The prevalence of vitamin D inadequacy amongst women with osteoporosis: an international epidemiological investigation

INTRODUCTION: Vitamin D is essential for calcium metabolism as well as for fracture prevention, and a recent review suggested that the optimal serum 25(OH)D lies in the region of 50-80 nmol L-1 (20-32 ng mL-1). A high prevalence of inadequacy has been reported in many studies but the prevalence of inadequacy amongst women with osteoporosis in different regions of the world has not been well characterized. SETTING AND SUBJECTS: A multinational study of 18 countries at various latitudes (range 64N-38S) was conducted in 2004 and 2005 to determine the average levels of serum 25(OH)D and the prevalence of vitamin D inadequacy. A total of 2606 postmenopausal women with osteoporosis (low bone mineral density, history of fragility fracture) seeking routine medical care were enrolled and serum 25(OH)D levels were measured at a single laboratory visit. RESULTS: Mean serum 25(OH)D level was 26.8 ng mL-1 (SE 0.3) and ranged from 7 to 243 ng mL-1. Regional mean values were highest in Latin America (29.6 ng mL-1, SE 0.6) and lowest in the Middle East (20.4 ng mL-1, SE 0.5). Overall, 64% of women had serum levels<30 ng mL-1. Serum parathyroid hormone reached a nadir at serum 25(OH)D levels>35 ng mL-1. In nonequatorial countries, women recruited during the winter months had somewhat lower serum 25(OH)D levels than those recruited during the summer months in some, but not all, countries. CONCLUSIONS: Low levels of serum 25(OH)D are common amongst women with osteoporosis. The results underscore the value of assuring vitamin D adequacy in these women.

A Surface Displacement Analysis for Volcan Pacaya from October 2001 through March 2013 by Means of 3-D Modeling of Precise Position GPS Data

Volcán Pacaya is one of three currently active volcanoes in Guatemala. Volcanic activity originates from the local tectonic subduction of the Cocos plate beneath the Caribbean plate along the Pacific Guatemalan coast. Pacaya is characterized by generally strombolian type activity with occasional larger vulcanian type eruptions approximately every ten years. One particularly large eruption occurred on May 27, 2010. Using GPS data collected for approximately 8 years before this eruption and data from an additional three years of collection afterwards, surface movement covering the period of the eruption can be measured and used as a tool to help understand activity at the volcano. Initial positions were obtained from raw data using the Automatic Precise Positioning Service provided by the NASA Jet Propulsion Laboratory. Forward modeling of observed 3-D displacements for three time periods (before, covering and after the May 2010 eruption) revealed that a plausible source for deformation is related to a vertical dike or planar surface trending NNW-SSE through the cone. For three distinct time periods the best fitting models describe deformation of the volcano: 0.45 right lateral movement and 0.55 m tensile opening along the dike mentioned above from October 2001 through January 2009 (pre-eruption); 0.55 m left lateral slip along the dike mentioned above for the period from January 2009 and January 2011 (covering the eruption); -0.025 m dip slip along the dike for the period from January 2011 through March 2013 (post-eruption). In all bestfit models the dike is oriented with a 75° westward dip. These data have respective RMS misfit values of 5.49 cm, 12.38 cm and 6.90 cm for each modeled period. During the time period that includes the eruption the volcano most likely experienced a combination of slip and inflation below the edifice which created a large scar at the surface down the northern flank of the volcano. All models that a dipping dike may be experiencing a combination of inflation and oblique slip below the edifice which augments the possibility of a westward collapse in the future.

Characterization of the type I secretion system of the RTX toxin ApxII in "Actinobacillus porcitonsillarum"

Strains of Actinobacillus porcitonsillarum are regularly isolated from the tonsils of healthy pigs. A. porcitonsillarum is non pathogenic but phenotypically it strongly resembles the pathogenic species Actinobacillus pleuropneumoniae, thereby interfering with the diagnosis of the latter. A. porcitonsillarum is hemolytic but unlike A. pleuropneumoniae, it contains only apxII genes and not apxI or apxIII genes. In contrast to the truncated apxII operon of A. pleuropneumoniae, which lacks the type I secretion genes BD, characterization of the apxII operon in A. porcitonsillarum revealed that it contains an intact and complete apxII operon. This shows a typical RTX operon structure with the gene arrangement apxIICABD. The region upstream of the apxII operon is also different from that in A. pleuropneumoniae and contains an additional gene, aspC, encoding a putative aspartate aminotransferase. Trans-complementation experiments in Escherichia coli and A. pleuropneumoniae indicated that the entire apxII operon of A. porcitonsillarum is sufficient to express and secrete the ApxIIA toxin and that the ApxIIA toxin of A. pleuropneumoniae can be secreted by the type I secretion system encoded by apxIIBD. These findings suggest that the complete apxII operon found in A. porcitonsillarum might be an ancestor of the truncated homologue found in A. pleuropneumoniae. The genetic context of the apxII locus in A. porcitonsillarum and A. pleuropneumoniae suggests that in the latter, the contemporary truncated operon is the result of a recombination event within the species, rather than a horizontal transfer of an incomplete operon.