Travels and researches among the lakes and mountains of Eastern & Central Africa : from the journals of the late James Frederick Elton

from the journals of the late J. Frederick Elton, F.R.G.S., H.B.M. Consul at Mozambique ; edited and compiled by H.B. Cotterill

Na 1 Nachlass Max Horkheimer, 699 - Cultural Aspects of National Socialism. A Research Project (p. IX 170.15-17a - IX 170.19)

Neumann, Franz: Memorandum über Gespräche mit Harold Lasswell. 30.03.1941, Typoskript mit handschriftlichen Korekturen, 4 Blatt; Neumann, Franz: Memorandum über Gespräche mit Goodvin Watson. 21.05.1941, Typoskript, 2 Blatt; [Anderson, Eugene N.:] "Professor Anderson's Notes and criticisms to the project of German society and culture". Typoskript, 7 Blatt; "Budget for the proposed Research Project of Cultural Aspects of National Socialism". Handschriftliche Notizen, 1 Blatt; Institut of Social Research: Brief an Rockefeller Foundation, New York, 24.06.1941 verschiedene Typoskripte, zum Teil mit handschriftlichen Korrekturen, circa 35 Blatt; ein Manuskript, 6 Blatt; ein Entwurf, Typoskript, 1 Blatt; Adorno, Theodor W.: 2 Briefe an I. Berlin, ohne Ort, 1940-1941; Empfehlungsschreiben zur Unterstützung des Projekts, von: Lutz, Ralph H.: 1 Brief (Abschrift) an Frederick Pollock, 11.07.1941; MacIver, Robert M.: 1 Brief (Abschrift): an New York Foundation, ohne Ort, 07.07.1941; Shotwell, James T.: 1 Brief (Abschrift) an Frederick Pollock, Woodstock, 08.07.1941; Radin, MAx: 1 Brief (Abschrift) an New York Foundation, [Los Angeles], 08.07-1941; 5 Blatt; Antwortbriefe an das Institut bzw. Max Horkheimer aufgrund der Zusendung des Umrisses des Forschungsprojektes, von: Lorwin, Lewis L.; Wooleton, H.; O'Quin, Patricia, Odum, Howard W.; Fay, Sidney B.; Merriam, Charles E.; Hoover, Calvin B.; Garrison, Lloyd K.; März bis Mai 1941, 8 Blatt;

Richard O. Brooks – James Bernard Murphy (eds.), Augustine and Modern Law (Philosophers and Law), Farnham – Burlington, Ashgate, 2011. ISBN 978-0-7546- 2894-1, LIV-517 p.

Fil: Peretó Rivas, Rubén. Consejo Nacional de Investigaciones Científicas y Técnicas

Fitotecnia práctica. Por W. J. C. Lawrence, Ediciones Librería del Colegio. Buenos Aires, 1951.

Fil: F. F. G..

Revised age models and foraminiferal records obtained for the Last Interglacial period in six marine sediment cores

The dataset contains the revised age models and foraminiferal records obtained for the Last Interglacial period in six marine sediment cores: - the Southern Ocean core MD02-2488 (age model, sea surface temperatures, benthic d18O and d13C for the period 136-108 ka), - the North Atlantic core MD95-2042 (age model, planktic d18O, benthic d18O and d13C for the period 135-110 ka), - the North Atlantic core ODP 980 (age model, planktic d18O, sea surface temperatures, seawater d18O, benthic d18O and d13C, ice-rafted detritus for the period 135-110 ka), - the North Atlantic core CH69-K09 (age model, planktic d18O, sea surface temperatures, seawater d18O, benthic d18O and d13C, ice-rafted detritus for the period 135-110 ka), - the Norwegian Sea core MD95-2010 (age model, percentage of Neogloboquadrina pachyderma sinistral, sea surface temperatures, benthic d18O, ice-rafted detritus for the period 134-110 ka), - the Labrador Sea core EW9302-JPC2 (age model, percentage of Neogloboquadrina pachyderma sinistral, sea surface temperatures, benthic d18O for the period 134-110 ka).

(Table 3) Sedimentation rates of stage 1 and last glacial maximum from different Holes during cruises of RRS Discovery in 1984-1985 and 1987-1988, and RRS James Clark Ross in 1992-1993

Within the Scotia Sea, the axis of the Antarctic Circumpolar Current (ACC) is geographically confined, and sediments therefore contain a record of palaeo-flow speed uncomplicated by ACC axis migration. We outline Holocene and Last Glacial Maximum (LGM) current-controlled sedimentation using data from 3.5-kHz profiles, cores and current meter moorings. Geophysical surveys show areas of erosion and deposition controlled by Neogene basement topography. Deposition occurs in mounded sediment drifts or flatter areas, where 500-1000 m of sediment overlies acoustic basement. 3.5-kHz profiles show parallel, continuous sub-bottom reflectors with highest sedimentation rates in the centre of the drifts, and reflectors converging towards marginal zones of non-deposition. Locally, on the flanks of continental blocks (e.g. South Georgia), downslope processes are dominant. The absence of mudwaves on the sediment drifts may result from the unsteadiness of ACC flow. A core transect from the ACC axis south to the boundary with the Weddell Gyre shows a southward decrease in biogenic content, controlled by the Polar Front and the spring sea-ice edge. Both these features lay farther north at LGM. The cores have been dated by relative abundance of the radiolarian Cycladophora davisiana, and by changes in the biogenic Ba content, a palaeoproductivity indicator. Sedimentation rates range from 3 to 17 cm/ka. The grain size of Holocene sediments shows a coarsening trend from south to north, consistent with strongest bottom-current flow near the ACC axis, though interpretation is complicated by the presence of biogenic grains. Year-long current meter records indicate mean speeds from 7 cm/s in the south to 12 cm/s in the north, with benthic storm frequency increasing northwards. LGM sediments are predominantly terrigenous and show a clearer northward-coarsening trend, with well-sorted silts in the northern Scotia Sea. Assuming a constant terrigenous source, this implies stronger ACC flow at the LGM, contrasting with weaker Weddell Gyre flow deduced from earlier work.