BUSCADOR RECOLECTA

1 file, The Cape Verde Frontal Zone (CVFZ) is a highly dynamic region located in the southern boundary of the Canary Current Eastern Boundary Upwelling Ecosystem. Due to the interaction of the Cape Verde Front with the Mauritanian coastal upwelling, the area features large vertical and horizontal export fluxes of organic matter. Full-depth profiles were recorded during FLUXES I cruise, with four consecutive transects defining a box embracing the giant filament of Cape Blanc and the Cape Verde front. Fifteen levels were sampled in medium and long stations (down to 4000 dbar) and 10 levels in short stations (down to 2000 dbar) where inorganic nutrients (NO3, NO2, Si(OH)4 and PO4), dissolved organic carbon/total dissolved nitrogen (DOC/TDN), and suspended particulate organic carbon and nitrogen (POC and PON) were sampled. Micromolar concentrations of nutrient salts were determined simultaneously by segmented flow analysis in an Alliance Futura autoanalyser. The determination of suspended POC and PON was carried out by high temperature catalytic oxidation at 900 °C in a Perkin Elmer 2400 elemental analyser. DOC and TDN were analysed by high temperature catalytic oxidation at 680 °C with a Shimadzu TOC-V analyser connected in line with a TNM1 measuring unit. Alongside with water samples conductivity, temperature and depth (CTD; SeaBird SBE911 plus), and dissolved oxygen (SeaBird SBE43), fluorescence of chlorophyll (SeaPoint SCF), and turbidity (SeaPoint STM) were measured. CTD conductivity was calibrated with water samples taken from the rosette and analysed on board with a Guildline 8410-A Portasal salinometer. Samples for dissolved oxygen (O2) determination were analysed on board by the Winkler potentiometric method. The chlorophyll (Chl) fluorescence sensor was calibrated with water samples taken at 4 depths in the photic layer which were estimated fluorometrically by means of a Turner Designs bench fluorometer 10-AU, Horizon 2020 (H2020), grant/award no. 817806: Sustainable management of mesopelagic resources; Ministerio de Ciencia e Innovación (MICINN), grant/award no. CTM2015-69392-C3: Constraining organic carbon fluxes in an eastern boundary upwelling ecosystem (NW Africa): the role of non-sinking carbon in the context of the biological pump; Ministerio de Ciencia e Innovación (MICINN), grant/award no. PID2019-109084RB-C21: Biogeochemical impact of mesoscale and sub-mesoscale processes along the life history of cyclonic and anticyclonic eddies: plankton variability and productivity, Peer reviewed

7 files, Knowledge of the three-dimensional movement patterns of elasmobranchs is vital to understanding their ecological roles and exposure to anthropogenic pressures. To date, comparative studies among species at global scales have mostly focused on horizontal movements. Our study addresses the knowledge gap of vertical movements by compiling the first global synthesis of vertical habitat use by elasmobranchs from data obtained by deployment of 989 biotelemetry tags on 38 elasmobranch species. Elasmobranchs displayed high intra- and interspecific variability in vertical movement patterns. Significant vertical overlap was observed for many epipelagic elasmobranchs, indicating an increased likelihood to display spatial overlap, biologically interact, and share similar risk to anthropogenic threats that vary on a vertical gradient. We highlight the critical next steps towards incorporating vertical movement into global management and monitoring strategies for elasmobranchs, emphasising the need to address geographic and taxonomic biases in deployments and to concurrently consider both horizontal and vertical movements, Peer reviewed

The Aneto Glacier, is the largest glacier in the Pyrenees. Its shrinkage and wastage have been continuous in recent decades, and there are signs of accelerated melting in recent years. In this study, changes in the surface and ice thickness of the Aneto Glacier from 1981 to 2022 are investigated using historical aerial imagery, airborne LiDAR point clouds, and UAV imagery. A GPR survey conducted in 2020, combined with data from photogrammetric analyses, allowed us to reconstruct the current ice thickness and also the existing ice distribution in 1981 and 2011. Over the last 41 years, the total glaciated area has shrunk by 64.7% and the ice thickness has decreased, on average, by 30.5 m. The mean remaining ice thickness in autumn 2022 was 11.9 m, as against the mean thicknesses of 32.9 m, 19.2 m reconstructed for 1981 and 2011 and 15.0 m observed in 2020 respectively. The results demonstrate the critical situation of the glacier, with an imminent segmentation into two smaller ice bodies and no evidence of an accumulation zone. We also found that the occurrence of an extremely hot and dry year, as observed in the 2021–2022 season, leads to a drastic degradation of the glacier, posing a high risk to the persistence of the Aneto Glacier, a situation that could extend to the rest of the Pyrenean glaciers in a relatively short time., Peer reviewed

5 files.-- The CETUS dataset contains effort-based occurrence records collected during a cetacean monitoring programme in the Eastern North Atlantic, since 2012, The CETUS dataset contains data collected within the CETUS Project (www.cetusproject.com), a cetacean monitoring programme in the Eastern North Atlantic, running since 2012. The project is led by the Interdisciplinary Centre of Marine and Environmental Research (CIIMAR - University of Porto, Portugal), in partnership with TRANSINSULAR - Grupo ETE, a Portuguese company for maritime transport, that offers its cargo ships to be used as a platforms of opportunity to monitor cetaceans along routes between Continental Portugal and Madeira, Azores, Canary and Cape Verde islands. On-board trained marine mammal observers collect data on: survey effort, cetacean and other megafauna occurrences, as well as marine traffic and meteorological conditions. Data is provided in the recent OBIS-ENV-DATA format, and comprises 8913 georeferenced positions associated with 3195 occurrences of 44 marine taxa, This research was partially funded by the EU FEDER/FEMP and Portuguese Foundation for Science and Technology (FCT) under the Portugal2020 (Lisboa2020, Algarve2020 and MAR2020) Programme through project OBSERVA.PT (MAR-01.04.02-FEAMP-0002), Peer reviewed

2 tables, 2 figures, Supporting information for the article https://doi.org/10.3390/su14116472, Table S1 – Relative abundance of molecular species of fatty acids (expressed as % of total pool of fatty acids) of Hermetia illucens larvae fed with different substrates retrieved from the literature surveyed.-- Table S2: Dataset used on MetaboAnalist to perform the statistical analysis.-- Table S3 - Top 10 peer-reviewed scientific journals publishing scientific research addressing the fatty acid profile of Hermetia illucens retrieved from WoS™ and Scopus. (Journals publishing 5 or less articles on this topic were grouped as Others).-- Figure S1: Box plots and kernel density plots before and after normalization. The boxplots show at most 50 features due to space limitations. The density plots are based on all samples. Data transformation: Log Normalization; Data scaling: Autoscaling.-- Figure S2: Hierarchical clustering of substrates shown as dendrogram (distance measures using Euclidean, and clustering algorithm using Ward’s Distance).-- References, Peer reviewed

1 figure, 3 tables, Supporting information for the article https://doi.org/10.1016/j.wasman.2022.01.035, Figure S1 - Box plots and kernel density plots before and after normalization. The density plots are based on all samples. Data transformation: Log Normalization; Data scaling: Autoscaling.-- Table S1 – Amino acids content from substrates of the five study groups: control group (a), 25% replacement (b), 50% replacement (c), 75% replacement (d) and 100% replacement (e)) of expired fish feed. (g/100 g total amino acids). OHPro: hydroxyproline. Errors are the confidence intervals for n=2 (replicates of analysis) and α =0.05.-- Table S2 – Amino acids content of Black Soldier Fly larvae (g/100 g total amino acids). Errors are the confidence intervals for n=2 (replicates of analysis) and α=0.05.-- Table S3 - Fatty acid composition from substrates lipid extracts of the five study groups: control group (a), 25% replacement (b), 50% replacement (c), 75% replacement (d) and 100% replacement (e) of expired fish feed. Abundances are expressed in relative abundance (%) and values are means of five samples (n = 5) ± standard deviation, Peer reviewed

This dataset was used to analyze survival probabilities of adult Audouin’s gull depending on early conditions (density-dependence and Winter NAO) experienced by the individuals., Capture mark recapture data of Audouin gulls breeding from 1995 until 2009 in Mediterranean locations including Ebro Delta, Chafarinas Islands, Columbretes Islands and Mallorca islets in the Balearic Islands. Individuals are shown in rows and years in columns followed by the cohort on which they were born, and the environmental covariates associated to that year. This data set has been used for the publication: Payo-Payo, A.; Sanz-Aguilar, A. and Oro, D. (2022) Long-lasting effects of harsh early-life conditions on adult survival of a long-lived vertebrate. OIKOS., We acknowledge financial support through projects RESET (CGL2017-85210-P), IBISES (ref. CGL2013-42203-R) and MINOW (ref. H2020- 634495)., This work was funded through projects RESET (CGL2017-85210-P) and IBISES (ref. CGL2013-42203-R). APP was supported by a predoctoral fellowship of the Ministry of Education (FPU-AP 2012-0869). ASA is supported by a postdoctoral contract co-funded by the Regional Government of the Balearic Islands and the European Social Fund (ref. PD/003/2016) and a Ramón y Cajal fellowship ( Ref. RYC-2017- 22796)., The data file contains resight histories of Audouin’s gulls born at Ebro Delta and observed during breeding seasons 1995 to 2009. This file contains one line per individual; one column per encounter occasion (from column 1 to 15 were code 1 indicate resight at Ebro Delta colony and code 2 resight at other colony); one line indicating the number of individual capture histories (column 16); and three further columns indicating the standardized values of early life individual covariates (columns 17, 18, and 19; for DD, WNAO, and DD*WNAO, respectively)., No

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

SCAN-1997 Cruise (29HE19970114) carried out on the Research Vessel Hespérides in 1997, Geodynamics and Paleoceanography of continental margins and basins: northern Antarctic Peninsula. (SCAN´ 97). Objectives of the SCAN 97 campaign: 1) Complete the study of the Powell Basin. 2) In the northwestern Wedell Sea, the mechanisms of continental fragmentation and backarc basin development models have been studied. The structure, seismic stratigraphy and evolution have been investigated, with the objective of studying the Cenozoic subduction along the Jane backarc and Jane arc. 3) The border between the Antarctic / Scotia plates has been studied in order to establish the current and Cenozoic dynamics between this larger plate limit in the South Atlantic

MAYC-97_ORINOCO Cruise (29HE19970225) carried out on the Research Vessel Hespérides in 1997, Continental margin and deep basins: sedimentary record of paleoenvironmental and paleoclimatic variability paleoenvironmental and paleoclimatic variability. The research focuses on the study of the submarine fans of the Orinoco (area of ​​Venezuela) and the Magdalena (area of ​​Colombia) and will address the study of the recent sedimentary record (less than 5 million years) from the most shallow environments of the continental margin (300 meters deep) to the deepest environments such as the ocean basins to more than 5000 meters deep