A provisional host-index of the fungi of the United States, by W.G. Farlow and A.B. Seymour.

pt.1

Reise nach den Inseln Teneriffa, Trinidad, St. Thomas, St. Crux und Porto-Rico; auf Befehl der französischen Regierung, vom 30. Sept. 1796 bis zum 7. Juni 1789, unter der Leitung des Capitain Baudin unternommen, von Peter Le Dru. Mit Bemerkungen begleitet, nebst einer allgemeinen Ubersicht des ganzen westindischen Archipels, vorzüglich in Rücksicht der Kolonialwaaren, von E. A. W. Zimmermann.

Bd.2 (1811)

Sobre el Art Director. Paradigmas creativos: W. Addison, P. Rand y F. Depero

El present projecte descriu els inicis de la comunicació visual i la importància d’aquesta per els comerços que van néixer a rel de la Revolució Industrial. Analitza el moviment modern i l’aparició de la figura del Art Director als Estats Units en una època liderada per l’Avantguardisme i el Futurisme. S’endinsa en els treballs de tres figures importants en el món del disseny gràfic: William Addison, Paul Rand i Fortunato Depero. L’objectiu d’aquest treball es mostrar la influencia d’aquestes figures en la publicitat.

40Ar/39Ar dating of Penninic Front tectonic displacement (W Alps) during the Lower Oligocene (31-34 Ma)

Direct absolute dating of the Penninic Frontal Thrust tectonic motion is achieved using the Ar-40/Ar-39 technique in the Pelvoux Crystalline Massif (Western Alps). The dated phengites were formed syn-kinematically in shear zones. They underline the brittle-ductile stretching lineation, pressure-shadow fibres and slickensides consistent with underthrusting of the European continental slab below the propagating Penninic Thrust. Chlorite-phengite thermobarometry yields 10-15 km and T similar to 280 degrees C, while Ar-40/Ar-39 phengite ages mainly range between 34 and 30 Ma, with one younger age at 27 Ma. This Early Oligocene age range matches a major tectonic rearrangement of the Alpine chain. Preservation of prograde Ar-40/Ar-39 ages is ascribed to passive exhumation of the Pelvoux shear zone network, sandwiched between more external thrusts and the Penninic Front reactivated as an E-dipping detachment fault. Partial resetting in the Low Temperature part of argon spectra below 24 Ma is ascribed to brittle deformation and alteration of phengites.