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Conyza blinii is a unique traditional Chinese medicine growing in Sichuan, China, which has soils with an abundant iron content. This Fe-enriched environment contributes to a variety of terpenoids in C. blinii, such as blinin and saponin, which play an important role in the process of resisting abiotic stress. The relationship between Fe and terpenoid metabolism was studied to explore the Fe tolerance mechanism of C. blinii. In this study, C. blinii was treated with ferrous iron solutions, and the effect of ferrous iron on the synthesis of blinin and saponins was further studied by spectrophotometry and liquid chromatography. Additionally, gene expression was detected by qRT-PCR. Under ferrous treatment, the blinin content of C. blinii increased, while the total saponin content decreased. When the ferrous concentration reached 200 μM, the difference in metabolite production was the largest. Furthermore, it was found that blinin and saponins have synchronous and opposite accumulation trends, characterized by time dependence. The gene expression results of key enzymes in the MVA and MEP pathways showed the same trends. In this process, the expression of CbNudixs played a key role in switching the material flux between MVA and MEP by catalyzing the dephosphorylation of isoprenoid diphosphate. In this study, it was found that under ferrous iron stimulation, the terpenoid content in C. blinii was different, and the metabolic pathways of MVA and MEP were periodically regulated.

Some acidic red soils in hilly regions of subtropical China were degraded as a result of slope erosion following the removal of natural vegetation, primarily for fuel. Revegetation is important for the recovery of the degraded ecosystem, but plant growth is limited by the low fertility of eroded sites. One factor contributing to the low fertility may be low inoculum density of arbuscular mycorrhizal (AM) fungi. Compared to red soils under natural vegetation or in agricultural production, substrates on eroded sites had significantly lower AM fungal propagule densities. Thus, the management and/or application of AM fungi may increase plant growth and accelerate revegetation. Thirteen species of AM fungi were identified in red soils by spore morphology. Scutellospora heterogama, Glomus manihotis, Gigaspora margarita, Glomus aggregatum and Acaulospora laevis were among the most common according to spore numbers. Pot cultures were used to isolate and propagate 14 isolates of AM fungi indigenous to red soil. The effectiveness of each fungus in promotion of growth of mungbean was evaluated in red soil. For comparison, three isolates from northern China, known to be highly effective in neutral soils, and two isolates from Australia, known to be from acidic soil were used. Effectiveness was positively related to root infection (r 2 = 0.601). For two of these isolates, Glomus caledonium (isolated from northern China) and Glomus manihotis (an isolate indigenous to red soil), the applied P concentration giving the highest infection and response to infection was approximately 17.5 mg P kg−1 soil. In field experiments in which this concentration of P was applied, the five most effective isolates were tested on mungbean. The Glomus caledonium isolate from northern China was the most effective, followed by the indigenous Glomus manihotis isolate. The Glomus caledonium isolate was also shown to be effective on Lespedeza formosa, which is commonly used in revegetation efforts. We conclude that inoculation of plants with selected isolates of AM fungi may aid in revegetation efforts on eroded red soils in subtropical China.

Sulphur cycling was evaluated in a 20 to 60 year old Norway spruce (Picea abies L. Karst) ecosystem in the Black Forest near Schluchsee, SW Germany, by means of stable sulphur isotope analysis. Soil and plant material were analysed for S-content and S-isotopic composition to gather information on the S-distribution in the ecosystem. Two out of three adjacent watershed areas, highly comparable to each other were fertilized with MgSO4 and (NH4)2SO4 respectively, where sulphate was enriched in the 34S-isotope compared to the sulphur present in the ecosystem. As the fertilizer S served as a tracer, comparison of the S-isotopic composition of total and inorganic S in the soil and S in spruce needles from both the treated and the control sites led to new information of S-turnover processes. The S-isotopic composition of spruce needles changed markedly after the fertilizer application. Within half a year a shift towards the S-isotopic composition of the fertilizers sulphate indicated uptake of the sulphate by the trees, although this uptake did not become visible with the S content of the needles. Regarding the soil, a shift in the S-isotopic composition of the total sulphur was not that striking as with the needles, although the phosphate extractable sulphate showed a clear shift towards the S-isotopic composition of the fertilizer sulphate.

Immobilization and mineralization of the tracer nitrogen (K15NO3) applied to the soil together with several organic matters during their decomposition was investigated in incubation experiments. After incubation for three months at 30°C, the decomposition rates of rice straw, hardwood bark, sawdust, softwood bark and peat moss were 41, 15, 7, 5, and 5%, respectively. After incubation for three months at 30°C, 100 and 80% of the fertilizer nitrogen were immobilized in the treatment with 2.0% of rice straw and sawdust carbon, respectively. These resulted in the lowered uptake of the fertilizer nitrogen by plants. In case of peat moss and barks, the amount of fertilizer nitrogen which transformed to the organic nitrogen fractions was quite small and the plant uptake of the nitrogen was hardly affected. Remineralization of the immobilized nitrogen was clearly observed after 2 months' incubation in case where rice straw carbon was added to the extent of 0.5 and 1.0%, but it was not observed in case where other organic matter carbon was added. The data showed that peat moss and barks were highly resistant to the action of microorganisms. As a results the immobilization process of the fertilizer nitrogen incubated with these organic matter was quite slow.

We investigated the effects of three plant growth promoting rhizobacteria (PGPR), on Biological Nitrogen Fixation (BNF), nodulation and growth promotion by soybean (Glycine max) var. Osumi plants. The strains, Aur 6, Aur 9 and Cell 4, belong toPsedomonas fluorescens, Chryseobacterium balustinum andSerratia fonticola, respectively. Inoculation modes for the PGPRs andSinorhizobium fredii (carried out through irrigation), were examined. In the first mode, PGPRs andS. fredii were co-inoculated. In the second mode, we first inoculatedS. fredii and after the PGPRs, which were added 5 or 10 days later (each inoculation being an independent treatment). In the third mode, the PGPRs were inoculated first, and theS. fredii was inoculated 5 days later. We also included treatments inoculated with only the PGPRs (one PGPR per treatment) and only withS. fredii. Plants were maintained in a greenhouse under controlled environmental conditions, and were sampled 3 months after sowing. The results obtained showed the effects of the inoculation sequence. The most significant effects on growth parameters (stem plus leaf weight and fresh root weight) were found when inoculations with PGPR andS. fredii were at different times or when we inoculated only with PGPR and the plants were watered with nitrogen. Co-inoculation had no positive effects on any parameter, probably due to competition between the PGPR andS. fredii. Our results indicate that the inoculation modes with PGPR and rhizobia play a very important role in the effects produced. Thus, although plant growth promoting rhizobacteria may interact synergistically with root-nodulating rhizobia, plant growth promoting rhizobacteria selected for one crop should be assessed for potentially hazardous effects on other crops before being used as inoculants.

Suitable N source supply is critical to improve plant growth and N uptake, but the importance of nitrate (NO3−) for rice (Oryza sativa L.) and microbiota is often neglected in acidic paddy soils where ammonium (NH4+) is dominant. This study aimed to explore the differential effects of NH4+ and NO3− on rice growth, fertilizer nitrogen recovery efficiency (FNRE), and rhizosphere bacterial community in acid soil. Two rice varieties, Kasalath (Al-sensitive indica) and Koshihikari (Al-tolerant japonica), were exposed to different N sources with or without lime in an acid soil. Liming and NO3− application solely improved the growth and FNRE of the Al-sensitive rice, namely, by increasing soil pH and alleviating Al toxicity. Compared with liming and rice variety, N source had a more pronounced influence on rhizobacterial community composition. Of the two sources, NO3− had a stronger effect on the rhizobacterial community than NH4+. Remarkably, rice plants fed with NH4+ specifically recruited Desulfosporosinus and Desulfitobacterium associated with ferric NH4+ oxidation in the rhizosphere, whereas those exposed to NO3− recruited Alicyclobacillus with NO3−-reducing iron oxidation ability. Three keystone taxa were identified in a rhizobacterial co-occurrence network analysis: Alicyclobacillus, which was positively associated with rice growth and FNRE, and Acidobacteriales and WPS-2, both with negative associations. Compared with NH4+, NO3− enhances the growth and FNRE of Al-sensitive rice and exerts dominant effects on the rhizobacterial community, which indicates the importance of NO3− for rice and has instructive implications for N management in acid soil.

1. Studies of the transformation of urea and ammonium sulphate in the Sudan Gezeira soil, when incubated under field conditions in polythene bags, were carried out with two rates of nitrogen, different moisture levels and frequency of wetting and drying during the winter and summer months. 2. The pattern of the transformation was nearly the same for the two levels of nitrogen added but there was a difference in magnitude. Urea hydrolysis was arrested during the first week in the open-bag system in the summer months. A low recovery of ammonia with ammonium sulphate and urea was associated with early ammonia volatilization losses. 3. There was a marked accumulation of nitrite in the first two weeks especially in moist closed bags, thereafter it decreased to low values. 4. Nitrate accumulated gradually under winter conditions, more so with closed bags than open ones. By contrast, little nitrate nitrogen was formed during the hot summer months, this being associated with high ammonia accumulation throughout the incubation period.

Durum wheat is sensitive of acid soils because it lacks effective genes for Al3+ tolerance. Previous research showed introgression of the TaMATE1B and TaALMT1 genes individually increased the Al3+ tolerance of durum wheat. Here we aimed to (a) combine the genes into a single durum line, (b) compare the various introgression lines and (c) establish the effectiveness of the introgressions in improving the acid soil tolerance in the field. Durum wheat lines homozygous for Al3+-tolerant alleles of TaMATE1B and TaALMT1 were crossed to develop a line that incorporated both genes. The parental cultivar, lines with the individual genes and the line with both genes introgressed were screened for Al3+ tolerance by hydroponic and soil cultures in a growth cabinet. The lines were also assessed for biomass production and grain yield in the field on acid soils. The durum wheat lines with the various Al3+-tolerance genes introgressed performed better based on root growth than Jandaroi, the parental cultivar, in both hydroponic and soil assays when grown in a cabinet. The various introgression lines were tolerant of acid soils compared to Jandaroi when grown in the field as assessed by shoot biomass and grain yield. The TaALMT1 and TaMATE1B genes improve the acid soil tolerance of durum wheat with indications that combining both genes is the most effective strategy. The various lines will be valuable to breeders who wish to enhance the acid soil tolerance of durum germplasm.