平台石墨炉原子吸收光谱法直接测定人眼视网膜下液中微量铬、锰

本文采用平台和硝酸镁硝酸钯混合基体改进剂相结合的方法,使铬和锰的灰化温度从1200℃提高至1600℃,克服了大量钾、钠、钙、镁等共存元素的干扰,可直接测定样品中微量铬和锰。对于铬和锰的检出限分别为5.6×10~(-11)g和9×10~(-11)g,相对标准偏差分别为8.7％和7.5％,测定结果与等离子体发射光谱法结果一致。

Investigation of EscA as a chaperone for the Edwardsiella tarda type III secretion system putative translocon component EseC

Edwardsiella tarda is an important Gram-negative enteric pathogen affecting both animals and humans. It possesses a type III secretion system (T3SS) essential for pathogenesis. EseB, EseC and EseD have been shown to form a translocon complex after secretion, while EscC functions as a T3SS chaperone for EseB and EseD. In this paper we identify EscA, a protein required for accumulation and proper secretion of another translocon component, EseC. The escA gene is located upstream of eseC and the EscA protein has the characteristics of T3SS chaperones. Cell fractionation experiments indicated that EscA is located in the cytoplasm and on the cytoplasmic membrane. Mutation with in-frame deletion of escA greatly decreased the secretion of EseC, while complementation of escA restored the wild-type secretion phenotype. The stabilization and accumulation of EseC in the cytoplasm were also affected in the absence of EscA. Mutation of escA did not affect the transcription of eseC but reduced the accumulation level of EseC as measured by using an EseC-LacZ fusion protein in Ed. tarda. Co-purification and co-immunoprecipitation studies demonstrated a specific interaction between EscA and EseC. Further analysis showed that residues 31-137 of EseC are required for EseC-EscA interaction, Mutation of EseC residues 31-137 reduced the secretion and accumulation of EseC in Ed. tarda. Finally, infection experiments showed that mutations of EscA and residues 31-137 of EseC increased the LD50 by approximately 10-fold in blue gourami fish. These results indicated that EscA functions as a specific chaperone for EseC and contributes to the virulence of Ed. tarda.

Using the ribosomal internal transcribed spacer (ITS) as a complement marker for species identification of red macroalgae

Barcodes based on mitochondrial cytochrome oxidase (mtDNA CO1) sequences are being used for broad taxonomic groups of animals with demonstrated success in species identification and cryptic species discovery, but it has become clear that complementation by a nuclear marker system is necessary, in particular for the barcoding of plants. Here, we propose the nuclear internal transcribed spacer (ITS) as a potentially usable and complementary marker for species identification of red macroalgae, as well as present a primary workflow for species barcoding. Data show that for most red macroalgal genera (except members of the family Delesseriaceae), the size of ITS region ranges from 600 to 1200 bp, and contains enough variation to generate unique identifiers at either the species or genus levels. Consistent with previous studies, we found that the ITS sequence can resolve closely related species with the same fidelity as mtDNA CO1. Significantly, we confirmed that length polymorphism in the ITS region (including 5.8S rRNA gene) can be utilized as a character to discriminate red macroalgal species. As a complementary marker, the verifiable nuclear ITS region can speed routine identification and the detection of species, advance ecological and taxonomic inquiry, and permit rapid and accurate analysis of red macroalgae.

Expression of human epidermal growth factor gene in cyanobacteria

The human epidermal growth factor (hEGF) is a small single-chain polypeptide of 53 amino acid residues. It can stimulate the proliferation of many cell types, mainly those of epidermal and epithelial tissues both in vivo and in vitro. A vector pRL-hEGF was constructed using plasmids pRL-489 and pUC-hEGF. The synthetic hEGF gene was recombined into the downstream of strong promoter psbA in plasmids pRL-489. Then, the vector was introduced into Synechococcus sp. PCC 7002 and Anabaena sp. PCC 7120 by triparental conjugative transfer. The transformation was confirmed by PCR amplification. The pRL-hEGF is thought to be retained as a plasmid form in the transgenic Anabaena sp. PCC 7120, since it can be recovered. However, it has been integrated into the chromosome of Synechococcus sp. PCC 7002 as there is no duplication origin in the pRL-hEGF in this cyanobacterium. and plasmid cannot be isolated from the Synechococcus sp. PCC 7002 either. The radioimmunoassay (RIA) proved that the hEGF gene has been expressed as the protein existed in these two strains of transgenic cyanobacteria, and the hEGF protein in Anabaena sp. PCC 7002 could be secreted into the medium.

Radiolarian distribution in surface sediments of the northern and central South China Sea

Radiolarian distribution in surface sediments of 104 stations from northern and central South China Sea show that the abundance and diversity of radiolarians increase with the water depth and are related to radiolarian concentrations from the water column, diminished terrigenous input, variability in calcareous shell content and the rate of silica and carbonate dissolution in the deep sea. According to the appearances of individual species in surface sediments at particular depths, seven faunal boundaries distribution are recognized at water depths of 100, 450, 650, 1000, 1200, 1400 and 2500 m. Four radiolarian assemblages in the sediments were identified by applying clustering procedures. Geographic distributions of these four assemblages coincide with present-day hydrologic features of the surface waters in this area.

Experimental study on the fractionation of yttrium from holmium during the coprecipitation with calcium carbonates in seawater solutions

The partitioning of Y and Ho between CaCO3 (calcite and aragonite respectively) and seawater was experimentally investigated at 25 degrees C and I atm. Both Y and Ho were observed to be strongly partitioned into the overgrowths of calcite or aragonite. Their partition coefficients, D-Y and D-Ho, were determined to be similar to 520-1400 and similar to 700-1900 in calcite, similar to 1200-2400 and similar to 2400-4300 in aragonite, respectively. Y fractionates from Ho during the coprecipitation with either calcite or aragonite. Within our experimental conditions, the fractionation factor, k = D-Y/D-Ho, was determined to be similar to 0.62-0.77 in calcite and similar to 0.50-0.57 in aragonite, respectively. The aqueous complexation of Y and Ho, which is a function of solution chemistry, probably plays an important role in both the partitioning and the fractionation. Further analyses suggest that the difference in covalency between Y and Ho associated with changes in their coordination environments is the determinant factor to the Y-Ho fractionation in the H2CO3-CaCO3 System.

7500aBP以来冲绳海槽北部海洋古环境的演化特征

本文采用冲绳海槽北部柱状岩芯DOC024，通过对其微体古生物分析和地球化学分析，结合浮游有孔虫氧、碳同位素数据、AMS14C 测年结果和已有的研究资料，对7500年以来该区域古生产力演化、古上升流演化及黑潮对该区域的影响进行了分析探讨。 冲绳海槽北部，九州西南海区，全新世晚期7.5ka BP以来，该区的钙质和硅质生物生产力存在着显著的差异，钙质生物的生产量高值出现在7.0ka BP 左右，但在7.0-6.4ka BP 之后明显下降而且十分稳定；而3.0ka BP 左右是硅质生物生产量的高值期，3.0ka BP 之前硅质生物生产力逐渐增加，之后呈下降趋势；表层海水初级生产力亦在7.0ka BP 左右出现短暂的高值，之后呈下降趋势，波动较频繁，0.9kaBP前后也出现了较明显的高值。古生产力的这一变化过程可能主要反映了黑潮与陆架水混合过程，以及与其相关的上升流强度的变动。 冲绳海槽北部、九州西南海区，全新世7.5-7.0ka BP陆源物质影响明显， 7.0kaBP前后黑潮侵入并与陆架水强烈混合，7.0-6.0ka BP 期间黑潮影响逐渐控制了该区，上升流开始发生，温跃层开始变浅；约在6.0-2.0ka BP 之间上升流持续稳定发育，温跃层深度逐渐下降：6.0-5.0ka BP上升流影响作用于温跃层但对表层影响较小，5.0-4.0ka BP海水表层温度受上升流冷水影响降低；而约2.0-1.2ka BP，上升流减弱，海水表层温度回升；近1200 年来上升流加强、温跃层深度减小的趋势更加显著。上升流的发育明显地控制着温跃层深度的变化，上升流强度与黑潮强度密切相关，且在一定范围内有线性关系，冲绳海槽北部冷涡区域附近海洋环境的变化也存在着明显的区域性特征。 由于受冲绳海槽北部复杂的海洋环境、DOC024 柱状样中7.5ka BP 左右火山活动的扰动作用，使我们难以准确而详细地探讨全新世黑潮在冲绳海槽北部的变动；但根据对数据的分析讨论，并结合已有研究成果可以得出以下认识：在冲绳海槽北部，7.5aBP前后黑潮强度减弱，以至于几乎完全失去了对该海区的影响；7.0-2.0kaBP上升流的稳定发育说明了黑潮较稳定，仅有小幅波动；2.0-1.2kaBP上升流减弱，黑潮减弱；1.2kaBP伴随着气候的变暖，黑潮增强且幅度较大；0.3kaBP 随着气候变冷，黑潮有所减弱；总体上自7.0aBP前后黑潮入侵以来黑潮对该区的影响一直存在，而6.6kaBP以来黑潮底层水团对该区的影响比较稳定。

海滨锦葵种子油脂提取及制备生物柴油研究

生物柴油是绿色清洁可再生能源，大力发展生物柴油对解决影响我国经济可持续发展的能源危机和环境危机具有重要意义。 本文就海洋滩涂能源油料植物海滨锦葵油脂的提取和制备生物柴油技术进行了研究。 1、利用超临界CO2流体萃取技术提取海滨锦葵籽油。结果表明超临界CO2流体萃取技术提取海滨锦葵籽油的最佳工艺参数为：萃取压力25MPa，萃取温度45℃，CO2流量18kg.h-1，萃取时间为120min，在该工艺条件下萃取三次，海滨锦葵籽油萃取率达到19.35%。 2、以海滨锦葵籽仁为原料，利用水酶法提取海滨锦葵籽仁油。水酶法提取海滨锦葵籽油的最佳工艺参数为：酶用量0.024ml.g-1，提取温度63℃，固液比1/6，提取时间为230min，在该工艺条件下海滨锦葵籽油提取率达到24.28%。 3、海滨锦葵油制备生物柴油的最佳工艺参数为：搅拌强度为1800r.min-1，催化剂KOH用量为海滨锦葵油质量的1%，醇油摩尔比6/1，反应时间50min，反应温度65℃，在该工艺条件下，酯交换反应三次，酯交换率达到97.8%。 4、利用固定化脂肪酶Novo435催化海滨锦葵油酯交换制备生物柴油。结果表明海滨锦葵油固定化脂肪酶催化法制备制备生物柴油的最优工艺参数为反应温度47℃，反应时间31h，催化剂用量18%，搅拌强度900r.min-1，醇油摩尔比3.2/1。在该工艺条件下酯交换率达到92.68%。 5、利用超临界法制备生物柴油，结果表明海滨锦葵油超临界法制备生物柴油的最佳工艺条件为：反应温度为300℃，反应压力为12MPa，反应时间为9min，搅拌强度为300r.min-1，醇油摩尔比为30/1。在此条件下，酯交换反应三次，酯交换率可达97.62%。 6、利用超声波辅助法制备生物柴油。结果表明海滨锦葵油超声波辅助法制备生物柴油的最佳工艺参数为：超声波功率为180W，催化剂KOH用量为海滨锦葵油质量的0.6%，反应温度65℃，醇油摩尔比7/1，在该工艺条件下酯交换反应三次，酯交换率达到99.85%。

大气季节内振荡对东亚夏季风活动的影响研究

利用ERA40逐日再分析资料、NCEP/NCAR2逐日再分析资料、中国740个测站日降水资料、上海台风研究所提供的西太平洋热带气旋资料、Kaplan等重建的月平均SSTA资料、NOAA逐日长波辐射（OLR）等资料，应用离散功率谱分析、带通滤波、EOF分析等统计方法，研究了东亚夏季风(EASM）的移动特征、东亚地区季节内振荡(ISO)的基本特征、季节内振荡对东亚夏季风活动的影响、季节内振荡对东亚夏季风异常活动的影响机理。主要结论如下： （1）综合动力和热力因素定义了可动态描述东亚夏季风移动和强度的指数，并利用该指数研究了东亚夏季风的爆发和移动的季节内变化及其年际和年代际变化特征。研究发现，气候平均东亚夏季风前沿分别在28候、33候、36候、38候、40候、44候出现了明显的跳跃。东亚夏季风活动具有显著的年际变率，主要由于季风前沿在某些区域异常停滞和突然跨越北跳或南撤引起，造成中国东部旱涝灾害频繁发生。东亚夏季风的活动具有明显的年代际变化，在1965年、1980年、1994年发生了突变，造成中国东部降水由“南旱北涝”向“南涝北旱”的转变。 （2）东亚季风区季节内变化具有10~25d和30~60d两个波段的季节内振荡周期，以30-60d为主。存在三个主要低频模态，第一模态主要表征了EASM在长江中下游和华北地区活动期间的低频形势；第二模态印度洋-菲律宾由低频气旋式环流控制，主要表现了ISO在EASM爆发期间的低频形势；第三模态主要出现在EASM在华南和淮河活动期间的低频形势。第一模态和第三模态是代表东亚夏季风活动异常的主要低频形势。 （3）热带和副热带地区ISO总是沿垂直切变风的垂直方向传播。因此，在南海-菲律宾东北风垂直切变和副热带西太平洋北风垂直切变下，大气热源激发菲律宾附近交替出现的低频气旋和低频反气旋不断向西北传播，副热带西太平洋ISO以向西传播为主。中高纬度地区，乌拉尔山附近ISO以向东、向南移动或局地振荡为主；北太平洋中部ISO在某些情况下向南、向西传播。 （4）季风爆发期，伴随着热带东印度洋到菲律宾一系列低频气旋和低频反气旋， 冷空气向南输送，10~25天和30~60天季节内振荡低频气旋同时传入南海加快了南海夏季风的爆发。在气候态下，ISO活动表现的欧亚- 太平洋（EAP）以及太平洋-北美（PNA）低频波列分布特征(本文提出的EAP和PNA低频波列与传统意义上的二维定点相关得到的波列不同)。这种低频分布形式使得欧亚和太平洋中高纬度的槽、脊及太平洋副热带高压稳定、加强，东亚地区的低频波列则成为热带和中高纬度ISO相互作用影响东亚夏季风活动的纽带。不同的阶段表现不同的低频模态，30~60d低频模态的转变加快了EASM推进过程中跳跃性；30-60d低频模态的维持使得EASM前沿相对停滞。 （5）30-60d滤波场，菲律宾海域交替出现的低频气旋和低频反气旋不断向西北传播到南海-西太平洋一带。当南海-西太平洋地区低频气旋活跃时，季风槽加强、东伸，季风槽内热带气旋（TC）频数增加；当南海-西太平洋低频反气旋活跃时，季风槽减弱、西退，TC处于间歇期，生成位置不集中。 （6）在El Nino态下，大气季节内振荡偏弱，北传特征不明显，但ISO由中高纬度北太平洋中部向南和副热带西太平洋向西的传播特征显著，东亚地区ISO活动以第三模态为主，EASM集中停滞在华南和淮河流域，常伴随着持续性区域暴雨的出现，易造成华南和江淮流域洪涝灾害，长江和华北持续干旱。在La Nina态下，大气季节内振荡活跃，且具有明显的向北传播特征，PNA低频波列显著，东亚地区ISO活动以第一模态单峰为主；EASM主要停滞在长江中下游和华北地区，这些地区出现异常持续强降水，华南和淮河流域多干旱；在El Nino态向La Nina态转换期，ISO活动以第一模态双峰为主，长江中下游常常出现二度梅。

青海省三江源区人工草地生态系统CO_2通量

了解三江源人工草地净生态系统CO_2交换(Net ecosystem CO_2 exchange, NEE)的季节变化规律和主要生物因子及环境因子对这些过程的影响将有助于认识青藏高原人工草地生态系统碳循环、生态价值、功能,以及对三江源区的生态安全的重要意义.该研究利用涡度相关技术,于2005年9月1日至2006年8月31日对位于青海腹地的垂穗披碱草(Elymus nutans)人工草地的NEE及生物和环境因子进行观测,阐明NEE及其组分的动态变化特征和影响因子.三江源区人工草地生态系统的日最大吸收量为2.38gC•m~(-2)•d~(-1),出现在7月30日.日间最大吸收率和最大排放率都出现在8月,分别为-6.82和2.95/μmol CO_2•m~(-2)•s~(-1).在生长季,白天的NEE主要受光合有效辐射(Photosynthetically active radiation, PAR)变化控制, 同时又与叶面积指数和群落多样性交互作用,共同调节光合速率和光合效率的强度.最大光合同化速率为2.46～10.39μmol CO_2•m~(-2)•s~(-1),表观初始光能利用率为0.013～0.070μmol CO_2•μmol~(-1)PAR.在碳交换日过程中,NEE并不完全随着PAR的增加而增大,当PAR超过某一值(>1200μmol•m~(-2)•s~(-1))时,NEE随PAR的增加而降低.受温度的影响,生长季的生态系统的呼吸商Q10(1.8)小于非生长季节的(2.6).生态系统呼吸主要受温度的控制,同时也受到叶面积指数的显著影响.生长季昼夜温差大并不利于生态系统的碳获取.三江源区人工草地生态系统是一个较强的碳汇,为-49.35gC•m~(-2)•a~(-1).

青藏高原药用植物唐古特山莨菪和唐古特大黄光合作用对强光的响应

与唐古特大黄相比，唐古特山莨菪的表观光合量子效率（AQY）较高，但最大净光合速率（Pmax）较低．在光强小于1200μmol•m^-2•s^-1时，后者用于碳同化的电子传递占总光合电子传递的比例（JC/JP）比前者高，而分配于光呼吸的电子传递（JO/JP）及Rubisco氧化和羧化速率的比值（VO/VC）则相反；光强大于1200μmol•m^-2•s^-1以后两种植物的这些参数都趋向稳定．随光强增加，后者叶片吸收光能分配于热耗散（D）的增加斜率较前者高，表明两高山植物对强辐射的适应方式略有不同。加强光呼吸途径的耗能代谢和PSII天线热耗散份额是唐古特山莨菪适应高原强辐射的主要方式，而提高叶片光合能力则是唐古特大黄的一种适应方式。

青藏高原矮嵩草草甸和金露梅灌丛草甸CO2通量变化与环境因子的关系

利用涡度相关技术观测了青藏高原两个典型的生态系统即矮嵩草（Kobresia humilis）草甸和金露梅（Potentilla fruticosa）灌丛草甸的CO2通量，并就2003年8月份的数据，分析了生态系统通量变化与环境因子的关系。8月份是这两个生态系统的叶面积指数达到最高也是相对稳定的时期，在此期间矮嵩草草甸和金露梅灌丛草甸净碳吸收量分别达56．2和32．6g C•m^-2，日CO2吸收量最大值分别为12．7μmol•m^-2•s^-1和9．3μmol•m^-2•s^-1，排放量最大值分别为5．1μmol•m^-2•s^-1和5．7μmol•m^-2•s^-1。在相同光合有效光量子通量密度（PPFD）条件下，矮嵩草草甸CO2吸收速度大于金露梅灌丛草甸；在PPFD高于1200μmol•m^-2•s^-1。的条件下，随气温增加，两生态系统的CO2吸收速度都下降，但矮嵩草草甸的下降速度（-0．086）比金露梅灌丛草甸（-0．016）快。土壤水分影响土壤呼吸，并且影响差异因植被类型不同而不同。生态系统日CO2吸收量随昼夜温差增加而增大；较大的昼夜温差导致较高的净CO2交换量；植物反射率与CO2通量之间存在负相关关系。

A New Triterpenoid from Amoora dasyclada

Five compounds were isolated from the EtOH extraction of the stem of Amoora dasyclada (How et T. Chen) C. Y. Wu (Meliaceae). On the basis of spectroscopic methods, their structures were elucidated as 24, 25-epoxy-tirucall-7-ene-3, 23-dione (1), 24, 25, 26, 27-tetranortirucall-7-ene-3-oxo-23(21)-lactone (2), taraxerone (3), taraxerol (4) and b-sitosterol (5). Among them, compound 1 was a new triterpenoid, compounds 3-5 were firstly obtained from this plant; compound 2, an tetranortriterpenoid, was firstly isolated from natural sources, and its NMR data were assigned for the first time. Moreover, the D7-bond and the Me-14 in compound 2 were never changed, which has never been found in other tetranortriterpenoids. And the biosynthetic pathway of tetranortriterpenoid was further discussed.

Oxalate decarboxylase from Agrobacterium tumefaciens C58 is translocated by a twin arginine translocation system

Oxalate decarboxylases (OXDCs) (E.C. 4.1.1.2) are enzymes catalyzing the conversion of oxalate to formate and CO2. The OXDCs found in fungi and bacteria belong to a functionally diverse protein superfamily known as the cupins. Fungi-originated OXDCs are secretory enzymes. However, most bacterial OXDCs are localized in the cytosol, and may be involved in energy metabolism. In Agrobacterium tumefaciens C58, a locus for a putative oxalate decarboxylase is present. In the study reported here, an enzyme was overexpressed in Escherichia coli and showed oxalate decarboxylase activity. Computational analysis revealed the A. tumefaciens C58 OXDC contains a signal peptide mediating translocation of the enzyme into the periplasm that was supported by expression of signal-peptideless and full-length versions of the enzyme in A. tumefaciens C58. Further site-directed mutagenesis experiment demonstrated that the A. tumefaciens C58 OXDC is most likely translocated by a twin-arginine translocation (TAT) system.