Whole-plant mineral partitioning during the reproductive development of rice ( Oryza sativa L.)

Minimal information exists on whole-plant dynamics of mineral flow. Understanding these phenomena in a model plant such as rice could help in the development of nutritionally enhanced cultivars. A whole-plant mineral accumulation study was performed in rice (cv. Kitaake), using sequential harvests during reproductive development panicle exertion, grain filling, and full maturity stages in order to characterize mineral accumulation in roots, non-flag leaves, flag leaves, stems/sheaths, and panicles. Partition quotient analysis showed that Fe, Zn, Cu and Ni are preferentially accumulated in roots; Mn and Mg are accumulated in leaves; Mo, Ca, and S in roots and leaves; and K in roots, leaves and stems/sheaths. Correlation analysis indicated that changes in the concentrations of mineral pairs Fe-Mn, K-S, Fe-Ni, Cu-Mg, Mn-Ni, S-Mo, Mn-Ca, and Mn-Mg throughout the reproductive development of rice were positively correlated in all four of the above ground organs evaluated, with Fe-Mn and K-S being positively correlated also in roots, which suggest that root-to-shoot transfer is not driven simply by concentrations in roots. These analyses will serve as a starting point for a more detailed examination of mineral transport and accumulation in rice plants. to


Introduction
Plants are the primary source of nutrients for human nutrition. Staple seed crops such as rice (Oryza sativa L.) supply the majority of daily dietary nutrients for billions of people. However, rice has a low density of mineral nutrients, and for those whose diets are high in staple foods, micronutrient malnutrition is widespread (Kumar et al., 2016). To keep up with population growth and to improve the nutrition and health of rice consumers, the development of high-quality rice varieties becomes increasingly important (Duan & Sun, 2005). Biofortification, which consists of the use of plant breeding and/or transgenic approaches to develop new cultivars with the potential to increase the nutrient concentration of edible portions of crop plants (Sperotto et al., 2012a), has emerged as one possible solution to alleviate malnutrition.
Despite the increasing number of studies about the physiology and regulation of uptake of several minerals from the rhizosphere, such as potassium (Very & Sentenac, 2003), phosphorus (Raghothama & Karthikeyan, 2005), sulphur (Smith et al., 1997;Takahashi et al., 2000), iron (Curie & Briat, 2003), and zinc (Ghandilyan et al., 2006), the lack of knowledge about how minerals are moved into or out of vascular tissues, translocated to vegetative tissues and loaded into seeds is one of the barriers to seed biofortification (Colangelo & Guerinot, 2006;Sperotto et al., 2012a).
Uncovering mineral ion fluctuation in plants is a critical first step towards understanding the processes that regulate the plant's ion transport and accumulation. These studies involve the quantitative and simultaneous evaluation of the elemental composition of living organisms and the changes in this composition caused by physiological stimuli or developmental stage. In this way, ionomics has the ability to capture information about the mineral state of an organism under different tested conditions (Huang & Salt, 2016).
In this paper, we assessed growth dynamics of the whole plant (panicles, leaves, stems/sheaths and roots) over the period of reproductive development in rice. Leaf tissues were separated into non-flag and flag leaves, due to the known role of the flag leaf in the synthesis and translocation of photoassimilates to the rice seeds (Abou-khalifa et al., 2008), and due to the poorly understood role of each as a source of nutrients to the developing rice seeds . We also describe the accumulation of ten mineral nutrients (Fe, Zn, Cu, Mn, Mo, Ni, Ca, Mg, K and S) in these organs over time. All of these nutrients are essential to plant growth and participate in crucial metabolic pathways. Understanding mineral accumulation in rice organs is the first step to elucidate the puzzle of plant nutrient partitioning.

Elemental analysis by Inductively Coupled Plasma -Optical Emission Spectrometry (ICP-OES)
All tissues were harvested and dried in a 60° C oven for 48 h. Dried tissues were ground and 250 mg were predigested overnight in borosilicate glass tubes with 4 mL of redistilled 98.8 % HNO 3 . One milliliter of concentrated trace metal grade HClO 4 was added to the predigested tissues and heated at 100° C for 1 h, 150° C for 1 h, 180° C for 1 h and then at 210° C to dryness (1-2 h). Digestions were performed using a heating block (Model 1016, Tecator, Hoganas, Sweden) with an exhaust-collecting manifold. Digests were resuspended in 15 mL of redistilled 2 % HNO 3 . Concentrations of Fe, Zn, Cu, Mn, Mo, Ni, Ca, Mg, K and S were determined by inductively coupled plasma-optical emission spectroscopy (CIROS ICP Model FCE12; Spectro, Kleve, Germany). Tomato leaves and rice flour standards (SRM 1573A and 1568A, respectively; National Institute of Standards and Technology, Gaithersburg, MD, USA) were digested and analyzed along with the rice samples to ensure digestion efficacy. Mineral content was determined by multiplying each sample's concentration by dry weight.

Partition quotient calculation
To evaluate the partitioning of minerals within a rice plant during its reproductive development, changes in each tissue's content were normalized to changes in each tissue's weight, relative to the whole plant. The dry weight of each organ was calculated as a percentage of total plant weight at each time point, and mineral content of each organ was calculated as a percentage of total plant mineral content at each time point. Using these values, the normalized partitioning of each mineral within the plant was calculated by dividing each organ's percentage mineral content by its percentage dry weight, and multiplying by 100, which we refer to as the partition quotient (PQ), as described by Waters & Grusak (2008).

Statistical analysis
When appropriate, data were subjected to analysis of variance (ANOVA) and means were compared by the Tukey HSD (Honestly Significant Differences) (p ≤ 0.05). The Levene's test (for homogeneity of variance) was used prior to ANOVA. Data with unequal variances were subjected to Welch analysis and means were compared by the Dunnett-C test. Pearson's correlation analyses were carried out using two significance levels (p ≤ 0.05 and 0.01). All the statistical analyses were performed using the SPSS Base 19.0 for Windows (SPSS Inc., USA).

Growth dynamics
Organ-specific growth dynamics throughout the reproductive development of Kitaake plants are presented in Fig. 1. At all time points, stems/sheaths comprised most of the plant's mass, with panicles as the second largest organ during GF and FM stages. At the PE stage, a small dry weight of roots and a large dry weight of non-flag leaves and stems/sheaths were observed with a shoot/root ratio of 24.0. Thereafter, the shoot/ root ratios decreased to 18.9 and 18.3 at the GF and FM stage, respectively. At all stages, except PE, flag leaf was the tissue with the lowest mass, with an increase of only 5% from PE to GF and 36% from GF to FM (differences not statistically significant). Roots and panicles were the tissues with the highest percentage mass increases from PE to GF and from GF to FM stages, with 93 and 61% for roots, and 377 and 240% for panicles.

Mineral accumulation during the reproductive development of rice
Mineral concentrations of certain organs changed substantially during the reproductive development of Kitaake plants. In general, mineral content was closely associated with plant dry weight and accumulated throughout the experiment (Table S1 [suppl.]). Fe concentrations in roots decreased 46% from PE to GF and increased 30% from GF to FM stages. Such decrease in Fe concentration from PE to GF can be explained by an increase in root dry weight ( Fig. 1), since Fe content did not change significantly between PE and GF. Both the increases in dry weight ( Fig. 1) and Fe concentration are responsible for the increased root Fe content during FM stage (Table S1 [suppl.]). Opposite to roots but similar to each other, panicles, non-flag leaves and stems/sheaths showed a peak in Fe concentrations at GF, then decreased. Fe content mirrored the increase from PE to GF in non-flag leaves and stems/sheaths, then leveled off or increased from GF to FM, but did not decrease as concentrations did. This was particularly notable in panicles where the decrease in Fe concentration from GF to FM was offset by a large increase in dry weight, such that Fe content continued to rise notably throughout the time course. Flag leaf Fe concentration also increased from PE to GF, but then slightly increased again from GF to FM. The increase in Fe concentration combined with little to no increase in dry weight was mirrored with a continuous rise in Fe content over time (Table S1 [ The Zn concentration dynamics showed two different patterns in rice organs. First, in non-flag leaves, stems/ sheaths and roots, an increase in Zn concentrations was detected from PE to GF stages. The decrease in root Zn concentration from GF to FM resulted in no change in root Zn content at the last time point. Nonflag leaves showed similar Zn content dynamics, with increased content only from PE to GF stages (Table S1 [suppl.]). Second, flag leaves and panicles showed no significant increases in Zn concentrations throughout the reproductive development. As a result of slight increases in dry weight and Zn concentration from GF to FM stages (both not statistically significant), flag leaf Zn contents showed a significant increase at the last time point. Due to the high increase in panicle dry weight during the reproductive development of rice ( Fig. 1), panicle Zn content increased throughout the experiment (Table S1 [   The Cu concentrations in panicles, non-flag leaves and flag leaves increased from PE to GF then maintained similar values from GF to FM. When combined with consistent increases in dry weight over both time periods, Cu contents in these organs increased throughout the PE to FM stages. Stems/sheaths showed a constant increase in Cu concentration, dry weight, and content throughout the experiment. In contrast, roots showed a 3-fold increase in Cu concentration from PE to GF, followed by a sharp decrease from GF to FM, resulting in no net change in root Cu content (Table S1 [suppl.]).
The Mn concentrations and contents showed a more consistent pattern among the analyzed organs, except for roots. In all organs other than roots, an increase in Mn concentrations from PE to GF was seen, followed by a decrease from GF to FM stages. Roots, in contrast, showed reduced Mn concentrations from PE to GF. In spite of the opposite change in concentrations, due to dry weight increases, Mn contents increased from PE to GF stages in all the five organs (Table S1 [ The Mo concentrations in roots and panicles showed a decrease from PE to GF followed by a slight increase from GF to FM. Stems/sheaths showed a similar increase in Mo concentration from GF to FM; but did not undergo the initial decrease in Mo. In contrast, flag leaves decreased in Mo concentration from PE to GF, while non-flag leaves showed no change in Mo concentration throughout the experiment. In spite of these variable patterns in Mo concentrations between organs, the pattern of Mo content was similar in all the organs analyzed, with an increase from PE to FM stages (Table S1 [suppl.]).
Four out of the five analyzed organs showed the same pattern of Ni concentration and content. Except in flag leaves, all the other organs showed that Ni concentrations and contents increased from PE to GF, then decreased from GF to FM stages. In flag leaves, there was a constant increase in both concentration and content of Ni throughout the experiment (Table S1 [ The macronutrients Ca, Mg, K and S showed similar concentrations and contents dynamics. In non-flag leaves, flag leaves and stems/sheaths, these mineral concentrations and contents tended to increase over the reproductive development. In panicles, only mineral contents increased over the experiment. The same was seen in roots, except for Ca. Roots during GF stage showed extremely low values of Ca concentration and content, with a subsequent increase at the FM stage (Table S1 [ To search for relationships among the ten mineral's concentrations through the reproductive development of rice plants, Pearson's correlation analyses were performed for the individual tissues. As seen in Fig.  2c, flag leaf was the organ with the highest number of positive correlations between elements, because most of the minerals showed an increase from PE to GF with little or no increase from GF to FM stages. Zn differed from the other nine elements by showing instead a (nonsignificant) reduction in flag leaf concentration from PE to GF. Root was the only organ in which negative correlations were found (Fig. 2e). In this organ, Fe was positively correlated with Mn and Mo, and negatively correlated with Cu and Ni. Zn and Cu (positively correlated to each other) were both negatively correlated to Mg and Ca. While several minerals were significantly correlated within each of the five organs, only two pairs of minerals were positively correlated in every organ analyzed: Fe-Mn and K-S, although Fe-Ni, Cu-Mg and Mn-Ni were positively correlated in four of the five organs, but showed a negative correlation in roots (Fig. 2), while S-Mo, Mn-Ca, and Mn-Mg were also positively correlated in all four above-ground tissues, but were not significantly correlated (neither positive nor negative) in the roots.
A PQ value, representing the proportional mineral content in an organ relative to the proportional dry weight of that organ, was calculated to allow comparison of the dynamics of partitioning of minerals throughout the reproductive development of rice plants regardless of differences in plant size, and to check if the contents of minerals are relatively higher in one specific organ. When the percentage contribution of the organ to the plant's dry weight is the same as the percentage contribution to the plant's total content of the mineral being evaluated, the PQ value is equal to 100. As seen in Fig. 3, roots were the organs with the highest PQ values, except for Mn (Fig. 3d) and Mg (Fig.  3h); panicles showed the lowest values, reaching over 100 only for Zn (Fig. 3b) and Ni (Fig. 3f) during the first time point (panicle exertion). PQ for Fe (Fig. 3a) and Cu (Fig. 3c) were similar, with root PQ consistently 5-fold, and as much as 10-fold larger than PQ for all other organs. For Mn (Fig. 3d), Mo (Fig. 3e), Ca (Fig.  3g), Mg (Fig. 3h) and S (Fig. 3j), PQ values increased during the time periods in non-flag and flag leaves, reaching values > 200, and up to 300 for Ca. Stems/ sheaths PQ values tended to increase throughout reproductive development for almost all the minerals, however, only K had PQ values above 100 at all three time points (Fig. 3i).

Discussion
In this study, we characterized organ-specific changes in dry matter and essential mineral (Fe, Zn, Cu, Mn, Mo, Ni, Ca, Mg, K and S) contents and concentrations to monitor the net flow of minerals into and through the rice plant over reproductive development. Each of these nutrients has a critical function in plants and is required in varying amounts among different plant tissues.

Growth and mineral dynamics -single element
According to our analysis, three different patterns of mineral accumulation could be detected during the rice plant's reproductive development (Table S1 [suppl.] and Fig. 3). First, Fe, Zn, Cu and Ni were preferentially accumulated in roots. Silveira et al. (2007) also detected higher Fe levels in roots than in shoots of different rice cultivars. Fe is mainly required for photosynthesis, respiration, sulphate assimilation, hormone synthesis, nitrogen fixation, as well as DNA synthesis and repair (Puig et al., 2007;Sperotto et al., 2010). A large portion of the Fe in plants is in the apoplast, particularly in the roots. Most of this apoplastic pool is in the basal roots and older parts of the root system (Römheld & Nikolic, 2007). We found Fe PQ values of about 100 in nonflag and flag leaves (Fig. 3a). It is already known that a significant proportion of Fe is also localized within the chloroplast of rapidly growing leaves (Marschner, 1995), mainly as ferritin, which also occurs in seeds, where it can serve as an Fe source that is degraded during germination, as shown in pea (Lobréaux & Briat, 1991). However, in general, concentration of Fe in seeds is lower than in the vegetative organs (Römheld & Nikolic, 2007), corroborating our extremely low Fe PQ values in panicles (Fig. 3a). Under different external Fe supplies, Sperotto et al. (2012b) showed that Fe remobilization from vegetative tissues to the rice seeds can occur, but is greatly dependent on Fe supply. In Fesufficient conditions, the seed Fe seems to be largely fulfilled by continuous root uptake and direct xylem transport (Sperotto, 2013), which corroborates the decrease in Fe PQ levels detected in roots from PE to the following stages (Fig. 3). Zn PQ values decreased in roots throughout the reproductive development of rice, along with Zn PQ values from non-flag leaves (Fig. 3b). Under sufficient Zn supply, most of the seed Zn comes from root uptake and direct xylem transport, and is also transported via phloem from leaves and stems/sheaths (Impa et al., 2013). Surprisingly, Zn PQ values increased in stems/ sheaths. There are numerous reports of the temporary accumulation of Zn in stems (Ruano et al., 1987;Simmons et al., 2003). In panicles, Zn PQ values were higher in PE than in GF and FM stages. The highest seed Zn concentration following foliar Zn applications in wheat was reported at the beginning of seed development (around 10 days after anthesis or around the early milky stage), suggesting that applying foliar Zn during early stages of wheat reproductive development could be an effective way of increasing seed Zn concentration through efficient flag leaf export to the grain (Ozturk et al., 2006). Indeed, it has been shown that high Zn accumulation during early seed development is possibly related to protein synthesis (Martre et al., 2003). Zinc is a key structural component of a large number of proteins, and the most critical micronutrient affecting protein synthesis in plants (Obata et al., 1999). It has important functions in enzymatic activity, in transcription factors, and is a cofactor in more than 300 proteins (Palmgren et al., 2008;Ricachenevsky et al., 2015). It is important to highlight that Zn was the only element with PQ values around 100 in panicles during FM stage. Wu et al. (2010) showed that large amounts of the Zn in rice seeds at maturity had been translocated from other plant parts, and not directly acquired by the roots. In addition, Zn from upper leaves can be remobilized to the seeds (Sperotto, 2013), which could explain, at least in part, the decrease in Zn PQ values in roots and nonflag leaves during the reproductive stage (Fig. 3b).
Copper is involved in crucial processes including ethylene perception, cell wall metabolism and oxidative stress protection (Puig et al., 2007). Also, a role for Cu in molybdenum cofactor biosynthesis has been reported (Kuper et al., 2004). Cu has limited transport in plants; therefore, the highest concentration is often in root tissue (Chaignon et al., 2002a,b). Analysis of 16 different forage species revealed that root tissues accumulated the highest Cu concentrations (28.8 mg/ kg), followed by leaves (15.5 mg/kg) and stems (8.4 mg/kg) (Pederson et al., 2002). A similar pattern was found in our work, with concentrations ranging from 40 to 149 mg/kg in roots, 8 to 15 mg/kg in leaves, and 5 to 9 mg/kg in stems/sheaths.
Nickel is very important for certain enzyme activities, maintaining proper cellular redox state and various other biochemical, physiological and growth responses (Yusuf et al., 2011). Also, Ni is part of the active site of the enzyme urease, which catalyzes the hydrolysis of urea to ammonia and bicarbonate (Polacco et al., 2013). Ni distribution in plants depends on their developmental stage. In accordance with our results in rice, the highest Ni concentrations in roots of Avena sativa were registered at the tillering and booting stages (Andreeva et al., 2000). Also similar to our results, Dwivedi et al. (2007) found that most of the Ni was confined to roots in all the three tested rice cultivars, despite the known high mobility of Ni through xylem tissues of shoots and its high transport capacity from root to shoot (Krämer et al., 1996).
The second pattern of mineral accumulation during the reproductive development of rice was seen for Mn and Mg, which are mostly accumulated in leaves (Table  S1 [suppl.] and Fig. 3). Manganese is an essential plant micronutrient with an indispensable function as a catalyst in the oxygen-evolving complex of photosystem II (Schmidt et al., 2016). Mn also serves as a cofactor in essential processes such as photosynthesis, lipid biosynthesis and oxidative stress (Socha & Guerinot, 2014). Mn passively moves from the root to the shoot in the xylem-sap transpirational stream (Ramani & Kannan, 1987). In contrast, re-translocation within the phloem is complex, with leaf Mn being immobile, but root and stem Mn being able to be re-mobilized (Loneragan, 1988), which could explain high Mn PQ values in leaves and low Mn PQ values in roots and stems/sheaths. The net effect of the variable phloem mobility gives rise to a redistribution of Mn in plant parts typical of a nutrient with low phloem mobility (Humpries et al., 2007). Yet, according to Pearson & Rengel (1994), the Mn content of wheat leaves increases throughout grain development, corroborating our data.
Over 300 enzymes are known to be Mg-dependent, and changes in the Mg concentration significantly affects the membrane potential (Kobayashi & Tanoi, 2015), which can disrupt absorption and transport of nutrients. Also, Mg plays a central role in plant chlorophyll biosynthesis and carbon fixation as a cofactor of a series of enzymes involved in carbon metabolism (Guo et al., 2015). The amount of Mg accumulated differs among various plant organs, with a tendency towards greater allocation of Mg to transpiring organs such as leaves, rather than to roots (Drossopoulos et al., 1996). In cucumber, Mg concentration was seven times higher in shoots (70 µmol/g fresh weight) than in roots (10 µmol/g fresh weight) (Bengtsson & Jensen, 1983). Yet, Mg accumulation in the younger leaves of cucumber is higher after flowering and fruiting (Bengtsson & Jensen, 1983), which is in accordance to the flag leaf Mg PQ values obtained in our work (Fig. 3h).
The third pattern of mineral accumulation during reproductive development in rice was accumulation in multiple tissues, as seen for Mo, Ca, and S, which were accumulated in roots and leaves; and K, which was accumulated in roots, leaves and stems/sheaths (Table S1 [suppl.] and Fig. 3). The transition metal Mo is essential for plants as it is required by a number of enzymes that catalyze key reactions in nitrogen assimilation, purine degradation, phytohormone synthesis, and sulfite detoxification. Moreover, a tight connection between Mo and Fe metabolisms is presumed (Bittner, 2014). The allocation of Mo to the various plant organs varies considerably among plant species, but generally the concentration of Mo is highest in seeds (Gupta & Lipsett, 1981) and in the root nodules of N 2 -fixing plants (Marschner, 1995). On the other hand, in crop species such as tomato (Solanum lycopersicum L.), alfafa (Medicago sativa L.), and soybeans (Glycine max Merr.), Mo concentration in leaves has been found to exceed the concentration in stems (Gupta & Lipsett, 1981). According to our results (Table S1 [suppl.] and Fig. 3e), one more crop species (rice) can be added to this list.
Calcium is required for structural roles in the cell wall and membranes, as counter-cation for inorganic and organic anions in the vacuole and plays an essential role as intracellular messenger in the cytosol (Marschner, 1995). The concentration of cytoplasmic Ca in plant cells increases in response to various developmental conditions and environmental factors (Hochmal et al., 2015). Ca concentration, content and PQ values decreased in roots during grain filling stage (Table S1 [suppl.] and Fig. 3g). Most of this Ca content was probably transported to leaves, which accumulated more Ca during grain filling than during the panicle exertion stage (Fig. 3g). Ca moves readily into transpiring organs such as mature leaves (Clarkson, 1984). On the other hand, Ca xylem transport into organs that do not have a high transpiration rate is low (Kirkby & Pilbeam, 1984).
Sulphur is involved in different functions and aspects of plant metabolism (Briat et al., 2015). Sulphur is a vital component of proteins, due to its presence in the amino acids cysteine and methionine, as well as an active constituent of numerous coenzymes and prosthetic groups, Fe-S centers, coenzyme-A, thiamine, lipoic acid, S-adenosylmethionine, glutathione, and many more (Kopriva et al., 2015). Plant families and species show large variations in S concentration. In general, graminaceous species have lower S levels than dicotyledonous crops. Within each genus, however, species producing S-containing secondary metabolites accumulate more S than those without this capacity. We found higher S concentration in rice roots, although in general, photosynthetically active leaves show the highest S concentration of all plant organs (Haneklaus et al., 2007).
Potassium is indispensable to plant growth and contributes to the maintenance of membrane potential, ion homeostasis, and osmoregulation (Shin, 2014). It is also involved in enzyme activation, protein synthesis, photosynthesis, and stomatal movements (Luan et al., 2016). It is already known that K is taken up from the soil solution at high rates and is quickly distributed in plant tissues and cell organelles, owing to low-and high-affinity K channels (Glass, 1983). Potassium ions cycle via xylem from roots to upper plant parts and via phloem from leaves to roots. The direction of K movement depends on the physiological demand. However, for optimum grain filling, a high K concentration in leaves is required for the translocation of assimilates to the grains and for protein synthesis in these grains (Mengel et al., 1981).
Most of the mineral concentrations and PQ values decreased in panicles during the reproductive development (Table S1 [suppl.] and Fig. 3). This pattern is seen to varying degrees and is probably related to starch accumulation, which enhances panicle dry weight and dilutes mineral concentrations. It is important to highlight that the mobility of each mineral can certainly affect the remobilization level to developing seeds (Marschner, 1995). However, other factors such as ligation to chelators, number of seeds (sink strength), continued uptake by the roots, and different efficiencies in the use of nutrients (Sperotto, 2013) can influence seed mineral accumulation.

Growth and mineral dynamics -element interactions
It is important to note that several mineral concentrations are influenced by Fe supply in rice plants. Sperotto et al. (2012b) showed that low Fe supply (5 mM) lead to higher accumulation of Zn, Cu and Ni in roots, Mn, Ca, Mg and K in leaves and Zn in stems/ sheaths and a smaller accumulation of Fe, Mn and Ca in roots and Zn and Ni in leaves. On the other hand, high Fe supply (200 mM) promoted higher accumulation of Fe in roots and Zn in leaves, and a smaller accumulation of Fe in leaves and stems/sheaths, and Zn, Cu and K in roots.
Significant correlations were found among the concentrations of ten mineral elements through the reproductive development of rice. In particular, concentrations of Fe-Mn and K-S were positively correlated in every analyzed organ. Fe-Ni, Cu-Mg and Mn-Ni were positively correlated in four of the five organs, showing a negative correlation in roots (Fig.  2). Most of the correlation studies were made in brown or polished grains, instead of vegetative organs. Zeng et al. (2005) showed a significant positive correlation between Fe and Mn content in brown rice and Distelfeld et al. (2007) showed a clear association between Fe and Mn concentrations in wheat grains. Parida et al. (2003) observed that Fe contents in plants of Trigonella increased with the increase in the Ni concentration applied and Yang et al. (1996) reported a significant negative correlation between Ni concentration in roots and Fe and Mn influx in roots of cabbage (Brassica oleracea L.) and Mn influx in roots of maize (Zea mays L.). Zeng et al. (2005) showed a significant positive correlation between Cu and Mg in brown rice. In a study using young spinach (Spinacia oleracea L.), where Cu concentration in nutrient solutions was increased from zero to 10 mg/L, Cu toxicity symptoms did occur, and there was a significant suppression in Mg accumulation in the roots from 372 mg/kg to 203 mg/kg (Ouzounidou et al., 1998). Sperotto et al. (2012b) reported that Cu and Mg were positively correlated in four of the five rice organs tested under different Fe supplies. Positive correlation between Fe and Zn concentrations, found in three of the five analyzed tissues (Fig. 2), was previously reported in rice grains by our group (Sperotto et al., 2009).
As previously stated by Baxter et al. (2012), the physiological and molecular drivers of mineral responses and the rules governing the relationship between many elements are far from clear. One method to search for a better understanding of these rules is to look at plant mineral dynamics not only at a whole plant level but also at the individual organ level. This, coupled with studies looking at the expression of genes encoding transporters, channels, chelators and transcription factors, will ultimately reveal the rules that govern nutrient uptake, distribution and storage.
Our findings indicate when and where minerals are accumulated in this specific rice cultivar under artificial aerated hydroponic growth conditions during the entire reproductive stage. Correlation analyses are also important to future studies, since they provide information about which minerals show the same concentration pattern during the reproductive stage, which can be useful for future biofortification strategies aiming for simultaneous mineral increases in rice plants.