No description available.

Thesis (Ph.D.)--Texas Christian University, 2009. / Title from dissertation title page (viewed May. 5, 2009). Includes abstract. Includes bibliographical references.

Thesis (M.S.)--University of Wisconsin--La Crosse, 1972. / Digitized and made available by the University of Wisconsin--La Crosse, Murphy Library. Includes bibliographical references (leaves 40-41). Online version of print edition.

Thesis (M.S.)--University of Wisconsin--Madison, 1966. / eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.

Published also as Thesis (Ph. D.)--University of Pennsylvania, 1906. / Includes bibliographical references (p. 153-160).

Thesis (M.A.)--Georgia State University, 2006. / Title from title screen. Jack Boozer, committee chair; Shirlene Holmes, Marian Meyers, committee members. Electronic text (138 p.) : digital, PDF file. Description based on contents viewed June 19, 2007. Includes bibliographical references (p. 28-30).

Bottomland hardwood forests present a unique opportunity to examine the ecological response to hydrologically altered river and floodplain systems. These ecosystems, under natural conditions, are floodplain forests directly linked to the river. However, with major alterations to the river-floodplain system, bottomland hardwood forests can now provide insight into the loss of river connectivity and history of the flood pulse. This study reviewed the age distribution and growth of Quercus lyrata Walt. and the anatomical response of Quercus spp. to high magnitude floods in the 19th and 20th century in an old-growth Mississippi River floodplain forest in southeastern Missouri. Tree-ring samples collected from 43 trees at Big Oak Tree State Park contain physiological signatures (`flood rings') associated with growing season floods in the 20th century, and similar signatures are present in years corresponding to historical floods of the 19th century. The duration of 20th century Mississippi River growing season floods were examined to compare the occurrence of flood rings and the duration and intensity of floods on the Mississippi River at New Madrid, Missouri. Patterns in the occurrence of flood rings are developed as a response to alterations to the Mississippi River, river floodplain, and park hydrologic system.

Due to habitat degradation and overharvest (Colombo et al. 2007) sturgeon populations are declining throughout their global distribution (Pikitch et al. 2005). In North America, five sturgeon species are listed as endangered or threatened due to overharvest and habitat degradation. One species of direct concern is the pallid sturgeon (Scaphirhynchus albus ) (Boreman 1997). The morphologically similar shovelnose sturgeon (S. platorynchus) is not listed as endangered but has become a cause for concern due to poor reproductive success and declining recruitment of their offspring to the adult population, likely a result of lack of proper spawning habitat and early life foraging opportunities (Wildhaber et al. 2007). Despite listing the pallid sturgeon as endangered and increasing concern about population decline, little information is available about the foraging ecology of age–0 Scaphirhynchus sturgeon. To ensure these sturgeon populations persist in the Middle Mississippi River, a better understanding of sturgeon foraging success during early life is imperative. I quantified age–0 Scaphirhynchus sturgeon (total length (TL) range: 14–200 mm; small < 50 mm TL, large 50–200 mm TL) diets during 2004–2008 to determine whether foraging behavior changed as a function of stage height, water temperature, water velocity, size class of sturgeon, and macrohabitat. I also examined whether energy density (cal/g) and selection of prey varied across size class and macrohabitat. Age–0 Scaphirhynchus sturgeon were collected from the Middle Mississippi River during spring (March, April, May), summer (June, July, August), and fall (September, October, November). Each prey item in diets was identified to family and measured to calculate dry weight. Ephemeroptera, Diptera pupae, and Chironomidae were the dominant taxa that were consumed across all years and seasons. Large sturgeon had a broader diet, consuming more non–dominant taxa. Abiotic factors differed across macrohabitats and thus influenced foraging behavior. Sturgeon occupying the island upstream tip (IUT) macrohabitat had the largest mean mass in diet and those at the island downstream tip (IDT) had the lowest mean mass in diet. Conversely, energy density of sturgeon was highest at IDT and lowest at IUT. Small sturgeon avoided macroinvertebrates that were outside the dominant prey taxa whereas large sturgeon selected for Chironomidae across all macrohabitats. Diets of age–0 Scaphirhynchus sturgeon vary as a function of size and are influenced by interacting of abiotic and biotic factors at each macrohabitat. As age–0 Scaphirhynchus sturgeon grow, their diet broadens. Diet of young sturgeon interacts with energy condition in counterintuitive ways that requires more study. Because foraging success differs among habitats and is likely linked to recruitment, habitat quality and quantity in the Middle Mississippi River is likely critical for sturgeon population density and growth.

Knowledge of habitats used by riverine fishes throughout their life history is important for management and conservation. Naturally occurring chemical markers in otoliths have recently been used to determine natal origins and environmental history of fishes in a variety of marine and freshwater environments. However, to our knowledge no studies have examined the applicability of this technique in large floodplain rivers in United States. We evaluated otolith microchemistry and stable isotopic composition as tools for determining origins of fishes in the upper and middle Mississippi and lower Illinois Rivers, their tributaries, and associated floodplain lakes. Fishes were collected from 21 sites during summer 2006 and 2 additional sites in spring 2007. Water samples were obtained from the same 23 sites plus three additional sites during summer and fall 2006 and spring 2007. Otoliths and water samples were analyzed for δ18O, and a suite of trace elements; otoliths were also analyzed for δ13C. Tributaries, floodplain lakes, and the Illinois and Mississippi Rivers had distinct isotopic and elemental signatures. Tributaries on the Missouri and Illinois sides of the middle Mississippi River could also be differentiated by their elemental and isotopic fingerprints. Otoliths reflected differences in water chemistry among habitats. Results indicate that otolith microchemistry and stable isotope analyses provide a potentially effective means of determining origins and environmental history of fishes in large river-floodplain systems.

Insight into environments and habitats that contribute recruits to adult fish stocks in riverine systems is vital for effective population management and conservation. Catfishes are important recreational species in the Mississippi River and are commercially harvested. However, contributions from main channel and tributary habitats to catfish recruitment in large rivers such as the middle Mississippi River (between St. Louis, MO and Cairo, IL) are unknown. Stable isotope and trace elemental signatures in otoliths have been useful for determining environmental history of fishes in a variety of aquatic systems, including the Mississippi River. The objectives of this study were to identify the principle natal environments of channel catfish Ictalurus punctatus and blue catfish I. furcatus in the middle Mississippi River (MMR) using otolith stable oxygen isotopic composition (δ18O) and strontium:calcium ratios (Sr:Ca). Catfish were sampled in the MMR during July-October 2013 and 2014 and lapilli otoliths were analyzed for δ18O and Sr:Ca. Water samples from the MMR and tributaries were collected seasonally from 2006-2014 to characterize site-specific signatures. Persistent differences in water δ18O and Sr:Ca among the MMR and tributaries (including the upper Mississippi, Illinois, and Missouri rivers as well as smaller tributaries) were evident, enabling identification of natal environment for individual fish. Results indicated that blue and channel catfish stocks in the MMR primarily recruited from the largest rivers (Missouri and Mississippi rivers) in our study area and received minimal influence from smaller tributaries. Recruitment and year class strength investigations and efforts aimed at enhancing blue and channel catfish spawning and nursery habitats should be focused in the large rivers with less emphasis in the smaller tributaries.