The Effect of Abiotic Factors on the Male Mate Searching Behavior and the Mating Success of Aphidius ervi (Hymenoptera: Aphidiidae)

The effect of wind speed and distance from the source on the male response of the aphid parasitoid, Aphidius ervi (Hymenoptera: Aphidiidae), to a pheromone source was studied in a wind tunnel. The number of males taking flight, entering the plume and successfully reaching the source, decreased at wind speeds >50 cm/s. Furthermore, the proportion of those attempting upwind flight that fell to the ground increased with increasing wind speed. In contrast, distance from the source had no significant effect on any of the parameters examined. While male flight behavior was significantly reduced at 70 cm/s, some males walked to the source when there was a bridge connecting the pheromone source and the release platform. This suggests that ambulatory behavior could be a significant component of male mate searching in A. ervi when wind conditions are too strong for upwind flight. The possible effects of variation in atmospheric pressure on male flight behavior to the long distance pheromone, as well as to the short distance one, were also investigated. No significant effects of atmospheric pressure were observed. These findings differ significantly from those previously reported for another aphid parasitoid, A. nigripes, and the reasons for such differences are discussed.     

藏东南大气氮湿沉降动态变化——以林芝观测点为例

利用量雨器和湿沉降收集仪在藏东南通过2a的试验, 研究了该区大气氮素沉降的浓度、沉降量以及季节变化规律.结果表明:藏东南大气氮素湿沉降(无机氮)为1.33～3.05 kg/ (hm2·a),平均值为2.36 kg/ (hm2·a),降水中铵态氮和硝态氮的平均浓度分别为0.36 mg/L和0.10 mg/L ,NH+4-N/ NO-3-N接近4 .各形态氮月均浓度之间差别较大,具有明显的季节性,其中NH+4-N月均浓度动态变化明显,5、6、7月份浓度较高(＞0.5 mg/L),NO-3-N 12月份浓度(0.49 mg/L)为全年最高;氮浓度的季节变化,以春冬较高,夏秋季较低,离散程度以春季最大.降水量与各形态氮沉降呈一定幂型负相关,相关系数为0.705,0.641,分别达到0.006 (NH+4-N)和0.019(NO-3-N)的显著水平.氮月沉降以5～6月份最高,占全年的32.3%;氮季沉降以夏季所占比例最高,约占50%,冬季最低(2%～3%).     

Somatostatin: A Novel Substrate and a Modulator of Insulin-Degrading Enzyme Activity

Insulin-degrading enzyme (IDE) is an interesting pharmacological target for Alzheimer's disease (AD), since it hydrolyzes β-amyloid, producing non-neurotoxic fragments. It has also been shown that the somatostatin level reduction is a pathological feature of AD and that it regulates the neprilysin activity toward β-amyloid.In this work, we report for the first time that IDE is able to hydrolyze somatostatin [k_cat (s^− 1) = 0.38 (± 0.05); K_m (M) = 7.5 (± 0.9) × 10^− 6] at the Phe6-Phe7 amino acid bond. On the other hand, somatostatin modulates IDE activity, enhancing the enzymatic cleavage of a novel fluorogenic β-amyloid through a decrease of the K_m toward this substrate, which corresponds to the 10-25 amino acid sequence of the Aβ(1-40). Circular dichroism spectroscopy and surface plasmon resonance imaging experiments show that somatostatin binding to IDE brings about a concentration-dependent structural change of the secondary and tertiary structure(s) of the enzyme, revealing two possible binding sites. The higher affinity binding site disappears upon inactivation of IDE by ethylenediaminetetraacetic acid, which chelates the catalytic Zn²⁺ ion. As a whole, these features suggest that the modulatory effect is due to an allosteric mechanism: somatostatin binding to the active site of one IDE subunit (where somatostatin is cleaved) induces an enhancement of IDE proteolytic activity toward fluorogenic β-amyloid by another subunit. Therefore, this investigation on IDE-somatostatin interaction contributes to a more exhaustive knowledge about the functional and structural aspects of IDE and its pathophysiological implications in the amyloid deposition and somatostatin homeostasis in the brain.     

Pedoecological effects of a sand-fixing poplar (Populus simonii Carr.) forest in a desertified sandy land of Inner Mongolia, China

To assess the pedoecological effects of a 23-year old poplar ( Populus simonii Carr.) forest on soil amelioration and vegetation restoration via soil erosion reduction and atmospheric dust retention in a desertified sandy land ecosystem, daily dynamics of wind speed, sand transport and dust deposition rates were monitored over an erosive period from April through June in 2001, using fixed observation sites located at different positions within and around the forest. Soil and vegetation characteristics at these sites were also measured. The observation sites were placed at distances of 15H (as control), 6H and 3H (H is mean tree height) from the forest edge of the windward side (abbreviated CK, 6H-W and 3H-W respectively), forest center (FC), and at distances of 0H, 6H and 8H from the forest edge of the leeward side (FE-L, 6H-L and 8H-L respectively). Daily mean wind speed was significantly lower in different observation sites than CK, with FC having the greatest reduction of wind speed and 6H-W the least reduction. Daily transport rate of sand by wind was also significantly lower in different observation sites than CK, with FE-L having the greatest reduction of wind erosion and 6H-W the least reduction. The fact that the poplar forest will lose its functions against wind at a distance of about 12-fold tree height from the forest edge of the leeward side suggests that the effective wind-preventing range of the poplar forest is about 150 m. There was marked spatial and seasonal distribution of dust-fall rate. Over space, the rate of dust-fall was much greater within the forest than outside the forest. Over time, the daily dust deposition rate was greatest in April, followed in decreasing order by May, June, July, September and August, closely linked to the seasonal distribution pattern of dust storm. Significant positive changes in soil and vegetation parameters of the different observation sites during the 23 years that the poplar forest was established suggest the perceptible pedoecological effects of the poplar forest on soil development and restorative succession of plant community within its immediate vicinity through windbreak, soil erosion reduction and atmospheric dust retention. Understanding these pedoecological effects may aid in the design of protective forest systems in arid and semi-arid areas.     

Spatial and temporal variation of atmospheric nitrogen deposition in the North China Plain

A monitoring network of nine sites was established to determine the spatial and temporal variation of atmospheric nitrogen (N) deposition in the North China Plain (NCP) over a two-year period. The annual bulk deposition of inorganic N in the North China Plain ranged from 18.4 to 38.5 kg/hm² and averaged 28.0 kg/hm². The concentration of NH₄ -N and NO₃^--N in rainwater averaged 3.76 and 1.85 mg/L, respectively, which were significantly higher than the values at background sites in China (normally less than 0.5 mg/L). Annual bulk deposition of inorganic N in the Beijing area (32.5 kg/hm²) was higher than that in Shandong and Hebei provinces (21.2 kg/hm² on an average). Also bulk N deposition was much greater in Dongbeiwang and Fangshan than in Yanqing and Shunyi counties. Significant spatial variation of bulk deposition was observed in the Beijing area because of variation of precipitation, and 60% of bulk deposition occurred from June to September. Bulk deposition of NH₄ -N was 2.0 times that of NO₃^--N deposition at the rural monitoring sites. However, the situation was reversed at the Beijing Academy of Agricultural-Forestry Sciences (BAAFS), the unique urban monitoring site. The results suggest that reduced N in precipitation is dominant in rural regions, but oxidized N is the major form in urban regions. The positive relationship between inorganic N deposition and precipitation can be fitted by a power equation (r²= 0.67), showing an increase of NH₄ -N and NO₃^--N inputs with increased precipitation. Wet deposition of N accounted for 73% of the bulk deposition, implying that dry deposition of N, particularly NH₄ -N from dust, is important in the North China Plain.     

Effects of elevated atmospheric CO2 on soil enzyme activities at different nitrogen application treatments

It has been predicted that elevated atmospheric CO₂ will increase enzyme activity as a result of CO₂-induced carbon entering the soil. The objective of this study was to investigate the effects of elevated atmospheric CO₂ on soil enzyme activities under a rice/wheat rotation. This experiment was conducted in Wuxi, Jiangsu, China as part of the China FACE (Free Air Carbon Dioxide Enrichment) Project. Two atmospheric CO₂ concentrations (580±60) and (380±40) μmol·mol^-1) and three N application treatments (low-150, normal-250 and high-350 kg N·hm^-2) were included. Soil samples (0-10 cm) were collected for analysis of β-glucosidase, invertase, urease, acid phosphates and β-glucosaminidase activities. The results revealed that with elevated atmospheric CO₂ β-glucosidase activity significantly decreased (P < 0.05) at low N application rates; had no significant effect with a normal N application rate; and significantly increased (P < 0.05) with a high N application rate. For urease activity, at low and normal N application rates (but not high N application rate), elevated atmospheric CO₂ significantly increased (P < 0.05) it. With acid phosphatase elevated atmospheric CO₂ only had significant higher effects (P < 0.05) at high N application rates. Under different CO₂ concentration, effects of N fertilization are also different. Soil β-glucosidase activity at ambient CO₂ concentration decreased with N fertilization, while it increased at elevated CO₂ concentration. In addition, invertase and acid phosphatase activities at elevated CO₂ concentration, significantly increased (P < 0.05) with N treatments, but there was no effect with the ambient CO₂ concentration. For urease activity, at ambient CO₂ concentration, N fertilization increased it significantly (P < 0.05), whereas at elevated CO₂ concentration it was not significant. Additionally, with β-glucosaminidase activity, there were no significant effects from N application. In general, then, elevated atmospheric CO₂ increased soil enzyme activity, which may be attributed to the following two factors: (1) elevated atmospheric CO₂ led to more plant biomass in the soil, which in turn stimulated soil microbial biomass and activity; and (2) elevated atmospheric CO₂ increased plant photosynthesis, thereby increasing plant-derived soil enzymes.     

2003年稻纵卷叶螟重大迁入过程的大气动力机制分析

为了探明稻纵卷叶螟灾变性迁入的大气动力学机制,本研究在ArcGIS中对2003年我国稻纵卷叶螟的时空分布规律进行了简要的地学分析。在此基础上,选取了有典型意义的重大迁入过程2个,从PCVSATTM接收系统中调取覆盖各迁飞过程的实测气象数据和T213数值预报产品,输入MM5中尺度数值预报模式对迁飞和降落期间的大气动力场进行了数值模拟和客观分析。结果表明：（1）用850 hPa和925 hPa高度风向来分别描述稻纵卷叶螟北迁和南迁主迁飞层种群迁移的方向是比较合适的。北迁时,从源地到迁入地之间有比较一致的偏南气流;南迁时,从源地到迁入地之间则有相对均一的偏北气流。水平风场上的气旋式曲率区有利于害虫的起飞迁出,反气旋式曲率区则有利于其迁入降落。（2）垂直气流场中下沉气流的推动作用是稻纵卷叶螟迁入和降落的最直接大气动力机制,当稻纵卷叶螟迁入某一即将危害的稻区时,其降落前36～12 h以内的850 hPa等压面上常表现为相对强而宽广的下沉气流区。（3）在稻纵卷叶螟迁入与为害前36～12 h内的高空850 hPa和925 hPa散度场上,降虫区上空对应着比较一致的高值正散度区,表明有较强的下沉气流存在,这对降虫十分有利。（4）850 hPa、925 hPa等压面上的水平流场、垂直气流场和散度场的特征分布对预测稻纵卷叶螟的迁入和降落具有很好的指示意义。     

Airborne pollen sampling in Toledo, Central Spain

Toledo is one of the main tourist spots of Spain, attracting around two million visitors per year. Its geographical situation in the vast and scarcely monitored Region of Castilla La Mancha and the high number of tourists (especially in the spring) has resulted in the Spanish Aerobiology Network (REA) making this city a major study objective. Air monitoring studies carried out using REA sampling procedures commenced in October 2002. Thirty-two pollen types were identified during the sampling period (October 2002 to October 2004). The annual Pollen Index (PI) was 44124 for the agricultural year October 2002–October 2003, and 29666 in the same period of 2003–2004. The most abundant taxa were, in decreasing order of dominance: Cupressaceae, Quercus, Poaceae, Populus, Olea, Urticaceae, Platanus, Pinus and Ulmus. Other, less well-represented pollen taxa included Salix, Alnus, Fraxinus and Tamarix, which were characteristic of riverside areas, and Morus, Artemisia and Chenopodiaceae. The presence of Castanea pollen grains originating from chestnut crops far away from the city was clearly an example of long-distance transport. The highest concentrations of airborne pollen were detected from March to May and also in January, due to the flowering of Cupressaceae species. In general, there was a correlation between pollen and meteorological parameters: a positive correlation with temperature and a negative correlation with rainfall and humidity during the pre-peak period. A negative correlation between temperature and some tree pollen taxa was detected in the principal pollen period correlation analysis due to their long pollination periods.     

不同大气校正方法对森林叶面积指数遥感估算影响的比较

利用TM原始图像以及经过6S模型和基于影像自身的Gilabert模型大气校正后的地面绝对反射率图像,分别计算了褒河流域阔叶林和针阔混交林2种林型的5类光谱植被指数(SR、NDVI、MNDVI、ARVI和RSR),并建立各林型森林叶面积指数与同时相的各个植被指数的相关关系。结果表明,2种大气校正模型均显著提高了各植被指数与森林叶面积指数的相关关系,除了对森林叶面积指数与植被指数SR和NDVI的相关关系影响不显著外,对森林叶面积指数与植被指数MNDVI、ARVI和RSR相关关系的影响均非常显著。说明不同大气校正模型对叶面积指数的遥感估算结果有较大影响。因此,在利用遥感数据进行定量分析、信息提取和生态遥感应用时,不仅要进行大气校正,而且还要慎重选择大气校正模型和植被指数。     

城市林地与非林地大气SO２季节动态变化

SO2作为主要的大气污染物之一,对人体与环境具有严重危害,导致酸雨后危害更大,尤其是长江以南省区污染严重。对长沙和株洲市区内2种类型区域———城市林地与城市非林地空气SO2浓度通过近1a(2004-01~2005-01)的同时进行对比定位观测,用甲醛吸收副玫瑰苯胺分光光度法分析,结果表明:从两市2种类型采样地空气SO2浓度水平总体与分别来看,SO2浓度年内变化均具有明显季节性波动特征(p=0·001),冬季最高,秋季最低;除冬季二者SO2浓度较为接近外,其他各季株洲非林地观测区SO2浓度均高于同季节长沙非林地观测区SO2浓度。空气SO2浓度季节性变化与当地的地理环境、气候条件、采暖期与工业生产布局等因素有较大的关系。其中,燃煤、降水、风速风向和气温是影响空气SO2浓度变化主要的污染源与气候条件因素。空气SO2浓度水平还与所在地有无林木覆盖关系密切。无林地空气SO2浓度年均值(0·18±0·08)mg/m3,有林地空气SO2浓度年均值(0·09±0·07)mg/m3,二者间存在极其显著差异(p=0·001)。林木生理活性季节性变化对植物调节空气SO2浓度季节变化的能力有一定的影响。按林地SO2浓度减缓效应大小排序,依次是夏季(55·4%)>冬季(54·1%)>秋季(49·3%)>春季(29·6%)。城市森林作为一种有效的生物措施在控制和治理城市大气SO2污染实践中具有重要作用,不失为一种经济可行、高效的环境保护措施,应着力提高城市森林覆盖率。