BUSCADOR RECOLECTA

Los datos constarían de 24 directorios, uno para cada terremoto con los datos brutos, procesados, y resultados. Se pueden comprimir/empaquetar en un archivo tar. El contenido se describe en el archivo README., Data files and modelling results of regional centroid moment tensors obtained for earthquakes in the 2016 South Alboran seismic crisis, and presented in the article "Earthquake crisis unveils the growth of an incipient continental fault system", by Eulàlia Gràcia et al. Large continental faults extend for thousands of kilometres to form boundaries between rigid tectonic blocks. These faults are often associated with prominent topographic features, and they can produce large earthquakes. Here we present first evidence of such a major tectonic structure in its initial growing stage, the Al-Idrissi Fault System (AIFS), in the Alboran Sea. Until now, this fault system had always been described as a complex diffuse boundary between Eurasia and Nubia plates. However, combining newly acquired high-resolution bathymetric and seismic reflection data, together with seismological analyses of the 2016 Mw 6.4 earthquake offshore Morocco – the largest event ever recorded in the area – we unveil a 3D geometry for the AIFS, which definitively correspond to a crustal-scale boundary. We report evidence of left-lateral strike-slip displacement, characterize fault segmentation and demonstrate that the AIFS is the source of the 2016 events. The occurrence of the Mw 6.4 earthquake together with historical and instrumental events supports that the AIFS is currently growing through propagation and linkage of its segments. Thus, the AIFS provides a unique model for inception and growth of a young continental fault system., MINECO CGL2011-30005-C02-02, CTM2015-70155-R and Acción IDRISSI (MINECO/FEDER), The structure of the dataset is indicated in README.txt, Peer reviewed

Ex situ programmes have become critical for improving the conservation of many threatened species, as they establish backup populations and provide individuals for reintroduction and reinforcement of wild populations. The Iberian lynx was considered the most threatened felid species in the world in the wake of a dramatic decline during the second half of the 20th century that reduced its numbers to around only 100 individuals. An ex situ conservation programme was established in 2003 with individuals from the two well-differentiated, remnant populations, with great success from a demographic point of view. Here we evaluate the genetic status of the Iberian lynx captive population based on molecular data from 36 microsatellites, including patterns of relatedness and representativeness of the two remnant genetic backgrounds among founders, the evolution of diversity and inbreeding over the years, and genetic differentiation among breeding facilities. In general terms, the ex situ population harbours most of the genetic variability found in the two wild populations and has been able to maintain reasonably low levels of inbreeding and high diversity, thus validating the applied management measures, and potentially representing a model for other species in need of conservation, Peer reviewed

Los detalles de la metodología y los resultados se pueden encontrar en: Domínguez-Castro, F., Vicente-Serrano, S.M., Tomás-Burguera, M., Peña-Gallardo M., Beguería S., El Kenawy A., Luna, Y., Morata, A. High-spatial-resolution probability maps of drought duration and magnitude across Spain. https://doi.org/10.5194/nhess-2018-289 Acceso mediante licencia: http://opendatacommons.org/licenses/odbl/1-0/, This dataset includes 1.1 km spatial resolution of the Generalized Pareto parameters (X0, alpha, Kappa) of drought duration and magnitude for SPI and SPEI at 1, 3, 6 and 12 months timescales and the maximum drought duration and magnitude risk maps for 50 and 100 years for SPI and SPEI at 1, 3, 6 and 12 months timescales. This dataset contains two zip files “parameters” and “risk_maps”. Parameters zip file contains 16 netCDF3 (8 for drought magnitude and 8 for drought duration) each one provides the Generalized Pareto parameters (1:X0, 2:alpha, 3:Kappa) for one index (SPI or SPEI) and one timescale (1, 3, 6 and 12 months). Risk_maps zip file contains 8 netCDF3 (4 for maximum drought magnitude and 4 for maximum drought duration) each one provides the risk maps for 4 time scales (1, 3, 6, 12 months) of one index (SPI or SPEI) and one time period (50 or 100 years). Each netCDF file contains 1115 longitudes and 834 latitudes., This work was supported by the following research projects: CGL2014-52135-C03-01 and PCIN-2015-220 financed by the Spanish Commission of Science and Technology and FEDER, 1560/2015; Herramientas de monitorización de la vegetación mediante modelización ecohidrológica en parques continentales financed by the Red de Parques Nacionales. IMDROFLOOD financed by Water Works 2014; a co-funded call of the European Commission and INDECIS, Peer reviewed

Supporting raw data for the article entitled "Real space manifestations of coherent screening in atomic scale Kondo lattices", to be accepted by Nature Communications, Financial support was provided by the Spanish Plan Nacional de I+D+i (grants MAT 2013-46593-C6-3-P, MAT2016-78293-C6-6-R, MAT2015-66888-C3-2-R and FIS2015-64886-C5-3-P), Charles University (programme PRIMUS/Sci/09) and the European Union through programmes Interreg-POCTEFA (Grant TNSI/EFA194/16) and H2020-EINFRA-5-2015 MaX Center of Excellence (Grant No. 676598). MML, MP and DS acknowledge the use of SAI at Universidad de Zaragoza. RR acknowledges The Severo Ochoa Centers of Excellence Program (Grant No. SEV-2017-0706) and Generalitat de Catalunya (Grant No. 2017SGR1506 and the CERCA Programme)., Peer reviewed

This dataset includes the information from thirty-six samples collected in August 2014 from 12 stations along a transect crossing the Gulf of Lions, from the coast off Gruissan to the eastern side of the Gulf of Fos (French coast, NW Mediterranean). It includes the density and biomass of all microbenthic organisms collected (identified to the lowest taxonomic level). It also includes the information on the main variables describing the environmental characteristics of the samples stations: Latitude, Longitude, Distance, Depth, Escherichia coli, Enterococci, Silt, Clay, Very fine sands, Fines sands, Medium sands, Pore water, Organic Matter, Organic Carbon, Hydrocarbons C10-C40, Nitrogen, Phosphorous, Aluminium total, Arsenium total, Cadmium total, Chrome total, Copper total, Iron total, Mercury total, Nickel total, Lead total, Zinc total, HAPs, total PCBs, Acénaphtylène, Fluoranthène , Benzo (b) fluoranthène , Benzo (k) fluoranthène, Benzo (a) pyrène , Benzo (ghi) pérylène, Indéno (1,2,3 cd) pyrène, Anthracène, Acénaphtène, Chrysène, Dibenzo (a,h) anthracène, Fluorène, Naphtalène, Pyrène, Phénanthrène, Benzo (a) anthracène, PCB 28, PCB 52, PCB 101, PCB 118, PCB 138, PCB 153, PCB 180, PCB totaux calculés, Monobutylétain, Dibutylétain, Tributylétain, Triphénylétain., This dataset includes the information from thirty-six samples collected in August 2014 from 12 stations along a transect crossing the Gulf of Lions, from the coast off Gruissan to the eastern side of the Gulf of Fos (French coast, NW Mediterranean), and refers to the density and biomass per square metre of the macrobenthos, as well as to all common descriptors of the sediments, including organic and inorganic contaminants, and the most relevant sea surface satellite vaiables., Peer reviewed

Peer reviewed

These data sets are associated with an article that is currently under review.-- Estos conjuntos de datos están asociados a un artículo que está actualmente en proceso de revisión, A new code for anisotropic traveltime tomography is presented. We describe the equations governing the anisotropic ray propagation algorithm and the modified inversion solver. This code can provide better understanding of the Earth's subsurface in the rather common geological contexts in which seismic velocity displays a weak dependency on the polar angle of ray propagation. We study the sensitivity of two medium parametrizations and compare four inversion strategies on a canonical model. The synthetic data sets for all these tests can be found in this repository directory, Project FRAME (Formation of geological domains in the Western Iberian Margin and tectonic reactivation of their limits), reference # CTM2015-71766-R, funded by the Spanish Ministry of Economy and Competitivity, Project SOUND (Seismic Modelling Using Natural Source Data) funded by Repsol, Table of contents • Inputs – All necessary input files. ◦ ani ◦ picks ◦ vel • Synthetic_Data – All synthetic data sets ◦ For_Sensitivity_and_Accuracy ▪ delta ▪ parallel_velocity ▪ epsilon ▪ parallel_velocity_finer ◦ For_Inversion_Tests • 3.1_Sensitivity – Sensitivity results ◦ 0.25pi_rad ◦ 0_rad • 3.2_Accuracy – Accuracy results ◦ 0.25pi_rad ◦ 0_rad ◦ overall_average • 3.3_Inversion_results – Inversion tests results ◦ Figure_5 ◦ Figure_6 ◦ Figure_7 ◦ Figure 8 • 3.4_Modeling_delta – Results for delta modeling tests ◦ Figure_9 ◦ Table_8-epsilon ◦ Table_9-epsilon ◦ Figure_10 ◦ Table_8-perpendicular_velocity ◦ Table_9-perpendicular_velocity • Supplementary – Files for supplementary figures ◦ FigS1 ◦ FigS2, Peer reviewed

Material suplementario (Figuras S1-S4 y Tablas S1-S4 del artículo Fernandez-Turiel, J.-L.; Perez-Torrado, F. J.; Rodriguez-Gonzalez, A.; Saavedra, J.; Carracedo, J. C., Rejas, M.; Lobo, A.; Osterrieth, M.; Carrizo, J. I.; Esteban, G.; Gallardo, J.; Ratto, N. (2019). The large eruption 4.2 ka cal BP in Cerro Blanco, Central Volcanic Zone, Andes: Insights to the Holocene eruptive deposits in the southern Puna and adjacent regions. Estudios Geológicos 75(1): e088. https://doi.org/10.3989/egeol.43438.515, This dataset compiles SEM images, modelled isopach map and topographic profiles, and data of radiocarbon ages, parameters of Tephra2 and AshCalc codes of Holocene volcanic ashes of of Southern Puna and neighbouring areas (NW Argentina). SEM images detail differences among the Bolsón de Fiambalá, Cerro Blanco and Cueros de Purulla fallout ash deposits. Tephra2 code was used to simulate the ash fallout, and the AshCalc code to compare different methods for ash volume estimates associated with the 4.2 ka cal BP eruption of the Cerro Blanco Volcanic Complex. Topographic profiles are used to explain the secondary thickening of fallout ash deposits., MINECO, CGL2011-23307, Proyecto QUECA, Peer reviewed

Sedimentation of particles in the ocean leads to inhomogeneous horizontal distributions at depth. The present dataset contains density and trajectory data for particle sedimentation computed from the velocity field given by a ROMS simulation at 1/12 x 1/12 degrees of horizontal resolution in the region of Benguela (south east Atlantic). Direct particle sampling as well as the result of a geometrical approach are included., Peer reviewed

Supplementary data file 1 “genomeplot_WT_hetR_-N_chromosome.pdf”. Overview (chromosome) combining log2-normalized expression values (left y axis) from the microarray analysis of cultures of wild type and hetR strain subjected to nitrogen deprivation for 0-6-12-24 hours as indicated by coloured lines, with the reads numbers from the RNA-Seq dataset in (Mitschke, J., Vioque, A., Haas, F., Hess, W.R., and Muro-Pastor, A.M. (2011). Dynamics of transcriptional start site selection during nitrogen stress-induced cell differentiation in Anabaena sp. PCC7120. Proc. Natl. Acad. Sci. USA 108, 20130-20135) (right y axis). Supplementary data file 2 “genomeplot_WT_hetR_-N_plasmids.pdf”. Overview (six plasmids combined) combining log2-normalized expression values (left y axis) from the microarray analysis of cultures of wild type and hetR strain subjected to nitrogen deprivation for 0-6-12-24 hours as indicated by coloured lines, with the reads numbers from the RNA-Seq dataset in (Mitschke, J., Vioque, A., Haas, F., Hess, W.R., and Muro-Pastor, A.M. (2011). Dynamics of transcriptional start site selection during nitrogen stress-induced cell differentiation in Anabaena sp. PCC7120. Proc. Natl. Acad. Sci. USA 108, 20130-20135) (right y axis). Supplementary data file 3 “genomeplot_WT_+N_-N_chromosome.pdf”. Overview (chromosome) combining log2-normalized expression values (left y axis) from the microarray analysis of cultures of wild type at 0 and 8 h after nitrogen depletion and at 0 and 8 h after NH4 addition as indicated by coloured lines, with the reads numbers from the RNA-Seq dataset in (Mitschke, J., Vioque, A., Haas, F., Hess, W.R., and Muro-Pastor, A.M. (2011). Dynamics of transcriptional start site selection during nitrogen stress-induced cell differentiation in Anabaena sp. PCC7120. Proc. Natl. Acad. Sci. USA 108, 20130-20135) (right y axis). Supplementary data file 4 “genomeplot_WT_+N_-N_plasmids.pdf”. Overview (six plasmids combined) combining log2-normalized expression values (left y axis) from the microarray analysis of cultures of wild type at 0 and 8 h after nitrogen depletion and at 0 and 8 h after NH4 addition as indicated by coloured lines, with the reads numbers from the RNA-Seq dataset in (Mitschke, J., Vioque, A., Haas, F., Hess, W.R., and Muro-Pastor, A.M. (2011). Dynamics of transcriptional start site selection during nitrogen stress-induced cell differentiation in Anabaena sp. PCC7120. Proc. Natl. Acad. Sci. USA 108, 20130-20135) (right y axis). Supplementary data file 5 “Co-expression network”. Cytoscape (www.cytoscape.org) file corresponding to the co-expression network constructed., Peer reviewed