Great Britain, Palestine and the Jews : Jewry's celebration of its national charter

Digitalisiert in Kooperation mit dem YIVO Institute for Jewish Research am Center for Jewish History, NY

The Congo Slave State : a protest against the new African slavery ; and an appeal to the public of Great Britain, of the United States, and of the Continent of Europe

by Edmund D. Morel

Mario Lanza als Caruso, Rollenbild, Kniestück, in: Joe Pasternak: The great Caruso

Signatur des Originals: S 36/F10889

Mario Lanza als Caruso, Rollenbild, in: Joe Pasternak: The great Caruso

Signatur des Originals: S 36/F10890

Great leaders of Hebrew history from Manasseh to John the Baptist

by Henry Thatcher Fowler

The Jews of the Empire and the Great War : by Michael Adler

Digitalisiert in Kooperation mit dem YIVO Institute for Jewish Research am Center for Jewish History, NY

The installation sermon of the very Rev. Dr. Joseph Herman Hertz : Chief rabbi of the United Hebrew Congregations of the British Empire ; Monday, April 14th, 5673-1913 ; at the Great Synagogue London

Digitalisiert in Kooperation mit dem YIVO Institute for Jewish Research am Center for Jewish History, NY

Members of "The Samoan Expeditionary Force" who made the supreme sacrifice in the Great War, 1914-1918

[by Stephen John Smith, late 5th (Wellington) Regiment, secretary Samoa administration in military occupation, 1915-1918]

Great Barrier Reef coral element/Ca and stable isotope data and U-Th ages from IODP Expedition 325

Tropical south-western Pacific temperatures are of vital importance to the Great Barrier Reef (GBR), but the role of sea surface temperatures (SSTs) in the growth of the GBR since the Last Glacial Maximum remains largely unknown. Here we present records of Sr/Ca and d18O for Last Glacial Maximum and deglacial corals that show a considerably steeper meridional SST gradient than the present day in the central GBR. We find a 1-2 °C larger temperature decrease between 17° and 20°S about 20,000 to 13,000 years ago. The result is best explained by the northward expansion of cooler subtropical waters due to a weakening of the South Pacific gyre and East Australian Current. Our findings indicate that the GBR experienced substantial meridional temperature change during the last deglaciation, and serve to explain anomalous deglacial drying of northeastern Australia. Overall, the GBR developed through significant SST change and may be more resilient than previously thought.

Th-U ages of a stalagmite from the Kleegruben Cave (Table 1)

A mass-spectrometric uranium-series dated stalagmite from the Central Alps of Austria provides unprecedented new insights into high-altitude climate change during the peak of isotope stage 3. The stalagmite formed continuously between 57 and 46 kyr before present. A series of 'Hendy tests' demonstrates that the outer parts of the sample show a progressive increase of both stable C and O isotope values. No such covariant increase was detected within the axial zone. This in conjunction with other observations suggests that the continuous stable oxygen isotope profile obtained from the axial zone of the stalagmite largely reflects the unaltered isotopic composition of the cave drip water. The delta18O record shows events of high delta18O values that correlate remarkably with Interstadials 15 (a and b), 14 and 12 identified in the Greenland ice cores. Interstadial 15b started rapidly at 55.6 kyr and lasted ~300 yr only, Interstadial 15a peaked 54.9 kyr ago and was even of shorter duration (~100 yr), and Interstadial 14 commenced 54.2 kyr ago and lasted ~3000 yr. This stalagmite thus represents one of the first terrestrial archives outside the high latitudes which record precisely dated Dansgaard-Oeschger (D/O) events during isotope stage 3. Provided that rapid D/O warmings occurred synchronously in Greenland and the European Alps, the new data provide an independent tool to improve the GRIP and GISP2 chronologies.