Populations of all stages of three species of Hydropsychidae, Hydropsyche simulans, Cheumatopsyche campyla, and Cheumatopsyche lasia were sampled fro September, 1971, to August, 1972, on the Brazos River in Palo Pinto County, Texas. Supplemental observations relating to emergence, mating and oviposition, and larvae food habits were continued to July, 1973. The purpose of this study was to elucidate the life cycles and ecology of this Hydropsychidae complex.

The purpose of this report is threefold: 1) to provide a description and discussion of research undertaken in the Aquilla Lake area, Hill County, Texas, in 1979 and 1980; 2) to propose a regional research design for the entire Central Brazos region; and 3) to analyze evidence from the Aquilla investigations in terms of the proposed regional perspective. / text

Thesis (M.E.S.)--Baylor University, 2008. / Includes bibliographical references (p. 52-57)

Thesis (Ph. D.)--University of Texas at Austin, 2004. / Supervisor: David R. Maidment. Vita. Includes bibliographical references. Also available from UMI.

Most major Phanerozoic mass extinctions induced permanent or transient changes in ecological and anatomical characteristics of surviving benthic communities. Many infaunal marine organisms produced distinct suites of biogenic structures in a variety of depositional settings, thereby leaving an ichnological record preceding and following each extinction. This study documents a decrease in burrow size in Thalassinoides-dominated ichnoassemblages across the Cretaceous-Paleogene (K-Pg) boundary in shallow-marine sections along the Atlantic Coastal Plain (Walnridge Farm, Rancocas Creek, and Inversand Quarry, New Jersey) and the Gulf Coastal Plain (Braggs, Alabama and Brazos River and Cottonmouth Creek, Texas). At New Jersey sites, within a regionally extensive ichnoassemblage, Thalassinoides ichnospecies (isp.) burrow diameters (DTh) decrease abruptly by 26-29% (mean K=15.2 mm, mean Pg=11.2 mm; n=1767) at the base of the Main Fossiliferous Layer (MFL) or laterally equivalent horizons. The MFL has been previously interpreted as the K-Pg boundary based on last occurrence of Cretaceous marine reptiles, birds, and ammonites, as well as iridium anomalies and associated shocked quartz. Across the same event boundary at Braggs, Alabama, DTh of simple maze Thalassinoides structures from recurring depositional facies decrease sharply by 22% (mean K=13.1 mm, mean Pg=10.2 mm; n=26). Similarly, at the Cottonmouth Creek site, Texas, Thalassinoides isp. occurring above the previously reported negative £_13C shift and the first occurrence of Danian planktonic foraminifera are 17% smaller in diameter (mean K=21.5 mm, mean Pg=17.9 mm; n=53) than those excavated and filled prior to deposition of a cross-bedded, ejecta-bearing sandstone complex commonly interpreted as the Chicxulub ¡¥event deposit¡¦. At both of these impact-proximal regions, the Cretaceous and Paleogene burrows were preserved in similar lithologies, suggesting that a reduction in size cannot be attributed to sedimentological factors. At all localities, up-section trends in DTh are statistically significant (fÑfnf¬0.05; non-parametric Kruskal-Wallis test). Using the burrow diameter as a proxy for tracemaker body size, a reduction in DTh above the K-Pg boundary likely reflects dwarfing within the post-extinction community of decapod crustaceans. Dwarfing during the early recovery stages of the end-Cretaceous mass extinction, as recorded by ichnofossils, occurred within glauconite-producing (New Jersey), carbonate (Alabama), and siliciclastic (Texas) depositional environments and appears to be widespread. Because this ichnological signal appears to be a general phenomenon across the crisis interval, trace-fossil analysis provides a potential in-situ field method for constraining and correlating the stratigraphic position of the K-Pg and other extinction events, particularly in the absence of other macroscopic, microscopic, and geochemical indicators. Whereas overprinting of the original marine ichnofabric by morphologically similar continental traces is not a concern in lithified sections of Alabama and Texas, such an occurrence must be considered within unconsolidated sections. Within the Hornerstown Formation of New Jersey, a pervasive Thalassinoides framework contains traces of burrowing bees and wasps. Due to their penetration of up to 1 m, excavations just beyond the weathering front are insufficient for exposing the original marine ichnofabric. Insect burrow diameters (7-25 mm) are within the range of Thalassinoides traces (4-31 mm), exhibit occasional branching, and lack of ornamentation (bioglyphs) on the burrow walls. Therefore neither size nor gross morphology are adequate for distinguishing these widely diachronous and unrelated ichnites, especially when the insect burrows have been filled. However, the presence of backfill menisci and a beige clay halo help distinguish the ancient marine burrows, whereas highly oxidized fill and the occurrence of a terminal brooding chamber are diagnostic of modern insect burrows. / Geology

Genetic variation was examined at 19 loci encoding enzymatic and general proteins Notropis lutrensis from the Brazos River in Texas. The thermal regime of the Brazos River below Possum Kingdom Reservoir is altered due to the release of water from the hypolimnion. Summer water temperatures fluctuate as much as 7^oC. Levels of heterozygosity at the malate dehydrogenase-2 locus were correlated with the degree of water temperature fluctuation at each locality. The isozymes from three homozygous patterns of supernatant malate dehydrogenase (Mdh-l, Mdh-2) exhibited different activities at different experimental temperatures.

I investigated how land use and human activities affect the sources and cycling of carbon (C) in subtropical rivers. Annually rivers receive a large amount of terrestrial C, process a portion of this C and return it to the atmosphere as CO2. The rest is transported to the ocean. Land use and human activities can affect the sources and fate of terrestrial C in rivers. However, studies on these effects are limited, especially in the humid subtropics. I combined measurements of the partial pressure of dissolved CO2 (pCO2), C isotopes (13C and 14C) and solid-state 13C nuclear magnetic resonance (NMR) to study C cycling in three subtropical rivers in Texas, two small rivers (Buffalo Bayou and Spring Creek) and a midsized river (the Brazos). My pCO2 data show that small humid subtropical rivers are likely a large source of atmospheric CO2 in the global C cycle. My measurements on pCO2, C isotopic and chemical composition of dissolved inorganic C (DIC) and particulate organic C (POC) revealed four types of effects of land use and human activities on river C cycling. First, oyster shells and crushed carbonate minerals used in road construction are being dissolved and slowly drained into Buffalo Bayou and the lower Brazos and may be a source of river CO2 released to the atmosphere. Second, river damming and nutrient input from urban treated wastewater stimulate algal growth and reduce CO2 evasion of the middle Brazos. Third, urban treated wastewater discharge is adding old POC to the middle Brazos and decomposition of the old POC adds to the old riverine DIC pool. Fourth, agricultural activities coupled with high precipitation enhance loss of old organic C (OC) from deep soils to the lower Brazos, and decomposition of the old soil OC contributes to the old CO2 evaded. I document for the first time the river C cycling effects of the use of carbonate minerals in construction and the riverine discharge of urban wastewater. Results presented here indicate the need to study disturbed river systems to better constrain the global C budget.

Not available / text

This dissertation develops and utilizes a methodology for combining data drawn from the manuscript census returns and the county tax rolls to study landless farmers during the period from 1850 until 1880 in three Texas Brazos River Valley counties: Fort Bend, Milam, and Palo Pinto. It focuses in particular on those landless farmers who appear to have had no option other than tenant farming. It concludes that there were such landless farmers throughout the period, although they were a relatively insignificant factor in the agricultural economy before the Civil War. During the Antebellum decade, poor tenant farmers were a higher proportion of the population on the frontier than in the interior, but throughout the period, they were found in higher numbers in the central portion of the river valley. White tenants generally avoided the coastal plantation areas, although by 1880, that pattern seemed to be changing. Emancipation had tremendous impact on both black and white landless farmers. Although both groups were now theoretically competing for the same resource, productive crop land, their reactions during the first fifteen years were so different that it suggests two systems of tenant farming divided by caste. As population expansion put increasing pressure on the land, the two systems began to merge on terms resembling those under which black tenants had always labored.