Thesis (Ed. D.)--University of Missouri-Columbia, 1998. / Typescript. Vita. Includes bibliographical references (leaves 194-205). Also available on the Internet.

Thesis (Ed. D.)--University of Missouri-Columbia, 1998. / Typescript. Vita. Includes bibliographical references (leaves 194-205). Also available on the Internet.

Thesis (Ph. D.)--University of Missouri-Columbia, 1999. / Typescript. Vita. Includes bibliographical references (leaves 128-139). Also available on the Internet.

Thesis (D. Min.)--Northern Baptist Theological Seminary, Lombard, Ill., 1998. / Abstract. Includes bibliographical references (leaves 359-368).

Thesis (Ph. D.)--University of Wisconsin--Madison, 1969. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references.

Thesis (D. Min.)--Covenant Theological Seminary, 2005. / Abstract. Includes bibliographical references (leaves 166-171).

Thesis (D. Min.)--Covenant Theological Seminary, 2005. / Abstract. Includes bibliographical references (leaves 166-171).

This thesis is an interdisciplinary comparative analysis of the socio-economic developments of three regions in Anatolia: Lycia, Isauria and north central Anatolia in the late antique period (c. AD 330-600s). I present the most up-to-date picture of late antique settlement in these regions by collating recent evidence, particularly amphorae and settlement remains, derived from research conducted in these regions over the past few decades. From this picture, I analyse what the location of settlement and archeological remains within sites may reveal concerning the ways in which settlements participated in local, region and interregional exchange networks. As these three regions share the common geographic features of bordering major maritime areas and encompassing mountainous interiors, I examine how geography may have impacted the location of settlement and the movement of goods and people. By integrating areas located on opposite Anatolian coastlines, I examine how differing maritime networks may have impacted settlement development. This tripartite comparison attempts to establish northern Anatolia alongside its southern counterpart in the discourse of late antique economy and settlement development. Alongside this regional analysis, I discuss methodological considerations, such as the ways in which the current state of research and various research methods impact our analysis and interpretation of late antique settlement development. This study reveals that sub-regions within Lycia, Isauria and north central Anatolia developed in diverse ways and that the ways in which each region participated in wider exchange differed. I argue that overarching narratives of development, such as 'prosperity' and 'decline' do not accurately reflect the development of these regions. In sum, this thesis contributes an up-to-date analysis of the settlement development of Lycia, Isauria and north central Anatolia to the wider discourse of late antique regional development, which engages and challenges discourse surrounding the economic development of these regions in Late Antiquity.

A population of the red-eared slider, Pseudemys scripta, in north central Texas was studied from 1975 to 1980. A life history energy budget was developed for a typical individual in the population and the population dynamics were estimated. A growth model relating growth rate to mean plastron length (PL) was developed from recapture data and used to 1) establish age classes and 2) age individuals. Growth rate was highly variable in both sexes. Females grew more rapidly than males and attained a larger maximum size (230 mm and 195 mm PL in females and males respectively). Females reached sexual maturity in their ninth year at a PL of 185-190 mm. Males matured in their sixth year at a PL of 90-100 mm. Females produced three clutches annually; clutch size ranged from 7 to 14 (X=10.3; N=20). Ova were enlarged in the early spring and ovulation began in late April and early May. Egg laying occurred from mid- May through June. Both egg size and clutch size increased with female body size. Lipid levels were variable within and among seasons. No annual lipid cycling pattern was evident in females. The proportion of assimilated energy devoted to reproduction, a measure of reproductive effort (RE), by females, was 13 per cent the first year of maturity (9 y) and increased to 20 per cent by their twentieth year. Lifetime RE was 16 per cent. Population density was estimated as 51 males and 50 females per ha in a 8.2-ha area of the lake. Young juveniles (less than 2 y) were not present although other subadult age classes were about equally represented. Fewer adults were encountered. An annual total production of 4000 eggs was estimated for the population present in 1977. A survival rate of from 2 to 18 per cent was estimated for the period between egg laying to 3 y. The large group of turtles younger than 10 y represented an expanding (Rₒ=1.8) lake population and the small group of older turtles were the remnants of a creek population present before Moss Lake was formed. The demographic environment, high juvenile mortality and low adult mortality, was suggested as a primary selective force shaping the life history characteristics of the Moss Lake scripta population.

This study integrates detailed mapping of Tertiary deposits along the divide between the lower Bear River basin and the Cache Valley basin with several other techniques to generate a depositional model, define extension-related structures, and compile a geologic history for this part of the northeastern Basin and Range province. The study area is situated along the topographic divide between Box Elder and Cache Counties, Utah, from the Wellsville Mountains north almost to Clarkston Mountain. These ranges are cored by folded and thrusted Paleozoic rocks. They are bound on the west by normal faults of the Wasatch fault zone and on the east by the West Cache fault zone. Between these two fault zones, poorly consolidated Tertiary deposits of the Wasatch Formation and Salt Lake Formation overlie Paleozoic rocks in the foothills and low divide between the north-trending ranges. The Miocene to Pliocene Salt Lake Formation accumulated above non-tuffaceous conglomerates of the Paleocene to Eocene Wasatch Formation, up to 0.5 km thick in the Wellsville Mountains, but thin or absent northward. The Salt Lake Formation in the study area consists of an apparently non-tuffaceous lower conglomerate member, up to 0.5 km thick in the Wellsville Mountains, and a widespread younger tuffaceous and lacustrine member, at least 1 km thick. The traditional names of Collinston Conglomerate and Cache Valley Member were used for these two lithologies. The Cache Valley Member was further subdivided into a local tuffaceous basal conglomerate, a widespread tuffaceous subunit, and an overlying oolitic subunit. Normal faults in the study area comprise three groups. North-striking normal faults are the youngest, and include major range-bounding faults. East-striking normal faults are less numerous, and are cut by the north-striking faults. The southwest-dipping low-to moderate-angle Beaver Dam fault separates the Cache Butte Divide and Junction Hills from the Wellsville Mountains. It may be unique within the area of study, and may comprise a newly identified segment of the Wasatch fault zone. Most of its displacement appears to pre-date the late Miocene, at the time that previous authors have suggested for the onset of Basin-and-Range normal faulting.