Resultados de investigación

Gridded monthly climate projection dataset underpinning the IPCC AR6 Interactive Atlas for the impact-relevant variables and indices., The IPCC WG1 Interactive Atlas is an online tool that provides interactive visualizations and geospatial data related to the physical scientific basis of climate change. This platform allows users to explore and visualize geographical information interactively and dynamically. It presents data using maps, charts, and other visualizations, enabling users to understand complex information spatially and temporally. The interactive Atlas includes climate data for relevant variables, key climate indicators, and trends, all derived from climate model simulations., The IPCC-WGI AR6 Interactive Atlas dataset comprises monthly gridded data from global (CMIP5, CMIP6) and regional (CORDEX) model projections for the impact-relevant variables and indices featured in the IPCC Interactive Atlas (https://interactive-atlas.ipcc.ch)., Peer reviewed, 2

Contents: Repo Contents. -- System Requirements. -- Installation Guide. -- Demo. -- License. -- Issues. -- Citation, Peer reviewed

Los datos pertenecen al trabajo Ginsbach, Laura F.; González Grau, Juan Miguel: of Understanding life at high temperatures. Relationships of molecular channels in enzymes of methanogenic Archaea and their growth temperatures, Figure 4. Amplitude and average of the molecular tunnel dimensions, length (A, D, G), surface (B, E, H) and volume (C, F, I) (in Å), predicted for the methyl-CoM reductase (Mmr) gene subunits, alpha (A, B, C), beta (D, E, F) and gamma (G, H, I) from methanogenic Archaea classified in three classes of optimum growth temperature (<50ºC; 50-80ºC; >80ºC). Grey bars correspond to the amplitude of data observed for estimates of the molecular tunnel dimensions. Red squares represent the average dimensions for each Figure 5. Amplitude and average of the molecular tunnel dimensions, length (A, D, G), surface (B, E, H) and volume (C, F, I) (in Å), predicted for the heterodisulfide reductas (Hdr) gene subunits, A (A, B, C), B (D, E, F) and C (G, H, I) from methanogenic Archaea classified in three classes of optimum growth temperature (<50ºC; 50-80ºC; >80ºC). Grey bars correspond to the amplitude of data observed for estimates of the molecular tunnel dimensions. Red squares represent the average dimensions for each growth temperature class. Error bars for the average values represent a standard deviation., This is funding from the Ministry of Science and Innovation, project EQC2019-005634-P (cofunded by FEDER) and PID2020-119373GB-I00., Peer reviewed

20 páginas, con dos fotografías y un gráfico. El artículo dio a conocer documentación inédita sobre las primeras décadas de administración española en lo que es hoy Bolivia, conservada en el Archivo Histórico Municipal de Cochabamba., [EN] This paper is the first result of a long-term research project aimed at reconstructing the system of land tenure and food procurement in the valley of Cochabamba, Bolivia, under Inca rule; this valley was one of the main sources of agricultural production in the Incan empire, as it would be in the viceroyalty of Peru following the discovery of the Potosí silver mines in 1545. The first objective of the project was to locate Canata, the administrative center in the valley and its vicinity before and after the Spanish conquest up to the founding of the town of Oropesa (present-day city of Cochabamba) in 1571. The location of Canata had been a subject of much debate among Bolivianists since the 19th century. Our research involved analyzing lawsuit files prior to 1571 that are kept in the city council archives as well as doing archaeological surface surveys of the possible areas where material remains of Canata could be found. The result was the identification of the site in Tupuraya, a north-east suburb of the present-day city of Cochabamba, where pre-Inca as well as Inca remains have been found and where colonial-period structures can still be seen. In addition, the analysis of the archival documents shed light on the circumstances of the founding of Oropesa in 1571., [ES] Este trabajo es el primer fruto de un proyecto a largo plazo de reconstrucción del sistema de tenencia de la tierra y los modos de aprovechamiento económico del valle de Cochabamba (Bolivia) bajo el imperio inca. El valle de Cochabamba fue uno de los principales graneros de este imperio, como lo sería del virreinato español tras el descubrimiento de las minas de Potosí en 1545. El primer objetivo del proyecto era ubicar la localidad de Canata, que fue el centro administrativo del valle y su entorno antes y después de la conquista española, hasta la fundación de la villa de Oropesa (actual ciudad de Cochabamba) en 1571. El emplazamiento de Canata había sido un tema muy discutido entre los historiadores bolivianos desde el siglo XIX. Nuestro trabajo consistió en analizar los expedientes sobre litigios de tierras anteriores a 1571 guardados en el Archivo Histórico Municipal de Cochabamba y hacer una prospección arqueológica de superficie de las posibles zonas del valle donde Canata pudo haber estado ubicada. El resultado fue una identificación del emplazamiento de la localidad en un lugar llamado hoy Tupuraya, al noreste de la ciudad Cochabamba, donde se han hallado restos incas y pre-incas y todavía existen viviendas de la época colonial. Los documentos analizados también arrojan nueva luz sobre las circunstancias de la fundación de Oropesa en 1571., Archivo Histórico Municipal de Cochabamba (Bolivia), Peer reviewed

Abstract: A detailed biostratigraphy is established, using the high foraminiferal abundance and diversity at Trowbarrow Quarry, which is also proposed as a stratotype section for the late Asbian (late Viséan), a substage not previously formally subdivided. The foraminiferal assemblages suggest that the early Asbian has to be revised, which has implications for the chronostratigraphy of many late Viséan outcrops in Britain, which are probably erroneously interpreted. From the upper part of the Park Limestone Formation at Trowbarrow Quarry, near the base of the section, the transition between foraminifers assigned to the early and late Asbian (Cf6α-β to Cf6γ subzones) is identified. The Urswick Limestone Formation contains excellent biostratigraphic records of many important taxa, allowing the subdivision of the formation into five foraminiferal assemblage zones for the late Asbian, namely Cf6γ1a, Cf6γ1b, Cf6γ2a, Cf6γ2b and Cf6γ2c. The last assemblage is currently only recognised in the North Pennines and at Trowbarrow. These assemblages allow revision of the stratigraphic range of many taxa used as biostratigraphic markers in Britain and Ireland. Owing to its excellent foraminiferal record, the late Asbian subdivisions will significantly facilitate the reinterpretation of other well-known Asbian platform carbonate successions in Britain. Although with some faunal differences, the base of the late Asbian can be confidently correlated to other European zonal schemes, with its base equivalent to the base of the former V3bγ or more recent MFZ14 foraminiferal zones of Belgium, and the base of the Mikhailovian Substage in Russia., Peer reviewed

The present document develops the laboratory protocols to analyse plastic pollution in freshwater environmental samples, although the methods followed can be extrapolated to other ecosystems. These protocols are developed in the framework of the PLASTICØPYR project, which aims to tackle plastic pollution associated with mountain tourism activities by developing transversal actions involving several stakeholders. These guidelines are developed in order to quantify plastic pollution in different river habitats, from large items (macro- and mesoplastics) to tiny plastic particles (microplastics). The protocols are developed for the analysis of microplastics (MicP) up to 63 µm, from samples from the water column, the fluvial sediments, the fluvial biota (i.e., brown trout and biofilm), as well as plastic particles present in the atmosphere (either wet or dry deposition). The MicP analysis is done following the Nile Red method, a fluorescent dye that facilitates the observation of small particles. Although Nile Red cannot provide chemical characterisation, it can be compatible with MicP identification techniques, such as FTIR (Fourier-transform infrared spectroscopy). The samples procedure includes: the extraction of MicP from the inorganic matrix by density separation (using ZnCl2), a digestion step with hydrogen peroxide and catalysed with Fenton's reagent to eliminate the organic remains and finally, the staining of the sample with Nile Red., Peer reviewed

Fundación General CSIC (Programa ComFuturo); TURBOMIX project (CGL2015-73100-EXP). With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), • lat: latitude • lon: longitude • x, x coordinate • y: y coordinate • time: time • sst: Sea Surface Temperature • hsst: Singularity exponents of Sea Surface Temperature, Peer reviewed

The table lists all the DNA sequences (COI mit) studied to date, of specimens belonging to the Rhyacophila fasciata Group and published in different articles. Due to the progressive increase of sequences obtained in successive publications, they have been compiled in this table for consultation by researchers interested in this material. The document will be updated with new sequences as the following studies are published., The table includes the following information: species and specimen number, sex, locality of collection, latitudinal and longitudinal geographical coordinates, altitude, accession numbers to GenBank, voucher number from Tissues and DNA Collection, voucher number of Entomological Collection, both from Museo Nacional de Ciencias Naturales, Consejo Superior de Investigaciones Científicas (MNCN-CSIC), accession number and/or collection in other Collections, and legit (Leg.) of specimens., No

It is a contribution of the Marine Zooplankton Ecology Group (2017 SGR 87), Proper thermal adaptation is key to understanding how species respond to temperature. However, this is seldom considered in protozooplankton and mixoplankton experiments. In this work, we studied how two heterotrophic dinoflagellates (Gyrodinium dominans and Oxyrrhis marina), one heterotrophic ciliate (Strombidium arenicola), and one mixotrophic dinoflagellate (Karlodinium armiger) responded to warming, comparing strains adapted at 16, 19 and 22 °C and those adapted at 16 °C and exposed for 3 days at 19 and 22 °C (acclimated treatments). Neither CNP contents nor the corresponding elemental ratios showed straightforward changes with temperature, except for a modest increase in P contents with temperature in some grazers. In general, the performance of both acclimated and adapted grazers increased from 16 to 19 °C and then dropped at 22 °C, with a few exceptions. Therefore, our organisms followed the “hotter is better” hypothesis from 16 to 19 °C; above 19 °C, however, the results were variable. Despite the disparity in the responses between species and physiological rates, in general, it seems that 19 °C-adapted organisms performed better than acclimated-only organisms. However, at 22 °C, most species were at the limit of their metabolisms and were unable to fully adapt. Nevertheless, adaptation to higher temperatures conferred some advantages prior to sudden increases in temperature (up to 25 °C) that simulated a heatwave episode. In summary, adaptation to temperature seems to confer a selective advantage to protistan grazers within a narrow range (i.e., ca. 3 °C). Adaptation to much higher temperatures (i.e., 6 °C) does not confer any clear physiological advantage (with few exceptions; e.g., the mixotroph K. armiger), at least within the time frame of our experiments, This research was funded by Grant CTM2017-84288-R by Fondo Europeo de Desarrollo Regional (FEDER)/ Ministerio de Ciencia, Innovación y Universidades—Agencia Estatal de Investigación (AEI), and by Grant PID2020-118645RB-I00 by Ministerio de Ciencia e innovación (MCIN)/AEI/ 10.13039/501100011033 and by “ERDF A way of making Europe”. With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), Para 4 especies: Volumen (µm3/depredador), Tasa crecimiento (µ 1/d), Tasa de ingestion (cells/ind/d), Eficiencia bruta de crecimiento (GGE, %), Peer reviewed

Datos incluidos: Anexo 1. Selección bibliográfica Anexo 2. Selección bibliográfica / Extractos Anexo 3. Selección artículos publicaciones periódicas Anexo 4. Selección fuentes documentales Anexo 5. Índice temático Anexo 6. Fuentes documentales esenciales, El productor y distribuidor de cine, y gran aficionado a la historia, Javier de Garcillán, descubrió de manera fortuita, en un estudio sobre el geógrafo Alexander Dalrymple, la expedición capitaneada por Pedro Fernández de Quirós en 1605. Esta expedición, cuyo mando acabaría en manos del piloto de la segunda nave, Luis Báez de Torres, tras el abandono de Quirós y su regreso a Acapulco, conduciría al descubrimiento del estrecho en 1606, que posteriormente, tomaría el nombre del piloto, Estrecho de Torres. La extrañeza y sorpresa que produjo en Garcillán la intranscendencia de este hecho, junto a la casi ausencia de estudios de la historiografía española sobre esta “hazaña marinera”, estimularon la curiosidad del distribuidor. En torno a 1998, comenzó un trabajo de recopilación de fuentes que le llevó a visitar desde los grandes archivos, bibliotecas y librerías de nuestro país hasta los más importantes del continente australiano, pasando por todos aquellos de cualquier país (Italia, Estados Unidos, Gran Bretaña…) en los que pudiera “descubrir” nuevos documentos que arrojaran luz sobre este hecho histórico y que facilitaran el “acceso” al laberinto. Su objetivo “la publicación de un libro de gran formato y divulgación en una editorial comercial que sirviera de base a la elaboración y distribución de una película documental” quedó desgraciadamente cercenado con la muerte de Javier de Garcillán en el año 2007. En 2013, este extenso fondo documental llegó al CCHS - CSIC de la mano de la investigadora Ana Rodríguez y la productora López Li Films. En él hemos “buceado” con el objeto de destacar aquellas fuentes que “iluminen” el proceso del descubrimiento, “Esta investigación ha recibido financiada por el Ministerio de Economía y Competitividad (MINECO). Ref.: HAR2011-15924-E”, Peer reviewed