CdTe/ZnS 量子点荧光可逆调控研究ctDNA 与吡柔比星的相互作用

水相合成了谷胱甘肽修饰的CdTe/ZnS 量子点(GSH-CdTe/ZnS QDs). 从原子力显微镜照片可以看出, 合成的核壳型GSH-CdTe/ZnS QDs 具有良好的分散性. 当吡柔比星与GSH-CdTe/ZnS QDs 相互作用时, 吡柔比星吸附在GSH-CdTe/ZnS QDs 的表面, 通过光诱导电子转移的方式猝灭GSH-CdTe/ZnS QDs 的荧光. 然后向GSH-CdTe/ZnS QDs-吡柔比星体系中加入ctDNA, 吡柔比星从GSH-CdTe/ZnS QDs 表面脱落后嵌入ctDNA 双螺旋结构中, 光诱导电子转移过程被阻断, GSH-CdTe/ZnS QDs 的荧光恢复. 根据GSH-CdTe/ZnSQDs 荧光的猝灭和恢复, 实现了量子点荧光的可逆调控. 结合共振瑞利散射和紫外吸收光谱, 讨论了GSH-CdTe/ZnS QDs 吡柔比星-ctDNA 的相互作用机理, 建立了一种研究蒽醌类抗癌药物与核酸相互作用的光谱方法.     

空气中低浓度铅对女工生殖机能影响的调查

目的：研究长期暴露在低铅环境下女工生殖机能是否受到影响。方法：单盲法问卷调查。结果：在空气铅浓度为0．035～0．048mg／m3作业环境中工作，接铅作业女工的月经先兆症状以及痛经、团经的发生率明显高于非铅作业女工（P＜0．05）。结论：空气中低浓度铅对女工生殖机能有一定影响。     

基于全局注意力引导的肺结节分割方法

肺结节的精确分割能有效地辅助医生的治疗诊断工作,但由于不同患者所呈现的肺结节病灶形式多种多样,基于传统专家系统和统计学习的方法难以获得准确的肺结节分割结果。针对这种情况,提出一种由全局注意力引导的注意力机制,达到了从一张完整的胸部影像切片中自动定位并分割出肺结节的效果。该方法首先对目标区域进行肺实质分割,再利用区域建议网络（region proposal network,RPN）进一步缩小感兴趣区域,并生成注意力权重图,最后使用融合了残差网络（residual network,ResNet）与卷积长短期记忆网络（convolutional long short-term memory,ConvLSTM）的结构结合注意力权重进行肺结节分割。将所提方法在肺图像数据库联盟（lung image database consortium,LIDC-IDRI）数据集上进行了全面的评估,结果表明,本文方法分割结果的平均dice得分（标准差）为89.97%（8.9%）,具有出色的分割性能,精度相较其他方法取得一定提升。进一步在相同数据集上将所提方法的肺结节分割结果与4位放射科医生的手工标注结果进行了比较,结果表明本文方法的分割结果与医生们的标注结果的一致性达到了85.81%,相较于医生们手工标注之间的一致性高出了3.39%。     

Petrogenesis of Aoyougou high-silica adakite in the North Qilian orogen, NW China: Evidence for decompression melting of oceanic slab

A trondhjemitic body occurs in the Aoyougou area,the western part of the North Qilian orogen.It is geochemically characterized by high SiO 2,Na 2 O (high Na/K),elevated Sr/Y and (La/Yb) N,positive Sr anomaly,relatively enriched large ion lithophile elements (LILEs) and light rare earth elements (LREEs),and depleted Nb,Ta,Ti,resembling the high-silica adakite.Zircon U-Pb SHRIMP dating yields a weighted mean age of 438±3 Ma.This age is significantly younger than eclogitization ages of 460-490 Ma in the North Qilian orogen,suggesting that formation of the adakite postdates the subduction of oceanic crust in association with closure of the ancient Qilian Ocean.Whole-rock Sr and Nd isotopic analyses give initial ratios of I Sr =0.7044 0.7047 and Nd (t)=3.0 4.1,indicating that they are derived from partial melting of the juvenile oceanic crust.In view of the tectonic evolution of the North Qilian orogen,the high-silica adakite was probably derived from decompression melting of the exhumed eclogite at the depth of ～60 km.     

Occurrence of Neoproterozoic low-grade metagranite in the western Beihuaiyang zone,the Dabie orogen

Based on detailed field investigations and petrographic observations, we discovered Neoproterozoic-emplaced granite from the metavolcanics of the Dingyuan Formation in the western Beihuaiyang zone, the Dabie orogen. This study reports the results of zircon U-Pb dating and preliminary petrographic observations on two metagranite samples. The studied rocks experienced epidote-amphibolite facies metamorphism and strong structural deformation. Their U-Pb ages are 726 ± 6 and 758 ± 12 Ma, respectively, similar to those for the Luzhenguan complex in the eastern segment of the Beihuaiyang zone. In combination with previously determined 635 ± 5 Ma low-grade metagabbro, this study suggests the occurrence of at least two types of Neoproterozoic intrusive rocks in the Beihuaiyang zone, the northern margin of the South China Block (SCB): 726–758 Ma metagranite and 635 Ma metagabbro. These rocks occur within the metamorphosed Ordovician volcanic zone (originally named the Dingyuan Formation) and are in tectonic contact to each other, but they formed in different tectonic settings. The protolith ages for the Neoproterozoic low-grade metaigneous rocks are in good agreement not only with ages for two episodes of mid- and late-Neoproterozoic mafic and felsic magmatism in the Suizhou and Zaoyang area, Hubei Province, but also agree with protolith ages of ultrahigh-pressure metaigneous rocks in the Dabie-Sulu orogenic belt. In view of their tectonic relationships to country rocks, it appears that these Neoproterozoic low-grade rocks are exotic and they may have been detached and scraped from subducting SCB crust in the early Triassic during the initial continental subduction, and thrusted over Paleozoic metamorphosed rocks in the southern margin of the North China Block during continental collision.     

Phylogenetic relationships and divergence times of the family Araucariaceae based on the DNA sequences of eight genes

Araucariaceae is one of the most primitive families of the living conifers, and its phylogenetic relationships and divergence times are critically important issues. The DNA sequences of 8 genes, i.e., nuclear ribosomal 18S and 26S rRNA, chloroplast 16S rRNA, rbcL, matK and rps4, and mitochondrial coxl and atpl, obtained from this study and GenBank were used for constructing the molecular phylogenetic trees of Araucariaceae, indicating that the phyiogenetic relationships among the three genera of this family should be （（Wollemia, Agathis）, Araucaria）. On the basis of the fossil calibrations of Wollemia and the two tribes Araucaria and Eutacta of the genus Araucaria, the divergence time of Araucariaceae was estimated to be （308± 53） million years ago, that is, the origin of the family was in the Late Carboniferous rather than Triassic as a traditional view. With the same gene combination, the diver- gence times of the genera Araucaria and Agathis were （246 ± 47） and （61 ±15） Ma, respectively. Statis- tical analyses on the phylogenetic trees generated by using different genes and comparisons of the divergence times estimated by using those genes suggested that the chloroplast matK and rps4 genes are most suitable for investigating the phylogenetic relationships and divergence times of the family Araucariaceae.     

Petrochemical characteristics of leucogranite and a case study of Bengbu leucogranites

Leucogranites have a relatively narrow variation in SiO2 content （70.5%-75.5%）. Giving similar SiO2 content, leucogranites have relatively higher Al2O3 （〉13.5%） and lower TFeO ＋ MgO （〈2.5%） contents than those of normal granites. These petrochemical characteristics suggest that leucogranites are de- rived from partial melting at relatively low temperature and are not significantly affected by fractional crystallization. In the present study, we propose that the Al2O3 vs SiO2 and TFeO ＋ MgO vs SiO2 dia- grams can be used to distinguish leucogranites from normal granites. In addition, we report the major element compositions of the Jurassic granitic intrusions from Jingshan-Tushan-Mayishan in the Bengbu area, east-central China. Using the Al2O3 vs SiO2 and TFeO ＋ MgO vs SiO2 diagrams and the comparison with the High Himalayan leucogranites in mineralogical and petrochemical characteristics, we suggest that the Jingshan-Tushan-Mayishan intrusions belong to a leucogranite belt. Similar to those of the High Himalayan leucogranites, the Bengbu leucogranites have low Mg# values, indicating that they resulted from low temperature dehydration partial melting of the subducted continental crust of the South China Block at the crustal depth.     

The geological characteristics of oceanic-type UHP metamorphic belts and their tectonic implications: Case studies from Southwest Tianshan and North Qaidam in NW China

The geological characteristics of ultrahigh-pressure （UHP） metamorphic belts formed by deep subduction of oceanic crust are summarized in this paper. Oceanic-type UHP metamorphic belt is characterized by its protolithlc assemblage of typical oceanic crust, the peak metamorphic temperature 〈600℃, P-T path undergoing blueschist facies during prograde and retrograde metamorphic evolution, reepectively, with low geothermal gradient of cold subduction. The further study of oceanic-type UHP metamorphic belt is very significant for constructing metamorphic reaction series of cold subduction zone, for understanding how aqueous fluids were transported into deep mantle and for classifying the types of UHP metamorphism in cold subduction zone. The uplift and exhumation mechanism of oceanic UHP metamorphic rocks is one of the most challenging problems in the study of UHP metamorphism, which is very important for understanding the geodynamic mechanism of solid Earth. As a traveler eubducted into the mantle depth end then uplifted to the surface, oceanic-type UHP metamorphic belts witness the bulk process from the subduction to exhumation and is an ideal target to study the geochemical behavior end cycling of elements in subduction zones. The tectonic evolution of one convergent orogenic belt can be usually divided into two stages of oceanic subduction and followed continental subduction and collision, and the two best-established examples of orogenic belts are Alpa and Himalaya. Therefore, the study of oceanic-type UHP metamorphic belt is the frontier of the current plate tectonic theory. As two case studies, the current status and existing problems of oceanic-type UHP metamorphic belts in Southwest Tianshan and North Qaidam, NW China, are reviewed in this paper.     

我国典型湖泊磷浓度对水体指标及蓝藻水华爆发趋势的潜在影响——基于Meta分析

水体富营养化可引发蓝藻水华,对水生态环境和饮用水的安全产生严重危害,揭示蓝藻水华的发生机理和变化规律是防治的基础。基于1989—2019年公开发表的相关研究,提取583对有效数据,利用Meta分析了我国典型湖泊中磷浓度对水体指标及蓝藻水华爆发趋势的影响。结果表明：磷浓度对水体透明度（SD）产生负效应,对溶解氧（DO）含量、高锰酸盐指数（COD_Mn）和叶绿素a （Chla）含量产生正效应。随着磷浓度的增加,上述4种指标呈现不同的变化趋势：磷浓度对DO含量的正效应逐渐转变为负效应,在磷的质量浓度为0.2~0.3 mg/L时负效应最大（亚热带季风气候）;对SD的负效应随磷浓度的增加先增大后略有减小,在磷的质量浓度为0.1~0.2 mg/L时负效应最大;COD_Mn和Chla含量对磷浓度的响应趋势基本相似,在亚热带季风气候条件下,磷的质量浓度分别为0.2~0.3 mg/L和>0.3 mg/L时二者的正效应最大。此外,与温带季风气候地区相比,在磷的质量浓度为0~0.1 mg/L时亚热带季风气候地区的湖泊水质更容易受磷浓度的影响,蓝藻水华爆发的风险相对较高。     

<Superscript>40</Superscript>Ar/<Superscript>39</Superscript>Ar isochron ages of lawsonite blueschists from Jiuquan in the northern Qilian Mountain,NW China,and their tectonic implications

Using laser ⁴⁰Ar/³⁹Ar dating method, we have gotten the metamorphic ages of lawsonite blueschist and epidote blueschist from Jiuquan, northern Qilian Mountain, NW China. The high quality laser ⁴⁰Ar/³⁹Ar dating of glaucophane from lawsonite blueschist gives an isochron age of 413±5 Ma. The isochron age obtained from phengite in epidote blueschist is 415±7 Ma. These data, combining with peak metamorphic P-T conditions and regional geological setting, allow us to infer that the lower limit of the ages of the prograde subduction metamorphism from lawsonite blueschist facies to epidote blueschist facies occurred at ca. 413–415 Ma, which also suggests that the formation of lawsonite blueschist in the northern Qilian Mountain maybe resulted from the corner flow in the cold subduction zone. This study shows that the final closing time of the northern Qilian remnant oceanic basin is about 413–415 Ma, which also represents the convergent age between the North China Craton and the Qaidam block.