Differences in Abdominal and Liver Fat Accumulation Between Obesity-Matched Adults With and Without Type 2 Diabetes

Despite attempts to identify the mechanisms by which obesity leads to the development of Type 2 Diabetes (T2D), it remains unclear why some but not all adults with obesity develop T2D. Given the established associations between visceral adipose tissue (VAT) and liver fat with insulin resistance, we hypothesized that compared to age and obesity matched adults who were non-diabetic (NT2D), adults with T2D would have greater amounts of VAT and liver fat. The International Study of Prediction of Intra-Abdominal Adiposity and Its Relationship with Cardiometabolic Risk/Intra-Abdominal Adiposity (INSPIRE ME IAA) aims to study the associations between VAT and liver fat and risk of developing T2D and cardiovascular disease. Four thousand, five hundred and four participants were initially recruited; from this, 2383 White and Asian adults were selected for this ancillary analysis. The NT2D and T2D groups were matched for age, body mass index (BMI) and waist circumference (WC). The T2D and NT2D groups were also compared to participants with either impaired fasting glucose (IFG) or impaired glucose tolerance (IGT; IFG/IGT)). Abdominal adipose tissue was measured by computed tomography; liver fat was estimated using computed tomography-derived mean attenuation. Secondary analysis determined whether differences existed between NT2D and T2D groups in VAT and liver fat accumulation within selected BMI categories for Whites and Asians. We report across sex and race, T2D and IFG/IGT groups had elevated VAT and liver fat compared to the NT2D group (p<0.05). VAT was not different between IFG/IGT and T2D groups (p>0.05), however liver fat was greater in the T2D group compared to the IFG/IGT group in both Whites and Asians (p<0.05). Within each BMI category, the T2D group had elevated VAT and liver fat compared to the age and anthropometrically matched NT2D group in both Whites and Asians (p<0.05). With few exceptions, abdominal subcutaneous adipose tissue was not different in the T2D or IFG/IGT groups compared to the NT2D group independent of sex and race. Compared to age and obesity-matched adults who are NT2D, we observe that White and Asian adults with T2D, and those with IFG/IGT, present with greater levels of both VAT and liver fat.

THE IMPACT OF VIRUS INFECTION IN DEREGULATION OF CYTOKINE PRODUCTION UPON SECONDARY BACTERIAL INFECTION

Dendritic cells (DCs) secrete cytokines such as interleukin-23 (IL-23) when stimulated with certain Toll-like receptor (TLR) agonists and infected with pathogens such as P. aeruginosa. IL- 23 is a proinflammatory cytokine that plays a critical role in the proliferation and differentiation of the IL-17 producing Th17- CD4 T helper cells. The lack of efficient cytokine production from antigen-presenting cells, such as DCs, can impact CD4 differentiation and thus impair the immune responses against pathogens. Clearance of some bacterial infections, such as Klebsiella pneumonia and Listeria monocytogenes has been shown to be dependent on the induction of IL-23 and therefore, deregulation of these cytokines as a direct result of virus infection may impede immune responses to secondary infections. Here, an inhibition of TLR ligand or P. aeruginosa-induced IL- 23 expression in Lymphocytic Choriomeningitis Virus (LCMV)-infected bone marrow-derived dendritic cells (BMDCs) has been demonstrated, indicating that an important function of these cells is disrupted during virus/bacterial coinfection. While production of TNF-α was unaffected in LPS stimulated cells, TNF-α was significantly inhibited in bacterium infected cells by LCMV. Type I IFN in LPS or LCMV infected cell was not detected and therefore, ruling out the possibility of cytokine suppression by Type I IFN. The production of IL-10 was high in BMDCs infected with LCMV and stimulated with LPS or bacteria. Analysis of multiple cytokines produced in this coinfection model demonstrated that LCMV infection impacts specific cytokine production upon LPS or bacterium infection, which may be important for bacterial clearance. This data is important for future immunotherapy use in viral/bacterial coinfection scenarios.

Analysis of Evidence from Core Sample Fractures in Stewardson Lake Uranium Prospect

This study was performed to characterize evidence of potential unconformity-type U mineralizing fluids in drill core fractures from the Stewardson Lake prospect, in the Athabasca Basin, located in Northern Saskatchewan and Alberta, Canada. Fractures were visually classified into eight varieties. This classification scheme was improved with the use of mineralogical characterization through SEM (Scanning Electron Microscope) and XRD analyses of the fracture fills and resulted in the identification of various oxides, hydroxides, sulfides, and clays or clay-sized minerals. Fractures were tallied to a total of ten categories with some commonalities in color. The oxidative, reductive or mixed nature of the fluids interacting with each fracture was determined based on its fill mineralogy. The measured Pb isotopic signature of samples was used to distinguish fractures affected solely by fluids emanating from a U mineralization source, from those affected by mixed fluids. Anomalies in U and U-pathfinder elements detected in fractures assisted with attributing them to the secondary dispersion halo of potential mineralization. Three types of fracture functions (chimney, composite and drain) were defined based on their interpreted flow vector and history. A secondary dispersion halo boundary with a zone of dominance of infiltrating fluids was suggested for two boreholes. The control of fill mineralogy on fracture color was investigated and the indicative and non-indicative colors and minerals, with respect to a secondary dispersion halo, were formally described. The fracture colors and fills indicative of proximity to the basement host of the potential mineralization were also identified. In addition, three zones of interest were delineated in the boreholes with respect to their geochemical dynamics and their relationship to the potential mineralization: a shallow barren overburden zone, a dispersion and alteration zone at intermediate depth, and a second deeper zone of dispersion and alteration.