High-resolution ammonite and carbon isotope stratigraphy across the Triassic-Jurassic boundary at New York Canyon (Nevada)

The Triassic-Jurassic boundary is generally considered as one of the major extinctions in the history of Phanerozoic. The high-resolution ammonite correlations and carbon isotope marine record in the New York Canyon area allow to distinguish two negative carbon excursions across this boundary with different paleoenvironmental meanings. The Late Rhaetian negative excursion is related to the extinction and regressive phase. The Early Hettangian delta(13)C(org) negative excursion is associated with a major floristic turnover and major ammonite and radiolarian radiation. The end-Triassic extinction-Early Jurassic recovery is fully compatible with a volcanism-triggered crisis, probably related to the Central Atlantic Magmatic Province. The main environmental stress might have been generated by repeated release of SO(2) gas, heavy metals emissions, darkening, and subsequent cooling. This phase was followed by a major long-term CO(2) accumulation during the Early Hettangian with development of nutrient-rich marine waters favouring the recovery of productivity and deposition of black shales. (C) 2004 Elsevier B.V. All rights reserved.

En el destierro del arte

En los años 30 del siglo XX, mientras las primeras vanguardias artísticas recorren Europa, María Zambrano y Martin Heidegger denuncian la pérdida del lugar del arte. El arte, para Zambrano, ya no da a ver, sólo se ve como arte. Por ello, perdió la tierra, está desterrado. Para Heidegger, por su parte, muchas de las obras de arte del siglo XX no pueden establecer un mundo y producir la tierra. En ese destierro del arte nos situaremos para interrogar el papel de la música en el pensamiento de ambos filósofos

Lake dwellers occupation gap in Lake Geneva (France-Switzerland) possibly explained by an earthquake-mass movement-tsunami event during Early Bronze Age

High-resolution seismic and sediment core data from the 'Grand Lac' basin of Lake Geneva reveal traces of repeated slope instabilities with one main slide-evolved mass-flow (minimum volume 0.13 km3) that originated from the northern lateral slope of the lake near the city of Lausanne. Radiocarbon dating of organic remains sampled from the top of the main deposit gives an age interval of 1865-1608 BC. This date coincides with the age interval for a mass movement event described in the 'Petit Lac' basin of Lake Geneva (1872-1622 BC). Because multiple mass movements took place at the same time in different parts of the lake, we consider the most likely trigger mechanism to be a strong earthquake (Mw 6) that occurred in the period between 1872 and 1608 BC. Based on numerical simulations, we show the major deposit near Lausanne would have generated a tsunami with local wave heights of up to 6 m. The combined effects of the earthquake and the following tsunami provide a possible explanation for a gap in lake dwellers occupation along the shores of Lake Geneva revealed by dendrochronological dating of two palafitte archaeological sites.

The lower Triassic anachronistic carbonate facies in space and time

The end-Permian mass extinction greatly affected the sedimentary record, but the sedimentary response was not limited to the Permian-Triassic boundary interval. This transformation extended to sedimentation that spanned the entire Early Triassic. Calcimicrobialites play an important role throughout this time interval, and at least four main events of anomalous carbonate deposition can be shown. A post-extinction calcimicrobial unit occurs above the extensive Permian skeletal carbonate platform exposed in the Taurus Mountains (southern Turkey), in south Armenia, north-west north and Central Iran along the Zagros Mountains. The calcimicrobial unit formed during the flooding of the platform that took place during the earliest Triassic. A similar calcimicrobialite formed during late Griesbachian to Dienerian time atop the shallow Permian skeletal carbonate platform largely exposed in south China. A third event occurred during the Early Olenekian on the first Mesozoic isolated pelagic plateau (Baid seamount, Oman Mountains). Here the change in carbonate sedimentation is reflected in the occurrence of thrombolites and carbonate seafloor fans. Near the end of Early Triassic time, unusual carbonate deposition is recorded both on an isolated pelagic plateau of the Western Tethys (Halstatt limestone of Dobrogea, Romania) and on the eastern Panthalassa margin of the western United States. In the western United States, the event is represented by stromatolites and thrombolites in the Virgin Limestone of the Moenkopi Formation and by seafloor fans in the middle and upper members of the Union Wash Formation. These unusual episodes of anomalous carbonate deposition illustrate a fundamental change in sedimentation that occurred in the aftermath of the end-Permian mass extinction.

Mineralogical alteration of artificial meteorites during atmospheric entry. The STONE-5 experiment

The generic concept of the artificial meteorite experiment STONE is to fix rock samples bearing microorganisms on the heat shield of a recoverable space capsule and to study their modifications during atmospheric re-entry. The STONE-5 experiment was performed mainly to answer astrobiological questions. The rock samples mounted on the heat shield were used (i) as a carrier for microorganisms and (ii) as internal control to verify whether physical conditions during atmospheric re-entry were comparable to those experienced by "real" meteorites. Samples of dolerite (an igneous rock), sandstone (a sedimentary rock), and gneiss impactite from Haughton Crater carrying endolithic cyanobacteria were fixed to the heat shield of the unmanned recoverable capsule FOTON-M2. Holes drilled on the back side of each rock sample were loaded with bacterial and fungal spores and with dried vegetative cryptoendoliths. The front of the gneissic sample was also soaked with cryptoendoliths. <p>The mineralogical differences between pre- and post-flight samples are detailed. Despite intense ablation resulting in deeply eroded samples, all rocks in part survived atmospheric re-entry. Temperatures attained during re-entry were high enough to melt dolerite, silica, and the gneiss impactite sample. The formation of fusion crusts in STONE-5 was a real novelty and strengthens the link with real meteorites. The exposed part of the dolerite is covered by a fusion crust consisting of silicate glass formed from the rock sample with an admixture of holder material (silica). Compositionally, the fusion crust varies from silica-rich areas (undissolved silica fibres of the holder material) to areas whose composition is "basaltic". Likewise, the fusion crust on the exposed gneiss surface was formed from gneiss with an admixture of holder material. The corresponding composition of the fusion crust varies from silica-rich areas to areas with "gneiss" composition (main component potassium-rich feldspar). The sandstone sample was retrieved intact and did not develop a fusion crust. Thermal decomposition of the calcite matrix followed by disintegration and liberation of the silicate grains prevented the formation of a melt.</p> <p>Furthermore, the non-exposed surface of all samples experienced strong thermal alterations. Hot gases released during ablation pervaded the empty space between sample and sample holder leading to intense local heating. The intense heating below the protective sample holder led to surface melting of the dolerite rock and to the formation of calcium-silicate rims on quartz grains in the sandstone sample. (c) 2008 Elsevier Ltd. All rights reserved.</p>

Obispos y gladiadores: El recurso a los profesionales del anfiteatro en disputas por la elección episcopal.

[spa]La costumbre de enrolar a combatientes del anfiteatro (arenarii) como guardia personal en el marco de luchas faccionales sobrevivió durante el siglo IV. Incluso si en la mayor parte de casos este fenómeno se explica por razones políticas, conocemos dos ejemplos en los que los candidatos a obispo recurrieron a gladiadores para triunfar sobre sus oponentes. El primer ejemplo está relacionado con la elección de Silvano (en el 305 o en el 307/308), quien llegó a hacerse elegir obispo de Cirta (actual Constantine)gracias a la ayuda del arenarius Muto. Esta ayuda quedó bien demostrada por el testimonio de diversas personas durante el proceso seguido contra Silvano en el 320, en el que se reconoció su culpabilidad y se le condenó al exilio. El segundo ejemplo es el del papa Dámaso (366), elegido obispo de Roma en la iglesia de Lucina el mismo día en el que el diácono Ursino era escogido en la basílica de Julio. En el conflicto siguiente, Dámaso convocó a arenarii, quadrigari y fossores, quienes acudieron en su ayuda fuertemente armados. Éstos atacaron la basílica en la que se habían refugiado los partidarios de Ursino y el resultado del asalto fue de 137 muertos. [eng]The habit of engaging fighters of the amphitheatre (arenarii) as a personal guard in the factional struggles survived during the 4th century. Although in most cases it was about political causes, we know two examples where the candidates to be bishops turned to gladiators in order to overcome their opponents. The first example is that of election of Silvanus (305 or 307-308), who got the bishopric of Cirta (the modern Constantine) thanks to the help of the arenarius Mutus. This help was proved by the testimony of several witnesses during the trial which was followed against Silvanus in 320, where his guilt was admitted and he was condemned to the exile. The second exemple is that of the the Pope Damasus (366), elected bishop of Rome in the church of Lucina in the same day as the deacon Ursinus was elected in the basilica of Julius. In the conflict that was to follow, Damasus called arenarii, quadrigarii and fossores who came to help him heavily armed. They attacked the basilica where the supporters of Ursinus had taken refuge and as a result of the assault 137 people died.

Poesia de Josep Carner a Bèlgica: creació, revisió, selecció, traducció

Capítol 4 del llibre 'Josep Carner: l'exili del mite (1945-1970)', sobre la poesia publicada per Carner durant la seva llarga estada a Bèlgica.

La voluntad del retorno: correspondencia desde el exilio catalán

[cat] El presente artículo ofrece una aproximación al complejo fenómeno del exilio provocado por la Guerra Civil española desde un punto de vista poco analizado hasta este momento: el estudio a través de los epistolarios existentes de los sentimientos personales que hizo aflorar este abandono forzado del país (miedos, deseos, esperanzas, incertidumbres, preocupaciones e inquietudes, ánimos, etc.). Para conseguir esta visión más personal hemos basado nuestra investigación en el análisis de unas fuentes que consideramos poco trabajadas hasta el momento como son los epistolarios. El estudio de éstos, ya sean fuentes primarias depositadas en fondos de archivos diversos de Catalunya como los epistolarios editados, nos ha permitido obtener un testimonio personal y de primera mano de un fenómeno, el del exilio, tratado principalmente hasta ahora desde un punto de vista colectivo. El análisis, centrado básicamente en personajes catalanes y en el periodo comprendido entre 1939 y 1946 (cuando se desvanece definitivamente la esperanza que la victoria aliada provoque el fin del régimen) pone de manifiesto una voluntad común: el ansia del retorno.

Mekatronisen portaattomasti säädettävän ajoneuvotehonsiirtokoneiston suunnittelu ja simulointi

Työn tarkoituksena on tutkia tehonsiirron ratkaisuja, jotka mahdollistavat jatkuvanopeus ja -momentinsäädön. Työ on rajattu käsittämään kahta eri planeettavaihdetuotetta. Tutkimuksen kohteena ovat valittujen vaihdetuotteiden planeettapyörästöjen eri kytkentämahdollisuudet ja niiden vaikutus toisiinsa. Vaihteiden teknistä toteutusta ja toimivuutta tarkastellaan fyysisten testien, simuloinnin sekä analyyttisen laskennan avulla. Apuna työssä on käytetty Dymola simulointiohjelmaa, jossa kinemaattisten kuvakeliitäntöjen avulla on rakennettu virtuaalimalli tarkastellusta tuotteesta ja sen toiminnasta. Tietokoneen avulla luotua dynaamista simulointimallia on muokattu tutkimuksen edistyessä differentiaalisesti jatkuvasäätöisen momentinmuuntimen aikaan saamiseksi. Tuotteissa on käytetty aurinkopyörällisiä ja aurinkopyörättömiä planeettapyörästöjä. Ensimmäisessä tutkittavassa tuotteessa on kolme planeettapyörästöä ja toisessa kaksi. Teholähteeksi käy polttomoottori tai sähkömoottori. Välitys- ja pyörimissuhteiden muuntoon vaikuttaa planeettavaihteistoon kytketty sähkömoottori, jonka toimintaa voidaan ohjata erikseen. Työssä on selvitetty, millaisia kulmanopeuksia ja momentteja eri ajanhetkellä ja eri pisteissä simulointimallia esiintyy.Lisäksi selvitetään vaihteistojen portaattoman välityssuhteen muuntomahdollisuudet. Tarkoituksena on saada realistista informaatiota tutkittavien laitteiden toiminnasta. Johtavana ajatuksena on modernien menetelmien käyttäminen uusien innovaatioiden toimivuuden ja äärikohtien tutkimiseksi.

La Història oral com a patrimoni cultural immaterial: estudi de cas

En aquest treball es parteix de la concepció que la història oral i les històries de vida són elements del patrimoni cultural immaterial i com a tals caldria conservar i protegir. S’exposa el testimoni d’un ciutadà de Girona, Narcís Lecha, el meu avi matern, durant el període de la Segona República, la Guerra Civil i l’exili. A partir del qual extraurem diferents aspectes col•lectivament rellevants. L’objectiu principal d’aquest treball és l’estudi i la difusió d’una història de vida que ens aporta coneixement sobre un període cabdal de la nostra història

La Història oral com a patrimoni cultural immaterial: estudi de cas

En aquest treball es parteix de la concepció que la història oral i les històries de vida són elements del patrimoni cultural immaterial i com a tals caldria conservar i protegir. S’exposa el testimoni d’un ciutadà de Girona, Narcís Lecha, el meu avi matern, durant el període de la Segona República, la Guerra Civil i l’exili. A partir del qual extraurem diferents aspectes col•lectivament rellevants. L’objectiu principal d’aquest treball és l’estudi i la difusió d’una història de vida que ens aporta coneixement sobre un període cabdal de la nostra història

Geografías familiares bajo la dictadura franquista: exilio, clandestinidad, prisión

Este texto ahonda en las geografías políticas, sociales y familiares de Aurèlia Pijoan, la primera mujer que, médico de profesión, ha accedido a un cargo de representación municipal en Lleida. Casada con Luis Pérez García-Lago –secretario general del PSUC y la UGT en la Lleida de los años trenta y posteriormente máximo responsable del partido en el exilio mejicano-, continuó su compromiso a través de la Unión de Mujeres Españolas de México de la que llegó a convertirse en secretaria general. El artículo pretende, a la vez que reflexionar sobre el diálogo que se establece entre recuerdo y olvido, hacer visible la historia de los sin historia a partir de un centro de gravedad concreto, puesto que los itinerarios personales y familiares de Aurèlia Pijoan permiten recorrer las diversas caras del universo represivo franquista: exilio,clandestinidad y prisión.

Intracranial Aneurysm Rupture Is Predicted by Measures of Solar Activity.

OBJECTIVE: The cause precipitating intracranial aneurysm rupture remains unknown in many cases. It has been observed that aneurysm ruptures are clustered in time, but the trigger mechanism remains obscure. Because solar activity has been associated with cardiovascular mortality and morbidity, we decided to study its association to aneurysm rupture in the Swiss population. METHODS: Patient data were extracted from the Swiss SOS database, at time of analysis covering 918 consecutive patients with angiography-proven aneurysmal subarachnoid hemorrhage treated at 7 Swiss neurovascular centers between January 1, 2009, and December 31, 2011. The daily rupture frequency (RF) was correlated to the absolute amount and the change in various parameters of interest representing continuous measurements of solar activity (radioflux [F10.7 index], solar proton flux, solar flare occurrence, planetary K-index/planetary A-index, Space Environment Services Center [SESC] sunspot number and sunspot area) using Poisson regression analysis. RESULTS: During the period of interest, there were 517 days without recorded aneurysm rupture. There were 398, 139, 27, 12, 1, and 1 days with 1, 2, 3, 4, 5, and 6 ruptures per day. Poisson regression analysis demonstrated a significant correlation of F10.7 index and RF (incidence rate ratio [IRR] = 1.006303; standard error (SE) 0.0013201; 95% confidence interval (CI) 1.003719-1.008894; P < 0.001), according to which every 1-unit increase of the F10.7 index increased the count for an aneurysm to rupture by 0.63%. A likewise statistically significant relationship of both the SESC sunspot number (IRR 1.003413; SE 0.0007913; 95% CI 1.001864-1.004965; P < 0.001) and the sunspot area (IRR 1.000419; SE 0.0000866; 95% CI 1.000249-1.000589; P < 0.001) emerged. All other variables analyzed showed no significant correlation with RF. CONCLUSIONS: We found greater radioflux, SESC sunspot number, and sunspot area to be associated with an increased count of aneurysm rupture. The clinical meaningfulness of this statistical association must be interpreted carefully and future studies are warranted to rule out a type-1 error.