大气CO_2和O_3浓度升高对银杏构件生长的影响

采用开顶箱模拟试验,探讨了大气CO2和O3浓度升高对银杏构件生长的影响。结果表明:高浓度O3抑制银杏主枝和侧枝生长(P<0.01);高浓度CO2对银杏粗生长影响不显著(P>0.05),但在高浓度O3和CO2、O3复合气体条件,银杏粗生长受到严重抑制(P<0.01);高浓度CO2可促进银杏叶片面积和干物质的增加,并能提高叶片含水量和抗干旱能力,但在高浓度CO2、O3复合气体条件下,叶片面积增加不显著(P>0.05),而干物质增加极显著(P<0.01);O3对银杏叶片构件生长有明显抑制作用,叶面积大小和干物质量明显低于对照株(P<0.05)。

第94届美国生态学会年会在新墨西哥州阿尔伯克基召开

<正>美国生态学会(ESA)第94届年会于2009年8月2日到7日在新墨西哥州阿尔伯克基(Albuquerque)的国际会议中心举行,3000多人参加此次会议。会议主题是"Ecological Knowledge and a Global Sustainable Society"。8月2日下午5时,美

利用SEDD模型模拟岷江上游小流域的年产沙量

以GIS为平台,建立了泥沙输移分布模型SEDD(sediment delivery distributed model),包括模拟流域年侵蚀量的修正通用水土流失方程RUSLE(revised universal soil loss equation)和模拟泥沙输移比SDR(sediment delivery ratio)的方程.利用该模型模拟了岷江上游黑水、镇江关流域的年侵蚀、产沙量及其空间分布特征.模拟结果表明:两个流域侵蚀强度以轻度和中度侵蚀为主,并伴有强度侵蚀;流域产沙量低,不到侵蚀总量的5%;泥沙输移比与流域产沙量的空间分布相似,均呈现在河流附近较高、其他区域接近零的格局;灌木林地和林地是主要的产沙源,两种类型的产沙量之和约占流域总产沙量的70%.

Development of SSR primers from EST sequences and their application in germplasm identification of Porphyra lines (Rhodophyta)

This paper reports the development of SSR markers from EST data and their utilization in germplasm identification of Porphyra. The publicly available EST (expressed sequence tag) sequences of Porphyra were searched from the Internet (www.kazura.or.jp/en/plant/porphyra/EST/). From a total of 20,779 obtained EST sequences, 391 SSRs (simple sequence repeats) were analysed with SSRIT software (www.gramene.org/db/searches/ssrtool). From those, 48 SSR primer-pairs were designed and tested by commonly used SSR reaction conditions using 22 Porphyra DNA samples as templates. Results showed that 41 SSR primer-pairs gave good amplification patterns. These were used to conduct SSR analyses of genetic diversity and variety identification of the 22 Porphyra lines. A dendrogram and the DNA fingerprints of the Porphyra lines were developed based on the obtained SSR data.

The effects of CpG-C oligodeoxynucleotides on innate immune responses in Eriocheir sinensis (H. Milne-Edwards, 1853)

CpG oligodeoxynucleotides (ODNs) can stimulate the immune system, and therefore are widely used as a therapeutic vaccination and immune adjuvant in human. In the present study, CpG-C, a combination of A- and B-class ODN, was injected into Chinese mitten crab Eriocheir sinensis at three doses (0.1, 1 and 10 mu g crab-1), and the reactive oxygen species (ROS) levels, activities of total intracellular phenoloxidase (PO) and lysozyme-like activities, the mRNA transcripts of EsproPO, EsCrustin and EsALF were assayed to evaluate its modulating effects on the immune system of crab. The ROS levels in all treated and control groups were significantly increased from 6 to 24 h, except that ROS in 0.1 mu g CpG-C-treated crabs was comparable to that of the blank at 6 h. The PO activity was significantly enhanced and EsproPO transcripts were down-regulated (P < 0.01) at 6 h after the injection of 0.1 mu g CpG-C, with no significant changes in the other dosage treatments. The lysozyme-like activities and EsCrustin transcripts in the CpG-C-treatment groups were significantly higher than those of controls. The mRNA expression of EsALF remained almost constant in all the groups during the treatment. These results collectively suggested that CpG-C could activate the immune responses of E. sinensis, and might be used as a novel immunostimulant for disease control in crabs.

添加钛镁元素对热浸镀锌层性能的影响

热浸镀锌及其合金在世界各国已得到广泛的应用。为提高镀锌层性能，往镀浴中添加各种微量元素已经有了许多研究。但是对于在高纯锌中添加微量元素，排除由于锌浴不纯而导致的性能差异，报道很少。 本文选择高纯锌，在排除其它元素干扰的情况下，制备了添加钛、镁元素的热浸镀锌合金镀层，考察了分别添加钛、镁元素及同时添加钛镁元素后镀层在海水环境中的腐蚀行为及其耐蚀性能。 由于钛熔点（1668℃）远高于锌熔点（419.5℃），镁在高温下极易氧化，因而制备中间合金。在分别用分光光度法和原子吸收法测定准确含量后，按计算量进行添加。热浸镀层最外层和镀液合金成分基本一致，镀液合金性能可以反映镀层性能，制备锌钛、锌镁合金电极，进行电化学性能测试，发现添加钛、镁元素能够提高合金在海水中的耐腐蚀性能。 采用烘干溶剂法进行热浸镀，选择合适的工艺条件，助镀剂为ZnCl2、NH4Cl的混合溶液，温度460℃，镀液为添加不同含量钛镁的锌液。对所得镀层进行表观质量检测，镀层质量合格，其中添加钛元素后镀层亮度增加。镀层厚度是考察镀层性能的重要指标，通过测量发现镀层比较均匀，添加钛元素后镀层厚度减薄，添加镁元素后镀层厚度稍有增加，同时添加钛镁元素，镀层厚度稍高于单独添加钛元素，但比纯锌镀层要薄许多。添加微量钛镁后，镀层阻抗谱图和极化曲线图形状都没有大的改变，EIS等效电路拟合结果表明添加钛镁元素后镀层极化电阻增加，镀层在海水中耐蚀性能有所提高。 为进一步检测镀层的耐蚀性能，进行了中性盐雾试验，添加钛镁元素后镀层腐蚀失重减少，腐蚀失重率降低，耐盐雾腐蚀性能提高；室内模拟全浸实验所的结果与盐雾试验具有一致性，镀层刚开始时腐蚀较快随后比较稳定。

海北高寒草甸生态系统定位站辐射气候特征

以2000—03到2001—02的辐射观测资料，分析了海北高寒草甸生态系统定位站地区辐射及各分光辐射的变化特征．将为高寒草甸生态系统的物质循环、能量流动、草地生产力形成机制等问题的研究提供科学依据。结果表明：海北站区Eg、Er、UV、PAR、NIR和En具有明显的日、年变化，年内其总量分别达6278．867MJ／m^2、1515．139MJ／m^2、311．242MJ／m^2、2576．777MJ／m^2、3397．404MJ／m^2和2542．950MJ／m^2，其中在植物生长期的5—9月分别为3181．215MJ／m^2、698．021MJ／m^2、165．955MJ／m^2、1133．965MJ／m^2、1673．871MJ／m^2和1668．805MJ／m^2。年内Er、UV、PAR、NIR和Eh占Eg的比例分别为0．242、0．048、0．410、0．540和0．410，在植物生长期分别为0．219、0．052、0．413、0.528和0．527。对Eg和PAR提出了下列形式的模拟求算式．Eg=Eg0（0．089．7＋0．9768S／S0）和PAR=-3.8044＋0.4177％，模拟效果较好，可利用有关常规气象观测资料进行估算。

青藏高原红景天药材的HPLC指纹图谱

利用高效液相色谱法建立了青藏高原红景天的色谱指纹图谱.固定相采用C18反相色谱柱,流动相为甲醇:0.1%磷酸水(v/v＝15:85);检测波长220 nm;流速为1.0 mL/min.通过比较发现红景天样品的8个主要共有峰,可作为鉴别红景天药材的主要依据.方法简便快速,为中药品种的鉴定提供了较全面的信息.

塔里木盆地柯坪-巴楚露头区白云岩成岩作用机理研究

Through field outcrop dolomite observation, laboratory petrography (macroscopy, microscopy, cathodeluminescence and scan electronic microscopy), geochemistry (carbon-oxygen-strontium isotopes and trace elements) and fluid inclusion microthermometry study in Keping-Bachu area of Tarim Basin, it can be inferred that there are existing eight dolomite texture types within four evolution phases in Keping-Bachu area of Tarim Basin. The paragenesis of different dolomite texture types and associated minerals in Keping-Bachu area has been established. The carbon and oxygen isotopes of saddle dolomites and matrix dolomites overlap greatly. The Strontium isotopes results of Keping-Bachu outcrop area show that the strontium isotopes differentiation of the matrix and saddle dolomites is not obvious, the reason of which is that there is thousands of Cambrian-Ordovician dolomite strata below the stratum bearing the saddle dolomite. In the process of the heat flow upward migration, the isotopes of the heat interacts with the host rock, which leads to the similarity betwwen the strontium of the saddle dolomite and matrix dolomite. The strontium isotope of the saddle dolomite is not very radiogenic. the six types samples within four phases in the study area show Eu negatively. Comparing to the other types of samples, the δEu of saddle dolomite is relatively high falling into the range of 0.510-0.874, which shows that the saddle dolomite forms in the hydrothermal setting and is affected by the hydrothermal activity to some extend.The Lan/Ybn of saddle dolomite is high up to 15.726, which means that the HREE is very rich. It belongs to the typical hydrothermal genesis model. The δCe of saddle dolomite is positive anomaly, which is the result of high effect from the land source debris. The homogeneous temperature of the saddle dolomite falls into two ranges 110-120℃ and 125-160℃, after pressure correction, they are 141-152℃，157.5-196℃, the salinity of the saddle dolomite can reach to 20-25%. With the comparing with the burial history, the Th of the saddle dolomite is high than the ambient strata temperature, these data show that the saddle dolomite is of hydrothermal origin. The evolution trend of different dolomite and associated minerals is from matrix dolomite, dolomite cementation, saddle dolomite, quartz to calcite. Alonging with this evolution trend, the temperature of the diagenetic flow initiated from 80-100℃, after rising to 135-160℃, then gradually declined. Finally, a structurally-controlled dolomitization model is established in Keping-Bachu area of Tarim Basin.

南海沉积物中的放射虫及其古环境意义

In this paper a systematic study of radiolarian from surface sediments of all the South China Sea (SCS) has initially been done for its deposit ecology, biogeography and paleoenvironment significance. The paleoenvironment information obtained by radiolarian analysis and other sedimentary method for core samples is also made use as the synthesis proxy for revealing the paleoenvironment changes in the SCS and the relations of it with the past globe change during last 200ka. Some results come out of this study as: 1) Radiolarian skeleton chemistry composition and skeleton morphological features were analyzed, chiefly dividing them as 15 types of basic morphological features: 2) Analysis of biogeographical feature demonstrates that the fauna in SCS obviously belonging to a transitional type of west Pacific - Indian Ocean and has a particularity of itself: 3) Tendency of radiolarian population distribution is lower in shallow continental shelf area, increasing gradually toward the abyssal region; 4) Nine character boundaries of radiolarian depth distribution in the sediments from whole the South China Sea may be recognized; 5)Two radiolarian transfer functions for paleotemperature and paleo-primary productivity in the South China Sea have also been established respectively. The equation of transfer function for winter paleotemperature has only an average estimated error of 0.18678 ℃ and the equation for paleo-primary productivity has the calculation accuracy of 85.31%; 6) Changes of radiolarian individuals, numbers of species and H(S) values in core NS93-5 show the completely different oceanic geographical circumstance and ecology structure in the Last Maximum Glacial with present; 7) The abundance variation of some raiolarian warm species and cold species indicate the changes of water masse features along with the paleoenvironment evolution, showing that this sea area clearly is controlled in 6 issues of oxygen isotopes by the cold water masses; 8) By comparative analysis of δ ~(18)O curves with GISP2;s ice core can core 17940 of the northern SCS, the occurring characters of D/O's events 1-21 and Heinrich's events H1-H6 have been revealed in this sea area by core NS93-5, which prove the existence of paleoclimatic tele-connections between the southern SCS and Arctic region since about 200ka BP.