Des céramiques aux hommes : étude céramique des premiers horizons fouillés sous la cathédrale Saint-Pierre de Genève (1er millénaire av. J.-C. - 40 apr. J.-C.)

Résumé Le travail présenté est basé sur l'analyse systématique des 145'157 fragments de céramique émanant de 2137 ensembles recueillis entre 1976 et 2003 lors de la fouille de la cathédrale Saint-Pierre. Datés entre le Ier millénaire av. J-C. et le XIXe siècle, ils témoignent de l'ampleur et de la richesse des activités menées au sein de ce site phare de la ville de Genève. Les particularités observées pour les six premiers horizons reconnus, qui couvrent une période comprise entre le Ier millénaire av. J.-C. et 40 apr. J.-C., liées aux structures a priori énigmatiques mises en évidence lors de la fouille, ont orienté le champ d'étude vers une compréhension fine du mobilier recueilli dans ces strates anciennes. Ainsi cadrée, l'étude s'est concentrée sur 237 complexes céramiques ayant livré 23'129 fragments. La corrélation stratigraphique menée sur les 8000 m2 de terrain fouillé a permis de porter l'analyse sur la répartition spatiale du corpus considéré. Développée également sur le plan diachronique, cette démarche a largement contribué à la définition des activités menées sur le site. Ainsi, la concentration de fragments de panses d'amphore et de vaisselle de table importée de Campanie au pied d'un tertre mis en évidence sous le choeur de la cathédrale a conduit à reconnaître l'existence d'un banquet funéraire témoignant de l'ensevelissement sous tumulus d'un aristocrate allobroge décédé entre 120 et 70 av. J.-C. Réparties sur la totalité de la surface occupée par la nef de la cathédrale et des rues la flanquant, les quelques 1024 coupes à boire de La Tène finale mises au jour ont quant à elles permis d'identifier les surfaces de gravier qu'elles scellaient comme une aire de rassemblement ayant abrité des banquets tenus périodiquement. Le maintien de ces activités rituelles et collectives jusqu'au milieu du Ier siècle de notre ère conclut l'analyse diachronique. La mise en perspective historique des données recueillies sur le terrain souligne l'importance de l'antique oppidum extremum des Allobroges, dont le sort fut en 58 av. J.-C. à l'origine de la Guerre des Gaules.

The magmatic to hydrothermal evolution of the intrusive Mont Saint-Hilaire Complex: Insights into the late-stage evolution of peralkaline rocks

The Cretaceous Mont Saint-Hilaire complex (Quebec, Canada) comprises three major rock units that were emplaced in the following sequence: (I) gabbros; (II) diorites; (III) diverse partly agpaitic foid syenites. The major element compositions of the rock-forming minerals, age-corrected Nd and oxygen isotope data for mineral separates and trace element data of Fe-Mg silicates from the various lithologies imply a common source for all units. The distribution of the rare earth elements in clinopyroxene from the gabbros indicates an ocean island basalt type composition for the parental magma. Gabbros record temperatures of 1200 to 800 degrees C, variable silica activities between 0 center dot 7 and 0 center dot 3, and f(O2) values between -0 center dot 5 and +0 center dot 7 (log delta FMQ, where FMQ is fayalite-magnetite-quartz). The diorites crystallized under uniform a(SiO2) (a(SiO2) = 0 center dot 4-0 center dot 5) and more reduced f(O2) conditions (log delta FMQ similar to-1) between similar to 1100 and similar to 800 degrees C. Phase equilibria in various foid syenites indicate that silica activities decrease from 0 center dot 6-0 center dot 3 at similar to 1000 degrees C to < 0 center dot 3 at similar to 550 degrees C. Release of an aqueous fluid during the transition to the hydrothermal stage caused a(SiO2) to drop to very low values, which results from reduced SiO(2) solubilities in aqueous fluids compared with silicate melts. During the hydrothermal stage, high water activities stabilized zeolite-group minerals. Fluid inclusions record a complex post-magmatic history, which includes trapping of an aqueous fluid that unmixed from the restitic foid syenitic magma. Cogenetic aqueous and carbonic fluid inclusions reflect heterogeneous trapping of coexisting immiscible external fluids in the latest evolutionary stage. The O and C isotope characteristics of fluid-inclusion hosted CO(2) and late-stage carbonates imply that the surrounding limestones were the source of the external fluids. The mineral-rich syenitic rocks at Mont Saint-Hilaire evolved as follows: first, alkalis, high field strength and large ion lithophile elements were pre-enriched in the (late) magmatic and subsequent hydrothermal stages; second, percolation of external fluids in equilibrium with the carbonate host-rocks and mixing processes with internal fluids as well as fluid-rock interaction governed dissolution of pre-existing minerals, element transport and precipitation of mineral assemblages determined by locally variable parameters. It is this hydrothermal interplay between internal and external fluids that is responsible for the mineral wealth found at Mont Saint-Hilaire.

Molecular and isotopic characterization of organic samples from the wreck of the Saint-Etienne merchant ship (XVIIIth century): Identification of pitch, fat, hair and sulfur

The wreck U Pezzo, excavated within the Saint Florent Gulf in northern Corsica was identified as the pink, Saint Etienne, a merchant ship which sank on January 31, 1769. In order to determine the composition of organic materials used to coat the hull or to waterproof different parts of the pink, a study of several samples, using molecular biomarker and carbon isotopic analysis, was initiated. The results revealed that the remarkable yellow coat, covering the outside planks of the ship's bottom under the water line, is composed of sulfur, tallow (of ox and not of cetacean origin) and black pitch which corresponds to a mixture called ``couroi'' or ``stuff'. Onboard ropes had been submitted to a tarring treatment with pitch. Hairs mixed with pitch were identified in samples collected between the two layers of the hull or under the sheathing planking. The study also provides a key model for weathering of pitch, as different degrees of degradation were found between the surface and the heart of several samples. Accordingly, molecular parameters for alteration were proposed. Furthermore novel mixed esters between terpenic and diterpenic alcohols and the free major fatty acids (C(14:0), C(16:0), C(18:0)) were detected in the yellow coat. (C) 2009 Elsevier Ltd. All rights reserved.