California digest supplement, 1915-1919; a digest of the cases decided by the Supreme and Appellate courts of California and by the federal courts on questions of California law since Kerr's California digest, as contained in Raymond's 1916 supplement and in the 1917-1919 California current digests, inclusive, up to volume 178 California Supreme court reports, volume 37 California Appellate reports, and up to 58 California decisions, page 137; California Appellate decisions, page 258; 182 Pacific reporter (California cases), page 991; 258 Federal reporter (California cases), page 161; 39 Supreme court reporter (California cases), page 568. With references to Ruling case law, and important notes in American decisions, American state reports, Annotated cases, Lawyers' reports annotated, and American law reports, also an alphabetical table, direct and reverse, of all cases digested, showing on what page and under what subject each case is found digested in this digest, and also where the various California cases are cited in annotations in "The American series of annotated reports".

Mode of access: Internet.

DIVINDADES MLK E CULTO A MOLEK NOS QUADROS DA CRISE RELIGIOSA NO FINAL DA MONARQUIA DE JUDÁ (2 Reis 16,3; 17,17.31; 21,6; 23,10; KTU 1.100; 1.118; 1.161)

A dissertação é dirigida a um especial e não resolvido problema na descrição do desenvolvimento religioso de Israel. Em textos do Antigo Testamento acerca do sacrifício de humanos, há uma unidades literárias autônomas relacionadas ao culto a mOlek. Porém, alguns pesquisadores sustentam que o culto a mOlek não tem esta característica. A dissertação aspira a investigar este argumento, concentrando-se em fontes históricas (2Reis 16,3; 17,17.31; 21,6; 23,10). Discutindo fontes ugaríticas duas listas de divindades e um texto funerário nós perguntares acerca das características das divindades mLlK nas culturas cananéias. Em síntese, mOlek é uma divindade ctônica mas não é destinatária de sacrifícios humanos.(AU)

Depression to decolonization:Berclays Bank (DCO) in the West Indies, 1926-1962. By Kathleen E.A. Monteith. Kingston: University of the West Indies Press, 2008. xvi + 355pp. Illustrations, tables. figures, appendix, bibliography, notes, index. $30.00. ISBN: 879-976-640-198-6.

Book review

Stable isotope ratios and paleoceanaographic reconstructions from sediment cores 80-548 and 161-978A

Largely continuous millennial-scale records of benthic d18O, Mg/Ca-based temperature, and salinity variations in bottom waters were obtained from Deep Sea Drilling Project Site 548 (eastern Atlantic continental margin south of Ireland, 1250 m water depth) for the period between 3.7 and 3.0 million years ago. This site monitored mid-Pliocene changes in Mediterranean Outflow Water (MOW) documented by continuously high Nd values between -10.7 and -9. Site 978 (Alboran Sea, 1930 m water depth) provides a complementary record of bottom water variability in the westernmost Mediterranean Sea, which is taken to represent MOW composition at its source. Both sites are marked by a singular and persistent rise in bottom water salinities by 0.7-1.4 psu and in densities by ~1 kg m-3 from 3.5 to 3.3 Ma, which is matched by an average 3 °C increase in bottom water temperatures at Site 548. This event suggests the onset of strongly enhanced deep-water convection in the Mediterranean Sea and a related strengthened MOW flow, which implies a major aridification of the Mediterranean source region. In harmony with model suggestions, the enhanced MOW flow has possibly intensified Upper North Atlantic Deep Water formation.

Annotated record of the detailed examination of Mn deposits from DSDP Site 161, Leg 16 (Cores 16-161-1 and 16-161A-14)

DSDP 161 is located on the lower west flank of the East Pacific Rise about midway between the Clipperton and Clarion fracture zones which define the boundaries of a large structural block in the eastern Pacific. The site is about 4,000 km west of the present crest of the Rise. It is located near the northern edge of a zone of thick Cenozoic sediments which marks the general location of the equatorial zone of high biological productivity.