Seasonal variation in oxygen isotope composition of waters for a montane larch forest in Mongolia

Measurements of water oxygen isotopic composition were conducted in the 2003 growing season for a montane larch (Larix sibirica Ledeb.) forest in northern Mongolia, a transitional area from the south Siberian taiga to the Asian steppe. Oxygen isotopic composition of foliar water and its daily variability were found to be sensitive to atmospheric evaporative demand. During most of the growing season, water sources used by larch trees were from the upper 30-cm surface layer of the soil when precipitation input was large, and were from the deeper layer when the water supply at the upper soil layer was limited. The Keeling plot method suggested that the forest returned soil water to the atmosphere predominantly by means of canopy transpiration during the peak growth period (in August).     

Multi-proxy studies in palaeolimnology

Multi-proxy studies are becoming increasingly common in palaeolimnology. Eight basic requirements and challenges for a multi-proxy study are outlined in this essay – definition of research questions, leadership, site selection and coring, data storage, chronology, presentation of results, numerical tools and data interpretation. The nature of proxy data is discussed in terms of physical proxies and biotic proxies. Loss-on-ignition changes and the use of transfer functions are reviewed as examples of problems in the interpretation of data from multi-proxy studies. The importance of pollen analysis and plant macrofossil analysis in multi-proxy studies is emphasised as lake history cannot be interpreted without knowledge of catchment history. Future directions are outlined about how multi-proxy studies can contribute to understanding biotic responses to environmental change.     

Analysis of the Relationships between Growth, Photosynthesis and Carbohydrate Metabolism Using Quantitative Trait Loci (QTLs) in Young Maize Plants Subjected to Water Deprivation

One hundred to 120 maize recombinant inbred lines at the mature fourth leaf stage derived from F-2 and Io parental lines were grown in a glasshouse and were deprived of water for 9 days in order to detect pertinent markers of the physiological response to water stress which may be used for breeding. Carbohydrate metabolism QTLs were compared to photosynthesis gas exchange QTLs. The locations of these QTLs were further compared with those of morphological trait QTLs when water availability varied. The traits ranged from three enzyme activities (invertase, sucrose-P synthase, ADP glucose pyrophosphorylase) and hexose, sucrose, starch content to CO₂ uptake and stomatal conductance, water status, leaf size, root/shoot ratio, and ABA (leaf, root and xylem sap). Four main results were obtained (1) only 14 % of QTLs were common to both drought and watered treatments, confirming the existence of stress specific chromosome regions, (2) the QTLs tended to form clusters, frequently consisting of QTLs from different classes (growth, photosynthesis, water status, carbohydrate metabolism and ABA), (3) carbohydrate metabolism trait QTLs were more frequently co-located with growth trait QTLs than photosynthesis related ones, especially in control conditions, (4) one co-location was observed between the three enzyme activities implied in sucrose and starch metabolism and a corresponding structural gene, which can be considered as a candidate gene for explaining part of the variability of each enzymatic trait (invertase, sucrose-P synthase, ADPglucose pyrophosphorylase). It is concluded that, carbohydrate metabolism provides valuable traits for understanding and improving maize responses to water stress.     

Effect of Silt, Water and Periphyton Quality on Survival and Growth of the Mayfly Heptagenia Sulphurea

The herbivorous mayfly Heptagenia sulphurea is characteristic of rivers with stony bottoms. Records from the 20th century showed that this species had disappeared from the Common Meuse in the Netherlands, probably due to river regulation or changes in water quality. A field survey in 2003 showed that H. sulphurea was present in the Geul tributary, approximately 300 m upstream of its confluence with the Common Meuse. H. sulphurea has not recolonized the Common Meuse despite improvements in water quality over the last decades. Concentration of suspended sediments in the River Meuse, however, is still high, much higher than in the beginning of the 20th century. The presence of a silt layer may limit the return of H. sulphurea in this river by reducing availability and quality of its food. The prime objective of this study was to investigate the impact of silt on survival and growth of H. sulphurea in a laboratory experiment. Furthermore, the impact of water and periphyton quality from the Common Meuse on survival and growth of this mayfly was also investigated. Results showed that neither water quality nor cultured periphyton from the Common Meuse reduced survival and growth of H. sulphurea. The presence of a silt layer resulted in a significantly lower growth rate of the mayfly larvae. It is concluded that the silt layer reduces the accessibility of the food. Covering of food is possibly one of the main factors limiting the recolonization of H. sulphurea and probably other benthic grazers in the Common Meuse.     

应用肠道微生物示踪地表水粪便污染的研究进展

人和动物的粪便已成为水污染的重要污染源, 严重威胁着饮水安全和经济发展。水质污染微生物的传统检测指示菌是总大肠菌群、粪大肠菌群、埃希大肠菌、肠球菌和梭菌属。经过调查发现, 上述指示菌由于在体外能存活并繁殖, 并且不同宿主之间没有差异性, 不能准确用于追踪污染粪便的来源, 因此该指标难以直接说明粪便污染源和污染程度。最近的研究表明, Faecalibaterium作为水体粪便污染来源追踪的指示微生物具有很多优点。本文综述了粪便污染指示菌以及其相关替代方法在水质检测中的研究进展, 对各种指示菌进行了优、缺点比较, 展望了Faecalibaterium的应用前景。     

水流对团头鲂(Megalobrama amblycephala)幼鱼游泳行为的影响

为探讨团头鲂幼鱼(Megalobrama amblycephala)游泳行为对水流的响应规律,该文通过特制鱼类游泳行为测定装置,测定了团头鲂幼鱼在25℃,0、0.1、0.2、0.3、0.4m/s流速条件下的游速、游距、转角、至中心点的距离及游泳轨迹。结果表明:随着流速的增大,个体游速、游距及转角值均相应增大。0、0.1及0.2m/s流速组间的游速、游距及转角差异均不显著(P>0.05),但显著小于0.3和0.4m/s组别,且0.3和0.4m/s流速组之间差异均不显著(P>0.05);整个时间段内,个体至中心点的距离随流速增大并未呈现明显规律性,各流速间差异不显著(P>0.05),游速与游距呈显著线性正相关,而与转角呈显著线性负相关,与至中心点的距离则无相关性;游泳轨迹随水流增大趋向复杂化。     

Seasonal plasticity of Ludwigia grandiflora under light and water depth gradients: An outdoor mesocosm experiment

Abiotic factors in the introduced area can limit the establishment of exotic species. Adaptation to new abiotic parameters through plastic responses is important for their establishment and distribution pattern. Survival and growth of exotic hydrophytes are related to their plasticity and their ability to adapt to local conditions. Light and water depth are two of the predominant factors determining survival, growth, distribution and abundance of aquatic plants. Although many studies have been carried out on the effect of water level and light on plant performance, their potential interactions are poorly understood. Here, we carried out an outdoor mesocosm experiment, in order to test the role of water depth, light intensity and their potential interactions on the growth and vigour of the invasive macrophyte species Ludwigia grandiflora. Three light intensities (100%, 70% and 50% of sunlight) and three water depths (30, 50 and 80 cm) were tested over a 6-week period, in spring, summer and autumn 2011. We showed that the mortality, biomass, apical and lateral growth of L. grandiflora, as well as its biomass allocation, varied according to the season and responded to both light intensity and water depth. Interactions between water depth and light intensity can have an amplifying effect on the growth of L. grandiflora. Similarities between shade and deep water adaptation responses were observed. A higher biomass and a high morphological plasticity in response to these factors were found particularly at the beginning of the life cycle. Although the invasive amphibious L. grandiflora shows a high tolerance to different water levels and light intensities, the optimal growth conditions for L. grandiflora in our experiment seem to be under full sunlight and in 30 cm of water. Colonization of light or low shade aquatic habitats, as well as shallow environments, can occur due to the high plasticity of L. grandiflora. These results may be important relative to increasing level of water bodies under climatic changes.