|
32P in plants (μmol g−1 DW roots) |
32P in roots (%) |
32P in leaves (%) |
---|
 | +Fe | -Fe | +Fe | -Fe | +Fe | -Fe |
---|
KH
2
32
PO
4
|
Ferrihydrite | 90.93 ± 5.46 a | 37.74 ± 5.66 B* | 49.2 | 69.5 | 50.8 | 30.5 |
Fe-Citrate | 104.00 ± 16.36 a | 63.51 ± 3.43 A* | 37.6 | 62.6 | 62.4 | 37.4 |
Fe-PS | 97.36 ± 8.66 a | 56.17 ± 2.09 A* | 44.7 | 68.1 | 55.3 | 31.9 |
(
32
P)Vivianite
|
Ferrihydrite | 0.11 ± 0.03 b | 0.13 ± 0.01 C | 76.0 | 88.7 | 24.0 | 11.3 |
Fe-Citrate | 0.11 ± 0.01 b | 0.13 ± 0.01 C | 76.9 | 88.3 | 23.1 | 11.7 |
Fe-PS | 0.11 ± 0.01 b | 0.19 ± 0.02 C* | 76.3 | 91.4 | 23.7 | 8.6 |
- The plant ability to accumulate P was evaluated by 32P uptake experiments on Fe-sufficient (+Fe) and Fe-deficient (−Fe) plants. Up to 24 h, −Fe and + Fe plants were treated with three unlabelled Fe-sources (Ferrihydrite, Fe-Citrate or Fe-PS) provided in conjunction with two different labelled 32P-sources: KH2
32PO4 or (32P)Vivianite. Data are means ± SD of three independent experiments. Small letters, refer to statistically significant differences among Fe-sufficient plants; capital letters, refer to statistically significant differences among Fe-deficient plants, asterisks, refer to statistically significant differences between the two growth condition (−Fe vs + Fe). ANOVA Holm–Sidak, P < 0.05, n = 3). DW, dry weight