松杉类植物花粉发育和传粉生物学的研究

本文用光学显微镜结合荧光技术对青扦花粉的发育过程进行了观察;用共聚焦显微镜观察了白扦生长花粉管细胞内的游离Ca2+分布;利用原子力显微镜对雪松和水杉花粉外壁的亚结构进行了研究：用透射电镜、扫描电镜及解剖镜等技术研究了侧柏、北美香柏、红豆杉、粗榧和白皮松的传粉机制，结果如下。 青扦花粉的发育过程与松科其它一些植物花粉的发育模式相似。从小孢子母细胞到成熟花粉约二十天左右。小孢子母细胞进入减数分裂前彼此分开，但在某些部位仍有连接。细胞质内有大量淀粉粒，在减数分裂过程中减少或消失，没有观察到明显的淀粉粒带。减数分裂中的胞质分裂为同时型，四分体为四面体型。小孢子刚从四分体释放出来时，气囊已开始形成，细胞中含大量淀粉粒。随着小孢子的发育，其体积增大，并出现液泡，细胞核移向一侧。小孢子第一次不对称分裂产生一个大的中央细胞和一个小的原叶细胞。中央细胞不久就进行第二次分裂产生精子器原始细胞和第二原叶细胞。原叶细胞形成后，其与中央细胞或精子器原始细胞之间的壁逐渐沉积胼胝质，以后随着原叶细胞的退化，胼胝质壁消失。精子器原始细胞分裂形成管细胞和生殖细胞，生殖细胞在散粉前分裂形成体细胞（精原细胞）和柄细胞（不育细胞）。成熟花粉为5细胞，但两个原叶细胞已退化消失。 白扦花粉在10%蔗糖+0.01%硼酸的液体培养基内培养12小时后开始萌发。在正常生长的花粉管中，其顶端有一个透明区，而透明区后则含有大量的贮藏物质颗粒。在停止生长的花粉管中透明区消失，而整个花粉管顶端也被储藏物质颗粒充满。正常生长的花粉管顶端有一个较高的Ca2+浓度。在停止生长的花粉管内不具有这样一个Ca2+梯度。 雪松和水杉二种花粉外壁中由孢粉素构成的亚结构单位形态相似，均呈颗粒状，但大小略有不同。雪松的长56-99 nm，宽42-74;水杉的长81-118 nm，宽43-98 nm。在雪松中这些亚单位紧密排列组成短棒状或球状的花粉外壁结构单位，再由几个到十几个这样的结构单位组成较大的岛屿状结构。在这些岛屿状结构之间有大小不一的空隙存在，整个花粉外壁由这样一些岛屿状结构交互连接形成。水杉花粉外壁的亚单位排列也较紧密，且有3-10个成群分布的趋势，但各群之间界限不明显。此外，雪松和水杉的花粉外壁亚单位均无螺旋状排列趋势，这一结果倾向于支持Southworth关于花粉外壁亚单位颗粒状并呈网状排列的观点。 白皮松胚珠倒生，其发育过程与松属的其它种相似，成熟胚珠珠孔端具两手臂状结构，有利于接收花粉。花粉具气囊。传粉期间，没有观察到传粉滴产生，但珠心顶端细胞解体形成花粉室。花粉室内可接受一至几个花粉，花粉在花粉室内的位置无明方向性。传粉时，胚珠处于大孢子线细胞时期。花粉在花粉室内萌发形成花粉管进入珠心组织，花粉管在珠心内生长一段时间后停止生长，并于次年春天重新启动生长。离体生长的花粉管顶端常有胼胝质产生，但顶端区域后的花粉管壁上却无胼胝质沉积。 侧柏、北美香柏、红豆杉和粗榧均为直生胚珠。传粉时胚珠产生传粉滴。在红豆杉胚珠发育早期，珠心表面细胞轮廓清晰;而在后期，其珠心表面则形成了一层膜状结构。这层膜状结构在传粉前随珠心细胞的解体而破裂，珠心细胞的降解产物参与了传粉滴形成。在传粉前和传粉期，珠心细胞内含大量的线粒体、内质网、高尔基体和小泡。传粉滴主要由珠心细胞分泌形成。这四种植物的花粉均无气囊，属可湿性花粉。红豆杉和粗榧的花粉水合时，内壁膨胀，外壁开裂。通常情况下，红豆杉花粉的外壁保留在传粉滴的表面，而花粉的其它部分沉入传粉滴内。侧柏和北美香柏的传粉滴授粉后，花粉进入传粉滴导致传粉滴的明显收缩。在侧柏中传粉滴授粉后100分钟内就完全收缩进入珠孔。传粉滴收缩的速率与所授花粉数量和花粉的种类有关。与侧柏亲缘关系较近植物花粉引起传粉滴的收缩速率和侧柏自身花粉引起的传粉滴收缩速率相似;反之，收缩速率变慢。侧柏传粉滴的收缩可能主要是由于花粉减弱胚珠分泌的结果。但授粉不引起红豆杉和粗榧传粉滴的明显收缩。在红豆杉和粗榧中，从授粉到传粉完全收缩需要20-24小时。这两种植物传粉滴的收缩可能主要是蒸发引起的非代谢性过程，与侧柏和美香柏属于不同的传粉滴收缩机制。

Islet-1 is required for ventral neuron survival in Xenopus

Islet-1 is a LIM domain transcription factor involved in several processes of embryonic development. Xenopus Islet-1 (Xisl-1) has been shown to be crucial for proper heart development. Here we show that Xisl-1 and Xisl-2 are differentially expressed in th

Relaxation of yeast mitochondrial functions after whole-genome duplication

Mitochondria are essential for cellular energy production in most eukaryotic organisms. However, when glucose is abundant, yeast species that underwent whole-genome duplication (WGD) mostly conduct fermentation even under aerobic conditions, and most can

大豆根瘤菌种群多样性及结瘤特性研究

环境因子及土著根瘤菌是影响人工接种根瘤菌剂接种效果的两个主要因素。论文分为二部分。第一部分首先考察了外界因素对根瘤菌剂接种效果的影响。应用GUS（葡萄糖苷酶）基因标记技术将标记基因GUS导入受体菌S.fredii 8855，标记菌体形成的根瘤可被GUS染色缓冲液染成兰色，而土著菌形成的根瘤不能着色，由此即可十分简便地确定土著菌的影响程度。盆栽实验表明，S.fredii 8855的结瘤抗酸碱能力高于土著菌，能在土壤中较大范围内迁移。当它的根瘤占有率不小于43％时，接种能显著提高大豆产量。大豆产量与根瘤根瘤占有率呈正相关(r = 0.98)，而与总瘤数关系不大(r = 0.13)。土壤氮素显著抑制其结瘤，补加磷能缓解这种抑制作用。研究发现应用快生型大豆根瘤菌剂为保证接种效果，接种量至少应为土著根瘤菌数量的10~5倍，同时施用磷肥会提高接种效果。只有当接种根瘤菌的占瘤率在40％以上时接种才可能达到增产目的。第二部分较为系统地考察了新疆主要大豆产区耕作土中大豆根瘤菌种群数量、种群结构及种群共生、遗传多样性。新疆大豆地耕作土中含有数量较高的大豆根瘤菌，数量每克土大多在10~5-10~6之间，种群结构大多以快生型根瘤菌为主。对分离的28株根瘤共生及遗传多样性进行了分析，土著大豆根瘤菌菌株间结瘤能力有一定差异，快生型大豆根瘤菌总体结瘤能力高于慢生型，但差异不显著(p <= 0.05)，形成的根瘤大小也有较大差异。根瘤菌种群中菌株间为植物提供的生物固氮量存在明显差别，但仅有20％的菌株能明显促进植物生长，有1/3的菌株具有较高的固氮能力。慢生型大豆根瘤菌固氮能力明显高于快生型，但二者之间差异未达到显著水平(p < 0.05)。根瘤菌结瘤力与固氮活性之间的相关性分析发现许多根瘤菌形成的根瘤为无效根瘤。重复序列（重复基因外回文REP和肠细菌重复基因间共同序列ERIC）结合聚合酶链式反应(ERP和ERIC－PCR)用于大豆根瘤菌染色体指纹分析，分析结果表明新疆土著大豆根瘤菌具有复杂的遗传多样性，遗传相近程度具有一定的地域性，来自同一地区的根瘤菌株具有较高的遗传相似性。新疆土著大豆根瘤菌在相似水平0.5可分为两大类群，一个类群包括所有慢生型根瘤菌，另一类群为所有快生型根瘤菌。在相似水平0.6大豆根瘤菌可分为5个聚群，快生型根瘤菌分为二个主要聚群和一个次要类群，慢生型根瘤菌分为二个次要类群。主要聚群中一个聚群结瘤能力较高但固氮能力较低，另一聚群结瘤能力和固氮量均较低；次要聚群中快生型和一个慢生型聚群固氮能力较高但结瘤力低，另一慢生型聚群固氮能力和结瘤力均较高。以上研究表明，新疆绿洲农业生态系统中大豆根瘤菌具有一定种质特异性，尽管次要类群具有相对较高的因氮活性，但由于多数根瘤菌形成的根瘤为固氮活性很低的无效根瘤，占优势的主要聚群固氮活性较低，因此土著根瘤菌生物固氮量不能满足作物对氮素的需求，在新疆人工施用根瘤菌剂具有现实意义，但接种的根瘤菌剂可能受到对环境适应性强、结瘤能力高的土著根瘤菌优势类群强有力的竞争。

功能菌剂的混合发酵研究

随着化工行业的发展，大量有毒有害难降解有机物随工业废水的排放进入环境，这些物质能够在环境中长期存在、积累和扩散，通过食物链对动植物的生存及人类的健康造成不良影响。本文以苯酚、对氯硝基苯、氯苯和十六烷为模拟污染物，以前期研制的功能菌剂为对象，经过紫外线线诱变筛选出优于出发菌株的功能菌，对诱变后功能菌的理化性能进行了研究，对菌种进行了鉴定，在此基础上，就其相互之间的微生态关系进行研究，为混合发酵提供理论基础，并就其最佳发酵条件及发酵参数进行了研究，最后对发酵产品的性能进行了检测。目前，国内外有关功能菌剂的研究还存在多方面的不足，主要包括：①由于多菌种混合发酵过程较为复杂，各菌之间存在复杂的相互作用，影响因素较多，关于菌种之间的相互关系研究得很少，环境功能菌剂的发酵方法大多采用单独发酵后混合的方式。单独发酵对原材料、设备和能源的利用率较低，对于多菌种制剂发酵，在设备、能源和原材料的方面造成的浪费更大，将会大幅增加菌剂的生产成本，影响多菌种功能菌剂的发展；②功能菌剂生产过程的质量控制方面研究得较少；③功能菌剂产品的稳定性、抗冲击性能研究得较少，对环境微生物制剂的研究主要集中在菌种选育和培养条件优化方面。 通过本论文研究，得到以下主要结论。 （1）在紫外线诱变处理中，用紫外线对发生一定程度退化的出发菌株进行诱变处理后，六株具有高效降解性能的菌株被筛选出来，诱变筛选出的菌株形态和ERIC-PCR指纹图谱与出发菌株相比发生了明显改变；而且诱变后的菌株对目标难降解底物的降解能力均得到改善，其中，FPN、FCB、F14、FEm对目标底物的降解率提高了20%以上；诱变后菌株经过7次连续传代接种后，对目标难降解底物的降解率无显著变化，具有一定的遗传稳定性。并对诱变后的功能菌进行了初步的鉴定，这6株菌都分别是芽孢杆菌。 （2）对诱变后的功能菌相互之间的微生态关系进行了研究，通过抑菌实验、生长量以及基质消耗量的比较，确定它们之间的生长关系是无害共栖关系，可以进行混合发酵。 （3）对该功能菌剂进行发酵培养条件研究，结果表明发酵培养基的最佳成分（g/L）：葡萄糖 31.0g/L、玉米粉10.0g/L、磷酸氢二钾1.0g/L、硫酸铵1.1g/L、硫酸镁0.55g/L。通过研究不同的培养条件对菌体生长和降解性能的影响，确定了最佳培养条件：培养基初始pH7.5；最适温度32℃；培养基装液量125mL（250 mL三角瓶），以及培养时间对降解性能的影响，培养20 h的产物对降解最为有利。通过研究添加不同目标污染物对菌体生长和降解性能的影响，确定了添加目标污染物的最佳量以及最佳时间：苯酚投加量：1.125 g/L，对氯硝基苯投加量：0.1 g/L；最佳投加时间为发酵培养开始后4 h。 （4）以摇瓶分批发酵最优条件为基础，对FPN、F10、FCB、FNa、F14 和 FEm进行了摇瓶分批发酵试验。以摇瓶分批发酵试验数据为依据，对功能菌剂分批发酵动力学进行了研究，建立了菌体生长和基质消耗的动力学模型，拟合模型能较好的反映功能菌剂分批发酵过程。 （5）功能菌剂和活性污泥协同作用，可以提高系统的生物降解能力，功能菌剂投加量为2%，新鲜活性污泥3500 mg/L，降解24 h条件下，功能菌剂和活性污泥的协同作用对COD的去除率和对照组相比，最多的提高了36.8%。功能菌剂和活性污泥协同作用以及活性污泥的单独作用，其生物降解过程均符合一级反应动力学过程，功能菌剂和活性污泥协同作用的生物降解动力学方程为：，相关系数97%。采用SBR运行方式，引入功能菌剂的SBR系统明显能够改善和提高生物降解的效率。与仅有活性污泥的系统相比，系统对COD的平均去除率可以提高27.1%，同时，系统的耐负荷冲击以及耐毒害冲击的性能比仅有活性污泥的SBR系统强，特别是负荷冲击对引入功能菌剂的SBR系统影响很小。仅有活性污泥的SBR系统经过负荷冲击和毒害冲击之后，不能恢复到冲击之前的水平，而且系统有效作用时间的周期比引入功能菌剂的SBR系统相比大大缩短，而引入功能菌剂的SBR系统处理效果较为稳定，恢复能力很强。 Along with the development of industries, many recalcitrant organic chemicals have been discharged into natural environments together with wastewaters and can exist in waters, soil and sediments for a long time without degradation. These haz-ardous substances, their byporducts and metabolizabilities can be highly toxic, mu-tagenic and carcinogenic, thereby threatening animals, plants and human health through food chain. Consequently the removal of these compounds is of significant interest in the area of wastewater treatment. In this dissertation, the phenol, hydro-quinone, chlorobenzene and hexadecane treated as the model pollutants, the func-tional microorganism agent was used as the starting strains, they treated with ultra-violet light, and then the mutant strains with high degradation ability were screened out and identified primarily, the relationship between these stains were studied, the medium composition and fermentation conditions were optimized, the degradation ability of the fermented production was tested. The literature survey indicates that the study of the microorganism agent is far from complete and more information is re-quired on following problems. 1, Because of the complexity of relationship in mixed fermentation and the complicated factors, the study is hardly to process.2, There is a lack of information on the quality control of the producing process .3, And there is a lack of information on the stability about the microorganism agent. In this dissertation, the main results of the present study could be summarized as follows: (1)The degenerate starting strains were treated with the ultraviolet light, and six mutant strains with high biodegradation ability were screened out by using the me-dium with selective pressure of model pollutants. The mutant strains had great changes in colonialmorphology and ERIC-PCR fingerprinting. And the mutant strains got obvious advantages over the starting strains in degradation ability and over 20% improvement of removal rates was achieved for FPN、FCB、F14 and FEm. The de-gradation ability of the mutant strains was stable after seven generations. After that, the mutant strains were primarily identified as bacillus respectively. (2) The relationship between these mutant strains was studied. By the compari-son of antibiosis effect, biomass and consumption of substrate, the relationships were neutralism and they could be mixed fermented. (3) The optimized cultivation conditions were as follows: glucose 31.0 g/L, corn power 10 g/L, K2HPO4 1.0 g/L, (NH4)2SO4 1.1 g/L, MgSO4 0.55 g/L, initial pH7.5, temperature 32℃, working volume 125 mL/250 mL, and cultivation time 20h (con-sidering the time effect on degradation ability), adding pollutants phenol (1.125 g/L) and hydroquinone (0.1 g/L) into the broth at 4 h after cultivation. (4) Based on the above optimum condition, the batch fermentation was per-formed with strains FPN, F10, FCB, FNa, F14 and FEm in shake flask. The batch fermentation kinetics was studied based on the experimental data. Two kinetic models were constructed which could reflect the regularity of growth and substrate consump-tion in the process of batch fermentation. (5) The co-operation of functional microorganism agent and activated sludge could raise biodegradation of system by adding some microorganism agent and 3500 mg/L fresh activated sludge. Bioaugumentation by the addition of high effective deg-radation culture enhanced the treatment effect of SBR system and the COD removal rate was increased by 20%-36.8%. Its biodegradation matched first-order dynamical reaction equation, and the reaction equation was ln0.2327.391ct=−+. The micro-organism agent had the effect of optimization to activated sludge micro-ecosystem. The SBR system adding 2% microorganism agent, the average COD removal rate of that was increased by 27.1% and stronger anti-shock ability to load and toxicant were achieved (compared with SBR system just adding activated sludge). Especially the load-shock has barely effect to the SBR system adding microorganism agent. After the load and toxicant shock, the SBR system just adding activated sludge couldn’t come back to original level and the activated sludge micro-ecosystem was frustrated. The applying of microorganism agent increased biological activity and system’s re-sistance ability to load shock and toxicant shock.

ATM与BRCA1的双杂合性通过影响若干通路增加肿瘤发生风险

<正>目的:流行病学统计数据表明杂合性与肿瘤发生相关。ATM和BRCA1都是DNA损伤修复通路中的多功能基因,其单杂合性对于肿瘤易感性的影响已见报道,但双杂合

On-line voltammetric monitoring of dissolved Cu and Ni in the Gulf of Cadiz, south-west Spain

Geochemical processes in estuarine and coastal waters often occur on temporally and spatially small scales, resulting in variability of metal speciation and dissolved concentrations. Thus, surveys, which are aimed to improve our understanding of metal behaviour in such systems, benefit from high-resolution, interactive sampling campaigns. The present paper discusses a high-resolution approach to coastal monitoring, with the application of an automated voltammetric metal analyser for on-line measurements of dissolved trace metals in the Gulf of Cadiz, south-west Spain. This coastal sea receives metal-rich inputs from a metalliferous mining area, mainly via the Huelva estuary. On-line measurements of dissolved Cu, Zn, Ni and Co were carried out on-board ship during an eight-day sampling campaign in the study area in June 1997. A pumping system operated continuously underway and provided sampled water from a depth of ca. 4 m. Total dissolved metal concentrations measured on-line in the Gulf of Cadiz ranged between <5 nM Cu (<3 nM Ni) ca. 50 km off-shore and 60–90 nM Cu (5–13 nM Ni) in the vicinity of the Huelva estuary. The survey revealed steep gradients and strong tidal variability in the dissolved metal plume extending from the Huelva estuary into the Gulf of Cadiz. Further on-line measurements were carried out with the automatic metal monitor from the bank of the Odiel estuary over a full tidal cycle, at dissolved metal concentrations in the μM range. The application confirmed the suitability of the automated metal monitor for coastal sampling, and demonstrated its adaptability to a wide range of environmental conditions in the dynamic waters of estuaries and coastal seas. The near-real time acquisition of dissolved metal concentrations at high resolution enabled an interactive sampling campaign and therefore the close investigation of tidal variability in the development of the Huelva estuary metal plume.

Validation and in situ application of an automated dissolved nickel monitor for estuarine studies

The validation of a fully automated dissolved Ni monitor for in situ estuarine studies is presented, based on adsorptive cathodic stripping voltammetry (AdCSV). Dissolved Ni concentrations were determined following on-line filtration and UV digestion, and addition of an AdCSV ligand (dimethyl glyoxime) and pH buffer (N-2-hydroxyethylpiperazine-N′-2-ethanesulphonic acid). The technique is capable of up to six fully quantified Ni measurements per hour. The automated in situ methodology was applied successfully during two surveys on the Tamar estuary (south west Britain). The strongly varying sample matrix encountered in the estuarine system did not present analytical interferences, and each sample was quantified using internal standard additions. Up to 37 Ni measurements were performed during each survey, which involved 13 h of continuous sampling and analysis. The high resolution data from the winter and summer tidal cycle studies allowed a thorough interpretation of the biogeochemical processes in the studied estuarine system.

Automated voltammetric system for shipboard determination of metal speciation in sea water

An automated and semi-intelligent voltammetric system is described for trace metal analysis. The system consists of a voltammeter interfaced with a personal computer, a sample changer, 2 peristaltic pumps, a motor burette and a hanging mercury drop electrode. The system carries out fully automatically approximately 5 metal determinations per hour (including at least 3 repetitive scans and calibration by standard addition) at trace levels encountered in clean sea water. The computer program decides what level of standard addition to use and evaluates the data prior to switching to the next sample. Alternatively, the system can be used to carry out complexing ligand titration with copper whilst recording the labile copper concentration; in this mode up to 8 full titrations are carried out per day. Depth profiles for chromium speciation in the Mediterranean Sea and a profile for copper complexing ligand concentrations in the North Atlantic Ocean measured on board-ship with the system are presented. The chromium speciation was determined using a new method to differentiate between Cr(III) and Cr(VI) utilizing adsorption of Cr(III) on silica particles.

The Obduction of Equatorial 13 degrees C Water in the Pacific Identified by a Simulated Passive Tracer

The obduction of equatorial 13 degrees C Water in the Pacific is investigated using a simulated passive tracer of the Consortium for Estimating the Circulation and Climate of the Ocean (ECCO). The result shows that the 13 degrees C Water initialized in the region 8 degrees N-8 degrees S, 130 degrees-90 degrees W enters the surface mixed layer in the eastern tropical Pacific, mainly through upwelling near the equator, in the Costa Rica Dome, and along the coast of Peru. Approximately two-thirds of this obduction occurs within 10 years after the 13 degrees C Water being initialized, with the upper portion of the water mass reaching the surface mixed layer in only about a month. The obduction of the 13 degrees C Water helps to maintain a cool sea surface temperature year-round, equivalent to a surface heat flux of about -6.0 W m(-2) averaged over the eastern tropical Pacific (15 degrees S-15 degrees N, 130 degrees W-eastern boundary) for the period of integration (1993-2006). During El Nino years, when the thermocline deepens as a consequence of the easterly wind weakening, the obduction of the 13 degrees C Water is suppressed, and the reduced vertical entrainment generates a warming anomaly of up to 10 W m(-2) in the eastern tropical Pacific and in particular along the coast of Peru, providing explanations for the warming of sea surface temperature that cannot be accounted for by local winds alone. The situation is reversed during La Nina years.

Origin and Pathway of Equatorial 13 degrees C Water in the Pacific Identified by a Simulated Passive Tracer and Its Adjoint

The origin and pathway of the thermostad water in the eastern equatorial Pacific Ocean, often referred to as the equatorial 13 degrees C Water, are investigated using a simulated passive tracer and its adjoint, based on circulation estimates of a global general circulation model. Results demonstrate that the source region of the 13 degrees C Water lies well outside the tropics. In the South Pacific, some 13 degrees C Water is formed northeast of New Zealand, confirming an earlier hypothesis on the water's origin. The South Pacific origin of the 13 degrees C Water is also related to the formation of the Eastern Subtropical Mode Water (ESTMW) and the Sub-Antarctic Mode Water (SAMW). The portion of the ESTMW and SAMW that eventually enters the density range of the 13 degrees C Water (25.8 < sigma(theta) < 26.6 kg m(-3)) does so largely by mixing. Water formed in the subtropics enters the equatorial region predominantly through the western boundary, while its interior transport is relatively small. The fresher North Pacific ESTMW and Central Mode Water (CMW) are also important sources of the 13 degrees C Water. The ratio of the southern versus the northern origins of the water mass is about 2 to 1 and tends to increase with time elapsed from its origin. Of the total volume of initially tracer-tagged water in the eastern equatorial Pacific, approximately 47.5% originates from depths above sigma(theta) = 25.8 kg m(-3) and 34.6% from depths below sigma(theta) = 26.6 kg m(-3), indicative of a dramatic impact of mixing on the route of subtropical water to becoming the 13 degrees C Water. Still only a small portion of the water formed in the subtropics reaches the equatorial region, because most of the water is trapped and recirculates in the subtropical gyre.