Microsoft Word - 10-Agra_32993.doc 1234 Original Article Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 INFLUENCE OF ZINC DEFICIENCY ON THE MINERAL COMPOSITION OF MAIZE PLANTS IN CONTRASTING SOILS INFLUÊNCIA DA DEFICIÊNCIA DE ZINCO NA COMPOSIÇÃO MINERAL DE PLANTAS DE MILHO EM SOLOS CONTRASTANTES Caio Ricardo dos Santos DOMINGUES 1 ; Julierme Zimmer BARBOSA 2 ; Rangel CONSALTER 2 ; Maisa dos SANTOS 1 ; Wiliam Magrim ADAM 1 ; Antonio Carlos Vargas MOTTA 3 1. Mestre em Ciência do Solo, Universidade Federal do Paraná - UFPR, Curitiba, PR, Brasil; 2. Doutorando em Ciência do Solo Universidade Federal do Paraná - UFPR, Curitiba, PR, Brasil; 3. Professor, Doutor, Universidade Federal do Paraná - UFPR, Curitiba, PR, Brasil. mottaufpr@gmail.com ABSTRACT: In Brazil, Zn deficiency is common in soils used for maize cultivation. However, the changes in the mineral composition in plants with Zn deficiency have been little studied. Thus, this study aimed to evaluate the relationship between Zn deficiency and the mineral composition in the parts of maize plants grown under contrasting soils. Maize was grown in greenhouse conditions with increasing of Zn rate (0, 0.125, 0.25, 0.5 and 1.0 mg kg-1) in two soils (Ferralsol and Cambisol). After 60 days of emergence, the plant were separated into roots, stalk nodes, stalk internodes, leaves and leaf sheath, and subsequently determined the dry matter and mineral composition (P, Ca, Mg, K, Zn, Fe, Mn, Cu and Al). Besides the symptoms commonly described for Zn deficiency, darkening of the stalk nodes was found (related to the preferential accumulation of Fe), and also occurred maize P deficiency in the Ferralsol. The Zn deficiency favored increasing concentrations of Fe, Mn and Al in all parts of maize plants in Cambisol, whereas in Ferralsol this did not happen for any of the elements analyzed. Relations between the elements and Zn were more correlated with maize dry matter production than Zn concentrations in leaves, leaf sheaths and stalk nodes. In conclusion, the accumulation of minerals in maize was favored by Zn deficiency, especially for maize in Cambisol. KEYWORDS: Zea mays L. Fe accumulation. Metal toxicity. P availability. Stalk nodes. INTRODUCTION An estimated half of agricultural soils used in the world are Zn deficient, having an average value of only 50 mg kg-1 as a total concentration (ALLOWAY, 2008). For highly weathered soil in Brazil, the Zn deficiency has been shown to be critical since the majority of soil parent materials were poor in Zn and the weathering process depleted its reservoir even more (MARQUES et al., 2004). Additionally, when these weathering acid soils were incorporated to crop production, the soil pH was adjusted by liming, there decrease in Zn availability in soil (KABATA-PENDIAS, 2011). Maize is known as a crop sensitive to lack of Zn, whereas availability in the soil is related to the productive potential of maize (ALLOWAY, 2008; PUGA et al., 2013). It is the second most produced crop in Brazil, and the country is the world's third largest producer (USDA, 2016). Despite this ranking, the average yield continues to be low with great potential for its improvement. This can be seen in many regions of Brazil where there is high technological level used in maize farming and favorable environment conditions, allowing yields 2 or 3 fold higher than the Brazilian national average. To evaluate the Zn nutritional diagnosis, foliar analysis has been used by considering one absolute value, such as the critical level, or range of sufficiency. In some cases, however, the foliar Zn analysis has failed to explain the low yield despite its concentration being above the critical concentration or within the sufficiency range (HIATT; MASSEY, 1958; NAMBIAR; MOTIRAMANI, 1981). To improve the results of leaf analysis the nutritional status has considered the Zn balance with other nutrients. The Zn versus Fe balance has been studied as the foliar Fe/Zn ratio and showed to be more efficient than the absolute value of the Zn concentration (ZARE et al., 2009). However, lack of Zn expressed a higher number of genes than Fe, Mn and Cu and involved the higher number of proteins related to the absorption and efflux of Cu, Fe, Mn and Ni (WHITE, 2012). In general, Zn deficiency in maize appears as a yellow striping of the leaves, under severe deficiency the plants a reddish or yellowish streak about one-third of the way from the leaf margin. Moreover, although little known, it has been reported that the stalk nodes of Zn-deficient maize present a dark color (VITOSH et al., 1994), which can be useful for enriching the information via visual symptoms. Similar symptoms in the stalk Received: 26/01/16 Accepted: 06/06/16 1235 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 were associated with high concentrations of Fe in soils with high availability of this element (SAYRE, 1930). Thus, considering the effects of Zn on the accumulation of Fe and other metals (NAMBIAR and MOTIRAMANI, 1981; CHILIAN et al., 2015), it is possible that: the darkness of the stalk nodes in Zn deficiency is related to the accumulation of Fe and other metals; the amount of Fe in the soil can be decisive for results. However, even with 12 different soils, the relationship between the plant growth and Zn concentrations or Fe/Zn ratio is not clear (ZARE et al., 2009). Even Nambiar and Motiramani (1981) observed relationship between production and the Fe/Zn ratio only within each soil studied individually. This indicates that soil possibly has a strong influence on the dynamics of Zn uptake by the plant and, consequently, the critical levels of Zn and Fe/Zn ratio. Thus, the present study aimed to evaluate the relationship between Zn deficiency and the mineral composition in parts of maize plants grown under contrasting soils. MATERIAL AND METHODS The experiment was conducted in a plastic greenhouse (without light control and partial temperature control) in Curitiba, Paraná State, Brazil. Due to lack of light control, it is important to inform that the experiment was conducted in a period (between November and December 2013) in which the cultivation of maize is recommended in the region. The temperature control of the greenhouse had air extractors and an air humidifying system and automatically activates when the temperature reached 28°C, remaining in operation until the temperature drops below 28°C. Acid soil material from a Ferrasol and a Cambisol (FAO, 2006) were collected (0-20 cm layer) in pine plantations, with no record of fertilizer or lime application. Granulometric analysis (densimeter method) showed the following results: sand, 70 and 90%; silt, 5 and 2.5%; clay, 25 and 7.5%, respectively, Ferralsol and Cambisol. Chemical analysis of soil samples (Table 1) showed that the soils were deficient in Zn and, in general, presenting low fertility. Table 1. Chemical properties of soils (S) before of liming and fertilization, from Jaguariaiva – Paraná state - Brazil. S1 pH2 Ca2+ Mg2+ K+ Al3+ H+Al3+ CEC BS m P Fe Zn Cu Mn OC -------------------- cmolc dm -3 ------------------- % % ----------- mg dm-3 --------- g dm-3 1 3.4 0.3 0.1 0.05 1.5 5.4 5.85 7.7 76.9 2.6 166 0.4 0.3 0.1 11.6 2 3.9 0.2 0.1 0.02 1.0 5.0 5.32 6.4 75.7 2.1 84 0.4 0.3 1.8 11.4 1 Soil 1 and 2 are, respectively, Ferralsol and Cambisol. 2 pH (CaCl2 0.01 mol L -1); Ca2+, Mg2+, Al3+ (extracted with KCl 1mol L-1); H+ + Al3+ (calcium acetate 0.5 mol L-1 extraction); organic carbon (OC) (volumetric method by potassium dichromate); K+, P, Mn, Fe, Cu and Zn (Mehlich-1 extraction); Base saturation (BS); Al3+ saturation (m). The collected soil materials were sieved by passing through a polypropylene mesh with 4 mm aperture before drying. Subsequently, the sieved material received lime in order to reach 70% base saturation. A mix (1:1) of pure CaCO3 and MgCO3 was applied and kept incubated for two weeks. The limed soil materials were kept covered to maintain the moisture. Note that the pH increase with liming reduces the availability of Zn and Mn, Fe, Cu, Ni and B. Thus, liming likely accentuated the lack of Zn in Ferralsol and Cambisol. After the incubation period, 6 kg of dried soil materials was weight and put in vases for a total of 40 vases. Analytic reagents were used to prepare a solution and this was applied on the soil surface in each vase in the following amount and source: 200 mg kg-1 of N, P2O5 and K2O; 0.5 mg kg -1 B, 1 mg kg-1 of Cu and 0.2 mg kg-1 Mo in the form of urea, monocalcium phosphate, potassium chloride, boric acid, sodium molybdate and copper chloride, respectively. After the nutrient application, the treatments were performed by adding 0; 0.125; 0.25; 0.5 and 1.0 mg kg-1 of Zn as analytic ZnCl2. The lower Zn levels (up to 0.5 mg kg-1) were chosen to obtain different stages of deficiency (moderate to severe). However, the highest level was chosen to provide the plants with conditions without severe deficiency. Each experimental unit consisted of a glazed vase filled with soil. The soil material was mixed after each procedure (sieving, liming, incubation, nutrients application and Zn application) in order to maintain homogeneity. The moisture was also determined after sieving, incubation, and nutrients application in order to calculated dry weight base equivalent application. Five seeds of Agroceres F1 Hybrid RR maize were sown and 10 days after emergence thinning was conducted, maintaining only two 1236 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 seedlings per vase. Irrigation of the vases was performed daily as needed, using deionized water. At the end of the experiment, 60 days after seedling emergence plant height was determined. The shoot was cut at 1 cm from the soil surface and brought to the lab where the shoots were separated into stalks and leaves. The stalk was laid on a wooded table and longitudinal cut was performed in the middle in order to have an internal view of the stalk nodes and internodes. Photographs were taken (Fujifilm A220 camera) of the plant with the inside of the stalk exposed. The stalk was cut again into nodes, internodes and sheath leaves. The soil with roots was pulled out of the vase and was put on a 4 mm sieve and gently handles to release the soil. After most of the soil was lost a spray of pressurized water was applied. In the laboratory, roots were cleaned again under running water to remove the small soil particles from inside the root mass. Finally, the root was immersed in NaOH 1.25 mol L-1 for 15 minutes and again under deionized water. The root and shoot fractions then were dried at 60 °C for 48 hours to obtain the dry matter production which was ground in Willey mill and passed through a 1 mm sieve. The chemical analysis of the maize fractions (roots, stalk nodes, stalk internodes, leaves and leaf sheaths) was performed by dry digestion; a sub- sample of 1g was calcined in a porcelain crucible in muffle furnace at 500°C for 3 hours. After cooling of the crucibles, the ash was digested with 3 mol L-1 HCl and the crucibles remained in the muffle at 500°C for 3 more hours. Afterwards, 10-ml of 3 mol L-1 HCl was then added and the crucibles remained for 10 minutes on a hot plate at 70 °C. The digestion solutions were filtered in filter paper and the extracts collected in 100-ml volumetric flasks. To gauge the volumetric flasks, deionized water was used. The following were determined in the obtained extracts: K with flame emission spectrometer (Digimed, MD-62); P with UV-VIS spectrometer (Bel Photonics, SP2000), colorimetry via ammonium molybdate-vanadate; Ca, Mg, Fe, Mn, Zn, Cu, and Al with atomic absorption spectrometer (Varian, AA240FS). The difference (%) of Fe, Mn, Cu, Zn, P, K, Ca and Mg in the stalk nodes compared to stalks internodes was obtained based on element concentration and content. The experimental was arranged in a completely randomized design with 2 x 5 factorial (2 soils and 5 Zn rates), with four replications, and each experimental unit consisted of a vase with two plants. However, for the results of stalk internodes a factorial 2 x 4 was used, because the plant growth was so reduced under the absence of Zn that it was not possible to obtain enough mass to run analysis for this treatment. For data analysis we performed variance (ANOVA). Where the ANOVA result was significant, the data were analyzed by regression for Zn rates and by Least Significant Difference (LSD) test to compare the soils. Pearson correlations between some data were also obtained. For all tests, the minimum level of 5% significance level was adopted. RESULTS AND DISCUSSION Symptoms of nutritional deficiency associated with Zn were observed in maize plants for both soils. In the control, with the absence of Zn, the seedling had reduced growth and necrosis of all leaves in Cambisol, while in Ferralsol it was observed interveinal chlorosis in new leaves and necrotic spots on the intermediate leaves. These results indicate that the Cambisol Zn deficiency was more severe, leading to leaf necrosis (BROADLEY et al., 2012). A larger plant was observed when 0.125 and 0.250 mg kg-1 were used, compared to the control. The symptoms were characterized by interveinal chlorosis on young leaves with subsequent general chlorosis of these leaves, stiff leaves and internode growth reduction. Although still being deficient, the two lower Zn rates improved maize nutrition, including Cambisol where plants showed no necrosis in the leaves. At the 0.5 mg kg-1 Zn rate only interveinal chlorosis in new leaves was observed in the Cambisol, whereas in Ferralsol these symptoms were also observed at the dose of 1.0 mg kg-1. In addition, in Ferralsol, regardless of the amount of Zn added, a purple color on the old leaves was observed. Therefore, in Ferralsol there is simultaneous Zn and P deficiency, which must be kept in mind to understand the possible changes in elemental composition. When the stalk was split in the middle by a longitudinal cut, the node internal areas were dark under Zn deficiency (Figure 1), for both soils, but in Ferralsol plants present this symptom at all Zn rates. Therefore, when Zn deficiency symptoms were detected on leaves, there also occurred darkening of the stalk nodes, indicating that the nodes can be used as additional tools for visual diagnosis, corroborating with Vitosh (1994). 1237 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 Figure 1. Cut stalk of maize grown with increasing Zn rates. For Cambisol: A = without Zn addition; B = addition of 0.125 mg kg-1 Zn; C = increasing Zn rate addition. For Ferralsol: D = without Zn addition; E and F = addition of 0.125 mg kg-1 Zn; G = addition of 0.25 mg kg-1 Zn; H = addition of 0.5 mg kg-1 Zn; I = addition of 1.0 mg kg-1 Zn. Bars of 1 cm (A, B, D and E) and 10 cm (C, F, G, H and I). The dry matter results confirmed the condition of high Zn deficiency for both soils (Figure 2). But, higher growth and Zn response were obtained for Cambisol compared to Ferrasol, which differs in the two higher Zn rates for roots, leaves, sheath leaves and total dry matter, and the three higher Zn rates for nodes and internodes of the stalks. Our results confirm an earlier observation that Zn promotes plant growth by enhancing hormonal and protein syntheses since it is required to form tryptophan amino acid that is a precursor of indole acetic acid (BROADLEY et al., 2012). Positive responses to Zn application have been obtained in several studies, which report superiority in the production of dry matter in maize (KANAI et al., 2009; ZARE et al., 2009) and wheat (ALAM; SHEREEN, 2002; ZHAO et al., 2011). The difference in response between the soils to the Zn application may be associated to variation in P availability, which changed the P concentrations in maize leaves (Table 2). This difference is due to the higher clay content in Ferralsol (25%) compared to Cambisol (7.5%). Furthermore, due to its more advanced weathering degree, the Ferralsol probably contains more oxides in the clay fraction. Therefore, considering the ability of these minerals to adsorb the P (GÉRARD, 2016); there was a likely lower P availability in Ferralsol due to higher adsorption of this element in the soil mineral fraction. Thus, although phosphate fertilization was conducted, it is likely that P fixation made less P available to the plants in Ferralsol. 1238 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 0.0 0.5 1.0 1.5 2.0 35.0 y = -0.03 + 3.14x - 1.68x2 R2 = 0.95** y = 0.14 + 0.38x R2 = 0.91** *** D ry m at te r (g p la n t- 1 ) 0 2 4 6 8 10 35 y = -0.12 + 15.47x - 7.02x2 R2 = 0.94** y = 1.22 + 2.18x R2 = 0.95** ** BA Ferralsol Cambisol 0 1 2 3 4 35 y = -0.46 + 4.30x - 2.81x2 R2 = 0.94** y = 0.015 + 0.20x R2 = 0.99** ** * C 0.0 0.2 0.4 0.6 0.8 1.0 0 2 4 6 8 35 y = -0.07 + 15.96x - 9.52x2 R2 = 0.95** y = 1.01 + 1.95x R2 = 0.80** ** 0.0 0.2 0.4 0.6 0.8 1.0 D ry m at te r (g p la n t- 1 ) 0 4 8 12 35 y = -0.75 + 26.60x - 15.10x2 R2 = 0.92** y = 1.06 + 3.25x R2 = 0.86** ** ED 0.0 0.2 0.4 0.6 0.8 1.0 0 5 10 15 20 25 30 35 y = -1.13 + 64.10x - 35.04x2 R2 = 0.93** y = 3.45 + 8.01x R2 = 0.89** ** F Zn rates (mg kg-1) 0.0 0.5 1.0 1.5 2.0 Zn rates (mg kg-1) 0.0 0.5 1.0 1.5 2.0 Zn rates (mg kg-1) 0.0 0.5 1.0 1.5 2.0 ) 35.0 Figure 2. Dry matter of roots (A), stalk nodes (B), stalk internodes (C), leaves (D), sheath leaves (E) and total (F) of maize grown in Ferrasol and Cambisol with increasing Zn rates. ** = Significant at 1% for Zn rates; * = difference (significant at 5% by LSD test) between soils. Table 2. Concentration of K, Ca, Mg and P (g kg-1) in leaves of maize grown in two soils with application of Zn rates Soil 1 Soil 2 Soil x Zn Zn rates (mg kg -1 ) Equation R 2 0.0 0.125 0.25 0.5 1.0 K 1 ns * 20.2* 23.8 25.0 22.4* 18.8* y = 22.1 ns 2 26.8 26.3 24.5 13.4 11.1 y = 27.6 - 18.1x 0.82** Ca 1 * ns 11.5 6.8 7.1 5.5 4.3 y = 10.4 - 16.4x + 10.4x2 0.84** 2 10.6 5.8 4.9 3.4 2.9 y = 9.7 - 21.6x + 15.2x2 0.90** Mg 1 ns * 7.7* 5.4 5.4 4.9 4.4 y = 7.1 - 7.8x + 5.2x2 0.89** 2 10.4 5.3 5.3 4.1 3.5 y = 9.2 - 18.2x + 12.8x2 0.81** P 1 * ns 4.0 5.5 3.2 1.6 0.9 y = 4.5 - 4.2x 0.74** 2 7.5 9.2 8.8 2.1 1.5 y = 8.8 - 8.2x 0.72** 1 Ferralsol = 1, Cambisol = 2; 2 not significant (ns) or significant at 5% (LSD test) for soil and interaction soil versus Zn rates, and ** significant at 1% for Zn rates. In general, a reduction of element concentrations in leaves, leaf sheaths, internodes and stalk nodes of the maize stem in response to the Zn addition. However, the stabilization thereof, by the application of 1 mg kg-1 Zn, or a stable Zn supply condition, is clear (Figure 3; Table 3). The roots showed variable results among the analyzed elements and soils. Moreover, the variations between soils occurred mainly Fe and Mn. The influence of Zn on nutrients and Al, especially when it was deficient (Figure 3; Table 3), could be related to complex interactions between plant physiology and soil environment. Many changes in plant metabolism, root exudation and rhizosphere could be expected. The reduction of the concentrations of elements in maize (mainly leaves, leaf sheaths and stalk nodes) in response to the addition of Zn is related to: (i) the possibility that more phytosiderophores exudation in the rhizosphere of maize occurred under a Zn deficiency condition, as highlighted by Römheld (1991) for grasses, favoring the complexation and absorption of less available forms of soil Zn. However, phytosiderophores can increase the acquisition of other micronutrients such as Mn and Cu, and especially Fe. 1239 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 0.0 0.2 0.4 0.6 0.8 1.0 0 20 40 60 80 100 120 140 Roots Stalks nodes Leaves Sheath leaves Stalks internodes 0.0 0.2 0.4 0.6 0.8 1.0 F e (m g k g- 1 ) 0 400 800 1200 1600 2000 2400 0.0 0.2 0.4 0.6 0.8 1.0 0 400 800 1200 1600 2000 2400 0.0 0.2 0.4 0.6 0.8 1.0 Z n ( m g k g- 1 ) 0 20 40 60 80 100 120 140 0.0 0.2 0.4 0.6 0.8 1.0 M n ( m g k g -1 ) 0 25 50 75 100 125 150 0.0 0.2 0.4 0.6 0.8 1.0 0 25 50 75 100 125 150 0.0 0.2 0.4 0.6 0.8 1.0 C u ( m g k g -1 ) 0 20 40 60 80 100 0.0 0.2 0.4 0.6 0.8 1.0 0 20 40 60 80 100 Zn rates (mg kg-1) 0.0 0.2 0.4 0.6 0.8 1.0 A l (m g k g -1 ) 0 100 200 300 400 500 Zn rates (mg kg -1 ) 0.0 0.2 0.4 0.6 0.8 1.0 0 100 200 300 400 500 A B C D E F G H I J Figure 3. Concentrations of Zn (A, F), Fe (B, G), Mn (C, H), Cu (D, I) and Al (E, J) in the roots, stalk nodes, stalk internodes, leaves and leaf sheaths of maize grown in Ferrasol (A-E) and Cambisol (F-J) with increasing Zn rates. 1240 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 Table 3. Effect of soil, Zn rates (with equation and determination coefficient - R2) and interaction soil versus Zn rates in concentration of elements (Zn, Fe, Mn, Cu and Al) for maize grown in Ferralsol and Cambisol Maize fraction Soil Soil x Zn Ferralsol Cambisol Equation R2 Equation R2 Zn R ns ns y = 35.6 + 23.0x 0.95** y = 38.7 ns SN ns * y = 68.7 - 152.9x + 108.7x 2 0.98* y = 27.5 + 105.1-8.30*x 0.86* SI ns ns y = 89.5 - 67.2x 0.97* y = 74.4 - 168x + 111x2 0.96* L ns ns y = 23.7 ns y = 26.6 ns SL ns ns y = 24.8 ns y = 28.6 ns Fe R * ns y = 1696 ns y = 1501 - 803.8x 0.90** SN * ns y = 1024 - 959.1x 0.79** y = 751.3 - 732.1x 0.67** SI * ns y = 807 -858x 0.72** y = 543 - 1628x + 1109x2 0.93** L * * y = 593.8 - 556.1x 0.91** y = 931.5 - 934.6x 0.80** SL ns ns y = 316.5 - 265.1x 0.83** y = 366.4 - 308.8x 0.71** Mn R * ns y = 15.9 ns y = 19.1 - 38.6x + 29.6x2 0.97** SN * ns y = 25.8 - 21.6x 0.84** y = 18.4 - 17.4x 0.82** SI * ns y = 33 ns y = 50.2 - 149x + 105x2 0.87* L ns ns y = 94.7 - 77.1x 0.89** y = 133.4 - 313.2x + 194.8x2 0.98** SL * * y = 16.8 ns y = 34.6 - 79.6x + 59.6x2 0.89** Cu R ns ns y = 18.4 + 11.4x 0.98** y = 19.2 ns SN ns * y = 35.1 - 69.4x + 43.2x 2 0.96** y = 13.1 + 75.9 -6.95*x 0.94** SI ns ns y = 51.8 ns y = 43.1 - 112x + 78x2 0.98** L ns ns y = 33.8 - 67.8x + 44.3x 2 0.97** y = 39.9 -1.63*x 0.74* SL ns ns y = 20.9 - 38.4x + 27.2x 2 0.98* y = 23.2 - 48.1x + 30.8x2 0.91* Al R ns ns y = 297 ns y = 347.0 - 161.4x 0.79* SN ns * y = 168.8 - 349.1x + 221.1x 2 0.99* y = 32.7 + 426.9 -11.31*x 0.99** SI ns ns y = 352 - 278x 0.92** y = 163 - 434x + 300x2 0.95** L ns ns y = 19.2 + 37.8 -7.18*x 0.96* y = 15.4 + 42.5 -11.46*x 0.97* SL * * y = 26.4 ns y = 26.6 + 62.6 -12.85*x 0.99** R, root; SN, stalk nodes; SI, stalk internodes; L, leaves; SL, sheath leaves; ns = not significant; * = Significant at 5%; ** = Significant at 1%. In addition, the reverse may also occur, for example, the lack of Fe increases Zn levels in maize, as evidenced by Kanai et al. (2009). (ii) the maize also boots the release of other chemicals in the rhizosphere, such as organic acids, enzymes, amino acids, gaseous molecules and H+ and OH-; that vary with nutritional status and may increase or reduce the acquisition of certain elements (BADRI; VIVANCO, 2009). (iii) the changes in C deposition via maize roots modify the microbial community in the rhizosphere and thus may indirectly be favored microorganisms that present an element solubilizing capacity (MARSCHNER, 2012). (iv) the occurrence of competition between ionic forms during uptake, interference with chelation process during uptake and translocation and the competitive inhibition during unloading in the xylem may also affect Zn interaction with other elements (WHITE, 2012; CHILIAN et al., 2015). In soil with higher Fe concentrations (Ferralsol) high concentrations of Fe were registered in the first fractions (roots, internode and stem node) of maize plants. However, the leaf Fe concentrations were lower in Ferralsol (Figure 3; Table 3). Thus, 1241 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 the soil was important to explain the variations of Fe in the roots, internodes and stalk nodes. However, variations in Fe in leaves indicate that the mechanisms related to Fe transport (BROADLEY et al., 2012) were more important than their availability in soil. Furthermore, high Fe concentrations in the first fractions of maize may have been favored by P deficiency in Ferralsol, considering that the P deficiency favors the exudation of low molecular weight organic acids (BADRI; VIVANCO, 2009). Compared to Ferralsol (Figure 3; Table 3), plants grown in Cambisol had lower Mn concentrations in stalk nodes, while concentrations in root, stem internodes and leaf sheath were higher. For Cambisol, higher Mn concentrations in most plant fractions indicates that they may be due to higher initial concentrations of Mn in this soil (Table 1), similar to what was observed for Fe. Furthermore, Cambisols present higher concentration of amorphous fractions or low crystallinity, with higher possibility of being solubilized by organic acids released by the roots. However, the more general difference between Mn and Fe was the distribution of elements in the tissues because the Mn showed higher concentrations in the leaves and stalk internodes, whereas the Fe showed higher concentrations in root and stalk nodes. The Fe showed a natural trend to accumulate in the roots. However, in the aerial part, the Fe showed a natural trend to accumulate in the stalk nodes, since it was the only element for which the concentration in the nodes was always higher than in internodes, regardless of the soil and the Zn rates (Figure 3; Table 3). This was confirmed via the concentration of Fe in stalk nodes being 40% to 470% (based on concentration) and 175% to 700% (based on content) higher than in the internodes (Figure 4). Fe Zn Mn Cu Al P K Ca Mg D if fe re n ce ( % ) -100 0 100 200 300 400 500 0.125 mg Zn kg-1 0.25 mg Zn kg-1 0.5 mg Zn kg-1 1.0 mg Zn kg-1 A * *** * * ### Fe Zn Mn Cu Al P K Ca Mg D if fe re n ce ( % ) -100 0 100 200 300 400 500 C * Fe Zn Mn Cu Al P K Ca Mg D if fe re n ce ( % ) 0 200 400 600 800 D *** * Fe Zn Mn Cu Al P K Ca Mg D if fe re n ce ( % ) 0 200 400 600 800 B * * * *** * Figure 4. Difference (%) of Fe, Mn, Cu, Zn, P, K, Ca and Mg in the stalk nodes in comparison to stalk internodes of maize grown in Ferralsol (A and B) and Cambisol (C and D) with increasing Zn rates. Based on concentration (A and C) and content (B and D). * All Zn rates present significant difference (LSD test; p<0.05). # Only three Zn rates. Corroborating with the results of this study, Brown and Holmes (1955) using radioactive Fe, observed its preferential accumulation in maize stalk nodes compared to internodes, and in Cu deficient plants this buildup was intensified. The most probable explanation for this fact was presented by Shane et al. (2000) who indicated that for maize, vascular bundles were in axial internodes, while stalk nodes were in axial and transversal. This made the node areas highly congested with vascular bundles and approximately 97% of the axial vessels being interrupted by end walls in the area. In addition, these end walls have a low porosity (<20 nm) on the basis of nodes and between axial and transverse vessels within the nodes, acting as a filter. In the stalk of maize plants grown in soil with 1242 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 high concentrations of available Fe, Sayre (1930) observed accumulation of this element in the form of dark-colored crystals, especially in the nearby cells of the vascular bundles. McClean et al. (2001) reported Fe accumulation in leaves and stems of grass (Festuca spp.) as crystals of magnetite [Fe3O4], ɛ-Fe2O3, hematite [α-Fe2O3] and calcium ferrate hexahydrate [3CaO.Fe2O3.H2O]. Similarly, Rodríguez et al. (2005) found Fe-crystals inside Imperata cylindrica (L.) Rauschel (grass) cultivated in soil with high Fe availability, corresponding to 50% of jarosite [KFe3(SO4)2(OH)6]. Thus, it is possible that the higher Fe, resulting from Zn deficiency (Figure 2), may also provide conditions for the Fe precipitation and the consequent darkening of nodes. In the case of Ferralsol, it found that the darkening of the stalk nodes occurred even with the addition of Zn (although to a lesser degree), which should have been favored by the deficiency of P and higher Fe levels in stalk nodes for this soil. Contrary to that expected and observed for plant growth, the leaf Zn concentration did not change as result of its addition (Figure 3A, F; Table 3). A difficulty to associate Zn leave concentration and maize yield was observed by Ritchey et al. (1986) who applied 3 kg ha-1 of Zn and observed a twofold yield increase with no significant change in Zn, three years in row. The same problem has been observed by Hiatt and Massey (1958) under controlled conditions, who found severe, middle and no deficiency symptoms for maize leaves with 18, 9 and 16 mg kg-1 Zn, without, low and normal Zn supply via nutritive solution. Zare et al. (2009) observed that variations in Zn concentrations in maize leaves, with and without deficiency, were dependent on the soil type, allowing high or low levels in deficient plants. Correlations between the Zn and matter production (Table 4) failed (leaves) or showed negative values, as in stalk nodes (r = - 0.51), confirming the results presented above (Table 3). Thus, accumulation of Zn with in stalk nodes can indicate Zn deficiency. However, the balance between the Zn and other elements, represented by element/Zn ratios (P/Zn, K/Zn, Ca/Zn, Mg/Zn, Cu/Zn, Mn/Zn, Fe/Zn and Al/Zn) showed better than Zn alone in leaves, sheath leaves or stalk nodes. However, it is worth noting that the best results using element/Zn ratio occurred when the leaves were used as diagnostic tissue. These results corroborated with the proposal of Nambiar and Motiramani (1981) and Zare et al. (2009), who indicated the ratios as an alternative when Zn concentration in leaves fails to explain plant growth. Table 4. Pearson correlation for dry matter (DM) versus Zn concentrations or element/Zn ratio in leaves or stalk nodes of maize grown in Ferrasol and Cambisol with increasing Zn rates Zn P/Zn K/Zn Ca/Zn Mg/Zn Cu/Zn Mn/Zn Fe/Zn Al/Zn All data (Ferralsol + Cambisol) Leaves -0.33 -0.02 -0.14 -0.31 -0.09 -0.48 -0.76* -0.53* -0.33 Sheath leaves -0.16 -0.24 -0.62* 0.31 0.01 -0.62* -0.07 -0.53* 0.03 Stalk nodes -0.51* 0.07 -0.14 0.27 0.70* -0.25 -0.36 -0.42 0.17 Ferralsol Leaves -0.29 -0.57* -0.06 -0.52* -0.38 -0.62* -0.73* -0.64* -0.59* Sheath leaves 0.29 0.22 -0.50* -0.40 -0.45 -0.75* 0.09 -0.73* 0.31 Stalk nodes -0.53* 0.17 0.56* 0.40 0.76* -0.30 -0.42 -0.45 0.09 Cambisol Leaves -0.46 -0.28 -0.03 -0.11 0.01 -0.46 -0.88* -0.72* 0.33 Sheath leaves -0.54* -0.46 -0.58* 0.18 0.36 -0.85* -0.15 -0.60* -0.06 Stalk nodes -0.65* 0.06 -0.29 0.19 0.64* -0.35 -0.40 -0.37 0.00 * = significant at 1%. For leaves, the Mn/Zn (r = - 0.76) and Fe/Zn (r = - 0.53) ratios showed to be the best correlations to explain maize growth (Table 4). Since Zn application presented a large decrease in Fe in the plant tissue under Zn lack (RITCHEY et al., 1986; CHILIAN et al., 2015), the Fe/Zn ratio in maize 1243 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 leaves has been proposed as a diagnostic tool (NAMBIAR and MOTIRAMANI, 1981). The same authors and Zare et al. (2009) suggested that ratio values between 2 and 6 for Fe/Zn were the most suitable for maize cultivation. However, the highest correlation was obtained by Mn/Zn ratio in the leaves (Table 4) since its concentration gradually decreased due to Zn application. In a practical way, the plants showed good growth with a Mn/Zn ratio close to 0.95, while plants with low growth had a ratio close to 3.5. In addition, other fractions showed interesting results, such as the leaf sheaths (r = - 0.62) and stalk nodes (r = 0.70), with significant correlations for K/Zn and Cu/Zn, and Mg/Zn, respectively. In time, the soil also differed (Table 4), but only in Ferralsol was there significant correlation for P/Zn, Ca/Zn, Cu/Zn, Al/Zn (besides Fe/Zn and Mn/Zn), indicating that the changes caused in the ionome of maize leaves due to simultaneous deficiency of Zn and P in this soil favored more elements being correlated with the accumulation of dry matter. CONCLUSIONS In Zn-deficient plants we found reduced seedling growth, leaf necrosis (only Cambisol), interveinal chlorosis in new leaves, necrotic spots on the intermediate leaves, internode shortening and darkening of maize stalk nodes. P deficiency was also found in Ferralsol. The Zn deficiency increased Fe, Mn and Al concentrations in all maize plant parts in Cambisol, while in Ferralsol this did not happened for any of the elements analyzed. In both soils the darkening of maize stalk nodes was related to the preferential accumulation of Fe. Regarding nutritional diagnosis, the Zn concentrations in the stalk nodes correlate better with dry matter accumulation than in leaves or leaf sheaths. However, using the element/Zn ratios, there is an increase of the correlations using leaves, stalk nodes, and leaf sheaths. RESUMO: No Brasil, a deficiência de Zn é comum em solos utilizados para o cultivo do milho. Contudo, as mudanças na composição mineral das plantas resultantes da deficiência de Zn têm sido pouco estudadas. Assim, esse estudo objetiva avaliar a relação entre a deficiência de Zn e a composição mineral nas partes de plantas de milho cultivadas em solos contrastantes. O milho foi cultivado em casa de vegetação com doses crescentes de Zn (0; 0,125; 0,25; 0,5 e 1,0 mg kg-1) em dois solos (Latossolo e Cambissolo). Após 60 dias da emergência, as plantas foram fracionadas em raízes, nós do colmo, entrenós do colmo, folhas e bainha das folhas, sendo, posteriormente, determinadas a matéria seca e a composição mineral (P, Ca, Mg, K, Zn, Fe, Mn, Cu e Al). Além dos sintomas comumente descritos para deficiência de Zn, constatou-se escurecimento dos nós do colmo (relacionado ao acúmulo preferencial de Fe), sendo que no Latossolo também ocorreu deficiência de P. A deficiência de Zn favoreceu o aumento das concentrações de Fe, Mn e Al em todas as partes das plantas de milho no Cambissolo, enquanto que no Latossolo isso não ocorreu para nenhum dos elementos analisados. As relações entre os elementos e o Zn foram mais correlacionadas com a produção de matéria seca do milho que as concentrações de Zn em folhas, bainhas das folhas e nós do colmo. Pode-se inferir que a acumulação de minerais no milho foi favorecida pela deficiência de Zn, principalmente no Cambissolo. PALAVRAS-CHAVE: Zea mays L. Acumulação de Fe. Toxidez por metais. Disponibilidade de P. Nós do colmo. REFERENCES ALAM, S. M.; SHEREEN, A. Effect of different levels of zinc and phosphorus on growth and chlorophyll content of wheat. Asian Journal of Plant Sciences, Faisalabad, v. 1, p. 364-366, 2002. http://dx.doi.org/10.3923/ajps.2002.364.366 ALLOWAY, B. J. Zinc in soils and crop nutrition. 2 ed. Brussels: International Zinc Association & International Fertilizer Industry Association. 2008. 135p. BADRI, D. V.; VIVANCO, J. M. Regulation and function of root exudates. Plant, Cell and Environment, Malden, v. 32, n. 6, p. 666-681, 2009. http://dx.doi.org/10.1111/j.1365-3040.2009.01926.x 1244 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 BROADLEY, M.; BROWN, P.; CAKMAK, I.; RENGEL, Z.; ZHAO, F. Function of nutrients: micronutrients. In: MARSCHNER, P. (ed.). Marschner’s mineral nutrition of higher plants. Ed. 3. San Diego: Elsevier Science, 2012. p. 191-248. http://dx.doi.org/10.1016/B978-0-12-384905-2.00007-8 BROWN, J. C.; HOLMES, R. S. Iron, the limiting element in a chlorosis: Part I. Availability and utilization of iron dependent upon nutrition and plant species. Plant Physiology, Waterbury, v. 30, n. 5, p. 451-457, 1955. http://dx.doi.org/10.1104/pp.30.5.451 CHILIAN, A.; BANCUTA, R. O.; BANCUTA, I.; SETNESCU, R.; ION, R.-M.; RADULESCU, C.; SETNESCU, T.; STIHI, C.; GHEBOIANU, A. I.; CHELARESCU, E. D. Study of the influence of Zn concentration on the absorption and transport of Fe in maize by AAS and EDXRF analysis techniques. Romanian Reports in Physics, v. 67, n. 3, p. 1138-1151, 2015. GÉRARD, F. Clays minerals, iron/aluminum oxides, and their contribution to phosphate sorption in soils - A myth revisited. Geoderma, v. 262, p. 213-226, 2016. http://dx.doi.org/10.1016/j.geoderma.2015.08.036 HIATT, A. J.; MASSEY, H. F. Zn levels in relation to zinc content and growth of corn. Journal of Agronomy, Madson, v. 50, p. 22-24, 1958. Food and Agriculture Organization (FAO). World reference base for soil resources. Rome: FAO, 2006. 116p. KABATA-PENDIAS, A. Trace elements in soils and plants, 4th ed. London, New York: Taylor & Francis. 2011. 505 p. KANAI, M.; HIRAI, M.; YOSHIBA, M.; TADANO, T.; HIGUCHI, K. Iron deficiency causes zinc excess in Zea mays. Soil Science and Plant Nutrition, Tokyo, v. 55, p. 271–276, 2009. http://dx.doi.org/10.1111/j.1747- 0765.2008.00350.x MARQUES, J. J.; SCHULZE, D. G.; CURI, N.; MERTZMAN, S. A. Trace element geochemistry in Brazilian Cerrado soils. Geoderma, v. 121, n. 1-2, p. 31-43, 2004. http://dx.doi.org/10.1016/j.geoderma.2003.10.003 MARSCHNER, P. Rhizosphere biology. In: MARSCHNER, P. (ed.). Marschner’s mineral nutrition of higher plants. Ed. 3. San Diego: Elsevier Science, 2012. p. 369-388. http://dx.doi.org/10.1016/B978-0-12- 384905-2.00015-7 MCCLEAN, R. G.; SCHOFIELD, M. A.; KEAN, W. F.; SOMMER, C. V.; ROBERTSON, D. P.; TOTH, D.; GAJDARDZISKA-JOSIFOVSKA, M. Botanical iron minerals: correlation between nanocrystal structure and modes of biological self-assembly. European Journal of Mineralogy, Sttutgart, v. 13, p. 1235-1242, 2001. NAMBIAR, K. K. M.; MOTIRAMANI, D. P. Tissue Fe/Zn ratio as diagnostic tool for prediction of Zn deficiency in crop plants (in maize). Plant and Soil, Cham, v. 60, p. 357-367, 1981. http://dx.doi.org/10.1007/BF02149632 PUGA, A. P.; PRADO, R. M.; FONSECA, I. M.; VALE, D. W.; AVALHÃES, C. C. Ways of applying zinc to maize plants growing in Oxisol: effects on the soil, on plant nutrition and on yield. Idesia, Arica, v. 31, n. 3, p. 29-37, 2013. http://dx.doi.org/10.4067/S0718-34292013000300005 RITCHEY, K. D.; COX, F. R; GALRÃO, E. Z.; YOST, R. S. Disponibilidade de Zn para as culturas de milho, sorgo, e soja em Latossolo Vermelho-Escuro argiloso. Pesquisa Agropecuária Brasileira, Brasília, v. 21, n. 3, p. 215-225, 1986. RODRÍGUEZ, N.; MENÉNDEZ, N.; TORNERO, J.; AMILS, R.; FUENTE, V. Internal iron biomineralization in Imperata cylindrica, a perennial grass: Chemical composition, speciation and localization. The New Phytologist, v. 165, p. 781–789, 2005. http://dx.doi.org/10.1111/j.1469-8137.2004.01264.x 1245 Influence of zinc deficiency… DOMINGUES, C. R. S. et al. Biosci. J., Uberlândia, v. 32, n. 5, p. 1234-1245, Sept./Oct. 2016 RÖMHELD, V. The role of phytosiderophores in acquisition of iron and other micronutrients in graminaceous species: An ecological approach. Plant and Soil, Cham, v. 130, p.127-134, 1991. http://dx.doi.org/10.1007/BF00011867 SAYRE, J. D. Accumulated iron in the nodes of corn plants. Plant Physiology, Waterbury, v. 5, p. 393-398, 1930. http://dx.doi.org/10.1104/pp.5.3.393 SHANE, M. W.; MCCULLY, M. E.; CANNY, M. J. The vascular system of maize stems revisited: Implications for water transport and xylem safety. Annals of Botany, Oxford, v. 86, p. 245-258, 2000. http://dx.doi.org/10.1006/anbo.2000.1171 United States Department of Agriculture. USDA. Foreign Agricultural Service. World Agricultural Production. Circular Series. June 2016. 27 p. 2016. VITOSH, M. L.; WARNCKE, D. D.; LUCAS, R. E. Secondary and micronutrients for vegetables and field crops. East Lansing: Michigan State University. 1994. 18p. WHITE, P. J. Ion uptake mechanisms of individual cells and roots: short-distance transport. In: MARSCHNER, P. (ed.). Marschner’s mineral nutrition of higher plants. Ed. 3. Elsevier Science, 2012. p. 7-47. http://dx.doi.org/10.1016/B978-0-12-384905-2.00002-9 ZHAO, A. Q.; BAO, Q. L.; TIAN, X. H.; LU, X. C.; WILIAM, J. G. Combined effect of iron and zinc on micronutrient levels in wheat (Triticum aestivum L.). Journal of Environmental Biology, Vikas Nagar, v. 32, n. 2, p. 235-239, 2011. ZARE, M.; KHOSHGOFTARMANESH, A. H.; NOROUZI, M.; SCHULIN, R. Critical soil zinc deficiency concentration and tissue iron: zinc ratio as a diagnostic tool for prediction of zinc deficiency in corn. Journal of Plant Nutrition, Florence, v. 32, p. 1983-1993, 2009. http://dx.doi.org/10.1080/01904160903308101