Report on a special investigation of the UNI Malcolm Price Laboratory School for the period July 1, 2006 through March 31, 2009

Report on a special investigation of the UNI Malcolm Price Laboratory School for the period July 1, 2006 through March 31, 2009

Report on a review of selected general and application controls over the Iowa Public Employees’ Retirement System (IPERS) I-Que Pension Administration System for the period March 24, 2009 through April 22, 2009

Report on a review of selected general and application controls over the Iowa Public Employees’ Retirement System (IPERS) I-Que Pension Administration System for the period March 24, 2009 through April 22, 2009

Stable isotope compositions of mammoth teeth from Niederweningen, Switzerland: Implications for the Late Pleistocene climate, environment, and diet

Oxygen and carbon isotope compositions of well-preserved mammoth teeth from the Middle Wurmian (40-70 ka) peat layer of Niederweningen, the most important mammoth site in Switzerland, were analysed to reconstruct Late Pleistocene palaeoclimatic and palaeoenvironmental conditions. Drinking water (delta(18)O values of approximately -12.3 +/- 0.9 parts per thousand were calculated front oxygen isotope compositions of mammoth tooth enamel apatite using a species-specific calibration for modern elephants. These delta(18)O(H2O) values reflect the mean oxygen isotope composition of the palaeo-precipitation and are similar to those directly measured for fate Pleistocene groundwater from aquifers in northern Switzerland and southern Germany. Using a present-day delta(18)O(H2)o-precipitation-air temperature relation for Switzerland, a mean annual air temperature (MAT) of around 4.3 +/- 2.1 degrees C can be calculated for the Middle Wurmian at this site. This MAT is in good agreement with palaeotemperature estimates on the basis of Middle Wurmian groundwater recharge temperatures and beetle assemblages. Hence, the climatic conditions in this region were around 4 degrees C cooler during the Middle Wurmian interstadial phase, around 45-50ka BP, than they are today. During this period the mammoths from Niederweningen lived in an open tundra-like, C(3) plant-dominated environment as indicated by enamel (delta(13)C values of -11.5 +/- 0.3 parts per thousand and pollen and macroplant fossils found in the embedding peat. The low variability of enamel delta(13)C and delta(18)O values from different mammoth teeth reflects similar environmental conditions and supports a relatively small time frame for the fossil assemblage. (C) 2006 Elsevier Ltd and INQUA. All rights reserved.

Special investigation of Iowa Association of Skills USA-VICA, for the period September 1, 2001 through September 30, 2008

Special investigation of Iowa Association of Skills USA-VICA, for the period September 1, 2001 through September 30, 2008

Special report on the Former Russell Community School District for the period July 1, 2007 through June 30, 2008

Special report on the Former Russell Community School District for the period July 1, 2007 through June 30, 2008

Report on a special investigation of the Keokuk County Sheriff’s Office for the period July 1, 2006 through April 15, 2009

Report on a special investigation of the Keokuk County Sheriff’s Office for the period July 1, 2006 through April 15, 2009

Stratigraphical discontinuities, tropical landscape evolution and soil distribution relationships in a case study in SE-Brazil

On a regional summit surface in the county of Piracicaba (SP) within the Peripheric Depression of São Paulo, formed of discontinued flattened tops, there is an abrupt transition between a Typic Hapludox and a Kandiudalfic Eutrudox, together with two stoneline layers. Using stratigraphical, mineralogical, and cartographic studies, this transition and the soil distribution of this surface were studied, correlating them with the different parent materials and the morphoclimatic model of landscape evolution in Southeastern Brazil. The Typic Hapludox was formed on a sandy Cenozoic deposit (Q) that overlies a pellitic deposit of the Iratí formation (Pi), representing a regional erosive discordance. Westwards to the Piracicaba River, this sequence is interrupted by a diabase sill overlain by a red clayey material which gave origin to the Kandiudalfic Eutrudox. Two post-Permian depositional events were identified by the two stonelines and stratigraphical discontinuities. The first event generated the deposition of a sandy sediment in the form of levelled alveoluses on regional barriers, most of these formed by dikes and diabase sills, probably during a drier phase. The second depositional event, leading to the deposition of the red clay was probably the dissection of the previously formed pediplane during a humid climate, followed by another pedimentation process during a later, drier period.

Reaudit report on the City of St. Charles, Iowa for the period July 1, 2005 through June 30, 2006

Reaudit report on the City of St. Charles, Iowa for the period July 1, 2005 through June 30, 2006

Reaudit letter to the City of Ottumwa for the period July 1, 2005 through June 30, 2006, as well as certain issues applicable to the year ended June 30, 2005 and subsequent periods

Reaudit letter to the City of Ottumwa for the period July 1, 2005 through June 30, 2006, as well as certain issues applicable to the year ended June 30, 2005 and subsequent periods

Report on the Unemployment Insurance Tax Redesign Project administered by Iowa Workforce Development for the period July 1, 2002 through June 30, 2009

Report on the Unemployment Insurance Tax Redesign Project administered by Iowa Workforce Development for the period July 1, 2002 through June 30, 2009

Audit report on the Honey Creek Resort operated by Central Group Management, LLC for the period from inception (September 18, 2008) to June 30, 2009

Audit report on the Honey Creek Resort operated by Central Group Management, LLC for the period from inception (September 18, 2008) to June 30, 2009

Report on a review of the funding for construction of the Lewis and Clark Interpretive Center at Lewis and Clark State Park in Monona County for the period February 25, 1999 through December 31, 2008

Report on a review of the funding for construction of the Lewis and Clark Interpretive Center at Lewis and Clark State Park in Monona County for the period February 25, 1999 through December 31, 2008

Report on payments made subsequent to recipients’ dates of death under the Medicaid program administered by the Department of Human Services for the period July 1, 2006 through December 31, 2008

Report on payments made subsequent to recipients’ dates of death under the Medicaid program administered by the Department of Human Services for the period July 1, 2006 through December 31, 2008

Special investigation of the City of Truro for the period January 1, 2003 through February 18, 2009

Special investigation of the City of Truro for the period January 1, 2003 through February 18, 2009

Report on the City of Hills Fire Department, also known as Hills Fire Fighters, for the period July 1, 2006 through September 30, 2009

Report on the City of Hills Fire Department, also known as Hills Fire Fighters, for the period July 1, 2006 through September 30, 2009