Resultados de investigación

Supplementary data of the analysis "A single-tree approach to determine climate-growth patterns of European beech and their seasonality in the species southern distribution area"., Peer reviewed

This study tested the feasibility of using the Crustastun™ device to stun the American lobster (Homarus americanus) in order to: (i) Determine the effect of the stunning duration on the recovery and behaviour; (ii) Asses physiological disturbances caused by the stunning protocol and subsequent recovery; and, (iii) Evaluate any impact on meat quality following electrical stunning. This study demonstrated the reversibility of CrustastunTM stunning, distinguishing it from terminal dispatch method. Stress induced by electrical stunning was evidenced by the elevated L-lactate levels in the haemolymph, highlighting the use of this metabolite as an indicator of secondary stress response, This study was supported by a company that preferred to remain uncited and co-funded by the Spanish government though the “Severo Ochoa Center of Excellence” accreditation (CEX2019-000928-S), Each of the following are separate pages of the excel file: Animal information; Activity; Righting; Physiology; Meatquality, Peer reviewed

This research used samples and/or data provided by the Arctic Century Expedition, a joint initiative led by the Swiss Polar Institute (SPI), the Antarctic and Arctic Research Institute (AARI), and GEOMAR Helmholtz Centre for Ocean Research Kiel (GEOMAR), and funded by the Swiss Polar Foundation. GL and ZAK acknowledge that this project has been made possible by a grant from the Swiss Polar Institute, Dr Frederik Paulsen. GPF acknowledges funding from the Academy of Finland (Grant No. 342227). ZAK acknowledges this project has received funding from the Horizon Europe program under Grant Agreement No. 101137680 (Project CERTAINTY), With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), Peer reviewed

The data include parameters of climate reconstructions|paleoceanography with a geographic location of Mediterranean Sea, North Atlantic Ocean. The time period coverage is from 16065 to 131 in calendar years before present (BP). See metadata information for parameter and study location details, This research was funded by ERC-Consolidator grant TIMED (Contract Agreement 683237), TRANSMOW project (PID2019-105523RB-I00) and MORIA project (PID2022-138010OB-I00) from the Agencia Estatal de Investigación (Spain). Members of the research group of Marine Geosciences from the Universitat de Barcelona thank the Generalitat de Catalunya for the 2021 SGR 01195 grant and IC for the ICREA-Academia Award. We thank the Universitat de Barcelona (Facultat de Ciències de la Terra, Departament de Dinàmica de la Terra I de l'Oceà), and the Sapienza Università di Roma (Department of Earth Sciences), which supported the research with the Doctoral School “Vito Volterra” Grant. We are grateful for the ship time provided by IPEV on the Marion Dufresne within the EuroFLEETS GATEWAY project (Grant Agreement 228344), With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), Peer reviewed

Four OBS are provided in the input folder, and the parfile. Readme explains how to run the code with this sample data., The work has been supported by projects CONNECT with reference PID2021-128851OA-I00, ATLANTIS (PID2019-109559RB-I00) and THREAT (PID2021-128513OA-I00), funded by the Spanish Ministry of Science and Innovation. ICM has also had funding support of the–Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), of the Spanish Research Agency (AEI), Peer reviewed

1. Description of methods used for collection-generation of data: Grain size fraction (gravel, sand, silt, clay) was determined using a particle-size analyzer. Pb-210 was determined with alpha spectrometry. Metals were analyzed with an Inductively Coupled Plasma Mass Spectrometer. Total mercury was determined by atomic absorption spectrophotometric detection. 4. Instruments, calibration and standards information: Particle-size analyzer: Horiba Partica LA-950v2. Alpha spectrometry: Passivated Implanted Planar Silicon (PIPS) detectors (CANBERRA, Mod. PD-450.18 A.M). Inductively Coupled Plasma Mass Spectrometer: Agilent, 7900 model. Atomic absorption spectrophotometry: AMA-254. Standards for metals: Reference materials NIST 2702, IAEA 457 and MESS-3. 7. Quality-assurance procedures performed on the data: Standard measurements, The dataset Metals_Alorda-Montiel.csv includes data regarding sediment cores collected in the Mar Menor coastal lagoon. Each row corresponds to a sediment section id, which follows this structure: Corename depthmin - depthmax. Example: OPC1 0-1, which applies to the section from 0 to 1 cm from the core OPC1. The variables are Depth (in cm, and accounting for the medium depth of each section), Pb_210 (Pb-210 specific activity, in Bq/kg), Error_Pb_210 (Pb-210 specific activity error, in Bq/kg), Na (g/kg), Al (g/kg), Si (g/kg), P (mg/kg), S (g/kg), K (g/kg), Ca (g/kg), Ti (mg/kg), Cr (mg/kg), Fe (g/kg), Ni (mg/kg), Cu (mg/kg), Zn (mg/kg), As (mg/kg), Sr (mg/kg), Ag (mg/kg), Cd (mg/kg), Pb (mg/kg), Hg (mg/kg), Gravel (%), Sand (%), Silt (%) and Clay (%). The purpose of this dataset is to show the data used in the article "A Century of Sediment Metal Contamination of Mar Menor, Europe's Largest Saltwater Lagoon". (2024-12-03), This work was funded by the Agencia Estatal de Investigación (AEI) of the Spanish Ministry of Science and Innovation through the OPAL project (PID2019-110311RB-C21) and the WINDERS project (TED2021-130710B-I00). This work contributes to the María de Maeztu Programme (CEX2019-000940-M) for Units of Excellence of the Spanish Ministry of Science and Innovation. I.A-M acknowledges financial support from FPI grant PRE2020-092343. A.A-O acknowledges support from MCIN/AEI RYC2021-034455-I. J. R-P acknowledges financial support from FPU grant FPU20/01369. I. A-M, V. R., A. A-O., J. R-P. and J. G-O. belong to the consolidated group Marine and Environmental Biogeosciences Research Group - MERS, funded by grant 2021-SGR 00640 from the Direcció General de Recerca. A.P. belongs to the consolidated research group on littoral and oceanic processes, funded by grant 2021SGR 00433 from Generalitat de Catalunya. C. G-R thanks the sabbatical fellowship awarded by PASPA-DGAPA from Universidad Nacional Autónoma de México. M. D-F acknowledges financial support from grant JDC2022-050316-I funded by MCIN/AEI/10.13039/501100011033 and by the European Union - NextGenerationEU/PRTR, and support from the Grup d'Hidrologia Subterrània - GHS (Universitat Politècnica de Catalunya) funded by grant 2021-SGR 00609 from Generalitat de Catalunya. This work is contributing to the ICM 'Center of Excellence' Severo Ochoa (grant CEX2024-001494-S funded by Spanish Agency of Investigation grant AEI 10.13039/501100011033). This work is also part of the THINKINAZUL programme supported by the Spanish Ministry of Science and Innovation with funding from European Union NextGenerationEU (PRTR-C17.I1) and by Fundación Séneca with funding from Comunidad Autónoma Región de Murcia (CARM) (Spain). A. G. B. acknowledges funding from MerTerMar (PID2019-III722RJ-I00), Peer reviewed

Supplementary material for "Complex architecture of mud volcano systems: new insights on flow pathways unravel intricate fluid circulation" https://doi.org/10.1130/B37954.1, Shuhui Xu is supported by the China Scholarship Council (CSC), and Walter Menapace is supported by the H2020 MSCA-IF-TURBOMUD project (grant 101018321). This research was funded in part by the Austrian Science Fund (FWF; grant M 3146-417 N) and projects CTM2015-70155-R (INSIGHT) and PID2020-114856RB-100 (ICEFLAME) funded by the Spanish Ministry of Science and Innovation (MCIN/ AEI/10.13039/501100011033). The European project EUMarineRobots (EUMR) is acknowledged for cofunding the M167 expedition (grant 731103), With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), Peer reviewed

[Data description:] Excel file with variables used in model selection to analyse the reaction and breeding success probabilities of Bonelli’s Eagles. All variables are described in the document., Fieldwork for the long-term breeding monitoring was self-financed throughout the study period by J.E. Martínez., Peer reviewed

Climate change is impacting ecosystems worldwide, and the Mediterranean Sea is no exception. Extreme climatic events, such as marine heat waves (MHWs), are increasing in frequency, extent, and intensity during the last decades, which has been associated with an increase in mass mortality events for multiple species. Coralligenous assemblages, where the octocoral Paramuricea clavata lives, are strongly affected by MHWs. The Medes Islands Marine Reserve (NW Mediterranean) was considered a climate refugia for P. clavata, as their populations were showing some resilience to these changing conditions. In this study, we assessed the impacts of the MHWs that occurred between 2016 and 2022 in seven shallow populations of the octocoral P. clavata from a Mediterranean Marine Protected Area. The years that the mortality rates increased significantly were associated with the ones with strong MHWs, 2022 being the one with higher mortalities. In 2022, with 50 MHW days, the proportion of total affected colonies was almost 70%, with a proportion of the injured surface of almost 40%, reaching levels never attained in our study site since the monitoring was started. We also found spatial variability between the monitored populations. Whereas few of them showed low levels of mortality, others lost around 75% of their biomass. The significant impacts documented here raise concerns about the future of shallow P. clavata populations across the Mediterranean, suggesting that the resilience of this species may not be maintained to sustain these populations face the ongoing warming trends, This work was supported by the long-term monitoring programme of the marine natural parks of Catalonia, funded by Departament de Territori i Sostenibilitat of the Generalitat de Catalunya public agreements PTOP2017-130 and PTOP-2021-3. This work was also financially supported by Heatmed project RTI2018-095346-BI00 funded by Agencia Española de Investigación AEI MICIU/AEI/10.13039/501100011033 and ‘ERDF A way of making Europe’, and Corfun project TED2021-131622B-I00 funded by MICIU/AEI/10.13039/501100011033 and ‘European Union NextGenerationEU/PRT’. C.L acknowledges the support by Catalan Institution for Research and Advanced Studies ICREA. All authors are part of the Marine Conservation research group funded by Generalitat de Catalunya [2021 SGR 01073], Peer reviewed

With funding form the Spanish government through the "Severa Ochoa Centre of Excellence" accreditation (CEX2019-000928-S), This work was supported by the long-term monitoring program of the marine natural parks of Catalonia, funded by Departament de Territori i Sostenibilitat of the Generalitat de Catalunya public agreements PTOP2017-130 and PTOP-2021-3. This work was also financially supported by Heatmed project RTI2018-095346-BI00 funded by MICIU/AEI/10.13039/501100011033 and ‘ERDF A way of making Europe’, and Corfun project TED2021-131622B-I00 funded by MICIU/AEI/10.13039/501100011033 and ‘European Union NextGenerationEU/PRT’. P.C. was supported by the European Union-Next Generation EU Maria Zambrano Program (ZAMBRANO 21-26). C.L. acknowledges the support by ICREA Academia. All authors are part of the Marine Conservation research group [2021 SGR 01073], Peer reviewed