湖泊沉积中的^10Be含量变化――有助于识别第四纪古冰川的有无

IEECAS SKLLQG

改性纳米羟基磷灰石/PLGA复合材料的制备及生物活性

以低聚乳酸接枝改性的羟基磷灰石纳米粒子(op-HA)和聚丙交酯-乙交酯(PLGA)制备的生物可降解纳米复合材料(op-HA/PLGA)为研究对象,采用FTIR,TGA,ESEM和EDX分析其接枝反应、接枝率、表面形貌和钙磷沉积情况,通过在材料膜表面接种兔成骨细胞进行体外培养,采用荧光染色、NIH ImageJ图像分析和Real-time PCR综合评价细胞在材料表面的形态、黏附面积比、增殖能力和基因表达水平,以此评价新型骨修复纳米复合材料op-HA/PLGA的表面性质和生物活性.研究结果表明,op-HA的表面接枝率为8.3%,掺入至PLGA后可形成富含钙磷的粗糙表面,促进成骨细胞的黏附、扩展和增殖,提高Ⅰ型胶原蛋白(Collagen-Ⅰ)、骨形态蛋白-2(BMP-2)和骨连接蛋白(Osteonectin)的基因表达水平,提高材料的钙磷沉积能力.op-HA/PLGA具有良好的细胞相容性和...

Preparation and Bioactivity of the Composite of PLGA and Hydroxyapatite Nanocrystals Surface-grafted with L-lactic Acid Oligomer

The hydroxyapatite (HA) nanocrystals of 100-200 nm in length and 20-30 nm in width were hydrothermally synthesized by the reaction of phosphoric acid and calcium hydroxide. Lactic acid oligomer surface grafted HA(op-HA) nanoparticles were obtained by oligomeric lactic acid with a certain molecular weight grafting onto the HA surface to form a Ca carboxylate bond in the absence of any catalyst. The op-HA was further blended with poly(lactide-co-glycolide) (PLGA) to prepare the nanocomposite of op-HA/PLGA. FTIR, TGA, ESEM and EDX were used to analyze grafting reaction, the graft ratio of op-HA, surface topography and calcium deposition of the composites, respectively. The rabbit osteoblasts were seeded and cultured on the surface of composites in vitro. The cell morphology, adhesion, proliferation and gene expression were evaluated with FITC staining, NIH image J software and the analysis of real-time PCR, respectively. The results show that the graft ratio of op-HA is 8.3% (mass fraction). The op-HA/PLGA nanocomposite possessed more suitable surface properties, including roughness and plenty of calcium and phosphor. It exhibited better cell adhesion, spreading and proliferation of rabbit osteoblasts, compared to pure PLGA.

Self-assembled silver nanoparticle monolayer on glassy carbon: an approach to SERS substrate

In this paper, the fabrication of an active surf ace-enhanced Raman scattering (SERS) substrate by self-assembled silver nanoparticles on a monolayer of 4-aminophenyl-group-modified glassy carbon (GC) is reported. Silver nanoparticles are attached to the substrate through the electrostatic force between the negatively charged silver nanoparticles and the positively charged 4-aminophenyl groups on GC. The active SERS substrate has been characterized by means of tapping-mode atomic force microscopy (AFM), indicating that large quantities of silver nanoparticles are uniformly coated on the substrate. Rhodamine 6G (R6G) and p-aminothiophenol (p-ATP) are used as the probe molecules for SERS, resulting in high sensitivity to the SERS response, with the detection limit reaching as low as 10(-9) m. This approach is easily controlled and reproducible, and more importantly, can extend the range of usable substrates to carbon-based materials for SERS with high sensitivity.

Electrocatalytic reduction of oxygen at multi-walled carbon nanotubes and cobalt porphyrin modified glassy carbon electrode

The multi-walled carbon nanotubes (MWNTs) modified glassy carbon electrode exhibited electrocatalytic activity to the reduction of oxygen in 0.1 M HAc-NaAc (pH 3.8) buffer solution. Further modification with cobalt porphyrin film on the MWNTs by adsorption, the resulted modified electrode showed more efficient catalytic activity to O-2 reduction. The reduction peak potential of O-2 is shifted much more positively to 0.12 V (vs. Ag/AgCl), and the peak current is increased greatly. Cyclic voltammetry (CV), transmission electron microscopy (TEM), X-ray photoelectron spectroscopy (XPS) and atomic force microscopy (AFM), were used to characterize the material and the modified film on electrode surface. Electrochemical experiments gave the total number of electron transfer for oxygen reduction as about 3, which indicated a co-exist process of 2 electrons and 4 electrons for reduction of oxygen at this modified electrode. Meanwhile, the catalytic activities of the multilayer film (MVVNTs/CoTMPyP)(n) prepared by layer-by-layer method were investigated, and the results showed that the peak current of O-2 reduction increased and the peak potential shifted to a positive direction with the increase of layer numbers.

活性炭对蔗糖的吸附特性

活性炭吸附蔗糖是一种化学吸附过程，蔗糖是以单分子铺展的形式被吸附于活性炭表面，其吸附速率由内扩散所控制。

螺旋藻基因组结构分析和藻胆蛋白的适应性进化

螺旋藻 (Spirulina，或称节旋藻 Arthrospira) 是一类丝状不形成异型胞的蓝藻，常分布于湖泊、池塘和半咸水中。作为目前利用最广泛的经济微藻，螺旋藻的规模培养、生理生化以及分子遗传等都受到了广泛的关注。但由于缺乏足够的基因组信息，影响了螺旋藻的品种改良以及进一步的基因功能产品的开发。 本研究从挑取单藻丝开始，建立了钝顶螺旋藻 (Spirulina platensis) 的纯培养体系，并构建插入片段分别为1-2Kb和4-6Kb的基因组文库，利用鸟枪法进行全基因组测序，共得到具有8倍覆盖度的7.4Mb拼接后的基因组数据。在该草图中，预测有7795个开放读码框 (ORFs)，其中包括长度小于120个氨基酸的ORFs和非全长ORFs。在所有蛋白编码序列中，约有39%的基因是螺旋藻特有的，此外，还有389个基因相对于其他蓝藻，与非蓝藻基因有着更高的相似性。通过Pfam结构域聚类分析发现，螺旋藻含有特有的结构域，如Peptidase_MA、DMT、OB、ATP-grasp、Flavokinase 等。 由于目前尚未有成熟的螺旋藻遗传转化系统，而其体内复杂的限制性内切酶系可能是妨碍外源基因顺利导入和整合的关键因素。在此草图的基础上，我们利用比较基因组学和分子进化的手段，深入分析了螺旋藻及其他蓝藻的限制修饰系统 (Restriction-modification system)，为建立螺旋藻的遗传转化技术，并实现后续的螺旋藻基因功能验证模式奠定了基础。 螺旋藻及其他蓝藻的基因组计划提供了大量基因组序列和结构信息，有助于我们深入了解光合微生物基因的结构、功能和进化，以及环境因子或特定突变是如何塑造其基因组的。本文以藻胆蛋白为例，利用分子进化和群体遗传学理论，描绘出一幅藻胆蛋白进化的动态图景，并分析了环境 - 结构 - 功能之间的相互联系，为藻类捕光色素进化机制理论提供了科学依据。 本研究结果发现低光适应型原绿球藻和海洋聚球藻的藻红蛋白中正选择位点分布有着显著差异，提示二者的藻红蛋白基因有不同的进化模式；正选择作用位点多集中在藻胆蛋白的色基结合区域及XY发卡结构处，这些结构域主要与藻胆蛋白的光能捕获、能量传递和结构组装有关。该研究结果不仅揭示了正选择作用的重要性，而且提示光质、光强和能量传递压等可能是潜在的正选择压力。此外，又深入研究了高光和低光适应型两个生态群体的原绿球藻藻红蛋白基因系统发育、种内多态性和种间变异度，以此揭示环境因子对藻胆蛋白进化的影响。 本研究首次对螺旋藻全基因组进行测序，并以藻胆蛋白为例，从分子进化角度揭示其结构和功能的关系，并首次提出正选择压力可能是促使藻胆蛋白功能分化的主要原因，并认为原绿球藻中藻红蛋白的进化呈现出不同的模式，新的捕光色素的出现以及其所处的海洋环境可能使藻红蛋白获得了新的功能。

Safety of tetanus toxoid in pregnant women: A hospital-based case-control study of congenital anomalies

Reported are the results of the Latin American Collaborative Study of Congenital Malformations (ECLAMC), a hospital-based case-control study of 34 293 malformed and 34 477 matched nonmalformed newborn controls. No statistical differences were found between the malformed and control groups, exposed or not exposed to tetanus toroid.

黄铁矿热转变过程的岩石磁学研究

Pyrite is the most stable iron-sulfide in reduced environment, and plays an important role in geochemical iron-sulfur cycling of sediments. Thus, the presence of pyrite in sediments and rocks is an important indicator of sedimentary environments. Previous studies on the thermal products of pyrite showed that all of the products (e.g., pyrrhotite, magnetite, hematite) have strong capability of carrying remanence. To deepen our understanding of the environmental and paleomagnetic significances of pyrite, the mineral transformation processes of pyrite upon heating were systematically investigated in this study using intergrated rock magnetic experiments (in both argon and air atmospheres) and X-ray diffraction analysis. The room temperature susceptibility of the paramagnetic pyrite is about 2.68×10-5 SI. In argon atmosphere (reducing environment), pyrite was transformed into monoclinic stable single domain (SD) pyrrhotite above 440 C. The corresponding coercive force and remanence coercivity are about 20 mT and 30 mT, respectively. In contrast, in air atmosphere (oxidation environment), the intermediate thermal products of pyrite are magnetite and pyrrhotite, which were quickly further oxidated to SD hematite, which has coercivity of about 1400 mT. In addition, the hematite particles gradually grow from SD to PSD grain size region by multiple heating runs. The transformation processes of pyrite in oxidation atomosphere can be interpreted by three possible pathways: (1) pyrite→magnetite→hematite; (2) pyrite→pyrrhotite→magnetite→hematite; and (3) pyrite→pyrrhotite→hematite. Low-temperature magnetic experiments show no transitions for pyrite. Despite that low-temperature magnetic method is not suitable for identification of pyrite, it is clear in this study that the high-temperature thermomagnetic measurements (e.g.,  -T and J-T curves) are very sensitive to the presence of pyrite in sediments and rocks. Nevertheless, for the thermal treatment products, low-temperature magnetic measurements showed the 34 K transition of pyrrhotite and the 250 K Morine transition of hematite. Iron-sulfide has also been found on Martian meteorolites by other workers. Therefore, systematic study of rock magnetism of pyrite (and other iron-sulfides) and their products will have great significances for both paleomagnetism and planetary magnetism.