A Hebrew Deluge story in cuneiform : and other epic fragments in the Pierpont Morgan Library

by Albert T. Clay

Fragments from the Cairo Genizah in the Freer Collection

ed. by Richard Gottheil ...

Le savoir des religions. Fragments d’historiographie religieuse

L’histoire des religions ne saurait se passer d’une réflexion préalable sur ses propres conditions d’élaboration. Qu’est-ce qu’un « savoir religieux », qu’est-ce qu’un savoir « sur le religieux », en quoi et comment se distinguent-ils l’un de l’autre ? Ce livre est issu d’une série de recherches et d’enquêtes portant sur des horizons historiques et culturels contrastés. Il montre comment un scribe mésopotamien, un philosophe grec, un clerc bouddhiste, un égyptologue contemporain, un historien des religions, etc, élaborent leurs savoirs, comment ces savoirs se transforment et se perpétuent, quelles fonctions ils remplissent, qui les met en oeuvre, où et comment ils s’enracinent, pourquoi ils meurent.

Schnidejoch und Lötschenpass. Archäologische Forschungen in den Berner Alpen. Schnidejoch et Lötschenpass. Investigations archéologiques dans les Alpes bernoises.

Archäologie in den Hochalpen: Vom Rückgang der Gletscher sind auch archäologische Objekte betroffen. Über Jahrtausende hinweg haben sie im Eis überdauert, nun kommen sie zum Vorschein. Im Hitzesommer 2003 fand eine Wanderin am Schnidejoch ein fremdartiges Objekt aus Birkenrinde. Es erwies sich als Teil eines 4800 Jahre alten Bogenfutterals. In den Jahren 2004 bis 2011 unternahm der Archäologische Dienst des Kantons Bern über 30 Begehungen der Nordseite und – zusammen mit der Walliser Kantonsarchäologie – auch der Südseite des Schnidejochs. Zahlreiche weitere Funde aus Holz, Leder und Metall konnten geborgen und wissenschaftlich untersucht werden. Einzigartige Funde Zu den spektakulärsten Funden vom Schnidejoch zählt das Bogenfutteral aus Birkenrinde. Weiter stechen aus den rund 900 Funden ein Pfeilbogen, mehrere vollständige Pfeile und Fragmente einer Schale aus Ulmenholz hervor. Es handelt sich dabei um das älteste Holzgefäss der Schweiz. Weitere herausragende Funde sind ein bronzezeitliches Holzgefäss aus Birkenrinde, eine bronzezeitliche Gewandnadel sowie Bekleidung und Schuhe aus Leder. Archéologie dans les Alpes bernoises Le recul des glaciers a aussi un impact sur les découvertes archéologiques. Il fait réapparaître des objets préservés dans les glaces depuis des millénaires. Pendant l’été caniculaire de 2003, une randonneuse a découvert un objet singulier en écorce de bouleau, qui s’est avéré être un morceau de carquois vieux de 4800 ans. De 2004 à 2011, le Service archéologique du canton de Berne s’est rendu plus de trente fois sur le versant nord du Schnidejoch et, en collaboration avec le Service d’archéologie du canton du Valais, sur le versant sud de ce col. De nombreux autres objets en bois, cuir et métal ont pu être mis au jour et étudiés scientifiquement. Des découvertes uniques Le carquois en écorce de bouleau constitue l’une des découvertes les plus sensationnelles du Schnidejoch. Parmi les quelque 900 objets mis au jour figurent un arc, plusieurs flèches complètes et les fragments d’un bol en bois d’orme. Ce bol est le plus ancien récipient en bois de Suisse. D’autres trouvailles spectaculaires ont été faites, notamment un récipient en écorce de bouleau et une épingle à vêtements datant de l’Âge du Bronze ainsi que des vêtements et des chaussures en cuir.

tRNA-derived fragments target the small ribosomal subunit to fine-tune translation

Post-transcriptional cleavage of RNA molecules to generate smaller fragments is a widespread mechanism that enlarges the structural and functional complexity of cellular RNomes. In particular, fragments deriving from both precursor and mature tRNAs represent one of the rapidly growing classes of post-transcriptional RNA pieces. Importantly, these tRNA-derived fragments (tRFs) possess distinct expression patterns, abundance, cellular localizations, or biological roles compared with their parental tRNA molecules [1]. Here we present evidence that tRFs from the archaeon Haloferax volcanii directly bind to ribosomes. In a previous genomic screen for ribosome-associated small RNAs we have identified a 26 residue long fragment originating from the 5’ part of valine tRNA (Val-tRF) to be by far the most abundant tRF in H. volcanii [2]. The Val-tRF is processed in a stress- dependent manner and was found to primarily target the small ribosomal subunit in vitro and in vivo. Translational activity was markedly reduced in the presence of Val-tRF, while control RNA fragments of similar length did not show inhibition of protein biosynthesis. Crosslinking experiments and subsequent primer extension analyses revealed the Val-tRF interaction site to surround the mRNA path in the 30S subunit. In support of this, binding experiments demonstrated that Val-tRF does compete with mRNAs for ribosome binding. Therefore this tRF represents a ribosome-bound non-protein-coding RNA (ncRNA) capable of regulating gene expression in H. volcanii under environmental stress conditions probably by fine-tuning the rate of protein production [1].

tRNA-derived fragments target the small ribosomal subunit to fine-tune translation

Post-transcriptional cleavage of RNA molecules to generate smaller fragments is a widespread mechanism that enlarges the structural and functional complexity of cellular RNomes. In particular, fragments deriving from both precursor and mature tRNAs represent one of the rapidly growing classes of post-transcriptional RNA pieces. Importantly, these tRNA-derived fragments (tRFs) possess distinct expression patterns, abundance, cellular localizations, or biological roles compared with their parental tRNA molecules [1]. Here we present evidence that tRFs from the archaeon Haloferax volcanii directly bind to ribosomes. In a previous genomic screen for ribosome-associated small RNAs we have identified a 26 residue long fragment originating from the 5’ part of valine tRNA (Val-tRF) to be by far the most abundant tRF in H. volcanii [2]. The Val-tRF is processed in a stress- dependent manner and was found to primarily target the small ribosomal subunit in vitro and in vivo. Translational activity was markedly reduced in the presence of Val-tRF, while control RNA fragments of similar length did not show inhibition of protein biosynthesis. Crosslinking experiments and subsequent primer extension analyses revealed the Val-tRF interaction site to surround the mRNA path in the 30S subunit. In support of this, binding experiments demonstrated that Val-tRF does compete with mRNAs for ribosome binding. Therefore this tRF represents a ribosome-associated non-protein-coding RNA (rancRNA) capable of regulating gene expression in H. volcanii under environmental stress conditions probably by fine-tuning the rate of protein production [3].

tRNA-derived fragments target the small ribosomal subunit to fine-tune translation

Post-transcriptional cleavage of RNA molecules to generate smaller fragments is a widespread mechanism that enlarges the structural and functional complexity of cellular RNomes. In particular, fragments deriving from both precursor and mature tRNAs represent one of the rapidly growing classes of post-transcriptional RNA pieces. Importantly, these tRNA-derived fragments (tRFs) possess distinct expression patterns, abundance, cellular localizations, or biological roles compared with their parental tRNA molecules [1]. Here we present evidence that tRFs from the halophilic archaeon Haloferax volcanii directly bind to ribosomes. In a previous genomic screen for ribosome-associated small RNAs we have identified a 26 residue long fragment originating from the 5’ part of valine tRNA (Val-tRF) to be by far the most abundant tRF in H. volcanii [2]. The Val-tRF is processed in a stress-dependent manner and was found to primarily target the small ribosomal subunit in vitro and in vivo. Translational activity was markedly reduced in the presence of Val-tRF, while control RNA fragments of similar length did not show inhibition of protein biosynthesis. Crosslinking experiments and subsequent primer extension analyses revealed the Val-tRF interaction site to surround the mRNA path in the 30S subunit. In support of this, binding experiments demonstrated that Val-tRF does compete with mRNAs for ribosome binding. Therefore this tRF represents a ribosome-associated non-coding RNA (rancRNA) capable of regulating gene expression in H. volcanii under environmental stress conditions probably by fine-tuning the rate of protein production [3].

An Avron rule for fragments of R-mingle

Axiomatic bases of admissible rules are obtained for fragments of the substructural logic R-mingle. In particular, it is shown that a ‘modus-ponens-like’ rule introduced by Arnon Avron forms a basis for the admissible rules of its implication and implication–fusion fragments, while a basis for the admissible rules of the full multiplicative fragment requires an additional countably infinite set of rules. Indeed, this latter case provides an example of a three-valued logic with a finitely axiomatizable consequence relation that has no finite basis for its admissible rules.

Selective sampling during catastrophic disruption: Mapping the location of reaccumulated fragments in the original parent body

In this paper, we simulate numerically the catastrophic disruption of a large asteroid as a result of a collision with a smaller projectile and the subsequent reaccumulation of fragments as a result of their mutual gravitational attractions. We then investigate the original location within the parent body of the small pieces that eventually reaccumulate to form the largest offspring of the disruption as a function of the internal structure of the parent body. We consider four cases that may represent the internal structure of such a body (whose diameter is fixed at 250 km) in various early stages of the Solar System evolution: fully molten, half molten (i.e., a 26 km-deep outer layer of melt containing half of the mass), solid except a thin molten layer (8 km thick) centered at 10 km depth, and fully solid. The solid material has properties of basalt. We then focus on the three largest offspring that have enough reaccumulated pieces to consider. Our results indicate that the particles that eventually reaccumulate to form the largest reaccumulated bodies retain a memory of their original locations in the parent body. Most particles in each reaccumulated body are clustered from the same original region, even if their reaccumulations take place far away. The extent of the original region varies considerably depending on the internal structure of the parent. It seems to shrink with the solidity of the body. The fraction of particles coming from a given depth is computed for the four cases, which can give constraints on the internal structure of parent bodies of some meteorites. As one example, we consider the ureilites, which in some petrogenetic models are inferred to have formed at particular depths within their parent body. (C) 2014 Elsevier Ltd. All rights reserved.

Ms. lat. qu. 142 Katalogband - Catalogue d'une importante collection de tableaux choisis dans diverses écoles et formant le cabinet de feu M. Fr. Wilmans de Francfort su le Mein par George, appréciateur d'objets d'arts

Alte Signatur: Art.Ff. 528

Stable isotope record and lithic fragments distribution in sediments of MIS9-14 of the North Atlantic

Stable isotope and ice-rafted debris records from three core sites in the mid-latitude North Atlantic (IODP Site U1313, MD01-2446, MD03-2699) are combined with records of ODP Sites 1056/1058 and 980 to reconstruct hydrographic conditions during the middle Pleistocene spanning Marine Isotope Stages (MIS) 9-14 (300-540 ka). Core MD03-2699 is the first high-resolution mid-Brunhes record from the North Atlantic's eastern boundary upwelling system covering the complete MIS 11c interval and MIS 13. The array of sites reflect western and eastern basin boundary current as well as north to south transect sampling of subpolar and transitional water masses and allow the reconstruction of transport pathways in the upper limb of the North Atlantic's circulation. Hydrographic conditions in the surface and deep ocean during peak interglacial MIS 9 and 11 were similar among all the sites with relative stable conditions and confirm prolonged warmth during MIS 11c also for the mid-latitudes. Sea surface temperature (SST) reconstructions further reveal that in the mid-latitude North Atlantic MIS 11c is associated with two plateaus, the younger one of which is slightly warmer. Enhanced subsurface northward heat transport in the eastern boundary current system, especially during early MIS 11c, is denoted by the presence of tropical planktic foraminifer species and raises the question how strongly it impacted the Portuguese upwelling system. Deep water ventilation at the onset of MIS 11c significantly preceded surface water ventilation. Although MIS 13 was generally colder and more variable than the younger interglacials the surface water circulation scheme was the same. The greatest differences between the sites existed during the glacial inceptions and glacials. Then a north - south trending hydrographic front separated the nearshore and offshore waters off Portugal. While offshore waters originated from the North Atlantic Current as indicated by the similarities between the records of IODP Site U1313, ODP Site 980 and MD01-2446, nearshore waters as recorded in core MD03-2699 derived from the Azores Current and thus the subtropical gyre. Except for MIS 12, Azores Current influence seems to be related to eastern boundary system dynamics and not to changes in the Atlantic overturning circulation.