Sabbatliche Erinnerungen, 1852

[Paulus Cassel]

Die vollständigen Gebete der Israeliten für das ganze Jahr

uebersetzt und mit erklärenden Anmerkungen begleitet von R. J. Fürstenthal

Kilka slów o dziele Modły Starozytne Izraelitów z komentarzem "Moreh Derech" przez Daniela Neufelda

Mathias Bersohn

Die Hoschanot des Gaon R. Saadia

von Alexander Kohut

L' arbre de la vie : prières pour les malades, les mourants et les morts ; rite allemand et portugais (hébreu-français)

traduites ou composées par A. Ben Baruch Créhange

Altjüdische liturgische Gebete

ausgew. und mit Einleitungen hrsg. von D. W. Staerk

Prières journalières à l'usage des juifs portugais ou espagnols : ce volume contient les Prières de tous les Jours Ouvriers, des Samedis, des Ros-Hodes, de Hanouca, de Pourim, avec leurs Paraschiot, du Jeûne particulier & autres Prières, traduites de l'Hébreu ; auxquelles on a ajouté des notes élémentaires, pour en faciliter l'intelligence

par Mardochée Venture

Randbemerkungen zum täglichen Gebetbuche (Siddur)

von A. Berliner

Thermo -modulation of MuSVts110 splicing by inhibitory RNA sequences

Viral systems have contributed tremendously to the understanding of eukaryotic molecular biology. The proportional pattern of retroviral RNA expression offers many clues into the alternative splicing of cellular transcripts. The MuSVts110 virus presents an unusual expression system, where the mechanistic combination of RNA splicing and cellular transformation can be physiologically manipulated. Splicing of MuSVts110 pre-mRNA occurs inefficiently (30%-50%) at 33$\sp\circ$C or below and is subdued at 39$\sp\circ$C ($<$5%). Like most alternatively spliced cellular and retroviral transcripts, the MuSVts110 pre-mRNA contains cis-acting intron and exon sequences that attenuate splicing. These include a splicing inhibitory sequence at the 3$\prime$ end of the MuSVts110 v-mos exon, called the E2 Distal Element (E2DE), and a sub-optimal 3$\prime$ splice site. The E2DE directly inhibits MuSVts110 RNA splicing in a sequence-specific fashion at 39$\sp\circ$C but not at 28$\sp\circ$C, potentially through the association of cellular factors. Inefficient MuSVts110 splicing is pre-dominantly attributed to the utilization of multiple weak branchpoint sequences located between $-113$ and $-34$ nucleotides upstream of the 3$\prime$ splice site. The molecular control of MuSVts110 splicing, represented primarily by scattered multiple inefficient branchpoint sequences that are conditionally modulated by the E2DE at higher growth temperatures, is discussed. ^

Stable isotope record and planktonic foraminiferal fragmentation of the late Pleistocene section of ODP Hole 134-828A

A high-resolution record of foraminiferal fragmentation (a dissolution indicator) for the last 250 k.y. (isotopic Stages 1 to 7) is identified in the upper 61.9 m of Ocean Drilling Program (ODP) Hole 828A, west Vanuatu. This record is comparable in detail to the atmospheric CO2 record and the d18O stack. Phase shifts between preservation spikes and maximum ice volumes (d18O of Globigerinoides sacculifer) are analogous to those on Ontong Java Plateau. Mass spectrometer (AMS14C) dating of a sample taken at the base of dissolution cycle B1 and the position of the last glacial maximum indicates a lag in time of ~8 k.y. in the Vanuatu region for the last glacial termination. When dissolution spikes are compared with minimum ice volumes there is no phase shift for the last two glacial terminations. The difference between Vanuatu and Ontong Java Plateau may be explained by local CO2 sinks and the interplay between intermediate and deep water masses. Terrigenous input increasingly affected sediment of Hole 828A on the North d'Entrecasteaux Ridge (NDR) as it approached Espiritu Santo Island. Mud and silt suspended in mid-water flows become important after 125 ka, while turbidites bypass the New Hebrides Trench only towards the last glacial maximum (LGM). Terrigenous supply seems to affect the lysocline profile that changed from an "open ocean" to a "near continent" type, thus favoring dissolution. Fragmentation of planktonic foraminifers is a more sensitive indicator of lysocline variations than is foraminiferal susceptibility to dissolution, the foraminiferal dissolution index, the abundance of benthic foraminifers, or CaCO3 content. A modern foraminiferal lysocline for the neighboring area (between 10°S and 30°S, and 160°E and 180°E) is found at 3.1 km below sea level, compared to west Vanuatu where it is shallower. The past lysocline level was deeper than 3086 m during intervals of dissolution minima, and ranged from ~2550 to 3000 m during intervals of dissolution maxima. The high sedimentation rates (in the order of 10 to 50 cm/k.y.) found in Hole 828A offer a great potential for future high-resolution studies either in this hole or other western localities along the NDR. Areas of high sedimentation near continental regions have been discarded for paleoceanographic and/or paleoclimatic studies. Nonetheless, conditions analogous to those found in Hole 828A are expected to occur in many trench areas around the world where mid-water flows have preserved as yet undiscovered fine high-resolution sedimentary records.

Stable oxygen isotope record of corales from the Red Sea

In order to assess the ability of Porites corals to accurately record environmental variations, high-resolution (weekly/biweekly) coral delta18O records were obtained from four coral colonies from the northern Gulf of Aqaba, which grew at depths of 7, 19, 29, and 42 m along one transect. Adjacent to each colony, hourly temperatures, biweekly salinities, and monthly delta18O of seawater were continuously recorded over a period of 14 months (April 1999 to June 2000). Contrary to water temperature, which shows a regular and strong seasonal variation and change with depth, seawater delta18O exhibits a weak seasonality and little change with depth. Positive correlations between seawater delta18O and salinity were observed. The two parameters were related to each other by the equation delta18O Seawater (per mil, VSMOW) = 0.281 * Salinity - 9.14. The high-resolution coral delta18O records from this study show a regular pattern of seasonality and are able to capture fine details of the weekly average temperature records. They resolve more than 95% of the weekly average temperature range. On the other hand, attenuation and amplification of coral seasonal amplitudes were recorded in deep, slow-growing corals, which were not related to environmental effects (temperature and/or seawater delta18O) or sampling resolution. We propose that these result from a combined effect of subannual variations in extension rate and variable rates of spine thickening of skeletal structures within the tissue layer. However, no smoothing or distortion of the isotopic signals was observed due to calcification within the tissue layer in shallow-water, fast-growing corals. The calculations from coral delta18O calibrations against the in situ measurements show that temperature (T) is related to coral delta18O (delta c) and seawater delta18O (delta w) by the equation T (°C) = -5.38 (delta c - delta w) -1.08. Our results demonstrate that coral delta18O from the northern Gulf of Aqaba is a reliable recorder of temperature variations, and that there is a minor contribution of seawater delta18O to this proxy, which could be ignored.