Report of Recommendations to the Iowa Department of Human Services, Central Distribution Center, June 30, 2002

State Agency Audit Report

South Central Iowa Regional E-911 Service Board, June 30, 2002

Other Audit Reports

Central Iowa Juvenile Detention Center in Eldora Iowa, June 30, 2001 & June 30, 2002

Other Audit Reports

Central Iowa Juvenile Detention Center, June 30, 2003

Other Audit Report

South Central Iowa Regional E-911 Service Board, June 30, 2002 and June 30, 2003

Other Audit Report

Essays in banking and corporate finance

Abstract This paper presents a model of executive compensation in which the executive is risk-averse and has specific knowledge -knowledge about the optimal actions to take that is costly to transfer to the principal. The model generates predictions that are consistent with the available evidence and provides a rationale for a number of unresolved puzzles in executive compensation. Notably, we find that relative performance evaluation is optimal only if the quality of specific knowledge is low. We also show (1) why some common risk components are not filtered out of executives' pay, (2) why performance is more likely to be evaluated relative to aggregate market movements than relative to industry movements, and (3) why executives with higher perceived abilities are given stronger incentives. Finally, we demonstrate that the relation between risk and incentives may be positive or negative, depending on the quality of the executive's specific knowledge.

Oxygen isotope compositions of iron oxides from high-grade BIF-hosted iron ore deposits of the Central Hamersley Province, Western Australia: Constraints on the evolution of hydrothermal fluids

The Hamersley province of northwest Australia is one of the world's premier iron ore regions with high-grade martite-microplaty hematite iron ore deposits mostly hosted within banded iron formation (BIF) sequences of the Brockman Iron Formations of the Hamersley Group. These high-grade iron ores contain between 60 and 68 wt percent Fe, and formed by the multistage interaction of hydrothermal fluids with the host BIF formation. The oxygen isotope compositions of magnetite and hematite from BIF, hydrothermal alteration assemblages, and high-grade iron Ore were analyzed from the Mount Tom Price, Paraburdoo, and Charmar iron ore deposits. The delta(18)O values of magnetite and hematite from hydrothermal alteration assemblages and high-grade iron ore range from -9.0 to -2.9 per mil, a depletion of 5 to 15 per mil relative to the host BIF. The delta(18)O values are spatially controlled by faults within the deposits, a response to higher fluid flux and larger influence the isotopic compositions by the hydrothermal fluids. The oxygen isotope composition of hydrothermal fluids (delta(18)O(fluid)) indicates that the decrease in the (18)O content of iron oxides was due to the interaction of both basinal brines and meteoric fluids with the original BIF. Late-stage talc-bearing ore at the Mount Tom Price deposit formed in the presence of a pulse of delta(18)O-enriched basinal brine, indicating that hydrothermal fluids may have repeatedly interacted with the BIFs during the Paleoproterozoic.

Report of Recommendations to the Iowa Department of Human Services - Central Distribution Center, June 30, 2003

State Agency Audit Report

Creatine, central nervous system and creatine deficiency syndromes

It was long thought that most of brain creatine was of peripheral origin. However, recentworks have demonstrated that creatine crosses blood-brain barrier only with poor efficiency, and thatCNS must ensure parts of its creatine needs by its own creatine synthesis pathway, thank to the brainexpression of AGAT and GAMT (creatine synthesis) and SLC6A8 (creatine transporter). This newunderstanding of creatine metabolism and transport in CNS allows a better comprehension of creatinedeficiency syndromes, which are due to deficiencies in AGAT, GAMT and SLC6A8 and mainly affectthe brain of patients who show severe neurodevelopmental delay and present neurological symptomsin early infancy.

Late Pliensbachian-Early Toarcian (Early Jurassic) environmental changes in an epicontinental basin of NW Europe (Causses area, central France): A micropaleontological and geochemical approach

We present an integrated work based on calcareous nannofossil and benthic foraminiferal assemblages, and geochemical analyses of two Upper Pliensbachian-Lower Toarcian sections located in the central-South France. The studied sections, Tournadous and Saint-Paul-des-Fonts, represent the proximal and the distal part, respectively, of the Jurassic Causses Basin, one of the small, partly enclosed basins belonging to the epicontinental shelf of the NW Tethys. At the transition from Late Pliensbachian to Early Toarcian, the Causses Basin recorded an emersion in response to the global sea-level fall. Our data indicate severe environmental conditions of marine waters, including salinity decrease and anoxia development, occurring in the Early Toarcian. The acme of this deterioration coincides with the Early Toarcian Anoxic Event (T-OAE) but, due to the restricted nature of the basin. anoxia persisted until the end of the Early Toarcian. mainly in the deeper parts of the basin. The micronutrients and organic organic-matter fluxes were probably high during the entire studied time interval, as shown by nannofossil and foraminiferal assemblages. However, nannoplankton production drastically decreased during the T-OAE, as demonstrated by very low nannofossil fluxes, and only taxa tolerant to low-saline surface waters could thrive. At the same time, benthic foraminifers temporarily disappeared in response to sea-bottom anoxia. Our study demonstrates that environmental changes related to the T-OAE are well-recorded even in small, partly enclosed basins of NW Europe, like the Causses Basin. Within this area, the effects of global changes. like sea sea-level and temperature fluctuations, are modulated by local conditions mainly controlled by the morphology of the basin. (C) 2008 Elsevier B.V. All rights reserved.

Rational Partisan Theory with fiscal policy and an independent central bank

The empirical evidence testing the validity of the rational partisan theory (RPT) has been mixed. In this article, we argue that the inclusion of other macroeconomic policies and the presence of an independent central bank can partly contribute to explain this inconclusiveness. This article expands Alesina s (1987) RPT model to include an extra policy and an independent central bank. With these extensions, the implications of RPT are altered signi ficantly. In particular, when the central bank is more concerned about output than public spending (an assumption made by many papers in this literature), then the direct relationship between in flation and output derived in Alesina (1987) never holds. Keywords: central bank, conservativeness, political uncertainty. JEL Classi fication: E58, E63.

Report on Special Investigation of the Central Point Coordination for Calhoun and Pocahontas Counties for the Period July 1, 1998 through May 31, 2004

Report on a Special Investigation of the Central Point Coordination for Calhoun and Pocahontas Counties.

Localização inicial da ponta de cateter central de inserção periférica (PICC) em recém-nascidos

Estudo transversal com coleta prospectiva de dados, que objetivouidentificar o posicionamento inicial da ponta do cateter central de inserção periférica (PICC) e verificar a prevalência de sucesso de sua inserção em neonatos. Os dados foram coletados no berçário anexo à maternidade do Hospital das Clínicas da Faculdade de Medicina da Universidade de São Paulo, entre março e setembro de 2006. Dos 37 neonatos submetidos à inserção do cateter PICC, a taxa de sucesso no procedimento foi de 72,3% (27 neonatos); destes, quatro (14,8%) estavam com as pontas dos cateteres alojadas nas veias axilar ou inominada; outros três (11,1%), alojadas em veia jugular. Estes cateteres foram removidos por desvio de trajeto. 13 (48,2%) estavam com as pontas alojadas em átrio direito, cujos cateteres foram tracionados para reposicionamento da ponta para a veia cava superior.