A New Sauropod Dinosaur from the Late Cretaceous Gaogou Formation of Nanyang,Henan Province

A new sauropod dinosaur Baotianmansaurus henanensis gen. et sp. nov. from the Cretaceous Gaogou Formation of Neixiang, Henan Province is erected. It is characterized by somphospondylous presacral vertebrae; a highly-developed lamina system on the dorsal vertebrae; transverse process supported by four laminae; and the dorsal portion of the anterior centroparapophyseal lamina is bifurcated, with a small branch extending to the ventral surface of the prezygapophysis. It represents a new titanosauriform sauropod.     

黄河流域城市生态效率演化特征及门槛效应

基于非期望产出视角测度黄河流域城市生态效率,探讨2003—2017年黄河流域城市生态效率时空演化特征及资源禀赋的门槛效应。结果表明：① 黄河流域城市生态效率呈稳步上升态势,但全域和资源型城市表现出一定梯度效应,有两极分化现象;② 各城市生态效率总体呈东高西低、南高北低格局,并存在显著空间溢出效应,不同类型城市演化存在显著的时空惯性。③ 资源禀赋存在显著门槛效应,资源型城市生产性服务业集聚与生态效率呈“U”型关系,制造业集聚在跨过门槛值后会产生抑制作用,产业协同集聚则始终具有正向作用;非资源型城市资源禀赋会削弱生产性服务业集聚的促进作用,制造业集聚及产业协同集聚的影响跨过门槛值后不显著。     

大地震前后实测地应力状态变化及其意义——以龙门山断裂带为例

实测地应力状态在连续地震事件前后的变化特征,对于应用地应力实测数据探索开展地震预报等研究有重要意义,但一直以来缺少典型实例研究。以龙门山断裂带西南段的跷碛和映秀地区为研究区,利用该地区汶川地震前至芦山地震后获得的地应力实测数据,分析了表征地应力状态的特征参数在汶川和芦山地震事件前后变化特征,探讨了其对地震预报研究的意义。研究表明,跷碛地区地应力状态特征参数K_HV、K_Hh和μ_m变化表现为芦山地震后值（QQ-14）大于汶川地震前（QQ-99）,QQ-99结果大于汶川地震后值（QQ-09）,而主应力梯度系数变化为QQ-09>QQ-14>QQ-99;分析认为K_HV、K_Hh和μ_m变化规律能准确反映汶川和芦山地震事件前后跷碛地区构造应力场演化特征,而仅用主应力随深度变化梯度系数变化特征,不能完全准确地反映构造应力场调整变化情况;映秀地区,除K_Hh外,主应力随深度变化梯度系数、K_HV和μ_m均表现为汶川地震后结果大于震前,其变化反映的应力场调整变化特征需要补充数据检验;利用地应力状态参数变化规律开展地震预报探索研究时,长期的、可对比的高质量地应力测量数据是研究有所突破的关键。研究成果对于龙门山地区构造应力场和减灾防灾研究有重要意义,对于应用地应力数据探索开展地震预报研究等有参考价值。      

电子商务背景下县域物流的空间联系及其网络结构研究 ——以浙江省为例

互联网及移动互联网纵深拓展,电子商务随之发展壮大,县域物流的空间结构也加速演进,研究基于空间联系视角,通过引力模型、社会网络分析等方法刻画了浙江省县域物流空间联系特征及其网络结构,得出以下结论：① 空间联系网络的“核心-边缘”格局清晰,最大引力线核心区域结构较为稳定,边缘区的竞争演进仍在继续,而且空间联系格局层级性较为明显,浙北、浙东及浙中的网络复杂度稳步提升;② 物流空间联系势能的空间分布呈现从南到北逐渐集聚的趋势,与电子商务发展水平的空间拟合度较高;③ 物流网络多中心性格局演化呈稳定均衡化发展,在电子商务发展影响下,逐渐形成以杭州市辖区、宁波市辖区、义乌市、温州市辖区等为主导的四大县域物流圈。     

南秦岭勉略构造带中堂沟火山岩地球化学特征及其地质意义

通过对分布于勉略构造带中段三岔子西侧中堂沟地区的火山岩进行详实的野外地质剖面调查,发现其为一套绿片岩相浅变质火山岩,岩石组合以变安山岩为主,含有少量的变玄武岩和变英安岩,主体为钙碱性系列。岩石地球化学研究表明3类岩石均具有轻稀土富集型稀土配分曲线,并显示弱的Eu负异常;微量元素方面,岩石普遍富集大离子亲石元素Cs、Rb、Ba,亏损高场强元素Nb、Ta,相对亏损P、Ti,不活动微量元素Zr、Hf、Tb、Y等既无明显的相对亏损也无显著的相对富集。在La-La/Nb、Nb-Nb/Th和La/Yb-Sc/Ni等环境判别图解中,变玄武岩和变安山岩样品点均落在岛弧火山岩范围内,并结合其岩石组合特征指示该套火山岩应形成于大陆边缘弧(活动陆缘)环境。其中变玄武岩和变安山岩岩浆起源于楔形地幔的部分熔融,且有陆壳物质的参与;变英安岩的形成则与壳源物质的部分熔融有关。     

制图六体析读

西晋人裴秀的《制图六体》是研究中国古代测绘技术发展历程的重要历史文献资料。本文基于以往研究成果,结合裴秀编制《禹贡地域图》的基本方法和缘由,充分考量当时的测量技术发展水平,对《制图六体》进行了整体析读,在此基础上指出：作为六体核心的“准望”是中国古代所有精确测量的泛称,《制图六体》是以裴秀为代表的地图编绘者对地图测绘提出的基本要求总结,也是裴秀时代采用“计里画方”的绘图方法、利用区域地图结合文字考证绘制全域性地图的最好诠释。这一研究,补正了以往研究中的不足之处。     

一种改进的互复用调制方法

针对传统的互复用调制方法中,8种不同的输入信号组合值与6个不同相位量之间对应关系模糊的问题,提出了三码八相的互复用调制方法。基于三码八相互复用调制方法,利用与3路输入信号相关的指数因子,推导出了新的互复用基带调制信号表达式,实现了复用调制信号的相位翻转,得到了8个不同的相位值。仿真结果显示,三码八相互复用调制方法,保证了复用调制信号的恒包络特性,解决了输入码组合值与相位量之间对应关系的模糊度问题,研究结果对于GNSS组合中的信号调制有一定的参考价值。     

东昆仑南缘布青山构造混杂带哥日卓托洋岛玄武岩地球化学特征及构造意义

东昆仑南缘布青山地区哥日卓托一带出露一套洋岛玄武岩,主要由枕状玄武岩与杏仁状玄武岩组成,空间上与厚层-块状碳酸盐岩及薄层状硅泥岩相伴产出。详细的地质、地球化学特征研究表明,哥日卓托玄武岩SiO2质量分数为44.51%~48.43%,MgO为4.67%~6.99%,Na2O为1.74%~3.72%,TiO2为1.29%~1.85%,与拉斑玄武岩平均值相似。主量元素特征表明其主体属于亚碱性系列拉斑玄武岩,与冰岛拉斑玄武岩或夏威夷群岛喷发早期的拉斑玄武岩特征相类似。哥日卓托玄武岩∑REE为(68.71~133.50)×10-6,LREE/HREE为3.55~5.17,(La/Yb)N为3.07~5.32,稀土元素球粒陨石标准化配分曲线图呈现轻稀土元素富集右倾型。原始地幔标准化微量元素蛛网图表现出向上大隆起的富集形态。玄武岩微量元素判别表明其形成于洋岛构造环境。岩石成因研究表明陆壳物质对其混染的可能性较小,岩石成分主要受熔融源区控制,并估算其为由地幔源区1%~3%的尖晶石二辉橄榄岩部分熔融的产物。结合前人资料认为该套洋岛玄武岩形成于早石炭世,进一步证明布青山古特提斯洋石炭纪时很可能是一个北缘发育复杂被动大陆边缘而布青山地区发育深水洋盆、洋岛/海山遍布的有限洋盆系统。     

Ciliate Uronema marinum is the causative agent of scuticociliatosis in farm raised turbot Scophthalmus maximus

To identify the pathogen that causes scuticociliatosis in farmed-raised turbot Scophthalmus maximus , we isolated a ciliate from the brain tissue of an infected turbot and identifi ed it as Uronema marinum based on morphological and molecular evidence. We then infected the turbots in artifi cial laboratory settings with pure cultured U . marinum . The infected turbots showed syndromes similar to those observed in naturally infected ones. Furthermore, microscopic examination and PCR detection confi rmed the presence of the ciliate in the tissues of those laboratory-infected turbots. To our best knowledge, this is the fi rst report of scuticociliatosis caused by U . marinum in farm-raised turbot S . maximus in China.     

Distribution characteristics of lipids in hadal sediment in the Yap Trench

In this study, cored sediment samples collected by the Jiaolong Submersible at 6 779 m depth from the hadal zone of the Yap Trench in May 2016 were sliced in 1-cm interval from top to bottom, and lipids in each sediment layer were quantitatively and qualitatively analyzed. The vertical distribution profiles of the lipids in the sediment sample, their main existing forms, and their possible sources were investigated. The results show that the concentration of lipid in the surface sediment was the highest with the carbon number from 12 to 27, dominated by medium and short-chain lipids. The total concentration of fatty acids in surface sediment was much higher than those in the offshore and deep-sea areas, being up to 325.77 μg/g due to the funnel effect caused by the “V” terrain of the trench. Fatty acid 18.0 was the most abundant lipids in the sediment sample. Abnormal high concentrations of fatty acid 18.ω7 and alkanes indicated the existence of hydrothermal fluids in the study area. In addition, saturated fatty acids and monounsaturated fatty acids existed mainly in free form, and polyunsaturated fatty acids existed mainly in bound form. Most of the alkanes were in bound form, and their major source was autochthounous input. The carbon number of alcohols in the sediment sample ranged from 12 to 20, mainly existed in bound form. The source of fatty acids was mainly autochthonous input, and the neutral lipids had both marine and terrestrial origin. This is the first study of lipids in hadal sediment of the Yap Trench. The results will promote deeper understanding of organic carbon cycle in marine environment.