[Calcium and blood pressure]

The regulation of blood pressure is complex with several organs being involved. Intracellular calcium plays a crucial role in the regulation of cardiovascular functions: An increased influx of calcium into the vascular smooth muscle cells leads to an augmental muscular tone and therefore to an increased vascular resistance and rise in blood pressure. Parathormone plays a permissive role since it regulates the calcium-influx into the cells and thus increases the vasoconstrictive effect. There is a positive correlation between parathormone and blood pressure, present in primary as well as secondary hyperparathyroidism. Moreover, patients with essential hypertension have high parathormone levels already before hypertension is diagnosed. A calcium-rich diet (> 1000 mg calcium daily) slightly decreases blood pressure. This positive effect is due to parathormone suppression with a subsequently decreased calcium content in the vascular smooth muscle cells. A calcium-rich diet inhibits lipogenesis in the fat tissue; thus additionally improving the cardiovascular risk profile.

[Metaphylaxis of recurrent renal calcium stones]

Calcium containing renal stones represent a common medical problem and show a high rate of recurrence. Therefore, besides the treatment of acute stone episodes, also the prevention of new stone episodes is of crucial importance in the medical care of stone formers. To avoid stone recurrences, medical as well as dietary measures should be established based on the results of a thorough evaluation and the elaboration of an individual risk profile. This review article describes and discusses the currently established treatment options for the prophylaxis of calcium-containing renal stones.

Comparative acute effects of the calcium channel blockers tiapamil, nisoldipine, and nifedipine on blood pressure and some regulatory factors in normal and hypertensive subjects

To clarify the pharmacological profile of the two new calcium channel blockers tiapamil and nisoldipine in humans, their acute effects as compared with those of the reference agent nifedipine were assessed in 10 normal subjects and 10 patients with essential hypertension. Blood pressure (BP), heart rate (HR), plasma and urinary catecholamine, sodium and potassium, plasma renin and aldosterone levels, and urinary prostaglandin E2 and F2 excretion rates were determined before and up to 4 or 5 h (urine values) after intravenous injection of placebo (20 ml 0.9% NaCl), tiapamil 1 mg/kg body weight, nisoldipine 6 micrograms/kg, or nifedipine 15 micrograms/kg. The four studies were performed at weekly intervals according to Latin square design. All three calcium channel blockers significantly (p less than 0.05 or lower) lowered BP and distinctly increased sodium excretion in hypertensive patients, but had only little influence on these parameters in normal subjects. HR was increased in both groups. Changes in BP and HR were maximal at 5 min and largely dissipated 3 h after drug injection. Effects on BP and HR, as well as concomitant mild increases in plasma norepinephrine and renin levels that occurred in both groups, tended to be more pronounced (about double) following nisoldipine than following tiapamil or nifedipine at the dosages given. Plasma aldosterone, epinephrine levels, and prostaglandin excretion rates were not consistently modified. These findings demonstrate that tiapamil and nisoldipine possess distinct antihypertensive properties in humans. Different chronotropic and renin-activating effects of different calcium channel blockers may be determined, at least in part, by a different influence on sympathetic activity.(ABSTRACT TRUNCATED AT 250 WORDS)

High exchangeable calcium concentrations in soils on Barro Colorado Island, Panama

The soils on four lithologies (basaltic conglomerates, Bohio; Andesite; volcanoclastic sediments with basaltic agglomerates, Caimito volcanic; foraminiferal limestone, Caimito marine) on Barro Colorado Island (BCI) have high exchangeable Ca concentrations and cation-exchange capacities (CEC) compared to other tropical soils on similar parent material. In the 0–10 cm layer of 24 mineral soils, pH values ranged from 5.7 (Caimito volcanic and Andesite) to 6.5 (Caimito marine), concentrations of exchangeable Ca from 134 mmolc kg− 1 (Caimito volcanic) to 585 mmolc kg− 1 (Caimito marine), and cation exchange capacities from 317 mmolc kg− 1 (Caimito volcanic) to 933 mmolc kg− 1 (Caimito marine). X-ray diffractometry of the fraction < 2 μm revealed that smectites dominated the clay mineral assemblage in soil except on Caimito volcanic, where kaolinite was the dominant clay mineral. Exchangeable Ca concentrations decreased with increasing soil depth except on Caimito marine. The weathering indices Chemical Index of Alteration (CIA), Plagioclase Index of Alteration (PIA) and Weathering Index of Parker (WIP) determined for five soils on all geological formations, suggested that in contrast to expectation the topsoil (0–10 cm) appeared to be the least and the subsoil (50–70 cm) and saprolite (isomorphically weathered rock in the soil matrix) the most weathered. Additionally, the weathering indices indicated depletion of base cations and enrichment of Al-(hydr)oxides throughout the soil profile. Tree species did not have an effect on soil properties. Impeded leaching and the related occurrence of overland flow seem to be important in determining clay mineralogy. Our results suggest that (i) edaphic conditions favor the formation of smectites on most lithologies resulting in high CEC and thus high retention capacity for Ca and (ii) that there is an external source such as dust or sea spray deposition supplying Ca to the soils.

Bone healing around nanocrystalline hydroxyapatite, deproteinized bovine bone mineral, biphasic calcium phosphate, and autogenous bone in mandibular bone defects.

The individual healing profile of a given bone substitute with respect to osteogenic potential and substitution rate must be considered when selecting adjunctive grafting materials for bone regeneration procedures. In this study, standardized mandibular defects in minipigs were filled with nanocrystalline hydroxyapatite (HA-SiO), deproteinized bovine bone mineral (DBBM), biphasic calcium phosphate (BCP) with a 60/40% HA/β-TCP (BCP 60/40) ratio, or particulate autogenous bone (A) for histological and histomorphometric analysis. At 2 weeks, percent filler amongst the test groups (DBBM (35.65%), HA-SiO (34.47%), followed by BCP 60/40 (23.64%)) was significantly higher than the more rapidly substituted autogenous bone (17.1%). Autogenous bone yielded significantly more new bone (21.81%) over all test groups (4.91%-7.74%) and significantly more osteoid (5.53%) than BCP 60/40 (3%) and DBBM (2.25%). At 8 weeks, percent filler amongst the test groups (DBBM (31.6%), HA-SiO (31.23%), followed by BCP 60/40 (23.65%)) demonstrated a similar pattern and was again significantly higher as compared to autogenous bone (9.29%). Autogenous bone again exhibited statistically significantly greater new bone (55.13%) over HA-SiO (40.62%), BCP 60/40 (40.21%), and DBBM (36.35%). These results suggest that the osteogenic potential of HA-SiO and BCP is inferior when compared to autogenous bone. However, in instances where a low substitution rate is desired to maintain the volume stability of augmented sites, particularly in the esthetic zone, HA-SiO and DBBM may be favored. © 2014 Wiley Periodicals, Inc. J Biomed Mater Res Part B: Appl Biomater, 103B: 1478-1487, 2015.