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1 nine) in addition to some selenocysteine and selenate.
2 atile Se compounds when they were exposed to selenate.
3 erexpressors, both on media with and without selenate.
4 robably by an inability to chemically reduce selenate.
5  plants supplied with selenite compared with selenate.
6 whereas selenate-supplied plants accumulated selenate.
7 e from T. selenatis grown anaerobically with selenate.
8 cystine, methaneseleninic acid, selenite and selenate.
9 th myrosinase activity below 3.5-mmol sodium selenate.
10 ata) exposed to either 20 microM selenite or selenate.
11 ironmentally relevant mineral reductants for selenate.
12 o environmentally relevant concentrations of selenate.
13 y (88-95%) organic C-Se-C; the remainder was selenate.
14 the grain more efficiently than selenite and selenate.
15                                              Selenate-(18)O enrichment (epsilonO) was nearly identica
16 o or supranutritional amounts of selenium as selenate (200 or 400 mug/d) or as selenomethionine (200
17 orms was higher for selenite (100%) than for selenate (26%), the absolute concentration of organosele
18 than that measured from plants supplied with selenate, 38 times higher than from selenite, and six ti
19                 The mutants are resistant to selenate, a toxic analogue of sulfate.
20 (-1)DM) and the concentration (2-mmol sodium selenate) above which the content of phenolic compounds
21 cation of Se reduction and assimilation from selenate accumulated in the cladode tips into the two LC
22 teria had dramatically enhanced tolerance to selenate and a reduced level of Se accumulation.
23 ontent was lower in plants supplemented with selenate and accumulated mainly in the leaves compared w
24 ysis showed that cladode tips contained both selenate and C-Se-C forms.
25 ke step caused by diffusive exchange between selenate and chloride followed by a slower, high-fractio
26 h) assays, using different concentrations of selenate and competitor sulfate.
27 in mixed-type inhibition, in the presence of selenate and potassium thiocyanate.
28                     Herein, the mechanism of selenate and selenite adsorption on NU-1000 is explored
29 ested for their ability to adsorb and remove selenate and selenite anions from aqueous solutions.
30 ung leaf itself, there was 30% inorganic Se (selenate and selenite) in addition to 70% MeSeCys.
31  products, two foliar Se fertilisers (sodium selenate and selenite) were tested at four rates (0-10-2
32  capacity, and fastest uptake rates for both selenate and selenite, of all zirconium-based MOFs studi
33 e 53 nM (4.2 ppb Se) and 380 nM (30 ppb) for selenate and selenite, respectively.
34 ate-limiting steps in Se volatilization from selenate and selenite, time- and concentration-dependent
35 ed in high mortality to embryos/larvae while selenate and SeNPs were nontoxic.
36  from the elements, DeltaH(f,el), for Al(13) selenate and sulfate are -19,656.35 ( +/- 67.30) kJ.mol(
37  degrees C in 5 N HCl for the epsilon-Al(13) selenate and sulfate are -924.57 (+/- 3.83) and -944.30
38  affinity of the epsilon-Keggin clusters for selenate and sulfate, the enthalpy associated with two S
39 slow rate of oxygen isotope exchange between selenate and water under most environmental conditions d
40  The rate of oxygen isotope exchange between selenate and water was investigated at conditions of 10
41 sures, we examined the toxicity of selenite, selenate, and amorphous selenium nanoparticles (SeNPs).
42 rtant implications for the fate of chromate, selenate, and sulfate in subsurface environments and off
43 rized the adsorption mechanisms of chromate, selenate, and sulfate on Al-substituted ferrihydrite (0,
44 ctron acceptors such as antimonite, nitrate, selenate, and sulfate.
45                                     For both selenate- and selenite-supplied plants, Se accumulation
46  selectivity for the tetrahedral sulfate and selenate anions observed in competitive crystallization
47                      With either selenite or selenate as substrates, Se methylation was highly effici
48 btain energy by respiring anaerobically with selenate as the terminal electron acceptor.
49 e to dimethyl selenide (DMSe): (a) uptake of selenate, (b) activation of selenate by ATP sulfurylase,
50 4 mm or more behind the apex when exposed to selenate but in the meristem (approximately 1 mm from th
51 nificantly up-regulated in plants exposed to selenate but were low in plants supplied with selenite.
52 ): (a) uptake of selenate, (b) activation of selenate by ATP sulfurylase, and (b) conversion of selen
53  experiments were performed with selenite or selenate by equilibrating suspensions containing the nan
54                        A new organic-soluble selenate, [(C6H5)4P]3(O3SeOCH2OSeO3)(HSeO4), was synthes
55                                 As a result, selenate can be quantified in the presence of up to 1.5
56 m jarosite, TlFe3(OH)6(SO4)2, along with the selenate-capped jarosite analogues of potassium, KFe3(OH
57                                   Molybdate, selenate, chromate ("chromium VI"), arsenate, tungstate,
58                                              Selenate, chromate, and arsenate produce transient APX i
59 es in selenium speciation, with selenite and selenate co-occurring in most samples.
60 lubility product very similar to that of the selenate complex.
61 elenomethionine, sodium selenite, and sodium selenate) compounds.
62 s soil, or on gravel supplied with different selenate concentrations.
63         In addition, DeltaH(f,el) for sodium selenate decahydrate was calculated using data from high
64 t environmental conditions demonstrates that selenate-delta(18)O signatures produced by biogeochemica
65 that it will be possible to use the value of selenate-delta(18)O to investigate the biogeochemical be
66  and seleno-methionine exert this effect but selenate does not.
67 lated around ten times more efficiently than selenate due to different membrane transporters.
68 the kinetic isotope effects for (18)O within selenate during abiotic reactions with iron-bearing hydr
69             The sulfate:arsenate and sulfate:selenate exchange ratios were 1:2 and 1:1, respectively.
70                   Plants exposed to 5 microM selenate for 28 days contained predominantly selenate in
71  and for selenate on schwertmannite, whereas selenate forms outer-sphere complexes in the aluminum oc
72 rpose of this study was to determine whether selenate fortification of infant formula would improve t
73                                              Selenate fortification of infant formulas can improve th
74  (n = 7, mean body weight = 1312 g) received selenate-fortified preterm and full-term infant formulas
75 lenium (Se), occurring as oxidized inorganic selenate from hypersalinized agricultural drainage water
76            Cv removed 96% of Se (supplied as selenate) from the microcosm water column within 72 h, w
77 hwertmannite and 3 times higher than that of selenate in both phases.
78                                    Inorganic selenate in drainage water was metabolized differently i
79            Thereby, the biotransformation of selenate in pakchoi was similar to other Brassicaceae pl
80 selenate for 28 days contained predominantly selenate in the mature leaf tissue at a concentration of
81 o investigate the biogeochemical behavior of selenate, in an analogous fashion to the use of sulfate-
82  and subsequent oxidation/elimination of the selenated intermediate 14 with H2O2.
83 ted by supplementing inorganic selenium from selenate into sand.
84 luminite and schwertmannite for arsenate and selenate is compared, and the coordination geometries of
85  indicating that the ability to biotransform selenate is either inducible or developmentally specific
86 Our data suggest that Se volatilization from selenate is limited by the rate of selenate reduction, a
87    Root transcriptome changes in response to selenate mimicked the effects observed under sulfur star
88 num centered epsilon-Keggin clusters, Al(13) selenate, (Na(AlO(4))Al(12)(OH)(24)(SeO(4))(4)*12H(2)O)
89  The enzyme is specific for the reduction of selenate; nitrate, nitrite, chlorate, and sulfate were n
90 f ligand for arsenate on both phases and for selenate on schwertmannite, whereas selenate forms outer
91                When grown in the presence of selenate or selenite, these bacteria produced both organ
92 own in hydroponic solution supplemented with selenate or selenite.
93 um compared with plants supplied with SeMet, selenate, or selenite; they also accumulated more Se in
94 onally have evolved enhanced specificity for selenate over sulfate.
95 (approximately 5 microM), sulfate, chromate, selenate, phosphate, and chlorate did not bind even when
96 d classes of oxo compounds (i.e., vanadates, selenate, phosphate, sulfate, acetate, nitrate, and nitr
97 methylseleno-Cys concentration is lower, and selenate predominates.
98                      Specifically, uptake of selenate (probably by sulfate transporters) occurred at
99 after the initial uptake step, the extent of selenate reaction is well correlated with delta(18)O val
100 er culture death, with 1.3-6.1% of the added selenate recovered as organic metabolites.
101 e replicated in the laboratory via anaerobic selenate-reducing enrichment cultures.
102                                          The selenate reductase contains molybdenum, iron, and acid-l
103 n, and pH optimization of the membrane-bound selenate reductase from E. cloacae SLD1a-1.
104         Results show that the membrane-bound selenate reductase has optimum activity at pH approximat
105 elenium methyltransferases and a respiratory selenate reductase have also been described.
106                           The membrane-bound selenate reductase of Enterobacter cloacae SLD1a-1 is pu
107 eta-subunits of microbial nitrate reductase, selenate reductase, dimethyl sulfide dehydrogenase, ethy
108 on of selenate to selenite is catalyzed by a selenate reductase, previously shown to be located in th
109 tudies constitute the first description of a selenate reductase, which represents a new class of enzy
110 These results also indicate that sulfate and selenate reduction are developmentally correlated, and t
111 TPS and APR had a significant enhancement of selenate reduction as a proportion of total Se, whereas
112  that ATPS and APR are major contributors of selenate reduction in planta.
113 ession resulted in only a slight increase in selenate reduction to organic forms.
114 ntribute to Se isotope forensics to identify selenate reduction within field sites and to possibly di
115     APR2 is a key enzyme in both sulfate and selenate reduction, and its reduced activity in the loss
116 tion from selenate is limited by the rate of selenate reduction, as well as by the availability of Se
117 h other and to the previously isolated sel1 (selenate-resistant) mutants, and have been designated se
118 could be mediated by Fe(II)-rich minerals or selenate-respiring microorganisms.
119                           In the presence of selenate (Se((VI))), the precipitates formed remained sm
120                        Our results show that selenate (Se(VI)) is the dominant Se species in Rosita g
121 nt selenium oxyanions, selenite (Se(IV)) and selenate (Se(VI)), can be quantified down to 7.3 and 8.3
122 e, were optimised for five selenium species; selenate (Se(VI)), Selenite (se(IV)), selenocysteine (Se
123 rexpressors and wild type accumulated mostly selenate (Se(VI)).
124 ith selenocompounds (sodium selenite, sodium selenate, Se-Met, MeSeCys) or SeB [high-Se (H-SeB) or lo
125 amino acids" and related oxidation products, selenate, selenite, and other species relatable to the q
126 ous inorganic or organic species of Se (e.g. selenate, selenite, and Se-methionine [Met]) into gaseou
127 ession and SeMSC accumulation in response to selenate, selenite, and sulfate treatments showed that t
128 edium and amended with the selenium oxyanion selenate, selenite, or selenocyanate, produces volatile
129 d several SRM selective inhibitors including selenate, selenite, tellurate, tellurite, nitrate, nitri
130                         Besides selenite and selenate, selenosulfate was the most frequently occurrin
131                                              Selenate (SeO(4)(2-)) reduction to elemental selenium is
132 n selenium oxoanions selenite (SeO3(2-)) and selenate (SeO4(2-)) are toxic at intake levels slightly
133 onsumers of dissolved selenite (SeO3) versus selenate (SeO4) uptake into aquatic primary producer com
134                                              Selenate speciation (HSeO(4)(-) vs SeO(4)(2-)) also has
135 e- or SeMet-supplied wild-type plants and in selenate-supplied ATP-sulfurylase transgenic plants.
136 ic Se, most likely selenomethionine, whereas selenate-supplied plants accumulated selenate.
137 increased Se accumulation, whereas increased selenate supply increased sulfate accumulation in both r
138 nions examined were selenocyanate, selenite, selenate, tellurite, and tellurate.
139 activity was increased more by both doses of selenate than by the placebo in C-P class B patients.
140 selenium was increased more by 400 mug Se as selenate than by the placebo in C-P class C patients.
141 gation in these mutants is less sensitive to selenate than in wild-type plants.
142           Within the groups who responded to selenate, there was a considerable variation in response
143 s for the assimilation and volatilization of selenate to dimethyl selenide (DMSe): (a) uptake of sele
144                             The reduction of selenate to selenite is catalyzed by a selenate reductas
145 able to reduce selenite aerobically, but not selenate, to nano-Se.
146 CpNifS overexpression significantly enhanced selenate tolerance (1.9-fold) and Se accumulation (2.2-f
147      The present study showed that shoots of selenate-treated plants accumulated very low concentrati
148 of organoselenium (e.g. selenomethionine) in selenate-treated roots.
149 was actually approximately 5-fold higher for selenate-treated roots.
150        Root growth was adversely affected by selenate treatment in both ATPS and SAT overexpressors a
151 trations approximately 18-fold higher in the selenate treatment.
152                            Both selenite and selenate, two major inorganic forms of Se, are readily i
153 nvolve constitutive up-regulation of sulfate/selenate uptake and assimilation, associated with elevat
154 , 5 mM, 3 d) were also tested for effects on selenate uptake and sulfate transporters' expression.
155                               In S. pinnata, selenate uptake and translocation rates are constitutive
156 ed by 100-fold excess sulfate, which reduced selenate uptake by 100% in S. elata and 40% in B. juncea
157 entrations, apparently due to suppression of selenate uptake by sulfate, and insufficient nitrogen co
158 ccumulators S. elata and Brassica juncea for selenate uptake in long- (9 d) and short-term (1 h) assa
159                                          The selenate uptake rate for S. pinnata (1 h) was three- to
160                                  Sulfate and selenate uptake were investigated in both selenium (Se)
161  addition, high levels of sulfate suppressed selenate uptake, resulting in a dramatic reduction of Bo
162 sorption capacity but had a strong impact on selenate uptake, suggesting some kind of specific intera
163 expression and interactions with sulfate and selenate uptake.
164  doubt by the high peak at its position in a selenate versus sulfate difference Fourier.
165 ulfur, plants readily take up and assimilate selenate via sulfur transporters and enzymes and can eve
166     Based upon bulk solution concentrations, selenate was 9-fold more toxic to the roots than selenit
167                                   The Km for selenate was determined to be 16 microM, and the Vmax wa
168                                              Selenate was found to be stable throughout the entire di
169                                              Selenate was metabolized less than selenite in whole pla
170 n and Se dose for both fertilisers, although selenate was much more efficient.
171                                              Selenate was rapidly translocated to the shoot, away fro
172                                              Selenate was reduced to Se(0) by a green rust (chloride
173                                              Selenate was successfully bioremediated by microalgal me
174   Time-dependent kinetic studies showed that selenate was taken up 2-fold faster than selenite.
175         Laboratory algal cultures exposed to selenate were shown to produce and release selenomethion
176        It should be stressed that amounts of selenate were smaller than expected.
177 and inorganic selenium species (selenite and selenate) were not detected in the dialyzate.
178  accumulated relatively more C-Se-C and less selenate when growing adjacent to S. pinnata.
179 ulfate was the main mechanism for removal of selenate, whereas arsenate was removed by a combination
180 esPR plants showed directional growth toward selenate, while CP roots did not.
181 6-fold more Se and was tolerant to 20 microm selenate, while S. albescens suffered reduced growth, ch
182                    Simultaneous treatment of selenate with selenite significantly reduced SeMSC produ

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