Effects of starvation on larval growth, survival and metamorphosis of Ivory shell Babylonia formosae habei Altena et al., 1981 (Neogastropoda : Buccinidae)

The impact of starvation on larvae of Ivory shell Babylonia formosae habei was studied in a laboratory experiment. Newly hatched veligers showed considerable tolerance to starvation due to their endogenous yolk material, and time to the point-of-no-return (PNR; the threshold point during starvation after which larvae can longer metamorphose even if food is provided) was calculated to be 104.5 h. However, starvation still affected larval growth, survival, and metamorphosis. Mean shell length of larvae increased 49.77 mum day(-1) for nonstarved, but only 11.13 mum day (-1) for larvae starved for 108 h. After larvae began feeding, their growth rates rapidly recovered to the level of the nonstarved following short periods of starvation (less than 48 h), but were inhibited and unable to ever reach the level of the nonstarved when being starved beyond 48 h. Percent metamorphosis was 53.75% for the nonstarved, but all larvae died before 10 days for those starved for 108 h. Starvation not only affected larval time to reach metamorphosis, but also caused the delay in the time to metamorphosis. For the nonstarved, larvae took only 11.5 days to reach spontaneous metamorphosis, but they took 20 days to reach spontaneous metamorphosis when starved for 96 h, and this duration of delayed metamorphosis reached 8.5 days. Furthermore, the importance of yolk material for maintaining larval survival of B. formosae habei during starvation periods is also discussed. (C) 2004 Elsevier B.V. All rights reserved.

高温和光照对光系统I结构与功能的影响

光合膜上包含有捕光并将光能转化为化学能所必需的四类跨膜蛋白复合体，即PSII、PSI、Cytb6f和ATP合成酶，其中PSI利用吸收的光能诱导电子从膜内侧的PC传递至相对一侧的铁氧还蛋白，被还原的铁氧还蛋白在FNR（Fd-NADP+氧化还原酶）的作用下生成NADPH，因此关于PSI的研究是光合作用研究领域中的重大问题。为了进一步阐明PSI的结构和功能，本论文分别研究了热对PSI的影响和光诱导的PSI核心复合物（CPI）的积累过程： 1.以菠菜PSI颗粒为材料研究了热处理对PSI复合物的降解和失活作用; 2.以衣藻叶绿素暗合成突变体y-1为材料研究了类囊体膜形成过程（即光诱导的转绿过程）中PSI中CPI的变化。另外，由于膜脂在光合作用中具有重要的功能，本论文还研究了y-1突变体转绿过程中光合膜脂、脂肪酸的变化。 一．应用光谱学、氧电极和变性电泳等技术研究了高温(25oC~80oC)对PSI结构和功能的影响，主要结果如下： 1． 在热处理过程中，683nm组分（主要归属于LHCI）的吸收峰强度有显著的下降并发生峰位蓝移现象，显示该组分对热处理最敏感，首先遭到破坏。 2． 77K荧光显示随着处理温度的升高，728 nm处的峰强和峰位均发生了明显的变化，F728-F720和F680的比率下降，说明热处理抑制了LHCI 680向LHCI 730以及反应中心的能量传递。 3． SDS-PAGE显示PSI核心蛋白PsaA/B亚基以及LHCI亚基在热处理情况下发生了不同程度的降解和聚合。为了能够显著地观察到热处理对PSI多肽降解的影响，实验采用了更高的温度处理方法，结果显示，90oC、100oC时PsaA/B亚基完全降解，而LHCI亚基仍有少量存在，说明PSI核心蛋白PsaA/B比LHCI亚基具有更高的热敏感性。 4． 推测热处理情况下可能发生的机制是，捕光天线首先从PSI反应中心分离，随后发生了反应中心光化学反应的抑制，直至最后多肽的严重降解。 5． 利用红外光谱技术（FT-IR）对PSI蛋白二级结构的研究显示，PSI颗粒在60oC以上时发生了明显的蛋白构象变化,且随着温度的升高蛋白构象的变化越来越大，表明PSI蛋白具有较高的热稳定性和热变性温度，PSI蛋白酰胺I带(1700~1600 cm-1)二级结构的解析表明热处理过程中二级结构的主要变化是α-helical的下降和β-sheet的增加。 6． 利用CD光谱技术研究了热处理对PSI色素微环境的影响，结果表明热处理破坏了PSI色素蛋白复合物中色素的蛋白微环境，归属于LHCI的Chlb（645 nm处组分）在较低的温度处理条件下(25~60oC)蛋白微环境即发生破坏;随着处理温度的升高（70和80 oC），478 nm处（主要归属于LHCI的Chlb）和498 nm（归属于类胡萝卜素）处的CD信号强度快速下降，说明在高温条件下LHCI比核心复合物更敏感。 7． 研究发现，PSI的摄氧活性随着处理温度的升高而显著下降，70oC时几乎完全失去摄氧能力，表明70oC时PSI复合物受到了严重的破坏，这可能是由于热处理过程中色素的蛋白微环境以及蛋白结构尤其是PSI核心蛋白PsaA/B中跨膜α-helix的构象发生了严重的变化。 二．主要运用温和电泳和蛋白印迹技术检测了暗培养4天(脱绿)的y-1突变体在光照诱发的转绿过程中PSI的核心色素蛋白复合物（CPI）及其叶绿素脱辅基蛋白PsaA/B的变化。 1． 暗培养4天的衣藻脱绿细胞中，PSI的主要色素蛋白复合物-CPI完全缺失，然而核心多肽PsaA/B仍有一定量的积累，同时检测不到P700的含量。 2． 当脱绿的y-1细胞转移至光照下时，伴随着叶绿素的合成，色素蛋白复合物CPI和PsaA/B脱辅基蛋白的合成也逐渐达到正常水平，说明叶绿素和PsaA/B蛋白进行组装并形成了具有功能的PSI反应中心,P700含量也得到了恢复。 3． 实验证明了光照是形成光合系统色素蛋白复合物的重要前提。同时发现，叶绿体基因编码的PSI核心多肽PsaA/B能够在暗条件下合成。而根据资料(Berends et al.,1987)报道，在豌豆、大麦的黄化体中不能合成PsaA/B蛋白，这可能是由于在脱绿的y-1细胞中叶绿体仍然具有相对完整的大小和形状，而在叶绿体的被膜上定位着多种与光合作用相关的酶系统。 三. 利用薄层层析及气相色谱分析技术对转绿期间y-1突变体光合膜脂和脂肪酸组成的含量变化进行了分析。结果表明： 1． 光照能够促进各种脂的积累并影响脂的组成，同时有利于脂肪酸脱饱和酶的激活。MGDG中脂肪酸不饱和程度明显升高，表现为16:0及18:1的下降，以及16:4，18：2和18:3（9，12，15）等的升高，说明光照促进了MGDG sn-2位的16:0脱饱和为16:4以及sn-1位的18：1脱饱和为18:3，也说明MGDG是脂肪酸脱饱和的重要底物。 2． 已有的资料（Ohnishi和Yamada，1980;1983）指出PG及其sn-2位的16:1（3t）的合成是光依赖的，而本实验中，在衣藻的黄化细胞中含有相当量的PG及其特有的16:1（3t）（22.80%），且转绿过程中变化并不十分显著。这可能是由于黄化的y-1细胞中叶绿体的形状并没有发生很大变化，说明叶绿体被膜上的相应酶系统才是PG合成的必需因素。 3． 相比于脱绿的y-1细胞，光照12小时后，各种脂中18：2的百分含量有显著的增加，这来源于18：2是脂肪酸脱饱和的重要中间产物。

Carbonate cycle and its control factors in Kuroshio source region during the last 190ka BP

Two deep sea cores (Ph05-5, 16.05 degrees N, 124.34 degrees E, water depth 3382m and WP3: 22.15 degrees N, 122.95 degrees E, water depth 2700m) retrieved from the Kuroshio source region of the western Philippine Sea were selected to carry out the CaCO3 and calcareous nannofossil faunas study. Based on AMS(14)C data and comparing tire oxygen isotope curve with SPECMAP delta O-18 (Martinson et al., 1987) a stratigraphy was established. And, combining the changes of primary productivity and dissolution index of carbonate, the carbonate cycle and its control factors were analyzed in this region during the last 190ka BP. The carbonate contents showed higher values in the glacial periods and lower values during the interglacial and Holocene periods, which characteristics was similar to the tendency of "Pacific Type" carbonate cycle. However, there were high carbonate contents in the warm period and low values during the cold interval, which displayed the same tendency with the "Atlantic Type" carbonate cycle during the last glacial period (MIS4-2) in the east of Phillipines. The variations of primary productivity and carbonate dissolution index indicated that the carbonate dissolution was a major factor controlling the carbonate content in tire cast of Philippines, and the variations in carbonate contents were mainly affected by the productivity of calcareous organism in the Southeast of Taiwan. The "Atlantic Type" carbonate cycle in the cast of Phillipines during the last glacial period (MIS4-2) was an effect of the process of dissolution combined with the change of primary productivity.

花岗岩-LiF-NaF-H_2O体系液相不混溶的实验研究

Liquid segregation phenomena have been found and explained in the F(Li)-rich granites in south China by Wang Linakui et al. (1979; 1983). A number of experimental investigations into the liquid immiscibilities in the granites systems have been carried out (Anfilogov et al., 1983; Glyuk et al., 1971; Glyuk et al., 1973a; 1973b; kovalenko, 1978; Wang Liangkui et al., 1987). Nevertheless, the detailed scenarios of the liquid immiscibilities in the granitic magmas are much less understood. This experimental study is amide to get access to this problem. Starting materials are biotite granite +LiF(3-10%)+NaF(3-10%)+H_2O(30%). The experimental results have shown that the liquid immiscibilities of melts of different compositions occur at 1 kbar and 840 ℃ when 5wt% (LiF + NaF) are added to the granite samples. three kinds of glasses indicating of three types of coexisting immiscible melts have been observed: light blue matrix glass, melanocratic glass balls and leucocratic glass balls. It is interesting that we have observed various kinds of textures as follows: spherulitic texture, droplets, flow bands, swirls. All these textures can be comparable to those in the natural granitic bodies. Electron microprobe data suggest that these different kinds of glasses are of different chemical compositions respectively; matrix glasses are F-poor silicate melts; melanocratic balls correspond to F-rich silicate melts; and leucocratic balls are the melts consisting mainly of fluorides. Raman spectrometric data have indicated that different glasses have different melt structures. TFM Diagrams at 1000 * 10~5 Pa have been plotted, in which two miscible gaps are found. One of the two gaps corresponds to the immiscibility between F - poor silicate melt and F-rich silicate melt, another to that between the silicate melt and fluoride melt. The experiments at different pressures have suggested that the decreases in pressures are favorable to the liquid immiscibility. Several reversal experiments have indicated that the equilibria in different runs have been achieved. We have applied the experimental results to explain the field evidence of immiscibilities in some of granites associated with W-Sn-Nb-Ta mineralization. These field phenomena include flow structure, globular structures,mineralized globular patche and glass inclusions in topaz. We believe that the liquid immiscibility (liquid segregation) is a possible way of generation of F(Li)-rich granites. During the evolution of the granitic magmas, the contents of Li, F, H_2O and ore-forming elements in the magmas become higher and higher. The granites formed in the extensional tectonic settings commonly bear higher abundences of the above-mentioned elements. the pressures of the granitic magmas are relatively lower during the processes of their emplacements and cooling. The late-staged magmas will produce liquid immiscibilities, leading to the production of several coexisting immiscible melts with different chemical compositions. The flow of immiscible consisting magmas will produce F(Li)-rich granites. It is also considered that liquid immiscibilities are of great significance in the production of rare metal granites. The ore-forming processes and magmatic crystallization and metasomatic processes can be occur at the same time. The mineralisations of rare metals are related to both magmatic and hydrothermal processes.