The King Alfred millenary,

Mode of access: Internet.

History of the reign of Ferdinand and Isabella the Catholic /

Includes bibliographical references and index.

Napoleon and the Queen of Prussia : an historical romance /

Mode of access: Internet.

Real soldiers of fortune,

Major-General Henry Ronald Douglas MacIver.--Baron James Harden-Hickey.--Winston Spencer Churchill.--Captain Philo Norton McGiffin.--General William Walker, the king of the filibusters.--Major Burnham, chief of scouts.

Memoirs of Marguerite de Balois, written by herself.

Mode of access: Internet.

Caroline, the illustrious queen-consort of George II. and sometime queen-regent; a study of her life and time,

"A list of authorities": p. 627-29.

Hawaiian idylls of love and death,

"The following stories are concerned mainly with incidents bearing on the career of the first sovereign of the Hawaiian archipelago, Kamehameha I."--Introd.

Letters and poems of Queen Elisabeth (Carmen Sylva)

"Poems ('Vers libre') by Carmen Sylva": vol. II, p. 175-222.

Secret memoirs of Madame la marquise de Montespan,

Mode of access: Internet.

Frederick the Great, the memoirs of his reader, Henri de Catt (1758-1760)

Translation of: Unterhaltungen mit Friedrich dem Grossen.

A queen of indiscretions; the tragedy of Caroline of Brunswick, queen of England,

Mode of access: Internet.

Marie Antoinette and the downfall of royalty,

Covers the year 1792 to the proclamation of the republic. In continuation of "Marie-Antoinette and the end of the old reǵime" and "Marie Antoinette at the Tuileries."

(Table 1) Radiocarbon dates of core JM05-085-GC, South-Barents Sea

The Late Weichselian-Early Holocene variability of the North Atlantic Current has been studied with focus on the zonal component of this meridional transport during the transition from glacial to interglacial conditions. The investigated sediment core is from 409 m water depth in the SW Barents Sea. Eight Accelerator mass spectrometry (AMS) 14C dates show that the core covers the last 20,000 cal yr B.P. with a centennial scale resolution during Late Weichselian-Early Holocene. Planktic foraminiferal assemblages were analyzed using the >100 ?m size fraction and foraminiferal planktic and benthic d13C and d18O isotopes were measured. Furthermore, a range of physical and chemical analyses has been carried out on the bulk sediment samples. Four time periods have been identified which represent the varying oceanographic conditions in Ingøydjupet, a glacial trough located off the north coast of Norway in the SW Barents Sea. 1) The late glacial (before ca 15,000 cal yr B.P.) influenced by the nearby ice sheets with high amounts of sea ice- or iceberg-transported detritus. 2) The late Oldest Dryas stadial and the Bølling-Allerød interstadial (ca 15,000-12,700 cal yr B.P.) with cold surface water conditions influenced by the collapse of the nearby ice sheets, high amounts of sea ice- or iceberg-transported detritus and melt water and weak subsurface inflow of Atlantic Water. 3) The Younger Dryas cold stadial (12,700-11,650 cal yr B.P.) with low primary productivity and extensive sea ice cover and 4) The Preboreal and Early Holocene (11,650-6800 cal yr B.P. cal yr B.P.) with strong influx of Atlantic Water into the area, near absence of ice rafted debris and generally ameliorated conditions in both surface and bottom water masses as seen from a high flux of foraminifera and increased marine primary production.

Basin-scale architecture of deeply emplaced sill complexes : Jameson Land, East Greenland

We would like to thank reviewers Steffi Burchadt and Simon Passey for the considerate and careful reviews which improved this paper. Funding for data collection in study was provided from the research council of Norway through the PETROMAKS project 193059 and the Force Safari project. Funding for data analysis was provided from PETROMAKS through the Trias North project (234152). Dougal Jerram is partly supported by research council of Norway Centres of Excellence funding (223272, CEED). The data were acquired by Julien Vallet and Samuel Pitiot of Helimap Systems. Simon Buckley is acknowledged for help with data processing, and Gijs Henstra and Björn Nyberg for assistance in the field. Aka Lynge and Arild Andresen are thanked for logistical support