthropology, August 2001. / Includes bibliographical references. Also available on the Internet.

Thesis (M.A.) in History--University of Maine, 2002. / Includes vita. Bibliography: leaves 102-105.

This report is a case study of the Environmental Impact Statement (EIS) that was prepared by the U.S. Army Corps of Engineers Fort Worth District for the Upper Trinity River Central City Fort Worth, Texas EIS. It utilizes a system of best practices focused on four areas of concern: adequacy of the EIS public involvement and comment process, adequacy of the EIS content considerations, adequacy of analysis considerations, and adequacy of document quality. The basic premise of this report is that Environmental Impact Statements (EIS) should be analyzed outside of the Federal government in order to ensure that the National Environmental Policy Act (NEPA) remains a healthy statute that continues to serve the public. This particular EIS was chosen because of the magnitude of the project and the potential ramifications it poses for the City of Fort Worth. An important goal of this report is to not only evaluate this particular EIS, but to use it as a means for answering some general questions about the employment of NEPA in the Dallas and Fort Worth (DFW) Metroplex. Perhaps this report can also be of some assistance to individuals participating with the Corps’ preparation of the EIS for the Trinity River Corridor project in Dallas. / text

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Dene women are leading and directing efforts toward "healing" themselves, their families, and their communities. Employing a modality of montage and storytelling, this thesis explores this enigmatic concept of "healing" among Dene, and its gendered dimensions, in the community of Fort Good Hope, Northwest Territories. This account challenges the limitations of a resistance-hegemony paradigm often used to describe Aboriginal actions as embedded within colonial relations, and endeavours toward a more nuanced analysis which explores Dene "healing" beyond the colonial space. "Healing" is emerging as a vehicle for the assertion and celebration of Dene identity, Dene tradition and "Dene ways". This thesis further explores how many Dene women in Fort Good Hope are mobilizing the power of tradition, such as -aet'sechi/ (practices associated with "becoming woman"), as a means of "healing" social/health concerns, and influencing gender and power relations in the community.

Detailed study of strata associated with the glauconite-rich Floyds Knob Bed in the western Appalachian and eastern Illinois basins have corroborated previous interpretations that the unit is a widespread, largely synchronous marker horizon. However, in some areas there are multiple glauconite beds; in others a distinct bed is lacking, but the glauconite is dispersed throughout many beds, forming an interval rather than a distinct bed. In Kentucky and adjacent states, the Floyds Knob interval, in upper parts of the Lower-Middle Mississippian Borden-Grainger delta sequence and in lower parts of the Fort Payne carbonate sequence, was deposited at the end of loading-type relaxation during a flexural cycle in the Neoacadian (final) tectophase of the Acadian Orogeny. Tectonic influence, combined with a major late Osagean sea-level lowstand, created conditions that generated sediment starvation and shallower seas across widespread parts of the western Appalachian and eastern Illinois basins. In the absence of major sediment influx, glauconite was deposited uniformly across many major depositional settings, ranging from delta-platform to basinal environments. Especially important, however, is the newly reported occurrence of the Floyds Knob interval in basinal Fort Payne environments from south-central Kentucky, where it is represented by a thick, pelletal, glauconite-rich horizon that separates clastics at the base of the Fort. Payne Formation from carbonates at top. The study also provides the first-ever radiometric dating of the Floyds Knob glauconites, which suggests a late Osagean origin. These results support the existing biostratigraphic studies that point to a late Osagean origin for the Floyds Knob interval.