xvii, 175 leaves : ill. ; 29 cm Notes Typescript Thesis (Ph. D.)--University of Oregon, 2002 Includes vita and abstract Includes bibliographical references (leaves 150-175) Another copy on microfilm is located in Archives

ix, 119 leaves : ill., maps ; 28 cm Notes Typescript Thesis (Ph. D.)--University of Oregon, 1985 Includes vita and abstract Bibliography: leaves 108-119 Another copy on microfilm is located in Archives

Typescript. Includes vita and abstract. Bibliography: Includes bibliographical references (leaves 77-80). Description: xii, 80 leaves : ill. ; 29 cm. / The lower distributional limits (fronts) of callianassid shrimp populations were observed at five sites in South Slough, Coos Bay estuary, Oregon. Fronts at four sites exhibited similar shoreward-seaward movements while the remaining site showed drastic population reductions. Shrimp density and body size were found to be significantly greater above than below the front. There was no consistent pattern found in grain size or interstitial water content across the front. In a controlled predator-exclusion experiment, resulting shrimp densities were not significantly different among treatments. Front shifts showed no pattern in response to treatments. These results imply that fish predation is not responsible for front placement. Trawls taken on both sides of the front produced similar densities of a predatory fish, Leptocottus armatus. Because predation pressure was calculated to be roughly equal above and below the front, Leptocottus is not expected to be responsible for position and movements of these fronts.

Coastal marshes serve important ecologic and economic functions, such as providing habitat, absorbing floodwaters and storm surges, and sequestering carbon. Throughout the northern Gulf of Mexico, coastal marshes are disappearing due to wave attack, sea-level rise, sediment export, and subsidence. Marsh area increases when sediments accumulate at the marsh shoreline, accrete vertically, and when non-marsh areas are colonized by marsh vegetation. Marsh shoreline erosion results in net marsh loss when transgression rates at the marsh-water edge exceed upland-marsh migration. The balance between marsh destroying and marsh creating processes determines the long-term survivability of a marsh system. Thus, processes of shoreline change are important considerations when evaluating the overall health and vulnerability of coastal marshes. Shoreline erosion can be measured using remotely sensed data in a geographic information system. Using shoreline position delineated from aerial imagery, historic maps, and field surveys, shoreline change analysis estimates long- and short-term shoreline movements to identify erosion or accretion for coastal marshes at the Grand Bay National Estuarine Research Reserve (GBNERR) and Wildlife Refuge (GBNWR) on the border of Mississippi and Alabama, USA. However, these techniques do not directly provide information on sediment deposition on the marsh surface. To understand sediment deposition, four study sites provide in-situ measurements of sediment deposition using sediment plates and sediment tracers (silica beads) that were collected every three months. Analysis of the shoreline change data and in-situ sediment data for the GBNERR showed that in 2017, all of the shorelines at the study sites are eroding at rates between -0.50 m/yr and -3.39 m/yr, an average rate of -1.45 m/yr. Positive sediment deposition rates were measured from 5-20 meters inland of the marsh shoreline during each season (3-month period) (0.19 ± 0.05 cm [Fall], 0.26 ± 0.11 cm [Winter], 0.48 ± 0.12 cm [Spring], 0.63 ± 0.15 cm [Summer]), indicating sediment deposition increased with every season. Sediment tracer (silica-bead) counts confirmed that sediment was transported onto the marsh surface from eroding marsh shorelines. Higher energy sites had more beads deposited on the sediment plates than the low energy tidal creek site, due to the different wave and tidal conditions between the sites. Increased wave and tidal energy correlated to increased sediment transport further into the marsh. The relative importance of this marsh cannibalism for the long-term marsh survival depends on factors, such as wave attack, as they control the rate of persistent lateral marsh loss. This findings in this thesis suggests that material from eroding marsh edges contributes to the ability of the interior of marshes to maintain their elevation with respect to rising sea levels.

Thesis (M.S.)--University of Akron, 2006. / Title from PDF title page (viewed on Jan. 25, 2007). Includes bibliographical references (p. 62-68).

Estuaries are valuable ecosystems that are easily affected by human activities within the watershed. One determinant of water quality for in an estuary is the presence of suspended sediments. The use of satellite sensors to remotely sense visible and near-infrared reflectance allows for suspended particulate matter (SPM) and suspended particulate inorganic matter (SPIM) concentrations to be monitored on a repetitive synoptic scale. Previously presented algorithms for relating remote sensing reflectance (Rrs) and SPM/SPIM concentrations were evaluated for the Weeks Bay estuary in Alabama. Additionally, numerous potential SPM/SPIM concentration retrieval algorithms using the Landsat-8 satellite were determined through regression analysis, as well as through the consideration of the inherent optical properties of the water body. The most robust empirical algorithm produced an RMSE of 12.50% and utilized the band combination of Ln(Band4)/Ln(Band3), while the most robust semi-analytical algorithm produced an RMSE of 16.34% and utilized the band combination of Band4/Band3.

Changes in freshwater inputs due to water diversions and increased urbanization may alter the function and properties of estuarine ecosystems in South Texas. Freshwater and nitrogen inputs from the Mission and Aransas rivers to the federally designated Mission-Aransas National Estuarine Research Reserve (Mission-Aransas NERR) have received considerable attention in the past few years. However, freshwater inputs from two rivers (the San Antonio and Guadalupe rivers) that combine and drain into a neighboring bay (San Antonio Bay) may also provide a substantial nitrogen source to Aransas Bay, which is within the boundaries of the Mission-Aransas NERR. In order to study the influence of the San Antonio and Guadalupe rivers, an oyster species, Crassostrea virginica, was chosen to provide time-integrated information about freshwater contribution as a nitrogen source within the bays. Chapter One addresses variations in isotope values ([delta]¹⁵N and [delta]¹³C) in oyster adductor muscle tissue from 2009-2011 along a sampling transect from the head of San Antonio Bay through Aransas Bay. Stable carbon isotope values increased linearly from approximately -25 % to -17 %, while stable nitrogen isotope values decreased from approximately +16 % to +10 % along this transect. The patterns in stable carbon and nitrogen isotope values are consistent with substantial mixing of river-supplied water and nitrogen from San Antonio Bay into Aransas Bay. Variations in nitrogen isotopic signature between periods of sustained drought and flood conditions were relatively small, suggesting that riverine nitrogen contributions were similar regardless of the amount of freshwater inflow observed during the time frame of this study. Chapter Two addresses the isotopic equilibration time for adult oyster adductor muscle tissue using a year-long transplant experiment (November 2010-November 2011). Full representation of ambient water isotopic composition in oyster adductor muscle tissues was determined to occur roughly a year after transplant. Oyster adductor muscle could therefore be useful for long-term monitoring of nitrogen contribution from freshwater sources, and would be valuable to include in concert with water sampling and analysis of other tissues that have shorter integration rates for a comprehensive view of an estuarine system. / text

Typescript. Includes vita and abstract. Bibliography: Includes bibliographical references (leaves 54-60). Description: xi, 60 leaves : ill. ; 29 cm.

Typescript. Includes vita and abstract. Bibliography: Includes bibliographical references (leaves 90-96). Description: xii, 96 leaves : ill. ; 29 cm.

Typescript. Includes vita and abstract. Bibliography: Includes bibliographical references (leaves 87-100). Description: xiii, 100 leaves : ill. ; 29 cm.