Abstract
Consumed by populations in South America, Araucaria angustifolia seeds have received little study regarding elemental composition and nutritional value. Thirty-five seed sites from subtropical Brazil were sampled and seed concentrations of C, N, K, Ca, Mg, P, Fe, Zn, Mn, Cu, Mo, Ni, Co, Cr, Ba, and Cd were determined. The highest concentration of N was observed in samples from regions with Cfa climate (humid subtropical, oceanic climate, without dry season with hot summer) and igneous rock, which was superior to regions with Cfb climate (humid subtropical, oceanic climate, without dry season with temperate summer) and metamorphic rock. Seeds can be a source of nutrients: K (11.8 g kg−1), P (4.1 g kg−1), Mn (9.1 mg kg−1), Cu (7.2 mg kg−1), Mo (0.93 mg kg−1), and Cr (0.65 mg kg−1). Values for Ba (0.93 mg kg−1) and Cd (0.19 mg kg−1) indicated no risk to human health. This study expands knowledge regarding the elemental composition of A. angustifolia. Results indicate that these seeds have nutritional value, and their consumption can be a good strategy to improve overall human nutrition in this region of South America.
Electronic supplementary material
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Keywords: Recommended dietary allowances, Trace elements, Environmental variation, Conifers
Introduction
Commonly known as Brazilian Pine, Paraná Pine, or Candelabra Tree, Araucaria angustifolia (Bert) O. Ktze is a native tree of Brazil. Isolated individuals have also been found in northern Argentina and eastern Paraguay. Currently, A. angustifolia is on the list of endangered species since it occupies only 2% of its original range. However, economic, industrial, and cultural factors related to food usage of A. angustifolia seeds have contributed to the preservation of this species. Edible seeds of Araucaria angustifolia have been part of human diets as far back as pre-Columbian times (Reis et al. 2014; Polet et al. 2017). Cordenunsi et al. (2004) and Schveitzer et al. (2014) demonstrate that A. angustifolia seeds can be a source of starch and nutrients (e.g., Fe and Zn) lacking in human diets. In addition, there is current relevance to food technology investigation, especially in bakery products for people with celiac disease (Polet et al. 2017).
Araucaria angustifolia seed are primarily harvested from trees under native conditions in subtropical Brazil (extractivism) since there are few planted forests. In the region of occurrence, there are distinct environmental growth conditions (Alvares et al. 2013; Rabel et al. 2018). However, there is a lack of information regarding the nutritional composition of A. angustifolia seeds since past studies have only investigated isolated samples (Cordenunsi et al. 2004; Schveitzer et al. 2014). Thus, this study aimed to analyze the elemental composition of A. angustifolia seeds from a large area (175,200 km2) of subtropical Brazil to evaluate the level of toxic and beneficial elements and the possible implications for human health.
Materials and methods
Sampling areas and sample preparation
During June and September 2014, 35 seed samples of A. angustifolia were obtained from three southern states in Brazil (Paraná, Santa Catarina, and Rio Grande do Sul) (Online Resource 1; Online Resource 2). Seeds from mature fruits were collected from the ground below the tree canopy.
Samples were oven dried for 24 h (65 °C), seed shells were removed, and shelled seeds (pinions) were dried for an additional 48 h (65 °C). Only seeds with no visible damage were selected for analysis. Subsequently, dry pinion mass was calculated by the ratio of seed mass to seed number. Seeds were ground to pass through a 0.5 mm mesh.
Elemental analysis
Concentrations of carbon (C) and nitrogen (N) were determined by dry combustion in a non-metal element analyzer (Elementar, Vario EL III model, Hanau, Germany) using 15 mg per sample (analyzed in duplicate). Samples were weighed into sealed tin capsules and incinerated at a temperature of approximately 900 °C. Acetanilide (Acros Organics; Geel, Belgium) was used for instrument calibration.
Concentrations of other elements were determined by the wet method according to the SW-846 test method 3051A (Microwave Assisted Acid Digestion of Sediments, Sludges, Soils, and Oils method; USEPA 2007). Concentrations of potassium (K), calcium (Ca), magnesium (Mg), phosphorous (P), iron (Fe), zinc (Zn), manganese (Mn), copper (Cu), molybdenum (Mo), nickel (Ni), cobalt (Co), chromium (Cr), barium (Ba), and cadmium (Cd) in extracts were determined using an inductively coupled plasma optical emission spectrometer (ICP-OES, axial mode; Varian 720-ES model, Mulgrave, Victoria, Australia). For ICP-OES calibration, solutions containing increasing concentrations of analyzed elements were prepared from a multi-elemental standard solution (QuimLab, Curitiba, Brazil).
Estimating nutritional value
The nutritional value of A. angustifolia seeds was estimated by comparing element intake values (established from different indices) using 100 g seed portions (wet basis). Wet basis was used in calculations since A. angustifolia seeds are consumed at an average moisture content of 45% (Cordenunsi et al. 2004; Schveitzer et al. 2014). However, to obtain intake values closer to consumption conditions, content of elements in 55 g of seeds (dry basis) was considered to be equivalent to elemental content in a 100 g wet basis portion. The daily intake indices used for adults were as follows: recommended dietary allowances (RDA) for protein, K, Ca, P, Mg, Fe, Zn, Mn, Cu, Mo, and Cr; tolerable upper intake (TUI) for Mo, Co, Ba, Ni, and Cd; and estimated intake (EI) for Cr (WHO 1996; IOM 2001; FSA 2003; SCHER 2012). Protein values were estimated from total tissue N by multiplying by a conversion factor of 6.25.
Statistical analysis
For all data, we present descriptive statistics. In addition, seed dry matter and element concentration results were analyzed considering four sample groups representing different climatic conditions and parent rock (I—Cfa/igneous; ten samples; II—Cfb/igneous, eight samples; III—Cfb/sedimentary, twelve samples; and IV—Cfb/metamorphic, five samples). The data were subjected to the Shapiro–Wilk normality test, and normal data were subjected to the F test, while other data were subjected to the Kruskal–Wallis test. There was significant variation only in the Kruskal–Wallis test (p < 0.05), thus the Dunn’s test was applied to differentiate treatment effects (p < 0.05) for N concentrations. Statistical analyses were performed with the Assistat 7.7 program.
Results and discussion
Elemental composition
Mean C, K, N, and P content indicate that these were the four main nutrients in A. angustifolia seeds (Table 1). On average, 95.7% of inorganic constituents (excluding C) of A. angustifolia seeds were represented by K, N, and P (primarily soil derived), with K and N representing ~ 80.4%, corroborating results from other studies (Schveitzer et al. 2014; Cordenunsi et al. 2004; Liang et al. 2015).
Table 1.
Results of dry matter and elemental composition of Brazilian pine (Araucaria angustifolia) seeds from subtropical Brazil
| Variable | Unity | Mean | Median | SD | Maximum | Minimum |
|---|---|---|---|---|---|---|
| Dry matter | g seed−1 | 3.43 | 3.33 | 0.65 | 5.20 | 2.52 |
| C | g kg−1 | 383 | 382 | 9 | 408 | 370 |
| N | g kg−1 | 10.0 | 9.9 | 1.1 | 12.5 | 8.1 |
| K | g kg−1 | 11.8 | 11.7 | 1.1 | 14.7 | 9.7 |
| P | g kg−1 | 4.18 | 3.92 | 0.80 | 5.99 | 2.77 |
| Ca | g kg−1 | 0.29 | 0.28 | 0.08 | 0.52 | 0.11 |
| Mg | g kg−1 | 0.78 | 0.79 | 0.07 | 0.89 | 0.62 |
| Fe | mg kg−1 | 25.83 | 23.08 | 10.42 | 61.51 | 15.71 |
| Zn | mg kg−1 | 18.86 | 18.55 | 3.48 | 24.18 | 10.91 |
| Mn | mg kg−1 | 9.11 | 8.72 | 4.14 | 19.74 | 2.40 |
| Cu | mg kg−1 | 7.23 | 7.13 | 1.56 | 10.50 | 4.87 |
| Ni | mg kg−1 | 1.30 | 0.95 | 0.73 | 3.42 | 0.70 |
| Mo | mg kg−1 | 0.93 | 0.89 | 0.16 | 1.36 | 0.69 |
| Ba | mg kg−1 | 0.93 | 0.85 | 0.39 | 2.07 | 0.27 |
| Co | mg kg−1 | 0.45 | 0.39 | 0.13 | 0.79 | 0.32 |
| Cr | mg kg−1 | 0.65 | 0.49 | 0.36 | 1.76 | 0.35 |
| Cd | mg kg−1 | 0.19 | 0.19 | 0.01 | 0.23 | 0.17 |
Ca and Mg content in A. angustifolia seeds from subtropical Brazil (Table 1) were similar to those observed in other studies (same species), but lower than seeds of other species such as Brazil nuts (Naozuka et al. 2011) and walnuts (Rodushkin et al. 2008). A convergent aspect among these species is that Mg concentrations are approximately double that of Ca. Seed Ca and Mg variations may be due to reduced Ca phloem transport aggravated by lower transpiration of fruits compared to leaves. In addition, Ca has less remobilization from leaf and branch tissues since it is predominantly associated with cell walls (White 2012) and oxalate crystals (Barbosa et al. 2017).
Micronutrients with the highest concentrations were Fe and Zn, and Mo and Ni were the lowest (Table 1). While there was wide variation in micronutrient in seeds or nuts of various species, the highest concentrations occur for Fe, Zn, or Mn (Anderson and Smith 2005; Naozuka et al. 2011; Vanhanen and Savage 2013; Souza et al. 2014). Concentrations of Fe and Zn ranged from 15.7 to 61.5 mg kg−1 and 10.9 to 24.1 mg kg−1 (Table 1), suggesting A. angustifolia may have genetic potential for genotype selections for higher concentrations of these nutrients.
The mean Ba content in A. angustifolia seed (Table 1) was similar to or lower than reported for other nuts and seeds (Rodushkin et al. 2008). In general, Co and Cr concentrations in seeds and nuts varied between 0.07 and 1.9 and 0.01 and 5.9 mg kg−1, respectively (Özkutlu et al. 2011; Vanhanen and Savage 2013; Liang et al. 2015). Thus, concentrations of these elements in A. angustifolia seeds (Table 1) were similar to concentrations recorded in other species. The average Cd content in A. angustifolia seeds was 0.19 mg kg−1 (Table 1) below the maximum level allowed for polished rice (0.4 mg kg−1) and wheat (0.2 mg kg−1) (CAC 2015).
Nitrogen was the only element with varying concentration among the classification groups (Fig. 1). The average N concentration was 10.8 g kg−1 in Group I, which was higher than the 9.2 g kg−1 observed in Group IV (Cfb/metamorphic rock). Group II (Cfb/igneous rock) and Group III (Cfb/sedimentary rock) did not differ among groups, with mean concentrations of 9.9 and 10.1 g kg−1, respectively. In general, soils originating from basalt material in Group I (Cfa/igneous rock) are clayey or very clayey and generally have high organic matter content. During summers in Brazil (December to March), the hot (average temperature ≥ 22 °C) Cfa climate (Alvares et al. 2013) may have favored organic matter decomposition. It is important to note that summer environmental variations can influence A. angustifolia trees since this is the period of most intense growth and seed filling. However, seed N concentrations observed in Groups II and III do not seem to be solely influenced by climate, indicating that other factors such as genetic variation, atmospheric N, and edaphic conditions may have influenced results. Studies with more intensive sampling are required to confirm these results and to explore the effects on other elements.
Fig. 1.
Nitrogen concentration of Araucaria angustifolia seeds. The lower boundary of the box indicates the 25th percentile and the upper boundary, the 75th. Whiskers above and below the box indicate the 95th and 5th percentiles. Lines within the box mark the median (solid line) and mean (dash line). Group I: Cfa/igneous rock; Group II Cfb/igneous rock; Group III: Cfb/sedimentary rock; Group IV: Cfb/metamorphic rock. Different lowercase letters (a, b) inside boxes indicate that groups differ by Dunn’s test (p < 0.05)
Nutritional value
Protein contribution from seed intake ranged from 5.0 to 7.7% of recommended dietary allowance (Table 2). In comparison, A. angustifolia seeds contribute less to protein intake than legume seeds, nuts, amaranth, maize, wheat and barley, but approach that of white rice (Young and Pellett 1994; King et al. 2008). However, it is important to emphasize that these protein contribution values are only approximate indicators of dietary contributions since amino acid composition, antinutritional factors (tannins, amylase inhibitors, cyanogen), and food preparation techniques can influence overall protein utilization (Young and Pellett 1994). In the case of A. angustifolia seeds, the most traditional form of preparation is by cooking in water, which has an inexpressive effect on protein concentration, raises total phenolics and quercetin concentrations (probably from the seed coat), and decreases amylose, glucose, fructose, and sucrose (Cordenunsi et al. 2004). Although A. angustifolia seeds (Table 2) contribute less to protein intake compared to other seeds (Young and Pellett 1994; King et al. 2008), the amino acid composition resembles that of cereals such as wheat and corn (Leite et al. 2008). Additionally, these authors reported that lysine was present in higher quantities than observed in wheat, corn, and rice flours, and that methionine and valine were higher in comparison to soybean.
Table 2.
Contribution to the recommended dietary allowances (RDA), tolerable upper intake (TUI), and estimated intake (EI) indices with the consumption of 100 g of Araucaria angustifolia seeds from southern Brazil
| Element | Index | Value | RDA, TUI or EI contribution (%) | ||||
|---|---|---|---|---|---|---|---|
| Mean | Median | SD | Maximum | Minimum | |||
| Proteina | RDA | 51 g | 6.2 | 6.1 | 0.7 | 7.7 | 5.0 |
| Kb | RDA | 3500 mg | 18.5 | 18.4 | 1.6 | 23.2 | 15.2 |
| Pa | RDA | 700 mg | 32.8 | 30.6 | 6.3 | 47.1 | 21.8 |
| Caa | RDA | 1000 mg | 1.6 | 1.6 | 0.5 | 2.9 | 0.7 |
| Mga | RDA | 370 mg | 11.7 | 11.8 | 1.0 | 13.3 | 9.2 |
| Fea | RDA | 14 mg | 9.7 | 9.0 | 3.2 | 20.9 | 6.2 |
| Mna | RDA | 2.0 mg | 25.0 | 23.1 | 11.2 | 54.3 | 6.7 |
| Zna | RDA | 9 mg | 11.4 | 11.8 | 2.0 | 14.8 | 6.7 |
| Cua | RDA | 0.90 mg | 43.6 | 43.4 | 8.3 | 64.2 | 29.2 |
| Moa | RDA | 45 μg | 115 | 93 | 20.7 | 165 | 84.6 |
| Moa | TUI | 2000 μg | 2.6 | 2.5 | 0.5 | 3.7 | 1.9 |
| Cra | RDA | 30 μg | 121 | 115 | 64.9 | 321 | 64.6 |
| Crb | EI | 770 μg | 4.7 | 3.6 | 2.5 | 12.5 | 2.5 |
| Nid | TUI | 1000 μg | 7.2 | 6.1 | 3.9 | 18.8 | 3.8 |
| Bac | TUI | 1300 μg | 4.0 | 3.6 | 1.7 | 8.7 | 1.1 |
| Cob | TUI | 1400 μg | 1.8 | 1.6 | 0.5 | 3.1 | 1.3 |
| Cdd | TUI | 65 μg | 16.3 | 16.3 | 0.9 | 19.2 | 14.3 |
A. angustifolia seeds contributed more than 18% of RDA values for K, P, Mn, Cu, Mo, and Cr (Table 2). Evaluating the nutritional value of A. angustifolia seeds, Cordenunsi et al. (2004) observed that only Mg and Cu were supplied in considerable amounts relative to RDA values. An elemental evaluation of A. angustifolia seeds from the state of Santa Catarina (Brazil) found that these seeds were a great source of P, Mg, Fe, Mn, and Cu for human diets (Schveitzer et al. 2014). While A. angustifolia seeds are not high in protein, they are low in sodium (Na), a vitamin C source (28 mg 100 g−1) (NEPA 2011), and their consumption can help meet recommended intake values for several nutrients (Table 2).
Despite the average contribution of Mo and Cr exceeding 100% of RDA, the values are within the maximum tolerated limit (TUI) for Mo and the estimated mean intake (EI) for Cr. With stone pine cultivated in New Zealand, Vanhanen and Savage (2013) reported that the consumption of 50 g of seeds provides a contribution above RDA critical levels for Cr, Cu, Mg, Mn, and Zn.
Conclusion
C, N, K, P, Ca, Mg, Fe, Mn, Zn, Cu, Ni, Mo, Ba, Cr, Co, and Cd content in A. angustifolia seeds were generally similar to those reported for other seeds. The lithology and climate of southern Brazil affected only the N concentration of A. angustifolia seeds from subtropical Brazil. Based on the estimated contributions to RDA, A. angustifolia seeds can be a source of beneficial nutrients (primarily K, P, Mn, Cu, Mo, and Cr), while values for Ba and Cd do not indicate health risks. Thus, consumption of A. angustifolia seeds can be a good strategy to improve overall human health.
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Acknowledgements
The authors are grateful to Sérgio Mudrovitsch de Bittencourt (Emater), Oromar Bertol (Emater), Gervazia Zimmer, Elaine Inês Zimmer, Marisane Antunes, Rosemari Poggere, Michael Kreusch, Tiago Budziak, Gasparina Mendes França Buratto, Jacy Buratto and Delmar Santin for help in seeds collection and to Elidiane da Silva for design of study area map.
Footnotes
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