Journal articles on the topic 'St. George Utah'

The history of Southeast Missouri State University parallels that of other teacher education institutions. It started as Southeast Missouri Normal School in 1873 and reached university status in 1972. A department of Geology and Geography was established in 1909, becoming the Geography Department in 1915. In 1924, the sciences were combined into the Science Department. In 1960, this became the Division of Science and Mathematics and the Department of Earth Sciences was formed. An earth science major began in 1937, with separate geology and geography majors established in 1958. Recently the Department has developed more specialized, job-oriented programs in mining geology and in cartography. Since 1983 the Department has also operated a field camp, headquartered on the campus of Dixie College, St. George, Utah.

ABSTRACT Two types of unusual concretions with similar biotic contents but markedly different shapes and distributions were found in close stratigraphic proximity within the Lower Jurassic Whitmore Point Member of the Moenave Formation in St. George, Utah. Both types of concretions formed in lacustrine sediments and contain abundant ganoid fish scales, numerous ostracode carapaces, and apparent rip-up clasts. Elongate, cylindrical concretions developed in parallel and regularly spaced rows in one horizon, and comparatively flat and irregularly shaped and distributed concretions formed in an overlying layer only a few centimeters above. Microprobe and Raman analyses of concretion samples reveal abundant hematite in both concretions as well as groundmass minerals dominated by silica in the cylindrical concretions and dolomite in the flat concretions. The abundance of fish skeletal debris in concretions from two consecutive horizons may suggest recurring fish mass mortality in ancient Lake Dixie, the large lake that occupied the St. George area during the Early Jurassic. We propose a model for the formation of the concretions based on their shapes, distributions, and chemistry. In this model, accumulations of disarticulated fish debris were colonized and consolidated by microbial mats and shaped by oscillatory flow (in the case of the cylindrical concretions) or lack thereof (in the case of the flat concretions). Then, after burial, groundwater chemistry and possibly the metabolic activities of microorganisms led to the precipitation of minerals around and within the masses of fish material. Finally, diagenetic alteration changed the mineral makeups of the cylindrical and flat concretions into what they are today.

New invertebrate trace fossils from the Lower Jurassic Moenave Formation at the St. George Dinosaur Discovery Site at Johnson Farm (SGDS) continue to expand the ichnofauna at the site. A previously unstudied arthropod locomotory trace, SGDS 1290, comprises two widely spaced, thick, gently undulating paramedial impressions flanked externally by small, tapered to elongate tracks with a staggered to alternating arrangement. The specimen is not a variant of any existing ichnospecies, but bears a striking resemblance to modern, experimentally generated crayfish walking traces, suggesting a crayfish or crayfish-like maker for the fossil. Because of its uniqueness, we place it in a new ichnospecies, Siskemia eurypyge. It is the first fossil crayfish or crayfish-like locomotion trace ever recorded.

A new microconchid tentaculitoid,Microconchus utahensisnew species, is described from the Lower Triassic (Spathian) Virgin Formation of two localities (Hurricane Cliffs and Beaver Dam Mountains) near St George, Utah. This small encrusting tubeworm, previously referred to erroneously asSpirorbis, has a laminated shell microstructure containing minute pores (punctae). The population from deeper water facies of the Beaver Dam Mountains is more abundant than that from Hurricane Cliffs and the tubes are significantly larger in size. Although represented by only one species (M. utahensis), microconchids are by far the most dominant component of the otherwise impoverished sclerobiont assemblage of the Virgin Formation, which also includes rare cemented bivalves and probable foraminifers. Whereas the remainder of the Virgin fauna is quite diverse, the low diversity of encrusters suggests a slow recovery from end-Permian mass extinctions. Indeed, more typically Mesozoic sclerobiont assemblages dominated by cyclostome bryozoans and serpulid polychaetes did not appear until the Late Triassic, probably Rhaetian.

Abstract Objectives To determine the relationship among body fat, cardiorespiratory fitness, and carotid artery thickness in a large group of older adults. Methods Data were collected at the Huntsman World Senior Games held in St. George, Utah between 2016–2019. Participants visited the Dixie Convention Center (St. George, UT) for free health screenings associated with the Games. The data were cross-sectional; for repeat participants only the most recent results were analyzed. The measures of interest for this study included: body fat, body mass index (BMI), cardiorespiratory fitness (predicted VO2max), and carotid artery intima media thickness (CIMT). Body fat percentage was measured using bioelectrical impedance. BMI was calculated via weight (kg) and height (m2). Predicted VO2max was calculated at rest using a heart rate monitor and the validated Polar fitness test. CIMT was obtained via images of the right and left carotid arteries, visualized and captured with a portable diagnostic ultrasound system. Differences by sex were determined using independent t-tests. Multiple regression was used to examine associations between measures. Results For this analysis, 649 participants (232 women; 326 men; 68.13 ± 8.71 y, 25.15 ± 4.92 kg/m2) were included. Women had a higher body fat percentage than men (32.00 vs. 22.42%) (t < 0.0001). However, men had a significantly higher BMI (26.28 vs. 24.01 kg/m2) and cardiorespiratory fitness (40.22 vs. 38.82 ml/kg/min) (t < 0.05) than women. Accounting for age and sex, body fat % significantly predicted CIMT thickness (P < 0.05) but BMI (P = 0.0853) and cardiorespiratory fitness did not predict CIMT thickness (P > 0.05). Conclusions CIMT thickness appears to be related to body fat percentage among older adults. Subsequent studies could examine how reduction in body fat changes CIMT thickness and how that influences risk of chronic disease, such as stroke. Funding Sources There was no funding for this project.

Carbon-isotope stratigraphy of the Furongian (stage 10; Upper Cambrian) and Tremadocian (lowermost Ordovician) reveals distinct variations from the carbonates of the Berry Head and Watts Bight formations of the East Isthmus Bay section that accumulated in a shallow-marine setting on the eastern Laurentian platform in a passive margin setting in western Newfoundland, Canada. The East Isthmus Bay δ13C values show insignificant correlation with their Sr (R2 = 0.04), Mn (R2 = 0.001) and Fe (R2 = 0.02) counterparts, implying preservation of at least near-primary C-isotope compositions. The investigated section is largely fossil poor, but the δ13C profile shows a pattern with distinct variations that can be matched with those of the western Laurentian Lawson Cove Auxiliary Boundary Stratigraphic Section and Point (ASSP) section, Utah, USA. Therefore, it was possible to reconstruct a conodont biozonal scheme by matching the δ13C profile with its counterpart from the Lawson Cove ASSP section. At the base of the East Isthmus Bay section, the δ13C profile exhibits a broad excursion (the top of the Herllnmaria – Red Tops Boundary), which can be matched with the base of the Eoconodontus Zone (mid-Furongian), followed by an enrichment trend through the Cordylodus intermedius Zone (top Furongian). A positive excursion (Hirsutodontus simplex spike) is recorded in the Cordylodus intermedius Zone (top Cambrian), and a prominent positive peak characteristic for the Cordylodus lindstromi Zone is recorded from the top of the investigated section. The δ13C values of the Newfoundland carbonates are generally ∼1‰ Vienna Pee Dee Belemnite lower than those of Lawson Cove, which is likely attributable to a relatively higher productivity and (or) organic burial in the Utah region.

The Chinle Formation and the lower part of the overlying Wingate Sandstone and Moenave Formation were deposited in fluvial, lacustrine, paludal, and eolian environments during the Norian and Rhaetian stages of the Late Triassic (~230 to 201.3 Ma), during which time the climate shifted from subtropical to increasingly arid. In southern Utah, the Shinarump Member was largely confined to pre-Chinle paleovalleys and usually overprinted by mottled strata. From southeastern to southwestern Utah, the lower members of the Chinle Formation (Cameron Member and correlative Monitor Butte Member) thicken dramatically whereas the upper members of the Chinle Formation (the Moss Back, Petrified Forest, Owl Rock, and Church Rock Members) become erosionally truncated; south of Moab, the Kane Springs beds are laterally correlative with the Owl Rock Member and uppermost Petrified Forest Member. Prior to the erosional truncation of the upper members, the Chinle Formation was probably thickest in a southeast to northwest trend between Petrified Forest National Park and the Zion National Park, and thinned to the northeast due to the lower Chinle Formation lensing out against the flanks of the Ancestral Rocky Mountains, where the thickness of the Chinle is largely controlled by syndepositional salt tectonism. The Gartra and Stanaker Members of the Ankareh Formation are poorly understood Chinle Formation correlatives north of the San Rafael Swell. Osteichthyan fish, metoposaurid temnospondyls, phytosaurids, and crocodylomorphs are known throughout the Chinle Formation, although most remains are fragmentary. In the Cameron and Monitor Butte Members, metoposaurids are abundant and non-pseudopalatine phytosaurs are known, as is excellent material of the paracrocodylomorph Poposaurus; fragmentary specimens of the aetosaurs Calyptosuchus, Desmatosuchus, and indeterminate paratypothoracisins were probably also recovered from these beds. Osteichthyans, pseudopalatine phytosaurs, and the aetosaur Typothorax are especially abundant in the Kane Springs beds and Church Rock Member of Lisbon Valley, and Typothorax is also known from the Petrified Forest Member in Capitol Reef National Park. Procolophonids, doswelliids, and dinosaurs are known but extremely rare in the Chinle Formation of Utah. Body fossils and tracks of osteichthyans, therapsids, crocodylomorphs, and theropods are well known from the lowermost Wingate Sandstone and Moenave Formation, especially from the St. George Dinosaur Discovery Site at Johnson Farm.

The Chinle Formation and the lower part of the overlying Wingate Sandstone and Moenave Formation were deposited in fluvial, lacustrine, paludal, and eolian environments during the Norian and Rhaetian stages of the Late Triassic (~230 to 201.3 Ma), during which time the climate shifted from subtropical to increasingly arid. In southern Utah, the Shinarump Member was largely confined to pre-Chinle paleovalleys and usually overprinted by mottled strata. From southeastern to southwestern Utah, the lower members of the Chinle Formation (Cameron Member and correlative Monitor Butte Member) thicken dramatically whereas the upper members of the Chinle Formation (the Moss Back, Petrified Forest, Owl Rock, and Church Rock Members) become erosionally truncated; south of Moab, the Kane Springs beds are laterally correlative with the Owl Rock Member and uppermost Petrified Forest Member. Prior to the erosional truncation of the upper members, the Chinle Formation was probably thickest in a southeast to northwest trend between Petrified Forest National Park and the Zion National Park, and thinned to the northeast due to the lower Chinle Formation lensing out against the flanks of the Ancestral Rocky Mountains, where the thickness of the Chinle is largely controlled by syndepositional salt tectonism. The Gartra and Stanaker Members of the Ankareh Formation are poorly understood Chinle Formation correlatives north of the San Rafael Swell. Osteichthyan fish, metoposaurid temnospondyls, phytosaurids, and crocodylomorphs are known throughout the Chinle Formation, although most remains are fragmentary. In the Cameron and Monitor Butte Members, metoposaurids are abundant and non-pseudopalatine phytosaurs are known, as is excellent material of the paracrocodylomorph Poposaurus; fragmentary specimens of the aetosaurs Calyptosuchus, Desmatosuchus, and indeterminate paratypothoracisins were probably also recovered from these beds. Osteichthyans, pseudopalatine phytosaurs, and the aetosaur Typothorax are especially abundant in the Kane Springs beds and Church Rock Member of Lisbon Valley, and Typothorax is also known from the Petrified Forest Member in Capitol Reef National Park. Procolophonids, doswelliids, and dinosaurs are known but extremely rare in the Chinle Formation of Utah. Body fossils and tracks of osteichthyans, therapsids, crocodylomorphs, and theropods are well known from the lowermost Wingate Sandstone and Moenave Formation, especially from the St. George Dinosaur Discovery Site at Johnson Farm.

36 Background: ASCO published a position statement regarding home infusion of anticancer therapy in June 2020. This statement recommends independent research to evaluate the safety and effectiveness of home infusions. Intermountain Healthcare (IM) incorporated this statement into its oncology care with an IRB-approved, prospective single-arm pilot study to determine the safety and feasibility of home administration of checkpoint inhibitor (CPI) immunotherapy with synchronous telemedicine visits. Methods: Patients with cancer receiving treatment at Intermountain Medical Center and Intermountain Cancer Center St. George were screened for enrollment into an IRB-approved, non-randomized pilot study of 20 patients. Eligibility criteria required patients to receive a CPI for an FDA-approved indication, live in Washington County or Salt Lake County, Utah, and have commercial payer coverage of CPI home infusion. Eligible patients were required to receive 2 doses of CPI at an infusion center, and patients who experienced an infusion reaction were excluded from receiving home infusion. Home infusion nurses are trained in oncology, CPIs, and home infusion reaction protocol. During synchronous video visits, infusion nurses are trained to perform the hands-on portions of the physical exam. A financial analysis estimated cost to IM and commercial payers for routine and home CPI infusions. Results: 622 patients were screened, of which 104 were receiving a CPI. 64 patients lived in an eligible county and 19 patients had commercial payer coverage. Of patients on CPIs, 8.7% (9/104) met all eligibility criteria accounting for 1.4% (9/622) of all patients with cancer screened (Table). Financial analysis estimated $829 cost (excluding drug cost) to IM for standard infusion reimbursement compared to $599 for in-home CPI infusions, accounting for savings of $230 per infusion. Majority of cost savings are from elimination of infusion center facilities fee ($495). Analysis includes $269 for home infusion nurse wages. Subsequent analysis for commercial payer SelectHealth estimates $270 reimbursement savings for the payer. Conclusions: Home immunotherapy infusions are estimated to be cost effective for both IM and commercial payers. However, lack of drug coverage and the rural demographics of Utahns with cancer are barriers to home CPI infusions. The pilot study was discontinued per infeasibility stopping criteria.[Table: see text]

Abstract Spatial and temporal variation in stoichiometric and stable isotope ratios of animals contains ecological information that we are just beginning to understand. In both field and lab studies, stoichiometric or isotopic ratios are related to physiological mechanisms underlying nutrition or stress. Conservation and ecosystem ecology may be informed by isotopic data that can be rapidly and non-lethally collected from wild animals, especially where human activity leaves an isotopic signature (e.g. via introduction of chemical fertilizers, ornamental or other non-native plants or organic detritus). We examined spatial and temporal variation in stoichiometric and stable isotope ratios of the toes of Uta stansburiana (side-blotched lizards) living in urban and rural areas in and around St. George, Utah. We found substantial spatial and temporal variation as well as context-dependent co-variation with reproductive physiological parameters, although certain key predictions such as the relationship between δ15N and body condition were not supported. We suggest that landscape change through urbanization can have profound effects on wild animal physiology and that stoichiometric and stable isotope ratios can provide unique insights into the mechanisms underlying these processes.

Abstract The 18 March 2020 Mw 5.7 Magna, Utah, earthquake was the largest earthquake in Utah since the 1992 ML 5.8 St. George earthquake. The geologic setting of the Magna earthquake is well documented by recent geologic mapping at 1:24,000 scale and 1:62,500 scale at and near the epicenter northeast of Magna, Utah. Subsurface fault modeling from surficial geologic mapping, structural cross sections, deep borehole data, and geophysical data reveals a complex system of faulting concentrated in the hanging wall of the Weber and Salt Lake City segments of the Wasatch fault zone including the Harkers fault, the West Valley fault zone, and the newly interpreted Saltair graben. Based on geologic and geophysical data (seismic and gravity), we interpret the mainshock of the Magna earthquake as having occurred on a relatively gently dipping part of the Salt Lake City segment, with aftershocks concentrated in the Saltair graben and West Valley fault zone. Postearthquake rapid reconnaissance of geological effects of the Magna earthquake documented liquefaction near the earthquake epicenter, along the Jordan River, and along the Great Salt Lake shoreline. Subaerial and subaqueous sand boils were identified in regions with roadway infrastructure and artificial fill, whereas collapse features were noted along the shores of the Great Salt Lake. Potential syneresis cracking and pooling in large areas indicated fluctuating groundwater likely related to earthquake ground shaking. The moderate magnitude of the Magna earthquake and minimal geological effects highlight the critical importance of earthquake research from multidisciplinary fields in the geosciences and preparedness on the Wasatch Front.

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Eine Untersuchung zu Wirtschaftsstil und Wirtschaftskultur einer geistlichen Gemeinschaft (Schriften zur Sozial- und Wirtschaftsgeschichte, 35), Hamburg 2020, Dr. Kovaç, 530 S. / graph. Darst., € 139,80. (Maria Weber, München) Fuchs, Gero, Gewinn als Umbruch der Ordnung? Der Fall des Siegburger Töpfers Peter Knütgen im 16. Jahrhundert (Rechtsordnung und Wirtschaftsgeschichte, 19), Tübingen 2019, Mohr Siebeck, XIII u. 195 S. / Abb., € 59,00. (Anke Sczesny, Augsburg) Lotito, Mark A., The Reformation of Historical Thought (St Andrews Studies in Reformation History), Leiden / Boston 2019, Brill, XX u. 542 S. / Abb., € 160,00. (Andreas Bihrer, Kiel) Georg III. von Anhalt, Abendmahlsschriften, hrsg. v. Tobias Jammerthal / David B. Janssen (Anhalt‍[er]‌kenntnisse), Leipzig 2019, Evangelische Verlagsanstalt, 440 S., € 48,00. (Eike Wolgast, Heidelberg) Bauer, Stefan, The Invention of Papal History. 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Die Vorträge der Tagung des Instituts für kunst- und musikhistorische Forschungen der Österreichischen Akademie der Wissenschaften, des Niederösterreichischen Instituts für Landeskunde und des Instituts für Österreichische Geschichtsforschung der Universität Wien, Krems, 28. bis 29. Oktober 2016 (Studien und Forschungen aus dem Niederösterreichischen Institut für Landeskunde, 71), St. Pölten 2018, Verlag Niederösterreichisches Institut für Landeskunde, 432 S. / Abb., € 25,00. (Markus Friedrich, Hamburg) Die „litterae annuae“ der Gesellschaft Jesu von Otterndorf (1713 bis 1730) und von Stade (1629 bis 1631), hrsg. v. Christoph Flucke / Martin J. Schröter, Münster 2020, Aschendorff, 154 S. / Abb., € 24,90. (Markus Friedrich, Hamburg) Como, David R., Radical Parliamentarians and the English Civil War, Oxford 2018, Oxford University Press, XV u. 457 S. / Abb., £ 85,00. (Torsten Riotte, Frankfurt a. M.) Corens, Liesbeth, Confessional Mobility and English Catholics in Counter-Reformation Europe, Oxford / New York 2019, Oxford University Press, XII u. 240 S. / Abb., £ 60,00. (Ulrich Niggemann, Augsburg) Asche, Matthias / Marco Kollenberg / Antje Zeiger (Hrsg.), Halb Europa in Brandenburg. Der Dreißigjährige Krieg und seine Folgen, Berlin 2020, Lukas, 244 S. / Abb., € 20,00. (Michael Rohrschneider, Bonn) Fiedler, Beate-Christine / Christine van den Heuvel (Hrsg.), Friedensordnung und machtpolitische Rivalitäten. Die schwedischen Besitzungen in Niedersachsen im europäischen Kontext zwischen 1648 und 1721 (Veröffentlichungen des Niedersächsischen Landesarchivs, 3), Göttingen 2019, Wallstein, 375 S. / Abb., € 29,90. (Niels Petersen, Göttingen) Prokosch, Michael, Das älteste Bürgerbuch der Stadt Linz (1658 – 1707). Edition und Auswertung (Quelleneditionen des Instituts für Österreichische Geschichtsforschung, 18), Wien / Köln / Weimar 2019, Böhlau, 308 S. / Abb., € 50,00. (Beate Kusche, Leipzig) Häberlein, Mark / Helmut Glück (Hrsg.), Matthias Kramer. Ein Nürnberger Sprachmeister der Barockzeit mit gesamteuropäischer Wirkung (Schriften der Matthias-Kramer-Gesellschaft zur Erforschung der Geschichte des Fremdsprachenerwerbs und der Mehrsprachigkeit, 3), Bamberg 2019, University of Bamberg Press, 221 S. / Abb., € 22,00. (Helga Meise, Reims) Herz, Silke, Königin Christiane Eberhardine – Pracht im Dienste der Staatsraison. Kunst, Raum und Zeremoniell am Hof der Frau Augusts des Starken (Schriften zur Residenzkultur 12), Berlin 2020, Lukas Verlag, 669 S. / Abb., € 70,00. (Katrin Keller, Wien) Schaad, Martin, Der Hochverrat des Amtmanns Povel Juel. Ein mikrohistorischer Streifzug durch Europas Norden der Frühen Neuzeit (Histoire, 176), Bielefeld 2020, transcript, 249 S., € 39,00. (Olaf Mörke, Kiel) Overhoff, Jürgen, Johann Bernhard Basedow (1724 – 1790). Aufklärer, Pädagoge, Menschenfreund. Eine Biografie (Hamburgische Lebensbilder, 25), Göttingen 2020, Wallstein, 200 S. / Abb., € 16,00. (Mark-Georg Dehrmann, Berlin) Augustynowicz, Christoph / Johannes Frimmel (Hrsg.), Der Buchdrucker Maria Theresias. Johann Thomas Trattner (1719 – 1798) und sein Medienimperium (Buchforschung, 10), Wiesbaden 2019, Harrassowitz, 173 S. / Abb., € 54,00. (Mona Garloff, Innsbruck) Beckus, Paul, Land ohne Herr – Fürst ohne Hof? Friedrich August von Anhalt-Zerbst und sein Fürstentum (Quellen und Forschungen zur Geschichte Sachsen-Anhalts, 15), Halle 2018, Mitteldeutscher Verlag, 604 S. / Abb., € 54,00. (Michael Hecht, Halle) Whatmore, Richard, Terrorists, Anarchists and Republicans. The Genevans and the Irish in Time of Revolution, Princeton / Oxford, Princeton University Press 2019, XXIX u. 478 S. / Abb., £ 34,00. (Ronald G. Asch, Freiburg i. Br.) Elster, Jon, France before 1789. The Unraveling of an Absolutist Regime, Princeton / Oxford 2020, Princeton University Press, XI u. 263 S. / graph. Darst., £ 34,00. (Lars Behrisch, Utrecht) Hellmann, Johanna, Marie Antoinette in Versailles. Politik, Patronage und Projektionen, Münster 2020, Aschendorff, X u. 402 S. / Abb., € 57,00. (Pauline Puppel, Berlin) Müchler, Günter, Napoleon. Revolutionär auf dem Kaiserthron, Darmstadt 2019, wbg Theiss, 622 S. / Abb., € 24,00. (Hans-Ulrich Thamer, Münster) Prietzel, Sven, Friedensvollziehung und Souveränitätswahrung. Preußen und die Folgen des Tilsiter Friedens 1807 – 1810 (Quellen und Forschungen zur Brandenburgischen und Preußischen Geschichte, 53), Berlin 2020, Duncker & Humblot, 408 S., € 99,90. (Nadja Ackermann, Bern) Christoph, Andreas (Hrsg.), Kartieren um 1800 (Laboratorium Aufklärung, 19), Paderborn 2019, Fink, 191 S. / Abb., € 69,00. (Michael Busch, Rostock / Schwerin)