Using vegetation to characterize the avalanche to Canal del Roc Roig, Vall de Núria (Eastern Pyrenees, Spain)

Avalanche hazard maps of high accuracy are difficult to produce. For land-use planning and management purposes, a good knowledge of extreme run-out zones and frequencies of avalanches is required. In the present work, vegetation recognition (especially focused on Pinus uncinata trees) and dendrochronological techniques are used to characterize avalanches that have occurred in historical times, helping to determine both the extent of large or extreme avalanches and their occurrence in time. Vegetation was studied at the Canal del Roc Roig (eastern Pyrenees, Spain) avalanche path. The avalanches descending this path affect the railway that reaches the Vall de Núria resort and the run-up to the opposite slope. During winter 1996, two important avalanches affecting this path were well documented. These are compared with the results of the vegetation study, consisting of an inventory of flora, the recording of vegetation damages along eight transverse profiles at different altitudes on the path and a dendrochronological sampling campaign. The data obtained contributed to a characterization of the predominant snow accumulation in the starting zone, the 1996 avalanches and the range of frequencies of large avalanches. Also, traces of avalanches that increase the path mapped in the avalanche paths map published by the Institut Cartogràfic de Catalunya in 2000 were identified, improving the initial existing information.

Systematics and phylogeography of the Dysdera erythrina species complex (Araneae, Dysderidae) in Sardinia

Sardinia is the second largest island in the Mediterranean and, together with Corsica and nearby mainland areas, one of the top biodiversity hotspots in the region. The origin of Sardinia traces back to the opening of the western Mediterranean in the late Oligocene. This geological event and the subsequent Messinian Salinity Crisis and Pleistocene glacial cycles have had a major impact on local biodiversity. The Dysdera woodlouse hunter spiders are one of the most diverse ground-dweller groups in the Mediterranean. Here we describe the first two species of this genus endemic to Sardinia: Dysdera jana sp. n. and Dysdera shardana sp. n. The two species show contrasting allopatric distribution: D. jana sp. n. is a narrow endemic while D. shardana sp. n. is distributed throughout most of the island. A multi-gene DNA sequence phylogenetic analys based on mitochondrial and nuclear genes supports the close relationships of the new species to the type species of the genus Dysdera erythrina. Age estimates reject Oligocene origin of the new Dysdera species and identify the Messinian Salinity Crises as the most plausible period for the split between Sardinian endemics and their closest relatives. Phylogeographic analysis reveals deep genetic divergences and population structure in Dysdera shardana sp. n., suggesting that restriction to gene flow probably due to environmental factors could explain local speciation events. Taxonomy, phylogeny, DNA sequencing, Mediterranean biogeography, phylogeography

Presencia de la icnoespecie Dactyloidites Ottoi en el complejo de abanico costero de Sant Llorenç del Munt (Eoceno, Cuenca del Ebro, NE de España).

The presence of Dactyloidites ottoi is first recorded in the Eocene Sant Llorenç del Munt fan-delta complex. This constitutes the first citation for the Paleogene. The ichnospecies occurs in the lower part of a prograding fan-delta front sequence, associated to other traces produced by sediment-feeders. This association is substituted in the upper part of the sequence by abundant vertical Ophiomorpha indicating an increase of energetic conditions. The paleoenvironmental setting interpreted for Dactyloidites is consistent with that of previous described occurrences.

Tècnica d'execució del frontal gòtic de Sant Llorenç de Morunys: a propòsit del dibuix preparatori

Els traços primigenis del dibuix preparatori del Frontal de Sant Llorenç de Morunys, al Museu Diocesà i Comarcal de Solsona, s"observen a ull nu, sense haver d"emprar tècniques sofisticades, a causa d"una pèrdua important de l"estrat pictòric que, de conservar-se, impediria la lectura de les capes més profundes. S"han examinat aquestes traces, font de documentació privilegiada que se"ns ofereix per incrementar el coneixement de l"obra i també, per comprendre el procés d"elaboració d"una pintura sobre taula en el context del bisbat d"Urgell al tombant del segle XIII. Durant l"estudi ha estat possible reconstruir, amb el suport inestimable dels tractats medievals, la seqüència d"execució del dibuix preliminar: primer, la distribució provisional de les línies mestres a mà alçada, amb carbonet, seguit de la seva fixació amb una punta metàl·lica dura; segon, el traçat de l"esbós figuratiu, amb un estil tou, i el posterior repàs definitiu amb una agulla o punta afilada sobre l"estrat preparatori, creant un dibuix incís que romandria visible després de recobrir tota la superfície amb una làmina d"estany. Finalment, s"aplicaria una complexa policromia, que combinaria tècniques opaques i vernissos translúcids. La revisió d"un corpus d"obres catalanes de característiques similars, moltes en les reserves dels museus pel seu precari estat de conservació, podria aportar dades rellevants quant a les diferents tècniques del dibuix preparatori emprades en la pintura sobre taula d"època medieval.

Ager Tarraconensis 4. Els Antigons, una vil·la senyorial del Camp de Tarragona = Els Antigons, a High Status Villa in the Camp de Tarragona

La vil·la romana dels Antigons (Reus, tocant amb la Canonja) fou una de les més riques de l’ager Tarraconensis, raó per la qual ha merescut un tractament monogràfic. El nom ja indica la rellevància de les restes que s’hi han trobat des del segle XIX. És un jaciment dissortat, però: la construcció d’un complex industrial els anys 70 el va destruir en gran part i avui no en queda cap resta visible. En les excavacions d’urgència entre el 1976 i el 1979 es va recollir una importantíssima documentació. Destaca un forn del segle I dC on es produïen materials constructius i àmfores vineres. La vil·la experimentà un moment de gran riquesa la primera meitat del segle III, com ho indica el luxós nimfeu decorat amb estàtues, així com l’important abocador del mateix moment, que ha permès estudiar un abundantíssim conjunt de ceràmiques romanes. La vil·la perdurà almenys fins al segle V, i hi ha traces de freqüentació i ús en època visigòtica.

Active tectonics of the Alhama de Murcia fault, Betic Cordillera, Spain

We present an overview of the knowledge of the structure and the seismic behavior of the Alhama de Murcia Fault (AMF). We utilize a fault traces map created from a LIDAR DEM combined with the geodynamic setting, the analysis of the morphology, the distribution of seismicity, the geological information from E 1:50000 geological maps and the available paleoseismic data to describe the recent activity of the AMF. We discuss the importance of uncertainties regarding the structure and kinematics of the AMF applied to the interpretation and spatial correlation of the paleoseismic data. In particular, we discuss the nature of the faults dipping to the SE (antithetic to the main faults of the AMF) in several segments that have been studied in the previous paleoseismic works. A special chapter is dedicated to the analysis of the tectonic source of the Lorca 2011 earthquake that took place in between two large segments of the fault.

El neolític antic i l"inici de l"edat del bronze a les excavacions del nou conservatori del Liceu

[cat] En aquest article es presenta l"estudi interdisciplinari de les ocupacions prehistòriques recents (neolític i inici de l"edat del bronze) localitzades durant la construcció del Conservatori del Gran Liceu de Barcelona, al barri del Raval de la mateixa ciutat. Les restes ocupacionals corresponen a un assentament amb evidències d"estructures de combustió i diversos elements de suport. Hi destaca la conservació d"alguns magnífics fogars, així com un conjunt de materials abiòtics i biòtics que permeten augmentar el coneixement de les primeres comunitats agrícoles del Pla de Barcelona. [spa] En este artículo se presenta el estudio interdisciplinar de las ocupaciones prehistóricas recientes (Neolítico e inicio de la Edad del Bronce) localizadas durante la construcción del Conservatorio del Gran Liceo de Barcelona, en el barrio del Raval de la misma ciudad. Los restos de ocupación corresponden a un asentamiento con evidencias de estructuras de combustión y otros elementos de soporte. Entre ellos destaca la conservación de algunos magníficos hogares así como un conjunto de materiales abióticos y bióticos que permiten aumentar el conocimiento sobre las primeras comunidades agrícolas del llano de Barcelona. [eng] This paper presents the interdisciplinary study of the recent prehistoric occupations (Neolithic and Early Bronze Age) found during the construction of El Liceu Conservatoire in Barcelona"s El Raval district. Occupational remains correspond to a settlement with traces of combustion structures and several supporting elements. It emphasises the preservation of some magnificent fireplaces and a set of archaeological abitoic and biotic materials that can increase knowledge of the first farming communities in the Barcelona plain. [fra] Cet article présente l"étude interdisciplinaire des occupations préhistoriques récentes (néolithique et début de l"âge du bronze) localisées lors de la construction du Conservatoire du Grand Théâtre du Liceu (opéra) de Barcelone, dans le quartier du Raval. Les vestiges d"occupation correspondent à un établissement présentant des structures de combustion et différents éléments de support. On y remarque la conservation de quelques magnifiques foyers ainsi qu"un ensemble de matériaux abiotiques et biotiques qui peuvent enrichir les connaissances sur les premières communautés agricoles de la plaine de Barcelone.

Coherent patterns and self-induced diffraction of electrons on a thin nonlinear layer

Electron scattering on a thin layer where the potential depends self-consistently on the wave function has been studied. When the amplitude of the incident wave exceeds a certain threshold, a soliton-shaped brightening (darkening) appears on the layer causing diffraction of the wave. Thus the spontaneously formed transverse pattern can be viewed as a self-induced nonlinear quantum screen. Attractive or repulsive nonlinearities result in different phase shifts of the wave function on the screen, which give rise to quite different diffraction patterns. Among others, the nonlinearity can cause self-focusing of the incident wave into a beam, splitting in two "beams," single or double traces with suppressed reflection or transmission, etc.

Crassostrea patagonica (d'Orbigny, 1842) shell concentrations from the late Miocene Rio Negro province, NE Patagonia, Argentina

The Río Negro Formation (late Miocene-early Pliocene) mainly consists of continental deposits, but it contains a middle member of marine origin. It represents a transgressive-regressive sequence that can be seen at several outcrops along the N Patagonian coast. The taphonomical approach to the El Espigón marine deposits permits the identification of four main layers containing different kinds of skeletal accumulation, which mainly consist of oyster shells [Crassostrea patagonica (D'Orbigny, 1842)]. These concentrations display three different morphologies (pouches, pavements and bouquets) with a different taphonomic signature. These deposits were formed in shallow marine environments influenced by wave activity that produced valve concentrations of different entities. They contain several shell beds that represent event, composite, hiatal to lag skeletal concentrations. Traces of bioturbation in the sediment (Thalassinoides, Teichichnus) and bioerosion on the shells (Entobia, Gastrochaeonolites, Caulostrepsis), and encrusters (cirripeds, bryozoans), are also abundant in the outcrop and consititue common components of these Miocene materials. Layers 1 and 2 of the sequence were deposited in shoreface/foreshore environments at the beginning of a highstand systems tract, while layers 3 and 4 were deposited at the end, or at the beginning of a forced regression, in foreshore environments. A final erosional episode cut the top of the layer 4, which truncated the abundant bioturbaation developed there.

Morphological and Magnetic Properties of Superparamagnetic Carbon-Coated Fe Nanoparticles Produced by Arc Discharge.

Spherical carbon coated iron particles of nanometric diameter in the 5-10 nm range have been produced by arc discharge at near-atmospheric pressure conditions (using 5-8·10 4 Pa of He). The particles exhibit a crystalline dense iron core with an average diameter 7.4 ± 2.0 nm surrounded by a sealed carbon shell, shown by transmission electron microscopy (TEM), selected-area diffrac- tion (SAED), energy-dispersive X-ray analysis (STEM-EDX) and electron energy loss spectroscopy (EELS). The SAED, EDX and EELS results indicate a lack of traces of core oxidized phases showing an efficient protection role of the carbon shell. The magnetic properties of the nanoparticles have been investigated in the 5-300 K temperature range using a superconducting quantum interference device (SQUID). The results reveal a superparamagnetic behaviour with an average monodomain diameter of 7.6 nm of the nanoparticles. The zero field cooled and field cooled (ZFC-FC)magnetization curves show a blocking temperature (TB)at room temperature very suitable for biomedical applications (drug delivery, magnetic resonance imaging-MRI-, hyperthermia).