Salt-induced changes in photosynthetic activity and growth in a potential medicinal plant Bishop’s weed (Ammi majus L.)

Sixty seven-days-old plants of Ammi majus L. were subjected for 46 d to sand culture at varying concentrations of NaCl, i.e. 0 (control), 40, 80, 120, and 160 mM. Increasing salt concentrations caused a significant reduction in fresh and dry masses of both shoots and roots as well as seed yield. However, the adverse effect of salt was more pronounced on seed yield than biomass production at the vegetative stage. Calculated 50 % reduction in shoot dry mass occurred at 156 mM (ca.15.6 mS cm^–1), whereas that in seed yield was at 104 mM (ca.10.4 mS cm^–1). As in most glycophytes, Na⁺ and Cl^– in both shoots and roots increased, whereas K⁺ and Ca²⁺ decreased consistently with the successive increase in salt level of the growth medium. Plants of A. majusmaintained markedly higher K⁺/Na⁺ ratios in the shoots than those in the roots, and the ratio remained more than 1 even at the highest external salt level (160 mM). Net photosynthetic (P_N) and transpiration (E) rates remained unaffected at increasing NaCl, and thus these attributes had a negative association with salt tolerance of A. majus. Proline content in the shoots increased markedly at the higher concentrations of salt. Essential oil content in the seed decreased consistently with increase in external salt level. Overall, A. majusis a moderately salt tolerant crop whose response to salinity is associated with maintenance of high shoot K⁺/Na⁺ ratio and accumulation of proline in shoots, but P_N had a negative association with the salt tolerance of this crop.This revised version was published online in March 2005 with corrections to the page numbers.     

Gas exchanges of an endangered species Syringa pinnatifolia and a widespread congener S. oblata

Net photosynthetic rate (P _N), transpiration rate (E), water use efficiency (WUE), stomatal conductance (g _s), and stomatal limitation (L_s) were investigated in two Syringa species. The saturation irradiance (SI) was 400 µmol m^-2s^-1 for S. pinnatifolia and 1 700 µmol m^-2s^-1 for S. oblata. Compared with S. oblata, S. pinnatifolia had extremely low g_s. Unlike S. oblata, the maximal photosynthetic rate (P _max) in S. pinnatifoliaoccurred around 08:00 and then fell down, indicating this species was sensitive to higher temperature and high photosynthetic photon flux density. However, such phenomenon was interrupted by the leaf development rhythms before summer. A relatively lower P _N together with a lower leaf area and shoot growth showed the capacity for carbon assimilation was poorer in S. pinnatifolia.This revised version was published online in March 2005 with corrections to the page numbers.     

River forcing at work: ecological modeling of prograding and regressive deltas

Two explicit landscape simulation models were used to investigate habitat shifts in coastal Louisiana due to varying river forcing and sea level rise scenarios. Wetland conversion to open water and yearly shifts of marsh habitats in two contrasting estuarine regions were examined; the Atchafalaya delta which is a prograding delta area with strong riverine input, and the Barataria Basin is a regressive delta with high wetland loss which is isolated from riverine input. The models linked several modules dynamically across spatial and temporal scales. Both models consisted of a vertically integrated hydrodynamic model coupled with process-based biological modules of above and below ground primary productivity and soil dynamics. The models explored future effects of possible sea level rise and river diversion plans for 30 and 70-year projections starting in 1988. Results showed that increased river forcing had large land preservation impacts, and indicated that healthy functioning of the Mississippi Delta depends largely on inputs of freshwater, nutrients, and sediments in river water. These types of models are useful for research and as management tools for predicting the effects of regional impacts on structural landscape level changes.     

金矮生苹果叶片气体交换参数对土壤水分的响应

 在黄土高原半干旱地区,通过测定10年生金矮生苹果（Malus pumila cv. Goldspur）叶片气体交换参数与土壤水分的定量关系,探讨了土壤水分胁迫对光合作用的影响规律,以确定苹果园节水灌溉适宜的土壤水分调控标准。结果表明：叶片的净光合速率（Pn）、蒸腾速率（Tr）、水分利用效率（WUE）、气孔导度（Gs）、细胞间隙CO2浓度（Ci）和气孔限制值（Ls）对土壤水分的变化具有明显不同的阈值反应。土壤含水量（SWC）大约在田间持水量的60%～86%范围内,Pn和Tr均保持较高的水平,小于田间持水量的60%～86%后,两者均随土壤湿度的减少而明显下降。维持较高叶片水分利用效率（WUE）的SWC约在田间持水量的50%～71%左右。当SWC小于田间持水量的48%以后,Gs和Ls明显降低,而Ci急剧增加,水分胁迫条件开始直接作用于叶肉细胞,导致光合速率下降,由气孔限制因素转变为非气孔因素。据此我们认为：在半干旱黄土高原地区,金矮生苹果园节水灌溉适宜的SWC范围大约在田间持水量的50%～71%左右,所允许的土壤水分亏缺程度为田间持水量的48%左右。     

六盘山林区几种土地利用方式下土壤活性有机碳的比较

 应用KMnO4氧化法测定分析了六盘山林区天然次生林（杂灌林、山杨（Populus davidanda）和辽东栎（Querces liaotungensis）林）、农田、草地和人工林（13、18和25年华北落叶松（Larix principis-rupprechtii））土壤活性有机碳含量及分配比例的差异。结果表明：农田和草地土壤活性有机碳含量比天然次生林分别低60%和36%,差异主要在0～70 cm土层;人工林比农田和草地分别高129%和29%,差异主要在0～50 cm土层。农田和草地土壤活性有机碳分配比例比天然次生林分别低11%和4%以上, 差异主要在0～20 cm与70～110 cm土层;人工林比农田和草地分别高13.3%和5.3%,差异主要在0～110 cm土层。土壤活性有机碳含量和分配比例随土层加深而递减,其中天然次生林和人工林土壤活性有机碳含量随土层加深而递减的幅度比农田和草地中大,农田土壤活性有机碳分配比例随土层加深而递减幅度较大。不同土地利用方式间土壤活性有机碳含量的差异比活性有机碳分配比例的差异大,土壤活性有机碳含量随土层加深而递减的幅度比分配比例随土层加深而递减的幅度大。这可能由土壤有机碳的输入、稳定性、质量和根系分布等差异所致。结果说明土壤活性有机碳含量和分配比例随天然次生林变成农田或草地而降低,随农田或草地中造林而增加,且土壤活性有机碳含量的变化幅度比分配比例大。另外,土壤活性有机碳含量和分配比例在土壤剖面的分布也随土地利用变化而改变,其中活性有机碳含量的变化幅度比分配比例大。     

临床常见L型细菌的分布及耐药性变化分析

目的了解临床主要L型致病菌的分布以及对目前常用性变化趋势.方法对2000年7月～2003年7月临床分离的753株药性进行回顾性分析.结果金黄色葡萄球菌、大肠埃希菌、最常见,它们共同对阿米卡星霉素敏感,敏感率达77%以上,共同对罗红霉素、氨苄西林、克林霉素、阿奇霉素耐药,耐药率均在45%以上.结论与我院5年前及10年前L型细菌耐药性对比,抗生素耐药性已发生变迁.掌握L型细菌耐药性的动态,合理使用抗生素.     

Morphology and wall ultrastructure of the spores of the Lower Devonian plant Oocampsa catheta Andrews et al., 1975

The enigmatic Lower Devonian plant Oocampsa catheta Andrews et al. (Can. J. Bot. 53 (1975) 1719) is considered intermediate between the trimerophytes and progymnosperms. In order to shed light on its evolutionary relationships, the morphology and ultrastructure of its sporangium and spores were analysed using light, scanning electron and transmission electron microscopy. In addition, dispersed spores (Grandispora douglastownense McGregor (Palaeontographica B 142 (1973) 1) and Grandispora ?macrotuberculata (Trudy VNIGNI 37 (1963) 18) McGregor (Palaeontographica B 142 (1973) 1), considered to possibly represent forms derived from O. catheta, were also examined. It is concluded that G. douglastownense and G. ?macrotuberculata are probably end members of the same spore complex and most likely are dispersed spores produced by O. catheta. Oocampsa catheta spores are bilayered. An inner body has an innermost part consisting of continuous, parallel-stacked, laminae and an outermost part consisting of more erratic, anastomosing, laminae. The inner body is surrounded by an homogeneous outer layer that is extended at the equator forming a pseudozona, and is folded on the proximal surface forming the trilete mark and on the distal surface forming spinose ornament. The spores are partially camerate. On the inside of the sporangium wall there is a layer probably representing the residue left following degeneration of a (probably secretory) tapetum. Spore morphology, gross structure and wall ultrastructure are compared to that of extant and fossil plant groups, and it is concluded that the spores of O. catheta are highly distinctive and do not conform closely to any plant group, although they show most in common with the spores of the progymnosperms.     

Integrated responses of hydraulic architecture, water and carbon relations of western hemlock to dwarf mistletoe infection

Dwarf mistletoe (Arceuthobium spp.) is a hemiparasite that is said to be the single‐most destructive pathogen of commercially valuable coniferous trees in many regions of the world. Although its destructive nature is well documented in many respects, its effects on the physiology of its host are poorly understood. In the present study, water and carbon relations were characterized over a range of scale from leaf to whole tree in large (40‐ to 50‐m‐tall) individuals of western hemlock (Tsuga heterophylla (Raf.) Sarg.) that were either heavily infected, or uninfected with hemlock dwarf mistletoe (Arceuthobium tsugense). Specific hydraulic conductivity (k_s) of infected branches was approximately half that of uninfected branches, yet leaf‐specific conductivity (k_L) was similar because leaf area : sapwood area ratios (A_L : A_S) of infected branches were lower. Pre‐dawn and minimum leaf water potential and stomatal conductance (g_s) were similar among infected and uninfected trees because adjustments in hydraulic architecture of infected trees maintained k_L despite reduced k_s. Maximum whole‐tree water use was substantially lower in infected trees (approximately 55 kg d^?1) than in uninfected trees (approximately 90 kg d^?1) because reduced numbers of live branches in infected trees reduced whole‐tree A_L : A_S in a manner consistent with that observed in infected branches. Maximum photosynthetic rates of heavily infected trees were approximately half those of uninfected trees. Correspondingly, leaf nitrogen content was 35% lower in infected trees. Foliar δ¹³C values were 2.8‰ more negative in infected than in uninfected individuals, consistent with the absence of stomatal adjustment to diminished photosynthetic capacity. Adjustments in hydraulic architecture of infected trees thus contributed to homeostasis of water transport efficiency and transpiration on a leaf area basis, whereas both carbon accumulation and photosynthetic water use efficiency were sharply reduced at both the leaf and whole‐tree scale.     

Diurnal depression of leaf hydraulic conductance in a tropical tree species

Diurnal patterns of hydraulic conductance of the leaf lamina (K_leaf) were monitored in a field‐grown tropical tree species in an attempt to ascertain whether the dynamics of stomatal conductance (g_s) and CO₂ uptake (A_leaf) were associated with short‐term changes in K_leaf. On days of high evaporative demand mid‐day depression of K_leaf to between 40 and 50% of pre‐dawn values was followed by a rapid recovery after 1500 h. Leaf water potential during the recovery stage was less than ?1 MPa implying a refilling mechanism, or that loss of K_leaf was not linked to cavitation. Laboratory measurement of the response of K_leaf to Ψ_leaf confirmed that leaves in the field were operating at water potentials within the depressed region of the leaf ‘vulnerability curve’. Diurnal courses of K_leaf and Ψ_leaf predicted from measured transpiration, xylem water potential and the K_leaf vulnerability function, yielded good agreement with observed trends in both leaf parameters. Close correlation between depression of K_leaf, g_s and A_leaf suggests that xylem dysfunction in the leaf may lead to mid‐day depression of gas exchange in this species.