Thesis (Ph.D.)--Oregon, Dept. of Biology Vita Bibliography: l. 118-122

Thesis (Ph. D.)--University of Melbourne, 1972. / Includes appendices. Includes bibliographical references (p. 243-263).

Thesis (M.A.)--Central Connecticut State University, 1997. / Thesis advisor: Dr. Kim A. Wilson. " ... in partial fulfillment of the requirements for the degree of Master of Arts in Biology." Includes bibliographical references (leaves 47-56).

La glande surrénale est un organe endocrinien d’une importance vitale de par son rôle dans le maintien de l’homéostasie corporelle. Pour assurer cette fonction, le cortex surrénalien est divisé en différentes zones qui produisent des hormones spécifiques. Les mécanismes de la mise en place de cette zonation au niveau embryonnaire ainsi que de son maintien tout au long de vie sont encore inconnus de nos jours. Les gènes Rspo1 et 3 sont exprimés de manière très spécifique au niveau de la capsule mais ils codent pour des protéines secrétées qui agissent sur les cellules adjacentes de la zone glomérulée afin d’induire l’activation de la voie canonique Wnt/β-caténine. La délétion du gène Rspo3 pendant le développement embryonnaire entraine un défaut d’activation des voies Shh et Wnt/β-caténine et donc en conséquence un défaut de la mise en place de la zonation. Sa fonction reste également essentielle au cours de la vie adulte puisqu’elle assure à la fois le maintien de l’homéostasie tissulaire et de la zone glomérulée. L’absence du gène Rspo1, n’affecte pas le développement ni la zonation ou l’homéostasie de la glande surrénale. Par contre, si on l’exprime de façon ectopique dans tous le cortex surrénalien, entrainant une activation anormale de la voie Wnt/β-caténine dans cette zone, on peut observer une hyperplasie des glandes surrénales. A partir de 1 an d’âge, cette hyperplasie surrénalienne entraine une formation de tumeurs. Ce travail démontre donc que la capsule par le biais du gène Rspondin 3 agit comme un centre de signalisation capable de contrôler à la fois l’homéostasie par le remplacement des cellules endommagés et le maintien de la zonation de la glande surrénale / The adrenal gland is an endocrine organ of vital importance because of its role in the maintenance of body homeostasis. To ensure this function, the adrenal cortex is divided into different areas that produce specific hormones. The mechanisms of the establishment of this zonation at the embryonic level as well as its maintenance throughout life are still unknown today. The Rspo1 and 3 genes are expressed very specifically at the capsule level but they encode secreted proteins that act on the adjacent cells of the zona glomerulosa in order to induce the activation of the Wnt / β-catenin canonical pathway. The deletion of the Rspo3 gene during embryonic development leads to a lack of activation of the Shh and Wnt / β-catenin pathways and hence a lack of zonation. Its function is also essential during adult life since it ensures both the maintenance of tissue homeostasis and the glomerular zone. The absence of the Rspo1 gene does not affect development, zonation or homeostasis of the adrenal gland. On the other hand, its ectopical expression in all the adrenal cortex leads to an abnormal activation of the Wnt / β-catenin pathway in this area and thus to an hyperplasia of the adrenal glands. From 1 year of age, this adrenal hyperplasia leads to the formation of tumors. This work demonstrates that the capsule through the Rspondin 3 gene acts as a signaling center capable of controlling both homeostasis by replacing damaged cells and maintaining the zonation of the adrenal gland

The liver is an essential organ for cholesterol homeostasis. If this process becomes dysregulated, cardiovascular disease (CVD) develops. Zinc-fingers and homeoboxes 2 (Zhx2) as an important hepatic gene regulator and contributes to CVD. BALB/cJ mice, with mutant Zhx2 allele, have fewer atherosclerotic plaques compared to other strains on a high fat diet. In my dissertation, I focused on the liver phenotype in BALB/cJ mice on a high-fat diet and found increased liver damage compared to wild-type Zhx2 mice. These data indicates that reduced Zhx2 in the liver leads to CVD resistance, but increases liver damage. Therefore, Zhx2 has an important role in lipid metabolism and liver function. Hepatic alpha-fetoprotein (AFP) is expressed abundantly in the fetal liver and repressed after birth regulated through three enhancers (E1, E2, and E3). E3 activity is restricted to a single layer of hepatocytes surrounding central veins (pericentral region) along with glutamine synthetase (GS). In my dissertation, I explore pericentral gene regulation in the adult liver. A GS enhancer (GSe) also exhibits pericentral activity which, along with E3, is regulated by the β-catenin signaling pathway. Orphan receptors, Rev-erbα, Rev-erbβ, and RORα, contribute to E3 activity elucidating a potential mechanism for zonation.

Residual mapping is an automated groundwater-model calibration technique which rapidly identifies parameter-zone configurations, while limiting tendencies to over-parameterize. Residual mapping analyzes the model residual, or the difference between model-calculated head and spatially-interpolated observation data, for non-random trends. These trends are entered in the model as parameter zones. The values of hydrologic variables in each parameter zone are then optimized, using parameter-estimation software. Statistics calculated by the parameter-estimation software are used to determine the statistical significance of the parameter zones. If the parameter-value ranges for adjacent zones do not have significant overlap, the zones are considered to be valid. This technique was applied to a finite-difference, transient groundwater flow model of a major municipal well field, located in west-central Florida. A computer conde automates the residual mapping process, making it practical for application to large, transient flow models. The calibration data set includes head values from 37 monitor wells over a period of 181 days, including a 96-day well-field scale aquifer-performance test. The transient residual-mapping technique identified five significant transmissivity zones and one leakance zone.

Biogeographic patterns across a landscape are developed by the interplay of environmental processes operating at different spatial and temporal scales. This research investigated dynamics of salt marsh vegetation on the Skallingen salt marsh in Denmark responding to environmental variations at large, medium, and fine scales along both spatial and temporal spectrums. At the broad scale, this research addressed the importance of wind-induced rise of the sea surface in such biogeographic changes. A new hypothetical chain was suggested: recent trends in the North Atlantic Oscillation index toward its positive phase have led to increased storminess and wind tides on the ocean surface, resulting in increased frequency, duration, and magnitude of submergence and, hence, waterlogging of marsh soils and plants, which has retarded ecological succession. At the mid-scale, spatial patterns of vegetation and environmental factors were examined across tidal creeks. Sites closer to tidal creeks, compared to marsh interiors, were characterized by the dominance of later-successional species, higher bulk density, and lower nutrient contents and electrical conductivity. This finding implies that locations near creeks have experienced a better drainage condition than the inner marshes, which eventually facilitated the establishment of later-successional plants that are intolerant to physical stress. At the micro-scale, this research examined how the extent and mode of facilitation and competition vary for different combinations of plant species along physical gradients. Both positive and negative relationships were spatially manifested to a greater degree on the low marsh than on the mid marsh. This insight extends our current knowledge of scale-dependent interactions beyond pioneer zones to higher zones. On the low marsh, different types of bivariate point pattern (i.e., clustered, random, and regular) were observed for different combinations of species even at similar spatial scales. This finding implies that it is difficult to generalize at which scales competition and facilitation occur. To conclude, this research stresses the need for a holistic approach in future investigations of salt marsh biogeography. For example, based on results of this current research, it would be meaningful to develop a comprehensive simulation model that incorporates salt marsh ecology, geomorphology, and hydrology observed across scales.

Macrobenthos of the deep, northern Gulf of Mexico have been sampled with large box cores along multiple cross-depth transects extending from depths of 200 m out to 3700 m. Four major depth zones have been identified based on the faunal similarities (beta diversity) between geographic sites, with the two intermediate-depth zones being divided horizontally down the middle of the basin. The input of food resources appears to control the observed patterns. Each zone and sub-zone can be described by a characteristic animal density, biomass and biodiversity (alpha diversity). Highest densities and biomass occurred in two large submarine canyons, the Mississippi and De Soto Canyon, but the two habitats are markedly different. The alpha diversity displays an intermediate depth maximum. Species richness (gamma diversity) is highest on east mid-slope, due, we suggest, to habitat complexity, but alpha diversity is lowest at the canyon head due to extreme dominance by amphipods. Small mean individual size and low densities encountered are a reflection of the meager surface water primary production, albeit with exceptional isolated habitats in which detrital material is concentrated, such as canyons on the upper continental slope.

Estuarine wetlands and salt marshes are fundamentally driven by variations in freshwater inflow. In semi-arid salt marshes, such as the Nueces River Delta, TX, the stochastic nature of freshwater inflow events exposes resident organisms to a wide range of environmental conditions. In this study, we investigate (1) the relative importance of environmental variables on porewater salinity and (2) determination of freshwater inflow needs based on the response of emergent plants to salinity variations. Porewater salinity variations were tracked on a continuous basis with deployed conductivity sensors and on a synoptic basis with soil water extracts. We found that spatial patterns of porewater salinity were characterized by a high degree of variability in creekbank areas (23.8 ± 7.68) relative to interior marsh areas (44.2 ± 3.4). Our observations were used to test a simple model capable of predicting porewater salinities based on environmental variables. Both empirical measurements and model simulations indicated that semiannual tides play a critical role in controlling porewater flushing from precipitation and freshwater inflow events. Estimation of freshwater inflow needs for the Nueces Delta proceeded in two steps. First, we examined the response of three common emergent plants species (Borrichia frutescens, Spartina alterniflora, and Salicornia virginica) to variations in salinity. The abundance of one species in particular (S. alterniflora) was tightly coupled to salinity variations whereby salinities exceeding 25 ± 5 resulted in dramatic declines in coverage. Next, the relationship between freshwater inflow and porewater salinity was examined with respect to the salinity “tolerance” of S. alterniflora. Estimated inflow needs based on maintenance of substantial (> 20%) S. alterniflora coverage was comparable to both previous inflow needs estimates and mean annual inflows observed over the course of the study. The results of this study suggest that S. alterniflora abundance provides a reliable indicator of overall estuarine hydrological condition in the Nueces Delta. / text

Volatiles are fundamental to many aspects of kimberlite magmatism. However, the volatile compositions and concentrations are poorly defined. Enrichment of H in kimberlitic olivines, many of which are xenocrysts, suggests high water content, but the extent to which H exchanges between these xenocrysts and kimberlite magmas remains unclear. This study investigates zonation of H in kimberlite-hosted xenolith and macrocrystic olivines using Fourier transform infrared spectroscopy to constrain the extent of re-equilibration. Data show that, depending on locality, xenolith olivines exhibit either no H-zonation, or substantial H-depletion in their rims. Macrocrysts feature similar trends to xenolith olivines from the same intrusion. In terms of the rim:core ratio of H, strongly zoned olivines average ~0.5, whereas poorly zoned olivines average at ~0.9 (macrocrysts) or 1.0 (xenolith olivines). Locality-specific H-zonation could result from different magmatic thermal regimes, water concentrations, or ascent durations. If the magmas that contained weakly zoned olivines were anhydrous, their restricted zoning requires ascent durations (< 20 min at 1100 °C) that are considerably shorter than published estimates (~1-24 hr at 1100 °C). These findings suggest that elevated magmatic water concentrations minimized loss of H from olivine in these kimberlites, showing that non-equilibrated xenocrysts could indirectly record high water concentrations in the form of weak H-zonation. Strong H-depletion patterns in olivines from other kimberlites may reflect lower initial magmatic water concentrations, or loss of fluid to country rocks. Future studies could compare H-zonation to temperature and ascent rate estimates, and field relationships to better elucidate the causes of locality-specific H-zonation. An apparent correlation between diamond grade and H-zonation warrants further investigation. / This thesis includes an Electronic Appendix, available at http://dalspace.library.dal.ca