辽宁西部早白垩世朝阳翼龙科 (Chaoyangopteridae)化石一新种

中国辽宁西部早白垩世翼龙类化石非常丰富,其上部的九佛堂组翼龙类组合以含有丰富的无齿的古神翼龙科、朝阳翼龙科等进步类型而与下部的义县组翼龙类组合相区别。本文描述了辽宁西部建昌盆地九佛堂组一新的大型翼龙类化石,其以上下颌无齿、吻端指数为3.7、前颌骨背支细长且封闭鼻眶前孔背缘、很大的鼻眶前孔后端超过上下颌关节位置、轭骨的上颌骨突基部宽大而应被归入朝阳翼龙科(Chaoyangopteridae)神州翼龙属(Shenzhoupterus)。其以较大的体形(翼展2.05 m)、平直的上下颌咬合面、轭骨的眶后骨突较泪骨突长且基部略宽、第4～7颈椎长度依次减小等特征,区别于朝阳神州翼龙(Shenzhoupterus chaoyangensis),而被命名为三亚神州翼龙(新种)(Shenzhoupterus sanyainus sp. nov.)。这是辽宁西部早白垩世翼展最大且不具牙齿的翼龙类属种,它的发现丰富了九佛堂组翼龙类组合内容,对认识朝阳翼龙科的骨骼形态与生态习性亦具有积极意义。     

直脉蝎蛉科(昆虫纲长翅目) 3个异物同名和 1个种的修正

1996 年,张海春发表《新疆准噶尔盆地中生代直脉科(昆虫纲)昆虫化石》一文[古生物学报,35(4)：442-494],共有5个新种和5个老种,其中1个老种定为Mesopanorpa obscura(Martynov, 1927),包含3 个标本：① NIGP126378(92-T-22/K1),② NIGP126377(58SK15/K3),③ NIGP126376(92-T-22/K3)。另1个标本NIGP126379(93-HE-2K1,2)定为Protorthophlebia latipennis Tillyard, 1933。笔者在研究长翅目化石的过程中,发现张的4个标本系异物同名,前3 个标本即：① NIGP126378号标本勉强修订为1个近似种P. (Protorthophlebia) aff. obscura (Martynov,1925) Martynov,1927;② NIGP126377号标本修订为新名种Protorthophlebia(Protorthophlebia) badouwanica nom. nov.;③ NIGP126376号标本, 由于这个标本脉序结构与副蝎蛉科 Parachoristidae Tillyard, 1937的脉序特征相同,已被修订为另一个属、种Junggarochorista tuzigouensis Hong, 2009[13],已转移归入该科。④另1个标本NIGP126379号标本被修订为新名种 P.(Protorthophlebia) karamayiensis nom. nov.。上述被修订后的新名属、种在本文中作了必要的重新描述。修订的标本,都根据张海春论文中原标本照片显示的脉纹特征和文字描述。所修订学名的原标本均按原文的记录保存在中国科学院南京地质古生物研究所。     

科左后旗土地利用与资产管理问题之我见

本文通过对科左后旗土地利用现状及土地利用特点进行阐述和分析,总结了科左后旗土地利用与资产管理中存在的问题,地广人稀土地质量不高、房地产整体结构单一、持续发展阻力增加、土地利用总体规划与城市总体规划及相关规划衔接不够完善、城镇建设供给引导需求的机制没有建立起来、资源开发利用过程中对环境的破坏与可持续发展之间的矛盾,依据目前状况从六个方面对加强土地资产管理进行了建议。     

在子科滩草原上捡拾阳光

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中国海真寄居蟹属一新记录种(寄居蟹总科,活额寄居蟹科)

本文记述了采自中国南沙及北部湾的活额寄居蟹科Diogenidae真寄居蟹属Dardanus Paul’son 1新纪录种:丽螯真寄居蟹D.callichela Cook,1989。提供了形态描述、形态特征图及分种检索表,并讨论了其与近似种的区别。研究标本保存于中国科学院海洋生物标本馆(MBMCAS)。     

中国近海蟹守螺科(Cerithiidae)两新纪录种及常见种名修订

在系统整理研究中国科学院海洋研究所历年来在中国近海采集的蟹守螺科标本时,鉴定出属于蟹守螺属(Cerithium)的中国两新记录种,分别是:阶梯蟹守螺Cerithium novaehollandiae Adams in Swoerby,1855和锉形蟹守螺Cerithium scobiniforme Houbrick,1992。两新记录种分布于中国海南省沿海,栖息于潮间带至浅海的岩礁、砂或石砾质海底。文中对两新记录种的外部形态、软体部、厣特征和习性及地理分布等方面进行了论述,并与相似种进行了比较。且对中国近海蟹守螺科一些常见种名进行了修订。     

Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary

Distributions of the parameters of sedimentary grain sizes and their correlations were studied to trace the sources of silts and their movement trends in the Zhujiang River Estuary based on the analyses of grain sizes from more than 1080 sedimentary samples. The distributions of the median diameter, public value, quartile deviation, and skewness of sediments were complex in the Zhuiiang River Estuary mainly because of the impact of the matter source regions, distances from the source regions, and hydrodynamic conditions, such as waves, tidal currents, and coastal currents. Analyses of the parameters of the grain sizes for the various types of sediments showed that the distributions of the surface sediments in the Zhujiang River Estuary were controlled by many factors. Their matter sources were mainly the sediments discharged from the runoffs and ebb tidal currents, and from the open sea. The sediments mainly moved by suspension movement. The silts formed a large area of sediments with suspended fine silts in the Zhujiang River Estuary by internal adjustment transportation in the area, and moved toward the western coast of the Zhujiang River Estuary under the effect of Coriolis forces and coastal currents.     

表面波浪对海洋上层混合的作用

A new three-dimensional numerical model is derived through a wave average on the primitive N-S equations, in which both the＂Coriolis-Stokes forcing＂ and the＂Stokes-Vortex force＂ are considered. Three ideal experiments are run using the new model applied to the Princeton ocean model （POM）. Numerical results show that surface waves play an important role on the mixing of the upper ocean. The mixed layer is enhanced when wave effect is considered in conjunction with small Langmuir numbers. Both surface wave breaking and Stokes production can strengthen the turbulent mixing near the surface. However, the influence of wave breaking is limited to a thin layer, but Stokes drift can affect the whole mixed layer. Furthermore, the vertical mixing coefficients clearly rise in the mixed layer, and the upper ocean mixed layer is deepened especially in the Antarctic Circumpolar Current when the model is applied to global simulations. It indicates that the surface gravity waves are indispensable in enhancing the mixing in the upper ocean, and should be accounted for in ocean general circulation models.     

新疆库车盆地钾盐科探1井含盐系地球化学特征及找钾指示

在盐湖沉积演化过程中,钾盐矿物在盐类沉积的中晚期阶段才开始析出。因此,研究含盐系盐类的沉积地球化学特征,不仅可以从侧面获取岩盐的沉积物源和成盐古卤水蒸发浓缩程度等地球化学信息,而且更能揭示古盐湖钾盐富集趋势。文章通过对库车盆地钾盐科探1井钻取的岩芯样品进行高精度采样测试,得出岩盐中Mg×103/Cl、K×103/Cl、Li×103/Cl与K+、Mg2+、Li+、Ca2+、Cl-含量的垂向变化规律。并与库车盆地其他钻孔中的岩盐含钾性进行对比,同时,依据钻井剖面岩性特征,与潜江凹陷和大汶口凹陷含盐系剖面进行对比,论述研究区成盐的地球化学特征,对其钾盐成矿前景进行分析和评价。     

核心素养视角下新旧版《普通高中地理课程标准》比较研究

地理课程标准是地理课程改革的核心引擎。通过比较分析《普通高中地理课程标准(2017年版2020年修订)》与《普通高中地理课程标准(实验)》文本中地理学科核心素养相关“关键词”的特征,揭示它们在词频和分布方面的异同。研究表明:地理学科核心素养是三维目标的整合与创新,新课标构筑起正确价值观和地理思维的双重价值取向,更加突出以地理核心知识聚合课程内容和以地理实践力引领课堂教学。在新课标指引下,教师应以地理核心知识统整地理课程,采用地理信息技术发展学生地理思维,以地理实践活动革新地理教学手段和内容。