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MMC S1. Additional STM images relevant for this article are included in the Supplementary material., Peer reviewed

Supplementary List of References (cited in Table I)., Peer reviewed

Supplementary Information Fig. 1: Activity/depth profiles for 210Pb excess (blue diamonds) and 214Pb (orange squares) as a proxy for 210Pb supported activity for the upper and lower salt marshes studied.-- Supplementary Information Table 1. Mean (SE) of isotopic nitrogen and carbon values (‰) of salt marsh plant species and surficial sediments (2cm depth) collected at the eleven study sites. N indicates the number of samples analysed; it is indicated also when different sample numbers were analysed for Nitrogen (N) and Carbon (C). NM means no material found in the sampling units.-- Supplementary Information Table 2. Mean, quantiles (50, 2.5 and 97.5%) and SD of proportions of each carbon source for the surficial sediments (2cm depth) of each sampling site and according to plant species dominant of the salt marsh. POM is particulate organic matter. Asterisk (*) indicates the major median source contribution value when differentiate from the other sources. The quantiles 2.5 and 97.5% are Bayesian credible intervals. Dash (-) indicates organic matter source or dominant plant species no present in the site.-- Supplementary Information Table 3. Carbon and nitrogen isotopic signatures of organic matter allochthonous sources from the literature. POM: particulate organic matter.-- Supplementary Information Table 4. Summary of potential links between dependent and predictive variables incorporated in the SEM analysis and the rationale behind the potential link. Links predicted as positive are indicated with a blue dot, negative with red and neutral with black. OC: organic carbon, OM: organic matter, DOC: dissolved organic carbon, SAR: sediment accretion rate, C:N: carbon and nitrogen ratio. Interpretations for mean grain size are based on the So (sorting coefficient, with larger numbers for larger grains).-- Supplementary References., Peer reviewed

Organic carbon stocks, salt marsh plant biomass, crab burrow abundances and diameters. This data was generated by sampling at 11 salt marsh sites along 3000 km of coastal line in southern SW Atlantic coast in South America. Organic carbon stocks and burial rates extarcted from other publications and used to update global estimates are also included with their respective references. Values of biotic and abiotic drivers included in the Structural Equation Model (SEM) to evaluate their roles in belowground organic carbon stocks., Peer reviewed

Supplemental material includes a detailed information of the DFT calculations, a list of Stevens operators and the second quantization expression of the basis states, together with the derivation of the rate equation., Peer reviewed

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