This dissertation examines the shrimp industry in the Gulf of California from a political ecology perspective. The interaction between fishermen and their marine environment is explored, as well as the historical factors that led to vastly different types of fishermen in the communities of Guaymas and Empalme. Some have specialized in the harvesting of shrimp; others are diversified, multiple species fishermen. Some are highly industrialized offshore shrimpers; others are small-scale fishermen, more modest in their technology but more resilient when facing the current crisis in the shrimp industry. The underlaying causes of this crisis are explored by looking at state development policies, the assumptions behind fisheries management, and the configuration of markets. These have all emphasized specialization in the production of shrimp while ignoring the high interannual variability characteristic of shrimp populations. The end result: an overcapitalized, overexpanded industry and a possible overexploitation of shrimp stocks. Rather than addressing the root causes of the crisis, recent policies have instead transferred rights to the offshore fishery from cooperatives to private investors. At the same time there has been a concerted attack against small-scale producers. It is believed that by getting rid of this sector, catch per boat in the offshore sector will increase and overall "efficiency" will be improved. I compare industrialized trawlers and the small-scale sector and argue that the latter is currently producing high quality shrimp at lower monetary and ecological costs. But small-scale fishing is not equated with sustainability. Instead, differences among small-scale fishermen are analyzed. I contend that those who belong to traditional fishing families and have access to collective knowledge about the marine environment that has accumulated through generations, are better able to deal with a highly unpredictable environment and minimize risk. Those who do not have access to this knowledge have specialized in the harvesting of shrimp. I argue that a strategy of diversification is both more profitable in the short-term and sustainable in the long-run. Avoidance strategies among small-scale fishermen in response to externally imposed regulations are also examined. Fishermen are analyzed as individual profit maximizers and as community members who break the rules to serve collective interests. Just as individuals act collectively to deal with an unpredictable environment, they also act collectively to effectively challenge the institutions of rule-making.

The formation of the Gulf Co-operation Council (GCC) in 1981 was perceived by most observers to be a collective security response to the Iran-Iraq war. Despite this view, the group has endured ten years of integration in a turbulent region and has survived: external threats to its sovereignty, Islamic fundamentalism, the decline of oil prices, internal unrest, attempted coups, and the invasion and occupation of a constituent member. This poses the question: has the integration of these countries proved to be a success? This thesis attempts to answer this question with the aid of a three dimensional analysis. The first dimension examines the theory and practice of integration. Its primary objective is to provide an insight into integration. As the GCC can, at best, be categorised as a Customs Union, this chapter concentrates on Free Trade Areas and Customs Union theories and explores their relationships with tariffs, protectionism, developing countries, and politics. A review of the empirical analyses in the field is essential due to the fact that a mathematical technique is applied to GCC trade in the latter part of this thesis. The existence of political, economic and manpower factors are found to be more detrimental to the GCC's interests than its adherence or convergence to the theory and practice of integration. An analysis of these three factors constitutes the second dimension of the thesis. This commences by examining the Islamic antecedents of the member countries, pan-Islamism and nationalism in the 19th century, and Middle Eastern efforts at integration from the decline of the Ottoman Empire to the present. The establishment of the existing GCC nations and an examination of their natural resources, demography, industry, infrastructure, agriculture, and fisheries is covered, as is the impact of the 1990-91 occupation of Kuwait and the BCCI liquidation. A review of manpower factors includes an examination of the labour market in the pre and post 1973 period with emphasis given to the role of expatriate and indigenous labour. In addition, the influence of education, women in the workforce, nationality, and residence policies on indigenous labour is discussed. The third dimension reviews the prospects of the GCC. This is performed through the construction and utilisation of matrices which examine the similarity or dissimilarity of GCC trade to the World, Developed and Developing Countries. United Nations Standard Industrial Trade Category (SITC) data up to 3-digits, has been used to construct twenty seven 22 x 22 matrices. Nine of these matrices indicate GCC trade with the Rest of the World and are linked to economic and financial literature on the Gulf in order to examine their credibility. Eighteen matrices which indicate trade with the Developing and Developed World indentify potential trade creation, trade diversion and prospects. It is the conclusion of the thesis that the GCC has not succeeded in its integration efforts. The lack of co-ordination to perform as a single unit in economic, political, and military areas, the undemocratic political systems, the exploitation of expatriate labour, the segregation of indigenous labour, and most importantly, the wasted opportunities indicated by the matrices of greater trade creation with the Developed and Developing Countries contribute significantly to the ineffectiveness of the group.

Approved for public release, distribution is unlimited / Events at the beginning of the 21st century have brought a fundamental change to the security environment in the Kingdom of Saudi Arabia of a significance not witnessed in the region since the Iranian Revolution in 1979. The fall of Saddam Hussein's regime in 2003 eliminated the most significant external threat facing Saudi Arabia. At the same time, internal threats to the Kingdom appear to be increasing. The demographic and economic challenges facing the Kingdom are contributing to internal instability. Increased instances of political violence, particularly suicide bombings against targets within the Kingdom, have been carried out by terrorists linked to al-Qaeda. These attacks have targeted Westerners and, for the first time in May 2003, non-Saudi Muslims. This paper examines the security challenges facing Saudi Arabia at the start of the 21st century. It argues that while external threats to the Kingdom remain, the greater threat to security may lie within the Saudi state: the result of a failure to address current political realities. Major security challenges include the threat from Iran, economic and demographic pressures, the question of succession within the ruling al-Saud family and maintaining the U.S.- Saudi security partnership, a relationship which has endured over 50 years. / Captain, United States Air Force

Cheung Mong. / Thesis (M.Phil.)--Chinese University of Hong Kong, 2004. / Includes bibliographical references (leaves 115-121). / Abstracts in English and Chinese. / Abstract --- p.i / Acknowledgements --- p.iii / Table of Contents --- p.iv / List of Tables and Figures --- p.vi / Abbreviations --- p.viii / Chapter Chapter One --- Introduction: Why Different Policy Responses in Two Similar Crises? --- p.1 / Chapter 1.1 --- Central Question --- p.1 / Chapter 1.2 --- Main Argument --- p.2 / Chapter 1.3 --- The Layout --- p.4 / Chapter Chapter Two --- A Theoretical Framework for Analysis: The Concept of Strategic Culture --- p.6 / Chapter 2.1 --- Competing Explanations --- p.8 / Chapter 2.2 --- The Theory of Strategic Culture --- p.19 / Chapter 2.3 --- Defining Strategic Culture in this Research --- p.29 / Chapter 2.4 --- Research Method and Data --- p.37 / Chapter Chapter Three --- The Dual Sources of Strategic Culture in Postwar Japan --- p.39 / Chapter 3.1 --- Paradigm in the Ruling Level: Yoshida Doctrine --- p.40 / Chapter 3.2 --- Paradigm in the Social Level: Pacifism --- p.47 / Chapter 3.3 --- The Interaction between the Two Paradigms on Policy --- p.52 / Chapter 3.4 --- Summary --- p.56 / Chapter Chapter Four --- Japan's Responses to the Gulf Crisis: The Gap of Two Paradigms (1990-91) --- p.59 / Chapter 4.1 --- Searching for a New Identity: Four Views to Japan's Security --- p.60 / Chapter 4.2 --- The Two Competing Paradigms in the Eve of the Gulf Crisis --- p.65 / Chapter 4.3 --- A Strategic Cultural Explanation to the Reluctant Response on Overseas Dispatch --- p.72 / Chapter Chapter Five --- Japan's Responses to the Anti-Terrorism War: Moving towards An Unitary Paradigm (2001) --- p.82 / Chapter 5.1 --- "Japan's Emerging New Identity: The Notion of ""the Normal Nation""" --- p.83 / Chapter 5.2 --- Decline of the Pacifism --- p.92 / Chapter 5.3 --- Japan after the 911: Sending the SDF Overseas --- p.98 / Chapter Chapter Six --- Conclusion --- p.118 / Chapter 6.1 --- Japan Between the Pacifist Nation and Great Military Power --- p.109 / Chapter 6.2 --- The Significance and Limitation of the Research --- p.112 / Bibliography --- p.115

The corvina reina (Cynoscion albus) is an important part of the artisanal fishery in the Gulf of Nicoya, Costa Rica. Stock assessment on this sciaenid species has been restricted to the use of length-based methods because of the lack of age data. Direct age determination methodologies for tropical species often encounter serious difficulties such as poorly defined hyaline and opaque zones and lack of adequate techniques of ageing. This thesis presents the results of an age-determination study of Cynoscion albus based on otolith surface readings and microincrement analysis. Age estimates were obtained from counts of hyaline zones from surface readings using the light microscope and from microincrement readings from cross sections of the otolith using the scanning electron microscope. Validation of age estimates from surface readings was based on a linear regression of the age estimates from surface readings on age estimates from integrated daily increment readings. Growth of the otolith was studied using linear and multivariate regression methods and the results were used to construct multivariate models for prediction of age. Consistent estimates of age and fish growth parameters were obtained from surface and microincrement analysis. This study showed that Cynoscion albus is a slow-growing fish (K = 0.121) and reaches a large size (L∞ = 127.5 cm) and therefore is likely to suffer overfishing in the Gulf of Nicoya fishery. / Graduation date: 1993

A molecular phylogenetic approach was used to characterize the composition of microbial communities from two gas hydrate sedimentary systems in the Gulf of Mexico. Nucleic acids were extracted from three distinct locales on surface breaching gas hydrate mounds, i.e., sediment overlaying gas hydrate, sediment/hydrate interface and sediment-free hydrate, and from three sediment depths, i.e., 0-2, 6-8 and 10-12 cm, in Beggiatoa sp. mat-associated sediments located several meters from exposed gas hydrate. Samples were collected from a research submersible (water depth 550-575 m) during two research cruises aboard the R/V Seward Johnson I and II funded by the NSF Life in Extreme Environments program. The 16S rRNA gene and 16S rRNA were amplified using PCR and reverse transcription-PCR, respectively, from DNA and RNA extracted from the total microbial community. The primers targeted microorganisms at the domain-specific, i.e., Bacteria and Archaea, and group-specific, i.e., sulfate-reducing bacteria (SRB) and putative anaerobic methane-oxidizing (ANME) archaea, level. Sequence analysis of the Bacteria clones revealed that the microbial communities were primarily dominated by Deltaproteobacteria. Other Proteobacteria classes, including Epsilon- and Gammaproteobacteria, represented a large fraction of the total microbial community isolated from the sediment overlying hydrate sample and the metabolically active fraction of the 0-2 cm sediment depth sampled from the Beggiatoa sp. mat-associated sediments. Sequence analysis indicated the majority of the archaeal clones were most closely related to Methanosarcinales, Methanomicrobiales and distinct lineages within the ANME groups. Several novel lineages were identified including a fourth ANME-2 clade, i.e., ANME-2D, and three clades with no closely related previously sequenced 16S rRNA gene clones or isolates, i.e., Unclassified Bacteria groups 1 and 2 and Unclassified Euryarchaeota. These studies represent the first 16S rRNA gene and 16S rRNA phylogenetic-based description of microbial communities extant in sediment-free gas hydrate and in methane-rich hydrate-associated and Beggiatoa sp.-associated sediments from a hydrocarbon seep region in the Gulf of Mexico.

The goal of this record of study is to examine the major facets involved in managing several petroleum service projects located in three different countries in the Gulf of Guinea simultaneously, while effectively engaging in business development activities for the Oil and Industrial Services Group (OIS). This work also furnishes adequate background on related subject matters to enable understanding of the projects presented. The petroleum services sector is the back bone of the oil and gas industry. Services companies are vital to the success of all petroleum and energy producers in the USA, the Gulf of Guinea and the world. There is a need and demand for these service companies because they play various roles such as logistics, drilling, construction, dredging, pipe laying, procurement, food supply, human resource supply, etc. The Gulf of Guinea comprises of countries from west and central Africa. This project was limited to Nigeria, Equatorial Guinea and Cameroon. This area holds the largest petroleum reserves in Africa and plays a vital role in the global supply of petroleum. The Oil and Industrial Services Group (OIS), plans to establish herself as one of the leading petroleum service companies in this gulf. To manage this expansion, I have taken the role of Gulf of Guinea manager to apply my background as a petroleum engineer as well as my business skills to build a successful division of the company. This work provides a record of study of the management of services, projects and contracts carried out by the OIS group in the gulf of Guinea. The following are the specific projects in the Gulf of Guinea that I participated in: Managing delivering, maintenance and marketing of offshore vessels, Offshore pipe laying project, Integrated pipeline maintenance project, Development a petroleum technical training facilities, Agbami pipe insulation project, Engineering lift project and Capital budgeting analysis for potential investments. The details of the specific tasks of the job, including objectives, description, managerial role, nontechnical aspects, approaches, information sources, discussions and contributions are projected in the body of this literature.

Natural vents in the Gulf of Mexico are actively expelling water and hydrocarbons. They are ubiquitous along continental margins, and I characterize a single vent in the Ursa Basin at leaseblocks MC852/853. Seismic data reveal that the vent is elevated ~75 meters above the seafloor and is roughly circular with a ~1.2 km diameter. A transparent zone centered underneath the vent extends to ~1500 meters below seafloor; this zone is commonly interpreted to record the presence of gas. There is a strong negative polarity seismic reflection that rises rapidly at the vent’s boundaries and is horizontal within a few meters of the seafloor beneath the vent edifice. I interpret that this reflection records a negative impedance contrast, marking the boundary between hydrate and water above and free gas and water below: it is the bottom-simulating reflector. Salinities beneath the vent increase from seawater concentrations to >4x seawater salinity one meter below seafloor. Temperature gradients within the vent are ~15x the background geothermal gradient. I model the coexistence of high salinity fluids, elevated temperature gradients, and an uplifted bottom-simulating reflector with two approaches. First, I assume that high salinity fluids are generated by dissolution of salt bodies at depth and that these hot, saline fluids are expelled vertically. Second, I model the solidification of gas hydrate during upward flow of gas and water. In this model, free gas combines with water to form hydrate: salt is excluded and heat is released, resulting in the generation of a warm, saline brine. The two models result in predictable differences of salinity and temperature. A better understanding of the hydrogeological processes at vent zones is important for quantifying the fluxes of heat and mass from submarine vents and is important for understanding the conditions under which deep-sea biological vent communities exist. / text

Over 7000 sq. km of salt and six Plio-Pleistocene biostratigraphic horizons were mapped in the East Breaks and Garden Banks areas using a 12,000 km grid of seismic data and all obtainable well data. Structure mapping of allochthonous Jurassic salt and the six horizons (Globoquadrina altispira, Lenticulina 1, Angulogerina B, Hyalinea B, Trimosina A, and Sangamon Fauna) and isopachs of the intervals between these horizons revealed notable lateral variations in the area underlain by salt, in the degree of salt deformation, and in the size and thickness of associated intraslope basins. East of 94.5° W salt structures occupy 40% of the area and exhibit complex shapes that suggest a high degree of salt deformation. West of 94.5° W salt structures occupy 11% of the area and consist mostly of structurally simple salt stocks. A zone of high-offset north-south trending faults mark the transition between these two areas. Isopach maps of the six Plio-Pleistocene intervals (from 2.9 Ma to the present) reveal major shifts in the rates and locations of sediment accumulation. From 2.9 to 1.0 Ma. sediment-accumulation rates averaged only 0.8-1.3 mm/y with a maximum rate of 2.7 mm/y. From 1.0 to 0.69 Ma. sediment-accumulation rates averaged 5.8 mm/y with a maximum rate of 11.6 mm/y. This interval correlates to sediments deposited between the extinctions of Hyalinea balthica and Trimosina denticulata and recorded a major period of sediment loading/salt withdrawal between 1.0-0.69 Ma. From the end of this time to the present, sediment -accumulation rates averaged 1.7-2.1 mm/y with a maximum rate measured at 6.2 mm/y. Increased sediment influx during 1.0-0.69 Ma coincides with a major third order sea level lowstand and was focused in central Garden Banks. The restriction of such dramatically increased accumulation rates to this area suggests that sediment influx was accompanied by large-scale salt withdrawal. The increase in accommodation space created by salt withdrawal appears to be the most important factor affecting accumulation rates. Salt structural styles found on the upper continental slope are transitional between those found on the lower slope and those on the shelf. The shelf is dominated by isolated, individual salt stocks (km²) surrounded by kilometer thick sedimentary sections. The lower slope is dominated by broad, laterally continuous, allochthonous salt sheets (10³ km²) with moderate to thin sediment cover. The upper slope contains both of these structural styles plus intermediate size (10-10² km²) salt ridges and massifs. Observations made during this study suggest that differential sediment loading is the mechanism causing the changes in structural style. A Loading/Dissection model is presented to explain the formation of the three primary salt structural styles, their genetic relationship, and their observed distribution. Differential loading has dissected large salt sheets into numerous smaller and irregularly shaped ridges and stocks (like those found on the upper slope). Salt found on the upper slope originated in the Jurassic Louann Formation, but is now surrounded by Pleistocene age sediments. To achieve this relationship, it appears that some Jurassic salt has undergone at least two cycles of sediment loading and consequent diapirism. Salt/sediment relationships suggest that virtually all of the mapped salt is allochthonous. Repetitive sediment loading and salt structural development has not been previously documented and represents a step beyond the limits of current salt structural models. / text

The study area is located on the continental slope in the Green Canyon deep-water area of the Gulf of Mexico. This area is being investigated by the Bureau of Economic Geology as part of several active gas hydrate studies across the area. The chirp sonar profiles used in my study were collected with an Autonomous Underwater Vehicle (AUV) utilizing a frequency-modulated seismic (sonar) source that emitted a 2 to 8 kHz sweep (chirp) frequency signal (wavelengths less than 2 meters). The recording time is limited to about 50 milliseconds, with time zero occurring at the altitude of the AUV about 50 meters above the seafloor. The signal images to about 40 meters below the seafloor, and profiles are as long as 5 km. An interpretation of deep-water, near sea-floor geology has been conducted using both chirp sonar profiles and multibeam bathymetry. Seismic reflections from within the shallow sediments are caused primarily by contrasts in density, rather than acoustic velocity. Reflections were successfully simulated using a model with a constant velocity of 1560 m/s and densities of 2.1 g/cc for sand, 1.4 g/cc for mud, and 1.7 g/cc for silty sand. The chirp sonar profiles imaged near-seafloor geology at nearly a meter scale and allowed for detailed interpretation. The interaction of soft sediment deformation, creep movement and neo-tectonic activity related to gas expulsion controlled the actual topography of the sea-floor. The geologic time represented in the 50 milliseconds of chirp data recorded with the AUV, which is about 40 meters of depth, is approximately 0.050 Ma. B.P., consistent with a depositional rate of 0.8 meters per 1000 years. Reflection patterns are interpreted to be related to fluctuations in sea level. High reflectivities (density contrasts) are interpreted to be deposited during the last sea level low stand, and low reflectivities are interpreted as sedimentation during the last high stand. Sediments deposited during the low stand are proximal while others are distal, deposited in deeper water environments. Shallow structures observed in the chirp sonar profiles are mainly related to gas mobilization mechanisms, which shaped the topography of the seafloor in conjunction with soft sediment deformation and creep movement. The geomorphic features are related in some cases to gas expulsion zones such as pockmarks and mud volcanoes. Other structures are related to soft sediment deformation and creep mobilization. Soft sediment deformation is confined to the deepest part of the minibasin, while the other features are not depth dependent. Highly deformed intervals at the bottom of the sequence seem to control subsequent sedimentation. / text