Vitamin D status of seminomadic Fulani men and women.

The purpose of this study was to assess the vitamin D status of Fulani men and women in northern Nigeria. The Fulani are seminomadic pastoralists whose culture, economy, and diet are centered on cattle. Most of the foods consumed by the Fulani are not good sources of vitamin D. Also being Muslim, the women do not derive much benefit from the vitamin D-generating effects of sunlight due to their dress habits. Furthermore, childhood rickets is common in the region. Serum was collected from 22 Fulani men (age, 47.6 +/- 8.3 years; body mass index [BMI], 21.1 +/- 3.2 kg/m2) and 29 women (age, 55.5 +/- 13.5 years; BMI, 21.6 +/- 3.1 kg/m2) in rural northern Nigeria and analyzed for 25-hydroxyvitamin D2 and D3 using ultraperformance liquid chromatography coupled with mass spectrometry Eighty-three percent of the women and 45% of the men had serum 25-hydroxyvitamin D levels in the hypovitaminosis D range (10-30 ng/mL). In the males, there was a strong negative correlation between serum vitamin D and BMI (r = -0.49, p = .022) and percent body fat (r = -0.51, p = .015). No such correlations were observed in the Fulani women. Our main conclusion is that about half the men and most of the women in the Fulani community where this study was conducted are inadequately nourished with respect to vitamin D. A high prevalence of hypovitaminosis D indicates an elevated risk for rickets in children and bone fractures in adults.

Nanophase iron phosphate, iron arsenate, iron vanadate, and iron molybdate minerals synthesized within the protein cage of ferritin.

Nanoparticles of iron phosphate, iron arsenate, iron molybdate, and iron vanadate were synthesized within the 8 nm interior of ferritin. The synthesis involved reacting Fe(II) with ferritin in a buffered solution at pH 7.4 in the presence of phosphate, arsenate, vanadate, or molybdate. O2 was used as the oxidant to deposit the Fe(III) mineral inside ferritin. The rate of iron incorporation into ferritin was stimulated when oxo-anions were present. The simultaneous deposition of both iron and the oxo-anion was confirmed by elemental analysis and energy-dispersive X-ray analysis. The ferritin samples containing iron and one of the oxo-anions possessed different UV/vis spectra depending on the anion used during mineral formation. TEM analysis showed mineral cores with approximately 8 nm mineral particles consistent with the formation of mineral phases inside ferritin.