The composition, recruitment rates and fine-scale spatial dynamics of the sessile benthic community occupying hard substrata off Lee Stocking Island, The Bahamas, was determined through photography and the deployment of artificial substrata from September 1993 to September 1996. The study spanned 10 to 250 meters in depth. The benthic community exhibited a pronounced bathymetric zonation. Filamentous and macroalgae dominated the shallow communities , but were replaced by corals, sponges and endolithic algae with increasing depth. Living cover was high above 100 m, but declined significantly below this depth, being replaced by increasing amounts of bare and sediment-covered rock surfaces. Benthic zonation was shifted downward with respect to other locations in the western Atlantic, possibly due to the clear waters of Exuma Sound allowing relatively deep light penetration. Recruitment experiments were deployed during two time inten :als from 1994 to 1995. The experiments enabled the analysis of the effects of five treatments which differed in depth, orientation and degree of exposure. Recruitment of all sessile taxa declined sharply with depth. Peak recruitment for most taxa occurred between 20 m and 50 m. Recruitment experiments retrieved from sites located above 50 m exhibited high cover of :filamentous and macroalgae on exposed surfaces. Sponges, corals and other invertebrates dominated the cryptic surfaces. Dominance by polychaetes characterized the deeper sites. Fine-scale changes in community structure were determined through repeat photography of natural substrata and artificial settling panels. Numerical change indices were generated for changes in cover and additions and losses of individual organisms occurring over time. Each change index began at a relatively low value at the 10 m depth, increased to a maximum value at 30 m or 50 m and then declined with increasing depth. Numbers of fish grazing scars were positively correlated with the loss index and negatively correlated \\ith algal cover, suggesting that fish contribute to fine-scale changes in the sessile community. Important contributors to fine-scale spatial changes within the benthic community shift from algae to corals to sponges with increasing depth.

Thesis (M.A.)--Acadia University, 2000. / Includes bibliographical references (leaves 102-107). Also available on the Internet via the World Wide Web.

Holocene and Pleistocene grainstone deposits surrounding Ocean Cay located on the western margin of Great Bahama Bank provide key evidence for the comprehension of patterns, processes and petrophysical heterogeneity of carbonate grainstone shoals. New datasets consisting of high-resolution remote sensing data, acoustic Doppler current measurements, sub-bottom profiles, and sedimentological and petrophysical analyses offer an opportunity to elucidate the various factors in the deposition of a grainstone shoal complex and assess of how much of the sedimentary fabric and early diagenetic overprint influences the petrophysical characteristics of similar ancient deposits. The Holocene shoal complex investigated here includes the Cat Cay ooid shoal and the Ocean Cay tidal deltas, which collectively form a 1-3 km wide, 35 km long sand belt around Ocean Cay. These factors controlling the distribution, preservation and modification of these sediments are the antecedent Pleistocene topography, bathymetry, and hydrodynamics at this margin. High-resolution seismic data reveal that the laterally continuous and thick Cat Cay ooid shoal north of Ocean Cay is situated on top of a flat Pleistocene surface and located platformward of a Pleistocene rock ridge. This finding challenges the assumption of previous studies that an antecedent high is needed for ooid shoal initiation. In contrast, south of Ocean Cay, skeletal-rich tidal deltas occur east of rocky Pleistocene islands and formed over an irregular Pleistocene surface that is slightly shallower than the flat surface north of Ocean Cay. In addition to the antecedent topography, differences in shoal morphology and sediment attributes between the north and south areas around Ocean Cay are related to linkages among fluid flow patterns, shoal morphology and granulometry. The hydrodynamic data document the influence of tidal flows in modifying the shape of bars creating sinuous and parabolic forms during flood and ebb reversing flows. Spatial distribution of grain size and sorting is affected because high flow velocities (up to 100 cm sec-1) inside tidal channels and inlets can erode and remobilized sediments mixing skeletal grains, peloids and ooids. Dominance of flood tide across this Holocene shoal complex allowed tidal deltas to form bankward of inlets between rock islands. Tidal channels and inter-bar troughs can focus tidal flow during flood tide creating lobes platformward instead of previously assumptions on the effect of storm and formation of spillover lobes bankward. Cores from the subsurface at Ocean Cay show that the architecture of the Pleistocene grainstone facies is similar to the Holocene shoal configuration of bars, channels, and bioturbated stabilized areas. Cross-bedded oolitic/peloidal and bioturbated skeletal/peloidal facies exhibit facies-dependent petrophysical heterogeneity, and reveal depositional and early diagenetic controls on petrophysical properties. Porosity and permeability in the grainstones at Ocean Cay are high, up to 47% and up to 11500 mD, respectively. Early diagenesis modifies the pore geometry of the rock, thus reducing permeability. A comparison of petrographic and petrophysical properties of the Pleistocene shoal with those from the Pennsylvanian ooid shoals reveals that were strongly influenced by the original fabric and early near-surface diagenesis. The integration of data from both the modern and ancient carbonate systems provides a better understanding of the factors controlling shoal morphology, facies architecture, and rock properties. The results of this study can be used as a guide for interpreting heterogeneity and reservoir properties of analogous facies within ancient ooid shoals.

During the past 500 years, the Bahamas has been influenced by a wide array of settlers, including but not limited to, the Arawak Indians, Eleutherian Adventurers, British Loyalists, Creole slaves, liberated Africans as well as Chinese, Greek, Jewish, Lebanese, Jamaican and Haitian migrants. To date, however, only a few reports analyzing the genetic makeup and population dynamics of the Bahamas have been published, making this work pivotal in the endeavor to ascertain the genetic ancestry of these groups. As such, the current investigation was undertaken to genetically characterize six of the more densely populated islands throughout the Northwest (Grand Bahama and Abaco) and Central (Eleuthera, Exuma, Long Island and New Providence) Bahamas using different forensic marker systems. When autosomal STR markers are employed, the Bahamian collections were all found to receive differential contributions from the African, European, East Asian and Native American collections utilized in the analyses. Similar findings were also observed for two other Afro-Caribbean populations, Haiti and Jamaica, although the latter populace was found to share a greater proportion of its autosomal component with non-African sources than the former. On the contrary, analysis of the six Bahamian collections using high-resolution Y-chromosome markers identifies genetic signals emanating exclusively from Africans and Europeans, but this is likely the result of smaller sample sizes collected from each island and/or sex-biased gene flow from East Asian and Native American groups.

A major economic constraint in the Bahamas, and other small carbonates islands world-wide, is the lack of fresh water resources. To combat these socio-economic problems on San Salvador Island I sought to gain a more detailed understanding of the extent, behavior, and controls on the island’s fresh-water lens. DC electrical resistivity tomography and time-series geochemical data are used to study the fresh water lens at the Line Hole well field. Electrical Resistivity profiles are used to image the extent of fresh water resources. Time-series geochemical data provide information on the behavior of the fresh water resources as a function of time. The inversion models of the electrical resistivity profiles illustrate a fresh water lens less than 3 meters thick on average. The mixing zone is diffuse in nature, and substantially thicker than the fresh water lens. The geochemical results corroborate the fresh water lens dimensions predicted by the electrical resistivity model. In addition, mixed semi-diurnal and spring/neap tidal cycles are the primary control on the water level. Statistical analysis of specific conductance and temperature illustrate a positive and negative correlation with water level, respectively. Analysis of precipitation with respect to water level and geochemistry indicate low effective recharge rates during the period of study. The current state of the water resources at the Line Hole well field is strained. Despite moderate levels of freshening since the termination of pumping in December 2006; the system continues to be in a state of disequilibrium. The problem is compounded by abnormal thickening of the mixing zone due to communication of the well field with the ocean, and a limited volume of fresh water. In conclusion, the two techniques used in conjunction provide a non-invasive method of estimating fresh water resources in this type of setting. Conversely, the high RMS and L2 values for the electrical resistivity models and limited time-series data create a high level of uncertainty in the interpretation of results.