Characterization of quaternary ammonium compounds in Flourensia xerophytic communities and response to UV-B radiation

As part of ongoing studies aimed at characterizing molecular components involved in the ecophysiological adaptations of native xerophytic plants from central Argentina, we demonstrated the presence of compatible solutes in Flourensia campestris (FC) and Flourensia oolepis (FO), specifically glycine betaine (GB) through TLC, LC, 1H NMR and 13C-NMR. GB content (leaves: 38±7μmolg-1 DW; adult plants>seedlings), and distribution (capitula>vegetative leaves>reproductive leaves>shoots>roots) were similar to other quaternary ammonium compound (QAC) accumulators. Flourensia seedlings from both species protected from UV-B exposure - a major abiotic stress in these natural environments - showed a significant increase of GB in the leaves (p<0.01) and a significant decrease in the roots (p<0.05). In FC and FO xerophytic shrub-dominated communities QACs were detected for the first time in 41% of co-occurring species (N=39), 14 of 28 natives (50%) and 2 of 11 exotics (18%), being GB in natives only (57% of QAC accumulators). GB may be considered as a chemotaxonomical character for the genus Flourensia, since it was also detected in Flourensia hirta, Flourensia niederleinii, Flourensia riparia, Flourensia fiebrigii, Flourensia macroligulata and Flourensia heterolepis. Our controlled UV-B experiments, set up in the same natural environment where these species grow, clearly show that solar UV-B - and therefore oxidative stress - is involved in regulating GB contents and within-plant distribution in FC and FO seedlings. The findings in Flourensia co-occurring native species suggest that QACs accumulation may be considered as a community-specific ecophysiological trait in these xerophytic environments. .Fil: Piazza, Leonardo A.. Universidad de Buenos Aires. Facultad de Agronomia. Sede Polo Universitario Punilla Centro; ArgentinaFil: López, D.. Universidad de Buenos Aires. Facultad de Agronomia. Sede Polo Universitario Punilla Centro; ArgentinaFil: Silva, Mariana Paola. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Agronomia. Sede Polo Universitario Punilla Centro; ArgentinaFil: Lopez Rivilli, Marisa Juana. Universidad de Buenos Aires. Facultad de Agronomia. Sede Polo Universitario Punilla Centro; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Cantero, Juan Jose. Universidad Nacional de Río Cuarto. Facultad de Agronomía y Veterinaria; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Instituto Multidisciplinario de Biología Vegetal. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Instituto Multidisciplinario de Biología Vegetal; ArgentinaFil: Tourn, G. M.. Universidad de Buenos Aires. Facultad de Agronomia. Sede Polo Universitario Punilla Centro; ArgentinaFil: Scopel, Ana Leonor. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Instituto de Investigaciones en Biociencias Agrícolas y Ambientales. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones en Biociencias Agrícolas y Ambientales; Argentin

Seismic effects in archaeological sites: Archaeoseismological cataloguing and quantification

The analysis of the damage caused by seismic events in archaeological sites provides significant information about ancient and historic earthquakes that can improve seismic hazard analysis. In this paper a methodological analysis to quantify the deformation of structural damage recorded in archaeological sites is proposed. This methodology focuses on the establishment of the seismic/non-seismic origin of the observed damage and consists of three phases: (a) identification and inventory of damage; (b) quantification of deformation; and (c) incorporation of the results to seismic catalogues. The first phase is the inventory and mapping of the damage according with the classification of archaeological effects of earthquakes (EAEs). The second phase is to quantify the deformation of damage by setting different parameters such as the direction of maximum horizontal strain (ey). This analysis is performed at different levels: for each of the recorded EAEs, for all the records of a particular category of EAEs, and finally for the complete archaeological site including all the categories of EAEs. The homogeneity of the results (damage orientation) allows us to establish the seismic origin of deformations. This methodology has been developed in the Roman site of Baelo Claudia (Cádiz, Spain) and has been applied to different historical earthquakes in the Iberian Peninsula. To calibrate the method, analyses on oriented damage were carried out immediately after the recent instrumental earthquakes of Lorca 2011 (5.1 Mw, Spain) and Emilia Romagna 2012 (5.9 Mw; Italy).The analysis of the damage caused by seismic events in archaeological sites provides significant information about ancient and historic earthquakes that can improve seismic hazard analysis. In this paper a methodological analysis to quantify the deformation of structural damage recorded in archaeological sites is proposed. This methodology focuses on the establishment of the seismic / non-seismic origin of the observed damage and consists of three phases: (a) identification and inventory of damage; (b) quantification of deformation; and (c) incorporation of the results to seismic catalogues. The first phase is the inventory and mapping of the damage according with the classification of archaeological effects of earthquakes (EAEs). The second phase is to quantify the deformation of damage by setting different parameters such as the direction of maximum horizontal strain (ey). This analysis is performed at different levels: for each of the recorded EAEs, for all the records of a particular category of EAEs, and finally for the complete archaeological site including all the categories of EAEs. The homogeneity of the results (damage orientation) allows us to establish the seismic origin of deformations. This methodology has been developed in the Roman site of Baelo Claudia (Cádiz, Spain) and has been applied to different historical earthquakes in the Iberian Peninsula. To calibrate the method, analyses on oriented damage were carried out immediately after the recent instrumental earthquakes of Lorca 2011 (5.1 Mw, Spain) and Emilia Romagna 2012 (5.9 Mw; Italy).Este trabajo ha sido financiado por los proyectos CGL2015-67169-P (QTECTSPAIN, USAL) y CATESI-07 (IGME). Es una contribución al INQUA TERPRO Project 1299 y a los grupos de trabajo QTECT-AEQUA y GQMAEQU

Beryllium anomalies in solar-type field stars

We present a study of beryllium (Be) abundances in a large sample of field solar-type dwarfs and sub-giants spanning a large range of effective temperatures. The analysis shows that Be is severely depleted for F stars, as expected by the light-element depletion models. However, we also show that Beryllium abundances decrease with decreasing temperature for stars cooler than $\sim$6000 K, a result that cannot be explained by current theoretical models including rotational mixing, but that is, at least in part, expected from the models that take into account internal wave physics. In particular, the light element abundances of the coolest and youngest stars in our sample suggest that Be, as well as lithium (Li), has already been burned early during their evolution. Furthermore, we find strong evidence for the existence of a Be-gap for solar-temperature stars. The analysis of Li and Be abundances in the sub-giants of our sample also shows the presence of one case that has still detectable amounts of Li, while Be is severely depleted. Finally, we compare the derived Be abundances with Li abundances derived using the same set of stellar parameters. This gives us the possibility to explore the temperatures for which the onset of Li and Be depletion occurs.Comment: 16 pages, 13 figures, accepted for publication in Astronomy & Astrophysic

Reappraisal of the 1863 huércal‐overa earthquake (Betic cordillera, se spain) by the analysis of esi‐07 environmental effects and building oriented damage

This work reviews the 1863 Huércal‐Overa earthquake (VI‐VII EMS) based on the environmental seismic intensity scale (ESI‐07) and oriented archaeoseismological building damage. The performed analysis identifies 23 environmental effects (EEEs) and 11 archaeoseismological effects (EAEs), completing a total of 34 intensity data‐points within the intensity zone ≥ VI EMS. The new ESI intensity data quintuplicate the previous intensity data‐points ≥ VI EMS (five localities) for this event. Sixteen of the identified EEEs indicate the occurrence of intensity VII‐VIII within the Almanzora valley, south of Huércal‐Overa, over an area of ca. 12–15 km2. Anomalies in water bodies, slope movements, hydrogeological anomalies, ground cracking, and other effects (gas emissions, tree shaking) are the more diagnostic EEEs—with one of them indicating a local maximum intensity of VIII‐IX ESI‐07 (Alboraija lake). Environmental earthquake damage of intensity ≥ VI covers an area of c. 100 km2, compatible with a VIII ESI intensity event. The spatial distribution of EEEs and EAEs indicates that the zone of Almanzora River Gorge, which was depopulated during the earthquake epoch, was the epicentral area, and compatible with seismotectonic data from active shallow blind thrusting beneath the Almagro Range. The use of ESI data in nearly unpopulated areas help to fill gaps between damaged localities (EMS data) multiplying intensity data‐points, providing a better definition of the intensity zones and offering a geological basis to look for suspect seismic sourcesCGL2015-67169-

Catalogue of the geological effects of earthquakes in Spain based on the ESI-07 macroseismic scale: A new database for seismic hazard analysis

This paper summarizes the content and scope of the “Catalogue of Earthquake Geological Effects in Spain”. The catalogue has been published by the Geological Survey of Spain (IGME) and constitutes the first official publication (in Spain) on seismic hazard containing geological information. The catalogue gathers the 51 stronger earthquakes that have occurred in Spain since the Neolithic period to the present and classifies earthquakes with geological or archaeological seismic records in paleoseismic, ancient, historical and instrumental earthquakes. The catalogue offers a variety of parametric information, quality indexes (Qe, Qi, Qg), and Environmental Seismic Intensity Scale (ESI-07) based description of environmental damage structured in individual “event files”. Sixteen of the 51 catalogued events present full information files (full event files), with individualized analyses of the geological and geoarchaeological data as well as graphic information with hybrid ESI-EMS intensity maps, ShakeMaps (seismic scenarios) and complementary kmz files (Google Earth) for each of the sixteen selected earthquakes; among which is the well-known AD 1755 Lisbon earthquake-tsunami. These selected earthquakes present individual environmental earthquake effects (EEE) or earthquake archaeoseismological effects (EAE) files for each catalogued effect containing specific site geo-information and graphic data (photos, graphs, maps, etc.). The second edition of the catalogue record 1027 EEEs and 187 EAEs, of which 322 effects have individual filesThis research was funded by the Spanish Research Project MINECO-FEDER CGL2015-67169-P (QTECSPAIN-USAL). This is contribution of the QTECT-AEQUA Working Group

Quantification of SPIO using T2* and phase imaging

Proceeding of: 17th Scientific Meeting, International Society for Magnetic Resonance in Medicine, 18-24 April, 2009, Honolulu, Hawai, USAPublicad

The blaSHV-5 gene is encoded in a compound transposon duplicated in tandem in Enterobacter cloacae

AbstractThe presence of blaSHV-5 is described in a compound transposon, duplicated in tandem and flanked by IS26 copies on a 70-kb conjugative plasmid (pHNM1), in an Enterobacter cloacae strain associated with a nosocomial outbreak that occurred in Mexico