The lithospheric structures beneath the Pyrenees, which holds the key to settle long-standing controversies regarding the opening of the Bay of Biscay and the formation of the Pyrenees, are still poorly known. The temporary PYROPE and IBERARRAY experiments have recently filled a strong deficit of seismological stations in this part of western Europe, offering a new and unique opportunity to image crustal and mantle structures with unprecedented resolution. Here we report the results of the first tomographic study of the Pyrenees relying on this rich data set. The important aspects of our tomographic study are the precision of both absolute and relative traveltime measurements obtained by a nonlinear simulated annealing waveform fit and the detailed crustal model that has been constructed to compute accurate crustal corrections. Beneath the Massif Central, the most prominent feature is a widespread slow anomaly that reflects a strong thermal anomaly resulting from the thinning of the lithosphere and upwelling of the asthenosphere. Our tomographic images clearly exclude scenarios involving subduction of oceanic lithosphere beneath the Pyrenees. In contrast, they reveal the segmentation of lithospheric structures, mainly by two major lithospheric faults, the Toulouse fault in the central Pyrenees and the Pamplona fault in the western Pyrenees. These inherited Hercynian faults were reactivated during the Cretaceous rifting of the Aquitaine and Iberian margins and during the Cenozoic Alpine convergence. Therefore, the Pyrenees can be seen as resulting from the tectonic inversion of a segmented continental rift that was buried by subduction beneath the European plate.

A single measure of airborne concentrations of molds by impaction allows to establish useful thresholds by social services to estimate in a objective way the housing moldiness. Excluding the summer period, reproducibility of this kind of measure on 3 months, in the fixed limits, is 94.3%. The differences in terms of biodiversity of the unhealthy housing and those accommodating allergic patients imply a specific approach to decrease fungi airborne concentrations. The biodiversity of Penicillium raises the problem of the use of the single extract of Penicillium chrysogenum for skin-tests. The extent of the contaminated surfaces must be measured to assess the potential risk linked to spore contamination. Indeed, surface sampling mostly allows qualitative assessment of the environment.