Differences of ecological functions inside and outside the wetland nature reserves in Sanjiang Plain, China

Conservation effectiveness of wetland nature reserves is determined by both the management intensity inside the reserves and the hydrological status outside the reserves. Therefore, differences of ecological functions inside and outside the reserves are an integrated indictor for assessing conservation effectiveness. Based on the land use map created from Landsat-TM satellite image and 1:50000 Digital Elevation Model (DEM) data in the study area, the catchments that belong to the wetland reserves were determined as their hydrological sensitive zones by SWAT (Soil and Water Assessment Tool) hydrological model. The ecological function indices of wetland reserves and their corresponding hydrological sensitive zones were calculated through expert consultation and value assessment on wetland ecosystem service functions. The results showed that the ecological functions of national wetland reserves were better than those of local reserves in general. However, the wetland ecological functions of hydrological sensitive zones of the former were not always better than those of the latter. Meanwhile, clustering analysis showed that the wetland ecological functions of several adjacent reserves in Nongjiang-Bielahonghe watershed were similar. But correlation analysis found that there existed a remarkable positive correlation between the wetland ecological function indices of local reserves and their hydrological sensitive zones.     

The effect of cocultivation treatments on transformation efficiency in pea (<Emphasis Type="Italic">Pisum sativum</Emphasis> L.)

The effect of chemical additives (acetosyringone, AS; L-cysteine, CYS; dithiothreitol, DTT; glutathione, GSH; cellulase, CEL; pectinase, PEC) and light regimes (16/8 light/dark photoperiod, 16L/8D; continuous light, 24L; continuous dark, 24D) applied during cocultivation procedure of pea explants with Agrobacterium tumefaciens on transformation efficiency was studied. A hypervirulent strain of A. tumefaciens EHA 105 with two plasmids, namely pGT89 and pBIN19, both carrying reporter gus-int gene, and bar or nptII selectable marker gene, respectively, was used for genetic transformation of cotyledonary node explants of three dry seed pea cultivars Adept, Komet and Menhir. The focus was laid on cocultivation step (48 h) of transformation protocol. After chemical or physical treatments, transient GUS expression was recorded 20 days after cocultivation as a measure of successful transformation, using a four category scale (0 – without GUS expression, 1 – weak, 2 – medium and 3 – strong GUS expression) for calculation of IGE (Intensity of GUS Expression). Of the tested chemical cocultivation additives, 100 μM AS and 50 mg CYS significantly improved GUS expression (IGE value), while DTT, GSH and both macerating enzymes (CEL, PEC used either separately or in combination) either had no positive effect or were even negative. There were no statistically significant differences between the light regimes tested. Nevertheless, cocultivation in 24L, without chemical additives, reproducibly resulted in the highest frequency of explants scored in category 3 of GUS expression (followed by 24D and 16L/8D treatment). However, application of 100 μM AS reverted this trend. Cv. Adept yielded higher transformation frequencies than cvs. Menhir and Komet. Plasmid pGT89 produced a higher IGE value than pBIN19. Based on our results, the improved cocultivation step for pea consists of 48 h cocultivation at 20 ± 2°C, with 50 mg l⁻¹ CYS and 100 μM AS, 16L/8D photoperiod (or without AS in continuous light).     

Micro biochemical engineering to accelerate the design of industrial-scale downstream processes for biopharmaceutical proteins

The article examines how a small set of easily implemented micro biochemical engineering procedures combined with regime analysis and bioprocess models can be used to predict industrial scale performance of biopharmaceutical protein downstream processing. This approach has been worked on in many of our studies of individual operations over the last 10 years and allows preliminary evaluation to be conducted much earlier in the development pathway because of lower costs. It then permits the later large scale trials to be more highly focused. This means that the risk of delays during bioprocess development and of product launch are reduced. Here we draw the outcomes of this research together and illustrate its use in a set of typical operations; cell rupture, centrifugation, filtration, precipitation, expanded bed adsorption, chromatography and for common sources, E. coli, two yeasts and mammalian cells (GS-NSO). The general approach to establishing this method for other operations is summarized and new developments outlined. The technique is placed against the background of the scale-down methods that preceded it and complementary ones that are being examined in parallel. The article concludes with a discussion of the advantages and limitations of the micro biochemical engineering approach versus other methods.     

人工沟渠的生态环境效应研究综述

人工沟渠主要指以排水和灌溉为目的人工挖掘的水道.人工沟渠作为排水和引水的廊道改善了土壤的结构、促进了作物的生长,从而提高了农作物的产量;同时人工沟渠这种景观的存在对周围的环境也产生了巨大的影响.水文效应是被大家普遍接受的生态环境效应.在整个降雨期间或之后,观察显示出沟渠对出口径流的贡献：一些沟渠收集和向河流输送水;另一些沟渠收集水但是减慢了水流的速度.本文从水文效应、对元素地球化学循环、生物及其生境的影响到对生态环境整体影响方面总结了人工沟渠的生态环境效应,并对其进一步的研究提出一些建议,旨在最大限度发挥人工沟渠的生态环境效应,改善整个生态环境.     

Hydrologic Regime Controls Soil Phosphorus Fluxes in Restoration and Undisturbed Wetlands

Many wetland restoration projects occur on former agricultural soils that have a history of disturbance and fertilization, making them prone to phosphorus (P) release upon flooding. To study the relationship between P release and hydrologic regime, we collected soil cores from three restoration wetlands and three undisturbed wetlands around Upper Klamath Lake in southern Oregon, U.S.A. Soil cores were subjected to one of three hydrologic regimes—flooded, moist, and dry—for 7.5 weeks, and P fluxes were measured upon reflooding. Soils from restoration wetlands released P upon reflooding regardless of the hydrologic regime, with the greatest releases coming from soils that had been flooded or dried. Undisturbed wetland soils released P only after drying. Patterns in P release can be explained by a combination of physical and biological processes, including the release of iron‐bound P due to anoxia in the flooded treatment and the mineralization of organic P under aerobic conditions in the dry treatment. Higher rates of soil P release from restoration wetland soils, particularly under flooded conditions, were associated with higher total P concentrations compared with undisturbed wetland soils. We conclude that maintaining moist soil is the means to minimize P release from recently flooded wetland soils. Alternatively, prolonged flooding provides a means of liberating excess labile P from former agricultural soils while minimizing continued organic P mineralization and soil subsidence.     

Greenhouse gas buildup, sardines, submarine eruptions and the possibility of abrupt degradation of intense marine upwelling ecosystems

Widespread hypoxia and massive eruptions of noxious, radiatively active gases currently characterize the world's strongest eastern ocean upwelling zone. Theory, modelling results and observations suggest that the world's coastal upwelling zones will undergo progressive intensification in response to greenhouse gas buildup. This presents the prospect of progressive development of similarly degraded marine ecosystems in additional regions and of a contributing feedback loop involving associated additions to the global buildup rate of greenhouse gases, resulting further increases in upwelling intensity, creation of additional sources of greenhouse gas emissions, and so on. Abundant sardine stocks might be a mitigating factor opposing the process.     

影响祁连山区域地貌-水文系统各地理要素的主成分分析

祁连山区域地貌复杂,从而引起水文系统以及生态系统的复杂性。水文系统是引起生态系统复杂的重要原因之一。对影响祁连山区域地貌——水文系统的9个重要地理要素：即流域盆地的总高度、流域的海拔高度、流域周长、河道总长度、河道总数、平均分叉率、河谷最大坡度(度)、河源数以及流域面积进行了综合分析,将其归为3类,即流域盆地的规模,流域侵蚀状况和流域河系形态。在此基础上,认为若要在以后对影响祁连山区域地貌——水文系统地理要素进行分析时,可以直接选取流域面积,流域盆地出口的海拔高度和河道分叉率作为3类地理要素的代表,进行区域地貌——水文系统分析,从而能够降低分析问题的疑难程度与复杂性。     

三峡大老岭山地常绿落叶阔叶混交林林隙干扰研究 I．林隙基本特征

为探讨我国亚热带山地常绿落叶阔叶混交林的林隙干扰特征,对三峡大老岭地区这一植被类型进行调查,分析了植被中林隙的数量、类型及成因;林隙形成木（GM）的类型、数量、物种构成和径级结构,以及林隙和GM的多尺度空间格局特征。结果表明1）林隙密度为11.7个*hm-2;冠林隙和扩展林隙分别占森林面积的11.09%和27.06%。平均每个林窗的形成木为4.5株;单株GM形成的林隙只占17.46%,其中翻倒木集群性最强。对林隙形成的贡献大小次序是翻倒木>折干>枯立>折枝。2）林隙成因方面冬雪和春、秋冻雨的影响最大;病害影响其次;树木间的牵连和撞击扩大了林隙的范围;陡峭的地形增大林隙形成的机率;干旱的影响很小。3）68种GM主要是森林建群种;常绿树种形成林隙的平均机率高于落叶种。4）GM的胸径结构表明本地森林林隙干扰十分频繁。