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371.
Risheg H Graham JM Clark RD Rogers RC Opitz JM Moeschler JB Peiffer AP May M Joseph SM Jones JR Stevenson RE Schwartz CE Friez MJ 《Nature genetics》2007,39(4):451-453
Opitz-Kaveggia syndrome (also known as FG syndrome) is an X-linked disorder characterized by mental retardation, relative macrocephaly, hypotonia and constipation. We report here that the original family for whom the condition is named and five other families have a recurrent mutation (2881C>T, leading to R961W) in MED12 (also called TRAP230 or HOPA), a gene located at Xq13 that functions as a thyroid receptor-associated protein in the Mediator complex. 相似文献
372.
373.
Information processing along the course of a visual interneuron. 总被引:1,自引:0,他引:1
Locust ocellar retinal cells are innervated by giant second order cells, 2 mm long, which show discrete zones of integration along their course, including a major zone in the axonal length of the neuron. The complex synaptic arrangements which exist between higher-order afferent and efferent cells and these second order cells along their course suggests that transmission takes place by the electrotonic spread of slow potentials. The size and accessibility of these visual interneurons offers a unique preparation for examining mechanisms of graded synaptic transmission. 相似文献
374.
New Giemsa method for the differential staining of sister chromatids 总被引:127,自引:0,他引:127
375.
喜马拉雅山中段达索普粒雪芯中夏季风和尘埃信号记录研究 总被引:8,自引:2,他引:6
通过粒雪芯δ^18O和主要离子(Ca^2+,Mg^2+,NH^+4,SO^2-4和NO^-3)的分析表明,该粒雪芯年平均积累量为0.75m水当量。粒雪芯中δ^18O和主要离子浓度的季节变化表明,达索普冰川中高精度的记录了现代夏季风和尘埃信号。夏季风期间降水中δ^18O值由“降水量效应”所控制,雪层中较低δ^18O值则代表了夏季风信号。亚洲中部干旱半干旱区的春季尘暴输入是造成粒雪芯中Ca^2+,Mg 相似文献
376.
传统的正向遗传学主要用于克隆表型或功能已确定的基因。转座子标签突变体可用随机标签法从带有活性转座子的自交后代中筛选得到,或用定向标签法从杂交一代中筛选得到,即用目的基因的隐性突变统合体与具高度活性转座号的统合体杂交,极大多数的FI个体为正常表型,但其中会有极少量的表现隐性性状的转庄子插入突变体。正向基因标签和克隆法在利用异源和低拷贝数品系时尤其有用。采用反向fCR或热不对称交替PCR(TAIL-PCR)且很容易从单拷贝或低拷贝数品系中获得插入于两侧的基因组序列。TAIL-PCR由三轮连续的半巢式PCR组成,所… 相似文献
377.
378.
影响林木种子贮藏的因素 总被引:6,自引:2,他引:4
Ben S P Wang J Dale Simpson 《南京林业大学学报(自然科学版)》2006,30(1):1-7
为了每年提供造林新需的具有生活力的种子及长期保存种质资源,贮藏种子是必要的手段。种子寿命具有遗传性,且因树种而异。种子的贮藏特性可以分成5类:正常型、亚正常型、温带顽拗型、热带顽拗型和中间型。种子含水量和贮藏温度是影响种子贮藏是否成功的两个最重要因素。但因树种及其贮藏特性不同,种子含水量和贮藏温度的最适值也不同。为了保持正常型和亚正常型种子的生活力,这类种子必须密封贮藏;但对顽拗型种子,因其需要保持种子的代谢活性及要进行有氧呼吸,则需要气体交换。 相似文献
379.
Peng Xing Bao-zhong Ma Peng Zeng Cheng-yan Wang Ling Wang Yong-lu Zhang Yong-qiang Chen Shuo Wang Qiu-yin Wang 《矿物冶金与材料学报》2017,24(11):1217-1227
Huge quantities of zinc leaching residues (ZLRs) generated from zinc production are dumped continuously around the world and pose a potential environmental threat because of their considerable amounts of entrained heavy metals (mainly lead). Most ZLRs have not been properly treated and the valuable metals in them have not yet been effectively recovered. Herein, the deep cleaning of a ZLR and recovery of valuable metals via a hydrometallurgical route were investigated. The cleaning process consists of two essential stages:acid leaching followed by calcium chloride leaching. The optimum conditions for extracting zinc, copper, and indium by acid leaching were a sulfuric acid concentration of 200 g·L-1, a liquid/solid ratio of 4:1 (mL/g), a leaching time of 2 h, and a temperature of 90℃. For lead and silver extractions, the optimum conditions were a calcium chloride concentration of 400 g·L-1, a pH value of 1.0, a leaching time of 1 h, and a temperature of 30℃. After calcium chloride leaching, silver and lead were extracted out and the lead was finally recovered as electrolytic lead by electrowinning. The anglesite phase, which poses the greatest potential environmental hazard, was removed from the ZLR after deep cleaning, thus reducing the cost of environmental management of ZLRs. The treatment of chlorine and spent electrolyte generated in the process was discussed. 相似文献
380.
The paleoflow direction of the basal conglomerate of the Changzhougou formation is obtained by the paleocurrent analysis of certain sedimentary structures, and the ancient sedimentary environment of the Qian'an Region is determined by observing the psephicity and gradation of gravel in conglomerate. The results show that the paleoflow direction is from northwest to southwest, and the paleocurrent data manifest a single-peak style in a rose diagram. The average paleoflow direction in the Qian'an region is 265°. The basal conglomerate is of littoral facies, and the sediments of conglomerates are mainly sourced from Shanhaiguan. 相似文献