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Article

Spatial and Temporal Calcium Signaling and Its Physiological Effects in Moso Bamboo under Drought Stress

International Center for Bamboo and Rattan, State Forestry and Grassland Administration Key Laboratory of Bamboo and Rattan, Beijing 100102, China
*
Author to whom correspondence should be addressed.
Forests 2019, 10(3), 224; https://doi.org/10.3390/f10030224
Submission received: 25 January 2019 / Revised: 21 February 2019 / Accepted: 22 February 2019 / Published: 2 March 2019
(This article belongs to the Special Issue Physiological Responses to Abiotic and Biotic Stress in Forest Trees)

Abstract

:
Elevations in cytosolic free calcium concentration constitute a fundamental signal transduction mechanism in plants; however, the particular characteristics of calcium ion (Ca2+) signal occurrence in plants is still under debate. Little is known about how stimulus-specific Ca2+ signal fluctuations are generated. Therefore, we investigated the identity of the Ca2+ signal generation pathways, influencing factors, and the effects of the signaling network under drought stress on Phyllostachys edulis (Carrière) J. Houz. Non-invasive micro testing and laser confocal microscopy technology were used as platforms to detect and record Ca2+ signaling in live root tip and leaf cells of P. edulis under drought stress. We found that Ca2+ signal intensity (absorption capacity) positively correlated with degree of drought stress in the P. edulis shoots, and that Ca2+ signals in different parts of the root tip of P. edulis were different when emitted in response to drought stress. This difference was reflected in the Ca2+ flux and in regional distribution of Ca2+. Extracellular Ca2+ transport requires the involvement of the plasma membrane Ca2+ channels, while abscisic acid (ABA) can activate the plasma membrane Ca2+ channels. Additionally, Ca2+ acted as the upstream signal of H2O2 in the signaling network of P. edulis under drought stress. Ca2+ was also involved in the signal transduction process of ABA, and ABA can promote the production of Ca2+ signals in P. edulis leaves. Our findings revealed the physiological role of Ca2+ in drought resistance of P. edulis. This study establishes a theoretical foundation for research on the response to Ca2+ signaling in P. edulis.

1. Introduction

Calcium ions (Ca2+) are a primary signaling element for diverse cell processes in response to environmental cues. Ca2+ is a vital regulatory molecule for response to stress in plant growth and development [1,2]. When plants are affected by various physical stimuli, such as temperature, drought, salt, light, gravity, or chemical substances, such as plant hormones and pathogenic inducers, extracellular and intracellular sources of calcium release Ca2+ into the cytoplasm through Ca2+ channels. The spatio-temporal activity of membrane-localized Ca2+ channels or transporters causes an increase in cytosolic free calcium ion concentration (Ca2+)cyt, resulting in specific signals [3,4]. Almost all of the extracellular stimuli can lead to changes in intracellular (Ca2+)cyt. However, different stress stimuli can lead to variations in the pattern of Ca2+ spatial-temporal changes. There are significant differences in time, frequency, amplitude, and regional distribution. Studies have illustrated that plants may rely on different forms of Ca2+ to reflect the specificity of different stimulation signals to achieve signal transduction [5].
Although Ca2+ signaling has been extensively studied in other gramineous plants, such as rice, little is known about the Ca2+ signal identities and functions of the clonal plant Phyllostachys edulis (Carrière) J. Houz. Therefore, a better understanding of the calcium signal characteristics of bamboo under drought stress is an important prerequisite for the study of clonal habits of bamboo using signal transduction methods.
At present, research has shown that root tip cells of P. edulis seedlings transport Ca2+ from the extracellular region, cell walls, nucleus, and other calcium stores under drought stress. With increased duration of drought stress, the distribution of and changes in Ca2+ will produce regular fluctuations [6]. The more pronounced the drought stress, the greater the Ca2+ distribution in the root tip. Exogenous application of calcium fertilizer can relieve the physiological effects of drought stress and improve drought resistance in P. edulis [7]. Although roots constitute the most direct organ of water absorption, both Ca2+ uptake velocity and density of the different organ changed under drought stress [8]. Moreover, stomatal opening and closing behaviors were also regulated by Ca2+ signals at the cellular scale [9].
When there are no environmental pressures present, the majority of the Ca2+ in plant cells is distributed in the extracellular compartments, cell wall, vacuoles, and endoplasmic reticulum, with less concentrated distribution in the cytoplasm to prevent the precipitation of calcium and phosphoric acid [10]. To regulate this lower Ca2+ concentration in the cytoplasm, plant cells will actively export Ca2+. When a stimulus signal reaches a cell, plasma Ca2+ channels transiently increase Ca2+ permeability. When the cytoplasmic Ca2+ concentration increases to a certain threshold, it binds to calmodulin (CaM) to form Ca-CaM compounds, and thus activate CaM. Activated CaM further activates various key enzymes in the plant, which further phosphorylates and dephosphorylates phospholipase, nicotinamide adenine dinucleotide (NAD) kinase, and Ca2+-ATPase. In addition, it amplifies the initial stimulation signal and subsequently causes the cells to produce a physiological response corresponding to the signal, such as cell division, material synthesis, etc. [2,11].
Under drought stress, a complex signaling network is formed by a communication mechanism between regulatory signals. Ca2+ signaling can be combined with calcium receptors, such as CaM, to amplify the signal and transmit the oscillation to initiate stomatal closure and production of reactive oxygen species [12,13]. Previously, reactive oxygen species were considered toxic byproducts of plant metabolism. However, recent studies have shown that reactive oxygen species also have an important part to play in cellular signal transduction and regulation networks [14,15,16]. Abscisic acid (ABA) is a root chemical signal that plays an important role in regulating stomatal movement of plants under drought stress. H2O2 can be used as a downstream signal of ABA to activate Ca2+ channels in the plasma membrane. Involvement of ABA can induce stomatal closure by increasing Ca2+ concentration in guard cells [17]. Sha et al. used 25% PEG-6000 to simulate water stress in maize plants, inducing CaM gene expression in the leaves [18]. The study found that exogenous ABA treatment can also induce significant CaM gene expression, and that H2O2 is involved in ABA-induced CaM gene expression in the late regulation period.
The emergence of new technologies has made it possible to study changes in Ca2+ signaling in response to environmental stress in plants. Non-invasive microelectrode technology (NMT) and laser confocal microscopy are effective techniques for detecting Ca2+ signals. Antoine et al. demonstrated the influx of Ca2+ over the course of fertilization in maize with non-invasive microelectrode technology [19]. In addition, a live-cell Ca2+ imaging platform has been used to detect Ca2+ signals in the cytoplasm and nucleus of Arabidopsis thaliana (L.) Heynh. This technique was also used to observe the spatial-temporal distribution of Ca2+ in living cells of A. thaliana under stimulated adverse environmental conditions [20]. These studies use a method to generate Ca2+ signaling pathways by treating experimental materials with Ca2+ inhibitors. Ethylene glycol-bis (2-aminoethylether)-N,N,N’,N’-tetraacetic acid (EGTA), lanthanum chloride (LaCl3), and chlorpromazine (CPZ) are the most commonly used reagents. At present, laser confocal scanning microscopy has been used to study Ca2+ fluorescence localization in P. edulis cells under drought stress; however, most of these studies have been limited to the root tip [7] and few studies have been conducted on Ca2+ localization in cells located in the leaves of P. edulis using this technique.
To bridge this scientific gap, in this study we investigated the spatial-temporal location and flux velocity of Ca2+ ions by inducing drought stress in P. edulis with 20% PEG-6000. Using non-invasive micro-test technology (NMT) and laser confocal microscopy, we demonstrated the regularity of cellular Ca2+ dynamics in response to drought stress and provided measures of Ca2+ signaling in P. edulis leaf cells. We further studied the Ca2+ signaling pathway and analyzed the communication of the signal network pathway between Ca2+, H2O2, and ABA in leaf cells using Ca2+ inhibitors (Ca2+ channel blockers) and ABA. The aim of this study was to reveal the physiological role of Ca2+ in drought resistance and establish a theoretical foundation for the cellular response to Ca2+ signaling in P. edulis.

2. Materials and Methods

2.1. Plant Materials and Treatment

The sprouting seed materials used in this study were taken from the parent P. edulis from Guilin, Guangxi in September 2017. The thousand seed weight of these seed materials is equal to 22.75 ± 0.35 g. The P. edulis seeds were treated in November 2017. The seeds were soaked in warm water for 24 h at 50 °C, and then removed and disinfected with 5‰ potassium permanganate solution for 5 min. The sterilized seeds were then repeatedly washed with distilled water and germinated in an incubator in a dark environment set to a constant temperature of 25 °C. After the seeds germinated, the seedlings were selected for regular, even growth and placed in a Petri dish with pad disinfectant (lower layer) and filter paper (upper layer). The dishes were cultured at a constant temperature of 28 °C in an illumination incubator (PRX-1000B, Safe, Ningbo, China). The Petri dishes were set to point the roots vertically downwards. Proper humidity was maintained in the Petri dishes and any seeds found to be growing mold were removed. When the vertical root length reached approximately 3 cm, the seedlings were transferred to a Seed Germination Pouch (Phytotc CYG-98LB, size: 30 cm × 25 cm, Beijing Bioconsumable Tech., Ltd., Beijing, China) and cultured with a 12-h light period with a light intensity of 120–150 mmol m−2 s−1 and a temperature of 22 ± 2 °C. Figure 1 gives more details about the performance of the experimental materials.
For each experimental treatment, ten strains of P. edulis seedlings were selected in duplicate. To substitute drought stress, 20% polyethylene glycol-6000 (PEG, Coolaber, Beijing, China) was used for 5 min, 10 min, 15 min, and 30 min. Distilled water was used for the control (CK). In addition, Ca2+ inhibitors and ABA (Sigma-Aldrich, Shanghai, China) were used to treat P. edulis seedlings. The Ca2+ production pathway and its distribution were studied, and the effects of Ca2+ signaling on the H2O2/ABA signaling network were analyzed under drought stress. The Ca2+ inhibitors used in the experiment were extracellular Ca2+ chelating agent EGTA, Ca2+ channel blocker LaCl3, and CaM antagonist CPZ (Sigma-Aldrich, Shanghai, China). The dosage of additives was added according to the method of Lu [21].

2.2. Laser Confocal Microscopy Luminescence Imaging

Here, we present detailed instructions for laser confocal microscopy luminescence imaging of cytosolic Ca2+ and H2O2 concentration and distribution in root tip and leaf cells of P. edulis seedlings.

2.2.1. Esterified Fluorescent Probe Stock Solution Configuration

The calcium ion fluorescent probe Fluo-8 (AAT Bioquest, Sunnyvale, CA, USA) was fully dissolved in dimethyl sulfoxide (DMSO, Sigma-Aldrich, Shanghai, China) to a concentration of 1 mmol/L, −20 °C dark storage reserve.
2′,7′-dichloro fluorescin diacetate (H2DCFDA, Sigma-Aldrich, Shanghai, China) was made up of 50 mmol/L DMSO mother liquor, which was stored in a separate container and frozen.

2.2.2. Fluorescent Labeling

As to the root tip cells and leaf cells Ca2+ fluorescent labeling, we put the lower epidermis of the leaves of P. edulis seedlings flat on transparent tape and used a surgical blade to gently scrape the upper epidermis off the leaves. Then we placed the samples of lower epidermis in Hank’s balanced salt solution (without calcium ions) containing 20 μmol/L Fluo-8. We incubated them for 40 min in the dark at room temperature and rinsed the lower epidermis of P. edulis leaves with a buffer several times. We then incubated them again at room temperature for 20 min, ensuring that the esterification probe was fully dissolved. Finally we placed them on a glass slide and added 0.5 mL of Hank’s buffer to complete slice preparation.
As to the H2O2 fluorescent labeling of P. edulis leaf cells, the lower epidermis of P. edulis seedling leaves was first laid flat on transparent tape, and then the upper epidermis of the leaves was removed using a surgical blade and placed in MES, Free acid, monohydrate (Coolaber, Beijing, China) buffer to a final concentration of 50 μmol/L and incubated at room temperature in the dark for 15 min. We rinsed the lower epidermis samples several times with a buffer and placed them on glass slides. We then added 0.5 mL of buffer to complete slice preparation.

2.2.3. Laser Confocal Microscope Observation

Localization of Ca2+ fluorescence in P. edulis root tips and leaves: The prepared in vivo test slices were placed on a laser confocal microscope (LSM510, LeicaDM4, Berlin, Germany) for observation and scanning. Fluorescence intensity was controlled and all parameters were kept constant during the test (parameter settings: excitation wavelength 488 nm, BP 505-530, Pinhole 280, DG 581, AO 0.1, AG 1.34). At least three fields from different repeats were selected for each test. After the results were stable, one field of view was used for the analysis.
Localization of H2O2 fluorescence in root tips and leaves of P. edulis: The prepared in vivo test slices were placed on a laser confocal microscope (LSM510) for observation and scanning (parameter settings: excitation wavelength 488 nm, BP 505-530, Pinhole 386, DG 768, AO 0, AG 1). At least three fields from different repeats were selected for each test. After the results were stable, one field of view was used for analysis.

2.3. Measurement of Ca2+ Flux

Net Ca2+ flux was measured using non-invasive micro-test technology (Physiolyzer, Younger USA LLC, Amherst, MA 01002, USA; Xuyue (Beijing) Sci. & Tech. Co., Ltd., Beijing, China). NMT non-invasively measures Ca2+ fluxes with a high temporal and spatial resolution. It measures the concentration gradient of Ca2+ by means of selective microsensor oscillation between two points in the root tip of P. edulis seedlings (Figure 2).
After different test treatments, the roots were rinsed with redistilled water and immediately incubated in measuring solution to equilibrate for 10 min. Then, the roots were transferred to a measuring chamber containing 10−15 mL of a fresh measuring solution. Ions were monitored in the following solutions: 0.1 mM KCl, 0.1 mM CaCl2, 0.1 mM MgCl2, 0.5 mM NaCl, 0.3 mM MES, and 0.2 mM Na2SO4, following adjustment of the pH to 6.0. The measuring chamber was mounted on the micromanipulator, and the flux microsensor was positioned close to the root tip at four points: at the pileorhiza, meristematic zone, elongation zone, and mature zone (0 μm, 200 μm, 500 μm, and 800 μm from the root apex) of P. edulis seedlings.
The system setup parameters in the experiment are as follows. The Ca2+ flux microsensor (Φ4.5 ± 0.5 μm, XY-CGQ-01, Xuyue (Beijing) Sci. &Tech. Co., Ltd., Beijing, China) was filled with a backfilling solution (100 mM CaCl2) to a length of approximately 1.0 cm from the tip. The micropipettes were front filled with 40–50 μm columns of selective liquid ion-exchange cocktails (Ca2+ LIX, XY-SJ-Ca, YoungerUSA LLC, Amherst, MA, USA). An Ag/AgCl wire microsensor holder YG003-Y11 (Younger USA) was inserted in the back of the microsensor to make electrical contact with the electrolyte solution. YG003-Y11 (Younger USA) was used as the reference microsensor. Prior to the flux measurement, the flux microsensor was calibrated with a measuring solution having different concentrations of Ca2+ 0.1 mM and 0.01 mM. The electrodes with a Nernstian slope > 22 mV per decade were used in this study. Only the same flux microsensor was calibrated again according to the same procedure and standards after each test. Data was discarded if the post-test calibrations failed. The following figure shows the schematic and actual measurement of Ca2+ flux.
The data for Ca2+ fluxes were calculated by Fick’s law of diffusion as follows:
J = −D·(dc/dx)
where dx (30 μm) is the distance the flux microsensor moved repeatedly from one point to another perpendicular to the surfaces of the samples at a frequency of ca. 0.3 Hz.

2.4. Statistical Analysis

Data were analyzed by single factorial analysis of variance and statistical correlation analysis. The significance of differences among means was evaluated using the least significant difference test, with a family wise error rate of 0.05, using the Statistical Package for Social Sciences, v18.0 (SPSS Inc., Chicago, IL, USA). Significant differences are marked with alphabet.

3. Results and Discussion

3.1. Variation in the Flux and Distribution of Ca2+ among Different Parts of the Root Tips of P. edulis Seedlings under Drought Stress

The transient net Ca2+ flux was measured from different regions along the root axis using NMT in four different areas, the root apex and root hair zone, including pileorhiza, the meristematic zone, elongation zone, and mature zone (Figure 3a). Responses in the root apex Ca2+ flux are shown in Figure 3b. The results showed that there was a significant difference in the ability of P. edulis seedlings to absorb Ca2+ from different parts of the root tip after drought stress. The Figure 3b showed the most uptake of Ca2+ in pileorhiza. The pileorhiza was the area with the strongest Ca2+ signal response ability, and the Ca2+ concentration in the root pileorhiza was the highest. The elongation zone was the region with the strongest Ca2+ efflux. The intensity of Ca2+ uptake capacity at different parts of the root tip from strong to weak was: pileorhiza, mature area, meristematic zone, and elongation zone. The Figure 3c shows the fluorescence localization of P. edulis root tip cells by laser confocal microscopy. To better observe the distribution of Ca2+ in the pileorhiza, the corresponding heat map is shown in Figure 3d. Combined with Figure 3b, it can be concluded that there were differences in the responsiveness of different parts of the root tip of P. edulis to drought stress, which is reflected in both the Ca2+ flux and regional distribution.
We confirmed this difference in the results of Ying [7], which used laser confocal microscopy on fluorescence localization in the root tip. This study showed that Ca2+ absorption intensity in the elongation zone was weakest under drought stress, while Ying’s study showed that under drought stress, the Ca2+ in the root tip of P. edulis was mainly distributed in the pileorhiza and elongation zone; the distribution in the meristem area was relatively lower. This was due to the presence of a large number of small vacuoles in the cells of the elongation zone, which were not present in meristem zone. The vacuoles, as a calcium bank in plant cells, may provide a large amount of Ca2+ for P. edulis cytoplasm under drought stress. This leads to a greater concentration of Ca2+ in the elongate zone.

3.2. Effects of Drought Stress Duration on Ca2+ Absorption Regularity in the Pileorhiza of P. edulis

Under different durations of PEG-induced drought stress, we observed different conductivity, which represents leaf cell permeability (Figure 4a). An increase in drought stress duration caused electrolyte leakage in the cells, which in turn led to an increase in leaf conductivity. The cell membrane permeability of P. edulis seedlings increased, and there was a positive correlation between time and membrane permeability. The difference in conductivity increase between the 10- and 15-min treatments was higher than that in the 5–10 min period (difference in conductivity = 15.2%). The relative electrical conductivity of P. edulis seedlings under drought stress was 40.4% higher in the 30-min treatment than in the 15 min treatment. We observed significant correlation between Ca2+ flux and drought stress time (p < 0.01, Pearson correlation coefficient (r) = 0.967) (Figure 4b). All the flux data in Figure 4b represents stable and optimal real-time flux that can respond to Ca2+ concentration in response to drought stress. Relative to the control group, Ca2+ flux in pileorhiza of P. edulis seedlings gradually shifted from efflux to influx. Ten minutes of PEG treatment was found to be a “threshold”, after which efflux became influx. There was also a positive correlation between leachate conductivity and time as Ca2+ absorption intensity in the pileorhiza (p < 0.01, r = 0.976), and leaf membrane permeability increased.
Ca2+ flux in the pileorhiza of P. edulis seedlings in the control group (CK) maintained an out-of-range value of approximately 152 nmol m−2 s−1. Figure 5 showed that Ca2+ flux in the pileorhiza was only slightly changed in the experimental group after 5 min of PEG treatment, indicating that the slight degree of drought stress did not significantly induce the stress response leading to Ca2+ signaling in such a short time. When treated with PEG for 30 min, the Figure 5 shows a “V-shaped” pattern of ion uptake, with net flux first increasing and then decreasing. As drought stress time increased, Ca2+ flux gradually returned to control group standard of efflux. It is evident that there is a positive correlation between Ca2+ signal and drought stress time (Figure 5). Under drought stress, there is a “stress threshold” for the Ca2+ signal response. When the stress level reached this threshold, the Ca2+ flux at the pileorhiza underwent significant changes, which may be related to the plant’s ability to withstand drought stress.
Thirty minutes of PEG simulated drought stress showed obvious Ca2+ absorption in the pileorhiza, and Ca2+ flux oscillation increased. With the increase in the duration of drought stress, Ca2+ absorption increased. P. edulis seedlings were able to absorb Ca2+ from the extracellular environment under drought stress conditions, suggesting that while the intracellular calcium stores provide Ca2+ to the cytoplasm, Ca2+ absorbed from extracellular environment was also an important way to accumulate calcium signaling ions in the pileorhiza. It is suggested that Ca2+, as an important signaling molecule in response to drought stress, participated in the transmission of drought signaling to the roots of P. edulis seedlings.

3.3. Analysis of Ca2+ Signal Transport Patterns in the Pileorhiza of P. edulis under Drought Stress

The study of the Ca2+ signaling system in plant cells was mainly carried out by pretreatment of experimental materials with Ca2+ signal inhibitors [21]. Regulation of Ca2+ channels is vital. Plasma membrane Ca2+-permeable channels interact with Ca2+ activated nicotinamide adenine dinucleotide phosphate (NADPH) to form a self-amplifying system—a ROS-Ca2+ hub [22]. This system could provide the transduction and amplification of the initial Ca2+ or reactive oxygen species (ROS) stimuli into a more sustainable response, with implications for cell growth, hormonal signaling, and stress response [23,24]. To obtain further evidence of the role of plasma membrane Ca2+ channels in P. edulis root tips, different Ca2+ inhibitors and ABA were used to further determine the Ca2+ signaling pathways. Ca2+ signal intensity varied with time in the pileorhiza of P. edulis seedlings treated with LaCl3 (Ca2+ channel blocker), EGTA (extracellular Ca2+ chelating agent), and exogenous ABA.
To determine the factors affecting Ca2+ transport, Ca2+ flux in P. edulis root tip treated with a calcium antagonist and ABA was measured using NMT. As shown in Figure 6a, LaCl3 was applied to the P. edulis seedlings treated with PEG-induced drought stress. The LaCl3 treatment significantly impeded extracellular Ca2+ influx at the pileorhiza compared to the experimental group without LaCl3. Extracellular Ca2+ channels were involved in Ca2+ fluid transport. The extracellular Ca2+ in seedlings could enter cells through Ca2+ channels under drought stress, which was one of the reasons for the increase of cytoplasmic Ca2+ concentration.
In addition, EGTA was used to treat the roots of P. edulis seedlings under PEG-simulated drought stress. Ca2+ flux at the pileorhiza was almost always in a state of efflux (Figure 6b), while net Ca2+ flux of without EGTA treatment saw a pattern of "efflux-absorption-efflux". The EGTA-chelating extracellular Ca2+ increased, resulting in decreases of extracellular Ca2+ concentration and a decrease in the ability of pileorhiza to absorb Ca2+; this caused an increase in Ca2+ excretion. Ca2+ uptake in the pileorhiza with the addition of EGTA was significantly lower than in the CK. It is worth noting that treating the pileorhiza with EGTA and LaCl3 while under drought stress had the opposite effects on Ca2+ uptake curves. Ca2+ efflux rate from the pileorhiza of LaCl3 decreased as EGTA treatment increased. LaCl3 treatment hindered the Ca2+ channel in the pileorhiza, which led to a reduction of Ca2+ excretion from the pileorhiza.
Figure 6c shows Ca2+ absorption in the pileorhiza when treated with 30 μmol/L ABA for 10 min as PEG-induced drought stress treatment. Compared with the control, the ABA treatment showed a smaller oscillation in Ca2+ flux in the pileorhiza, and Ca2+ net flux reflected its strong absorption capacity. Therefore, ABA can promote the increase in Ca2+ absorption intensity in the pileorhiza of P. edulis seedlings. We conclude that ABA may activate the extracellular Ca2+ channel in the pileorhiza and promote Ca2+ uptake (Figure 6a,b). The efflux of ABA-induced Ca2+ spikes remained high among all treatments. These results further confirm that plasma membrane Ca2+ channels activity is involved in Ca2+ signaling in PEG-induced drought stress by controlling (Ca2+)cyt through Ca2+ influxes. Under drought stress, adding the Ca2+ channel blocker LaCl3 and extracellular Ca2+ chelating agent EGTA could significantly inhibit extracellular Ca2+ influx. Exogenous application of ABA could increase the ability of the pileorhiza to absorb Ca2+.

3.4. Analysis of Ca2+ Signaling Pathway in Leaves under Drought Stress

In addition to chemical signal root transduction, drought stress triggered Ca2+ movement in leaf cells. Ca2+ may regulate leaf stomatal movement to control transpiration and respiration, as a self-protection and adaption measure in response to environmental stress. To simultaneously monitor cell-specific Ca2+ P. edulis seedling leaves, we used a confocal microscope to record Ca2+ fluorescence localization (Figure 7).
CK is the Ca2+ fluorescence map of the lower epidermal cells treated with distilled water. Under normal water conditions, Ca2+ was mainly localized within the cell walls of guard cells, accessory cells, and long cells in P. edulis seedling leaves. Ca2+ was less commonly found to be distributed in the cytoplasm. As drought stress duration increased, Ca2+ concentration in the cytoplasm increased, except for in tethered cells. Among them, Ca2+ in long cells and guard cells increased significantly. The fluorescence intensity in the cytoplasm was also higher than that of the CK. Fluorescence intensity in the cytoplasm of accessory cells did not significantly increase. There were particularly pronounced differences in Ca2+ distribution in the 30 min PEG treatment. In addition to in tethered cells, the cytoplasmic fluorescence in all living cells, including guard cells, increased. Our results suggest that Ca2+ signals in response to PEG stress reflect distinct cellular Ca2+ dynamics.
With increased duration of drought stress, the fluorescence intensity in the cytoplasm of long cells increased. Only when a certain degree of drought stress was reached would Ca2+ in the cytoplasm of leaf guard cells escape from the cell wall and diffuse into the cytoplasm, resulting in a significant increase in the fluorescence intensity of the cytoplasm. In comparison, the Ca2+ in the cytoplasm of accessory cells was not obviously enhanced. To further verify that Ca2+ in the leaf cells of P. edulis was also transmitted through the cytoplasmic Ca2+ channels, three Ca2+ inhibitors were used to treat the seedlings under drought conditions. Ca2+ fluorescence localization under these conditions is shown in Figure 8.
To confirm the effect of calcium channels on Ca2+, we analyzed the Ca2+ fluorescence under three Ca2+ inhibitor treatments. The addition of CPZ inhibited the binding of Ca2+ to CAM in the seedlings; thus, the Ca2+ signal was not transmitted further. The results showed that after treatment with 0.1 mmol/L CPZ in the seedlings under PEG-simulated drought stress for 10 min, the brightness of the fluorescence in the cell wall and cytoplasm of the leaf cells was less than under the treatment without CPZ. Under drought stress, the Ca2+ in leaf cells of the P. edulis seedlings treated with 0.1 mmol/L CPZ were mainly distributed in the cell wall. The fluorescence brightness in the cell wall decreased more obviously than in other parts of the leaf.
We analyzed the distribution of Ca2+ in leaves treated with 3 mmol/L EGTA. Fluorescence intensity in the cell wall and cytoplasm reduced, indicating that Ca2+ concentration in the cell wall and cytoplasm decreased compared with the control group. This indicates that P. edulis seedling leaves can still take up Ca2+ from extracellular pathways under drought stress to produce calcium signals. Extracellular Ca2+ was chelated in the leaves under EGTA treatment, resulting in a decrease in extracellular Ca2+ uptake.
Treatment with LaCl3 prevents Ca2+ from extracellular entry, and Ca2+ in the cytoplasm of leaf cells significantly reduced. Ca2+ was mainly concentrated in the cell walls in this treatment (Figure 8). The results of Ca2+ fluorescence localization in leaf cells after treatment with 0.5 mmol/L LaCl3 for 10 min in drought-stressed P. edulis seedlings showed a decrease in Ca2+ fluorescence intensity in the cytoplasm of the cells. This was caused by the LaCl3 blocking the cytoplasmic Ca2+ channel, blocking extracellular Ca2+ entry through the cell wall. This shows that Ca2+ in the leaves of P. edulis can be transported through Ca2+ channels of the plasma membrane, absorbing Ca2+ from outside the cell, and using the potential difference to generate calcium signals.

3.5. Analysis of the Effects of Ca2+ Signals on H2O2 and ABA Signaling Pathways under Drought Stress

The H2O2 fluorescence localization map of P. edulis leaves is shown in Figure 9. H2O2 concentration in the leaf cytoplasm increased with drought stress time (Figure 9a). P. edulis seedling leaves treated with different Ca2+ inhibitors under PEG-simulated drought stress were subjected to laser confocal technology for H2O2 fluorescence localization to study the relationship between Ca2+ signaling and H2O2 in the stress signaling pathway (Figure 9b). Compared with CK, plants treated with 0.1 mmol/L CPZ showed lower leaf fluorescence, indicating that CPZ could also prevent H2O2 signal transduction. The calcium signals were unable to be transmitted normally, resulting in the decrease of H2O2 in the leaf cells. This indicates that the regulation of H2O2 activity requires the participation of Ca2+. Both 0.5 mmol/L LaCl3 and 3 mmol/L EGTA inhibited the production of H2O2 in guard cells, accessory cells, and long cells in leaves of P. edulis seedlings under drought stress. It is inferred that the Ca2+ signal is generated upstream of the active oxygen signal in the drought stress signaling network of P. edulis, and that H2O2 activity in leaf cells requires Ca2+ participation.
Laser confocal microscopy was used to detect the Ca2+ and H2O2 fluorescence signal in living leaf cells. The results indicated that the exogenous application of ABA under drought stress led to an increase in the concentration of Ca2+ and H2O2 in the mesophyll cells of P. edulis seedlings. Interestingly, there was a positive correlation between Ca2+ and H2O2 dynamics. ABA might activate Ca2+ channels of the plasma membrane and promote the production of Ca2+ signals in the pileorhiza of P. edulis seedlings.
H2O2 fluorescence intensity in guard cells was significantly higher in the ABA-treated group than in the group not treated with ABA (Figure 10). In plants, ABA is involved in many stress responses [25,26,27]. Regulatory systems of reactive oxygen species (ROS) are known to be integrated with other pathways involving Ca2+ signaling, protein kinases, and hormones pathways to regulate the defense mechanism in plants [28]. The existence of ABA-induced genes, which are expressed in stomatal guard cells, allows us to closely examine the role of Ca2+ [29]. In rice, the Ca2+/CaM-dependent protein kinase OsDMI3 has been shown to be required for ABA-induced antioxidant defense [30]. These results demonstrated that ABA also plays a key role in the signal transduction of Ca2+ in the signaling network of the leaves of P. edulis treated with drought stress. Ca2+ not only acted as the upstream signal of H2O2, but was also involved in the signal transduction process of ABA. ABA could promote the production of Ca2+ signaling in leaves and stimulate the burst of H2O2, a reactive oxygen species, in the guard cells. P. edulis may enhance drought tolerance via ABA-induced stomatal closure by ROS production.

4. Conclusions

This study indicated that the conductivity of P. edulis leaves increased with the degree of drought stress induced. Ca2+ is an important signaling molecule in response to drought stress in the root tip of P. edulis, especially in the transmission of stress signals and resistance to drought stress. Under drought stress, root tip cells of P. edulis can be used to transport Ca2+ from the extracellular environment to the cytoplasm, Ca2+ channels participate in extracellular Ca2+ transportation, and ABA may activate Ca2+ channels in the plasma membrane and promote Ca2+ signal production in the pileorhiza of P. edulis. In P. edulis leaves, Ca2+ can also be transported through the Ca2+ channels of the plasma membrane under drought stress, absorbing Ca2+ from outside the cell and generating Ca2+ signals through potential difference. The responsiveness of Ca2+ signals to drought stress in leaves of P. edulis from strong to weak was shown as follows: (1) long cells; (2) guard cells; (3) accessory cells; and (4) plug cells. Ca2+ acts as the upstream signal of H2O2 in the signal network of the mesophyll cells of the P. edulis under drought stress. It is also involved in ABA signal transduction process. ABA could promote Ca2+ signal production and stimulate H2O2 bursts in P. edulis leaves.
This study provides a method for the spatial and temporal localization of Ca2+ signaling and flux in P. edulis. Further research on Ca2+ signaling is essential, as it may help shed light on the physiology of P. edulis under stress. There are also areas for improvement in this study. The first is that processing the mesophyll samples may damage the cells or put them under stress conditions, thus affecting the Ca2+ fluorescence of the leaves under the laser confocal microscope. Autofluorescence of lignin can also have an effect on Ca2+ fluorescence. It is particularly important to improve this methodology in the future.

Author Contributions

X.J., C.C., and S.F. conceived and designed the experiments; X.J. performed the experiments; X.J. analyzed the data; L.W. and X.Z. contributed reagents/materials/analysis tools; X.J. wrote the paper, and C.C. revised it.

Funding

This research was funded by the International Centre for Bamboo and Rattan Center. Effects of Drought Stress on Water Physiology and Productivity of Phyllostachys edulis (grant number 1632018008).

Acknowledgments

The authors acknowledge the financial supports of the Foundation of International Centre for Bamboo and Rattan (No. 1632018008).

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. Cultivation of P. edulis sprouting seedlings.
Figure 1. Cultivation of P. edulis sprouting seedlings.
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Figure 2. Schematic diagram and measured photo of Ca2+ flux analysis by non-invasive micro-tests. The diagram is to demonstrate the principles behind NMT testing and is not to scale. The tip diameter of the microsensor is about 5 μm.
Figure 2. Schematic diagram and measured photo of Ca2+ flux analysis by non-invasive micro-tests. The diagram is to demonstrate the principles behind NMT testing and is not to scale. The tip diameter of the microsensor is about 5 μm.
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Figure 3. The flux and distribution of Ca2+ in different parts of Phyllostachys edulis root tips under drought stress. (a,b) Net Ca2+ fluxes in different parts of root tip of P. edulis seedlings under drought stress induced by 20% PEG for 10 min. At each position, an average Ca2+ flux was measured for 5 min before the electrode was repositioned (Data Repetition: 6 replicates). (c) Green fluorescence intensity is positively correlated with the Ca2+ concentration. The Ca2+ fluorescence localization at the root tip of the P. edulis seedlings treated with PEG-simulated drought stress for 10 min. (d) A heat map of a further analysis for (c), which clearly presented that the concentrated distribution of Ca2+ was in the pileorhiza of the P. edulis root tip cells under drought stress.
Figure 3. The flux and distribution of Ca2+ in different parts of Phyllostachys edulis root tips under drought stress. (a,b) Net Ca2+ fluxes in different parts of root tip of P. edulis seedlings under drought stress induced by 20% PEG for 10 min. At each position, an average Ca2+ flux was measured for 5 min before the electrode was repositioned (Data Repetition: 6 replicates). (c) Green fluorescence intensity is positively correlated with the Ca2+ concentration. The Ca2+ fluorescence localization at the root tip of the P. edulis seedlings treated with PEG-simulated drought stress for 10 min. (d) A heat map of a further analysis for (c), which clearly presented that the concentrated distribution of Ca2+ was in the pileorhiza of the P. edulis root tip cells under drought stress.
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Figure 4. Ca2+ flux of the pileorhiza cells of P. edulis seedlings under different durations of PEG-treatment. (a) The relative conductivity of leaves from P. edulis seedlings treated with PEG-simulated drought stress for 5 min, 10 min, 15 min, and 30 min (Data Repetition: 6 replicates). The control (CK) is represented by 0, which was a control group incubated with distilled water. The dashed curve (y = 0.0132x2 − 0.0406x + 0.2171, R² = 0.9615) represents the linear regression model for relative conductivity and PEG-simulated drought stress. (b) The depth of the red color represents the length of treatment time with 20% PEG simulating drought stress. From left to right in Figure 4b: the CK group, PEG-simulated drought stress treatment for 5 min, 10 min, 15 min, and 30 min, respectively. The flux data for each treatment in the figures reflected the steady-state real-time flux of maximum response to Ca2+ under drought stress (Data Repetition: 3 replicates); each segment of real-time data comprises flux data for three minutes.
Figure 4. Ca2+ flux of the pileorhiza cells of P. edulis seedlings under different durations of PEG-treatment. (a) The relative conductivity of leaves from P. edulis seedlings treated with PEG-simulated drought stress for 5 min, 10 min, 15 min, and 30 min (Data Repetition: 6 replicates). The control (CK) is represented by 0, which was a control group incubated with distilled water. The dashed curve (y = 0.0132x2 − 0.0406x + 0.2171, R² = 0.9615) represents the linear regression model for relative conductivity and PEG-simulated drought stress. (b) The depth of the red color represents the length of treatment time with 20% PEG simulating drought stress. From left to right in Figure 4b: the CK group, PEG-simulated drought stress treatment for 5 min, 10 min, 15 min, and 30 min, respectively. The flux data for each treatment in the figures reflected the steady-state real-time flux of maximum response to Ca2+ under drought stress (Data Repetition: 3 replicates); each segment of real-time data comprises flux data for three minutes.
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Figure 5. Changes in net Ca2+ flux in the pileorhiza of P. edulis seedlings after PEG-induced drought stress. Real-time Ca2+ flux by the pileorhiza of by PEG-induced drought stress for 5 min, 10 min, 15 min, 30 min, and CK, respectively (Data Repetition: 3 replicates).
Figure 5. Changes in net Ca2+ flux in the pileorhiza of P. edulis seedlings after PEG-induced drought stress. Real-time Ca2+ flux by the pileorhiza of by PEG-induced drought stress for 5 min, 10 min, 15 min, 30 min, and CK, respectively (Data Repetition: 3 replicates).
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Figure 6. Factor analysis of Ca2+ flux of P. edulis seedlings under drought stress (Data Repetition: 3 replicates). The white area represents Ca2+ oscillation in the pileorhiza after treatment of the P. edulis seedlings with distilled water (CK), and the black line graph in the blue area indicates the Ca2+ oscillation in the pileorhiza treated with 20% PEG-induced drought stress for 10 min. The red line in the blue region indicates Ca2+ oscillation under 0.5 mmol/L LaCl3 (a), 3 mmol/L EGTA (b), and 30 μmol/L ABA (c) in the 20% PEG treatment for 10 min.
Figure 6. Factor analysis of Ca2+ flux of P. edulis seedlings under drought stress (Data Repetition: 3 replicates). The white area represents Ca2+ oscillation in the pileorhiza after treatment of the P. edulis seedlings with distilled water (CK), and the black line graph in the blue area indicates the Ca2+ oscillation in the pileorhiza treated with 20% PEG-induced drought stress for 10 min. The red line in the blue region indicates Ca2+ oscillation under 0.5 mmol/L LaCl3 (a), 3 mmol/L EGTA (b), and 30 μmol/L ABA (c) in the 20% PEG treatment for 10 min.
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Figure 7. Localization of cellular Ca2+ dynamics in leaves of P. edulis seedlings. Calcium-fluorescence localization of the leaves of the P. edulis seedlings under drought stress for 5 min, 15 min, and 30 min induced by 20% PEG, respectively. The green fluorescence intensity represents the Ca2+ concentration and is positively correlated with the Ca2+ concentration.
Figure 7. Localization of cellular Ca2+ dynamics in leaves of P. edulis seedlings. Calcium-fluorescence localization of the leaves of the P. edulis seedlings under drought stress for 5 min, 15 min, and 30 min induced by 20% PEG, respectively. The green fluorescence intensity represents the Ca2+ concentration and is positively correlated with the Ca2+ concentration.
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Figure 8. Localization of cellular Ca2+ dynamics in leaves of P. edulis seedlings treated with different Ca2+ inhibitors and drought stress. Ca2+ fluorescence localization in leaves of plants treated with 20% PEG-induced drought stress and 0.1 mmol/L CPZ, 3 mmol/L EGTA, or 0.5 mmol/L LaCl3 for 10 min.
Figure 8. Localization of cellular Ca2+ dynamics in leaves of P. edulis seedlings treated with different Ca2+ inhibitors and drought stress. Ca2+ fluorescence localization in leaves of plants treated with 20% PEG-induced drought stress and 0.1 mmol/L CPZ, 3 mmol/L EGTA, or 0.5 mmol/L LaCl3 for 10 min.
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Figure 9. H2O2 fluorescence in P. edulis seedling leaves under drought stress. The green fluorescence intensity in the figure represents concentration of hydrogen peroxide, with more fluorescence indicating a higher concentration of H2O2. (a) H2O2 fluorescence localization at different treatment times (5 min, 15 min, and 30 min) using 20% PEG-induced drought stress. (b) The samples were treated with different Ca2+ inhibitors (CPZ, EGTA, and LaCl3) for 10 min under 20% PEG-induced drought stress.
Figure 9. H2O2 fluorescence in P. edulis seedling leaves under drought stress. The green fluorescence intensity in the figure represents concentration of hydrogen peroxide, with more fluorescence indicating a higher concentration of H2O2. (a) H2O2 fluorescence localization at different treatment times (5 min, 15 min, and 30 min) using 20% PEG-induced drought stress. (b) The samples were treated with different Ca2+ inhibitors (CPZ, EGTA, and LaCl3) for 10 min under 20% PEG-induced drought stress.
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Figure 10. Localization of fluorescence of Ca2+ and H2O2 in mesophyll cells after application of exogenous ABA under drought stress. (a) Calcium-fluorescence localization of leaves of P. edulis seedlings with distilled water. (b) Calcium-fluorescence localization of leaves of P. edulis seedlings under 20% PEG 6000-induced stress for 10 min. (c) Calcium-fluorescence localization of leaves of P. edulis seedlings with the application of 30μmol/L ABA to 20% PEG-induced stress for 10 min. (df) H2O2 fluorescence localization under the same treatment as above.
Figure 10. Localization of fluorescence of Ca2+ and H2O2 in mesophyll cells after application of exogenous ABA under drought stress. (a) Calcium-fluorescence localization of leaves of P. edulis seedlings with distilled water. (b) Calcium-fluorescence localization of leaves of P. edulis seedlings under 20% PEG 6000-induced stress for 10 min. (c) Calcium-fluorescence localization of leaves of P. edulis seedlings with the application of 30μmol/L ABA to 20% PEG-induced stress for 10 min. (df) H2O2 fluorescence localization under the same treatment as above.
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MDPI and ACS Style

Jing, X.; Cai, C.; Fan, S.; Wang, L.; Zeng, X. Spatial and Temporal Calcium Signaling and Its Physiological Effects in Moso Bamboo under Drought Stress. Forests 2019, 10, 224. https://doi.org/10.3390/f10030224

AMA Style

Jing X, Cai C, Fan S, Wang L, Zeng X. Spatial and Temporal Calcium Signaling and Its Physiological Effects in Moso Bamboo under Drought Stress. Forests. 2019; 10(3):224. https://doi.org/10.3390/f10030224

Chicago/Turabian Style

Jing, Xiong, Chunju Cai, Shaohui Fan, Lujun Wang, and Xianli Zeng. 2019. "Spatial and Temporal Calcium Signaling and Its Physiological Effects in Moso Bamboo under Drought Stress" Forests 10, no. 3: 224. https://doi.org/10.3390/f10030224

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