Mesianismo y política en la Alejandría helenística

Nuestra ponencia propone en primer lugar precisar qué significa realmente el término mesianismo. Desde el punto de vista investigativo nos interesan especialmente los trabajos sobre la cultura judía y cristiana entre los siglos II a.C. a II d.C. y los textos-fuente de esos estudios, debido a que el mesianismo dominaba muchos aspectos del ideario de ese período. La parte más relevante del trabajo se centra en las relaciones del pensamiento helenista de Filón con temáticas que resultan de la concurrencia de los ideales políticos y religiosos emergentes de la Biblia hebrea. Así, el tema general de la investigación será el pensamiento judío de Filón de Alejandría y los tópicos de la política: la conformación del pueblo, el mesianismo, la vida en el más allá, el destino individual y el de la comunidad, la elección divina y el universalismo

"Heliodoros/putifar" y el culto solar de Heliopolis (o las Etiópicas, una Loa a Augusto)

En este trabajo mostramos que, si hubo un culto solar en las Etiópicas de Heliodoro, no es el de Émesa del siglo III d.C. de los Severos, sino el de la antigua Heliópolis egipcia, que provee la base de la astronomía antigua. El gran sacerdote del templo del Sol (Ra) de Heliópolis se llamaba, en hebreo, "Putifar"; en griego, "Heliodoros": extraordinaria coincidencia, ya que el motivo de la mujer de Putifar de Génesis 39.7-20 ocupa un lugar destacado en la trama de la novela, pero ésta atiende estrictamente a sus modelos griegos clásicos. Proponemos, además, que la composición de la obra coincide con o surge del Carmen Sæculare de Horacio.

Age determination and paleotemperatures of sediment core MD95-2043 in the Alboran Sea

Past sea surface temperature (SST) evolution in the Alboran Sea (western Mediterranean) during the last 50,000 years has been inferred from the study of C37 alkenones in International Marine Global Change Studies MD952043 core. This record has a time resolution of ~200 years allowing the study of millennial-scale and even shorter climatic changes. The observed SST curve displays characteristic sequences of extremely rapid warming and cooling events along the glacial period. Comparison of this Alboran record with delta18O from Greenland ice (Greenland Ice Sheet Project 2 core) shows a strong parallelism between these SST oscillations and the Dansgaard-Oeschger events. Five prominent cooling episodes standing out in the SST profile are accompanied by an anomalous high abundance of Neogloboquadrina pachyderma sinistral which is confined to the duration of these cold intervals. These features and the isotopic record reflect drastic changes in the surface hydrography of the Alboran Sea in association with Heinrich events Hl-5.

"Heliodoros/putifar" y el culto solar de Heliopolis (o las Etiópicas, una Loa a Augusto)

En este trabajo mostramos que, si hubo un culto solar en las Etiópicas de Heliodoro, no es el de Émesa del siglo III d.C. de los Severos, sino el de la antigua Heliópolis egipcia, que provee la base de la astronomía antigua. El gran sacerdote del templo del Sol (Ra) de Heliópolis se llamaba, en hebreo, "Putifar"; en griego, "Heliodoros": extraordinaria coincidencia, ya que el motivo de la mujer de Putifar de Génesis 39.7-20 ocupa un lugar destacado en la trama de la novela, pero ésta atiende estrictamente a sus modelos griegos clásicos. Proponemos, además, que la composición de la obra coincide con o surge del Carmen Sæculare de Horacio.

Mesianismo y política en la Alejandría helenística

Nuestra ponencia propone en primer lugar precisar qué significa realmente el término mesianismo. Desde el punto de vista investigativo nos interesan especialmente los trabajos sobre la cultura judía y cristiana entre los siglos II a.C. a II d.C. y los textos-fuente de esos estudios, debido a que el mesianismo dominaba muchos aspectos del ideario de ese período. La parte más relevante del trabajo se centra en las relaciones del pensamiento helenista de Filón con temáticas que resultan de la concurrencia de los ideales políticos y religiosos emergentes de la Biblia hebrea. Así, el tema general de la investigación será el pensamiento judío de Filón de Alejandría y los tópicos de la política: la conformación del pueblo, el mesianismo, la vida en el más allá, el destino individual y el de la comunidad, la elección divina y el universalismo

Mesianismo y política en la Alejandría helenística

Nuestra ponencia propone en primer lugar precisar qué significa realmente el término mesianismo. Desde el punto de vista investigativo nos interesan especialmente los trabajos sobre la cultura judía y cristiana entre los siglos II a.C. a II d.C. y los textos-fuente de esos estudios, debido a que el mesianismo dominaba muchos aspectos del ideario de ese período. La parte más relevante del trabajo se centra en las relaciones del pensamiento helenista de Filón con temáticas que resultan de la concurrencia de los ideales políticos y religiosos emergentes de la Biblia hebrea. Así, el tema general de la investigación será el pensamiento judío de Filón de Alejandría y los tópicos de la política: la conformación del pueblo, el mesianismo, la vida en el más allá, el destino individual y el de la comunidad, la elección divina y el universalismo

"Heliodoros/putifar" y el culto solar de Heliopolis (o las Etiópicas, una Loa a Augusto)

En este trabajo mostramos que, si hubo un culto solar en las Etiópicas de Heliodoro, no es el de Émesa del siglo III d.C. de los Severos, sino el de la antigua Heliópolis egipcia, que provee la base de la astronomía antigua. El gran sacerdote del templo del Sol (Ra) de Heliópolis se llamaba, en hebreo, "Putifar"; en griego, "Heliodoros": extraordinaria coincidencia, ya que el motivo de la mujer de Putifar de Génesis 39.7-20 ocupa un lugar destacado en la trama de la novela, pero ésta atiende estrictamente a sus modelos griegos clásicos. Proponemos, además, que la composición de la obra coincide con o surge del Carmen Sæculare de Horacio.

Astronomically modulated Neogene sediment records of ODP Site 184-1148

General global cooling over the Neogene has been modulated by changes in Earth's orbital parameters. Investigations of deep-sea sediment sequences show that various orbital cycles can dominate climate records for different latitudes or for different time intervals. However, a comprehensive understanding of astronomical imprints over the entire Neogene has been elusive because of the general absence of long, continuous records extending beyond the Pliocene. We present benthic foraminiferal d18O and d13C records over the past 23 Ma at Ocean Drilling Program Site 1148 in the northern South China Sea and construct an astronomically tuned timescale (TJ08) for these records based on natural gamma radiation and color reflectance data at this site. Our results show that a 41 ka cycle has dominated sediment records at this location over the Neogene, displaying a linear response to orbital forcing. A 100 ka cycle has also been significant. However, it is correlated nonlinearly with Earth's orbital variations at the 100 ka band. The sediment records also display a prominent 405 ka cycle. Although this cycle was coherent with orbital forcing during the Oligocene and the early Miocene, it was not coherent with Earth's orbital variations at the 405 ka band over the whole Neogene. Amplification of Northern Hemisphere and Southern Hemisphere glaciation since the middle Miocene may be responsible for this change in sedimentary response. Our benthic foraminifera d18O and d13C records further exhibit amplitude variations with longer periods of 600, 1000, 1200, and 2400 ka. Apparently, these cycles are nonlinear responses to insolation forcing.

Oxygen and Carbon stable isotope ratios for Site U1334

The Oligocene-Miocene transition (OMT) (~23 Ma) is interpreted as a transient global cooling event, associated with a large-scale Antarctic ice sheet expansion. Here we present a 2.23 Myr long high-resolution (~3 kyr) benthic foraminiferal oxygen and carbon isotope (d18O and d13C) record from Integrated Ocean Drilling Program Site U1334 (eastern equatorial Pacific Ocean), covering the interval from 21.91 to 24.14 Ma. To date, five other high-resolution benthic foraminiferal stable isotope stratigraphies across this time interval have been published, showing a ~1 per mil increase in benthic foraminiferal d18O across the OMT. However, these records are still few and spatially limited and no clear understanding exists of the global versus local imprints. We show that trends and the amplitudes of change are similar at Site U1334 as in other high-resolution stable isotope records, suggesting that these represent global deep water signals. We create a benthic foraminiferal stable isotope stack across the OMT by combining Site U1334 with records from ODP Sites 926, 929, 1090, 1264, and 1218 to best approximate the global signal. We find that isotopic gradients between sites indicate interbasinal and intrabasinal variabilities in deep water masses and, in particular, note an offset between the equatorial Atlantic and the equatorial Pacific, suggesting that a distinct temperature gradient was present during the OMT between these deep water masses at low latitudes. A convergence in the d18O values between infaunal and epifaunal species occurs between 22.8 and 23.2 Ma, associated with the maximum d18O excursion at the OMT, suggesting climatic changes associated with the OMT had an effect on interspecies offsets of benthic foraminifera. Our data indicate a maximum glacioeustatic sea level change of ~50 m across the OMT.

Services PTAs: Lessons from Practice

Presentation given by Pierre Sauvé at the international conference on the political economy of liberalising trade in services at the Hebrew University in Jerusalem

Nanoindentation of Bridgman YBCO samples

In this study, the mechanical properties of YBa2Cu3O7−x, obtained by the Bridgman technique, were examined using a Berkovich tip indenter on the basal plane (0 0 1). Intrinsic hardness was measured by nanoindentation tests and corrected using the Nix and Gao model for this material. Furthermore, Vickers hardness tests were performed, in order to determine the possible size effect on these measurements. The results showed an underestimation of the hardness value when the tests were performed with large loads. Moreover, the elastic modulus of the Bridgman samples was 128 ± 5 GPa. Different residual imprints were visualised by atomic force microscopy and a focused ion beam, in order to observe superficial and internal fracturing. Mechanical properties presented a considerable reduction at the interface. This effect could be attributed to internal stress generated during the texturing process. In order to corroborate this hypothesis, an observation using transmission electron microscopy was performed.

Ferromanganese nodules and micro-hardgrounds associated with the Cadiz Contourite Channel (NE Atlantic): Palaeoenvironmental records of fluid venting and bottom currents

Ferromanganese nodule fields and hardgrounds have recently been discovered in the Cadiz Contourite Channel in the Gulf of Cadiz (850–1000 m). This channel is part of a large contourite depositional system generated by the Mediterranean Outflow Water. Ferromanganese deposits linked to contourites are interesting tools for palaeoenviromental studies and show an increasing economic interest as potential mineral resources for base and strategic metals. We present a complete characterisation of these deposits based on submarine photographs and geophysical, petrographic, mineralogical and geochemical data. The genesis and growth of ferromanganese deposits, strongly enriched in Fe vs. Mn (av. 39% vs. 6%) in this contourite depositional system result from the combination of hydrogenetic and diagenetic processes. The interaction of the Mediterranean Outflow Water with the continental margin has led to the formation of Late Pleistocene–Holocene ferromanganese mineral deposits, in parallel to the evolution of the contourite depositional system triggered by climatic and tectonic events. The diagenetic growth was fuelled by the anaerobic oxidation of thermogenic hydrocarbons (δ13CPDB=−20 to −37‰) and organic matter within the channel floor sediments, promoting the formation of Fe–Mn carbonate nodules. High 87Sr/86Sr isotopic values (up to 0.70993±0.00025) observed in the inner parts of nodules are related to the influence of radiogenic fluids fuelled by deep-seated fluid venting across the fault systems in the diapirs below the Cadiz Contourite Channel. Erosive action of the Mediterranean Outflow Water undercurrent could have exhumed the Fe–Mn carbonate nodules, especially in the glacial periods, when the lower core of the undercurrent was more active in the study area. The growth rate determined by 230Thexcess/232Th was 113±11 mm/Ma, supporting the hypothesis that the growth of the nodules records palaeoenvironmental changes during the last 70 ka. Ca-rich layers in the nodules could point to the interaction between the Mediterranean Outflow Water and the North Atlantic Deep Water during the Heinrich events. Siderite–rhodochrosite nodules exposed to the oxidising seabottom waters were replaced by Fe–Mn oxyhydroxides. Slow hydrogenetic growth of goethite from the seawaters is observed in the outermost parts of the exhumed nodules and hardgrounds, which show imprints of the Mediterranean Outflow Water with low 87Sr/86Sr isotopic values (down to 0.70693±0.00081). We propose a new genetic and evolutionary model for ferromanganese oxide nodules derived from ferromanganese carbonate nodules formed on continental margins above the carbonate compensation depth and dominated by hydrocarbon seepage structures and strong erosive action of bottom currents. We also compare and discuss the generation of ferromanganese deposits in the Cadiz Contourite Channel with that in other locations and suggest that our model can be applied to ferromanganiferous deposits in other contouritic systems affected by fluid venting.