猪孤雌激活胚胎的体外培养系统优化

胚胎体外培养的气相条件、培养基及生长因子是影响胚胎发育的关键因素。系统研究不同氧分压（7%O2和20%O2）和三种胚胎培养基(NCSU-23、 PZM-3、G3)及表皮生长因子(EGF)和碱性成纤维促进因子(bFGF）对孤雌激活胚胎的囊胚发育率及囊胚细胞数的影响。结果表明，与高氧(20%O2)条件相比，低氧条件下（7%O2）提高了胚胎的囊胚率和细胞数，有利于胚胎的发育。PZM-3能显著提高囊胚细胞数（P < 0.05，51.0±4.0 vs. 38.8±2.2），无论在高氧还是低氧下，PZM-3都是胚胎发育的一个效果稳定、高效的培养基。添加10ng/mL EGF或bFGF的NCSU-23对提高胚胎的囊胚发育率有显著效果（P < 0.05，36.2±5.3％，44.3±5.8％ vs. 20.7±6.3％），但不能提高囊胚细胞数（P > 0.05）。     

Clay mineral composition of river sediments in the Amazon Basin

Clay minerals are important in evaluating the maturity of suspended sediments, weathering intensity and source area. However, there are processes that can change the mineral assemblage such as river transportation, deposition, remobilization and tributary inputs. In terms of water discharge and sediment yield, the Amazon is one of the largest rivers in the world. Most of the suspended sediments come from the Andes, crossing the lowlands before reaching the ocean. This study measures the spatial distribution of clay mineral assemblages over the entire Amazon basin. The results obtained show the main features of the Amazon River main stem and larger tributaries from their sources to their confluence. Clay mineral composition highlights the evolution of the Madeira and Marañón–Solimões River, which start in the Andes with high illite + chlorite content. Downstream, smectite contents increase. Moreover, all shield tributaries show high kaolinite content. The lower Amazon River is characterized by relative high smectite content, different from the Andean sources. The clay mineral results show that suspended sediments of the Amazon River have three main sources: 1) the Andes mountains; 2) the Amazon shields and 3) the Piedmont basins, especially the Pastaza alluvial megafan and the Fitzcarrald Arch basin. Lateral bank erosion plays also a significant role, by the introduction of more mature sediments into the river, enriched in smectite.     

Germination and hyphal growth of Glomus mosseae in vitro: Effects of rhizosphere bacteria and cell-free culture media

Germination and growth of chlamydospores of the vesicular-arbuscular (VA) mycorrhizal fungus Glomus mosseae on water-agar medium under axenic conditions were compared after treatment with washed cells, cell-free supernatants and complete bacterial cultures. Spore germination was not affected by bacterial treatments, but the additions of complete bacterial cultures and cell-free supernatants significantly (P ⩽ 0.05) stimulated hyphal growth and the number of new vegetative vesicles formed per germinated resting spore.     

Comparison of the mineral composition of twelve standard nutrient solutions

In the past, a large number of standard nutrient solutions has been devised. To investigate if there is an essential difference between these standard solutions, the mineral composition of 12 standard nutrient solutions formulated between 1865 and 1994 are compared with each other. Half of these standard solutions contain ammonium (NH₄ ⁺) in a millimolar range. The effect of elemental speciation of the micronutrients in the 12 standard solutions on bioavailability is compared. The macronutrient composition is represented in trilinear coordinates, making a clear comparison of the proportions of both the cations and the anions possible. Also the pH and the total amount of ions present are compared.     

Clay mineral composition of some volcanogenous soils in Indonesia and the Philippines

Clay fractions of three Andosols and a Latosol occurring in Indonesia, and two Alluvial Soils derived from pyroclastic sediments in the Philippines were examined by means of chemical analyses, X-ray diffraction, differential thermal analysis, thermogravimetry, infrared absorption spectroscopy, and electron microscopy. The results are summarized as follows.

Allophane is a dominant clay mineral of young volcanogenous soils occurring in the tropics. Small amounts of halloysite, gibbsite, and imogolite are also found in some of the young volcanogenous soils. Halloysite and imogolite are relatively abundant in the surface soil, while gibbsite is more abundant in the subsoil. In the clay fraction of the young volcanogenous soils in the tropics, α-cristobalite is often present, but quartz occurs rarely. Small amounts of feldspars are also present in the Philippine soils. 2 : 1-type minerals are found to a small extent in some of the sample soils. The above results agree well with the results for Japanese Andosols, except for a difference in the primary mineral composition.     

Analysis of the mineral composition of taro for determination of geographic origin

The mineral composition of taro ( Colocasia esculenta (L.) Schott) was analyzed to develop a method to distinguish taro produced in Japan and China. The concentrations of 15 elements (Al, Ca, Cl, Mg, Mn, Br, Co, Cr, Cs, Fe, K, Na, Rb, Sc, Zn) were assayed using instrumental neutron activation analysis. The concentrations of NO(3)(-), SO(4)(2-), H(2)PO(4)(-), Cl(-), malate, and oxalate were measured by ion chromatography. The mean concentrations of H(2)PO(4)(-), Co, Cr, and Na significantly differed (P < 0.01) between taro grown in Japan and that grown in China. Discriminant analysis was performed to identify the most efficient combination of elements and compounds to discriminate the taro geographic origin. The highest percentage of correct classification was achieved with a two-variable model including H(2)PO(4)(-) and Co (100% for Japanese, 93.75% for Chinese). Principal component analysis and cluster analysis using all of the assayed elements and compounds were also conducted to determine which elements significantly accounted for the variation of the taro mineral composition. We report on the potential of H(2)PO(4)(-) and Co concentrations to differentiate taro grown in China and Japan and discuss the sources of variability in the taro mineral composition of our samples.     

Statistical differentiation of bananas according to their mineral composition

The concentrations of Na, K, Ca, Mg, Fe, Cu, Zn, and Mn were determined in banana cultivars Gran enana and Peque?a enana cultivated in Tenerife and in cv. Gran enana bananas from Ecuador. The mineral concentrations in the bananas from Tenerife and from Ecuador were clearly different. The cultivar did not influence the mineral concentrations except in the case of Fe. Variations according to cultivation method (greenhouse and outdoors) and farming style (conventional and organic) in the mineral concentrations in the bananas from Tenerife were observed. The mineral concentrations in the internal part of the banana were higher than those in the middle and external parts. Representation of double log correlations K-Mg and Zn-Mn tended to separate the banana samples according to origin. Applying factor and cluster analysis, the bananas from Ecuador were well separated from the bananas produced in Tenerife, and therefore, these are useful tools for differentiating the origin of bananas.     

Effect of turnip mosaic virus infection on the mineral composition of rutabaga

Abstract

The effect of Turnip Mosaic Virus (TuMV) infection on the elemental composition of rutabaga (Brassica napus ssp. rapifera (Metzg) Sinsk) at maturity was examined in the greenhouse. TuMV infection markedly reduced dry weight and dry matter percentage of leaves‐plus‐petioles but did not affect storage root development. Virus‐infected plants exhibited higher N, P, Mg and Zn, but lower K levels in leaf tissues. Nitrogen, Ca, Mg and Mn accumulated in storage root tissues as a result of TuMV infection.     

Effect of the anion citrate on the mineral composition of artificial casein micelles

The composition of artificial casein micelles (ACM) prepared at constant concentration of caseins, calcium (Ca), and phosphate (P(i)) in media with different citrate (Cit) concentrations was studied. The incorporation of the different mineral and protein components to the ACM was conditioned by the Cit concentration. In our working condition, the ACM size remained almost constant for Cit concentration ranging from 7 to 10 mM. This behavior could be indicating that the action of Cit essentially consists of a regulation of the Ca activity. The molar ratio at which Ca and P(i) were incorporated to the ACM varied for different Cit concentrations. At decreasing pH, the Ca/P(i) molar ratios for the remanent ions in the ACM were dependent on the Cit concentration. These observations could be related to a certain kind of competition between Cit, micellar calcium phosphate (MCP), and other groups able to bind Ca in the ACM.     

牛磺酸、谷酰胺、改良CR1和改良CR2培养液对牛受精卵体外发育的影响

本研究探讨了牛磺酸、谷酰胺、改良CR1 (CR1 无机盐成分 10% 胎牛血清) 和改良CR2 培养液(改良CR1 液 1 m m ol/L谷酰胺和绵羊输卵管分泌液浓度的多种氨基酸)对牛卵子体外受精后的分裂率、囊胚率和囊胚细胞数的影响。结果表明: 牛磺酸和谷酰胺对牛卵子受精后体外发育的影响依赖于胚胎培养液种类; 利用改良CR1 和改良CR2 培养液可成功生产可移植胚胎, 但它们所生产的可移植胚胎的效率无显著差异, 利用改良CR1 培养液生产可移植胚胎的成本更低一些。     

Mineral nutrition of Gypsophila in vitro root culture

Mineral nutrition of panicled gypsophila roots (Gypsophila paniculata L.) (Caryophyllaceae) cultivated in vitro in two media with different mineral composition, a classical Gamborg's B5 medium and a modified MH3 medium, was studied over a growth cycle of 28 days, by continuous measurement of mineral element consumption, without opening the culture flasks. The comparison between the total mineral element quantities consumed from media and those absorbed by roots at harvesting showed a good correspondence, proving the validity of the technique used and the absence of insolubilized mineral forms in the in vitro culture media. The mineral element composition of the MH3 medium was found to be better suited to Gypsophila paniculata root culture since all mineral nutrient elements are supplied in adequate quantities which are non‐limiting and non‐excessive. Culture on B5 medium showed that phosphorus (P) and copper (Cu) are probably the factors limiting growth and revealed an ammonium (NH₄ ⁺)/potassium (K⁺) ion antagonism. The in vitro roots, although uncoupled from the aerial part, behave like the roots of whole plants in several ways: the evolution of the medium pH corresponds to the form of the mineral nitrogen (N) consumed by the roots; sodium (Na) and chloride (Cl) are barely consumed and may be considered as non‐essential elements. Lastly, this in vitro root culturemodel makes itpossible to explain that the absorption of Na and Cl by the roots of whole plants is probably dependent on the transpiratory flow of the aerial part.     

Microbial community composition affects soil organic carbon turnover in mineral soils

Soil organic carbon (SOC) turnover is the most ubiquitous and ecologically fundamental process in soils. It is generally assumed that SOC is utilised by functionally redundant soil-specific microbial communities which do not differ in their capability to mineralise soil organic matter. To challenge this assumption, incubation experiments were conducted to analyse the community-specific effects on SOC turnover for six mineral soils under different land-use. Comparisons of respiration by a native soil community and an alien community both inoculated to sterilised soils revealed 29 ± 18% higher respiration by the native community (‘home-field advantage’). Increased soil microbial community diversity, as generated by mixing several microbial inoculants, did not result in increased mineralisation rates. Even under impaired conditions, in the presence of aged engine oil as a less decomposable substance, communities with higher diversity did not show higher respiration rates. Also, in non-sterilised soils, we detected the influence of the microbial community composition on respiration rates: Investigations on the effect of mixing two communities in a 50:50 untreated soil mixture showed declining respiration in three out of six cases (by 23.9 ± 5.9%) and increased respiration in one case (by 57%) compared to the mean respiration of the two unmixed soils. These effects were highly related to the microbial community capability, with only communities with low capability profiting from mixing with a second community. Our results question the assumption of redundancy of microbial community’s functionality for SOC mineralisation in soils.     

Phosphate fixation by ando soils different in their clay mineral composition

The phosphate fixation capacity at pH 4.5 and an equilibrium concentration of 250 mM phosphate was measured. The soil samples were divided into five groups according to their clay mineralogical composition. The first group soils contain opaline silica and allophanelike constituents, and some unidentified minerals, the second opaline silica and crystalline layer .i1icates, the third opaline silica and crystalline layer silicates with additional allophanelike constituents or aluminarich gel-like materials, the fourth allophanelike constituents, allophane and imogolite and the fifth crystalline layer silicates, allophanelike constituents and alumina-rich gel-like materials, plus some halloysite-like minerals, respectively. The first group soils had phosphate fixation capacities of 3,000 to 8,000, the second group soils 1,000 to 3,000, the third group loib 2,000 to 13,000, the fourth group soils 8,000 to 15,000 and the fifth group soil. 5,000 to 12,000 mg P₂O₅/100 g oven-dry soil, respectively. The fourth group soils in which allophane and imogolite predominated showed the highest phosphate fixation capacity.

The fractions which dissolved from almost all soil samples by treatments with 6% H₂O₂ Na₂S₂O₄-NaHCO₂-Na citrate and 2% Na₂CO₃ were estimated to have very high phosphate fixation capacities (8,000 to 19,000 mg P₂O₅/100 g dry-matter), and there was not much difference among the soil samples examined. Iron and aluminum combined with humus, allophanelike constituents, alumina-rich gel-like materials and halloysite-like minerals in addition to allophane and imogolite contribute to the phosphate fixation of Ando soils.     

Influence of mineral nutrition on denitrification on plants in nutrient solution culture

In solution culture experiments with spring wheat the effect of nitrogen sources, single nutrient deficiency and oxygen supply of the nutrient solution on denitrification was studied by means of the acetylene inhibition method. No denitrification was observed with ammonium nutrition, while denitrification was almost equally high with nitrate and a mixture of nitrate and ammonium nutrition. Discontinuing potassium for 7 and 14 days increased denitrification. Discontinuation of P for 14 days also increased total denitrification, whereas no difference from the complete nutrient solution was observed in Fe deficiency. Denitrification remained at a very low level, when Mg supply was discontinued. Denitrification potential of excised roots was high in K deficiency. It was also high at the beginning of Fe deficiency, whereas P and Mg deficiency had no effect on denitrification potential as compared to roots in complete nutrient solution. The differences in total denitrification are due to the effects of individual nutrient deficiency on root growth, root respiration and denitrification potential.     

Soil fauna alter the effects of litter composition on nitrogen cycling in a mineral soil

Plant chemical composition and the soil community are known to influence litter and soil organic matter decomposition. Although these two factors are likely to interact, their mechanisms and outcomes of interaction are not well understood. Studies of their interactive effects are rare and usually focus on carbon dynamics of litter, while nutrient dynamics in the underlying soil have been ignored. A potential mechanism of interaction stems from the role fauna plays in regulating availability of litter-derived materials in the mineral soil. We investigated the role of soil fauna (meso, macro) in determining the effect of surface-litter chemical composition on nitrogen mineralization and on the micro-food web in mineral soils. In a field setting we exposed mineral soil to six types of surface-applied litter spanning wide ranges of multiple quality parameters and restricted the access of larger soil animals to the soils underlying these litters. Over six months we assessed litter mass and nitrogen loss, nitrogen mineralization rates in the mineral soils, and soil microbes and microfauna. We found evidence that the structure of the soil community can alter the effect of surface-litter chemical composition on nitrogen dynamics in the mineral soil. In particular, we found that the presence of members of the meso- and macrofauna can magnify the control of nitrogen mineralization by litter quality and that this effect is time dependent. While fauna were able to affect the size of the micro-food web they did not impact the effect of litter composition on the abundance of the members of the micro-food web. By enhancing the strength of the impact of litter quality on nitrogen dynamics, the larger fauna can alter nitrogen availability and its temporal dynamics which, in turn, can have important implications for ecosystem productivity. These findings contribute to evidence demonstrating that soil fauna shape plant litter effects on ecosystem function.     

栽培基质对小叶榕块根生长的影响

应用正交设计的方法,研究了不同栽培基质对小叶榕(6个月苗龄)块根生长的影响,结果表明,不同栽培基质对小叶榕块根的生长影响差异显著.经过6个多月的种植试验, 6份沙子+2份椰糠+3份草炭+1份豆粕为栽培基质的小叶榕在块根生长上明显高于其他处理.     

Potassium behavior and clay mineral composition in the soil with low effectiveness of potassium application

ABSTRACT

Increasing exchangeable potassium (ExK) content in soil to an appropriate level is important to mitigate the transfer of radioactive cesium to crops. We focused on a buckwheat (Fagopyrum esculentum Moench) field with a low ExK content, despite the application of K, in Fukushima Prefecture, Japan (Field A), following the Tokyo Electric Power Company Fukushima Dai-ichi (No. 1) Nuclear Power Plant accident in March 2011. We examined the relationship between K concentration and clay mineral composition in the soil of Field A and compared the findings with another field in Fukushima Prefecture (Field B) to clarify whether K applied to the soil was leached or remaining fixed. Pot experiments showed that K concentration in water seepage from pots following irrigation was significantly lower in pots from Field A than in those from Field B. Soil ExK content after soybean cultivation was lower in soils of Field A than those of Field B. These results indicate that K applied to Field A was fixed in the soil. Analysis of clay mineral composition confirmed the distinctive vermiculitic nature of Field A soils. This clay mineralogy would be associated with the higher K fixation ability of Field A than Field B soils. This study demonstrated that K fixation in vermiculite was a factor preventing the increase in ExK content from K application to Field A.     

Effects of aluminum on mineral content of mycorrhizal fungi in vitro

The influence of Al³⁺ on the mineral content of mycorrhizal fungi was studied in vitro. Amanita muscaria (L. ex Fr.) Pers. ex Hooker whose growth is reduced and Lactarius piperatus (L. ex Fr.) S.F. Gray whose growth is stimulated by Al³⁺ where chosen for the experiments. 0, 0.1, 1, and 10mM A³⁺ were added as Al₂(SO₄)₃ · 18H₂O to modified M-40 medium. Al³⁺ drastically affected the mineral contents of the mycelia of both fungi: the Al, Ca, and Na contents increased while P, Mg, and K decreased with the increasing Al³⁺ concentrations in the media. On the other hand, some important differences between the two mycelia were detected. In the mycelia of Lacterius piperatus grown on the control media, there was about twice as much Ca content and a three times lower P content than in the Amanita muscaria mycelia. The Al³⁺ content in the mycelia of Lactarius piperatus grown on 10mM Al³⁺ was six times higher than in Amanita muscaria at the same concentration.     

Transformation kinetics of corn and clover residues in mineral substrates of different composition

Mineralization kinetics of corn and clover residues in quartz sand, loam, sand + 15% bentonite, and sand + 30% kaolinite have been studied. A scheme has been proposed for the transformation of plant residues in mineral substrates. Kinetic parameters of mineralization have been calculated with the use of a first-order two-term exponential polynomial. It has been shown that the share of labile organic carbon pool in the clover biomass is higher (57–63%) than in the corn biomass (47–49%), which is related to the biochemical composition of plant residues. The mineralization constants of clover residues generally significantly exceed those of corn because of the stronger stabilization of the decomposition products of corn residues. The turnover time of the labile clover pool (4–9 days) in all substrates and that of the labile corn pool (8–10 days) in sands and substrates containing kaolinites and bentonite are typical for organic acids, amino acids, and simple sugars. In the loamy substrate, the turnover time of labile corn pool is about 46 days due to the stronger stabilization of components of the labile pool containing large amounts of organic acids. The turnover time of the stable clover pool (0.95 years) is significantly lower than that of the stable corn pool (1.60 years) and largely corresponds to the turnover time of plant biomass.     

Effect of chromium VI on mineral element composition of bush beans

Bush beans (Phaseolus vulgaris L. cv Contender) were grown on perlite with nutrient solution and 0, 1, 2.5 and 5 ppm levels of Na₂CrO₄ Significant decrease of top growth and chlorosis in trifoliated leaves were observed for 2.5 and 5 ppm Cr, with Cr concentrations (μg/g) in tops:≥ 12.1, in roots:≥ 509.9. Cr decreased K, Na, Mg and Fe concentrations, and increased P and Mn concentrations in roots. In tops decreased N, K, Na and Fe concentrations and increased Mn and Ca concentrations were observed, Translocation of P, Zn, Cu and Fe was inhibited; Ca and Mn translocation was generally enhanced. P/Fe ratio was increased up to 60% in chlorotic plants, indicating a shift from Fe²⁺ to Fe³⁺.