Chlorophyll-type compounds in soil

Summary The quantities of chlorophyll-type compounds in a group of 24 arable soils were significantly correlated with nitrogen uptake (r=0.79 and yield (r=0.84) of ryegrass grown in pots in the glasshouse. Partial correlation coefficients showed the amounts of mineral N released on incubating the rewetted air-dry soils were related both to chlorophyll units (measure of chlorophyll-type compounds) and organic C. The chlorophyll units (CU) apparently represented some fraction of organic matter that liberated inorganic nitrogen, because the quantities of chlorophyll-type compounds in the soil were too small (only 0.5–3.0 pounds per acre) to supply this nitrogen. It is likely that the compounds were a residue that resisted decomposition. The CU in soil that had been ploughed from ley decreased very slowly during 3 years of arable cropping.     

干热河谷车桑子光合生理特性对氮磷添加的响应

氮磷养分是限制干热河谷植物生长的重要元素,不同土壤上植物受到的养分限制类型不同。光合作用作为植物生长发育的基础,不同土壤上氮磷养分添加对干热河谷植物光合生理特征的影响还没有报道。因此,以干热河谷优势植物——车桑子为研究对象,在元谋县不同海拔处采集土壤,设置加氮（+N）、加磷（+P）、氮磷同时添加（+NP）和不添加（CK）四个处理,研究车桑子光合响应曲线、叶绿素含量和叶绿素荧光特性对氮、磷添加的响应规律,并探讨光合响应特征与车桑子生长的关系：研究结果显示：1）不同海拔土壤上,车桑子光合生理特性对氮磷添加具有不同的响应。在低海拔燥红土上,氮添加处理（+N和+NP）提高了车桑子净光合速率、叶绿素含量和PSII活性;中海拔紫色土上,+NP促进了车桑子光合速率和叶绿素含量的提高;高海拔黄棕壤上,+N处理降低了车桑子净光合速率和PSII活性,而磷添加处理（+P和+NP）提高了车桑子净光合速率。2）车桑子光合特性对养分添加的响应取决于土壤的养分限制类型,限制性养分添加可以提高车桑子的净光合速率。3）燥红土上+P以及黄棕壤上+N对PSⅡ最大光化学效率（Fv/Fm）的降低更大程度上归于可变荧光Fv的减少而不是最小荧光F₀的增加,可减少养分限制对光系统II造成的伤害。4）三种土壤类型上车桑子的叶绿素含量和组成差异极显著,相比于燥红土和紫色土,黄棕壤上车桑子的叶绿素含量显著更高,而叶绿素a/b显著更低。综上,本研究结果表明,车桑子光合能力受到氮和磷的共同调节,不同土壤上光合生理特性的响应可增强植物对限制性养分的适应性,影响植物生长发育。     

Chlorophyll destruction in the presence of bisulfite and linoleic acid hydroperoxide

Chlorophyll was rapidly destroyed in the presence of bisulfite and linoleic acid hydroperoxide. Both bisulfite and linoleic acid hydroperoxide were required for chlorophyll destruction and both were consumed in the reaction; however, there was no oxygen requirement. Chlorophyll destruction occurred most readily in the slightly acidic pH region with little destruction occurring above pH 8. The free radical scavengers, hydroquinone and α-tocopherol, were very effective at inhibiting chlorophyll destruction, but the singlet oxygen quenchers, β-carotene, 2,5-dimethylfuran and 1,3-diphenylisobenzofuran, were only slightly effective. The addition of metal chelators indicated that metals were not participating in the reaction. The evidence indicates that chlorophyll was destroyed by a free radical mechanism. Based on the present results and that of others, it is suggested that chlorophyll was destroyed via oxidation by the alkoxy radical which was produced during the decomposition of linoleic acid hydroperoxide by bisulfite.     

Uncoupling of chlorophyll and nutrients in lakes – possible reasons,expected consequences

Total phosphorus and total nitrogen explained a low percentage of summer chlorophyll variability in epilimnia of the Great Masurian Lakes. Division of the whole data set into two subgroups of lakes improved approximation of the chlorophyll nutrient relationship but revealed also functional differences between the lakes distinguished in that way. Chlorophyll in eutrophic lakes correlated well with nitrogen and phosphorus, that in mesotrophic lakes (those with summer chlorophyll <=22 mg m^–3 as calculated in the model) was related to none of the nutrients. Higher summer chlorophyll content in epilimnetic waters was accompanied by higher chl:PP and chl:PN ratios. Algal adaptation to poor light conditions in eutrophic lakes is postulated as a possible reason for that difference.Chlorophyll – nutrient relationships varied with the trophic status of lakes. Epilimnetic chlorophyll strictly followed phosphorus changes in eutrophic lakes but did not do so in mesotrophic ones. Detailed comparison of selected meso- and eutrophic lakes showed marked differences in the seasonal changes of chlorophyll and nutrient concentrations and in sedimentation rates, especially in spring. Nutrient limitation rather than zooplankton grazing is suggested as a possible mechanism of controlling algal abundance and the sequence of spring events in a eutrophic lake. It is hypothesised that phosphorus turnover in eutrophic lakes is dominated by seasonal vertical fluxes, while in mesotrophic lakes it is more conservative with consumption and regeneration restricted mostly to metalimnion. Possible consequences of such conclusion are discussed in the paper.     

Ecology of algal communities of different soil types from Cierva Point, Antarctic Peninsula

During summer 2005/2006, we characterized three sampling sites on mineral soils and four on ornithogenic soils from Cierva Point, Antarctic Peninsula, in terms of topographic and abiotic features (altitude, slope, magnetic direction, temperature, texture, pH, conductivity, organic matter, moisture and nutrient concentrations), and compared their microalgal communities through taxonomic composition, species richness, diversity, chlorophyll a content and their variation in time. Average values of pH, moisture, organic matter and nutrient concentrations were always significantly lower in mineral than in ornithogenic soils. Low N/P mass ratio showed potential N-limitation of biomass capacity in the former. On the other hand, the results suggested that physical stability is not as a key stress factor for mineral soil microalgae. Chlorophyll a concentration was not only higher in ornithogenic soils, but it also showed a wider range of values. As this parameter was positively correlated with temperature, pH, nutrients, organic matter and moisture, we cannot come to conclusions regarding the influence of each factor on algal growth. Communities of mineral soils were significantly more diverse than those of enriched ornithogenic soils due to higher species richness as well as higher equitability. Also, their structure was steadier over time, as shown by a cluster analysis based on relative frequency of algal taxa. Although Cyanobacteria and Bacillariophyceae dominated almost all samples, Chlorophyceae represented 34% of the 140 taxa recorded, and most of them observed only in cultures. The detection under controlled conditions of a high latent species richness in harsh mineral soil sites shows that the composition and equitability of these microalgal communities would be more prone to modification due to the manifold local consequences of climatic change than those of ornithogenic soils.     

Factors governing nutrient status of mountain lakes in the Tatra Mountains

1. Nutrient and chlorophyll a levels, and bacterial numbers of 84 glacial lakes in the Tatra Mountains (Slovakia and Poland, Central Europe) were determined to assess the impact of catchment vegetation and water acidity on lake trophic status. 2. Catchment vegetation was the crucial factor governing nutrient content of lakes. 3. Concentrations of organic carbon, organic nitrogen, and chlorophyll a, and bacterial numbers were tightly correlated with total phosphorus (TP) content. Their levels were the highest in forest lakes, then decreased in alpine lakes with decreasing amount of catchment vegetation and soil cover, and were the lowest in lakes situated in bare rocks. 4. The above pattern was further modified by lake water acidity. Concentrations of TP, organic carbon, and chlorophyll a were lower in alpine lakes with pH between 5 and 6 than in more or less acid alpine lakes. Zooplankton was absent in all alpine lakes with pH between 5 and 6. 5. Nitrate concentrations followed an inverse trend to TP; lowest values were in forest lakes, then increased with decreasing amount of catchment soils and vegetation. Within the lakes of the same type of catchment vegetation, nitrate concentrations were negatively correlated to TP. N‐saturation of catchment areas and lake primary production were dominant processes controlling nitrate levels in lakes and nitrate contribution to lake acidification.     

Comparison of methods to assess water column primary production in wetlands

We compared a number of techniques to measure water column autotroph production in a shallow, hypereutrophic wetland: diurnal oxygen changes; light and dark bottle incubations; chlorophyll a concentrations; daily changes in pH; and algal volume. Productivity from diurnal oxygen changes calculated at 0.25, 0.5, 1, 2, 3, and 4 h intervals give similar estimates, but not 12 h intervals (dawn-dusk-dawn). Net productivity in bottles was slightly lower than that indicated by diurnal oxygen changes, and gross productivity in bottles was much lower than diurnal changes. Changes in pH correlated well with gross and net productivity measurements, as well as algal volume. Chlorophyll a is correlated with diurnal and bottle net productivity measurements and pH changes, but not algal volume. Since daily pH flux and oxygen changes provide a better overall assessment of ecosystem processes than standing crop or bottle incubations, they could be useful measurements for ecological engineers interested in assessing the ecosystem function.     

Nutritional Regulation of Organelle Biogenesis in Euglena: REPRESSION OF CHLOROPHYLL AND NADP-GLYCERALDEHYDE-3-PHOSPHATE DEHYDROGENASE SYNTHESIS

Nitrogen deficiency and the presence of specific organic carbon sources prevent chloroplast development in Euglena. In exponentially growing cultures, chlorophyll levels were low and independent of the nitrogen content of the growth medium. Chlorophyll levels increased in stationary phase and the amount of chlorophyll formed was proportional to the initial nitrogen content of the growth medium; the greater the concentration of nitrogen, the greater the amount of chlorophyll synthesized during stationary phase. Washing experiments demonstrated that the major nutritional factor inhibiting chlorophyll synthesis in stationary phase cultures grown on medium containing a high carbon to nitrogen ratio was the absence of nitrogen rather than the presence of utilizable organic carbon.     

Competition between soil bacteria and fusarium

Summary The phenomenon of competition has been characterized in liquid medium and sterile soil systems using a variety of soil bacteria andFusarium oxysporum f.cubense as test organisms. For most of the bacteria, suppression of the fungus was the result of a biologically induced nitrogen deficiency, this effect being reversed by the addition of excess inorganic nitrogen. High populations of competitors were found in two soils of neutral pH, but no isolates competed in the acid San Alejo loam.Agrobacterium radiobacter was able to compete when San Alejo loam was limed to about pH 6.6. Inhibition of the fungus by a number of gram-positive, spore-forming rods could not be accounted for in terms of competition for nutrients or by antibiotic production in artificial media.The competitive ability ofA. radiobacter when tested in twelve Central American soils was found to be related to pH in acid and neutral environments but was correlated with texture, organic-matter content and total nitrogen in soils of intermediate pH. In all soils where inhibition occurred, the competitive effect was overcome by additions of inorganic nitrogen. Excluding the group ofBacillus spp., the competitive ability of soil bacteria was related to the ability to develop in the absence of amino acids and growth factors but could not be correlated with growth rates of the bacteria in soil or liquid medium.It is suggested that competition for nutrients is a significant means of ecological control among members of the soil microflora and, together with competitive interactions for space and oxygen, may be the major factors governing the biological control of soil-borne fungi.The investigation was supported in part by a grant from the United Fruit Company. Agronomy Paper No. 471.     

叶绿素计SPAD-502在林业上应用

叶绿素是植物光合作用的色素,传统方法测定叶绿素一般采用分光光度法.本研究采用便携式叶绿素计SPAD-502测定落叶松人工林下4个主要阔叶树种绿色度（SPAD值）的季节变化,并与分光光度法测定的叶绿素含量进行相关性分析.结果表明,SPAD值与叶绿素含量具有显著的相关性,SPAD值能较好地反映树木叶绿素含量的变化.因此,使用叶绿素计测定树木的叶绿素含量是完全可行的,在一定条件下可代替叶绿素含量的直接测定.由于叶绿素计SPAD-502携带方便、测定简便、迅速,且不损坏叶片,应在林业研究中积极推广使用.     

Interactions Between High pH and Iron Supply on Nodulation and Iron Nutrition of Lupinus albus L. Genotypes Differing in Sensitivity to Iron Deficiency

Poor growth of white lupin (Lupinus albus L.) on alkaline soils may result from its sensitivity to iron deficiency and poor nodulation. This study examined interactive effects of iron supply and high pH on the growth and nodulation of three genotypes differing in their sensitivity to iron deficiency. Three genotypes (P27486, Ultra and WTD180) were grown for 17 days in buffered solutions with Fe supply of 0.2, 2 and 20 μM. Solution pH was adjusted to 5.2, 6.5 or 7.5. Plant growth, nodulation and nutrient concentrations in plants were measured. Decreasing Fe supply decreased chlorophyll concentration in young leaves by up to 92%. Increasing pH decreased chlorophyll concentration by an average of 40% at pH 6.5 and by 47% at pH 7.5. The decrease of chlorophyll was less obvious in P27485 than in Ultra or WTD180. Shoot biomass was reduced by up to 18% by Fe deficiency, with such decrease being less for P27486. Increasing pH exacerbated the effect of Fe deficiency on shoot biomass only of Ultra. Decreasing Fe supply decreased nodule number by an average of 54%, and increasing pH decreased nodule number by 80%. P27486 formed the greatest number of nodules while WTD180 the least. P27486 had high Fe uptake and low internal requirement. Irrespective of genotype, leaf chlorosis positively correlated with cluster root formation. The results suggest that a combination of Fe deficiency and high pH impaired nodulation in L. albus, and that selection of genotypes for both tolerance of iron deficiency and good nodulation at high pH is important for a successful lupin crop on alkaline soils.     

二氧化硫对地衣中共生藻菌营养关系影响研究

为探讨地衣对大气污染特别敏感的原因 ,分离淡腹黄梅衣 (Xanthoparmelliamexicana)的共生藻和共生真菌 ,并重新合成地衣 .研究了地衣及纯化培养的藻和菌在SO2 污染短期胁迫下的生理反应 .结果表明 ,叶绿素a比叶绿素b易受伤害 ;叶绿素对 0 .5mg·L-1的熏气最敏感 ,水溶液暴露时叶绿素PQa值的下降与SO2 的吸收量有相关性 .地衣中酸性磷酸酶活性主要由共生藻所决定 .丙二醇含量在共生藻和菌以及地衣样品中无显著差异 ;还原型谷胱甘肽GSH含量在共生菌中明显高于共生藻 ,并与SO2 胁迫强度密切相关 .可以作为地衣过氧化状态和受损的生物标志物 .共生真菌承担了地衣主要的抗氧化任务 ,由于物质与能量的消耗 ,共生藻比共生菌更容易受到伤害 .     

Effect of liming on mineralization of soil nitrogen as measured by plant uptake and nitrogen released during incubation

The effect of lime rates on oat yield and N uptake was measured in a 6-years pot experiment, using 12 acid surface soils (pH 4.7 to 6.0). Mineralization of nitrogen was measured by incubation of soil samples taken after harvest each year from the different lime treatments.Nitrogen uptake was significantly correlated with total N in the soils. Averaged over all 12 soils liming only to pH 7 or above, increased the oat yield significantly. Liming increased the N concentration of grain and the N uptake significantly during a 4-years period, indicating the effect of lime on N mineralization.The mineralization of organic N measured by incubation in the non-limed samples was highly correlated with the total N concentration, but it was not significantly related to the original pH of the soils. The amounts of N released as well as the duration of the lime effect on mineralization varied among soils. When pH was raised to 7 or above, considerable increases in N mineralization occurred in some soils. Based on average values, liming increased N mineralization significantly during a 3-years period. After 3 years, the lime treatments differed only slightly from the non-limed treatments.     

The effects of light acclimation during and after foliage expansion on photosynthesis ofAbies amabilis foliage within the canopy

Variation in the photosynthetic function ofAbies amabilis foliage within a canopy was examined and related to three different processes that affect foliage function: foliage aging, sun-shade acclimation that occurred while foliage was expanding, and reacclimation after expansion was complete. Foliage produced in the sun had higher photosynthesis at light saturation (A _max, mol·m^-2·s^-1), dark respiration (mol·m^-2·s^-1), nitrogen content (g·m^-2), chlorophyll content (g·m^-2), and chlorophylla:b ratio, and a lower chlorophyll to nitrogen ratio (chl:N), than foliage produced in the shade. As sun foliage becomes shaded, it becomes physiologically similar to shade foliage, even though it still retains a sun morphology. Shaded sun foliage exhibited lowerA _max, dark respiration, nitrogen content, and chlorophylla:b ratio, and a higher chl:N ratio than sun foliage of the same age remaining in the open. However, shaded sun foliage had a higher chlorophyll content than sun foliage remaining in the open, even though true shade foliage had a lower chlorophyll content than sun foliage. This anomaly arises because as sun foliage becomes shaded, it retains a higher nitrogen content than shade foliage in a similar light environment, but the two forms have similar chl:N ratios. Within the canopy, most physiological indicators were more strongly correlated with the current light environment than with foliage age or leaf thickness, with the exception of chlorophyll content.A _max decreased significantly with both decreasing current light environment of the foliage and increasing foliage age. The same trend with current light and age was found for the chlorophylla:b ratio. Foliage nitrogen content also decreased with a decrease in current light environment, but no distinct pattern was found with foliage age. Leaf thickness was also important for predicting leaf nitrogen content: thicker leaves had more nitrogen than thinner leaves regardless of light environment or age. The chl:N ratio had a strong negative correlation with the current light environment, and, as with nitrogen content, no distinct pattern was found with foliage age. Chlorophyll content of the foliage was not well correlated with any of the three predictor variables: current light environment, foliage age or leaf thickness. On the other hand, chlorophyll content was positively correlated with the amount of nitrogen in a leaf, and once nitrogen was considered, the current light environment was also highly significant in explaining the variation in chlorophyll content. It has been suggested that the redistribution of nitrogen both within and between leaves is a mechanism for photosynthetic acclimation to the current light environment. Within theseA. amabilis canopies, both leaf nitrogen and the chl:N ratio were strongly correlated with the current light environment, but only weakly with leaf age, supporting the idea that changing light is the driving force for the redistribution of nitrogen both within and between leaves. Thus, our results support previous theories on nitrogen distribution and partitioning. However,A _max was significantly affected by both foliage age and the current light environment, indicating that changes in light alone are not enough to explain changes inA _max with time.     

长江口及其邻近水域叶绿素a的垂直格局及成因初析

根据2005年9月~2006年5月逐季进行的4次多学科综合调查, 报道了长江口及其邻近水域叶绿素a的垂直分布特征, 并探讨了环境因子和长江冲淡水过程对浮游植物生物量垂直分布的影响。结果表明, 水柱平均叶绿素a在春季最高、冬季最低, 高值区位置因季节而异, 常出现在低盐或等盐线密集的水域; 河口区和外海区水体垂向混合均匀, 除夏季外叶绿素a的垂直变化均较小; 冲淡水区水体呈现层化特征, 叶绿素a高值集中分布在浅层水体。低盐的长江冲淡水占据上层水体, 良好的营养盐条件促进了浮游植物的生长; 外海高盐水控制的下层水体, 较低的营养盐浓度和较弱的光强不利于浮游植物生物量的积累。     

The Dry Limit of Microbial Life in the Atacama Desert Revealed by Calorimetric Approaches

The Atacama desert in Chile is one of the driest and most lifeless environments on Earth. It rains possibly once a decade. NASA examined these soils as a model for the Martian environment by comparing their degradation activity with Martian soil and looking for “the dry limit of life”. The existence of heterotrophic bacteria in Atacama soil was demonstrated by DNA extraction and by the isolation of microorganisms. So far, however, no data have been available about the metabolic activities in these soils due to the limitations of the existing methodologies when applied to desert soils. Calorimetry was used to obtain information on the metabolic and thermal properties of eleven soil samples collected at different sites in the Atacama desert. Differential scanning calorimetry and isothermal calorimetry were employed to determine the pyrolysis properties of the carbon‐containing matter and to measure biomass and microbial metabolism. They were compared to other soil properties such as total carbon and nitrogen, carbon to nitrogen ratio and pH. There was measurable organic matter in nine of the eleven samples and the heat of pyrolysis of those soils was correlated to the carbon content. In five of the eleven samples no biomass could be detected and the existence of basal microbial metabolism could not be established because all samples showed endothermic activity, probably from inorganic reactions with water. Six samples showed microbial activation after the addition of glucose. Carbon content, nitrogen content and the microbial activity after glucose amendment were correlated to the altitude and to the average minimum temperature of the sampling sites calculated from meteorological data. The detectable microbial metabolism was more dissipative with increasing altitude and decreasing temperature.     

Effect of Irradiance on Chlorophyll Estimation with the Minolta SPAD-502 Leaf Chlorophyll Meter

Leaf chlorophyll content may be used as an indirect indicatorof crop nitrogen status. Chlorophyll meter values (SPAD values)taken with the Minolta SPAD-502 chlorophyll meter in the shadeplantOxalis acetosellaL. and in winter wheat (Triticum aestivumL.)varied by 15 and 8%, respectively, with variation in irradiance.The lowest SPAD-values were measured at high irradiance. Duringa natural night-day-night cycle SPAD values for winter wheatwere lowest in the middle of the day, highest at low irradianceat dusk and dawn and intermediate in darkness before dawn andafter dusk. The results indicate that irradiance during measurementshould be considered when using the Minolta SPAD-502 chlorophyllmeter for the estimation of crop N-status.Copyright 1998 Annalsof Botany Company Chlorophyll meter, nitrogen, irradiance,Oxalis acetosellaL.,Triticum aestivumL., winter wheat.     

Pheopigment dynamics,zooplankton grazing rates and the autumnal ammonium peak in a Mediterranean lagoon

The dilution technique was used to estimate chlorophyll and pheopigment, net and gross production as well as zooplankton grazing over a 12-month period in a coastal lagoon in Southern France. Chlorophyll a (Cha) based gross growth rates of phytoplankton ranged from undetectable in February to 2.6 day⁻¹ in June, corresponding to 3.8 divisions per day. Cha-based grazing rates ranged from undetectable in February to 1.1 d⁻¹ in June. The seasonal growth pattern of picoplankton was similar to that of the whole community, with a peak in July, corresponding to four divisions per day. Grazing processes represented from 20 to 150% of the phytoplankton daily growth, and the grazing pressure was stronger on small phytoplankton cells than on larger cells. Gross growth rates of phytoplankton were related to zooplankton grazing rates, and both were related to water temperature. Mesozooplankton which escaped sampling or oysters had to be also invoked as additional sinks for the primary production. In the fall, pheopigment concentrations greater than chlorophyll concentrations coincided with high ammonium levels in the water column. Pheopigment a production rates were highly correlated to chlorophyll -based microzooplankton grazing rates. The pheopigment a to chlorophyll a ratio was correlated with ammonium concentrations and could be used an index of the balance between ammonium supply (degradation) and demand (uptake by phytoplankton). In addition, pheopigment degradation rates in absence of grazing could be related to irradiance, indicating photo-degradation of these compounds.     

Distribution and diversity of archaeal communities in selected Chinese soils

To understand the distribution and diversity of archaea in Chinese soils, the archaeal communities in a series of topsoils and soil profiles were investigated using quantitative PCR, T-RFLP combining sequencing methods. Archaeal 16S rRNA gene copy numbers, ranging from 4.96?×?10(6) to 1.30?×?10(8) copies?g(-1) dry soil, were positively correlated with soil pH, organic carbon and total nitrogen in the topsoils. In the soil profiles, archaeal abundance was positively correlated with soil pH but negatively with depth profile. The relative abundance of archaea in the prokaryotes (sum of bacteria and archaea) ranged from 0.20% to 9.26% and tended to increase along the depth profile. T-RFLP and phylogenetic analyses revealed that the structure of archaeal communities in cinnamon soils, brown soils, and fluvo-aquic soils was similar and dominated by Crenarchaeota group 1.1b and 1.1a. These were different from those in red soils, which were dominated by Crenarchaeota group 1.3 and 1.1c. Canonical correspondence analysis indicated that the archaeal community was primarily influenced by soil pH.     

Regulation of chlorophyll synthesis in the green alga golenkinia

Chlorophyll synthesis in Golenkinia is inhibited 10-fold by growth in darkness on acetate or by growth on elevated concentrations of acetate in the light, particularly if the growth medium contains low levels of nitrogen. Glucose has no such inhibitory effect. delta-Aminolevulinic acid, with a maximal effect at 0.01 m, but not its precursors, overrides the inhibitory effect of acetate and darkness, restoring chlorophyll synthesis. Glycine, succinate, and alpha-ketoglutarate, the precursors tested, all enter the cell. Cells forming chlorophyll produce significantly more aminolevulinic acid than do cells becoming bleached, further indicating the important regulatory role of this compound. Cyclic AMP has no effect on chlorophyll synthesis. These results are compared with those obtained studying other algae, and a mechanism relating light and acetate to chlorophyll formation is proposed.