Alfred James Hipkins, Kniestück, Profil, beim Musizieren

Signatur des Originals: S 36/F11580

James Nares, Brustbild

Signatur des Originals: S 36/G00108

Costume de Melle. Louise Fitz-James, Acte II.

Signatur des Originals: S 36/G10835

James Hook, Brustbild

Signatur des Originals: S 36/G01204

James Kwast, Brustbild

Signatur des Originals: S 36/G01336

James Kwast, Brustbild

Signatur des Originals: S 36/G01337

James Smith, Ganzfigurbildnis

Signatur des Originals: S 36/G02262

View of the Orchesta Organ in Westminster Abbey under the Direction of Mr. James Wyatt, for the Commemoration of Handel

Signatur des Originals: S 36/G02677

James Bartleman, Brustbild, Profil

Signatur des Originals: S 36/G02742

James Cook, Brustbild, Profil - James King, Brustbild

Signatur des Originals: S 36/G02908

An Inside View of the Pantheon exhibiting their Majesties Box & c. as fitted up under the direction of Mr. James Wyatt, for the Commemoration of Handel.

Signatur des Originals: S 36/G03858

James Bartleman, Brustbild

Signatur des Originals: S 36/G03906

Fanny Cerrito als Sylphide, Gustave Carey als James Reuben, Rollenbild, Doppelbildnis, in: Jean-Madeleine Schweitzhoeffer: La Sylphide

Signatur des Originals: S 36/G04001

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

Diversity and faunal composition of benthic foraminifera in Hole 44-390A on the Blake Nose Plateau

Benthic foraminiferal assemblages are a widespread tool to understand changes in organic matter flux and bottom-water oxygenation and their relation to paleoceanographic changes in the Upper Cretaceous oceans. In this study, assemblage data (diversity, total number, and number per species and gram) from Deep Sea Drilling Project (DSDP) Site 390 (Blake Nose, western North Atlantic) were processed for the lower Maastrichtian (Globotruncana falsostuarti - Gansserina gansseri Planktic Foraminiferal Zone). These data document significant changes in nutrient flux to the sea floor as well as bottom-water oxygenation during this time interval. Parallel to the observed changes in the benthic foraminiferal assemblages the number of inoceramid shells decreases, reflecting also a significant increase in bottom-water oxygenation. We speculate, that these data could reflect the onset of a shift from warmer low-latitude to cooler high-latitude deep-water sources. This speculation will predate the major reorganization of the oceanic circulation resulting in a circulation mode similar to today at the Early/Late Maastrichtian boundary by ~1 Ma and therefore improves our understanding of Late Cretaceous paleoceanography.