Napoléon et ses détracteurs,

Préface.--M. Taine.--Le prince de Metternich.--Bourrienne.--Madame de Rémusat.--L'abbé de Pradt.--Miot de Mélito.--Correspondance de Napoléon Ier.--L'homme et son œuvre.--Appendice.

Oeuvres de Fermat,

Bibliographie des travaux de Fermat avant les publications de son fils.--Le Diophante de Samuel Fermat (1670)--L'edition des Varia opera (1679)--Les autographes de Fermat.--Le premier projet d'édition complète et les papiers de Libri.--Le manuscrit Arbogast-Boncompagni.--Le manuscrit Vicq-d'Azyer-Boncompagni.--Les manuscrits de la Nationale, etc.: v.1, p. [ix]-xxxii.

Libres entretiens

No more published?

Jahrbuch des Deutschen Archäologischen Instituts.

Mode of access: Internet.

The second Belgian grey book.

"The translation contains only those portions of the book which are material to the position of Great Britain, namely, the whole of the first part and section 10 of the second part, which deals with the accusations brought against Belgium of having concluded a military agreement with Great Britain." cf. Prefatory note.

Oeuvres.

v. 1-3. De la recherche de la vérite.--v. 4. Conversations chrétiennes.--v. 5. Traité de la nature et de la grâce.--v. 10. Méditations chrétiennes et métaphysiques.--v. 11. Traité de moral.--v. 12-13. Entretiens sur la métaphysique et sur la religion. Entretiens sur la mort.--v. 14. Traité de l'amour de Dieu.--v. 15. Entretien d'un philosophie chrétien et d'un philosophie chinois.--v. 16. Réflexions sur la prémotion physique.--v. 17. Pièces joimtes, ecrits divers.--v. 18. Correspondance, actes et documents, 1638-1689.--v. 19. Correspondance, actes et documents, 1690-1715.

Sedimentology of the Okhotsk Sea

On the basis of two sedimentary records from the central Sea of Okhotsk, we reconstruct the closely coupled glacial/interglacial changes in terrigenous flux, marine productivity, and sea ice coverage over the past 1.1 Myr. The correspondance of our sedimentary records to the China loess grain size record (China loess particle timescale, CHILOPARTS) suggests that environmental changes in both the Sea of Okhotsk area and in SE Asia were closely related via the Siberian atmospheric high-pressure cell. During full glacial times our records point to a strong Siberian High causing northerly wind directions, the extension of the sea ice cover, and a reduced Amur River discharge. Deglacial maxima of terrigenous flux were succeeded by or synchronous to high-productivity events. Marine productivity was strengthened during glacial terminations because of an effective nutrient utilization at times of enhanced water column stratification and high nutrient supply from fluvial runoff and sea ice thawing. During interglacials, SE monsoonal winds prevailed, analogous to today's summer situation of a pronounced Mongolian Heat Low and a strong Hawaiian High. Strong freshwater discharge induced by high precipitation rates in the Amur drainage area and a seasonally reduced and mobile sea ice cover favored marine productivity (although being considerably lower than during the terminations) and a lowered flux of ice-rafted detritus.

Les limites du dialogue : Lahontan, les Jésuites, Bougainville

Collection : Cahiers d’histoire culturelle ; vol. 4