云南中部无量山大寨子黑长臂猿（Nomascus concolorjingdongensis）生态与行为研究

从2003年3月到2006年5月期间，在云南中部无量山大寨子（24°21′N, 100°42′E）对一个黑长臂猿种群进行了研究。2003年3月至2004年3月主要研究了 3个群体的鸣叫行为。2005年3月一个群体被习惯化，随后对其进行了14个月的连 续观察。在此期间，主要对食性、时间分配、栖息地选择和利用、过夜地及过夜 树的选择等方面进行了研究。这些资料将有助于了解黑长臂猿对其高海拔、高纬 度、季节性变化明显栖息地的适应性，并且对了解长臂猿独特的社会结构具有重 要意义。另外，本研究结合获得的行为生态方面的数据，通过漩涡模型（VORTEX） 对该种群未来动态进行了模拟，对大寨子种群的保护和发展提出了保护建议。 黑长臂猿叫声在所有长臂猿中频率最高。成年雄性能发出boom、简单重复 音节和调节音节；成年雌性只能发出成功的激动鸣叫和失败的激动鸣叫。两者互 相配合组成结构复杂的二重唱，配对个体很少单独鸣叫，青年个体经常会加入二 重唱。同一群内两个成年雌性多数时候一起鸣叫。配对个体平均两天鸣叫一次 （53%），每次鸣叫平均持续时间12.9 分钟，雌性激动鸣叫4.6 次，激动鸣叫的 平均时间间隔为115 秒，91.5%的鸣叫发生在日出前半小时和日出后3 小时之间。 通过对相邻群体间鸣叫行为的分析，结果发现相邻群体倾向于不在同一天鸣叫， 如果同一天鸣叫，鸣叫的时间间隔显著长于不在同一天鸣叫的时间间隔，这些结 果不支持鸣叫具有调节群体空间距离的功能（inter-group spacing）的假说。雄性 倾向选择一个区域内最高的树进行鸣叫，这可能是为了声音的远距离传播。另外 雄性对鸣叫树的选择也兼顾了安全因素。通过比较鸣叫前后个体间的距离，黑长 臂猿的鸣叫具有群内通讯的功能，鸣叫后个体间的距离显著短于鸣叫前的距离。 虽然鸣叫树的分布与食物斑块的分布在不同海拔段和不同网格内都呈现出了高 度的相关性，但不能确定黑长臂猿在食物斑块附近进行鸣叫就是为了对食物资源 进行防御。 利用扫描法对研究群体的食性和时间分配进行了研究。结果显示研究群体共 取食77 种植物和至少6 种动物，其中10 种重要食物占到取食比例的76.7%。在 10396 次确定食物类别的记录中，除无花果外的其它果实占25.5%，藤子叶和芽占21.0%，树叶和芽占19.2%，无花果占18.6%，花占9.1%，寄生植物的叶占6.3%， 另外其它食物占0.3%。黑长臂猿的食性具有明显的日变化和季节性变化。与其 它长臂猿相比，黑长臂猿的食性更加广泛。虽然黑长臂猿进食叶（藤子的叶和芽、 树叶和芽、寄生植物的叶）的比例稍多于进食果实（无花果和其它果实）的比例， 但当果实丰富时，它们仍然优先选择果实。 黑长臂猿平均在日出后33 分钟离开过夜树，在日落前128 分钟进入过夜树， 平均每天活动518 分钟。活动期间，黑长臂猿用于休息的时间最多，达到40.0%， 其次是取食28.7%，排在第三的是移动19.8%，排在第四的是觅食占到6.1%，鸣 叫占2.6%，玩耍和其它活动一共占活动时间的2.8%。时间分配具有明显的日变 化和季节性变化。食物和温度因素是影响黑长臂猿时间分配季节性变化的最主要 的原因。 群体一共利用129 个1 公顷的网格，如果包含在活动路线内的空隙，活动范 围达到151 公顷，主要由3 个大的山沟组成。黑长臂猿平均每天移动1391 米， 进入9 个网格，连续两天倾向于利用家域中的同一条山沟。群体平均每月仅利用 家域的19%~50%，集中利用家域中的小部分区域，除2 月份外群体总是选择利 用原始常绿阔叶林。形成这种现象的原因主要与食物的分布及其季节性变化有 关、并且与该群生活地区的地形有关。 黑长臂猿喜欢选择高大的，生长在陡坡上的树过夜，群体一般形成4 个不同 的小单元过夜（青年个体与成年雄性睡在一起，两个成年雌性与未独立的婴猿分 别睡在一起，亚成年雄性单独过夜），过夜时总是快速进入过夜树，然后立即安 静下来，利用很多棵不同的过夜树，并且间隔很长时间后才重复利用，这些行为 都是为了避免被捕食者发现和攻击。群体喜欢在山坡上过夜，并且在冬天喜欢选 择在长有寄生植物的大树枝上过夜，这些行为可能与研究地点冬天的低气温有 关。此外，过夜树的选择可能兼顾舒适和方便寻找食物的功能。 通过获得的生态学资料，结合近缘种生态学参数，利用漩涡模型（VORTEX） 对该种群未来动态进行了模拟。结果显示：大寨子亚种群是一个具有很强的潜在 繁殖力的种群，如果没有偷猎，亚种群在100a 之内不会灭绝，并且能迅速达到 环境容纳量。但是每年如果有1 只成年雄性和1 只成年雌性被猎杀，该种群将会在第78a 灭绝，且灭绝概率为100%。不同程度的死亡率对种群影响不大，但高 死亡率显著延缓了种群到达环境容纳量的时间。环境容纳量对种群遗传多样性损 失具有重要的影响，在没有猎杀的情况下，种群的长期存活需要一个较大的环境 容纳量。因此，在黑长臂猿受到严格保护、且栖息地主要在保护区内的今天，严 密监控火灾的发生，限制牲畜进入林区等人为干扰的影响，保护好黑长臂猿栖息 地是首要工作之一。但如果能使其栖息地周围的森林植被得到恢复，增加其栖息 范围，将有利于该地区黑长臂猿的发展。

滇南、滇东南黑长臂猿分布与数量及金平芭蕉河黑长臂猿栖息地选择与利用

长臂猿是现存最小的类人猿（俗称小猿），主要分布于东南亚的的热带雨林、季雨林及亚热带常绿阔叶林中，是典型的树栖灵长类动物。我国现有长臂猿3属5种，包括黑长臂猿(Nomascus concolor)、白颊长臂猿(N. leucogenys)、海南长臂猿(N. hainanus)、白掌长臂猿(Hylobates lar)和白眉长臂猿(Hoolock hoolock)。其中黑长臂猿是主要分布于我国云南省境内的一种长臂猿，在国外仅在越南北部和老挝西北部局部地区分布，越南北部的数量不足100只，老挝目前仅发现9群。 滇南、滇东南曾是黑长臂猿广泛分布的地区之一。为掌握该地区近年黑长臂猿分布及种群数量现状，从2003年7月～2004年12月，利用访问调查及利用鸣声定位法对该地区进行了调查。调查结果显示，在云南境内，近40 000 km2的范围内，黑长臂猿在红河以东可能已消失，而红河以西亦仅发现4～7个种群，且孤立分布于3个地区（金平芭蕉河2群6只，金平西隆山1－2群，绿春黄连山1～3群，总计不超过25只），而在江城牛倮河自然保护区、马关古林箐自然保护区、麻栗坡老君山自然保护区及屏边大围山自然保护区可能已绝迹。滇南、滇东南黑长臂猿分布区缩小及种群数量剧减，主要与栖息地丧失及过度捕猎有关。 在长臂猿数量与分布调查的基础上，我们于2004年底确定了以金平芭蕉河黑长臂猿的一个群体为研究对象进行行为生态观察。通过扫描与瞬时取样法记录，结合生境调查及物候监测，对其游走行为及生境利用格局进行了比较和分析，主要结论如下：⑴家域大小（活动范围）不是限制长臂猿日活动距离及活动时间的主要原因；⑵日活动距离及移动时间均与温度呈正相关；⑶食物资源分布及斑块丰富度一定程度上决定了长臂猿对栖息地选择与利用方式；⑷长臂猿对陡坡与沟谷利用强度较高，与其主要行为表现（如;过夜点、休息点、取食点选择）有关；⑸长臂猿过夜点选择与食物资源分布、群体间关系及鸣叫点选择无关，而可能与天气和安全性因素有关；⑹果实树分布对取食点、休息点选择作用明显，而物候变化及食物可得性可能是影响长臂猿对栖息地利用季节性变化的主要原因；⑺在一定程度上，人为干扰只是在短时间内改变了长臂猿的活动路线或时间，而对其总体的生境利用策略并没有太大影响。食物资源的分布及季节性变化在长臂猿的游走行为及生境利用中均起到了重要作用。

THE STUDY OF MICROSTRUCTURE IN IRON-DOPED AND SULFUR-DOPED INP CRYSTALS BY MEANS OF HREM AND COMPUTER-SIMULATION

The microstructures in iron- and sulphur-doped InP crystals were studied using both electron microscopy and electron diffraction. A modulated structure has been found in S-doped InP crystal, where the commensurate modulations corresponded to periodicities of 0.68 nm and 0.7 nm in real space and were related to the reflections of the cubic lattice in [111] and [113BAR] directions; they were indexed as q111* = 1/2(a* + b* + c*) and q113BAR* = 1/4(-a* - b* + 3c*), respectively. Single atomic layers of iron precipitate were observed, with preferred orientations along which precipitates are formed. Simulated calculations by means of the dynamical theory of electron diffraction using models for the precipitate structure were in good agreement with our experimental results. The relation between the modulated structure and the precipitates is also discussed.

青稞B组醇溶蛋白基因与上游调控区的克隆及基因表达

高等植物种子胚乳贮藏蛋白是种子发芽时的主要氮源，也是人类和动物食用植物蛋白的主要来源。大麦种子胚乳贮藏蛋白主要是醇溶蛋白（hordeins），占大麦胚乳总蛋白的50–60%。根据大麦醇溶蛋白的大小和组成特点，大麦醇溶蛋白被划分为三种类型：富硫蛋白亚类(B，γ-hordeins)、贫硫蛋白亚类（C-hordeins)以及高分子量蛋白亚类(D-hordeins)。B组和C组醇溶蛋白是大麦胚乳的两类主要贮藏蛋白，它们分别占大麦总醇溶蛋白成分的70–80%和10–12%。遗传分析表明，大麦B、C、D和γ-组醇溶蛋白分别是由位于大麦第五染色体1H（5）上的Hor2、Hor1、Hor3和Hor5位点编码。Hor2位点编码大量分子量相同但组成不同的B组醇溶蛋白（B-hordein）。B-hordein的种类、数量和分布是影响大麦酿造、食用及饲养品质的重要因素之一。为深入了解B-hordein基因家族的结构和染色体组织，探明Hor2位点基因表达的发育调控机制，最终达到改良禾谷类作物籽粒品质的目的，本研究以青藏高原青稞为材料，采用同源克隆法，分别克隆B-hordein基因和启动子，通过原核生物表达验证B-hordein基因功能，并利用实时定量PCR探索B-hordein基因表达时空关系，取得如下研究结果： 1. 以具有特殊B组醇溶蛋白亚基组成的9份青藏高原青稞为材料，根据GenBank中三个B-hordein基因序列（GenBank No. X03103, X53690和X53691）设计一对引物，通过PCR扩增，获得23个B-hordein基因克隆并对其进行了序列分析。核苷酸序列分析表明，所有克隆均包含完整的开放阅读框。有11个克隆都存在一个框内终止密码子，推测这11个克隆可能是假基因。推测的氨基酸序列分析表明，所有大麦B-hordein具有相似的蛋白质基本结构，均包括一个高度保守的信号肽、中间重复区以及C-端结构域。不同大麦种重复区内重复基元的数目有较大差异。青稞材料Z07–2和Z26的B-hordeins仅具有12个重复基元结构，更接近于野生大麦。这些重复基元数目的差异导致了重复区序列长度和结构的变异。这种现象极可能是由于醇溶谷蛋白基因在进化过程中染色体的不平衡交换或复制滑动所造成的。对所克隆基因和禾本科代表性醇溶谷蛋白基因进行聚类分析，结果表明所有来自栽培大麦的B-hordeins聚类成一个亚家族，来自野生大麦的B-hordeins以及普通小麦的LMW-GS聚类成另外一个亚家族，表明这两个亚家族的成员存在显著差异。此外，我们发现B-hordein基因推测的C-末端序列具有一些有规律的特征：即具有相同C-末端序列的B-hordein基因在系统发生树中聚类为同一个亚组（除BXQ053，BZ09-1，BZ26-5分别单独聚为一类外）。这个特征将有助于我们对所有B组醇溶蛋白基因家族成员进行分类，避免了在SDS-PAGE电泳图谱上仅依靠大小分类的局限性。 2. 根据上述克隆的青稞B-hordein基因的5’端序列设计三条基因特异的反向引物，以青稞Z09和Z26的基因组DNA为模板，采用SON-PCR和TAIL-PCR技术分离克隆出8个B-hordein基因的上游调控序列（命名为Z09P和Z26P）。序列分析表明，推测的TATA box位于–80 bp，CAAT–like box位于–140 bp处。此外，Z09P和Z26P中有六个序列在–300 bp处均存在一个由高度保守的EM基序和类GCN4基序构成的胚乳盒(Endosperm Box，EB)，在约–560 bp处存在一个胚乳盒类似结构。而Z09P-2和Z26P-3不存在保守的胚乳盒或其类似结构，预示着这两个启动子所调控的基因表达可能受不同类型反式作用因子的调节，推测该启动子对基因的表达调控具有多样性。 3. 将B-hordein基因的开放阅读框定向克隆到表达载体pET-30a中，将其导入大肠杆菌表达菌株BL21中进行外源基因的诱导表达以验证所克隆基因的功能。结果表明仅含重组子pET-BZ07-2和pET-BZ26-5的BL21细菌有目的表达蛋白产生。在诱导3 h时的蛋白表达量最高；3 mM IPTG诱导的蛋白表达量要高于1 mM IPTG诱导的表达量。这为分离纯化B-hordein蛋白以及进一步研究其对大麦籽粒品质的影响奠定基础。 4. 根据从青稞Z09和Z26中分离克隆的B-hordein基因序列设计一对基因特异的引物，同时，选择大麦α-微管蛋白基因（GenBank no. U40042）为看家基因并设计特异引物，利用实时荧光定量PCR检测了青稞籽粒4个胚乳发育时间段的B-hordein基因表达，荧光定量结果显示：两份材料中B-hordein基因的表达量均随发育过程的进行而逐渐升高。Z09中B-hordein基因在开花后7天开始转录，而Z26开花4天后就有低水平B-hordein的表达，这表明Z26中B-hordein基因可能比Z09表达的较早或者Z09中B-hordein基因表达水平较低以致于不能被检测到。此外，在4个不同的胚乳发育时期中，Z26中B-hordein基因的表达量均高于Z09材料。在开花12天到18天的过程中，Z09和Z26中B-hordein基因的表达水平有一个急剧性的升高。这说明在不同胚乳发育时期，Hor2位点的B-hordein等位基因变异体存在mRNA的差异表达。 Seed endosperm storage proteins in higher plants are the main resources of nitrogen for germinating and plant proteins for human and animals. Barley prolamins (also called hordeins) are the major storage proteins in the endosperm and account for 50–60% of total proteins. Hordeins are classically divided into three groups: sulphur-rich (B, γ-hordeins), sulphur-poor (C-hordeins) and high molecular weight (HMW, D-hordeins) hordeins based on the size and composition. B-hordeins and C-hordeins are two major groups and each respectively account for about 70-80% and 10-12% of the total hordein fraction in barley endosperm. Genetic analysis showed that B-, C-, C-, γ-hordeins are encoded by Hor2, Hor1, Hor3 and Hor5 locus on the chromosome 1H (5). Hor2 locus is rich in alleles that encode numerous heterogeneous B-hordein polypeptides. It is reported that B-hordein species, quantity and distribution are significant factors affecting malting, food and feed quality of barley. To understand comprehensively the structure and organization of B-hordein gene family in hull-less barley and explore the developmental control mechanisms of Hor2 locus gene expression and eventually to better exploitation in crop grain quality improvement, we isolated and cloned B-hordein genes and promotors of hull-less barley from Qinghai-Tibet Plateau by PCR, and testified their expression founction in bacteria expression system and explore their spatial and temporal expression pattern by quantitative real time PCR. Our results are as followed, 1. Twenty-three copies of B-hordein gene were cloned from nine hull-less barley cultivars of Qinghai-Tibet Plateau with special B-hordein subunits and molecularly characterized by PCR, based on three B-hordein genes published previously (GenBank No. X03103, X53690 and X53691). DNA sequences analyses confirmed that the six clones all contained a full-length coding region of the barley B-hordein genes. Eleven clones all contain an in-frame stop codon and they are probably pseudogenes. The analysis of deduced amino acid sequences of the genes shows that they have similar structures including signal peptide domain, central repetitive domain, and C-terminal domain. The number of the repeats was largerly variable and resulted in polypeptides in different sizes or structures among the genes. Twelve such repeated motifs were found in Z07–2 and Z26, and they are close to those of the wild barleys, and it is most probably caused by unequal crossing-over and/or slippage during replication as suggested for the evolution of other prolamins. The relatedness of prolamin genes of barley and wheat was assessed in the phylogenetic tree based on their polypeptides comparison. Our phylogenetic analysis suggested that the predicted B-hordeins of cultivated barley formed a subfamily, while the B-hordeins of wild barleys and the two most similar sequences of LMW-GS of T. aestivum formed another subfamily. This result indicated that the members of the two subfamilys have a distinctive difference. In addition, we found the B-hordeins with identical C-terminal end sequences were clustered into a same subgroup (except BXQ053，BZ09-1 and BZ26-5 as a sole group, respectively), so we believe that B-hordein gene subfamilies possibly can be classified on the basis of the conserved C-terminal end sequences of predicted polypeptide and without the limit of SDS-PAGE protein banding patterns. 2. The specific primers were designed according to the published sequences of barley B-hordein genes from Z09 and Z26. Using total DNA isolated from them as the templates, eight clones (designated Z09Pand Z26P) of upstream sequences of the known B-hordein genes was obtained by TAIL-PCR and SON-PCR. Sequences analysis shows that the putative TATA box was present at position –80 bp and CAAT-like box at position –140 bp. Besides, a putative Endosperm Box including an Endosperm Motif (EM) and a GCN4-Like Motif was found at position –300 bp in six clones, and another Endosperm-like box was found at positon –560 bp. While the Endosperm Box or Endosperm-like box was not found in Z09P-2 and Z26P-3. This may indicate that gene expression drived by the two promtors was probably controlled by different trans-acting factors and the genetic control mechanism of corresponding gene expression may be diverse. 3. The B-hordein genic region coding for the mature peptide was cloned into expression vector pET-30a and transformed into bacterial strain BL21 for identifying gene expression fountion. Protein SDS–PAGE analysis showed that only the transformed lysate with the pET-BZ07-2 and pET-BZ26-5 constructs produced proteins related to B-group hordeins of barley, and the mounts of proteins induced by 3 mM IPTG and 3 h were higher than other conditions. This established a base for isolating and putifying B-hordein and further exploring their effects on barley grain quality. 4. The gene-specific primers of B-hordein genes from Z09 and Z26 were used for the quantification of B-hordein gene expression. The α-tubulin gene from Hordeum vulgare subsp. vulgare (GenBank accession number U40042) was used as a control gene. The result shows the transcription of the B-hordein genes in Z09 was found 7 days after flowering, while the transcription of the B-hordein genes in Z26 was found 4 days after flowering, but at a very low level, and it suggested that the B-hordein genes in Z26 probably expressed earlier than those in Z09, or the B-hordein genes in Z09 expressed at so a lower level than Z26 that it can not detected. In addition, B-hordein genes in Z26 accession showed higher expression levels than those in Z09 in four developing stages. Furthermore, a progressive increase in the expression levels of the B-hordein genes between 12 and 18 days after anthesis was observed in both Z09 and Z26. It implies that the B-hordein allelic variants encoded by Hor2 locus exist the differential expression in mRNA levels of during barley endosperm development.

自养氨氧化混合种群特性和共存机理初步研究

组特殊自养氨氧化混合种群，表现：无机环境种群生长迅速、生物量高；在一个完全无机的自养生长环境中，不仅保持高氨氧化速率，并出现丰富的异养微生物种群；该种群置于异养、厌氧环境中，迅速表现出产氢特征。对于这样一个特殊的生态体系，研究其共生机理，以及联接这些种群之间的碳源和能源问题，将具有非常重要意义。我们拟从种群特征、细胞表面分泌产物、游离体系产物多糖、蛋白和脂肪酸方面开展研究。 第一部分，自养氨氧化混合种群的基本特征。采用氨氧化培养基，进行种群氨氧化特征研究；采用扫描电镜观察自养混合种群的微观特征；沉降、离心去除微生物种群，分析水相中的总有机碳、糖类等物质；利用LB培养基进行种群的分离、纯化，并采用DGGE手段对微生物种群结构进行分析。结果表明，接入菌种后（2/5000（V/V）），培养液中氨（200mg/L）在3－5天内快速降解；亚硝酸盐与氨氮变化呈负相关趋势，仅有少量硝酸盐含量（< 30mg/L）。氨氧化种群的生物量增长与氨氧化趋势一致，初始生物量7.75 mg/L(蛋白含量)，3-5天后生物量快速增长，并达到最高63.06 mg/L（蛋白含量）。电镜图片显示，种群外包裹一层粘液。离心除去菌体后，检测培养液总有机碳和糖的含量，同样表现出与生物量增长相似的特征，分别由初始的3.73、2.35 mg/L，3－5内天迅速增加，并分别达到最大值35.19、27.45 mg/L。经初步分离、纯化并对纯化菌株进行测序，获得了10株异养微生物分别为布鲁氏菌科苍白杆菌属、纤维单孢菌、类芽孢菌属、黄杆菌属、无色杆菌、鞘脂单胞菌、嗜麦芽寡养单胞菌、噬氢菌属、硫红球菌、假单胞菌；DGGE显示，约有20分条离带，我们对其中的两条优势条带进行切割回收测序，鉴定为欧洲亚硝化单胞菌（Nitrosomonas eur）。 第二部分：混合种群自养-异养菌共生的可能机制。在对微生物种群特征初步分析基础上，针对胞外糖类组分可能被微生物代谢分解，我们重点对微生物细胞蛋白质与糖类进行分析。采用超声结合RIPA裂解液裂解，SDS-PAGE电泳分析混合种群总蛋白种类，并通过氨基酸分析仪及红外光谱法分析氨基酸组成及蛋白红外特征。采用超声破碎结合反复冻融对细胞样品进行处理，提取液采用醇沉、Sevage脱氮白，凝胶过滤方法脱盐和分级分离。对提取物的糖分析包括：紫外扫描，红外光谱，核磁共振，单糖组成分析；扫描电镜观察菌群破裂现象。SDS-PAGE分析结果表明：氨氧化种群不同生长阶段都显示出42kD蛋白表达量很高，d4时42kD蛋白表达已经很强，4-7d内一直持续这种过量表达，直到d8后表达开始减弱。说明42kD蛋白可能与氨氧化密切相关。红外光谱分析显示：细胞提取物的特征峰分布在3427.42cm-1、1718.18 cm-1和1681.72 cm-1、1160.07和1086.74 cm-1，分别对应为OH、 C=O、C－O－C基团，表明具有蛋白的典型特征；氨基酸分析显示蛋白中的Gly,Asp,Ala,Glu含量相对较高。 提取物中胞外多糖分离谱图得到不均一组分，共得到6个收集峰；紫外扫描在201－213 nm处有多糖吸收峰，同样表明多糖成分不均一性；多糖红外光谱特征峰主要分别在3400.49 cm-1、2920.28 cm-1、1154.54和1087.52 cm-1，对应OH、－CH2－ or CH 、C－O－H or C－O－C等多糖特征基团；多糖提取物核磁共振1H d4.3～5.9之间出现强吸收峰，这是1H中，多糖存在的明显证据，1H NMR中，其中O-乙酰基的甲基上的氢信号为d1.1～1.3之间。糖肟全苯甲酸酯衍生物的HPLC测定中，得到单一的单糖峰，由于时间问题，还未进行更深入的试验；电镜图片显示，种群中的细胞有大量的破裂现象。 实验表明，自养氨氧化混合种群显示出快速的氨氧化速率，氨氧化过程生物量和有机质的增加明显。微生物种群包裹粘液层，并分离纯化出大量的异养菌；去除菌体后的游离培养液中存在有机质（包括多糖）说明无机自养生长体系中存在异养菌生长、繁殖的二次碳源；细胞提取物中蛋白条带数目多、种类丰富；细胞多糖提取物具有明显的多糖特征，以及单糖的存在。结合种群的显微特征和游离体系中的有机质的检测结果，我们认为，无机自养生长体系中，种群细胞生长过程中发生的破裂现象可能是导致大量的蛋白、多糖释放到游离胞外，并成为其他异养菌生长的碳源和氮源。这可能是自养体系中，大量异养菌共生的可能机制，至于是什么原因引起种群生长过程中产生的破裂现象，还有待下一步深入研究。 A group of mixed autotrophic ammonia oxidizing populations, having much biological characteristic tested by concerned personnel for pilot test: Performed rapid population growth and obtained high biomass in inorganic environment; Not only maintained a high rate of ammoxidation, promoted a wealth of heterotrophic microbial populations growth in a totally inorganic and autotrophic growth environment; Placed in heterotrophic and anaerobic environment,had the performance characteristics that could rapidly produce hydrogen.For such a special ecological system, Study its symbiotic mechanism and the connection between these populations of carbon and energy issues, will have a very important significance. We intended from the characteristics of the population, the secretion product of cell surface, free substance in the liquid medium like polysaccharide, protein and fatty acids carrying out research. Part I: The basic features of mixed autotrophic ammonia oxidizing populations . Use inorganic liquid medium, processed study for ammonia oxidation characteristics of the population; we used scanning electron microscopy to get micro-features of autotrophic ammonia oxidizing populations .The medium was carried out settlement and centrifugal then removed the microbial populations, after all of that we analysis the water phase for total organic carbon(TOC), carbohydrate and other substances; Solid ammonia oxidizing medium was adopted to separation and purification of population, DGGE means was for structure analysis of microbial population. The results showed that after the inoculum of bacteria (2 / 5000 (V / V)), ammonia in the culture medium (200 mg / L) was rapid degradation in 3-5 days; ammonia and nitrite have the negative correlation between changes in the trend, then only a small amount of nitrate content (<30mg / L). The biomass growth of ammoxidation population in line with the trend of ammonia oxidation, the initial volume of it was 7.75 mg / L (protein content), in 3-5 days upto 63.06 mg / L (protein content). Electron microscope image showed, the populations were wrapped in a layer of mucus, including the a large number ruptted micorbe , Centrifuge to remove bacteria, then detected the medium for total organic carbon and sugar content, result took on the same characteristics with biomass growth, that were from the initial 3.73、2.35 mg / L respectively, in 3-6 days achieved rapid increase in the maximum to 35.19、27.45 mg / L respectively. After initial separation、 purification ,then processed sequencing to strains purified and got the result that there were 10 heterotrophic microorganisms : Brucella Branch pale bacillus, Cellu lomonas, Bacillus species category, a Flavobacterium, colorless Bacteria, Aeromonas sheath fat, little support maltophilia Aeromonas, macrophages species hydrogen, sulphur-MI, Pseudomonas bacteria spores; DGGE display, there were 20 separation bands approximately. Part II: Mixed populations that autotrophic - heterotrophic bacteria symbiotic mechanism. On the basis of preliminary analysis of microbial population characteristics, aiming at extracellular carbohydrate components might be decomposition by microbial, we focused on microbial cell protein and carbohydrate analysis. Using ultrasound combined with RIPA lysis cracking the cells, SDS-PAGE electrophoresis analysis the total protein species of the population, and through the amino acid analyzer studied the compositions of amino acid and infrared spectroscopy analysis of a protein infrared characteristics. Using ultrasound combined with repeatedly freezing and thawing to treated the cell sample, then took the means that alcohol precipitation, deproteinization by Sevage, gel filtration aimed at desalination and grade separation to deal with the lysates . The extraction of sugar analysis included: UV scanning, IR, NMR, single-sugar composition analysis. SDS-PAGE analysis showed that: 42 kD protein expression was very high at different growth stages of mixed autotrophic ammonia oxidizing populations , on the fourth day, 42 kD protein expression had been very strong, 4-7d, it had continued this excessive expression, then started to weaken after 7 days. 42 kD protein that might be closely associated with ammonia oxidation. Infrared spectral analysis showed that: cell extracts with the characteristic that the peak distribution in 3427.42 cm-1、1718.18 cm-1 and 1681.72 cm-1、1160.07 cm-1 and 1086.74 cm-1 corresponding to OH、C = O、C-O-C Groups which had the typical characteristics of protein; and analysis showed that amino acids including Gly, Asp, Ala, Glu ,the content in the protein is relatively high. Exopolysaccharide in the extracts had the separation map that it was uneven, received a total of six collection peaks by the detection mode of phenol-sulphruic acid method ; ultraviolet scan in the 201-213 nm department had polysaccharide absorbing peak, the same ingredients that polysaccharide heterogeneity; infrared polysaccharide spectral characteristics of the main peak at 3400.49 cm-1, 2920.28 cm-1, 1154.54 and 1087.52 cm-1, corresponding OH,-CH2-or CH, C-O-H or C-O-C;and other characteristics of polysaccharide group; 1H NMR of polysaccharide extract appeared absorption peak between d4.3 ~5.9, which is the apparent evidence of polysaccharide, In 1H NMR, the hydrogen signal of one of O-acetyl was between 1.1 to 1.3. The determination of Sugar oxime whole benzoate derivatives by HPLC, there was a single-sugar peak, as a matter of time, yet more in-depth test. Summary: Mixed autotrophic ammonia oxidizing populations show us that it had the ability in ammonia oxidizing and it was great, organic matter and biomass increased significantly in the process of ammonia oxidation. Microbial populations was wrapped up slime layer, the phenomenon of cell breakdown obviously, and there were a lot of separation and purification of the heterotrophic bacteria; a lot of organic matter (including polysaccharides)remined in the medium that removal of cell indicated the inorganic system existed secondary carbon sources that could be used by the heterotrophic bacteria ; there were a large number proteins bands of cell extract, rich variety; cell extracts of polysaccharide had obvious characteristics of polysaccharide, and the existence evidence of single-sugar. Combined population of microscopic characteristics and free of organic matter in the test results, we believe that the health of inorganic system, population growth occurred in the course of the breakdown of the phenomenon is likely to lead to a lot of protein and polysaccharide released into the extracellular free, And other heterotrophic bacteria use them to the growth as carbon and nitrogen. This may be autotrophic system, the large number of heterotrophic bacteria symbiotic mechanism.

Two-stage photo-biological production of hydrogen by marine green alga Platymonas subcordiformis

A marine green alga, Platymonas subcordiformis, was demonstrated to photobiologically evolve hydrogen (H-2) after the first stage of photosynthesis, when subjected to a two-phase incubation protocol in a second stage of H2 production: anaerobic incubation in the dark followed by the exposure to light illumination. The anaerobic incubation induced hydrogenase activity to catalyse H? evolution in the following phase of light illumination. H,) evolution strongly depended upon the duration of anaerobic incubation, deprivation of sulphur (S) from the medium and the medium pH. An optimal anaerobic incubation period of 32 h gave the maximum H2 evolution in the second phase in the absence of sulphur. Evolution of H,) was greatly enhanced by 13 times when S was deprived from the medium. This result suggests that S plays a critical role in the mediation of H-2 evolution from R subcordiformis. A 14-fold increase in H-2 production was obtained when the medium pH increased from 5 to 8; with a sharp decline at pH above eight. H-2 evolution was enhanced by 30-50% when supplementing the optimal concentrations of 25 mM acetate and 37.5 mM glucose. (C) 2003 Elsevier B.V. All rights reserved.

Environmental Kuznets Curve for SO_2 Emissions in China

This study examines the link between the economic growth and the environmental quality. Based on a panel data set, a N-shaped Environmental Kuzents Curve has been found for the sample period: a cubic relationship between per capita GDP and emissions of sulphur dioxide (SO2). We also find that energy consumption is an important determinant of environmental degradation. The empirical results suggest that we should promote environmental protection as soon as possible.

STUDIES ON THE REACTIONS OF TRANSITION-METAL HYDRIDES WITH HETEROCUMULENES .6. REACTION OF CP2ZR(H)CL WITH RNCS (R=C6H5, 2-C10H7, C-C6H11 AND N-C4H9)

The novel NS-containing zirconacycle complexes Cp2ZrCl[SC(H)NR] (1a, R = C6H5; 1b, R = 2-C10H7; 1c, R= C-C6H11; 1d; R = n-C4H9) were obtained by insertion reactions of Cp2Zr(H)Cl with RNCS. 1(a-d) could react further with Cp2Zr(H)Cl to yield a sulphur-bridging compleX (Cp2ZrCl)2S (2) and a Schiff base RN=CH2. The crystal structure of la has been determined by X-ray analysis.

A MASS-SPECTROMETRIC STUDY OF ORGANIC PHOSPHORUS-COMPOUNDS .5. EI SPECTRA OF 1, 3, 2-OXAZAPHOSPHOLIDINE 2-SULFIDES DERIVATES

The mass spectral behaviour of 15 new type of organic phosphorus compounds with a considerable insecticidal activity, 1, 3,2-oxazaphospholidine 2-sulfides derivatives, under 70 eV electron impact has been studied by means of high and low resolution mass spectrometry as well as by B/E linked scan and MIKES/CID analysis. Discussion is focused into the isomerization between oxygen and sulphur in molecules and some rearrangement reactions.

PYRITE GENESIS DURING EARLY DIAGENESIS IN YELLOW SEA AND EAST-CHINA-SEA

The content and isotopic compositions of different sulphur species in pore-water and solid phases have been examined on five sediment cores taken from muddy sediment region in the Yellow Sea and the East China Sea. Relationships among these data have been investigated with the combination of morphology of mineral pyrite and organic matter so as to role out the diagenetic behaviour of sulphur species at the early stage of diagenesis in modern marine sediment and the origin of pyrite formation.

Effect of N fertilizer on the productivity and nutritive values of perennial grass mixtures in the alpine region of Qinghai-Tibetan Plateau, China

A study was conducted on grass mixtures that included smooth bromegrass (SB) + drooping wild ryegrass (DW), smooth bromegrass + Siberian wild ryegrass (SW) + crested wheatgrass (CW) and smooth bromegrass + Siberian wild ryegrass + drooping wild ryegrass + crested wheatgrass in the alpine region of Qinghai-Tibetan Plateau. The study was conducted from 1998 to 2000 to investigate the effects of N application rates and growing year on herbage dry matter (DM) yield and nutritive values. Herbage DM production increased linearly with N application rates. The effect of N application on DM yields was greater (P < 0.05) in the 2nd and 3rd production years than in the establishment year. Dry matter yields of SB + SW + CW and SB + SW + DW + CW can reach as high as 15 000 kg ha(-1) at 345 kg ha(-1) N rate in the 3rd growing year. With increased N application rates, crude protein (CP) contents and 48 h in sacco DM degradability of grasses increased (P < 0.05). No effect (P > 0.05) of N application was detected on organic matter (OM) and acid detergent fibre (ADF) concentration. It can be concluded that for increased biomass production in the alpine region of the Qinghai-Tibetan Plateau, a minimum of 345 kg N ha(-1) should be applied to grass stands in three split application of 115 kg N ha(-1), in early June, early July and late July

富硫流体的成因与硫酸盐还原作用研究

Origins of H_2S, thiols, thiophenes in natural gases and sulphur-enriched oils are complicated and thus some debates exist on them. The post-doctoral research is based upon oil- and gas-field data. Cases for study include Triassic Jianglingjiang Formation natural gases, Wolonghe Field, Sichuan Basin, Paleozoic oils and bitumen, Central Tarim, gases reserviored nearby Carboniferious - Ordovician unconformity, Hetianhe Field, Tarim Basin and sulphur-enriched oils in Tertiary reserviors in Jinxian Sag, Bohai Bay Basin. We have carried out analyses on the oils and gases for chemistry, δ~(13)C, δ~(34)S, and molecular composition of biomarkers, analyzed authigenetic pyrite forδ~(34)S, formation water for chemistry and δD and δ~(18)O along with petroleum system and burial history analyses, The aims are to assess the origins of the H2S and authigenetic pyrite, to discuss the possibility of reduced sulphur incorporation into hydrocarbons and to determine the mechanisms of hydrocarbon secondary alteration in the above four cases by comparison. The research shows that the reduced sulphur in the four cases is the result of thermochemical and biological sulphate reduction., TSR and BSR, respectively. No evidence indicates an origin of decomposition of organic matter or mantle - derived H2S in the cases. Elevated H_2S contents (up to 32%) in the Triassic Jialingjiang Formation are considered to result from TSR while relatively low H_2S (up to 2000ppm) in the Hetianhe Field resulted from BSR. However, it is not the case for the Central Tarim where relatively low H2S but abundant authigenetic pyrite occurr. Part of the H_2S in the Central Tarim reservoirs has reacted with iron released from clay minerals to precipitate pyrite. Thus, reduced sulphur δ~(34)S and reservoir temperatures rather than the H2S amount are reliable parameters to distinguish between TSR and BSR. TSR in Sichuan Basin Triassic Jialingjiang Formation and Central Tarim Paleozoic reservoirs are showed to take place at more than 125℃. the H2S and authigenetic pyrite have δ~(34)S close to parent anhydrite. In contrast, BSR in the reservoirs near the Carboniferous - Ordovician unconformity in the Hetianhe Field and in the Tertiary in the Jinxian Sag took place at temperatures less than 80℃with sulphide δ~(34)S as light as -24.9‰ and -12.5‰, anhydrite δ~(34)S as heavy as +26‰and +3 5-+40‰, respectively. Chemistry and isotopic composition of the natural gases change as the result of sulphate reduction. It has been observed that relative composition of light hydrocarbon gases is changed along with a rise in H_2S and CO_2. TSR in the Triassic Jialingjiang Formation and BSR in the Hetianhe Field result in a greater degree of preferential depletion of methane than larger molecular hydrocarbon gases. As TSR or BSR proceeds, hydrocarbon gases evolved to heavier carbon isotope as the result of kinetic isotopic fractionation, i.e., selective anaerobic oxidation of ~(12)C. Using the model of residual methane (Whiticar, 1999) to describe the relationship among the proportion of methane oxidation, isotopic shift and fraction factor, about 30% methane is calculated to have been oxidized during BSR in the western part of the Hetianhe Field. From the above, it can be concluded that in the area where H_2S is abundant, empiricalδ~(13)C -Ro relationships do not work. Sulphate reduction results in a rise in sulphur content, gravity and viscosity of an oil as well as changes in δ~(13)C and δ~(34)S. On special conditions, the reduced sulphur from sulphates might be incorporated into oils, i.e., the increasing sulphur is derived from secondarily reduced sulphur. A positive correlative relationship exists between sulphur content and δ~(34)S in the oils in Paleozoic reservoirs in Central Tarim, indicating that enhanced sulphur is ~(34)S-enriched, originated from TSR. The Jinxian oil with the highest sulphur content has the lightest δ~(34)S, suggesting part of the sulphur in the oil is ~(34)S-depleted, originated from BSR. In the Jinxian oil with increasing sulphur content, asphaltenes shows higher content and more negative δ~(13)C, and saturates shows evidence of biodegradetion and a decreasing content and a positive δ~(13)C shift. Thus, asphaltenes have δ~(13)C values closer to saturates. All the above indicate that the reduced sulphur has been incorporated into biodegradated saturates to generate new asphaltenes with relatively light δ~(13)C of saturates. Thiols and thiophenes in natural gases in the Triassic Jialingjiang Formation may result from reaction of H_2S with hydrocarbon. In the Jialingjiang Formation hydrocarbon gases are dominated by methane thus have a high dryness coefficient and thiols are showed to be positively related to H_2S content, suggesting that the thiols may result from H_2S reaction with short chain hydrocarbons. In contrast, high thiophenes occur in wet gases in Jurassic reservoirs with their source rock from sulphur - depleted type I kerogen, indicating that thiophenes may be a product of reaction of H2S with longer chain hydrocarbons.

内陆湖沼相和近海沼泽相沉积环境煤中微量元素和矿物的对比研究—以辽宁北票、江西建新和桥头煤研究为例

Using knowledge of geology, geochemistry, coal petrology, mineralogy, by means of a variety of advanced measuring methods such as inductively coupled plasma mass spectrometry (ICP-MS), inductively coupled atomic emission spectrometry (ICP-AES), X-ray powder diffraction (XRD), scanning electron microscopy with energy-dispersive spectrometer(SEM-EDS), sequential chemical extract and density fractions, the characteristics of trace elements and minerals in Jurassic Beipiao coal mine under inland limnetic sedimentary environment and in late Permian Jianxin and Qiaotou coal mines under paralic swamp sedimentary environment were studied. Compared with the average concentration in the world bituminous coals, the Beipiao coal was characterized by relatively high contents of Sc, Ti, Cr, Co, Ni, Zn, Se, Sr, Zr, Y, Ba, REE and Th, and lower contents of V, Rb, Cd, Sn, Pb, Bi and U; while the Jianxin coal was relatively enriched in Li, Sc, Ga, Sr, Y, Nb, Sb, Th and U, with low concentration of Be, Co, Ni, Cu, Ge, Zr, Mo, Cd, Cs, Ba, Pb and Bi; and the Qiaotou coal was enriched in Li, Sc, Sr, Nb, Ta, Zr, REE, Hf, Th and U, with low concentration of Be, V, Co, Ni, Cu, Ge, Mo, Cd, Cs, Ba, Tl, Pb and Bi. The concentrations of Ca, Mg and K in Beipiao coal are higher than those in Jianxin coal and Qiaotou coal, while Fe, S and Ti in Beipiao coal are lower than those in Jianxin coal and Qiaotou coal. The proximate analysis of coal samples was carried out, which indicated that Beipiao coal was medium- to high- ash (5.92-60.68%) with low sulphur coal, and Jianxin coal and Qiaotou coal was medium to high ash (8.85-46.33%) with high sulphur. The reflectivity was measured, which explained that Beipiao coal belonged to high volatile bituminous coal, Jianxin coal was low volatile bituminous coal and Qiaotou coal was low volatile anthracite. Quantitative maceral analyses were studied. The characteristics of rare earth elements (REE) were investigated, which showed that the total contents of REE were higher than that of the world's average content. With the increase of coal's metamorphic grade, the total contents of REE decreased from 98.5 X 10"6 of Beipiao coal to 94.2 X 10"6 of Jianxin coal, and to 75.9 X 10"6 of Qiaotou coal, and 5Eu reduced which indicated that the element Eu depleted. The characteristics of REE was controlled by the metamorphic grade of coal. And REE were mainly absorbed in clay minerals in Beipiao coal samples, while in Jianxin and Qiaotou coal mines, REE were primarily related to clay mineral and pyrite. The variation of trace elements in vertical direction of coal seams was studied, and the results showed that different trace elements differed greatly. The correlation between trace elements and ash were determined. Four major trace elements (aluminium-silicates, sulphide, carbonate and phosphate) accounted for the occurrence and distribution of most elements studied were determined. Coal samples were separated by density fraction, which showed that Cr, Cu, Mo and Pb were closely related to inorganic matters mainly distributed in P >2.6 and dropped remarkably in the density fractions P <2.3 . The occurrences of Co, Cr, Ni, As, Se, Mo, U were studied directly and quantitatively using sequential chemical extract with six steps, which showed that Co. Ni, Mo and U were mainly in the form of mineral, and As, Se chiefly in the form of organic state, while Cr mostly in the form of organic state and mineral. Major mineral phases presented in the Beipiao coal were Kaolinite, illite, quartz, calcite, and small amount of siderite, barite. While major mineral phases in Jianxin and Qiaotou coal were pyrite, kaolinite, and small amount of marcasite, rutile, sphalerite. This is the first time that the chromite in the coal was discovered in China, which indicates that Cr occurrence appeared in the form of chromite. The ratio of Sr/Ba, Sr/Ca and V/Ni in Beipiao coal mine under inland limnetic is smaller than that of in Jianxin and Qiaotou coal mines under paralic swamp. The ratio of K/Na and Th/U of Beipiao coal mine is higher than that of Jianxin and Qiaotou coal mine, which proved that Beipiao coal was not affected by sea water and Jianxin and Qiaotou coal were affected by sea water. Trace elements such as Cr, Ni, Mo in minerals were analyzed by SEM-EDS. The factors controlling the enrichment of trace elements can be divided into syngenetic stage factors and epigenetic stage factors.

贵州喀斯特山区植物营养元素和碳、氮、硫同位素组成研究--以贵阳花溪杨中流域为例

喀斯特的面积分布很广，占全球总面积的10%。我国喀斯特面积占国土面积的13%，主要集中在我国的南方。而贵州喀斯特山区位于西南喀斯特地貌最集中成片分布的中心区，是我国乃至世界热带、亚热带喀斯特地貌连续分布面积最大、发育最强烈的高原山区。和非喀斯特地区相比，贵州喀斯特山区由于碳酸盐岩的特殊理化特性，造成土层浅薄、土被不连续、岩石裸露率高、持水量低，适生树种少、群落结构单一、植被生长极其缓慢，生态环境十分的脆弱。加之人类不合理的活动，使得喀斯特山区植被退化非常严重。因此，开展贵州喀斯特山区植物的营养元素和碳、氮、硫同位素的研究是为了更好的了解该区植被的营养元素状况、生理生态特性以及营养元素的生物地球化学循环，更好地为该区森林、植被的治理、恢复以及生态系统的保护等提供决策依据。本研究选择典型喀斯特山区作为研究点，并以非喀斯特山区为对照。研究喀斯特山区植物的营养元素含量水平、分布状态、变异特征以及营养元素之间的相互关系和碳、氮、硫的同位素组成的种间差异、生境差异特征以及时空变化特征进行了研究。主要得到以下几点认识： 1、植物的N、P、K、Ca、Mg、S的平均含量大于1000 μg∙g-1； Fe、Mn、Al的平均含量在100 μg∙g¬-1～1000 μg∙g¬-1之间；Zn、Sr的平均含量为10 μg∙g¬-1～100 μg∙g¬-1之间；Cu和Mo的含量小于10 μg∙g¬-1，Mo最低(仅为0.17 μg∙g¬-1)。Ca、P、K、 Fe、Mn、S、Sr高于所报道的陆生植物元素的含量；Mg低于陆生植物的元素含量；其它元素在元素含量范围内。植物营养元素的特点为Ca>K>Mg型，和我国其它地区相比，喀斯特山区植被具有高钙的特征。 2、N、P、K、Mg为正态分布；Ca、Al、Fe、Mn、Cu、Zn、Sr、Mo、S为对数正态分布。Al、Fe、Mn、Sr的变异系数大于100%；N、P、K、Ca、Mg、S、Cu的变异系数小于60%。其中，Ca的变异系数最小(为11.8%)。P和K、P和Cu、Al和Fe、Al和Zn、Fe和Zn之间具有极显著的相关关系；N和P、P和Mg、K和Al、K和Cu、Ca和Sr、S和Mo之间具有显著的相关关系。 3、不同的生境下植物营养元素存在差异，差异在2倍范围内。其中，Mn、Al、Sr元素差异较大，分别达到2.1、1.5、1.4倍。 4、植物δ13C、δ15N、δ34S值的分布范围分别为-26.98‰～-29.15‰、-4.08‰～-0.79‰、-8.69‰～-6.04‰；平均值分别为-28.14‰、-2.41‰、-7.53‰。δ13C除了高于我国热带雨林区植物外，均低于其它地区，且变化范围较窄；不同地区之间植物的δ15N、δ34S值存在较大差异。 5、不同植物种之间的δ13C、δ15N、δ34S值存在较大的差异，不同生境条件下植物的δ13C、δ15N、δ34S值也存在差异。植物的δ13C值从生长初期到末期有降低的趋势；δ15N、δ34S则无一定的变化规律，不同的植物种的季节变化不同。植物的δ13C、δ34S随海拔的升高而增大，但δ15N随海拔的升高而降低。