Journal of Food Composition and Analysis 110 (2022) 104559 Contents lists available at ScienceDirect Journal of Food Composition and Analysis journal homepage: www.elsevier.com/locate/jfca Application of ED-XRF spectra for determination of macroelements in edible seaweeds Jelena Milinovic a, b, *, Filipe M.J. Figueiredo b, João Paulo Noronha a, José Sardinha b, c a LAQV/REQUIMTE, Department of Chemistry, NOVA School of Science and Technology, NOVA University Lisbon, 2829-516 Caparica, Portugal Centro de Recursos Naturais e Ambiente (CERENA), Instituto Superior Técnico, Universidade de Lisboa, Av. Rovisco Pais 1, 1049-001 Lisbon, Portugal c Departamento de Engenharia e Ciências Nucleares (DECN), Instituto Superior Técnico, Universidade de Lisboa, Campus Tecnológico e Nuclear, Estrada Nacional 10, 2695-066 Bobadela, Portugal b A R T I C L E I N F O A B S T R A C T Keywords: Edible seaweeds Macroelements Overlapping peaks ED-XRF spectra vs. ICP-OES Multivariate regression CVPLS NIPALS algorithm RMSE Method robustness The application of an increased number of edible seaweeds in gastronomy requires accurate, rapid, and nondestructive mineral evaluation. In this work, energy dispersive X-ray fluorescence (ED-XRF) spectra were used to determine Ca, K, and P in edible green, red, and brown seaweeds from the Portuguese coasts. ED-XRF raw spectra of seaweed samples were correlated against results of conventional inductively coupled plasma-optical emission spectrometry (ICP-OES), by the full cross-validation partial least-square (CVPLS) regression method, with nonlinear iterative partial least squares (NIPALS) algorithm. The standard reference material (Thallus laminariae) was used for the validation of CVPLS. Statistical parameters, correlation coefficients (R2), root mean square errors (RMSE), and bias, were used for the assessment of the CVPLS method. For selected minerals, R2 was high (0.88–0.95), while RMSE values (< 1.02) and bias (0) were low, thus indicating a viable potential for their routine analysis by ED-XRF. These findings highlighted the quality of ED-XRF spectral data, which can be used for an efficient non-destructive determination of macroelements in edible seaweeds on a large food industrial scale. 1. Introduction Edible seaweeds (marine algae) have been used as a food source for centuries (Chapman and Chapman, 1980; McHugh, 2003). Due to their valuable nutrition composition, currently, around 85% of the global seaweed industry is used as food products for direct human consumption (MacArtain et al., 2007; FAO, 2018). Among other nutrients, such as carbohydrates, fibers, etc., green, red, and brown seaweeds contain a large fraction of minerals, that can be present from 10% to 50% (w/w, referred to dry weight, dw) (Jensen, 1993). Sodium and potassium chlorides are dominant minerals, whereas more valuable Ca and P are present in lower contents in most of the seaweed species (Paiva et al., 2014; Rodrigues et al., 2015; Fleurence, 2016; Milinovic et al., 2021a). Based on their mineral composition, seaweeds can be selectively used to improve the quality of different food products. Thus, the biomass of some seaweeds or seaweed-derived products (e.g., Himanthalia elongata, Porphyra umbilicalis, Undaria pinnatifida) have been added to improve mineral profiles in some snacks, meat products, and/or drinks (López-López et al., 2010; Gupta and Abu-Ghannam, 2011; Gullón et al., 2020). Therefore, it is essential to know the exact levels of minerals in seaweeds, for their successful application in the development of func­ tional foods. The analysis of macroelements in food matrices usually implies timeconsuming wet digestion sample pretreatments before analysis by con­ ventional techniques, such as atomic absorption spectrometry (AAS) or inductively coupled plasma-optical emission spectroscopy (ICP-OES) (Varma et al., 2011; Malea et al., 2015; Rubio et al., 2017). Direct analysis of macroelements with minimal sample preparation is an alternative that would overcome the time-consuming limitation of sample preparation before conventional analysis. In this regard, energy dispersive X-ray fluorescence (ED-XRF) analysis can be used for the rapid cost-effective analysis of elements. This robust technique is rapid, non-destructive, and with minimized contamination risk and waste generation (Bosco, 2013). A small amount of sample enables fast * Corresponding author at: LAQV/REQUIMTE, Department of Chemistry, NOVA School of Science and Technology, NOVA University Lisbon, 2829-516 Caparica, Portugal. E-mail addresses: j.milinovic@fct.unl.pt (J. Milinovic), filipe.figueiredo@tecnico.ulisboa.pt (F.M.J. Figueiredo), jpnoronha@fct.unl.pt (J.P. Noronha), jose. sardinha@tecnico.ulisboa.pt (J. Sardinha). https://doi.org/10.1016/j.jfca.2022.104559 Received 31 December 2021; Received in revised form 26 March 2022; Accepted 30 March 2022 Available online 2 April 2022 0889-1575/© 2022 Elsevier Inc. All rights reserved. J. Milinovic et al. Journal of Food Composition and Analysis 110 (2022) 104559 Fig. 1. Location of seaweed samples collected along the central western Portuguese coasts, Cape Mondego and Óbidos Lagoon. high sample output, and the capability of simultaneous multi-element analysis (McComb et al., 2014). Although XRF has been used for the rapid multi-element food anal­ ysis, e.g., in vegetal foodstuffs (Gallardo et al., 2016) or infant milk powder (Herreros-Chavez et al., 2019), it has not been sufficiently addressed and studied in the direct elemental analysis of seaweeds (Bull et al., 2016; Brito et al., 2017; Turner et al., 2017). Rapid ED-XRF analysis of Ca, K, and Mg in seaweeds collected in Brazil, was cali­ brated by linear regression using ICP-OES results (Brito et al., 2017). For the accuracy of ED-XRF analysis, certified reference materials (CRMs) of plant origin were used and the recoveries ranged from 85% to 89% (for Ca) to 127–129% (for K). The accuracy of these results, calculated by the software algorithm, was affected by overlapping peaks of Ca and K (Bosco, 2013; Brito et al., 2017). This type of interference is the main disadvantage of ED-XRF analysis, caused by the phenomena of absorp­ tion of the emission signal by the other elements present in the matrix. To avoid these interferences and to improve the accuracy of results, mathematical corrections using different chemometrics tools, including multivariate regression analysis, can be applied to spectra. As a form of predictive modeling technique, the partial least square (PLS) regression with a developed algorithm can be run on ED-XRF spectra, which may serve for the determination of elements (Engelen et al., 2004; Nengsih et al., 2019). The objective of this research was to apply ED-XRF spectra for the determination of Ca, K, and P concentrations in edible seaweeds. In this context, integral ED-XRF spectral data were correlated with the inde­ pendently acquired (ICP-OES) data by PLS regression. To the best of our knowledge, these data are scarce in the literature and hence, do not provide a basis for comparison. Table 1 Seaweed species collected at the central western Portuguese coast. Seaweed species Traditional name Sampling season Sampling site Chlorophytae (green) Codium tomentosum Spongeweed autumn, 2019 Ulva rigida Sea lettuce autumn, 2019 Ulva sp Sea lettuce autumn, 2019 Rhodophytae (red) Gracilaria gracilis Cape Mondego Cape Mondego Óbidos Lagoon Slender wart weed spring, 2019 Osmundea pinnatifida Pepper Dulse spring, 2019 Porphyra sp Nori, Laver summer, 2019 Phaeophyceae (brown) Saccorhiza polyschides Furbelows summer, 2019 Undaria pinnatifida Wakame summer, 2019 Cape Mondego Cape Mondego Cape Mondego Cape Mondego Cape Mondego Table 2 Concentrations of Ca, K, and P (%, w/w, dw) in edible seaweeds determined by ICP-OES. Seaweed phylum Species Chlorophyta (green) Codium tomentosum Ulva rigida Ulva sp Rhodophyta (red) Gracilaria gracilis Osmundea pinnatifida Porphyra sp Phaeophyceae (brown) Saccorhiza polyschides Undaria pinnatifida Ca % (w/w, dw) K P 0.94 0.69 3.06 5.88 2.02 1.52 0.29 0.25 0.46 0.17 0.55 0.20 10.60 5.31 2.90 0.29 0.28 0.60 1.40 0.97 8.46 7.64 0.32 0.68 2. Materials and methods All chemical reagents were of analytical grade, purchased from commercial suppliers, and used as received. The certified standard stock solutions of macroelements were purchased from Merck Inorganic Ventures. Working solutions were prepared by diluting the stock solu­ tion with ultrapure Milli-Q water (18 MΩ cm− 1). Dry brown seaweed species Thallus laminariae (kelp) used as the standard reference material (SRM 3232), was purchased from the National Institute of Standards & Technology (NIST, Gaithersburg, MD, USA). acquisition of the ED-XRF spectrum, which describes the patterns of elements present, according to characteristic energies emitted by X-rays. The X-ray energies for each element are specific and increase with the atomic number of elements. The main advantages of ED-XRF analysis are high accuracy and precision, sensitivity (sub-ppm levels to %, w/w), 2.1. Seaweed samples Seaweeds were collected from the central western Portuguese coasts - Cape Mondego (40º11′ N, 08º54′ W), and the Óbidos lagoon (39º25′ N, 2 J. Milinovic et al. Journal of Food Composition and Analysis 110 (2022) 104559 Fig. 2. ED-XRF spectrum of SRM 3232. Peaks corresponding to P, K, and Ca are labelled. 09º13′ W) (Fig. 1). In total, eight seaweed species were sampled, of which three green (Codium tomentosum, Ulva rigida, Ulva sp), three red (Gracilaria gracilis, Osmundea pinnatifida, Porphyra sp), and two brown (Saccorhiza poly­ schides, Undaria pinnatifida) (Table 1). All species were collected in 2019, from spring (red species Gracilaira gracilis and Osmundea pinnatifida) to early autumn (green species), following the best ecological practices and favor weather conditions (Milinovic et al., 2020; Milinovic et al., 2021b). During sampling in spring and late summer/early autumn seasons, the physico-chemical parameters of seawater did not change significantly, i.e., the tempera­ ture was 16 ◦ C, pH 7.6 and 8.0, and salinity 31–35 ng L− 1 and 34–36 ng L− 1, respectively (Milinovic et al., 2021b, 2021c). Seaweed species were chosen based on their abundance at the sam­ pling sites, i.e., available in sufficient biomass to perform further ana­ lyses. Seaweeds were collected at the fully developed adult phase and their identification was performed using the morphological character­ istics and by systematical comparison with the MACOI Portuguese database (Pereira, 2009, 2012). Collected seaweed samples were washed with filtered seawater and their transportation was performed by rapid shipment to the laboratory facilities. All samples were washed thoroughly with distilled water to further remove salt, sand grains, and epiphytes, and then freeze-dried (CoolSafe 9 L, LaboGene™, Denmark) under conditions explained elsewhere (Milinovic et al., 2020). Freeze-dried samples were crushed and milled with a blender, and the grains were sifted through the lab­ oratory stainless steel sieve (R 20 cm, 120 mesh, 0.125 mm aperture). Representative samples of the fine fraction were kept in labeled poly­ propylene bags, sealed with a vacuum sealer, and stored in the freezer (at − 18 ◦ C) before analysis. HNO3 (v/v, 1:10) to avoid matrix interferences due to salinity. The digestion method and operational conditions of the analysis, as well as quality control, have been explained in detail elsewhere (Milinovic et al., 2021a, 2021b, 2021c). The determined concentrations of target elements expressed in % (w/w) refers to dry weight (dw) of seaweeds. The NIST certified values for the concentrations of Ca, K, and P in SRM 3232, were determined also by ICP-OES analysis, consistent with the Joint Committee for Guides in Metrology (JCGM, 2008; Yu et al., 2018; NIST, 2019). The SRM 3232, contains Ca, K, and P in respective concentrations: 1.23 ± 0.01%, 7.6 ± 0.1%, and 0.46 ± 0.01% (w/w, referred to dw). 2.3. ED-XRF spectral analysis of seaweed samples A portable ED-XRF analyzer (S1 Titan series 600, Bruker, Illinois, USA) equipped with an Rh X-ray source, was used for the elemental analysis of homogenized fine fraction seaweed samples. A representative portion of the sample (thickness = 10–15 mm) was placed in a poly­ ethylene cup (using Mylar film as sample support), positioned centrally above the detector window (active surface of 20 mm2) of the ED-XRF analyzer. The GeoMining calibration mode was selected for the anal­ ysis of macroelements via three-phase measurements, each 30 s. The voltage and current excitations used in the three phases were respec­ tively: 30 kV and 23.20 µA, 50 kV and 25.30 µA, and 15 kV and 22.35 µA. Spectra in the third phase of measurement (run at the lowest potential and energy), enable the analysis of the light elements, including Ca, K, and P. The K lines were used since they were the only ones observed for P and K, while for Ca the L line could be detected but was characterized by very low energy (0.34 keV). The raw spectral data were computed by Bruker’s Instrument Tools (v. 1.6.0.110). To obtain quantitative data, integral spectra were exported by Bruker Artax software (v. 8.0.0.476). 2.2. ICP-OES analysis of macroelements in seaweeds 2.4. ED-XRF spectra vs. ICP-OES: application of multivariate regression analysis Seaweed samples were analyzed for total Ca, K, and P concentrations by inductively coupled plasma-optical emission spectroscopy (ICP-OES, Horiba Jobin Yvon Activa M). Briefly, approximately 200 mg of the homogenized lyophilized samples were placed in a Teflon vessel, with added 2 mL of 2% HNO3. The solution in the closed vessel was heated in a microwave (CEM Mars 5) according to the following program: within the first 10 min, the temperature has been increased to 180 ◦ C and remained for the next 10 min. After cooling, 0.5 mL of 30% H2O2 was added to the solution, following a new digestion cycle, as previously described. Then, the sample was evaporated to 0.5 mL and Milli-Q water was added to the final volume of 25 mL. All samples were diluted in 2% The X-ray energy raw spectral data along with ICP-OES results were exported to Unscrambler™ to perform multivariate regression analysis. The multivariate modeling was based on full cross-validation partial least square (CVPLS) regression, applied to dependent (ED-XRF spectral data) and independent (ICP-OES results) datasets (Martens and Dard­ enne, 1998). The nonlinear iterative partial least squares (NIPALS) al­ gorithm was selected for CVPLS with Hotelling’s T2 outlier estimation at a 95% level of confidence (p < 0.05). The NIPALS algorithm was 3 J. Milinovic et al. Journal of Food Composition and Analysis 110 (2022) 104559 Fig. 3. ED-XRF spectra of edible seaweeds: A - green spp.; B - red spp.; C - brown spp. selected as the preferentially used algorithm that enables the model to be fitted on smaller datasets (Stott et al., 2017; Nengsih et al., 2019). The seven ED-XRF measurements of the SRM 3232 and each seaweed sample were used for the full cross-validation PLS. Given the small size of the available dataset, each replicate analysis (of the SRM 3232 and eight seaweed samples) was considered individually (n = 63). The crossvalidation used is a well-established model implemented in the Unscrambler™ program, based on a systematic resampling of the available data (Martens and Dardenne, 1998). This version of full model cross-validation differs from local component cross-validation, which only cross-validates each component locally, and doesn’t attempt to estimate the ‘true’ prediction error both for the calibration and valida­ tion sets. In the model input, the maximum number of components used was 7, thus assuring a more reliable CVPLS analysis. The number of 4 J. Milinovic et al. Journal of Food Composition and Analysis 110 (2022) 104559 Fig. 4. Original plots of CVPLS model for predicted Ca content (%) in seaweed samples by ED-XRF vs. ICP-OES results. Seven latent variables (factor - 7) were used to maximize the covariance between the predicted and independent dataset. The inserted squares contain statistical parameters of calibration (blue) and validation (red) which quantitatively explain the goodness of the model. Slope and offset (intercept) define the linear relationship between two variables of the regression line. High values of correlation, Pearson (R2), and correlation coefficient (R-square), together with low values of RMSE, SE, and bias describe a strong prediction of Ca. latent variables (LV) was computed but was not used as a critical parameter for the fitness of the method, since it has less influence (Martins et al., 2010). The statistical parameters used to explain the goodness of fit of the quantitative multivariate PLS analysis were: cor­ relation coefficient (R2), root mean square error (RMSE), and bias for both calibration and validation datasets. The robustness of the method was estimated by deliberate variations after removing some datasets (seaweed sample Ulva sp) and checking the parameters of the goodness of fit and occurrence of possible outliers in the results, at a significant level (p < 0.05). respectively. The concentration of P in all samples was present at the same order of magnitude as Ca, in a narrow range, from 0.25% (Ulva rigida) to 0.68% (Undaria pinnatifida). Ca and P concentrations were positively correlated (R2 = 0.90), after the exclusion of Porphyra sp. and Saccorhiza polyschides, which confirms the adequate ratio of both mac­ ronutrients (Ca/P > 1) in the analyzed seaweeds. In a proper human diet, a portion of about 1.0 g (dw) per day of seaweed (e.g., Codium tomentosum, Undaria pinnatifida) will provide an optimal intake of both macronutrients, vital for bone health and reduced risk of osteoporosis (Lee and Cho, 2015). Similar results were reported for the same edible species of seaweeds collected at different coastlines worldwide (Rupérez, 2002; Domínguez-Gonzalez et al., 2005; Flores et al., 2015; Rubio et al., 2017). Nutritional aspects of the results and the importance of selected species in gastronomy were discussed in detail elsewhere (Milinovic et al., 2021a). Concentrations of Ca, K, and P in the standard reference material seaweed Kelp powder (SRM 3232) - were in the same range as in the studied seaweed samples, which assured quality control purposes by the selected SRM (Yu et al., 2018; Linsinger and Botha, 2019). In some other works, the reference materials used were based on plant leaves (apple, 3. Results and discussion 3.1. ICP-OES concentrations of macroelements in seaweeds Concentrations of Ca, K, and P determined by ICP-OES analysis of eight seaweed species originating from the Western Portuguese coast are presented in Table 2. Concentrations of Ca and K varied one order of magnitude among the samples, i.e., from 0.17% (Gracilaria gracilis) to 3.06% (Ulva sp) and from 1.52% (Ulva sp) to 10.60% (Gracilaria gracilis), 5 J. Milinovic et al. Journal of Food Composition and Analysis 110 (2022) 104559 Fig. 5. Original plots of CVPLS model for predicted K content (%) in seaweed samples by ED-XRF vs. ICP-OES results. See Fig. 4 for detailed explanations of the parameters. peach, and/or spinach), which may not be suitable for external valida­ tion of methods due to their different chemical composition compared to seaweeds (Collins et al., 2014; Brito et al., 2017). The SRM 3232 used for the quality assurance of the in-house ED-XRF analysis showed that the recoveries for selected elements (after seven replicate measurements) were 112 ± 1% for Ca, 96 ± 4% for P, and 119 ± 2% for K. Although precision was acceptable, the accuracy of results for Ca and K was higher, as expected because of their overlapping peaks (Fig. 2) when pre-installed factory calibration software is used (Gallhofer and Lottermoser, 2018). Representative ED-XRF spectra with labeled macroelements of three sets of samples containing green, red, and brown seaweed species, respectively, are shown in Fig. 3. As can be seen, the three sets of samples, collected from the central western Portuguese coasts showed similar ED-XRF patterns. Low peaks of P (at 2.01 keV) were registered in all samples at low intensities, whereas K and Ca (at 3.31 and 3.59 keV; 3.69 and 4.01 keV, respectively), were registered at higher intensities. Among red species, the main peak for K showed the highest intensity in Gracilaria gracilis (Fig. 2 B) and this corresponds to the results deter­ mined by ICP-OES (Table 2), which is also visible in Fig. 3 C, for Sac­ corhiza polyschides and Undaria pinnatifida. Direct determination of macroelements by ED-XRF showed poor accuracy and linear regression for ED-XRF vs. ICP-OES results had a wide interval of R2 values, ranging from 0.35 (Ca) to 0.81 (P) (Table 1S). In the case of Ca, very low regression can be explained by extrapolation 3.2. ED-XRF spectral analysis of seaweeds In the selected GeoMining mode of ED-XRF, the limit of detection (LOD) for the analyzed macroelements ranged from 0.0035% to 0.0053% (w/w, dw). The upper limit of calibration concentrations for the analysis of P, K, and Ca, were 13.2%, 18.4%, and 31.0% (w/w, dw) respectively, thus providing direct sample analysis (without dilution). An ED-XRF spectrum of SRM 3232 with the main features for P, K, and Ca, is shown in Fig. 2. The small peak at 2.01 keV corresponds to P, while the most intense peak at 3.31 keV (Kα line) and several times lower, following an asymmetric peak at 3.59 keV (Kβ lines) are associ­ ated with K. A broad small peak at 3.69 keV corresponds to Ca (Kα line) and it overlapped with K. Another Ca peak (Kβ line) was observed at 4.01 keV. The peak typical for Mg (Kα at 1.25 keV) was not visible, which was restricted by the calibration package of the selected mode used. For the other two macroelements, S (Kα at 2.31 keV) and Cl (Kα at 2.62 keV), peaks were visible, but their concentrations were not deter­ mined by ICP-OES, and hence, they were not considered. 6 J. Milinovic et al. Journal of Food Composition and Analysis 110 (2022) 104559 Fig. 6. Original plots of CVPLS model for predicted P content (%) in seaweed samples by ED-XRF vs. ICP-OES results. See Fig. 4 for detailed explanations of the parameters. associated with overlapping peaks (Fig. 3). To avoid this problem, and to minimize erroneous software quantification due to chemical in­ terferences, ED-XRF spectral results were treated by chemometrics tools. In this context, the multivariate regression analysis was applied to EDXRF spectral results in order to achieve a more accurate quantification of major elements in seaweed matrices. the linear regression equations of calibration, all three macroelements showed higher correlation coefficients after the proposed multivariate regression model (Table 1S). For the calibration of Ca and P, 7 latent variables were necessary to maximize the relationship between depen­ dent (ED-XRF spectra) and independent variables (ICP-OES results). For the calibration datasets all three macroelements, showed high correla­ tion coefficients in the range from 0.88 (K) to 0.95 (P). RMSE and the associated standard errors (SE), commonly used as uncertainty measure of a model, were low (< 1.02), while bias was equal to zero. The vali­ dation datasets showed similar values (Figs. 4–6, Table 1S), thus con­ firming the goodness of fit in comparison with scarce data available in the literature. The robustness of the applied CVPLS method, tested after removing data of a sample from the Óbidos lagoon (Ulva sp), confirmed the goodness of fit. As an example, Fig. 7 shows original plots of the CVPLS model for predicted K content after excluding results for Ulva sp. (n = 56). Compared to the entire sample size (Fig. 5), the statistical parameters in the reduced sample size were improved, i.e., higher R2 (0.95) and lower RMSE (0.58) values (Fig. 7). Nevertheless, a lower sample size, affected the number of latent variables increasing it to the maximum number (7). Similar results were confirmed for Ca (R2 = 0.95, 3.3. Quantitative statistics: prediction of macroelements in seaweed samples The full cross-validation as superior multivariate modeling was used in the quantitative statistics, i.e., prediction model, thus providing cor­ rect true apparent prediction error (Martens and Dardenne, 1998). In this model, all available results were used for calibration and full cross-validation, and not removing some results from an already limited set of available samples to an independent validation dataset. Setting aside some of the results can reduce the predictive performance of the calibrated models and give an uncertain, systematically over-optimistic assessment of the predictive performance of models. The values of statistical parameters of the CVPLS model for pre­ dicting Ca, K, and P are shown in Figs. 4–6 and Table 1S. Compared to 7 J. Milinovic et al. Journal of Food Composition and Analysis 110 (2022) 104559 Fig. 7. Original plots of CVPLS model for predicted K content (%) in seaweeds, after exclusion of Ulva sp. (n = 56) by ED-XRF vs. ICP-OES results. See Fig. 4 for detailed explanations of the parameters. by statistically significant parameters (R2, RMSE, and bias) with smaller datasets (n = 56–63) having a limited set of samples available. The proposed method will be extended including more edible species (depending on their availability), as well as elements, towards scaling up to routine day-to-day analysis for food industrial applications. RMSE = 0.09), while no differences in model parameters were observed for P (R2 = 0.95, RMSE = 0.03). This can be explained by the differences in the range of concentrations of the three macroelements in selected samples (Table 2). To summarize, results demonstrated a significantly good correlation between ED-XRF spectra (dependent variables) and ICP-OES results (independent variables) for predicted macroelements in edible seaweeds after applied CVPLS multivariate analysis. The relatively high R2 values, low RMSE and bias provided an efficient and robust model to predict the concentrations of individual major mineral components in representa­ tive edible seaweeds. Funding This work was supported by the project “MAR-01.03.01-FEAMP0016-Alga4Food” which is funded by the European Maritime and Fish­ eries Fund and co-funded by the Operational program MAR2020 in the field of Sustainable development of Aquaculture in the domains of Innovation, Advice and Productive Investment - Innovation and Knowledge Action. F. Figueiredo and J. Milinovic gratefully acknowledge research fel­ lowships from Portuguese Agência Nacional de Inovação (ANI) and Mar2020 program (Portugal), respectively. J. 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