N+离子注入长豇豆对硝酸还原酶及氮代谢的影响

不同剂量的Ｎ＾＋离子注入长豇豆种子。豇豆开花结荚后，低剂量Ｎ＾＋离子处理能增加叶片的ＮＲ活性，促进ＮＯ＾－３－Ｎ向氨基酸和蛋白质的转化；减少ＮＯ＾－３－Ｎ的积累，提高叶片蛋白质和氨基酸含量。高剂量Ｎ＾＋离子处理抑制官种转化，豇豆结荚后期，叶片ＮＯ＾－３－Ｎ积累增多。     

Differences of Soil Microbial Biomass and Nitrogen Transformation under Two Forest Types in Central Germany

In order to observe the tree species effect on soil N status, soil microbial biomass C and N (C_mic, N_mic), potential N mineralization and potential nitrification (under laboratory incubation conditions, 22 °C) in different subhorizons (LOf₁, Of₂, Oh and mineral soil at 0–10 cm depth) were determined at three forest sites in central Germany. At each site, two contrasting stands (Beech, Norway spruce or Scots pine) were selected, where the initial soil conditions were similar. Three sampling dates that represented different stages of tree growth were selected: growing season - August, dormant season - November, after budbreak – April. In organic layers, C_mic-to-total C (C_t) ratios under beech and under conifer were 0.72–4.74% and 0.34–2.11%, respectively. N_mic-to-total N (N_t) ratios were 2.47–11.61% and 0.71–5.77%, respectively. Both concentrations of C_mic and N_mic were significantly affected by the stand type and sampling time. Potential N mineralization rates, ranging from 3.7 to 19.7 mg N kg⁻¹ d⁻¹, showed no clear pattern in relation to stand type. However, potential nitrification rates were mostly significantly higher under beech than under contrasting conifer. In mineral soils, concentrations of C_mic and N_mic showed a clear temporal pattern in the order: August>November>April. The average N_mic and N_mic-to-N_t were higher in soils from beech than conifer, while C_mic and C_mic-to-C_t ratios were similar between the two forest types. In organic layers, the highest values of C_mic-to-N_mic ratio and C_mic were found in November samples, especially under beech. By contrast, in mineral soils the highest value of C_mic-to-N_mic ratios were found in April samples, and at that time the C_mic concentrations were the lowest, especially under conifer. These results revealed the differences in microbial growth form and survival strategy associated with different tree species and soil layers.     

Transformation of14C labelled plant components in soil in relation to immobilization and remineralization of15N fertilizer

Summary Uniformly¹⁴C labelled glucose, cellulose and wheat straw and specifically¹⁴C labelled lignin component in corn stalks were aerobically incubated for 12 weeks in a chernozem soil alongwith¹⁵N labelled ammonium sulphate. Glucose was most readily decomposed, followed in order by cellulose, wheat straw and corn stalk lignins labelled at methoxyl-, side chain 2-and ring-C. More than 50% of¹⁴C applied as glucose, cellulose and wheat straw evolved as CO₂ during the first week. Lignin however, decomposed relatively slowly. A higher proportion of¹⁴C was transformed into microbial biomass whereas lignins contributed a little to this fraction.After 12 weeks of incubation nearly 60% of the lignin¹⁴C was found in humic compounds of which more than 70% was resistant to hydrolysis with 6N HCl. Maximum incorporation of¹⁵N in humic compounds was observed in cellulose amended soil. However, in this case more than 80% of the¹⁵N was in hydrolysable forms.Immobilization-remineralization of applied¹⁵N was most rapid in glucose treated soil and a complete immobilization followed by remineralization was observed after 3 days. The process was much slow in soil treated with cellulose, wheat straw or corn stalks. More than 70% of the newly immobilized N was in hydrolysable forms mainly reepresenting the microbial component.Serial hydrolysis of soil at different incubation intervals showed a greater proportion of 6N HCl hydrolysable¹⁴C and¹⁵N in fractions representing microbial material.¹⁴C from lignin carbons was relatively more uniformly distributed in different fractions as compared to glucose, cellulose and wheat straw where a major portion of¹⁴C was in easily hydrolysable fractions.     

Fate and Transport of High Explosives in a Sandy Soil: Adsorption and Desorption

Several areas of the Massachusetts Military Reservation (MMR) have soils with significant levels of high explosives (HE) contamination because of a long history of training and range activities (such as open burning, open detonation, disposal, and artillery and mortar firing). Site-specific transport and attenuation mechanisms were assessed in sandy soils for three contaminants of concern: the nitramine hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX), and the nitroaromatics 2,4-dinitrotolune (2,4-DNT) and 2,4,6-trinitrotoluene (TNT). For all three contaminants, linear distribution coefficients (K_d) were dependent on the fraction of organic carbon in soil. The nitroaromatics sorbed much more strongly than RDX in both soils. Over 120 hours, the desorption rate of RDX from field contaminated surface soil was much slower than its sorption rate, with the desorption K_d (1.5 L/kg) much higher than K_d for sorption (0.37 L/kg). Desorption of 2,4-DNT was negligible over 120 hours. Thus, applying sorption-derived K_d values for transport modeling may significantly overestimate the flux of explosives from MMR soils. Based on multiple component column transport tests, RDX will be the most mobile of these contaminants in MMR soils. In saturated columns packed with uncontaminated soil, RDX broke through rapidly, whereas the nitroaromatics were significantly attenuated by irreversible sorption or abiotic transformations.     

Fate and Transport of Naproxen in a Sandy Aquifer Material: Saturated Column Studies and Model Evaluation

Naproxen-C₁₄H₁₄O₃ is a nonsteroidal anti-inflammatory drug which has been found at detectable concentrations in wastewater, surface water, and groundwater. Naproxen is relatively hydrophilic and is in anionic form at pH between 6 and 8. In this study, column experiments were performed using an unconsolidated aquifer material from an area near Barcelona (Spain) to assess transport and reaction mechanisms of Naproxen in the aquifer matrix under different pore water fluxes. Results were evaluated using HYDRUS-1D, which was used to estimate transport parameters. Batch sorption isotherms for Naproxen conformed with the linear model with a sorption coefficient of 0.42 (cm³ g^?1), suggesting a low sorption affinity. Naproxen breakthrough curves (BTCs) measured in soil columns under steady-state, saturated water flow conditions displayed similar behavior, with no apparent hysteresis in sorption or dependence of retardation (R, 3.85-4.24) on pore water velocities. Soil sorption did not show any significant decrease for increasing flow rates, as observed from Naproxen recovery in the effluent. Sorption parameters estimated by the model suggest that Naproxen has a low sorption affinity to aquifer matrix. Most sorption of Naproxen occurred on the instantaneous sorption sites, with the kinetic sorption sites representing only about 10 to 40% of total sorption.     

Drainage and nitrate leaching in a crop rotation under different N-fertilizer strategies: application of capacitance probes

Quantification of drainage and nitrate leaching from cropping systems is necessary to optimize N-fertilizer application and determine the impact on groundwater quality. The objectives of this work were to (i) assess the use of capacitance probes for the continuous determination of the volume of drainage water and the amount of nitrate leached in a crop production system, and (ii) compare the effect of different N-fertilizer strategies to control nitrate leaching in a crop rotation in humid Mediterranean climate. A factorial (control and three fertilizer strategies) experiment was conducted during three cropping seasons in Navarra (Spain). Wheat (Triticum aestivum L.) was planted in 2002, barley (Hordeum vulgare L.) in 2003, and rapeseed (Brassica napus L.) in 2004. Daily soil water content measurements based on capacitance probes were used to calculate drainage at 1 m depth, by applying the water balance equation. Nitrate leaching was calculated as the drainage volume multiplied by the nitrate concentration of the soil solution extracted in ceramic cups. The results revealed distinct behaviour in three crop phases, viz.: (i) from planting to GS-25, with high risk of drainage and nitrate leaching, (ii) from GS-25 to the end of the drainage period, with little drainage and leaching, and (iii) from then to harvest, when no drainage or nitrate leaching took place. Drainage and soil mineral N content before planting were the main factors determining the amount of N leached. Splitting N-fertilizer application and the use of nitrification inhibitors are not likely to have a significant impact on subsequent N-leaching losses, provided that the N-fertilizer application is adjusted to crop N needs corrected by soil N supply.     

Sources of Nitrogen to the Riparian Zone of a Desert Stream: Implications for Riparian Vegetation and Nitrogen Retention

Riparian zones effectively remove nitrogen (N) from water flowing through riparian soils, particularly in agricultural watersheds. The mechanism of N removal is still unclear, especially the role of vegetation. Uptake and denitrification are the two most commonly studied mechanisms. Retention of groundwater N by plant uptake is often inferred from measurements of N in net incremental biomass. However, this assumes other sources of N are not contributing to the N demand of plants. The purpose of this work was to investigate the relative importance of three sources of available N to riparian trees in a desert stream—input in stream water during floods, input during baseflow, and mineralization of N from soil organic matter. Two approaches were used; a mass balance approach in which the mass of available N from each source was estimated, and a correlational approach in which indexes of each source were compared to leaf N for individual willow trees. Total N from all sources was 396 kg ha⁻¹ y⁻¹, with 172 kg ha⁻¹ y⁻¹ from mineralization, 214 kg ha⁻¹ y⁻¹ from the stream during baseflow, and 9.6 kg ha⁻¹ y⁻¹ from floods. Leaf N was significantly related to N mineralization rates and flood inputs; it was not related to baseflow inputs. We conclude that mineralization is a major source of available N for willow trees, subsidized by input of N from floods. Baseflow inputs are most likely removed by rapid denitrification at the stream–riparian edge, while higher rates of flood supply exceed the capacity of this “filter.” Received 18 January 2001; accepted 15 June 2001.     

Cloning and Characterization of a Rice Field Eel vasa-Like Gene cDNA and Its Expression in Gonads During Natural Sex Transformation

The vasa (vas)-related gene encodes an RNA helicase protein member of the DEAD-box family and plays key roles in germ-cell formation in higher metazoans. Using degenerate PCR and RACE, we cloned the vasa gene of the rice field eel (Monopterus albus), which is homologous to the Drosophila vasa gene. We named it ma-vas (Monopterus albus vas). Ma-vas encodes a protein of 618 amino acids, which contains all of the known characteristics of vasa homologs. RT-PCR analysis revealed that ma-vas was exclusively expressed in the gonads of the female, intersex, and male. During gonadal natural sex reversal, ma-vas is expressed in oocytes at all stages of oogenesis, in degenerating oocytes of ovotestis, and in spermatogonia and spermatocytes at early stages. The vasa positive signal was also observed in the peripheral layer of late ovary. It was not found, however, in that layer of the testis. Alkaline phosphatase (AKP) staining on the ovary and testis also indicated that some cells had differentiational potential in the peripheral layer of the ovary, suggesting that spermatogonia might arise from cells with AKP and vasa-positive staining in the peripheral layer of the female gonad.     

Original Articles: Nitrogen Mineralization in Two Unpolluted Old-Growth Forests of Contrasting Biodiversity and Dynamics

Studies in unpolluted, old-growth forests in the coastal range of southern Chile (42°30′S) can provide a baseline for understanding how forest ecosystems are changing due to the acceleration of nitrogen (N) inputs that has taken place over the last century. Chilean temperate forests, in contrast to their northern hemisphere counterparts, exhibit extremely low losses of inorganic N to stream waters. The objectives of this study were (a) to determine whether low inorganic N outputs in these forests were due to low rates of N mineralization or nitrification, and (b) to examine how biodiversity (defined as number of dominant tree species) and forest structure influence N mineralization and overall patterns of N cycling. Studies were conducted in a species-poor, conifer-dominated (Fitzroya cupressoides) forest with an even-aged canopy, and in a mixed-angiosperm (Nothofagus nitida) forest with a floristically more diverse and unstable canopy. Nitrogen mineralization rates measured in laboratory assays varied seasonally, reaching 6.0 μg N/g DW/day in both forests during late summer. Higher values were related to higher microbial activity, larger pools of labile inorganic N, and increased fine litter inputs. Field assays, conducted monthly, indicated positive net flux from N mineralization mainly from December to January in both forests. Annual net flux of N from mineralization varied from 20 to 23 kg/ha/year for the Fitzroya forest and from 31 to 37 kg/ha/year for the Nothofagus forest. Despite low losses of inorganic N to streams, N mineralization and nitrification are not inhibited in these forests, implying the existence of strong sinks for NO₃ ⁻ in the ecosystem. Field N mineralization rates were two times higher in the Nothofagus forest than in the Fitzroya forest, and correlated with greater N input via litterfall, slightly higher soil pH, and narrower carbon (C)–nitrogen ratios of soils and litter in the former. Differences in N mineralization between the two forest types are attributed to differences in biotic structure, stand dynamics, and site factors. Median values of net N mineralization rates in these southern hemisphere forests were lower than median rates for forests in industrialized regions of North America, such as the eastern and central USA. We suggest that these high N mineralization rates may be a consequence of enhanced atmospheric N deposition.     

Size, shape, and hydration of a self-associating human IgG myeloma protein: axial asymmetry as a contributing factor in serum hyperviscosity

Studies of sedimentation, diffusion, viscosity, and buoyant density have been carried out on a human IgG1-lambda myeloma protein (IgG-MIT) isolated from the serum of a patient with multiple myeloma and the hyperviscosity syndrome. In comparison with pooled normal IgG, IgG-MIT exhibits smaller sedimentation and diffusion coefficients, a larger intrinsic viscosity, and a larger frictional ratio. The preferential hydration of IgG-MIT in cesium chloride was found to be within the range of values typically observed for globular proteins. The data are consistent with prolate ellipsoid geometry, and suggest that the axial ratio of the IgG-MIT monomer is approximately 50% greater than that typically observed for IgG. The concentration dependencies of the hydrodynamic data for IgG-MIT confirm the previous finding of reversible, concentration-dependent self-association for this protein. IgG-MIT thus represents the first reported instance of an IgG paraprotein for which in vivo hyperviscosity effects appear attributable to a twofold mechanism involving geometric asymmetry and concentration-dependent polymerization. The results are discussed in terms of the significant heterogeneity in molecular dimensions which may exist among normal IgG proteins.     

Immobilization, stabilization and remobilization of nitrogen in forest soils at elevated CO2: a 15N and 13C tracer study

The fate of immobilized N in soils is one of the great uncertainties in predicting C sequestration at increased CO₂ and N deposition. In a dual isotope tracer experiment (¹³C, ¹⁵N) within a 4‐year CO₂ enrichment (+200 ppm_v) study with forest model ecosystems, we (i) quantified the effects of elevated CO₂ on the partitioning of N; (ii) traced immobilized N into physically separated pools of soil organic matter (SOM) with turnover rates known from their ¹³C signals; and (iii) estimated the remobilization and thus, the bio‐availability of newly sequestered C and N. (1) CO₂ enrichment significantly decreased NO₃^? concentrations in soil waters and export from 1.5 m deep lysimeters by 30–80%. Consequently, elevated CO₂ increased the overall retention of N in the model ecosystems. (2) About 60–80% of added ¹⁵NH₄¹⁵NO₃ were retained in soils. The clay fraction was the greatest sink for the immobilized ¹⁵N sequestering 50–60% of the total new soil N. SOM associated with clay contained only 25% of the total new soil C pool and had small C/N ratios (<13), indicating that it consists of humified organic matter with a relatively slow turn over rate. This implies that added ¹⁵N was mainly immobilized in stable mineral‐bound SOM pools. (3) Incubation of soils for 1 year showed that the remobilization of newly sequestered N was three to nine times smaller than that of newly sequestered C. Thus, inorganic inputs of N were stabilized more effectively in soils than C. Significantly less newly sequestered N was remobilized from soils previously exposed to elevated CO₂. In summary, our results show firstly that a large fraction of inorganic N inputs becomes effectively immobilized in relative stable SOM pools and secondly that elevated CO₂ can increase N retention in soils and hence it may tighten N cycling and diminish the risk of nitrate leaching to groundwater.     

The Lab-to-Field (LTF) Rating Scheme: A New Method of Investigating the Relationships between Laboratory Sublethal Toxicity Tests and Field Measurements in Environmental Effects Monitoring Studies

The Lab-to-Field (LTF) rating scheme is a straightforward method of relating the results of effluent toxicity tests to the field survey measurements and has proven to be a useful tool for interpretation of Environmental Effects Monitoring studies for pulp and paper mills in the province of Ontario. The LTF method uses the same five-level scale (level 1 for no or low response to level 5 for severe response) for rating the toxicity and field survey results. Regression analysis of LTF scores has revealed that the relationship between the Ceriodaphnia reproduction test and benthic invertebrate field survey measurements was significant (p < 0.001, r = 0.79). However, there were not sufficient data to determine if this can be used as a predictive tool. Nonetheless, Ceriodaphnia-to-benthic survey, Selenastrum-to-benthic survey and fathead-to-fish survey relationships were qualitatively rated strong or moderately strong in 94%, 75%, and 60% of the 16 studies, respectively. The LTF rating scheme would benefit from the use of a more sensitive species or life stage of fish to strengthen the sublethal test-to-fish survey relationship. Further validation of the lab-to-field relationship could be accomplished through the synoptic collection of effluent samples for sublethal tests and field measurements.     

Ventilation in the shore crab Carcinus maenas (L.) as a function of ambient oxygen and carbon dioxide: Field and laboratory studies

Ventilatory responses of crabs Carcinus maenas (L.) to changes in ambient oxygen and carbon dioxide were studied in field and laboratory experiments, over a range of Pw_O2 and Pw_co2 conditions encompassing natural variations observed in intertidal rock-pools. Ventilatory activity was assessed by recording gill chamber hydrostatic pressure and estimating the specific ventilation, Vw/M_O2, the reciprocal of the difference of oxygen concentrations in inspired and expired waters.

Variations in ambient oxygenation always induced large changes of ventilatory activity, hyperventilation in hypoxia, hypoventilation in hyperoxia. Conversely, Pw_CO2 changes either at constant P_O2 or in combination with different P_O2 values (hypoxic hypercapnia or hyperoxic hypocapnia) led only to small or even non-significant ventilatory responses. In the field, strong hyperventilation developed during tidal exposure at night, when the pool water became hypoxic and hypercapnic, whereas during the day the animals hypoventilated in progressively more hyperoxic and hypocapnic conditions.

Thus, in a typical intertidal animal such as C. maenas, the only ventilatory stimulus of ecological significance appears to be the ambient water oxygenation.     

Field Evaluation of Amitus bennetti (Hymenoptera: Platygasteridae), a Parasitoid of Bemisia argentifolii (Hemiptera: Aleyrodidae), in Cotton and Bean

Field cage experiments were conducted in Riverside, California to quantify the impact of releases of the parasitoid Amitus bennetti Viggiani & Evans on mortality of the whitefly Bemisia argentifolii Bellows & Perring. Single-row 50-m-long plots were planted with either cotton or bean. Cages were erected over the plants in each row, and adult whiteflies were released into the cages. Approximately 10 days later, adult parasitoids were released. Marked individual whiteflies were scored every 4 days for 6 weeks. Paired life tables were then constructed from census data from release and control cages over a single whitefly generation. Total whitefly mortality in release cages (71% in bean, 61% in cotton) was significantly greater than in control cages (25% in bean, 34% in cotton). The marginal rate for mortality attributable directly to the parasitism was 0.535 in the bean plots and 0.201 in the cotton plots. In addition, other mortality was greater in the release plots, possibly reflecting death of parasitized hosts before larval parasitoids could complete development. Parasitism was the greatest mortality factor in the study.     

10-Å CryoEM Structure and Molecular Model of the Myriapod (Scutigera) 6 × 6mer Hemocyanin: Understanding a Giant Oxygen Transport Protein

Oxygen transport in Myriapoda is maintained by a unique 6 × 6mer hemocyanin, that is, 36 subunits arranged as six hexamers (1 × 6mers). In the sluggish diplopod Spirostreptus, the 1 × 6mers seem to operate as almost or fully independent allosteric units (h ∼ 1.3; P₅₀ ∼ 5 torr), whereas in the swift centipede Scutigera, they intensively cooperate allosterically (h ∼ 10; P₅₀ ∼ 50 torr). Here, we show the chemomechanical basis of this differential behavior as deduced from hybrid 6 × 6mer structures, obtained by single-particle cryo-electron microscopy of the Scutigera 6 × 6mer (10.0 Å resolution according to the 0.5 criterion) and docking of homology-modeled subunits from Scutigera and two diplopods, Spirostreptus and Polydesmus. The Scutigera 6 × 6mer hemocyanin is a trigonal antiprism assembled from six smaller trigonal antiprisms (1 × 6mers), thereby exhibiting D3 point group symmetry. It can be described as two staggered 3 × 6mers or three oblique 2 × 6mers. Topologically, the 6 × 6mer is subdivided into six subunit zones, thereby exhibiting a mantle (24 subunits) and a core (12 subunits). The six hexamers are linked by 21 bridges, subdivided into five types: two within each 3 × 6mer and three between both 3 × 6mers. The molecular models of the 6 × 6mer reveal intriguing amino acid appositions at these inter-hexamer interfaces. Besides opportunities for salt bridges, we found pairs of carboxylate residues for possible bridging via a Ca²⁺ or Mg²⁺ ion. Moreover, we detected histidine clusters, notably in Scutigera, allowing us to advance hypotheses as to how the hexamers are allosterically coupled in centipede hemocyanin and why they act more independently in diplopod hemocyanin.     

Soluble ANPEP Released From Human Astrocytes as a Positive Regulator of Microglial Activation and Neuroinflammation: Brain Renin–Angiotensin System in Astrocyte–Microglia Crosstalk

Astrocytes are major supportive glia and immune modulators in the brain; they are highly secretory in nature and interact with other cell types via their secreted proteomes. To understand how astrocytes communicate during neuroinflammation, we profiled the secretome of human astrocytes following stimulation with proinflammatory factors. A total of 149 proteins were significantly upregulated in stimulated astrocytes, and a bioinformatics analysis of the astrocyte secretome revealed that the brain renin–angiotensin system (RAS) is an important mechanism of astrocyte communication. We observed that the levels of soluble form of aminopeptidase N (sANPEP), an RAS component that converts angiotensin (Ang) III to Ang IV in a neuroinflammatory milieu, significantly increased in the astrocyte secretome. To elucidate the role of sANPEP and Ang IV in neuroinflammation, we first evaluated the expression of Ang IV receptors in human glial cells because Ang IV mediates biological effects through its receptors. The expression of angiotensin type 1 receptor was considerably upregulated in activated human microglial cells but not in human astrocytes. Moreover, interleukin-1β release from human microglial cells was synergistically increased by cotreatment with sANPEP and its substrate, Ang III, suggesting the proinflammatory action of Ang IV generated by sANPEP. In a mouse neuroinflammation model, brain microglial activation and proinflammatory cytokine expression levels were increased by intracerebroventricular injection of sANPEP and attenuated by an enzymatic inhibitor and neutralizing antibody against sANPEP. Collectively, our results indicate that astrocytic sANPEP–induced increase in Ang IV exacerbates neuroinflammation by interacting with microglial proinflammatory receptor angiotensin type 1 receptor, highlighting an important role of indirect crosstalk between astrocytes and microglia through the brain RAS in neuroinflammation.