Antihypertensive Combination Treatment: State of the Art.

An adequate control of blood pressure is essential to reduce the risk of target organ damages and cardiovascular events in patients with hypertension. Yet, it is well recognized that a substantial proportion of treated patients remain hypertensive despite treatment. Several reasons have been evoked to explain why so many patients are not adequately controlled. Among them, medical inertia, a poor long-term adherence, and the need to prescribe several antihypertensive drugs to reach the target blood pressure have been identified as major limitations to the success of antihypertensive therapy. In this context, the use of single-pill combinations (SPC) containing two or three drugs in one pill has an important role in reducing the impact of some of these issues. Indeed, the use of SPC enables to reduce the pill burden and to improve the treatment efficacy without increasing the incidence of side effects. However, besides their major advantages, SPC have also some limitations such as a possible lack of flexibility or a higher cost. The purpose of this review is to discuss the place of SPC in the actual management of hypertension. The active development of new single-pill combinations in last years can be considered as a significant improvement in the physicians' capacity to treat hypertension effectively.

3-D density structure and geological evolution of Stromboli volcano (Aeolian Islands, Italy) inferred from land-based and sea-surface gravity data

We present the first density model of Stromboli volcano (Aeolian Islands, Italy) obtained by simultaneously inverting land-based (543) and sea-surface (327) relative gravity data. Modern positioning technology, a 1 x 1 m digital elevation model, and a 15 x 15 m bathymetric model made it possible to obtain a detailed 3-D density model through an iteratively reweighted smoothness-constrained least-squares inversion that explained the land-based gravity data to 0.09 mGal and the sea-surface data to 5 mGal. Our inverse formulation avoids introducing any assumptions about density magnitudes. At 125 m depth from the land surface, the inferred mean density of the island is 2380 kg m(-3), with corresponding 2.5 and 97.5 percentiles of 2200 and 2530 kg m-3. This density range covers the rock densities of new and previously published samples of Paleostromboli I, Vancori, Neostromboli and San Bartolo lava flows. High-density anomalies in the central and southern part of the island can be related to two main degassing faults crossing the island (N41 and NM) that are interpreted as preferential regions of dyke intrusions. In addition, two low-density anomalies are found in the northeastern part and in the summit area of the island. These anomalies seem to be geographically related with past paroxysmal explosive phreato-magmatic events that have played important roles in the evolution of Stromboli Island by forming the Scari caldera and the Neostromboli crater, respectively. (C) 2014 Elsevier B.V. All rights reserved.