Ms. Praed. 195 - [Sammelband in 2 Teilen: Konvolut aus Handschrift und Inkunabel]

Vorbesitzer: Dominikanerkloster Frankfurt am Main

Inc. hebr. 18 (Ausst. 195) - Arbaʿah ṭurim P. 1: Ṭur Oraḥ Ḥayim

Vorbesitzer: Wilhelm Carl von Rothschild

Ms.Ff.F.Stoltze 3. 195 - Brief von Elisabeth Mentzel an Lyda Stoltze

Stoltze-Denkmal

Ms. lat. qu. 97 Bd. 4 - Memorie originali risguardanti le belle arti, Nr. 179 - 195

Vorbesitzer: Michelangelo Gualandi;

Geochemical data and mineralogical properties of bulk sediment composition of ODP Hole 195-1202B

During Leg 195 of the Ocean Drilling Program, Site 1202 was drilled in the subtropical northwestern Pacific Ocean beneath the Kuroshio (Black Current) between northern Taiwan and the Ryukyu Island Arc on the northern flank of the I-Lan Ridge at 1274 m water depth. The upper 110 m of the Site 1202 section, composed of dark grey calcareous silty clay, provide an expanded record of environmental changes during the last 28 kyr. The sediments were deposited at high sedimentation rates between 3.0 and 5.0 m/kyr and peak values of 9.0 m/kyr between 15.1 and 11.2 ka BP. Variations in the modes and sources of detrital sediment input, as inferred from sediment granulometry, mineralogy, and elemental XRF-scanner data, reflect changes in environmental boundary conditions related to sea-level changes, Kuroshio variability, and the climate-driven modes of fluvial runoff. The provenance data point to increased sediment supply from northwestern Taiwan between 28 and 19.5 ka BP and from East China sources between 19.5 and 11.2 ka BP. The change in provenance at 19.5 ka BP reflects increased fluvial runoff from the Yangtze River and strong sediment reworking from the East China Sea shelf in the course of increased humidity and postglacial sea-level rise, particularly after 15.1 ka BP. The Holocene was dominated by sediments that originated from rivers in northeastern Taiwan. For the pre-Holocene period prior to 11.2 ka BP, low portions of sortable silt (63-10 ?m) show that the Kuroshio did not enter the Okinawa Trough, because of low sea-level. In turn, high proportions of sortable silt and sediment provenance from northeastern Taiwan point to strong ocean circulation under the direct and persistent influence of the Kuroshio during the Holocene. The reentrance of the Kuroshio to the Okinawa Trough was heralded by two pulses in relative current strengthening at 11.2 and 9.5 ka BP, as documented by stepwise increases in sortable silt in the lower Holocene section. From a global perspective, environmental changes in the southern Okinawa Trough show affinities to climate change in the western Pacific warm pool with little influence of climate teleconnections from the North Atlantic realm, otherwise seen in many other marine and terrestrial palaeoclimate records from southeastern Asia.

VARGAS MARTÍNEZ, Gustavo, Bolívar y el poder. México, UNAM, 1991, 195 p.

Fil: Zalazar, Oscar.

Dujovne, León: El pensamiento histórico de Benedetto Croce. Buenos Aires, Santiago Rueda, 1968. 195 págs.

Fil: Biagini, Hugo.

Escritos de filosofía. Buenos Aires, Centro de Estudios Filosóficos, 1978, Nº 1, 195 págs.

Fil: Licata, Rosa.

La Ley Federal 24.195 y la evaluación de la calidad de la educación

Fil: Agudo de Córsico, María Celia Mercedes. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación. Instituto de Investigaciones en Humanidades y Ciencias Sociales (UNLP-CONICET); Argentina.

Jacqueline Assael. Intellectualité et Theatralité dans l'ouvre d'Euripide, Paris, Publicactions de la Faculté de Lettres, Arts, et Sciences Humaines de Nice, Les Belles Lettres, 1993, 195 pp.

Fil: Nápoli, Juan Tobías. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.