[Archives de la Parole]. , La parabole de l'enfant prodigue : récit (dravidien, canara, province de Madras) / [Sir George Grierson], éd. ; Linguistic survey of India ; [D. Narayana Batt], voix

[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]. Etat du Karnara]

[Archives de la Parole]. , [Récit] : Indo-aryen, pata nûli, Province de Madras) / [Sir George Grierson], éd. ; Linguistic survey of India ; Voix parlée, homme

[Traditions. Asie. Inde. Présidence de Madras [i.e. Chennai]]

[Archives de la Parole]. , [The silly weaver girl] : récit (dravidien, malayālam, province de Madras) / [Sir George Grierson], éd. ; Linguistic survey of India ; [K.K. Achyutan], voix

[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]. État du Kérala. Kochi]

[Archives de la Parole]. , [Parable of the prodigal son] : Indo-aryen, dialecte sindhi, Province de Bombay / [Sir George Grierson], éd. ; Linguistic survey of India ; [Vishindas Bherumal], voix

[Traditions. Asie. Inde. Présidence de Bombay. Pakistan. Province du Sind. Haidarābād]

[Archives de la Parole]. , La parabole de l'enfant prodigue : Dravidien, Tamoul (groupe de l'Inde péninsulaire, Province de Madras) / [Sir George Grierson], éd. ; Linguistic survey of India ; [Krishnamacharya Ranga Nath], voix

[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]. Etat du Tamil Nadu. Thanjavur]

[Archives de la Parole]. , [The king and the margosa seed] : récit en dravidien, telugu, Province de Madras / [Sir George Grierson], éd. ; Linguistic survey of India ; [K. Divakara Rao], voix

[Traditions. Asie. Inde. Présidence de Madras [i.e. Chennai]. Ceded Districts]

[Archives de la Parole]. , [The silly weaver girl] : récit (dravidien, Malayalam, Province de Madras) / [Sir George Grierson], éd. ; Linguistic survey of India ; [C.K. Gopalamenon], voix

[Traditions. Asie. Inde. Présidence de Madras [i.e. Chennai]. Etat du Kerala. Région du Malabar]

[Archives de la Parole]. , La parabole de l'enfant prodigue : dravidien, malayālam, province de Madras / [Sir George Grierson], éd. ; Linguistic survey of India ; [K.K. Achyutan], voix

[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]. État du Kérala. Kochi]

VOLUMES RELIES du Cabinet des titres : recherches de noblesse, armoriaux, preuves, histoires généalogiques. « Estat des lettres d'anoblissement obtenues par les particuliers cy-après nommez dans la province de Normandie, veriffiez en la Chambre des comptes de ladite province et registrez en la Cour des aydes, depuis 1520 jusques à present. » (1661).

Il y a une table alphabétique des noms de personnes à la fin du volume.

VOLUMES RELIES du Cabinet des titres : recherches de noblesse, armoriaux, preuves, histoires généalogiques. « Catalogue général des gentilshommes de la province de Languedoc ».

« Copie faite sur l'imprimé, à Pézenas, l'an 1676 ; « avec notes de Charles d'Hozier et de d'Hozier de Sérigny (1756). — Il y a une table alphabétique des noms en tête du volume.

La régulation des interdépendances entre les forêts et l'eau domestique en Indonésie : études de cas sur le site de Lombok : les captages de Bak Pakem et de Ranget (Province du Nusa Tenggera Occidental, île de Lombok, Indonésie)

Ce working paper débute par une longue introduction, qui expose les spécificités du contexte institutionnel indonésien. Ensuite, la première partie traite des règles prévues sur l'île de Lombok (kabupaten de Lombok Barat, en Indonésie) pour gérer les usages des forêts et de l'eau potable ainsi que les règles qui visent à protéger le service forestier pour l'eau souterraine. Ensuite, en deuxième partie, deux études de cas montrent de quelle manière ces règles sont mises en oeuvre (ou pas) pour protéger les captages d'eau. L'écart entre les règles prévues et leur utilisation sur le terrain est expliqué, en troisième partie, à l'aide du cadre d'analyse des régimes institutionnels des ressources (RIR). Cette analyse permet de discuter en profondeur les mécanismes institutionnels en oeuvre et les enjeux en présence dans le contexte indonésien.

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.

Analysis of past and future dam formation and failure in the Santa Cruz River (San Juan province, Argentina)

Around 11.5 * 106 m3 of rock detached from the eastern slope of the Santa Cruz valley (San Juan province, Argentina) in the first fortnight of January 2005. The rockslide?debris avalanche blocked the course, resulting in the development of a lake with maximum length of around 3.5 km. The increase in the inflow rate from 47,000?74,000 m3/d between April and October to 304,000 m3/d between late October and the first fortnight of November, accelerated the growing rate of the lake. On 12 November 2005 the dam failed, releasing 24.6 * 106 m3 of water. The resulting outburst flood caused damages mainly on infrastructure, and affected the facilities of a hydropower dam which was under construction 250 km downstream from the source area. In this work we describe causes and consequences of the natural dam formation and failure, and we dynamically model the 2005 rockslide?debris avalanche with DAN3D. Additionally, as a volume ~ 24 * 106 m3of rocks still remain unstable in the slope, we use the results of the back analysis to forecast the formation of a future natural dam. We analyzed two potential scenarios: a partial slope failure of 6.5 * 106 m3 and a worst case where all the unstable volume remaining in the slope fails. The spreading of those potential events shows that a new blockage of the Santa Cruz River is likely to occur. According to their modeled morphometry and the contributing watershed upstream the blockage area, as the one of 2005, the dams would also be unstable. This study shows the importance of back and forward analysis that can be carried out to obtain critical information for land use planning, hazards mitigation, and emergency management.

Phlebotomines (Diptera, Psychodidae) in the Ribeira Valley Speleological Province - 1. Parque Estadual Intervales, state of São Paulo, Brazil

The identification of the sandfly fauna and investigation of some ecological aspects of its populations in areas frequented by tourists of the PEI, an Atlantic forest reserve with many caves, were the objective of this study. Captures were undertaken monthly from January 2001 to December 2002, with automatic light traps installed in 13 ecotopes, including caves, forests, domiciliary and peridomiciliary environments, and by aspiration in armadillo burrows. Additionally, although not at regular intervals, Shannon traps were installed in forests and anthropic environments, aspirations were made on cave walls, among roots and fallen leaves, and some insects were captured while biting researchers. A total of 891 sandflies belonging to 21 species were captured. Six hundred specimens representing 19 species were captured with light traps, 215 in anthropic (2.24 insects/trap) and 385 in extra-domiciliary (1.46 insects/trap) environments. Brumptomyia troglodytes was the most abundant species (the Standardised Index of Species Abundance = 0.705). Pintomyia monticola predominated in the Shannon traps and showed anthropophilic and diurnal activity. Psathyromyia pascalei predominated in the aspirations; the largest number being in armadillo burrows. Eleven species were captured in caves; although some might be troglophiles, the majority used these ecotopes as resting places. Nyssomyia intermedia, Nyssomyia neivai and Migonemyia migonei, implicated in the transmission of cutaneous leishmaniasis in the Southeastern Brazilian region, were all found, though in such low densities as to suggest minimal risk of the disease in the PEI.