A one-kilometer-diameter carbonate/hydrate mound in Mississippi Canyon Block 118 has been chosen to be the site of a multi-sensor, multi-discipline sea-floor observatory. Several surveys have been carried out in preparation for installing the observatory. The resulting data set permits discussing the mound’s structure in some detail. Samples from the water column and intact hydrate outcrops show gas associated with the mound to be thermogenic. Lithologic and bio-geochemical studies have been done on sediment samples from gravity and box cores. Pore-fluid analyses carried out on these cores reveal that microbial sulfate reduction, anaerobic methane oxidation, and methanogenesis are important processes in the upper sediment. These microbial processes control the diffusive flux of methane into the overlying water column. The activity of microbes is also focused within patches near active vents. This is primarily dependent upon an active flux of hydrocarbon-rich fluids. The geochemical evidence suggests that the fluid flux waxes and wanes over time and that the microbial activity is sensitive to such change. Swath bathymetry by AUV combined with sea-floor video provides sub-meter resolution of features on the surface of the mound. Seismic reflection profiling with source-signature processing resolves layer thicknesses within the upper 200-300m of sediment to about a meter. Exploration-scale 3-D seismic imaging shows that a network of faults connects the mound to a salt diapir a few hundred meters below. Analyses of gases from fluid vents and hydrate outcrops imply that the faults act as migration conduits for hydrocarbons from a deep, hot reservoir. Source-signature-processed seismic traces provide normal-incidence reflection coefficients at 30,000 locations over the mound. Picking reflection horizons at each location allows a 3-D model of the mound’s interior to be constructed. This model provides a basis for understanding the movement of fluids within the mound.

In order to analyze the stability of Eastern Black Sea Coastal Highway defense structures constructed with natural stone armor layers, hydraulic model tests were performed under both breaking and non-breaking waves. Eight different alternative cross-sections of the defense structures were constructed in the wave flume in Coastal and Harbor Engineering Laboratory, Civil Engineering Department, METU. Water depth was kept constant at a depth of 7.5 m in front of the structures. Model scale, &amp / #955 / L, was calculated as 1:31.08 using Froude Law. Experiments were carried out for wave heights, H, ranging between 3 &ndash / 7 m. with a wave period ranging between 6 &ndash / 11 sec in prototype. A comparative economical analysis of the alternative cross-sections of the defense structures has proven that cost (per meter) differs almost 50% between the alternative cross-sections.

Scleractinian cold-water corals are widely distributed in seaways and basins of the North Atlantic Ocean, including the Straits of Florida. These corals can form extensive biogenic mounds, which are biodiversity hotspots in the deep ocean. The processes that lead to the genesis of such cold-water coral mounds and control their distribution and morphology are poorly understood. This work uses an innovative mapping approach that combines 130 km2 of high resolution geophysical and oceanographic data collected using an Autonomous Underwater Vehicle (AUV) from five cold-water coral habitats in the Straits of Florida. These AUV data, together with ground-truthing observations from eleven submersible dives, are used to investigate fine-scale mound parameters and their relationships with environmental factors. Based on these datasets, automated methods are developed for extracting and analyzing mound morphometrics and coral cover. These analyses reveal that mound density is 14 mound/km2 for the three surveyed sites on the toe-of-slope of Great Bahama Bank (GBB); this density is higher than previously documented (0.3 mound/km2) in nearby mound fields. Morphometric analyses further indicate that mounds vary significantly in size, from a meter to up to 110 m in relief, and 81 to 600,000 m2 in footprint area. In addition to individual mounds, cold-water corals also develop in some areas as elongated low-relief ridges that are up to 25 m high and 2000 m long. These ridges cover approximately 60 and 70% of the mapped seafloor from the sites at the center of the Straits and at the base of the Miami Terrace, respectively. Morphometrics and current data analyses across the five surveyed fields indicate that mounds and ridges are not in alignment with the dominant current directions. These findings contradict previous studies that described streamlined mounds parallel to the northward Florida Current. In contrast, this study shows that the sites dominated by coral ridges are influenced by unidirectional flowing current, whereas the mounds on the GBB slope are influenced by tidal current regime. The GBB mounds also experience higher sedimentation rates relative to the sites away from the GBB slope. Sub-surface data document partially or completely buried mounds on the GBB sites. The sediments burying mounds are off-bank material transported downslope by mass gravity flow. Mass gravity transport creates complex slope architecture on the toe-of-slope of GBB, with canyons, slump scars, and gravity flow deposits. Cold-water corals use all three of these features as location for colonization. Coral mounds growing on such pre-existing topography keep up with off-bank sedimentation. In contrast, away from the GBB slope, off-bank sedimentation is absent and coral ridges grow independently of antecedent topography. In the sediment-starved Miami Terrace site, coral ridge initiation is related to a cemented mid-Miocene unconformity. In the center of the Straits, coral ridges and knobs develop over an unconsolidated sand sheet at the tail of the Pourtales drift. Coral features at the Miami Terrace and center of the Straits have intricate morphologies, including waveform and chevron-like ridges, which result from asymmetrical coral growth. Dense coral frameworks and living coral colonies grow preferentially on the current-facing ridge sides in order to optimize food particle capture, whereas coral rubble and mud-sized sediments accumulate in the ridge leesides. Finally, this study provides a method using solely acoustic data for discriminating habitats in which cold-water corals are actively growing. Results from this method can guide future research on and management of cold-water coral ecosystems. Taken together, spatial quantitative analyses of the large-scale, high-resolution integrated surveys indicate that cold-water coral habitats in the Straits of Florida: (1) are significantly more diverse and abundant than previously thought, and (2) can be influenced in their distribution and development by current regime, sedimentation, and/or antecedent topography.

Temperature is arguably the most important abiotic factor influencing the embryonic development in ectothermic species. Incubation temperature has demonstrated effects on offspring phenotypes in ectotherms, including traits such as sex, size, shape, colouration and post-hatch growth and survival. However, in endotherms the influence temperature has on development is relatively unexplored due to the narrow range of temperatures that embryonic endotherms are exposed to during develop. Megapode birds utilize environmental heat sources to incubate their eggs and therefore provide a potential model to test how temperature influences embryonic development and offspring phenotypes in endotherms. I used the Australian Brush-turkey (Alectura lathami), a megapode bird that incubates its eggs in mounds of soil and leaf litter to investigate the effects of temperature on embryonic development and chick morphology. Previous reports of Australian Brush-turkey incubation mound temperatures relied on spot measurements and theoretical modeling and thus have not provided a comprehensive examination of the range of temperatures Brush-turkey embryos are exposed to and how these might vary during the course of incubation. Therefore to examine the range of temperatures experienced by developing embryos I continuously recorded the temperature of eggs and mound material at naturally occurring positions within incubation mounds over the full developmental period. As in previous studies I found the average incubation temperature to be about 34°C, however egg temperatures typically fluctuated more than previously reported or predicted from modeling. The thermal tolerance of Brush-turkeys is remarkable compared to non-megapode birds, with embryos developing successfully despite prolonged exposure to sub-optimal temperatures over the range 25-40°C. I also demonstrated that the incubation period was negatively correlated with mean incubation temperature. To simplify the examination of temperature effects on embryonic development, constant temperature artificial incubation of Brush-turkey eggs was used to determine influence of incubation temperature on the energetics of embryonic development and the sex ratio, morphology and chemical composition of chicks. Because initial investigation of mound temperatures determined the mean incubation temperature in Brush-turkeys to be 34°C this was used as the preferred temperature for constant temperature incubation with 32°C and 36°C representing low and high temperatures respectively. Previously, the sex ratio of Brush-turkey chicks at hatching was shown to be temperature dependent. A thermally sensitive period early in development resulted in more females hatching from high temperature and more males hatching from low temperatures with an equal ratio at the preferred temperature. Using molecular sexing techniques to determine the sex of both failed embryos and chicks that hatched, I established that at laying the sex ratio of eggs was 50:50, and that temperature-dependent sex-biased embryo mortality was the mechanism behind the skewed sex ratio of chicks hatching from non-preferred temperatures. Low incubation temperature increased female embryonic mortality and high incubation temperature increased male embryonic mortality. This represents a novel mechanism operating to alter sex ratios in a bird species and offers an unparalleled system to explore sex allocation theory. It is well established that temperature influences the rate of development and the morphology of offspring in reptilian species. Also, in a previous study using artificially incubated Brush-turkey eggs, temperature was found to affect the mass of chicks but not their size (linear dimensions). This finding suggests that at different incubation temperatures the amount of yolk converted into tissue during embryonic development is influenced by incubation temperature. I tested this hypothesis by incubating eggs at different constant temperatures and found high incubation temperatures produce chicks with lighter yolk-free bodies and heavier residual yolks but similar linear dimensions compared to chicks hatching from lower temperatures. Because eggs incubated at low temperatures have longer incubation periods, I hypothesized the proportion of lipid in the yolk-free body would be higher in chicks emerging from eggs incubated at low temperature because more time is available for the conversion of yolk to fat bodies during embryonic development. This hypothesis was not supported as the composition of yolk-free chicks (total water, lipid, protein and ash) was not temperature dependent. A previous study in Malleefowl (Leipoa ocellata), another megapode bird, found that the total energetic cost of production was influenced by incubation temperature. Such that embryos developing at low temperatures required 72% more energy than embryos developing at high temperatures. However these findings were contrary to expectation from studies of reptilian incubation where the energetic cost of development is independent of temperature. Therefore I tested the hypothesis that the total energetic cost of development is temperature dependent in the Australian Brush-turkey. I used bomb calorimetry to measure the energy content of freshly laid eggs and of chicks (both the yolk-free body and residual yolk) that had hatched from eggs incubated 32oC, 34oC and 36oC. I found that the total energy content of chicks at hatching was greater in chicks emerging from eggs incubated at 34oC and 36oC compared to eggs incubated at 32oC. My thesis work demonstrated that incubation temperature is more variable for Brush-turkey embryos than for non-megapode birds and that even a small difference in temperature can have important effects on chick sex ratios, morphology and energy reserves. I have shown that incubation under artificial constant temperature conditions can significantly alter the developmental trajectories and phenotypic outcomes for chicks. In addition to laboratory based work, future studies should continue to examine how embryonic development and chick attributes are influenced by temperatures experienced under natural incubation conditions. Furthermore, investigation is required to determine how incubation temperature induced differences in hatchling phenotypes influence the post-hatch grow and fitness of chicks.

Thesis (Ph. D.)--University of Washington, 1988. / Vita. Bibliography: leaves [230]-248.

Thesis (Th. M.)--Dallas Theological Seminary, 2000. / Includes bibliographical references (leaves 153-160).

Thesis (D. Min.)--New Orleans Baptist Theological Seminary, 1997. / Abstract and vita. Includes bibliographical references (leaves 185-193).

Thesis (Th. M.)--Dallas Theological Seminary, 2000. / Includes bibliographical references (leaves 153-160).

Thesis (Th. M.)--Dallas Theological Seminary, 2000. / Includes bibliographical references (leaves 153-160).

Thesis (M.A.) -- University of Tennessee, Knoxville, 2005. / Title from title page screen (viewed on Sept. 1, 2005). Thesis advisor: Lynne P. Sullivan. Document formatted into pages (x, 229 p. : ill., maps (some col.)). Vita. Includes bibliographical references (p. 170-180).