Resultados de investigación

This article presents a 60 years wave hindcast from 1958 to 2017, covering the Colombian Caribbean basin. Each output consists on 6-hour field of significant wave height , mean wave period , and mean direction with a resolution of 11.8 11.4 . The simulation was performed using SWAN model forced with JRA-55 wind fields. Model data is validated against NOAA buoy 42058 located in the central Caribbean. The resolution and time spam of this database allows to perform either coastal engineering projects as well as to perform research in seasonal and interannual wave climate variability including large return periods to evaluate coastal vulnerability., AOR is supported by COLCIENCIAS (Departamento Administrativo de Ciencia, Tecnología e Innovación) through a PhD grant from “Convocatoria 727” and from a POGO fellowship at the Mediterranean Institute for Advanced Studies. Authors acknowledge financial support from the Spanish Government MICINN/FEDER through MOCCA Project (RTI2018-093941-B-C31)., Peer reviewed

Data acquisition: Satellite: ESA SMOS mission (Soil Moisture and Ocean Salinity). Filenames: BEC_CDM___SMOS__DAN_L4____YYYYMMDDT120000_0.05d_1d_EXP_v1.0.nc Documents: EO4SIBS_D6.8_D6.9, BEC ftp service: We serve netCDF data by means of a secure ftp server. NetCDF files from which the maps were made (and other additional data) can be downloaded from sftp address becftp.icm.csic.es at port 27500. If your browser is sftp compatible you can browse directly from sftp://becftp.icm.csic.es:27500 address. In order to download data you should be registered in our BEC ftp service. Registration is free, you can register just by filling the following form: https://bec.icm.csic.es/data-access-ftp/ If you need a dedicated ftp client (for instance FileZilla https://filezilla-project.org/) you should use the following configuration: Host: sftp://becftp.icm.csic.es username: your username password: your password Port: 27500, An Earth Observation Data Exploitation Platform for Science and Innovation in the Black Sea (EO4SIBS)'. To develop a new generation of algorithms that can ingest the wealth of spatial, temporal and spectral information provided by recent sensors providing high quality reference products for the blue and green ocean. Content: EO4SIBS experimental SMOS Colored Detrital Matter (CDM) L4 for the Danube mouth. Time coverage: 01 January, 2019 – 31 May, 2019; 01 December, 2019 – 31 December, 2019. Time resolution: Daily. Maps frequency generation: Daily. Spatial coverage: Latitude range: 44ºN-45.5ºN Longitude range: 28ºE-30.5ºE. Spatial resolution: 0.05 degrees. Spatial grid: WGS 84 / Regular longitude-latitude. YYYYMMDD: Day of the map. Sensor: Satellite SMOS / MIRAS. Format: NetCDF. Climate and Forecast (CF) conventions version: 1.6., European Space Agency under contract 4000127237/19/I-EF, With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), Peer reviewed

Gravity data on the Central Pyrenees: a step forward to help a better understanding of the Pyrenean structures http://hdl.handle.net/10261/256413, This database corresponds to the new Bouguer and residual Bouguer anomaly gravity data of the Central Pyrenees calculated from 3588 stations, of which 1140 are new observations acquired from surveys performed between 2018 and 2019. The processing, calculations and interpretations can be found in Gravity data on the Central Pyrenees: a step forward to help a better understanding of the Pyrenean structures (Ayala et al., 2020, DOI … ). Please note that there is a difference of one data from this database respect the number that appears on the paper. This is due to the identification of a duplicated point after the publication of the paper. The duplicated point has been deleted from this database., This database is part of the project CGL2017-84901-C2-2-P funded by MCIN/AEI/10.13039/501100011033 and "ERDF A way of making Europe", Peer reviewed

25 pages, 10 figures, 7 tables.-- This work is distributed under the Creative Commons Attribution 4.0 License, The Global Ocean Data Analysis Project (GLODAP) is a synthesis effort providing regular compilations of surface-to-bottom ocean biogeochemical bottle data, with an emphasis on seawater inorganic carbon chemistry and related variables determined through chemical analysis of seawater samples. GLODAPv2.2021 is an update of the previous version, GLODAPv2.2020 (Olsen et al., 2020). The major changes are as follows: data from 43 new cruises were added, data coverage was extended until 2020, all data with missing temperatures were removed, and a digital object identifier (DOI) was included for each cruise in the product files. In addition, a number of minor corrections to GLODAPv2.2020 data were performed. GLODAPv2.2021 includes measurements from more than 1.3 million water samples from the global oceans collected on 989 cruises. The data for the 12 GLODAP core variables (salinity, oxygen, nitrate, silicate, phosphate, dissolved inorganic carbon, total alkalinity, pH, CFC-11, CFC-12, CFC-113, and CCl4) have undergone extensive quality control with a focus on systematic evaluation of bias. The data are available in two formats: (i) as submitted by the data originator but updated to World Ocean Circulation Experiment (WOCE) exchange format and (ii) as a merged data product with adjustments applied to minimize bias. For this annual update, adjustments for the 43 new cruises were derived by comparing those data with the data from the 946 quality controlled cruises in the GLODAPv2.2020 data product using crossover analysis. Comparisons to estimates of nutrients and ocean CO2 chemistry based on empirical algorithms provided additional context for adjustment decisions in this version. The adjustments are intended to remove potential biases from errors related to measurement, calibration, and data handling practices without removing known or likely time trends or variations in the variables evaluated. The compiled and adjusted data product is believed to be consistent with to better than 0.005 in salinity, 1% in oxygen, 2% in nitrate, 2% in silicate, 2% in phosphate, 4 μmolkg-1 in dissolved inorganic carbon, 4 μmolkg-1 in total alkalinity, 0.01–0.02 in pH (depending on region), and 5% in the halogenated transient tracers. The other variables included in the compilation, such as isotopic tracers and discrete CO2 fugacity (fCO2), were not subjected to bias comparison or adjustments., The original data, their documentation, and DOI codes are available at the Ocean Carbon Data System of NOAA NCEI (https://www.ncei.noaa.gov/access/ocean-carbon-data-system/oceans/GLODAPv2_2021/, last access: 7 July 2021). This site also provides access to the merged data product, which is provided as a single global file and as four regional ones – the Arctic, Atlantic, Indian, and Pacific oceans – under https://doi.org/10.25921/ttgq-n825 (Lauvset et al., 2021). These bias-adjusted product files also include significant ancillary and approximated data and can be accessed via https://www.glodap.info (last access: 29 June 2021). These were obtained by interpolation of, or calculation from, measured data. This living data update documents the GLODAPv2.2021 methods and provides a broad overview of the secondary quality control procedures and results, This research has been supported by EU Horizon 2020 through the EuroSea action (grant no. 862626), internal strategic funding from NORCE Climate, Prociencia/UERJ (grant 2019–2021), IEO RADIALES and RADPROF projects, the UK Climate Linked Atlantic Sector Science (CLASS) NERC National Capability Long-term Single Centre Science Programme(grant no. NE/R015953/1), the BOCATS2 (PID2019-104279GBC21) project funded by MCIN/AEI/10.13039/501100011033 and contributing toWATER:iOS CSIC PTI, the NOAA Global Observations and Monitoring Division (fund reference 100007298), the Office of Oceanic and Atmospheric Research of NOAA Global Observations and Monitoring Division (fund reference 100007298), the Office of Oceanic and Atmospheric Research of NOAA, the BONUS INTEGRAL project (grant no. 03F0773A), the Australian Antarctic Program Partnership and the Integrated Marine Observing System, EU Horizon 2020 action SO-CHIC (grant no. 821001), and the Initiative and Networking Fund of the Helmholtz Association through the project “Digital Earth” (grant no. ZT-0025), Peer reviewed

[EN] This Excel file contains the raw data of the experiment reported in the article “Responses of Barley to High Ambient Temperature Are Modulated by Vernalization”, published in Frontiers in Plant Science, and referenced as Supplementary Table 7. Data are phenological development variables and yield-related variables for eight genotypes of barley grown in growth chambers, under four treatments combining presence/absence of vernalization and normal/high temperatures == [ES] Archivo excel con los datos de un experimento incluido en la publicación Ochagavía et al., en Frontiers in Plant Science. La primera hoja contiene la explicación de los datos, recogidos en la segunda hoja del archivo., Raw data (Supplementary Table 7) of article by Ochagavía et al., published in Frontiers in Plant Science., Funding of this research was provided was provided by project AGL2016-80967-R (Agencia Estatal de Investigación, Ministry of Economy and Competitiveness), project PID2019- 111621RB-I00 (Agencia Estatal de Investigación), grants A08_17R and A08_20R (Government of Aragón), and project GINOP-2.3.2-15-2016-00029 (Economic Development Programs of the Hungarian Ministry of Finance)., 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