Cicéron, Songe de Scipion, avec le commentaire de Macrobe.

N° 26 des mss envoyés à Paris par Maugerard en octobre 1802; cf. B.n.F., département des Manuscrits, Archives Modernes 497; — abbaye d'Echternach (dioc. de Trèves), cf. titre "Continet"; 1789. Le patrimoine libéré, 152 et n° 96

"Comment. Boetii in periermenias librum Aristotelis.

N° 22 des mss envoyés à Paris par Maugerard en octobre 1802; cf. B.n.F., département des Manuscrits, Archives Modernes 497; — abbaye d'Echternach (dioc. de Trèves), cf. titre "Continet"; 1789. Le patrimoine libéré, 152 et n° 96

Passiones et vitae sanctorum.

Abbaye Saint-Maur-des-Fossés ; cf. B. de Montfaucon, Bibliotheca bibliothecarum, II, 1739, p.1141-1143 : "38. 1060. Sanctorum Vitae in compendium redactae". Ex-libris : F. 3: "Sancti Germani a Pratis" (XVIIIe s.).

S. Johannes Chrysostomus, Homiliae (1-82v, 87v-111, 132v-226v), De compunctione cordis (226v-264v), Tractatus de reparatione lapsi (264v-303).

Abbaye Saint-Maur-des-Fossés ; cf. B. de Montfaucon, Bibliotheca bibliothecarum, II, 1739, p. 1141-1143 : "60. 1083. S. Joan. Chrysostomi Homiliae de diversis.". Ex-libris : F. Bv : « Iste liber est sancti Petri... », suivi d'un anathème (Xe-XIe s.) ; f. B : "Sti Germani a Pratis" ; f. 1 : « ex libris monasterii Sancti Germani a pratis Parisiorum ». France.

Exposition de Jean diacre sur la Genèse, etc.

Catalogue de l'abbaye de Corbie (éd. d'E. Coyecque, Cat des mss des bibliothèques de France, XIX, p.XI-XLVIII) XIIIe s.: n°246; 1621: n°420 Ex-libris : f.1 : « Sti Germani a Pratis »

Fulcoius Bellovacensis, Vita metrica sancti Mauri (1-12v).

Saint-Maur-des-Fossés. (C. Denoël).

Rolandus Passagerii, Summa artis notariae (3-76v).

Abbaye Saint-Maur-des-Fossés ; cf. B. de Montfaucon, Bibliotheca bibliothecarum, II, 1739, p. 1141-1143 : "96. 1117. Summa artis Notariae per M. Rollandinum. / Summa M. Thomae de Capua" — Abbaye de Saint Germain des Prés, Paris. Ex-libris : F. 3 : "Sti Germani a Pratis".

Mélanges de grammaire, de dialectique et de mathématiques.

Regula Enchiriadis (3v). — Boetii commenta in isagogas (5). — Marciani Capellae astronomia (46v). — Boetii musica (60). — Gerbertus Constantino (105v). — Boetii geometria (107). — De mensuris etc. (123v et 165v). — E Julio Frontino (130v), et Columella (131). — Recettes de médecine et autres (133). — Sur les mètres (148). — Marius Plotius sacerdos de metris (150). — Musica Fortunatiani (158v).

Moralités de Pierre le Bercheur sur les Métamorphoses d'Ovide.

Catalogue de l'abbaye de Corbie (éd. d'E. Coyecque, Cat des mss des bibliothèques de France, XIX, p.XI-XLVIII) 1621: n°429 Ex-libris : f.1 : « Sti Germani a Pratis » ; — au verso du dernier f. de garde : « Corbeiensis Monasterii »

Fragments de mss.

Contient : Lettres de Suger et pièces relatives à Suger et à Yves, abbé de S. Denis ; Lettre du comte Étienne à Ade, sa femme, sur la croisade ; Lettres d'Yves de Chartres ; Poëme d'Adalberon, adressé au roi Robert ; Charte de l'abbaye de Gigny en 898 et passion de S. Nazaire et S. Celse ; Registre de la confrérie de S. Maur et S. Fiacre à Paris ; Ad Paulum III Augustini bibliothecarii de Via Pauli et de fontibus inducendis in eam ; Cérémonial du sacre

Transforming growth factor beta 1 production by CD4+ CD25+ regulatory T cells in peripheral blood mononuclear cells from healthy subjects stimulated with Leishmania guyanensis.

Transforming growth factor beta (TGF-beta) has been shown to be a central immunomodulator used by leishmaniae to escape effective mechanisms of protection in human and murine infections with these parasites. However, all the information is derived from studies of established infection, while little is known about TGF-beta production in response to Leishmania stimulation in healthy subjects. In this study, TGF-beta1 production was demonstrated in peripheral blood mononuclear cells from healthy subjects never exposed to leishmaniae in response to live Leishmania guyanensis, and the TGF-beta1-producing cells were described as a distinct subpopulation of CD4(+) CD25(+) regulatory T cells. The suppressive properties of CD4(+) CD25(+) T cells were demonstrated in vitro by their inhibition of production of interleukin 2 (IL-2) and IL-10 by CD4(+) CD25(-) T cells in the presence of either anti-CD3 or L. guyanensis. Although neutralization of TGF-beta1 did not reverse the suppressive activity of CD4(+) CD25(+) T cells activated by anti-CD3, it reversed the suppressive activity of CD4(+) CD25(+) T cells activated by L. guyanensis. Altogether our data demonstrated that TGF-beta1 is involved in the suppressive activity of L. guyanensis-stimulated CD4(+) CD25(+) T cells from healthy controls.

Geological setting of the Guelb Moghrein Fe oxide-Cu-Au-Co mineralization, Akjoujt area, Mauritania

The Guelb Moghrein Fe oxide-Cu-Au-Co deposit is located at the western boundary of the West African craton in NW Mauritania. The wall rocks to the mineralization represent a meta-volcanosedimentary succession typical of Archaean greenstone belts. Two types of meta-volcanic rocks are distinguished: (1) volcanoclastic rocks of rhyodacite-dacite composition (Sainte Barbe volcanic unit), which form the stratigraphic base; (2) tholeiitic andesites-basalts (Akjoujt meta-basalt unit). The trace element signature of both types is characteristic of a volcanic arc setting. A small meta-pelitic division belongs to the Sainte Barbe volcanic unit. A meta-carbonate body, which contains the mineralization, forms a tectonic lens in the Akjoujt meta-basalt unit. It can be defined by the high X(mg) (=36) of Fe-Mg carbonate, the REE pattern and the delta(13)C values of -18 to -17 parts per thousand as a marine precipitate similar to Archaean banded iron formation (BIF). Additionally, small slices of Fe-Mg clinoamphibole-chlorite schist in the meta-carbonate show characteristics of marine shale. This assemblage, therefore, does not represent an alteration product, but represents an iron formation unit deposited on a continental shelf, which probably belongs to the Lembeitih Formation. The hydrothermal mineralization at 2492 Ma was contemporaneous with regional D(2) thrusting of the Sainte Barbe volcanic unit and imbrications of the meta-carbonate in the upper greenschist facies. This resulted in the formation of an ore breccia in the meta-carbonate, which is enriched in Fe, Ni, Co, Cu, Bi, Mo, As and Au. Massive sulphide ore breccia contains up to 20 wt% Cu. The ore fluid was aqueous-carbonic in nature and either changed its composition from a Mg-rich oxidizing to an Fe-rich reducing fluid or the two fluid types mixed at the trap site. All lithologies at Guelb Moghrein were deformed by D(3) thrusting to the east in the lower greenschist facies. The mobility of REE in the retrogressed rocks explains the formation of a second generation of hydrothermal monazite, which was dated at c. 1742 Ma. Archaean rocks of the West African craton extend to the west to Guelb Moghrein. The active continental margin was deformed and mineralized in the Late Archaean-Early Proterozoic and again reactivated in the Mid-Proterozoic and Westphalian, showing that the western boundary of the craton was reactivated several times.