Les réformes au prisme de l'autonomie et du contrôle des agents publics de base : le cas de la politique suisse du chômage

Cet article se propose de réfléchir aux réformes de l'administration en étudiant ce qu'elles deviennent au niveau des agents publics de base ou 'street-level bureaucrats'. Si la littérature qui leur est consacrée a jusqu'ici mis en avant à la fois l'autonomie décisionnelle de ces acteurs ainsi que les stratégies de contrôle de celle-ci, nous proposons ici de revisiter la problématique de l'autonomie et du contrôle à ce niveau en rendant compte de la manière dont elle est affectée par les réformes de « nouvelle gestion publique » d'une part, et les « nouvelles technologies de l'information et de la communication » d'autre part. Pour ce faire, la partie empirique présente les résultats préliminaires d'une recherche de l'auteur portant sur un type d'agent public aux premières lignes de la mise en oeuvre de la politique suisse du chômage, à savoir les taxateurs d'une caisse cantonale d'indemnisation, laquelle fonctionne selon une logique « néo-managériale ». Les données analysées montrent que si les éléments du dispositif NGP/TIC conduisent globalement à un renforcement considérable du contrôle hiérarchique et organisationnel d'une autonomie qui reste néanmoins importante, ceci s'accompagne également de modes d'appropriation spécifiques et intéressants dans ce qu'ils ont d'inattendu, de créatif voire de subversif au niveau des agents sur le terrain.

Climate and sea-level variations along the northwestern Tethyan margin during the Valanginian C-isotope excursion: Mineralogical evidence from the Vocontian Basin (SE France)

A high resolution mineralogical study (bulk-rock and clay-fraction) was carried out upon the hemipelagic strata of the Angles section (Vocontian Basin, SE France) in which the Valanginian positive C-isotope excursion occurs. To investigate sea-level fluctuations and climate change respectively, a Detrital Index (DI: (phyllosilicates and quartz)/calcite) and a Weathering Index (WI: kaolinite/(illite + chlorite)) were established and compared to second-order sea-level fluctuations. In addition, the mineralogical data were compared with the High Nutrient Index (HNI, based on calcareous nannofossil taxa) data obtained by Duchamp-Alphonse et al. (2007), in order to assess the link between the hydrolysis conditions recorded on the surrounding continents and the trophic conditions inferred for the Vocontian Basin. It appears that the mineralogical distribution along the northwestern Tethyan margin is mainly influenced by sea-level changes during the Early Valanginian (Pertransiens to Stephanophorus ammonite Zones) and by climate variations from the late Early Valanginian to the base of the Hauterivian (top of the Stephanophorus to the Radiatus ammonite Zones). The sea-level fall observed in the Pertransiens ammonite Zone (Early Valanginian) is well expressed by an increase in detrital inputs (an increase in the DI) associated with a more proximal source and a shallower marine environment, whereas the sea-level rise recorded in the Stephanophorus ammonite Zone corresponds to a decrease in detrital influx (a decrease in the DI) as the source becomes more distal and the environment deeper. Interpretation of both DI and WI, indicates that the positive C-isotope excursion (top of the Stephanophorus to the Verrucosum ammonite Zones) is associated with an increase of detrital inputs under a stable, warm and humid climate, probably related to greenhouse conditions, the strongest hydrolysis conditions being reached at the maximum of the positive C-isotope excursion. From the Verrucosum ammonite Zone to the base of the Hauterivian (Radiatus ammonite Zone) climatic conditions evolved from weak hydrolysis conditions and, most likely, a cooler climate (resulting in a decrease in detrital inputs) to a seasonal climate in which more humid seasons alternated with more arid ones. The comparison of the WI to the HNI shows that the nutrification recorded al: the Angles section from the top of the Stephanophorus to the Radiatus ammonite Zones (including the positive C-isotope shift), is associated with climatic changes in the source areas. At that time, increased nutrient inputs were generally triggered by increased weathering processes in the source areas due to acceleration in the hydrological cycle under greenhouse conditions This scenario accords with the widely questioned palaeoenvironmental model proposed by Lini et al., (1992) and suggests that increasing greenhouse conditions are the main factor that drove the palaeoenvironmental changes observed in the hemipelagic realm of the Vocontian Basin, during the Valanginian positive C-isotope shift. This high-resolution mineralogical study highlights short-term climatic changes during the Valanginian, probably associated to rapid changes in the C-cycle. Coeval Massive Parana-Etendeka flood basalt eruptions may explain such rapid perturbations. (C) 2011 Elsevier B.V. All rights reserved.