陆生蜗牛壳体同位素组成及其对生长季节的响应

Stable isotope compositions of land snail shells have a great potential as an indicator of paleoclimatic and paleoenvironmental changes. However, some key issues, such as the relationship of carbon isotope between snail food and local vegetation, and the uncertainty of the dominant factors about snail body fluid changes in oxygen isotope composition, remain less well known, strongly limiting shell isotopic application. In this study, we measure the stable isotope compositions on the shells of both live snails and fossils collected from the Chinese Loess Plateau and a loess sequence at Mangshan, Xingyang, respectively. Based on the analyses, the association of the stable isotope compositions of land snail shells with their growing seasons is investigated. In addition, the climatic and environmental significances of isotopic differences among several snail species are discussed. The main results and conclusions are presented as follows: 1. δ18O values for the shell lip samples of Bradybaena ravida redfieldi range from -6.79‰ to -1.92‰, and parallels to the monthly changes of local rain water δ18O, temperature and humidity. The compatibility of shell lip δ18O with monthly modeled shell δ18O indicates that the shell lip δ18O changes are mainly resulted from the 18O variations of rain-water. The shells of a land snail growing in spring could be enriched in 18O, and those growing in summer depleted in 18O. 2. Carbon isotope compositions of snail shells are controlled by their diet, which is affected by the relative proportion of C3 to C4. There are some differences in carbon isotopic compositions among different snail species, especially between P. orphana and V. tenera or P. aeoli. Shell δ13C for P. orphana is the most positive with an average of -5.88 ± 2.54 ‰. The C4 plant fraction of the food for “cold-aridiphilous” taxa, P. aeoli and V. tenera, is distinctly lower than that for “thermo-humidiphilous” taxa, P. orphana, indicating that summer is likely to be the main active season of P. orphana and spring of P. aeoli and V. tenera. Therefore, some discrepancy of carbon isotopic compositions among different species may be related to snail active season. 3. δ13C values among different species have a certain degree of positive correlation, which may be influenced by local vegetation ecosystem. δ13C value of the snail shells (especially P. orphana) shows an eastward increasing trend and consists with the variations of C4 plants biomass in Loess Plateau. The result shows that the carbon isotope in local vegetation ecosystem is one of the main factors influencing δ13C values of snail food. Therefore, both carbon isotopes of local vegetation ecosystem and snail active season contribute to the carbon isotopic differences among different snail species and in different areas. 4. δ13C values of living snail shells and soil organic matter have a positive correlation with each other, which further supports the view that carbon isotope in local vegetation ecosystem is one of the main factors influencing δ13C values of snail food. However, the range of δ13C values of snail food for various species in response to carbon isotope in local vegetation ecosystem is different. It is suggested that 13C enrichment of snail shells relative to local vegetation ecosystem has a potential to indicate snail active season and the degree of climate temperature and humidity. 5. There is a significant negative correlation between carbon and oxygen isotopic compositions of living snail shells in Loess Plateau. This result further supports that snail active season can be inferred based on the shell carbon and oxygen isotopic compositions. Moreover, there are some positive correlations between mean annual temperature and differences of shell δ13C values ( 13CV. tenera-P. orphana) and that of δ18O values ( 18OV. tenera-P. orphana) for P. orphana, a typical “thermo-humidiphilous” taxa, and V. tenera, a typical “cold-aridiphilous” taxa, respectively. It shows that  13CV. tenera-P. orphana and  18OV. tenera-P. orphana may have a potential to indicate mean annual temperature or the length of biological growing season. 6. Stable isotopes of land snail shell in the Mangshan loess sequence show that the shell δ18O value of “cold-aridiphilous” taxa V. tenera is more positive than “thermo-humidiphilous” taxa P. orphana and δ13C value of the former is more negative than the latter. In addition, the shell δ18O value of V. tenera varies significantly in different period. During the last glacial maximum, its δ18O value with an average of -7.89 ‰ is more negative than that (-5.88 ‰) from the last deglaciation to the early Holocene. This phenomenon indicates that its growing season during different period is significantly different. It tends to grow in summer in last glacial maximum. With climate warming, it prefers growing in spring with relatively low temperature. While the shell δ18O value of P. orphana varies in a little range, which shows that its activity season is shorter and mainly in summer. These results further support that the change of the snail growing season is one of the main factors of differences of carbon isotopic compositions among different snail species and varies with time. Furthermore, it is consistent that changes in magnetic susceptibility and trend of differences of shell δ18O values and δ13C values respectively between the two snail fossils. It is further testified that 13CV. tenera-P. orphana and  18OV. tenera-P. orphana may have a potential to indicate mean annual temperature or the length of biological growing season.

湛江湖光岩玛珥湖55ka以来植硅体化石记录及古环境变迁

The study of biogenic proxy of tropical and subtropical regions provides important evidence about the process and history of vegetation and environmental changes, and is of globally importance for understanding the dynamic mechanism of paleoclimatic and paleoenvironmental changes. The sediments from the Huguangyan Maar lake in Guangdong Province offer a continuous high-resolution record of the past 55 ka about environmental and vegetational changes. The studies of chronology, and physical, chemical environmental proxies have provided much important information about the paleoenvironmental and paleoclimatic histories. The phytolith, a new biogenicl proxy, has been used to determine the nature and types of plants in this area since the last 55 ka. This study presents a preliminary result about the characteristics of phytolith shapes, the variations of the fossils assemblages, and their significance for environmental changes. Moreover, the author probes the process of special specie evolution and their relationship to climatic parameters. The history of fire has been reconstructed based on the variations in charcoals. The main results and conclusions include: 28 types of phytoliths from 233 samples have been identified. Their environmental meanings are investigated in detail. Based on the variations in phytolith associations, the history and process of climatic and environmental changes in the last 55 kaBP have been established for this region. Climatic changes experienced eight intervals during this period, showing the variations of hot-humid to cool-try climate in the ten thousands years scale, and a shorter dry-hot climate condition in millennial scale. The history of palm plant has been established in this region. Two peaks appeared from 55-39 ka and since the Holocene. Plants in Bambusoideae have been growing in this area all the period, representing the impact of the East Asian summer monsoon. Bamboo plants have similar tendency in their abundance to palm plants, but with a lag of 1-2 ka BP. Panicoideae plants, the representative of C4 plants, have 6 flourishing periods occurred at 54.5, 44, 41.5, 32.5, 14, and 10 kaBP, respectively, reflecting 6 times short-term arid events. Charcoal record from the Huguang Marr lake reveals the history of nature fire, that mostly happened in dry period of last glacial from 55-10 kaBP, centered at 50-45, 40-35, 30-25, and 20-15kaBP, showing about a cycle of 10,000 years.

谷子和甘蔗C4型磷酸烯醇式丙酮酸羧化酶基因的克隆及其转基因水稻光合效率的提高

水稻是我国重要的粮食作物之一，它是一种典型的C3植物。与其它C3作物不一样的是，水稻的生长需要相对较高的温度和充足的阳光照射。然而高温和高光强的生长环境更加适合于C4植物的生长，更加有利于发挥C4植物高光合效率的特点。因此本论文希望将C4植物中固定CO2的酶磷酸烯醇式丙酮酸羧化酶基因导入水稻，获得一种更加适合高温和高光强生活环境的“C4型”水稻，这对于提高水稻的产量，满足人口增长对粮食需求具有重大意义。 本论文从C4植物谷子和甘蔗中克隆了其C4型磷酸烯醇式丙酮酸羧化酶cDNA基因，获得了具有自主知识产权的基因克隆，并将它们导入粳稻品种中花8号，进而对转基因材料的光合生理特性进行了研究。结果如下： 首次从谷子中得到了ppc基因两个cDNA克隆，分别命名为Mppc1和Mppc2。前者是一个C3型的ppc基因，它可能属于在根中特异表达的C3-2型ppc基因;后者是在绿色叶片中大量表达的C4型ppc基因。它们所编码的蛋白的氨基酸残基数分别为961和964，序列同源性为82.5%。C4型PEPC多出的3个氨基酸位于N末端。利用RACE的方法我们得到了谷子C4型ppc基因完整的cDNA序列，包括63bp的5'非编码区，2895bp的编码区和256bp的3'非编码区。 首次获得了甘蔗C4型ppc基因完整的cDNA序列的克隆，命名为Sppc。它包括95bp的5'非编码区、2886bp的编码区，和224bp的3'非编码区。 利用所克隆的基因，分别连上强组成型启动子Ubiquitin启动子和强光调控启动子Rubisco小亚基启动子后，再插入两个标记基因不同的表达载体pCB和pPCB的多克隆位点中，构建了八个含有外源ppc基因的植物表达载体pCB-Pubi-Mppc、pCB-Pubi-Sppc、pCB-PrbcS-Mppc、pCB-PrbcS-Sppc、pPCB-Pubi-Mppc、pPCB-Pubi-Sppc、pPCB-PrbcS-Mppc和pPCB-PrbcS-Sppc。再加上含有玉米完整的C4型ppc 核基因的载体pCB-ZMppc，共有9个载体。利用农杆菌介导法进行了水稻的转化，各个载体都获得了大量的转基因植株。对标记基因潮霉素磷酸转移酶基因hpt和磷酸甘露糖异构酶基因pmi以及导入的目的ppc基因的PCR扩增检测，结果显示绝大多数转基因植株都能扩增出目的片段，而未转化的植株则没有扩增产物。对部分转基因水稻的Southern和Western杂交以及RT-PCR分析都表明，无论从DNA水平、mRNA水平，还是从蛋白质水平上都证明外源ppc基因都成功地导入了水稻，并获得了正确的表达。 对各载体转基因植株PEPC活性大规模的测定表明，转入玉米完整C4型PEPC核基因（有内含子）的水稻表现出极大的表达效率，大多数转基因材料的PEPC活性为对照的10-20倍，其活性最高可达到对照的44倍。转入谷子和甘蔗PEPC基因cDNA的水稻，表达的效率很低，多数材料活性增加仅为对照的2-5倍，但也有极少数材料活性增加了10倍以上。用Rubisco小亚基启动子控制的ppc基因在水稻的表达活性要略高于Ubiquitin启动子控制的ppc基因。以上结果说明ppc基因的内含子在其转录或mRNA的稳定上起着重要作用。 对部分转基因材料气体交换特征的研究发现，随着转基因水稻PEPC活性的增加，净光合速率也有逐渐增加的趋势。其中PEPC活性最大的ZM24株系的三个单株净光合速率比对照增加了39.8%、13.7%和28.6%，而它们的PEPC活性比对照分别增加了21.2、21.9和23.6倍。 转PEPC水稻的净光合速率与气孔导度具有显著的相关性。这说明表达的外源ppc 基因产物PEPC参与了转基因水稻的气孔运动，使气孔开放程度增加。更有意义的是过表达PEPC的水稻具有更高的水分利用效率，这就增加了其耐旱能力。在光抑制条件下转基因水稻也具有更高的光合能力。这些特征表明转ppc基因的水稻比对照更加适合于水稻高温高光强和干旱的原生环境。

新型可控坍塌芯片连接技术(C4)及芯下材料力学性能研究进展

可控坍塌芯片连接 (C4)技术可以实现高速、高密度、小外形的封装 ,因此日渐得到关注和发展。然而 ,随着C4技术的普及 ,C4封装内由于芯片和基板间热膨胀系数 (CTE)的不匹配而引起的可靠性问题将日益突出 ,为此研究者在C4封装中引入芯下材料来提高C4封装的可靠性。文中侧重于制造工艺、可靠性以及最新进展对C4技术进行介绍 ,并且对C4技术中所用的芯下材料的力学性能及其对C4封装可靠性影响的研究现状进行评述