Organizational, direct support, and general support maintenance repair parts and special tools lists for installation kit MK-1820/GSG-10(V) (NSN 1290-01-070-8906) and power accessory kit MK-1821/GSG-10(V) (NSN 1290-01-071-4343).

Includes index.

Organizational, direct support, and general support maintenance repair parts and special tools list for installation kit, MK-1818/GSG-10(V) (NSN 1290-01-070-8908).

Includes index.

Operator's, organizational, direct support, and general support maintenance : electronics equipment installation kit MK-1819/GSG-10(V) (NSN 1290-01-070-8907) and power accessory kit MK-1821/GSG-10(V) (NSN 1290-01-071-4343) in cargo truck, 1 1/4 ton M561.

"1 June 1983."

A roll of the household expenses of Richard de Swinfield, bishop of Hereford, during part of the years 1289 and 1290.

The roll was under the charge of John de Kemeseye. cf. Pref.

Die Schlacht bei Benevent 26. Februar 1266.

Thesis (doctoral)--Friedrich-Wilhelms-Universitat, Berlin.

Beatrice Tyldesley /

Sadleir, M. 19th cent. fiction,

EVOCAÇÃO POÉTICA : O velar e o desvelar da obra pictórica Menino morto de Cândido Portinari à luz das concepções de Paul Tillich e de Martin Heidegger sobre as artes

A arte sempre esteve presente entre os humanos como um grande mistério. Sua característica polissêmica nos desafia a pensá-la como algo sempre aberto. Isto é, livre para que os indivíduos a experimentem de formas diversas. Nossa intenção, ao escolher a tela Menino morto do pintor Cândido Portinari, é mostrar que o encontro com uma obra de arte é forçosamente atual, vivo, surpreendente, extraordinário... Não apenas como um mero objeto de prazer, mas, sobretudo, como possibilidades de desvelar experiências originárias, abrindo gamas de sentidos que ajudam os seres humanos a significar a própria existência. Para seguir na investigação, privilegiam-se, nesta dissertação, os estudos sobre as artes do teólogo Paul Tillich e do filósofo Martin Heidegger. Para Tillich, numa obra de arte deve-se buscar o que se esconde no inaparente, pois é aí que reside a sua substância. Assim, na arte, como em qualquer manifestação cultural, por mais secular que aparente ser, se expressa sempre uma preocupação última. Para Heidegger, a arte é fonte de revelação da verdade. Todavia, essa revelação traz em si o ocultamento da mesma verdade, posto que a verdade e a não-verdade acontecem simultaneamente na obra de arte. Portanto, à luz dos estudos feitos por esses dois autores, tentamos captar o desnudar de Menino morto .(AU)

Epibenthic foraminiferal d13C in the Recent deep Arctic Ocean

Low planktic and benthic d18O and d13C values in sediments from the Nordic seas of cold stadials of the last glaciation have been attributed to brines, formed similar to modern ones in the Arctic Ocean. To expand on the carbon isotopes of this hypothesis I investigated benthic d13C from the modern Arctic Ocean. I show that mean d13C values of live epibenthic foraminifera from the deep Arctic basins are higher than mean d13C values of upper slope epibenthic foraminifera. This agrees with mean high d13C values of dissolved inorganic carbon (DIC) in Arctic Bottom Water (ABW), which are higher than mean d13CDIC values from shallower water masses of mainly Atlantic origin. However, adjustments for oceanic 13C-Suess depletion raise subsurface and intermediate water d13CDIC values over ABW d13CDIC ones. Accordingly, during preindustrial Holocene times, the d13CDIC of ABW was as high or higher than today, but lower than the d13CDIC of younger subsurface and intermediate water. If brine-enriched water significantly ventilated ABW, brines should have had high d13CDIC values. Analogously, high-d13CDIC brines may have been formed in the Nordic seas during warm interstadials. During cold stadials, when most of the Arctic Ocean was perennially sea-ice covered, a cessation of high-d13CDIC brine rejection may have lowered d13CDIC values of ABW, and ultimately the d13CDIC in Nordic seas intermediate and deep water. So, in contrast to the idea of enhanced brine formation during cold stadials, the results of this investigation imply that a cessation of brine rejection would be more likely.

(Table 1) Sample locations and clay mineral data of sediment surface samples from the Barents Sea region

A new surface sediment sample set gained in the western Barents Sea by the MAREANO program has been analysed for basic clay mineral assemblages. Distribution maps including additional samples from earlier German research cruises to and off Svalbard are compiled. Some trends in the clay mineral assemblages are related to the sub-Barents Sea geology because the Quaternary sediment cover is rather thin. Additionally, land masses like Svalbard and northern Scandinavia dominate the clay mineral signal with their erosional products. Dense bottom water, very often of brine origin, that flows within deep troughs, such as the Storfjorden or Bear Island Trough, transport the clay mineral signal from their origin to the Norwegian-Greenland Sea.