BUSCADOR RECOLECTA

Contents: 1 SI 1: Microgel characterization: temperature-dependent size, electrophoretic mobility 2 SI 2: Estimation of the self-propulsion velocity of colloidal clusters A Microgel characterization via dielectric spectroscopy B Theoretical estimation of EHDFs and dumbbell velocity 3 SI 3: Temperature control with plasmonic heating: Experiments and FEM simulations A Illumination and light absorption characterization B FEM modeling 4 SI 4: 3D-printed trap design for sequential capillarity-assisted particle assembly of microgels 5 SI 5: Yield of the sCAPA of R-G-PS trimers 6 SI 6: Estimation of the swimming velocity for R-G-PS trimers with different opening angles 7 SI 7: Determination of the chirality, rotational diffusion, and angular velocity of the active clusters 8 SI 8: Dynamical parameters of the experimental microswimmers 9 SI 9: Switching of chirality between states 10 SI 10: Calculation of microgel overlap on R-G-PS trimers 11 SI 11: Ensemble MSDs for chiral and non-chiral clusters 12 Suppporting Movies 13 References, Suppporting Movies: Movie S1: Movie of the active motion of a 120-cluster under an AC field (800Hz, 7V Vpp) recorded at 10 fps and sped up three times for visualization. The particle trajectory is color-coded by the temperature, as described in the main text. Only the PS particle is visible in the bright-field images. Movie S2: Movie of the active motion of a 60-cluster under an AC field (800Hz, 7V Vpp) recorded at 10 fps and sped up three times for visualization. The particle trajectory is color-coded by the temperature, as described in the main text. Only the PS particle is visible in the bright-field images. Movie S3: Movie of the active motion of a 180-cluster under an AC field (800Hz, 7V Vpp) recorded at 10 fps and sped up three times for visualization. The particle trajectory is color-coded by the temperature, as described in the main text. Only the PS particle is visible in the bright-field images., Peer reviewed

Experimental details of the SEC/MALLS measurements; SAXS/SANS characterization of the PMMA/dPMMA crowders; analysis of the SANS data in terms of the generalized Gaussian coil; and details on background subtraction., Peer reviewed

[Construction] This raster was constructed from the freely available database (PVGIS © European Communities, 2001-2008) providing, in particular, monthly averages of the daily minimum temperature reconstructed over a grid with 1$\times$1km spatial resolution (Huld et al., 2006). These monthly averages correspond to the period 1995-2003 and were used by Abboud et al. (2019, 2020) to model Xylella fastidious dynamics in South Corsica. Load the raster in the R statistical software (v4.1.2): library(raster) ADMT=raster("average-daily-minimum-temperature_Corsica_Abboud-et-al_Forecasting.grd") print(ADMT) plot(ADMT) Summary information: class : RasterLayer dimensions : 108, 78, 8424 (nrow, ncol, ncell) resolution : 0.016667, 0.016667 (x, y) extent : 8.400708, 9.700734, 41.30018, 43.10021 (xmin, xmax, ymin, ymax) crs : +proj=longlat +datum=WGS84 +no_defs source : average-daily-minimum-temperature_Corsica_Abboud-et-al_Forecasting.grd names : layer values : -0.6748945, 6.75789 (min, max) References: - Abboud, C., Bonnefon, O., Parent, E., and Soubeyrand, S. (2019). Dating and localizing an invasion from post-introduction data and a coupled reaction–diffusion–absorption model. Journal of Mathematical Biology 79, 765–789. - Abboud, C., Parent, E., Bonnefon, O., and Soubeyrand, S. (2022). Forecasting pathogen dynamics with Bayesian model-averaging: Application to Xylella fastidiosa. Preprint. - Huld, T. A., Suri, M., Dunlop, E. D., and Micale, F. (2006). Estimating average daytime and daily temperature profiles within Europe. Environmental Modelling & Software 21, 1650–1661., Beyond Xylella, Integrated Management Strategies for Mitigating Xylella fastidiosa Impact in Europe (BeXyl) (Grant Agreement 101060593). Partner/Coordinador principal: Blanca B. Landa del Castillo, Investigadora Científica del Instituto de Agricultura Sostenible (IAS-CSIC)., Raster providing the average of the daily minimum temperature in Celsius degrees over January and February in Corsica from 1995 to 2003 with a 0.016667x0.0166671 resolution in latitude and longitude., Peer reviewed

The GEOVIDE cruise was carried out coast to coast between Portugal and Newfoundland via the south tip of Greenland, following the OVIDE line in the eastern part and crossing the Labrador Sea in the western part. The classical hydrographic rosette was cast 163 times at 78 different geographical positions called stations. While the CTD-O2 probe acquired continuous profiles of the “physical” variables (pressure, temperature, salinity and dissolved oxygen), 22 Niskin bottles were closed at different levels during the upcast to provide samples for biogeochemical analysis. After calibration, we find precisions for pressure, temperature, salinity and dissolved oxygen that fit the GO-SHIP international quality requirements. In parallel, but not simultaneously, a trace-metal rosette (TMR) was cast 53 times, also acquiring profiles of physical variables, and equipped with 24 Go-Flo bottles adapted for the sampling of trace metals. Depending on the number of operations, stations were identified as “Short” (one single CTD cast), “Large” (3 CTD casts), “XLarge” (up to 6) and “Super” (up to 11). All along the track of the ship, current magnitude and direction was measured by Ship Acoustic Doppler Current Profilers, down to 1000m depth. This dataset reports for the water mass proportions (from 0 to 1, i.e., from 0 to 100%) for the classical rosette for the following water masses: East North Atlantic Central Water of 16ºC (ENACW16) and of 12 ºC (ENACW12); Subpolar Mode Water of 8ºC (SPMW8), of 7ºC (SPMW7) and of the Irminger Sea (IrSPMW); Labrador Sea Water (LSW); Subarctic Intermediate Water of 6ºC (SAIW6) and of 4ºC (SAIW4); Mediterranean Water (MW); Iceland–Scotland Overflow Water (ISOW); Denmark Strait Overflow Water (DSOW); Polar Intermediate Water (PIW); and North-East Atlantic Deep Water lower (NEADWL). The dataset also contains the changes in oxygen due to the remineralisation of organic matter (DO2bio; in µmol kg-1)., No

Characterization data of a Pisum sp. germplams colection grown at Córdoba, Spain under three crop seasons, PROYECTO P20_00986 PAIDI2020 Junta Andalucía., Peer reviewed

Characterization data of a Vicia faba germplams collection grown at Córdoba, Spain at three sites during 2022 and 2023., PROYECTO P20_00986 PAIDI2020 Junta Andalucía., Peer reviewed

Characterization data of a Vicia sativa germplams colection grown at Córdoba, Spain under three crop seasons., PROYECTO P20_00986 PAIDI2020 Junta Andalucía., Peer reviewed

9 figures, 6 tables.-- S.3.1. Linear sweep voltammetry: The LSV experiments were performed at a scan rate of 50 mV·s-1 in oxygen-saturated 0.1 M KOH. The scan in the nitrogen-saturated electrolyte is also presented. Apart from the 5 electrodes with the CNT inks, a reference catalyst Pt/C (60%) was tested. S.4. Specific capacitance: We calculated the double-layer capacitance (DLC) from CV at scan rates ranging from 0 to 150 mV·s-1 on a GC electrode of 4 mm diameter and 0.06 μF·cm-2 specific capacitance. The capacitive current was determined as the difference between the cathodic and anodic current at a given potential. Capacitive currents were plotted vs. the scan rate (Figure 4.b) and the calculated slope was divided by 2 to obtain the electrode capacitance. Next, the specific capacitance was calculated dividing the electrode capacitance by the real specific surface area from AFM (Table S.6). The area of vertical nano-crevices is not considered because of the cantilever tip size, resulting in an underestimated surface. Nonetheless, the use of AFM to obtain the specific capacitance has been recommended in the case of low RF surfaces [13].-- S.5. Stability tests: The stability of the carbon-based catalysts was assessed on the GC electrode by CV. Up to 1,600 cycles were performed in the O2 saturated electrolyte without rotating the electrode. Two control measurements, before and after the series in static, were performed with a rotation speed of 1,600 rpm.-- Under a Creative Commons license CC-BY 4.0, S.1. Experimental details S.2. Characterization of the carbon materials S.2.1. Raman spectroscopy and sheet resistivity S.2.2. X-ray photoelectron spectroscopy (XPS) S.2.3. AFM measurements S.3. The full set of LSV curves in the RRDE S.3.1. Linear sweep voltammetry S.3.2. Koutecky-Levich (KL) analysis S.4. Specific capacitance S.5. Stability tests, Peer reviewed

Creating a century-long homogenized near-surface wind speed (WS) observation dataset is essential to improve our knowledge about the uncertainty and causes of WS stilling and recovery. We rescued paper-based WS records dating back to the 1920s at 13 stations in Sweden and established a four-step homogenization procedure to generate the first 10-member centennial homogenized WS dataset (HomogWS-se) for community uses among climatology, ecology, hydrology and energy industry. HomogWS-se can be used to study the WS variability and change, assess climate reanalysis, and constrain climate simulations for better future projection of changes in the WS and wind energy potential. HomogWS-se contains 13 individual text files with 10-member century-long homogenized monthly WS series, as well as the member-mean series., Peer reviewed

S1 Fig. Artifacts recovered in the courtyard. A: three Punic ointment jars made of vitreous paste. B: four bowls of Macedonian origin. C: a fragment of a sculpture carved in Pentelic marble. D: five sheep astargali bones (4 from the left foot and 1 from the right), with the lateral and medial facets modified by abrasion. a) plantar side. b) dorsal side. c) lateral and medial facets. S2 Fig. Physical trauma to the jaw and teeth caused by metal bits to the horses. A: wear to the upper and lower PM2 of EQ9, B: EQ1 bit, C: bone spurs on the diastema of female EQ20. S3 Fig. Vertebral body abnormalities to the horses. A: thoracic vertebrae of EQ45, T13-T18, lateral view, osteophytes affecting the anterior and posterior joints of the ventral area. B: thoracic vertebrae of SE quadrant, T5-T6, lateral view, osteophytes affecting the ventral area and intertransverse space. C: thoracic vertebrae of the SE quadrant, T15-T16, lateral view, vertebral ankylose osteophytosis. S4 Fig. Calibrated ranges for the Turuñuelo 14C dates on samples EQ35 and BO30 of Phase 1, EQ13 and EQ17 of Phase 2 and BO56 of Phase 3. S5 Fig. Schematic profile indicative of the accumulations of bones and sediments (Phases 1–3) in the courtyard. The view is from the eastern entrance of the courtyard toward the monumental western staircase. SP: slate paving. S6 Fig. View of the maxilla of EQ16 of Phase 1 bearing traces of a fresh blow to the right maxillary sinus possibly indicative of slaughter. S7 Fig. Thermoalteration of the bones of EQ2 during Phase 1. The bones of this equid reveal signs of dehydration, cracking and color change along the superficial cortical zone of the radius (A), talus (C) and calcaneus (D). The color changes affected the peripheral cementum of the labial surface of the maxillary dentition (B upper). The lingual surface (B lower) is less affected, probably due to protection offered by soft tissue such as the tongue. The predominance of reddish-brown, reddish-yellow and at times dark brown according to the Munsell chart suggest the bones were exposed to temperatures between 225 and 350º C. S8 Fig. Bone dislocations and displacements of Phase 1. 1. EQ 7: A) incisor bone, B) left maxilla with molars M1-2-3, C) occipital bone, D) axis displacement. 2 EQ35 atlas dislocation, 3–4 EQ35 femur and pelvis dislocation. S9 Fig. Bones of Phases 1 and 2 bearing traces of weathering. A) right hemimandible of EQ17 (Phase 2) revealing flaking and a fibrous texture on its exposed lateral surface (1) but no traces of weathering on its medial surface (2). B) Right tibia of BO55 (Phase 1) revealing flaking of its surface, especially on its exposed medial side (1), as opposed to its caudal surface (2). C) Right metacarpal (Phase 1, SE quadrant) revealing cracking of the cortex due to sun exposure on its exposed distal surface (1) but no traces on its plantar side (2). S1 Appendix. Microstratigraphic analyses of the courtyard. Archaeological sediments. S1 Table. A) Anatomical representation and B) Withers height stimations., Peer reviewed