中国明对虾Toll样受体基因的克隆与表达分析

对虾病害在世界范围内的广泛传播，给水产养殖和沿海农村经济造成了重大损失。自1993 年对虾白斑病暴发以来，中国明对虾的养殖一直一蹶不振。引起对虾大规模死亡的原因是多方面的，其主要原因是养殖环境恶化、对虾种质退化和抗病力下降。因此，深入开展对虾免疫机制研究，并在此基础上寻找对虾疾病防治的有效方法，改良种质和培育抗病品系，已成为对虾养殖业走可持续发展之路的当务之急。 Toll 样受体（Toll-like receptors, TLRs）家族是进化保守的哺乳动物模式识别蛋白（pattern recognition receptors, PRR），在先天免疫系统中起着非常重要的作用。本研究采用同源克隆和RACE（rapid amplification of cDNA ends）技术从中国明对虾中克隆到Toll 样受体同源基因，并将其命名为FcToll。它全长4115 bp，3’UTR 包含16 个poly A 尾巴，开放阅读框编码931 个氨基酸的多肽。预测的该多肽包含典型的Toll 样受体结构，分为胞外区、跨膜区和胞内区。其中胞外区有信号肽，有16 个富含亮氨酸的重复序列eucine-rich repeats, LRR），并含有2个LRR-C 末端基序和2 个LRR-N 末端基序；跨膜区是23 个氨基酸的一次跨膜结构域；胞内区是含有139 个氨基酸的TIR 结构域（Toll/Interleukin-1R）。克隆 发现FcToll 的基因组结构包含5 个外显子和4 个内含子。系统发生分析揭示FcToll归属于“昆虫型”的无脊椎动物Toll 样受体家族。组织分布研究发现FcToll 在中国明对虾中是组成型表达的，在淋巴器官中表达量较显著。分别利用不同病原体刺激健康的中国明对虾，Real-time PCR 发现该基因在刺激后表达水平呈现不同的表达谱：灭活鳗弧菌（Vibrio anguillarum）注射后5 小时，该基因表达显著 上调；而WSSV（white spot syndrome virus）注射后该基因表达则迅速下调，感染后23 小时内其表达水平均低于对应时间点的对照组。这就表明FcToll 可能参与中国明对虾的先天免疫防御，尤其可能参与入侵弧菌的免疫应答。

Effects of temperature and delayed initial feeding on the survival and growth of Japanese flounder larvae

The effects of the timing of initial feeding (0, 1, 2 3 and 4 days after yolk exhaustion) and temperature (15, 18 and 21degrees C) on the point-of-no-return (PNR), survival and growth of laboratory-reared Japanese flounder Paralichthys olivaceus larvae were studied under controlled conditions. The larvae reached PNR on 7(.)7, 5(.)2 and 4(.)2 days-post-hatching (dph) at 15, 18 and 2 V C, respectively. At each temperature, larval growth did not differ significantly among the delayed initial feedings 1 day before PNR but decreased significantly in larvae first fed after that. In the treatments where initial feeding was equally delayed, larvae grew significantly faster at 18 and 21degrees C than at 15degrees C. The larvae survived apparently better at 15 and 18degrees C than at 21degrees C when initial feeding was equally delayed. At each temperature, survival of the larvae first fed before PNR did not differ noticeably, while delayed initial feeding after that apparently reduced their survival. These results indicated that there existed a negatively temperature-dependent PNR in the Japanese flounder larvae. Survival and growth of the larvae strongly depended on temperature as well as the timing of initial feeding. High temperature accelerated the yolk exhaustion and growth of the larvae and thus reduced their starvation tolerance and survival. To avoid potential starvation mortality and obtain good growth, the Japanese flounder larvae must establish successful initial feeding within 2 days after yolk exhaustion at 15degrees C and within 1 day at both 18 and 21degrees C. (C) 2005 The Fisheries Society of the British Isles.

Structural studies on a novel fucogalactan sulfate extracted from the brown seaweed Laminaria japonica

A low molecular weight fucogalactan, obtained from the brown seaweed Laminaria japonica, was separated into three fractions (LF1, LF2 and LF3) by DEAE-Sepharose FF column chromatography. All three fractions contained predominantly fucose, sulfate group and galactose. The results showed that the main fraction LF2 consisted of L-fucose, D-galactose and sulfate at a molar ratio 6:1:9. Structural study on the LF2 was carried out by NMR spectroscopy. The backbone of LF2 was primarily (1 -> 3)-linked alpha-L-fucopyranose residues (75%) and a few (1 -> 4)-alpha-L-fucopyranose linkages (25%). The branch points were at C-4 of 3-linked alpha-L-fucopyranose residues by beta-D-galactopyranose unites (35%, molar ratio) or at C-2 of 3-linked alpha-L-fucopyranose residues by non-reducing terminal fucose unites (65%, molar ratio). Sulfate groups occupied at position C-4 or C-2, sometimes C-2, 4 to fucose residues, and C-3 and/or C-4 to galactose residues. The structure of LF2 was supposed as following: [GRAPHICS] (C) 2010 Elsevier B.V. All rights reserved.

青藏高原不同海拔矮嵩草抗逆性的比较研究

主要对生长在海拔4000m (大坂山) , 3200m (海北站) 和2200m (西宁) 地区同种矮嵩草的生理生态适应特性进行了比较研究。结果表明：生长在3个不同海拔地区的矮嵩草其生长发育和干物质积累具有明显差异,随着海拔高度的增加, 植株高度明显变低, 叶面积、叶绿素含量和干物质积累减少; 类胡萝卜素和类黄酮含量增加; 光合速率、光饱和点和光补偿点提高; 光呼吸强度减弱。在花果前期, 海拔4000m 处植株地上组织的蔗糖、果糖、葡萄糖和可溶性总糖含量分别比3200m 处的高65.4% , 110.2% , 121.6% 和84.6%; 地下组织的分别高5.6% , 17.8% , 88.6% 和43.8%。在枯黄前期, 两地地下组织的蔗糖、果糖、葡萄糖和可溶性总糖含量则高于地上组织的含量。同时, 大坂山和海北站地区的植株叶过氧化物酶活性平均比西宁的分别高88.2% 和38.8%。提示青藏高原地区高海拔矮嵩草其所以具有很强的抗逆能力, 这与它结构功能的特异性, 抗寒物质和过氧化物酶活性的明显增加密切相关。

Infrared heater arrays for warming ecosystem field plots

There is a need for methodology to warm open-field plots in order to study the likely effects of global warming on ecosystems in the future. Herein, we describe the development of arrays of more powerful and efficient infrared heaters with ceramic heating elements. By tilting the heaters at 45 degrees from horizontal and combining six of them in a hexagonal array, good uniformity of warming was achieved across 3-m-diameter plots. Moreover, there do not appear to be obstacles (other than financial) to scaling to larger plots. The efficiency [eta(h) (%); thermal radiation out per electrical energy in] of these heaters was higher than that of the heaters used in most previous infrared heater experiments and can be described by: eta(h) = 10 + 25exp(-0.17 u), where u is wind speed at 2 m height (m s(-1)). Graphs are presented to estimate operating costs from degrees of warming, two types of plant canopy, and site windiness. Four such arrays were deployed over plots of grass at Haibei, Qinghai, China and another at Cheyenne, Wyoming, USA, along with corresponding reference plots with dummy heaters. Proportional integral derivative systems with infrared thermometers to sense canopy temperatures of the heated and reference plots were used to control the heater outputs. Over month-long periods at both sites, about 75% of canopy temperature observations were within 0.5 degrees C of the set-point temperature differences between heated and reference plots. Electrical power consumption per 3-m-diameter plot averaged 58 and 80 kW h day(-1) for Haibei and Cheyenne, respectively. However, the desired temperature differences were set lower at Haibei (1.2 degrees C daytime, 1.7 degrees C night) than Cheyenne (1.5 degrees C daytime, 3.0 degrees C night), and Cheyenne is a windier site. Thus, we conclude that these hexagonal arrays of ceramic infrared heaters can be a successful temperature free-air-controlled enhancement (T-FACE) system for warming ecosystem field plots.

Diurnal, seasonal and annual variation in net ecosystem CO2 exchange of an alpine shrubland on Qinghai-Tibetan plateau

Thus far, grassland ecosystem research has mainly been focused on low-lying grassland areas, whereas research on high-altitude grassland areas, especially on the carbon budget of remote areas like the Qinghai-Tibetan plateau is insufficient. To address this issue, flux of CO2 were measured over an alpine shrubland ecosystem (37 degrees 36'N, 101 degrees 18'E; 325 above sea level [a. s. l.]) on the Qinghai-Tibetan Plateau, China, for 2 years (2003 and 2004) with the eddy covariance method. The vegetation is dominated by formation Potentilla fruticosa L. The soil is Mol-Cryic Cambisols. To interpret the biotic and abiotic factors that modulate CO2 flux over the course of a year we decomposed net ecosystem CO2 exchange (NEE) into its constituent components, and ecosystem respiration (R-eco). Results showed that seasonal trends of annual total biomass and NEE followed closely the change in leaf area index. Integrated NEE were -58.5 and -75.5 g C m(-2), respectively, for the 2003 and 2004 years. Carbon uptake was mainly attributed from June, July, August, and September of the growing season. In July, NEE reached seasonal peaks of similar magnitude (4-5 g C m(-2) day(-1)) each of the 2 years. Also, the integrated night-time NEE reached comparable peak values (1.5-2 g C m(-2) day(-1)) in the 2 years of study. Despite the large difference in time between carbon uptake and release (carbon uptake time < release time), the alpine shrubland was carbon sink. This is probably because the ecosystem respiration at our site was confined significantly by low temperature and small biomass and large day/night temperature difference and usually soil moisture was not limiting factor for carbon uptake. In general, R-eco was an exponential function of soil temperature, but with season-dependent values of Q(10). The temperature-dependent respiration model failed immediately after rain events, when large pulses of R-eco were observed. Thus, for this alpine shrubland in Qinghai-Tibetan plateau, the timing of rain events had more impact than the total amount of precipitation on ecosystem R-eco and NEE.

Chemical constituents from the whole plant of Euphorbia altotibetic

Four new jatrophane diterpenoids, altotibetin A (1), altotibetin B (2), altotibetin C (3), altotibetin D (4), and nine known compounds, beta-sitosterol, cycloart-23-ene-3beta,25-diol, cycloart-25-ene-3beta,24-diol, lupeol acetate, scopoletin, kaempferol, uracil, uridine, astragalin, and daucosterol have been isolated from the whole plant of Euphorbia altotibetic PAULS. Their structures were established by spectral methods, and the configurations of 1 and 2 were confirmed by X-ray analysis.

末次盛冰期以来中国陆地生态系统碳储量变化研究

Carbon is an essential element for life, food and energy. It is also a key element in the greenhouse gases and therefore plays a vital role in climatic changes. The rapid increase in atmospheric concentration of CO_2 over the past 150 years, reaching current concentrations of about 370 ppmv, corresponds with combustion of fossii fuels since the beginning of the industrial age. Conversion of forested land to agricultural use has also redistributed carbon from plants and soils to the atmosphere. These human activities have significantly altered the global carbon cycle. Understanding the consequences of these activities in the coming decades is critical for formulating economic, energy, technology, trade, and security policies that will affect civilization for generations. Under the auspices of the International Geosphere-Biosphere Programme (IGBP), several large international scientific efforts are focused on elucidating the various aspects of the global carbon cycle of the past decade. It is only possible to balance the global carbon cycle for the 1990s if there is net carbon uptake by terrestrial ecosystems of around 2 Pg C/a. There are now some independent, direct evidences for the existence of such a sink. Policymarkers involved in the UN Framework Convention on Climate Change (UN-FCCC) are striving to reach consensuses on a 'safe path' for future emissions, the credible predictions on where and how long the terrestrial sink will either persist at its current level, or grow/decline in the future, are important to advice the policy process. The changes of terrestrial carbon storage depend not only on human activities, but also on biogeochemical and climatological processes and their interaction with the carbon cycles. In this thesis, the climate-induced changes and human-induced changes of carbon storage in China since the past 20,000 years are examined. Based on the data of the soil profiles investigated during China's Second National Soil Survey (1979-1989), the forest biomass measured during China's Fourth National Forest Resource Inventory (1989-1993), the grass biomass investigated during the First National Grassland Resource Survey (1980-1991), and the data collected from a collection of published literatures, the current terrestrial carbon storage in China is estimated to -144.1 Pg C, including -136.8 Pg C in soil and -7.3 Pg C in vegetation. The soil organic (SOC) and inorganic carbon (SIC) storage are -78.2 Pg C and -58.6 Pg C, respectively. In the vegetation reservoir, the forest carbon storage is -5.3 Pg C, and the other of-1.4 Pg C is in the grassland. Under the natural conditions, the SOC, SIC, forest and grassland carbon storage are -85.3 Pg C, -62.6 Pg C, -24.5 Pg C and -5.3 Pg C, respectively. Thus, -29.6 Pg C organic carbon has been lost due to land use with a decrease of -20.6%. At the same time, the SIC storage also has been decreased by -4.0 Pg C (-6.4%). These suggest that human activity has caused significant carbon loss in terrestrial carbon storage of China, especially in the forest ecosystem (-76% loss). Using the Paleocarbon Model (PCM) developed by Wu et al. in this paper, total terrestrial organic carbon storage in China in the Last Glacial Maximum (LGM) was -114.8 Pg C, including -23.1 Pg C in vegetation and -86.7 Pg C in soil. At the Middle Holocene (MH), the vegetation, soil and total carbon were -37.3 Pg C, -93.9 Pg C and -136.0 Pg C, respectively. This implies a gain of-21.2 Pg C in the terrestrial carbon storage from LGM to HM mainly due to the temperature increase. However, a loss of-14.4 Pg C of terrestrial organic carbon occurred in China under the current condition (before 1850) compared with the MH time, mainly due to the precipitation decrease associated with the weakening of the Asian summer monsoon. These results also suggest that the terrestrial ecosystem in China has a substantial potential in the restoration of carbon storage. This might be expected to provide an efficient way to mitigate the greenhouse warming through land management practices. Assuming that half of the carbon loss in the degraded terrestrial ecosystem in current forest and grass areas are restored during the next 50 years or so, the terrestrial ecosystem in China may sequestrate -12.0 Pg of organic carbon from the atmosphere, which represents a considerable offset to the industry's CO2 emission. If the ' Anthropocene' Era will be another climate optimum like MH due to the greenhouse effect, the sequestration would be increased again by -4.3 - 9.0 Pg C in China.

红枫湖溶解有机质的分离富集、地球化学特征和环境效应

作为全球碳循环的主要组成部分，溶解有机质在水生生态系统的各种物理、化学和生物过程中起着十分重要的作用：它是湖泊异养型生物所需能量的主要提供者；是湖泊水体pH的调节剂和控制因素；能够与金属离子或有机污染物相互作用，从而影响它们的迁移转化、毒性和生物可利用性；溶解有机质也是饮用水氯化工艺中生成具有致癌作用消毒副产品的主要前驱物质。溶解有机质组成和结构十分复杂，一般由腐殖质和非腐殖质物质组成，相应的环境地球化学特征和行为也各不相同。因此，研究溶解有机质各分离组分的结构特征和环境效应，将有助于我们对溶解有机质复杂化学结构、循环特征及行为特征的深入理解；有助于揭示溶解有机质对环境中微量污染物的迁移、转化、毒性和生物有效性的影响机理和贡献因素；为水环境评价、预测、控制和管理提供科学依据。 本论文选择云贵高原山区湖泊—红枫湖为研究对象，利用XAD树脂分离技术，把湖泊水体中溶解有机质按极性的不同分成了疏水性酸、碱、中性物质和亲水性酸、碱、中性物质等六种有机组分。主要运用元素分析、有机碳分析仪、傅立叶变换红外光谱、紫外－可见分光光度，高效液相体积排阻色谱、三维荧光光谱和稳定同位素质谱仪等现代分析方法和手段，对各有机组分的地球化学特征及来源的进行了表征和探讨。同时利用荧光猝灭滴定技术研究了溶解有机质分离组分与铜的相互作用，利用顶空气相色谱法测定了各分离组分与氯气反应活性的大小，并确立了生成消毒副产物的主要前驱物质。本论文的研究成果主要有以下几点： 1.改进了分离流程：在XAD－8树脂分离溶解有机质流程的基础上，引入XAD－4树脂，对贵州红枫湖水体中溶解有机质进行了富集分离，得腐殖酸、富里酸、疏水性中性物质、亲水性酸、亲水性碱、亲水性中性物质等六种有机组分，回收率为82%。各分离组分的组成与其它天然水体的组成接近，其中以富里酸为主，占分离组分的51%。 2.溶解有机质分离组分化学结构特征的研究：元素分析表明疏水性组分具有较高的碳和硫含量，而亲水性组分O/C比较高，含有较多的含氧官能团；傅立叶变换红外光谱表明各分离组分在3424－3434 cm-1具有O-H和N-H的吸收峰，腐殖酸组分主要为含氮和聚糖物质，富里酸和亲水性酸表现强的羧基吸收峰。高效体积排阻色谱表明各六种有机组分的分子量较小，重均(Mw)和数均(Mn)分子量分别集中在1688-2355Da和1338-1928Da之间，其中Mw和紫外吸收比值(E2/E3)之间呈负相关关系；三维荧光光谱显示六种有机组分表现了4种不同类型的荧光峰，紫外区类富里酸荧光峰peakA和可见区类富里酸荧光峰peakC；疏水性中性物质还表现了两种类蛋白荧光峰peakB和peakD。荧光强度与紫外吸光系数SUVA254之间呈显著正相关关系，说明了产生荧光和紫外的物质具有某些相似的官能团，其中芳香官能团和共轭双键在这两类光谱的产生中具有重要作用。本研究进一步揭示了溶解有机质不同有机组分的分子量分布、荧光光谱特征和紫外吸收特征之间的一致性，反映了各有机组分之间的亲水、疏水与分子量、光谱特征之间的内在联系，本研究有助于加我们深对溶解有机质复杂性和相似性及化学结构与行为的进一步认识。 3.溶解有机质分离组分来源问题的探讨：我们利用δ13C及C/N比值并结合荧光光谱特征来指示溶解有机质的来源。各分离组分的δ13C及C/N比值表明富里酸主要来自陆源C3植被形成的土壤有机质，而腐殖酸、疏水性中性物质、亲水性酸、亲水性碱、亲水性中性物质属于陆源和内源的混合来源，其中腐殖酸、亲水性酸、亲水性碱接近红枫湖藻类一端，而疏水性中性物质和亲水性中性物质接近陆源一端。荧光光谱表明疏水性中性物质中含有类蛋白荧光峰，可能暗示了该组分还与人类活动有关。该研究加深了对溶解有机质来源的多样性和影响因素复杂性的认识。 4.溶解有机质分离组分与铜离子的相互作用，利用荧光猝灭滴定技术研究了分离组分与铜离子的相互作用，结果表明溶解有机质滴加铜离子后荧光强调显著降低，同时发射波长Em发生蓝移，而激发波长Ex基本不变，说明了分离有机组分在与铜离子相互作用后，π电子减少，共轭性和芳香型降低，直线型分子向非直线型分子转变；溶解有机质分离组分与铜相互作用的滴定曲线与修正的Stern-Volmer模型十分吻合；分离组分的稳定常数logK介于4.73-5.16之间（C峰）和4.64-5.24之间（A峰），logKA与logKC与总酸度以及与酚羟基之间存在显著相关性, 与羧基含量之间也有弱相关关系，说明铜离子优先与配体中强配位点（酚羟基）络合，其次为弱配位基（羧基）。该研究揭示了云贵高原山区湖泊溶解有机质分离组分与金属离子相互作用的差异性和影响因素，为水环境中金属离子迁移转化和毒性的评价提供理论依据。 5.溶解有机质分离组分卤代活性的比较：我们运用顶空气相色谱法测定了红枫湖分离组分与消毒剂反应生成有机卤代物的情况。结果表明红枫湖分离组分氯化消毒副产物主要以三氯甲烷(CHCl3)和二溴一氯甲烷(CHBr2Cl)为主，富里酸是生成三卤甲烷的主要前驱物质，同时富里酸的卤代反应活性也最强。该研究揭示了云贵高原山区湖泊中富里酸是生成消毒副产物的主要前驱物质，该组分以陆源有机质输入为主。因此，该研究对饮用水消毒具有一定的现实意义。

Performance of a mixed-conducting ceramic membrane reactor with high oxygen permeability for methane conversion

A mixed-conducting perovskite-type Ba0.5Sr0.5Co0.8Fe0.2O3-delta (BSCFO) ceramic membrane reactor with high oxygen permeability was applied for the activation of methane. The membrane reactor has intrinsic catalytic activities for methane conversion to ethane and ethylene. C-2 selectivity up to 40-70% was achieved, albeit that conversion rate were low, typically 0.5-3.5% at 800-900 degreesC with a 50% helium diluted methane inlet stream at a flow rate of 34 ml/min. Large amount of unreacted molecular oxygen was detected in the eluted gas and the oxygen permeation flux improved only slightly compared with that under non-reactive air/He experiments. The partial oxidation of methane to syngas in a BSCFO membrane reactor was also performed by packing LiLaNiO/gamma -Al2O3 with 10% Ni loading as the catalyst. At the initial stage, oxygen permeation flux, methane conversion and CO selectivity were closely related with the state of the catalyst. Less than 21 h was needed for the oxygen permeation flux to reach its steady state. 98.5% CH4 conversion, 93.0% CO selectivity and 10.45 ml/cm(2) min oxygen permeation flux were achieved under steady state at 850 degreesC. Methane conversion and oxygen permeation flux increased with increasing temperature, No fracture of the membrane reactor was observed during syngas production. However, H-2-TPR investigation demonstrated that the BSCFO was unstable under reducing atmosphere, yet the material was found to have excellent phase reversibility. A membrane reactor made from BSCFO was successfully operated for the POM reaction at 875 degreesC for more than 500h without failure, with a stable oxygen permeation flux of about 11.5 ml/cm(2) min. (C) 2001 Elsevier Science B.V. All rights reserved.

Cobalt boride catalysts for hydrogen generation from alkaline NaBH4 solution

Cobalt boride precursors were synthesized via chemical reaction of aqueous sodium borohydride with cobalt chloride, and followed by heat-treating at various temperatures. The as-prepared Co-B catalysts were characterized and analyzed by X-ray diffraction (XRD), nitrogen adsorption-desorption and catalytic activity test; and were adopted to help accelerating hydrolysis reaction of NaBH4 alkaline solution. The Co-B catalyst treated at 500 degrees C exhibits the best catalytic activity, and achieves an average H, generation rate of 2970 ml/min/g, which may give a successive H, supply for a 481 W proton exchange membrane fuel cell (PEMFC) at 100% H-2 utilization. (c) 2005 Elsevier B.V. All rights reserved.