[Voyage en Italie : 1824-1830]. , Arc d'Aragon, plan de l'arc d'aragon servant d'Entrée au château neuf à Naples : [coupe longitudinale, plan] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 235

[Voyage en Italie : 1824-1830]. , Arc d'Aragon : [détails divers] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 237

[Voyage en Italie : 1824-1830]. , Clef de l'Arc de Trajan à Benevent, au dixième de l'exécution : [coupe, élévation frontale, élévation latérale] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 30

[Voyage en Italie : 1824-1830]. , Arc de Trajan à Bénévent. Détails au dixième de l'exécution : [détails] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 31

Mineral inventory of continuously erupting basaltic andesites at Arenal volcano, Costa Rica: implications for interpreting monotonous, crystal-rich, mafic arc stratigraphies

Except for the first 2 years since July 29, 1968, Arenal volcano has continuously erupted compositionally monotonous and phenocryst-rich (similar to35%) basaltic andesites composed of plagioclase (plag), orthopyroxene (opx), clinopyroxene (cpx), spinel olivine. Detailed textural and compositional analyses of phenocrysts, mineral inclusions, and microlites reveal comparable complexities in any given sample and identify mineral components that require a minimum of four crystallization environments. We suggest three distinct crystallization environments crystallized low Mg# (<78) silicate phases from andesitic magma but at different physical conditions, such as variable pressure of crystallization and water conditions. The dominant environment, i.e., the one which accounts for the majority of minerals and overprinted all other assemblages near rims of phenocrysts, cocrystallized clinopyroxene (Mg# similar to71-78), orthopyroxene (Mg# similar to71-78), titanomagnetite and plagioclase (An(60) to An(85)). The second environment cocrystallized clinopyroxene (Mg# 71-78), olivine (<Fo(78)), titanomagnetite, and very high An (similar to90) plagioclase, while the third cocrystallized clinopyroxene (Mg# 71-78) with high (>7) Al/Ti and high (>4 wt.%) Al2O3, titanomagnetite with considerable Al2O3 (10-18 wt.%) and possibly olivine but appears to lack plagioclase. A fourth crystallization environment is characterized by clinopyroxene (e.g., Mg#=similar to78-85; Cr2O3=0.15-0.7 wt.%), Al-, Cr-rich spinel olivine (similar toFo(80)), and in some circumstances high-An (>80) plagioclase. This assemblage seems to record mafic inputs into the Arenal system and crystallization at high to low pressures. Single crystals cannot be completely classified as xenocrysts, antecrysts (cognate crystals), or phenocrysts, because they often contain different parts each representing a different crystallization environment and thus belong to different categories. Bulk compositions are mostly too mafic to have crystallized the bulk of ferromagnesian minerals and thus likely do not represent liquid compositions. On the other hand, they are the cumulative products of multiple mixing events assembling melts and minerals from a variety of sources. The driving force for this multistage mixing evolution to generate erupting basaltic andesites is thought to be the ascent of mafic magma from lower crustal levels to subvolcanic depths which at the same time may also go through compositional modification by fractionation and assimilation of country rocks. Thus, mafic magmas become basaltic andesite through mixing, fractionation and assimilation by the time they arrive at subvolcanic depths. We infer new increments of basaltic andesite are supplied nearly continuously to the subvolcanic reservoir concurrently to the current eruption and that these new increments are blended into the residing, subvolcanic magma. Thus, the compositional monotony is mostly the product of repetitious production of very similar basaltic andesite. Furthermore, we propose that this quasi-constant supply of small increments of magma is the fundamental cause for small-scale, decade-long continuous volcanic activity; that is, the current eruption of Arenal is flux-controlled by inputs of mantle magmas. (C) 2004 Elsevier B.V. All rights reserved.

[Voyage en Italie : 1824-1830]. , Panoplia Manuscrit grec du Vatican XII[e] Siècle. St François d'Assise. XIII[e] Siècle : [sept motifs : cinq personnages (trois hommes nimbés, une Vierge à l'enfant et un personnage non identifé), une croix, détail ornemental d'un arc] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 614

[Voyage en Italie : 1824-1830]. , Arc de Gallien. Sur une Echelle de 0,010 P.M. : [élévation, plan, coupe] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 491

[Voyage en Italie : 1824-1830]. , Arc de Janus. Détails au huitième de l'Exécution : fragments trouvé dans les fouilles en 1826 ; clef de la face principale ; chambranles et appui des mèches : [détails, élévations, plans, profils] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 493

[Voyage en Italie : 1824-1830]. , Arc de Janus. Détails au huitième de l'Exécution : [détails et profils de corniches] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 492

[Voyage en Italie : 1824-1830]. , Arc de Septime Sévère dans le Velabre : [élévation et plan de l'arc, détail de l'inscription] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, n. d

[Voyage en Italie : 1824-1830]. , Arc de Septime Sévère dans le Velabre : [coupe sur l'arc, détail de l'entablement, plan du plafond, détail des caissons] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 494

[Voyage en Italie : 1824-1830]. , de l'Arc de Titus à Rome. Sur une Echelle de 008 P.M : [élévation partielle et coupe verticale d'une des piles de l'arc, au niveau d'une table ; profil du soubassement] : [dessin] / h. L. [Henri Labrouste]

Référence bibliographique : Weigert, 495

[Voyage en Italie : 1824-1830]. , Frise de l'arc de Titus à Rome : [trois motifs : figures ailées des écoinçons et détail de la frise] : [dessin] / [Henri Labrouste]

Référence bibliographique : Weigert, 496

The ArgR regulatory protein, a helper to the anaerobic regulator ANR during transcriptional activation of the arcD promoter in Pseudomonas aeruginosa.

Pseudomonas aeruginosa, when deprived of oxygen, generates ATP from arginine catabolism by enzymes of the arginine deiminase pathway, encoded by the arcDABC operon. Under conditions of low oxygen tension, the transcriptional activator ANR binds to a site centered 41.5 bp upstream of the arcD transcriptional start. ANR-mediated anaerobic induction was enhanced two- to threefold by extracellular arginine. This arginine effect depended, in trans, on the transcriptional regulator ArgR and, in cis, on an ArgR binding site centered at -73.5 bp in the arcD promoter. Binding of purified ArgR protein to this site was demonstrated by electrophoretic mobility shift assays and DNase I footprinting. This ArgR recognition site contained a sequence, 5'-TGACGC-3', which deviated in only 1 base from the common sequence motif 5'-TGTCGC-3' found in other ArgR binding sites of P. aeruginosa. Furthermore, an alignment of all known ArgR binding sites confirmed that they consist of two directly repeated half-sites. In the absence of ANR, arginine did not induce the arc operon, suggesting that ArgR alone does not activate the arcD promoter. According to a model proposed, ArgR makes physical contact with ANR and thereby facilitates initiation of arc transcription.