Revision of “Parahagla lamina” Lin, 1982 and two new species of Aboilus (Orthoptera: Prophalangopsidae) from the EarlyMiddle Jurassic of Northwest China

The Lower and Middle Jurassic insects are rather poorly known from Northwest China. Here we restudy Parahagla lamina Lin, 1982 and transfer it from “Parahagla” to Aboilus Martynov, 1925. On the basis of the female forewing, we described two new species of the EarlyMiddle Jurassic, Aboilus tuzigouensis sp. nov. caome from Badaowan Foramtion at Tuzigou, Kelamayi, Xinjiang, Northwest China and A. jiyuanensis sp. nov. from Ma’ao Group, Jiyuan, Henan Province, Central China. The differences of the new materials from the other known species and their systematic positions are also discussed.     

Radiometric dating of sediments derived from metamorphic rocks of the Dabie orogenic belt in the Jurasic and Early Cretaceous

Using isotopic dating of tuff, heavy mineral and lithofacies, correlation of Jurassic strata on the northern margin of the Dabie orogenic belt (DOB) has been enabled in the Fenghuangtai, Zhougongshan, Maotanchang and Jingangtai formations, which might be as young as Early Cretaceous. Depositional systems have been interpreted as mainly alluvial fan, braided stream and overbank, secondarily fan-delta and lacustrine. The palaeocurrent systems of the Jurassic-Cretaceous basins can be divided into two classes: one transverse adjacent to the southern margin, the other longitudinal close to the middle flowing from west to east. Mesozoic sedimentary source rocks are mainly from the DOB and, according to their geochemistry, experienced evolution in a volcanic arc tectonic setting. The Jurassic-Cretaceous strata have been subdivided into four Chronosomes, and their overlapping progressively from east toward west implies that exhumation of the DOB characterized diachronous. Based on stratigraphic evidence from eclogite conglomerates found in the Maotanchang and Fenghuangtai formations, the first exposure of UHP (ultrahigh pressure) rocks in the DOB occurred in Jurassic-Lower Cretaceous time. Further, phengites and Triassic zircons found in the Lower Jurassic Fanghushan Formation suggest that denudation began in the Early Jurassic.     

谈社会心理对晚清翻译作品的影响

翻译不能脱离人而存在，而人是社会的人，必然要经历一个社会化的过程。所以，译本出现的过程中一定会受到社会心理因素的影响。本文选取晚清时期的翻译作品，阐述了翻译过程中社会心理因素对译本的塑造。     

评明清之际李闯时事小说中的文人思考

明末清初,一些文人纷纷以现实政治大事为题材,写作时事小说。这是中国文学史上的第一次。拟就李自成系列时事小说作分析,探讨这些身处鼎革的作者们,如何借小说以表达他们的关注与思考。     

准噶尔盆地阜北地区头屯河组砂岩自生绿泥石特征

自生绿泥石是砂岩储层中常见的成岩矿物.为了完善碎屑岩储层黏土矿物研究成果,并对准噶尔盆地阜北地区侏罗系头屯河组油气勘探提供地质依据,通过岩心采样观察、铸体薄片、扫描电镜、X射线衍射、核磁共振等测试分析手段,对阜北地区头屯河组砂岩储层中自生绿泥石胶结物的产状及其对储层物性的影响进行了研究.结果表明:头屯河组砂岩储层常见自生绿泥石胶结,形成于早成岩阶段早期,主要以孔隙衬里式胶结产出.头屯河组自生绿泥石包膜对于提高岩石的机械强度和抗压实能力有限,只有当自生绿泥石环边呈连续分布且有一定厚度时,才能抑制石英的次生加大;在保留更多原生孔隙的同时,也堵塞孔喉,导致储层渗透率降低.头屯河组自生绿泥石薄膜厚度临界值为8 μm,当厚度＜8μm时,随着自生绿泥石薄膜厚度增大,对压实作用的减缓能力越强,储层物性越好;一旦厚度＞8μm,自生绿泥石薄膜厚度与储层物性呈明显负相关,不利于储层发育.     

Late Neogene radiolarian absence event in the southern South China Sea and its paleoceanographic implication

Down-core variations of radiolarians at ODP Site 1143 in the southern South China Sea （SCS） are presented for the last 12 Myr. The fluctuations of radiolarian abundances since the Late Miocene can be divided into three stages： a high abundance stage at 12-5.96 Myr, a radiolarian absent stage at 5.96-3.30 Myr and a gradual increasing stage after 3.30 Myr. The three stages correspond to the forming and vicissitudes of the Western Pacific Warm Pool （WPWP） and the Eastern Asian Summer Monsoon （EASM）. The radiolarian absence event （RAE） was also absent of diatom and occurred nearly simultaneously with the closures of the Panama Isthmus and the Indonesian seaway, which probably caused the reorganization of oceanic circulation systems. Accompanied this circulation reorganization was the weakening of the WPWP and the EASM, which probably led to a weakened upwelling in the southern SCS. In addition dissolved silica （Dsi） content in surface seawater might be very low during 5.96-3.30 Myr due to the ＂biogenic bloom＂ event, which consumed a large amount of Dsi in the surface seawater. All these factors together might lead to a great decrease of siliceous production in the southern SCS and consequently caused the RAE. Moreover, the dissolution of siliceous skeletons might also influence the abundance of radiolarians.     

Late Neogene radiolarian absence event in the southern South China Sea and its paleoceanographic implication

Down-core variations of radiolarians at ODP Site 1143 in the southern South China Sea (SCS) are presented for the last 12 Myr. The ?uctuations of radiolarian abundances since the Late Miocene can be divided into three stages: a high abundance stage at 12–5.96 Myr, a radiolarian absent stage at 5.96–3.30 Myr and a gradual increasing stage after 3.30 Myr. The three stages correspond to the forming and vicissitudes of the Western Paci?c Warm Pool (WPWP) and the Eastern Asian Summer Monsoon (EASM). The radiolarian absence event (RAE) was also absent of diatom and occurred nearly imultaneously with the closures of the Panama Isthmus and the Indonesian seaway, which probably caused the reorganization of oceanic circulation systems. Accompanied this circulation reorganization was the weakening of the WPWP and the EASM, which probably led to a weakened upwelling in the southern SCS. In addition dissolved silica (Dsi) content in surface seawater might be very low during 5.96–3.30 Myr due to the ‘‘biogenic bloom” event, which consumed a large amount of Dsi in the surface seawater. All these factors together might lead to a great decrease of siliceous production in the southern SCS and consequently caused the RAE. Moreover, the dissolution of siliceous skeletons might also in?uence the abundance of radiolarians.     

鄂尔多斯盆地吴起王洼子地区早侏罗世沉积微相及古地貌恢复

应用印模法恢复的王洼子地区前侏罗纪古地貌主要由古河道、斜坡脊和沟组成.前侏罗纪古地貌控制着早侏罗世的沉积,延10期为辫状河亚相河道砂坝、泛滥平原,延9期为三角洲平原亚相分支河道、漫滩沼泽.研究区总体受西北物源的控制,发育北西--南东向的河道砂体.分析了侏罗系沉积前古地貌与延10、延9的成藏关系,认为油藏主要分布于紧邻高地的斜坡等地势相对较高的地带.河道砂体的发育控制着油藏的形成和分布,勘探区大面积位于古地貌的斜坡位置,北部的古河道下切河谷为延长组油气向上运移的通道.研究区侏罗系油藏发育,下一步勘探重点为前侏罗纪斜坡脊与延9、延10河道砂体的叠合区.     

Newly discovered Palaeolithic artefacts from loess deposits and their ages in Lantian,central China

Eight new Palaeolithic open-air sites were identified and 770 stone artefacts were collected from 2009 to 2011 in the Lantian area of the Bahe River valley, central China. Because the famous Homo erectus fossils were unearthed at the Gongwangling and Chenjiawo localities, and more than 30 Palaeolithic open-air sites were investigated in the 1960s in this region, the catchment of Bahe River is regarded as one of the most important hominin sites from the late early Pleistocene to the middle Pleistocene. These eight newly discovered open-air sites are located at the second(n = 6), third(n = 1) or higher terraces(n = 1) of the Bahe River. The Diaozhai section on the second terrace was sampled in detail. Two samples were collected for optically stimulated luminescence dating(OSL). The OSL results suggest that a buried lithic artefact layer at the Diaozhai site spans approximately 70–30 ka. The lithic assemblage analysis suggests that the stone artefacts were made of local pebbles/cobbles such as greywacke, quartz, sandstone and igneous rocks. The main percussion techniques that were used were direct hard hammer percussion and bi-polar techniques. The lithic artefacts comprise hammer stones, cores, flakes, retouched tools and flaking debris. Acheulian-type large cutting tools(LCTs) such as hand-axes, picks and cleavers were indentified in the Lantian region as well. This is the first time Acheulian-type LCTs from the late Pleistocene have been identified in this region. This study distinguishes age gaps between Western world and East Asian Acheulian-type tools.