Grain Unloading of Arsenic Species in Rice

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Grain Unloading of Arsenic Species in Rice 1[W] Anne-Marie Carey, Kirk G. Scheckel, Enzo Lombi, Matt Newville, Yongseong Choi, Gareth J. Norton, John M. Charnock, Joerg Feldmann, Adam H. Price, and Andrew A. Meharg* Institute of Biology and Environmental Sciences, University of Aberdeen, Aberdeen AB24 3UU, United Kingdom (A.-M.C., G.J.N., A.H.P., A.A.M.); National Risk Management Research Laboratory, United States Environmental Protection Agency, Cincinnati, Ohio 45224 (K.G.S.); Centre for Environmental Risk Assessment and Remediation, University of South Australia, Mawson Lakes, South Australia SA–5095, Australia (E.L.); Cooperative Research Centre for Contamination Assessment and Remediation of the Environment, Salisbury, South Australia 5106, Australia (E.L.); GSECARS Advanced Photon Source, Argonne National Laboratory, Argonne, Illinois 60439 (M.N., Y.C.); Centre for Molecular Environmental Science, University of Manchester, Manchester M13 9PL, United Kingdom (J.M.C.); Council for the Central Laboratory of the Research Councils Daresbury Laboratory, Daresbury, Warrington WA4 4AD, United Kingdom (J.M.C.); and Department of Chemistry, University of Aberdeen, Meston Walk, Aberdeen AB24 3TU, United Kingdom (J.F.) Rice (Oryza sativa) is the staple food for over half the world’s population yet may represent a significant dietary source of inorganic arsenic (As), a nonthreshold, class 1 human carcinogen. Rice grain As is dominated by the inorganic species, and the organic species dimethylarsinic acid (DMA). To investigate how As species are unloaded into grain rice, panicles were excised during grain filling and hydroponically pulsed with arsenite, arsenate, glutathione-complexed As, or DMA. Total As concentrations in flag leaf, grain, and husk, were quantified by inductively coupled plasma mass spectroscopy and As speciation in the fresh grain was determined by x-ray absorption near-edge spectroscopy. The roles of phloem and xylem transport were investigated by applying a 6 stem-girdling treatment to a second set of panicles, limiting phloem transport to the grain in panicles pulsed with arsenite or DMA. The results demonstrate that DMA is translocated to the rice grain with over an order magnitude greater efficiency than inorganic species and is more mobile than arsenite in both the phloem and the xylem. Phloem transport accounted for 90% of arsenite, and 55% of DMA, transport to the grain. Synchrotron x-ray fluorescence mapping and fluorescence microtomography revealed marked differences in the pattern of As unloading into the grain between DMA and arsenite-challenged grain. Arsenite was retained in the ovular vascular trace and DMA dispersed throughout the external grain parts and into the endosperm. This study also demonstrates that DMA speciation is altered in planta, potentially through complexation with thiols. Paddy rice (Oryza sativa) is particularly effective, compared to other cereals, at accumulating arsenic (As) in shoot and grain (Williams et al., 2007b). Rice is the staple food for over half the world’s population (Fageria, 2007) and rice represents a significant dietary source of inorganic As, a class 1, nonthreshold carcin- ogen, particularly in Southeast Asia (Meharg et al., 2009). Inorganic As levels in rice grain are problematic even where soil As is at background levels, derived from geogenic sources (Lu et al., 2009; Meharg et al., 2009). However, widespread pollution of paddy soils with As, leading to further elevation of grain As, has occurred in some regions due to base and precious mining (Liao et al., 2005; Zhu et al., 2008), irrigation of paddies with As-elevated groundwaters (e.g. Meharg and Rahman, 2003; Williams et al., 2006), and the use of arsenical pesticides (Williams et al., 2007a). Unlike other cereal grains, paddy rice cultivation is depen- dent of soils being anaerobic, and it is this anoxia that gives rise to elevated As concentrations in the plant. Anaerobic soil conditions lead to the mobilization of As as arsenite, where under aerobic systems arsenate dominates (Xu et al., 2008). Arsenite is efficiently 1 This work was supported by a Biotechnology and Biological Sciences Research Council Doctoral Training Grant. Portions of this work were performed at GeoSoilEnviroCARS (sector 13) and PNC/ XOR (sector 20), at the Advanced Photon Source, Argonne National Lab- oratory. GeoSoilEnviro Consortium for Advanced Radiation Sources is supported by the National Science Foundation-Earth Sciences (grant no. EAR–0622171) and Department of Energy-Geosciences (grant no. DE–FG02-94ER14466). Pacific Northwest Consortium Col- laborative Access Team Advanced Photon Source, Sector 20 facilities at the Advanced Photon Source, and research at these facilities, are supported by the U.S. Department of Energy-Basic Energy Sciences, a major facilities access grant from the Natural Sciences and Engineer- ing Research Council, the University of Washington, Simon Fraser University, and the Advanced Photon Source. Use of the Advanced Photon Source was supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences (under contract no. DE–AC02–06CH11357). The U.S. Environmental Protection Agency, through its Office of Research and Development, funded and man- aged a portion of the research; it has not been subject to Agency review and, therefore, does not necessarily reflect the views of the Agency, no official product endorsement should be inferred. * Corresponding author; e-mail [email protected]. The author responsible for distribution of materials integral to the findings presented in this article in accordance with the policy described in the Instructions for Authors (www.plantphysiol.org) is: Andrew A. Meharg ([email protected]). [W] The online version of this article contains Web-only data. www.plantphysiol.org/cgi/doi/10.1104/pp.109.146126 Plant Physiology Ò , January 2010, Vol. 152, pp. 309–319, www.plantphysiol.org Ó 2009 American Society of Plant Biologists 309

Transcript of Grain Unloading of Arsenic Species in Rice

Grain Unloading of Arsenic Species in Rice1[W]

Anne-Marie Carey, Kirk G. Scheckel, Enzo Lombi, Matt Newville, Yongseong Choi, Gareth J. Norton,John M. Charnock, Joerg Feldmann, Adam H. Price, and Andrew A. Meharg*

Institute of Biology and Environmental Sciences, University of Aberdeen, Aberdeen AB24 3UU, UnitedKingdom (A.-M.C., G.J.N., A.H.P., A.A.M.); National Risk Management Research Laboratory, United StatesEnvironmental Protection Agency, Cincinnati, Ohio 45224 (K.G.S.); Centre for Environmental Risk Assessmentand Remediation, University of South Australia, Mawson Lakes, South Australia SA–5095, Australia (E.L.);Cooperative Research Centre for Contamination Assessment and Remediation of the Environment, Salisbury,South Australia 5106, Australia (E.L.); GSECARS Advanced Photon Source, Argonne National Laboratory,Argonne, Illinois 60439 (M.N., Y.C.); Centre for Molecular Environmental Science, University of Manchester,Manchester M13 9PL, United Kingdom (J.M.C.); Council for the Central Laboratory of the Research CouncilsDaresbury Laboratory, Daresbury, Warrington WA4 4AD, United Kingdom (J.M.C.); and Department ofChemistry, University of Aberdeen, Meston Walk, Aberdeen AB24 3TU, United Kingdom (J.F.)

Rice (Oryza sativa) is the staple food for over half the world’s population yet may represent a significant dietary source ofinorganic arsenic (As), a nonthreshold, class 1 human carcinogen. Rice grain As is dominated by the inorganic species, and theorganic species dimethylarsinic acid (DMA). To investigate how As species are unloaded into grain rice, panicles were excisedduring grain filling and hydroponically pulsed with arsenite, arsenate, glutathione-complexed As, or DMA. Total Asconcentrations in flag leaf, grain, and husk, were quantified by inductively coupled plasma mass spectroscopy and Asspeciation in the fresh grain was determined by x-ray absorption near-edge spectroscopy. The roles of phloem and xylemtransport were investigated by applying a 6 stem-girdling treatment to a second set of panicles, limiting phloem transport tothe grain in panicles pulsed with arsenite or DMA. The results demonstrate that DMA is translocated to the rice grain withover an order magnitude greater efficiency than inorganic species and is more mobile than arsenite in both the phloem and thexylem. Phloem transport accounted for 90% of arsenite, and 55% of DMA, transport to the grain. Synchrotron x-rayfluorescence mapping and fluorescence microtomography revealed marked differences in the pattern of As unloading into thegrain between DMA and arsenite-challenged grain. Arsenite was retained in the ovular vascular trace and DMA dispersedthroughout the external grain parts and into the endosperm. This study also demonstrates that DMA speciation is altered inplanta, potentially through complexation with thiols.

Paddy rice (Oryza sativa) is particularly effective,compared to other cereals, at accumulating arsenic(As) in shoot and grain (Williams et al., 2007b). Rice isthe staple food for over half the world’s population(Fageria, 2007) and rice represents a significant dietarysource of inorganic As, a class 1, nonthreshold carcin-ogen, particularly in Southeast Asia (Meharg et al.,2009). Inorganic As levels in rice grain are problematiceven where soil As is at background levels, derivedfrom geogenic sources (Lu et al., 2009; Meharg et al.,2009). However, widespread pollution of paddy soilswith As, leading to further elevation of grain As, hasoccurred in some regions due to base and preciousmining (Liao et al., 2005; Zhu et al., 2008), irrigation ofpaddies with As-elevated groundwaters (e.g. Mehargand Rahman, 2003; Williams et al., 2006), and the useof arsenical pesticides (Williams et al., 2007a). Unlikeother cereal grains, paddy rice cultivation is depen-dent of soils being anaerobic, and it is this anoxia thatgives rise to elevated As concentrations in the plant.Anaerobic soil conditions lead to the mobilization ofAs as arsenite, where under aerobic systems arsenatedominates (Xu et al., 2008). Arsenite is efficiently

1 This work was supported by a Biotechnology and BiologicalSciences Research Council Doctoral Training Grant. Portions of thiswork were performed at GeoSoilEnviroCARS (sector 13) and PNC/XOR (sector 20), at theAdvancedPhoton Source,ArgonneNational Lab-oratory. GeoSoilEnviro Consortium for Advanced Radiation Sourcesis supported by the National Science Foundation-Earth Sciences(grant no. EAR–0622171) and Department of Energy-Geosciences(grant no. DE–FG02-94ER14466). Pacific Northwest Consortium Col-laborative Access Team Advanced Photon Source, Sector 20 facilitiesat the Advanced Photon Source, and research at these facilities, aresupported by theU.S. Department of Energy-Basic Energy Sciences, amajor facilities access grant from the Natural Sciences and Engineer-ing Research Council, the University of Washington, Simon FraserUniversity, and the Advanced Photon Source. Use of the AdvancedPhoton Source was supported by the U.S. Department of Energy,Office of Science, Office of Basic Energy Sciences (under contract no.DE–AC02–06CH11357). The U.S. Environmental Protection Agency,through its Office of Research and Development, funded and man-aged a portion of the research; it has not been subject to Agencyreview and, therefore, does not necessarily reflect the views of theAgency, no official product endorsement should be inferred.

* Corresponding author; e-mail [email protected] author responsible for distribution of materials integral to the

findings presented in this article in accordance with the policydescribed in the Instructions for Authors (www.plantphysiol.org) is:Andrew A. Meharg ([email protected]).

[W] The online version of this article contains Web-only data.www.plantphysiol.org/cgi/doi/10.1104/pp.109.146126

Plant Physiology�, January 2010, Vol. 152, pp. 309–319, www.plantphysiol.org � 2009 American Society of Plant Biologists 309

assimilated by rice roots through silicic acid transportpathway (Ma et al., 2008).

Knowledge of As metabolism and partitioningwithin plants, particularly rice, is still developingrapidly (Zhao et al., 2009). Several studies have nowshown that As in rice vegetative tissue and grain ispredominantly speciated as inorganic As and themethylated species dimethylarsinic acid (DMA), withvariable, though low, levels of monomethyl arsonicacid (MMA; Abedin et al., 2002a; Williams et al., 2005,2006; Norton et al., 2009). Arsenate is an analog ofphosphate and competes with phosphate for rice rootuptake (Abedin et al., 2002a) while arsenite is taken upby rice roots via silicic acid transporters (Ma et al.,2008). Abedin et al. (2002b) demonstrated that themethylated species DMA and MMA are also taken upby rice plants although at a much slower rate thaninorganic As, with the protonated neutral forms alsotransported through silicic acid pathway (Li et al.,2009). Arsenate is reduced to arsenite within the riceroot (Xu et al., 2008; Zhao et al., 2009), which thenenters the xylem via a silicic acid/arsenite effluxer (Maet al., 2008; Zhao et al., 2009). Arsenite may be detox-ified through complexation with thiol-rich peptidesincluding phytochelatins (PCs) and glutathione fol-lowed by sequestration into vacuoles (Bleeker et al.,2006; Raab et al., 2007b; Zhao et al., 2009). Raab et al.(2007a) found that while methylated As species aretaken up by rice roots much less efficiently thaninorganic species, they appear to be translocatedwithin the plant more efficiently. The comparativecontributions of xylem and phloem transport, in trans-location of As to the grain, are unknown.

Themain specieswithin rice grain, alongwith DMA,are inorganic As, particularly arsenite, which may becomplexed with thiols (Williams et al., 2005; Lombiet al., 2009). Nutrients are unloaded into the grain fromthe ovular vascular trace (OVT) into the nucellar tissueand from there are uploaded, via the apoplast into thefilial tissue (the aleurone and the endosperm; Krishnanand Dayanandan, 2003). Lombi et al. (2009) recentlysuggested that this may represent a physiologicalbarrier that As species crosswith differential efficiency.However, the transport and unloading of As to/intothe grain, which are key processes in terms of humanexposure to this contaminant, are far from being fullyunderstood.

This study investigated the differential efficiencywith which important As species are translocated andunloaded into the rice grain and the comparativecontributions of phloem and xylem transport. Ricepanicles were excised below the flag leaf node dur-ing grain development, 10 DPA, and treated to a hy-droponically administered 48-h pulse of arsenite,arsenate, arsenite glutathione, or DMA. Total As con-centrations in flag leaf, grain, and husk samples foreach treatment were quantified by inductively cou-pled plasma mass spectroscopy (ICP-MS), and Asspeciation in the fresh grain was determined byx-ray absorption near-edge spectroscopy (XANES)

analysis. To evaluate the contributions of phloem ver-sus xylem transport, a stem-girdling treatment wasapplied, using steam to destroy phloem cells in asecond set of panicles prior to a pulse of either DMA orarsenite. The spatial unloading of As species into thedeveloping grain was examined by synchrotron x-rayfluorescence (XRF) mapping, and fluorescence micro-tomography for the DMA and arsenite treatments.

RESULTS

Total As Concentrations in Tissues—Experiment A

Mean total As concentrations in flag leaf sampleswere 26.8 6 14.2, 7.56 6 1.31, 30.8 6 11.4, and 45.9 614.6 mg kg21 for when excised plants were exposed to13.3 mM arsenite glutathione, arsenite, arsenate, andDMA treatments, respectively (Fig. 1A). One-wayANOVA revealed As treatments had a highly signif-icant effect on flag leaf total As levels (P , 0.001) andAs levels were significantly lower for control leaves(0.107 6 0.004 mg kg21) compared to all other Astreatments. The DMA and arsenate treatments gavesignificantly higher flag leaf As than the arsenitetreatment, however, differences between the DMA,arsenate, and arsenite glutathione [As(GS)3] treat-ments, and between the arsenite and arsenite gluta-thione treatments, were determined not significant.The mean flag leaf As concentration for the 133 mM

arsenite treatment was 123.7 6 24.8 mg kg21, morethan 10-fold that of the 13.3 mM arsenite treatment.

Mean grain As concentrations (Fig. 1B) were, gen-erally, an order of magnitude lower than flag leafconcentrations, with the exception of the DMA treat-ment. ANOVA revealed that panicle As treatmentshad a highly significant effect on grain As levels (P ,0.001) and grain As concentrations were significantlylower for the controls (0.027 6 0.001 mg kg21) thanfor all other As treatments. Mean total As concentra-tions in the grain were similar for the As(GS)3, arsenite,and arsenate treatments (0.16 6 0.015, 0.18 6 0.098,and 0.29 6 0.029 mg kg21, respectively). The meangrain As level for the DMA treatment was significantlyhigher than all other treatments (12.5 6 3.84 mg kg21).Mean grain As for the 133 mM arsenite treatment was1.31 6 0.04 mg kg21, about 10-fold higher than thatthat of the 13.3 mM arsenite treatment.

As treatments had a highly significant effect on husktotal As (P, 0.001) and all As treatments led to highermean husk As levels than the control mean of 0.012 60.0008 mg kg21 (Fig. 1C). The arsenite glutathione,arsenite, and arsenate treatments led to comparativelysimilar husk As levels (0.286 0.06 mg kg21, 0.216 0.14mg kg21, and 0.73 6 0.24 mg kg21, respectively), withsignificant differences determined between arsenateand arsenite only. However, as with the grain, theDMA treatment led to significantly higher husk As lev-els, 6.66 1.15 mg kg21, than all other treatments. HuskAs for the 133 mM arsenite treatment was 2.1 6 0.1 mg

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kg21, about 10-fold higher than that of the 13.3 mM

arsenite treatment.The ratio of flag leaf As to grain As for each

treatment is reported in Figure 1D. The ratios of leafAs to grain As for the As(GS)3, arsenite, and arsenatetreatments were significantly higher than the controland DMA treatments (P = 0.001). Notably, the meanflag leaf to grain As ratios for the arsenite 13.3 mM

treatment and 133 mM treatments were not signifi-cantly different. The ratio of husk As to grain As isshown in Figure 1E. ANOVA revealed no significantdifferences between treatments.

Total Element Concentrations in Stem-GirdledGrain—Experiment B

Mean grain concentrations of As, rubidium (Rb),and strontium (Sr) for the stem-girdling experimentare reported in Figure 2. Based on the findings fromexperiment A, the arsenite treatment of 133 mM wasused to give high grain levels for tomography. AsDMAwas unloaded very efficiently into grain, the 13.3mM solution was utilized for tomography. One-wayANOVA determined that differences in mean wateruptake for treated panicles were not significantlydifferent (23 6 2 mL, 18.3 6 1.7 mL, and 23 6 1 mL

for the control, 133 mM arsenite, and 13.3 mM DMAtreatments, respectively, P = 0.123). Two-way ANOVArevealed that the As and stem-girdling treatments hadhighly significant effects on mean grain As concentra-tions (P , 0.001 for both) and there was a highlysignificant interaction between treatments (P , 0.001).There was no significant difference between meangrain As levels in stem-girdled control (no As) paniclesand mean grain As in non-stem-girdled control pan-icles (0.074 6 0.027 and 0.1 6 0.032 mg kg21, respec-tively, P = 0.9975). Stem girdling had a highlysignificant effect on grain treated with 13.3 mM DMA,leading to a 55% decrease in grain As concentration,12.8 6 0.54 mg kg21 for stem-girdled panicles com-pared with 28.66 1.1 mg kg21 in nonstem girdled (P,0.001). For panicles treated with 133 mM arsenite, stemgirdling had an even greater effect, with grain Asconcentrations 90% lower in stem-girdled plants com-pared with non-stem-girdled plants, 0.19 6 0.03 mgkg21 in stem-girdled plants compared with 1.676 0.41mg kg21 in nonstem girdled (P = 0.0012).

Two-way ANOVA revealed that stem girdling had ahighly significant effect on grain concentrations of thephloem marker, Rb (P , 0.001), with stem-girdledplants having significantly less Rb in the grain thannon-stem-girdled plants. For the As control plants,

Figure 1. Total As concentrations in flag leaf (A), grain (B), husk for rice and ratios of flag leaf As concentration to grain Asconcentration (C and D), and husk As concentration to grain As concentration for rice panicles excised at 10 DPA andhydroponically fed, over a 48-h period, a nutrient solution amended with one of five As treatments at 13.3 mM exposure (E). Notethat in D and E the ratios for the 133 mM arsenite treatment are included as they are ratios rather than absolute concentrations.Error bars represent 6SE of three replicates.

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mean grain Rb concentrations were 18.3 6 4.85 and221 6 84.9 mg kg21 for stem-girdled and non-stem-girdled panicles, respectively (P , 0.001). For plantstreated with 133 mM arsenite, mean grain Rb concen-trations were 34.9 6 5.4 mg kg21 for stem-girdledpanicles and 166 6 50.3 mg kg21 for non-stem-girdledplants (P = 0.048), and for DMA-treated grain, Rb con-centrations in the grain were also significantly lowerfor stem-girdled plants than for non-stem-girdledplants (21.6 6 4.9 mg kg21 and 372 6 27.2 mg kg21,P , 0.001). As treatments had no significant effecton grain Rb levels (P = 0.310) and there was no sig-nificant interaction between the As and stem-girdlingtreatments (P = 0.093). Two-way ANOVA revealedthat the As and stem-girdling treatments had nosignificant effect on grain levels of the xylem transportmarker, Sr (P = 0.234 and P = 0.963, respectively), andthere was no significant interaction between the twotreatments (P = 0.555). These results provide evidencethat Rb and Sr are efficient tracers for phloem and

xylem transport (Kuppelwieser and Feller, 1991) andthat the stem-girdled treatment produced the desiredresult.

Spatial Unloading of As into the Grain

Fluorescence microtomography images for experi-ment B of a virtual transverse slice, scanned across thegrain about halfway down the embryo, illustrate grainunloading of As, Rb, and Sr for rice grain treated with133 mM arsenite and 13.3 mM DMA, respectively. Theseimages are reported in Figure 3 for non-stem-girdledpanicles. The equivalent tomograms showing manga-nese (Mn), iron (Fe), copper (Cu), and zinc (Zn)distributions for both As treatments are shown inSupplemental Figure S1. Tomography imaging revealsa remarkable contrast in As unloading into the grain,between the DMA and arsenite treatments. The arse-nite-treated grain exhibits strong localization of Ascoincident with Sr, Mn, and Fe at the site of the OVT,

Figure 2. Total grain concentrations of As, Rb, and Srin rice grain hydroponically fed, over a 48-h period,nutrient solution amended with either 133 mM arse-nite or 13.3 mM DMA and 1 mM Rb and Sr, forpanicles which have been subjected to a 6 stem-girdling treatment. Error bars represent 6SE of threereplicates.

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the source of nutrient influx into the grain. Conversely,the image of As distribution for the DMA treatmentshows that As has not remained in the OVT but hasspread throughout the external parts of the grain withsome migration into the endosperm. This pattern isalso evident in the elemental XRF maps of As distri-bution for experiment A, presented in SupplementalFigure S2, for slices cut across the middle of fresh ricegrains. Tomography showed that neither As treatmentled to visible As accumulation in the embryo (Fig. 3).Stem girdling appeared to have no effect on the Asdistribution pattern, with tomograms showing identi-cal element distributions (data not shown) to those oftheir non-stem-girdled counterparts. For both As andstem-girdling treatments the phloem marker, Rb, isdispersed throughout the outer layers and is particu-larly enriched in the scutellum of the embryo while Sris restricted to the OVT (Fig. 3). Tomograms and XRFmaps for the arsenite and DMA treatments show thatMn and Fe are localized primarily in the OVT. Zn andCu, conversely, exhibit no such localization in the OVT.Cu appears enriched in the outer layers and theembryo of the grain. XRF maps show Zn is dispersedaround the outer layers of the grain, and enrichment inthe embryo is evident in the arsenite tomogram. Thisenrichment is less clear in the tomogram for the DMA-treated grain, probably due to the lower relative in-tensity.

XANES Speciation

For experiment A, XANES spectra collected for freshgrain are reported for each As treatment in Figure 4A,together with those for standards for several As spe-cies. Additional standards, acquired from anothersynchrotron source, are presented in Figure 5 to enablefurther evaluation of the results for DMA speciation.Absorption edge peaks (white line energies) for As stan-dards increased in the order As(GS)3 , MMA(III) ,AsIII , DMA(V) , MMA(V) , AsV, in agreementwith Smith et al. (2005) and Meharg et al. (2008). All

spectra exhibit features that indicated that more thanone species of As was present in the samples analyzed.Spectra for the control, arsenate, and 13.3 mM arsenitetreatments all exhibit features that can be ascribed tothe presence of reduced As species as well as a peakvery slightly to the left (lower energy) or concurrentwith the arsenate standard, indicating a substantialproportion of arsenate was present. It was observed(data not shown) that the beam caused reduction ofarsenate over several replicate spectra despite usage ofa sample cold stage, and so arsenate may be under-estimated. The 133 mM arsenite treatment exhibited amarkedly different speciation pattern within the grainthan the 13.3 mM treatment, with an absorption edgecorresponding to arsenite.

The spectrum for arsenite glutathione-treated rice,on the other hand, is shifted to the right, with respectto the As(GS)3 standard, suggesting the complex hasdissociated. Although the peak appears coincidentwith the DMA(V) standard, its broad nature indicatesthat it represents a mixture of species.

DMA, added as DMA(V), behaved very differentlyto the inorganic As species, with a striking shift of theirabsorption edge to the left of the DMA(V) standard,albeit while maintaining a shoulder concurrent withthe DMA(V) standard. This indicates that a proportionof added DMA(V) had altered speciation in the grain.This could occur, potentially, through some demeth-ylation and reduction to arsenite, or reduction to DMA(III), with or without thiol coordination. No DMA(III)standards could be run due to the high instability ofthis compound. Also, DMA(GS)3 is unstable (Raabet al., 2007c). However, XANES data collected at theDaresbury, United Kingdom synchrotron shows thatarsenite shares a similar spectra with that for dithiol-complexed DMA(V) and for the DMA(V)-DMA(III)sulphide dimer (Fig. 5). This highlights the limitationsof XANES speciation in distinguishing As species andhow the choice of standards can significantly influenceinterpretation of the data (Beauchemin et al., 2002),and indicates that methylated species may have been

Figure 3. Fluorescence microto-mography images showing distri-butions of As, Rb, and Sr for virtualcross section of rice grain pulsedwith 133 mM arsenite (top) and 13.3mM DMA (bottom).

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dithiol complexed rather than reduced or demeth-ylated.

As grain As levels were so high for the DMAtreatment, XANES could be collected for the differentgrain fractions, by manual separation (the pericarp, itis unclear whether this included the aleurone, can beslid off fresh grain) of this treatment (Fig. 4B). For theendosperm and developing embryo fractions, thespectrum, while having a peak corresponding toDMA(V), exhibited a shoulder/s peak at a lowerenergy than the DMA standard. The pericarp had aspectrum concurrent with, though broader than, theDMA(V) standard. The lower energy peak may beexplained by reduction and, potentially, further com-plexation with thiols, corresponding better with theDMA(III)-DMA(V) dimer thiol.

DISCUSSION

As Speciation and Accumulation in Grain

Translocation of DMA to the rice grain was over anorder of magnitude higher than for inorganic species.Abedin et al. (2002b) found that both MMA and DMAinflux into rice roots was low compared to arsenateand arsenite. A similar result was reported for maize

(Zea mays) by Abbas and Meharg (2008) for DMA.Raab et al. (2007a) found that for DMA and MMAplant uptake over 24 h in hydroponics, for a widerange of plant species tested, including rice, was muchlower than for arsenate and arsenite, but that translo-cation from root to shoot was much more efficient forthe methylated species. It was postulated by Raab et al.(2007b) that this was due to poorer thiol complexationof DMA and MMA, leading to less retardation whentranslocated through the plant. When As-PC com-plexes were analyzed in Helianthus annus, MMA-PCcomplexes could be detected, but only free DMAwasfound (Raab et al., 2005).

Grain As speciation is dominated by inorganic Asand DMA (Williams et al., 2005, 2007a). A survey byWilliams et al. (2005) of As speciation in rice grainfound that inorganic As accounted for between 64%and 81% of As in rice grain from Europe, Bangladesh,and India, and for 42% in U.S. rice grain, with DMAlargely accounting for the remainder. DMA content ofrice shoots is low, accounting for only 0% to 5% of Asspecies (Abedin et al., 2002a). It has not yet beenresolved how rice obtains DMA. While total plantaccumulation and/or in planta production of DMA islow (Zhao et al., 2009), export to grain is highlyefficient. The results presented here confirm that riceis remarkably efficient in the unloading of DMA into

Figure 4. Bulk As XANES for fresh rice grain hydro-ponically delivered a 48-h pulse of nutrient solutionspiked with 13.3 mM of different As species andXANES for separated grain parts of the DMA treat-ment. A, Analysis of bulk tissue; B, analysis ofseparated tissue.

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grain, with DMA distributed rapidly around the peri-carp/aleurone/subaleurone zone. Furthermore, theresults reported here for the stem-girdling experimentshow that phloem transport is responsible for themajority of arsenite transport to the grain, withphloem interruption reducing grain As by 90%.DMA is much more mobile than arsenite in both thephloem and the xylem. This explains why husk con-centrations of As in the first experiment were alsomarkedly higher for the DMA treatment than those forinorganic arsenite. It has been suggested that as anontranspiring tissue developing grain will be fedassimilates primarily via phloem transport, and theactively transpiring husk primarily via the xylem(Tanaka et al., 2007; Lombi et al., 2009). This appearsevident in the high concentrations of the phloemmarker, Rb, compared with the comparatively lowgrain levels Sr.At 13.3 mM exposure, the retardation of arsenate and

arsenite into the grain, as compared to DMA, wasprobably not due to thiol complexation, as bulkXANES analysis showed that for both arsenite andarsenate-exposed plants, speciation was dominated byarsenate, i.e. the arsenite had been oxidized. As arse-nate normally has a low affinity for thiol groups (Raab

et al., 2007c), thiol complexation, and, therefore, retar-dation in thiol-rich compartments of the grain cannotexplain the comparatively poor unloading of inorganicspecies from the OVT at low exposure concentrations.It may be possible that there is redox cycling of theinorganic As species in the grain, with the reducedform being thiol complexed; however, this is unlikely,as at higher arsenite exposure concentrations of 133mM, arsenite remains stable. In contrast, when maturegrain was analyzed, Lombi et al. (2009) found thatmuch of the inorganic As was thiol complexed. How-ever, the Lombi et al. (2009) study was for field-growngrain, where plants had been continuously exposed toAs through the root system, while in this study, the Aswas pulsed in hydroponically directly through thestem. The concentration-dependent alteration of arse-nite speciation in this study may indicate that athreshold, to induce reductases or other As-reducingcellular processes such as reduced glutathione pro-duction, is present in grain tissue, as arsenate is thethermodynamically stable arsenate species, and arse-nite is oxidized to arsenate in the low arsenite expo-sure treatment. When plants were fed with an As-PCanalog, As(GS)3, transfer into the grain was limited,and the thiol complex dissociated.

With respect to the DMA-exposed treatments pre-sented here, the situation is more complex as theDMA-exposed plants had As XANES absorption edgeshifted to lower energies than the DMA(V) standard,albeit with a shoulder on the DMA(V) standard ab-sorption edge. This indicates that most of the DMA(V)added has altered speciation. This finding confirmsthe observation of Meharg et al. (2008) for rice endo-sperm (i.e. polished rice) that was known to have ahigh DMA content by HPLC-ICP-MS detection fol-lowing extraction, yet the XANES analysis of thistissue found a much lower DMA content than wouldbe expected from the chromatographic quantification,again with the absorption edge shifted toward lowerenergies than the DMA(V) standard, toward that of thearsenite standard (Meharg et al., 2008). It should benoted however, that the Meharg et al. (2008) study wasbased on m-XANES analyses, which may not be rep-resentative of the overall speciation, and not bulkXANES. However, this difference between XANESand HPLC-ICP-MS quantification of DMA was alsoobserved by Lombi et al. (2009), with the percentage ofDMA in the endosperm found to be 36% via HPLC-ICP-MS analysis and only 26% through linear combi-nation analysis of XANES spectra. In this study, thereis a possibility that DMA underwent demethylation toarsenite in the grain tissue, though this could not beconfirmed by HPLC-ICP-MS as tissue weights weretoo small to perform speciation analysis. However, thecomplementary studies of Meharg et al. (2008) andLombi et al. (2009), which had both XANES andHPLC-ICP-MS speciation on the same sample, suggeststrongly that demethylation is not occurring in thisstudy, but that DMA(V) speciation is altered either byreduction and/or thiol coordination. DMA thiol com-

Figure 5. XANES spectra from different trivalent and pentavalent Asstandards.

Grain Unloading of Arsenic Species

Plant Physiol. Vol. 152, 2010 315

plexes are not observed in plant extracts due to theoxidizing nature of extraction conditions (Raab et al.,2007a). The advantage of XANES analysis is that itdetermines speciation in situ. It should, however, beborne in mind that questions regarding the reliabilityof quantification of XANES data have been raised and,as demonstrated here, XANES analysis relies on theanalysis of all relevant standards, and indeed thosestandards giving significantly resolved spectra fromeach other (Lombi and Susini, 2009; Williams et al.,2009).

As Localization in Grain

The tomography and XRF images reveal strikinglydifferent As distributions for inorganic and organicAs, showing that for the arsenite-exposed grain, Ashas remained in the OVT (situated opposite the em-bryo in tomography images and identifiable by thestrong localization of Mn and Fe in the XRF maps),while for the DMA-pulsed grain, As has dispersedinto, and throughout, the nucellar epidermis region,with migration into the outer parts of the endospermevident.

The coincidence of As with Mn and Fe at the site ofthe OVT (for arsenite) agrees with previous studies(Meharg et al., 2008; Lombi et al., 2009), where maturefilled grains have been mapped by synchrotron XRF,and the localization of As in the outer grain layer (forboth arsenite and DMA) also agrees with findings ofprevious studies that rice bran contains higher Ascompared with white rice (Ren et al., 2006; Sun et al.,2008). Indeed, the tomograms and XRF maps forarsenite and DMA presented here, equate to high Asin the bran polish of the grain, although it must beborne in mind that the grains in this study are stilldeveloping, and metabolically active, and do not nec-essarily reflect the final localization and speciationwithin the mature filled grain (Ren et al., 2006;Rahman et al., 2007; Sun et al., 2008; Lombi et al.,2009). The absence of As (and Mn and Fe) within theembryo disagrees with Lombi et al. (2009), however,again, it must be noted that the results presented hererepresent a developing caryopsis (and embryo) exper-imentally, and directly, pulsed with As over a veryshort time period. The enrichment of Zn and Cu in theembryo does agree with Lombi et al. (2009).

It is interesting that, although phloem interruptionby girdling the stem with steam substantially affectedgrain As concentrations for both the arsenite and theDMA treatments, it did not affect the spatial unloadingof As within the grain in either case. Therefore, whilethe ratio of phloem to xylem transport may be impor-tant in the rate of As transport to the grain, it may notbe important with regard to As mobility within thegrain. Lombi et al. (2009) noted that there appears to bea physiological barrier in the transfer of As from thematernal (OVT and nucellar tissue) to filial tissues(aleurone, endosperm, and embryo). It must be re-membered, however, that the Lombi et al. (2009) study

had mixed grain speciation, dominated by inorganicAs. The OVT comprises both phloem and xylem ele-ments and is the only supply of nutrients (and con-taminants) into the developing grain (Krishnan andDayanandan, 2003). Nutrients are unloaded symplas-tically into the chalazal tissue immediately below theOVT and from there apoplastically into the nucellarepidermis that encircles the grain (Krishnan andDayanandan, 2003). Nutrients unloaded into the nu-cellar epidermis spread throughout the nucellar epi-dermis, encircling the endosperm (as is evident in Fig.3 and Supplemental Figs. S1 and S2) and are thentransported, via the apoplast, radially inwards into thefilial tissue (Krishnan and Dayanandan, 2003). Theresults presented here support the existence of such abarrier and suggest that DMA is more efficient atcrossing it. If DMA is indeed more readily unloadedinto the nucellar tissue and uploaded into the aleurone(and ultimately deposited in the endosperm) thiswould explain why levels of DMA are higher in theendosperm compared with inorganic species and whyinorganic As is so high in the bran polish of rice grain.The similarities in As distribution between girdled andnongirdled treatments may suggest that either themechanism responsible for xylem/phloem unloadingis similar or that the limiting step in arsenite redistri-bution in the grain is the uptake from the apoplast intothe filial tissues.

It is necessary to revisit and update interpretation ofthe As XRF data of Meharg et al. (2008) and Lombi et al.(2009), as the new results presented here may explainwhy for some rice grain samples, As is very muchlimited to the region of theOVTwhile in others it ismoredispersed.Where the percentage ofDMA ishigh there ismore dispersal through the grain. InMeharg et al. (2008)a range of rice grain was analyzed. The percentage ofDMAdeterminedbyHPLC-ICP-MS for theBangladesh,Chinese, and U.S. brown grains in Meharg et al. (2008)was very similar (27%–28%). XRF maps showed that allexhibited amixture of high localization ofAs in theOVTregion with some dispersal around the pericarp/aleu-rone region (and inwards), which would be concurrentwith the presence of amixture ofDMAand inorganicAs(with higher concentrations of inorganic As). Although,interestingly, there does appear to be some variation inthe degree of dispersal throughout the grain with theBangladeshi grain in particular showing relatively littleAs in the interior parts of the grain with respect to theouter layer (Meharg et al., 2008). In Lombi et al. (2009) anXRF map was generated for a sample that had a partic-ularly high proportion of inorganic As and was corre-spondingly low inorganicAs.This showedAs tobeverymuch localized in theOVTregionwith limited dispersalaround the pericarp region (Lombi et al., 2009).

CONCLUSION

It should be noted that this system of pulsing thegrains directly with As species is considerably differ-

Carey et al.

316 Plant Physiol. Vol. 152, 2010

ent to the whole-plant system, having bypassed theinitial entry point for whole plants. Nonetheless, thisstudy demonstrates that As species differ in the effi-ciency with which they are translocated from the shootto the grain, and that DMA in particular is translocatedto the grain much more efficiently than inorganicspecies. Additionally, this study shows the spatialunloading of As into the rice grain following a pulseof a known As species, and demonstrates markeddifferences in As unloading into the grain betweenDMA and inorganic arsenite-fed grain. The resultspresented here also demonstrate the comparative con-tributions of xylem and phloem transport in grainunloading of As for arsenite and DMA, representing akey step forward for the development of strategiesrequired to lower grain As content, essential since riceis a predominant source of inorganic As, a class 1,nonthreshold carcinogen, to the human diet (Meharget al., 2009).This study also represents evidence that DMA(V)

speciation is altered in planta, potentially throughcomplexation with thiols, and highlights a key advan-tage of in situ XANES speciation versus extraction andchromatographic separation and detection of As spe-ciation. It also highlights the disadvantages of XANES;not all potential As species in plants are known, and asXANES analysis is dependent on the analysis of allrelevant standards, and indeed those standards givingsignificantly resolved spectra from each other, thepresence of unknown phases may go unrecognized.These limitations were only determined and overcomein this study by pulsing known As species into thegrain in isolation.

MATERIALS AND METHODS

Plant Growth and Panicle Treatments

A quick flowering rice (Oryza sativa) variety, Italica carolina, originally

obtained as part of the Rice HapMap (diversity) project (www.ricehapmap.

org), was used. Seeds were sown directly into trays of John Innes number 2

potting compost. Plants were transferred into 1 L pots after several weeks and

grown under tropical greenhouse conditions. Supplemental lighting was

provided at 150 mmol m22 s21 by sodium lamps and the temperature range

was kept within 23�C to 35�C. Plants were fed weekly with Sangral soluble

fertilizer (Sinclair), a 1:1:1 nitrogen:phosphorus:potassium plus 1 MgO mix,

diluted 1 in 100 (w/v). Rice panicles were marked by colored thread at

anthesis and at 10 DPA; similar sized, healthy looking panicles were excised

below the flag leaf node as described in Chen et al. (2007). All plants and

panicles were placed in darkness for 2 h prior to both the initial panicle

excision and transfer to nutrient solutions. Immediately following excision

from themain plant, the bottom 5 cm of the panicle stemwas removed, cutting

under water. Excisions and panicle transfer were conducted in low red light

conditions. These procedures reduced transpiration, limiting potential xylem

air bubbles at the base of the cut stems. Excised panicles were immediately

transferred to 100 mL Pyrex glass tubes each containing 50 mL of autoclaved

nutrient solution. The composition and pH (6.46 0.05) of the nutrient solution

was as described by Chen et al. (2007). As markers for phloem and xylem

transport, respectively, Rb and Sr were added to the treatment nutrient

solutions at a final concentration of 1 mM. Panicle stems were held in position

in the tubes, with a sterilized polyurethane foam bung (sliced vertically to

wrap around the plant stem) that was then covered with tinfoil to prevent

contamination of the solution and limit solution evaporation losses through

the bung. Panicles were then transferred to a growth chamber with a 12-h

photoperiod, a day/night temperature of 28�C/23�C, relative humidity of 80/

60, and light intensity of 1,200 mmol m22 s21. After 24 h panicles were

removed, rinsed with milliQ deionized water, and transferred to fresh tubes of

sterilized phosphate-free nutrient solution (50 mL) that had been spiked with

the appropriate As treatment. Treatment stock solutions were prepared by

dissolving the relevant amount of the appropriate salt in milliQ deionized

water. In every experiment there were three replicate panicles for each

treatment including three controls. For each treatment and control three

replicate panicles were used.

Two experiments were performed on rice panicles: A, where a range of As

species unloading into grain of non-stem-girdled plants was investigated,

with As speciation and localization investigated in fresh sliced grains, and B,

where arsenite and DMA unloading into 6 stem-girdled plants was investi-

gated, with As localized in intact grain through fluorescence microtomog-

raphy. In experiment B, panicles were also exposed to Rb and Sr as markers of

phloem and xylem flow, respectively (Kuppelwieser and Feller, 1991).

Experiment A consisted of six treatments including the control treatment

of no As. As treatments were a 48-h pulse of either 13.3 mM arsenate, arsenite,

arsenite glutathione, or DMA(V) or 133 mM of arsenite, and were assigned

randomly to panicles as they reached 10 DPA. Following the As pulse the flag

leaf of each treated panicle was cut at the base of the leaf blade (above the

ligule). Grains were selected from the top and middle regions of the panicle

and husks were separated manually. A subsample of the grains from each

panicle was immediately chilled to 4�C for the synchrotron analyses and the

remainder grains were oven dried, together with the flag leaves and husks, for

ICP-MS analysis. All samples were analyzed via ICP-MS for total As as

described below. For XANES speciation, one grain from each of the three

replicates of each treatment was selected and bulked together into a powder.

XRF elemental maps were collected for a single grain from one replicate of the

13.3 mM DMA and 133 mM arsenite treatments, respectively.

For the experiment B, As treatments were a 48-h pulse of 133 mM arsenite or

13.3 mM DMA(V) delivered to both stem-girdled and non-stem-girdled pan-

icles. Stem-girdled panicles were subjected to a 30 s jet of steam to a 1 cm area

of the stem between 1 and 2 cm below the panicle head, prior to excision from

the plant. This destroys the phloem cells, preventing further phloem transport

in to the rice grain while xylem vessels remain functional (Martin, 1982;

Kuppelwieser and Feller, 1991; Chen et al., 2007). Grains were selected and

separated for analysis as described above, with a portion of the grain from

each panicle being kept chilled for synchrotron analysis and the remainder

oven dried for ICP-MS analysis. One fresh grain from one replicate of each

treatment was then randomly selected for fluorescence tomography.

Total As Concentrations in Flag Leaf, Grain, and Husk

Total As concentrations were determined for digested samples by ICP-MS

(7500 Agilent Technologies) as described in Sun et al. (2008). Samples were

microwave digested in a scaled-down digestion volume of that described in

Sun et al. (2008) with 0.4 mL nitric acid added to approximately 0.04 g sample,

left overnight to predigest, and 0.4 mL hydrogen peroxide added immediately

prior to digestion. Following digestion the sample was made up to 10 mLwith

0.1 mL internal standard, 1,000 mg L21 indium. Quality control measures were

as described in Sun et al. (2008).

As Speciation of Rice Grain

As speciation was determined using bulk XANES. Rice grains were frozen

in liquid nitrogen and then powdered with pestle and mortar (for each

treatment 2–3 grains from each replicate were combined to form a bulk

powder). Powders were applied directly to Kapton polyimide tape that was

folded over to form a seal. For grain components of the DMA-treated grain,

the pericarp was pulled off the fresh grain and the rudimentary embryo was

identifiable and removed with a razor blade, leaving the endosperm. Each

part was frozen in liquid nitrogen, powdered, and directly applied to Kapton

polyimide tape as described above. The samples were inserted into a multi-

sample holder that was positioned on a cryostat stage (220�C) to limit beam

damage. The XANES spectra were collected at sector 20-ID (Pacific Northwest

Consortium Collaborative Access Team) at the Advanced Photon Source,

Argonne National Laboratory. The electron storage ring operated at 7 GeV

with a top-up fill status. The sector 20 undulator beamline includes a liquid

nitrogen-cooled Si (111) double crystal monochromator and this was calibrated

using the first inflection point of the silver LIII absorption edge (11,919 eV) for

measurements at the As K edge (11,868 eV), as in Smith et al. (2005). Spectra

Grain Unloading of Arsenic Species

Plant Physiol. Vol. 152, 2010 317

were obtained in fluorescence mode with a solid-state 13-element Ge(Li)

detector. As standards were analyzed as powders (diluted in BN) and

included: arsenite (NaAsO2), arsenate (NaH2AsO4), MMA(V), and DMA(V).

Spectra for MMA(III) and As(GS)3 were kindly provided the Environmental

Sciences Group of the Royal Military College of Canada and details can be

found in Smith et al. (2005).

DMA Derivatives XANES Spectroscopy

XANES absorption spectra at the As K edge were collected, for a range of

trivalent and pentavalent As standards, on station 16.5 at the Council for the

Central Laboratory of the Research Councils Daresbury Synchrotron Radia-

tion Source operating at 2 GeV with an average current of 150 mA, using a

vertically focusing mirror and a sagitally bent focusing Si(220) double crystal

monochromator detuned to 70% transmission to minimize harmonic rejection.

For the two model compounds data were collected in transmission mode at

ambient temperature. Data for the other samples were collected with the

station operating in fluorescence mode using an Ortec 30 element solid state

Ge detector. Data collection was performed in a liquid nitrogen-cooled

cryostat. Several scans were collected and summed for the each sample.

Synchrotron-Based Mapping of As Distribution in Grain

Elemental maps obtained by synchrotron radiation XRF are projections of

all the elements in the specific path of the x-ray beam so it is necessary to

prepare thin sections for in situ analyses (Lombi and Susini, 2009). This was

achieved taping two razor blades together, flash freezing grains in liquid

nitrogen, then slicing transversely across the middle of the grain. While this

technique did produce sections of even thickness, their thickness (approxi-

mately 1 mm), together with the penetration of the beam, led to the distortion

evident in Supplemental Figure S2. Grain sections were enclosed in Kapton

polyimide tape and, to limit beam damage, mounted on a cryostat (220�C)sample holder. Laterally resolved XRF analysis of the thin sections was

conducted at sector 20-ID of the Advanced Photon Source (APS) using a beam

size of approximately 2 mm and step size of 15 mm.

Fluorescence Microtomography

To overcome the sample preparation issues described above, fluorescence

microtomography was conducted on fresh rice grain pulsed with 13.3 mM

DMA and 133 mM arsenite and subjected to a 6 stem-girdling treatment at

sector 13 at the APS. As with XANES and XRF described above, the electron

storage ring operated at 7 GeV with a top-up fill mode. Fresh rice grain was

suspended from a rotation-translation stage in the path of a 3-mm x-ray beam

and translated across in 10-mm steps with a dwell time of 0.25 s per step. The

grain was then rotated 1� and the scan process repeated until a rotation of 0� to180� was complete. XRF intensities were collected using a 16-element Ge

detector. The resulting two-dimensional sine wave plots were reconstructed as

described in McNear et al. (2005).

Supplemental Data

The following materials are available in the online version of this article.

Supplemental Figure S1. Fluorescence microtomography images showing

distributions of Zn, Cu, Mn, and Fe for a virtual cross section of rice

grain pulsed with 133 mM arsenite (top) and 13.3 mM DMA (bottom).

Supplemental Figure S2. XRF elemental maps for a cross section of a

rice grain pulsed with 13.3 mM DMA (top) and 133 mM arsenite (bottom)

for 48 h.

ACKNOWLEDGMENTS

Spectra for MMA(III) and As(GS)3 were kindly provided by the Environ-

mental Sciences Group of the Royal Military College of Canada. We would

like to express our sincere gratitude to Claire Deacon, Norman Little, and

Dave Hadwen of the University of Aberdeen and to all the staff of sectors 13

and 20 at the Advanced Photon Source, particularly Robert Gordon, Dale

Brewe, and Nancy Lazarz, for their support.

Received August 12, 2009; accepted October 29, 2009; published October 30,

2009.

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