Densité, centralité et qualité urbaine : la notion d'intensité, outil pour une gestion adaptative des formes urbaines?

L'urbanisme durable réinterprète et réinvente le modèle de la ville dense. Il reconsidère les avantages de la proximité et pense l'organisation des relations entre la forme urbaine, les fonctions, les usages et les significations de la ville dans une visée de production de la qualité urbaine. Qualifier la ville c'est inscrire de la valeur dans l'espace. C'est faire de la ville un « trésor d'espaces », donner vie aux quartiers, organiser la mobilité, agencer des noyaux d'urbanité différenciés afin d'intensifier leurs multiples valeurs d'usage (économiques, sociales, écologiques, esthétiques). L'intensité urbaine révèle forcément la présence humaine et la manière dont la ville est vécue, représentée, signifiée et appropriée par ses habitants. L'article explore la notion d'intensité comme outil pour une gestion adaptative des densités urbaines et des tensions qu'elles engendrent. C'est aussi un plaidoyer pour une densification régulée dans une ville plurielle, réticulaire et polycentrique.

An introductory review on gravitational-deformation induced structures, fabrics and modeling

Recent studies have pointed out a similarity between tectonics and slope tectonic-induced structures. Numerous studies have demonstrated that structures and fabrics previously interpreted as of purely geodynamical origin are instead the result of large slope deformation, and this led in the past to erroneous interpretations. Nevertheless, their limit seems not clearly defined, but it is somehow transitional. Some studies point out continuity between failures developing at surface with upper crust movements. In this contribution, the main studies which examine the link between rock structures and slope movements are reviewed. The aspects regarding model and scale of observation are discussed together with the role of pre-existing weaknesses in the rock mass. As slope failures can develop through progressive failure, structures and their changes in time and space can be recognized. Furthermore, recognition of the origin of these structures can help in avoiding misinterpretations of regional geology. This also suggests the importance of integrating different slope movement classifications based on distribution and pattern of deformation and the application of structural geology techniques. A structural geology approach in the landslide community is a tool that can greatly support the hazard quantification and related risks, because most of the physical parameters, which are used for landslide modeling, are derived from geotechnical tests or the emerging geophysical approaches.

Remodeling of DNA replication structures by the branch point translocase FANCM

Fanconi anemia (FA) is a genetically heterogeneous chromosome instability syndrome associated with congenital abnormalities, bone marrow failure, and cancer predisposition. Eight FA proteins form a nuclear core complex, which promotes tolerance of DNA lesions in S phase, but the underlying mechanisms are still elusive. We reported recently that the FA core complex protein FANCM can translocate Holliday junctions. Here we show that FANCM promotes reversal of model replication forks via concerted displacement and annealing of the nascent and parental DNA strands. Fork reversal by FANCM also occurs when the lagging strand template is partially single-stranded and bound by RPA. The combined fork reversal and branch migration activities of FANCM lead to extensive regression of model replication forks. These observations provide evidence that FANCM can remodel replication fork structures and suggest a mechanism by which FANCM could promote DNA damage tolerance in S phase