| Literature DB >> 20652650 |
Jun Yan1, Fang Wang, Haibo Qin, Guoxiong Chen, Nevo Eviatar, Tzion Fahima, Jianping Cheng.
Abstract
Wild barley (Hordeum spontaneum), the progenitor of cultivated barley, is an important genetic resource for cereal improvement. Selenium (Se) is an essential trace mineral for humans and animals with antioxidant, anticancer, antiarthropathy, and antiviral effects. In the current study, the grain Se concentration (GSeC) of 92 H. spontaneum genotypes collected from nine populations representing different habitats in Israel was investigated in the central area of Guizhou Province, China. Remarkable variations in GSeC were found between and within populations, ranging from 0 to 0.387 mg kg(-1) among the 92 genotypes with an average of 0.047 mg kg(-1). Genotype 20_C from the Sede Boqer population had the highest GSeC, while genotype 25_1 from the Atlit population had the lowest. The mean value of GSeC in each population varied from 0.010 to 0.105 mg kg(-1). The coefficient of variation for each population ranged from 12% to 163%. Significant correlations were found between GSeC and 12 ecogeographical factors out of 14 studied. Habitat soil type also significantly affected GSeC. The wild barley exhibited wider GSeC ranges and greater diversity than its cultivated counterparts. The higher Se grain concentrations found in H. spontaneum populations suggest that wild barley germplasm confer higher abilities for Se uptake and accumulation, which can be used for genetic studies of barley nutritional value and for further improvement of domesticated cereals.Entities:
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Year: 2010 PMID: 20652650 PMCID: PMC3152716 DOI: 10.1007/s12011-010-8770-6
Source DB: PubMed Journal: Biol Trace Elem Res ISSN: 0163-4984 Impact factor: 3.738
Fig. 1Geographical location of Israeli Hordeum spontaneum populations used in the present study. 1, Mt. Hermon; 10, Maalot; 20, Sede Boqer; 22, Mehola; 24, Akhziv; 25, Atlit; 26, Caesarea; 32, Ein-Zukim; 37, “Evolution Canyon”
Ecogeographical Factors of the Nine Hordeum spontaneum Populations in Israel
| IDa | Population | Ln | Lt | Al | Tm | Ta | Tj | Td | Tdd | Ev | Rn | Rd | Hu14 | Huan | So |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 1 | Mt. Hermon | 35.75 | 33.28 | 1,530 | 11 | 20 | 1 | 19 | 6 | 160 | 1,400 | 70 | 52 | 58 | 1 |
| 10 | Maalot | 35.27 | 33.00 | 500 | 17 | 23 | 8 | 15 | 10 | 150 | 785 | 55 | 50 | 64 | 2 |
| 20 | Sede Boqer | 34.78 | 30.87 | 450 | 19 | 26 | 9 | 15 | 13 | 168 | 91 | 15 | 36 | 53 | 6 |
| 22 | Mehola | 35.48 | 32.13 | −150 | 22 | 30 | 13 | 17 | 13 | 180 | 270 | 39 | 34 | 53 | 3 |
| 24 | Akhziv | 35.10 | 33.05 | 10 | 20 | 26 | 12 | 13 | 10 | 130 | 620 | 56 | 60 | 67 | 3 |
| 25 | Atlit | 34.95 | 32.70 | 50 | 20 | 26 | 13 | 13 | 9 | 133 | 500 | 48 | 65 | 72 | 4 |
| 26 | Caesarea | 34.90 | 32.50 | 10 | 20 | 26 | 13 | 13 | 9 | 130 | 540 | 48 | 65 | 72 | 4 |
| 32 | Ein-Zukim | 35.44 | 31.74 | −200 | 24 | 31 | 15 | 16 | 12 | 210 | 100 | 20 | 35 | 52 | 6 |
| 37 | Evolution Canyon | 34.58 | 32.43 | 90 | 22.5 | 28 | 13 | 15 | 9 | 142 | 600 | 48 | 65 | 67 | 1 |
Geographical variables: Ln = longitude (decimal), Lt = latitude (decimal), and Al = altitude (meters). Temperature variables: Tm = mean annual temperature (°C), Ta = mean August temperature (°C), Tj = mean January temperature (°C), Td = mean seasonal temperature difference (°C), Tdd = mean daily temperature difference (°C), and Ev = mean annual evaporation. Water variables: Rn = mean annual rainfall (millimeters), Rd = mean number of rainy days, Hu14 = mean humidity at 1400 hours (percent), Huan = mean annual humidity (percent), and Dw = mean number of dewy nights in summer (millimeters). Dummy soil variables: So = soil types, 1 terra rosa, 2 rendzina, 3 alluvium, 4 sandy loam, 6 loess (desert soil)
aPopulation IDs and selected environmental data are based on [21]; Ein-Zukim data is based on [63]
Operating Parameters of the Hydride Generation-Atomic Fluorescence Spectrometry
| Parameters | Settings |
|---|---|
| Selenium hollow cathode lamp | 196.0 nm |
| Lamp current | 75 mA |
| Negative high voltage of photomultiplier | 265 V |
| Atomizer height | 8 mm |
| Atomization temperature | 200°C |
| Carrier HCL flow | 0.72 mol/L (6%) |
| KHB4 concentration | 1% ( |
| Carrier argon flow | 400 mL/min |
| Shield argon flow | 800 mL/min |
Fig. 2GSeC of 92 Hordeum spontaneum genotypes
GSeC of Nine Hordeum spontaneum Populations and Ten Hordeum vulgare Cultivars
| ID | Populations/variety | Samples | GSeC (mean ± SD; mg kg−1) | Range (mg kg−1) | CV (%) |
|---|---|---|---|---|---|
| 1 | Mt. Hermon | 9 | 0.015 ± 0.004 | 0.010–0.026 | 31 |
| 10 | Maalot | 10 | 0.019 ± 0.007 | 0.011–0.131 | 39 |
| 20 | Sede Boqer | 10 | 0.105 ± 0.133 | 0.010–0.387 | 128 |
| 22 | Mehola | 8 | 0.015 ± 0.004 | 0.010–0.021 | 27 |
| 24 | Akhziv | 8 | 0.015 ± 0.005 | 0.012–0.024 | 29 |
| 25 | Atlit | 8 | 0.010 ± 0.004 | 0.000–0.014 | 42 |
| 26 | Caesarea | 10 | 0.053 ± 0.087 | 0.010–0.244 | 163 |
| 32 | Ein-Zukim | 22 | 0.080 ± 0.072 | 0.015–0.211 | 90 |
| 37 | Evolution Canyon | 7 | 0.039 ± 0.046 | 0.014–0.123 | 12 |
| Sum of Wild barley | 92 | 0.045 ± 0.070 | 0.000–0.387 | 12–163 | |
| Zj1 | Yunpi 2 | 1 × 3 | 0.028 ± 0.003 | ||
| Zj2 | Yunpi 6 | 1 × 3 | 0.039 ± 0.008 | ||
| Zj3 | Zhexiu 12 | 1 × 3 | 0.134 ± 0.012 | ||
| Zj4 | E32380 | 1 × 3 | 0.073 ± 0.013 | ||
| Zj5 | Yangnongpi 5 | 1 × 3 | 0.077 ± 0.005 | ||
| Zj6 | Baoshan8640-1 | 1 × 3 | 0.000 ± 0.000 | ||
| Zj7 | Yancheng 01094 | 1 × 3 | 0.000 ± 0.000 | ||
| Zj8 | Zhexiu33 | 1 × 3 | 0.144 ± 0.010 | ||
| Zj9 | Ganpi 3 | 1 × 3 | 0.000 ± 0.000 | ||
| Zj10 | Supi 4 | 1 × 3 | 0.000 ± 0.000 | ||
| Sum of cultivars | 10 × 3 | 0.050 ± 0.056 | 0.000–0.144 | 112 |
Fig. 3Spearman's rho correlation between GSeC and ecogeographical data (Table 1) of the original sites of nine Hordeum spontaneum populations in Israel
GSeC of Hordeum spontaneum Originated From Five Different Soil Types in the Collection Site in Israel
| Soil type (in the collection site) | Samples | Population | Mean ± SD (mg kg−1) | Range (mg kg−1) | CV (%) | Tukey–Kramer HSD test, |
|---|---|---|---|---|---|---|
| 1, Terra Rosa | 16 | Mt. Hermon | 0.016 ± 0.004 | 0.010–0.026 | 23 | b |
| Evolution Canyon | ||||||
| 2, Rendzina | 10 | Maalot | 0.019 ± 0.007 | 0.011–0.031 | 39 | b |
| 3, Alluvium | 16 | Mehola | 0.015 ± 0.004 | 0.010–0.024 | 27 | b |
| Akhziv | ||||||
| 4, Sandy loam | 18 | Atlit | 0.034 ± 0.067 | 0.000–0.244 | 196 | b |
| Caesarea | ||||||
| 6, Loess | 32 | Sede Boqer | 0.088 ± 0.094 | 0.010–0.387 | 107 | a |
| Ein-Zukim | ||||||
| ANOVA |
|
aDifferent letters stand for significant differences among soil types