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| 1 | Re-Os isotope dating of molybdenites in the Huang-shaping Pb-Zn-W-Mo polymetallic deposit, Hunan Province, South China and its geological significance显示文摘The large-scale Huangshaping Pb-Zn-W-Mo polymetallic deposit is located in the central Nanling min- eralization zone, South China. Six molybdenite samples from the Huangshaping deposit were selected for Re-Os isotope measurement in order to define the mineralization age of the deposit. It yields a Re-Os isochron age of 154.8±1.9 Ma (2σ ), which is in accordance with the Re-Os model ages of 150.9― 156.9 Ma. This age is about 7 Ma younger than their host granite porphyry, which was dated as 161.6±1.1 Ma by zircon U-Pb method using LA-ICPMS. All these ages demonstrate that the Huang- shaping granite and related Pb-Zn-W-Mo deposit occurred in the middle Yanshanian period, when many other granitoid and related ore deposits emplaced and formed, e.g. the Qitianling granite and Furong tin deposit, the Qianlishan granite and giant Shizhuyuan W-Sn-Mo-Bi deposit and Jinchuantang Sn-Bi deposit in the nearby area. They constitute the main part of the magmatic-metallogenic belt of southern Hunan, and represent the large-scale metallogeny in middle Yanshanian in the area. The lower rhenium content in molybdenite of Huangshaping deposit suggests that the ore-forming material was mainly of crust origin. | YAO JunMing HUA RenMin QU WenJun QI HuaWen LIN JinFu DU AnDao | 2007 | Science China Earth Sciences2007，50，4： | 29 |
| 2 | Ecological evolution across the Permian/Triassic boundary at the Kangjiaping Section in Cili County, Hunan Province, China显示文摘The stratigraphic sequence of calcimicrobialite facies at the Permian-Triassic (P/Tr) boundary has well recorded the biotic and environmental transition across the end-Permian catastrophic events. The biostratigraphy, microfacies, carbon isotopes, and fossil records across the P/Tr boundary have been studied at the Kangjiaping Section in Cili County, Hunan Province. Three biostratigraphic zones, Palaeofusulina-Colaniella Zone, Hindeodus parvus Zone, and Isarcicella staeschei Zone, are identified. The excursion of δ13Ccarb exhibits a sharp negative shift in the calcimicrobialite at the P/Tr boundary, which is roughly accordant with the abrupt bioclastic decline. In addition, five types of microfacies are recognized, including algal-foraminifer bioclastic limestone, algal-laminated calcimicrobial limestone, oolitic grainstone, vermiculate limestone, and intraclastic wackstone. The results indicate that the changeover of ecosystem from metazoan reef to calcimicrobialite in Cili is a classic case of marine ecological evolution during the Paleozoic-Mesozoic transition. | WANG QinXian TONG JinNan SONG HaiJun YANG Hao | 2009 | Science China Earth Sciences2009，52，6： | 14 |
| 3 | Rhenium-osmium isotope constraints on the age and source of the platinum mineralization in the Lower Cambrian black rock series of Hunan-Guizhou provinces, China显示文摘The shale at the bottom of the Lower Cambrian black series in South China is rich in nonferrous metals, noble metals, rare and dispersed elements and radioactive elements, known as polyelement-rich bed. In order to date and trace the source of the platinum group elements, 6 samples were collected from the Zhongnan region of Guizhou Province, and the Ganzi- ping-Sancha region of Hunan Province. The contents and isotopes of Re and Os were measured. Re and Os are positively correlated with each other and the correlation coefficient between 187Os/188Os and 187Re/188Os is 0.99856. On the 187Os/188Os-187Re/188Os diagram, 6 sample points are well-distributed along the (542±11) Ma fitting isochron in high coincidence and with 0.84±0.12 as the initial 187Os/188Os value. The result displays that the age value of the major mineralization of Re, Os and other platinum group elements is (542±11) Ma, which is identical with the stratigraphical age of the wall rocks; the polyelement beds in Hunan and Guizhou provinces bear high isochroneity; the differences of the forming times of different materials in the polyelement bed of the same area do not surpass the error limit permissible for Re-Os date fitting; there exists no distinct time interval between the formation of the diagenetic veinlets and that of the polyelement bed, or the Re-Os isotope composition has not been distinctly changed by the former process; basaltic crust might be the major source of Re, Os, other platinum group and trace elements in the Lower Cambrian polyelement bed of Hunan and Guizhou provinces. | 李胜荣 肖启云 申俊峰 孙丽 刘波 阎柏琨 江永宏 | 2003 | Science China Earth Sciences2003，46，9： | 13 |
| 4 | Geochemistry of the Mesozoic basaltic rocks in southern Hunan Province显示文摘Southern Hunan Province is famous for its intensive rare, radioactive and other metal elements’ mineralizations. There is a relation between the basaltic rocks and mineralizations in space, time and ore forming elements. The Jurassic Cretaceous (204\81 Ma) basaltic rocks consists mainly of alkali\|basalt and tholeiitic basalt formed in plate environment. Trace elements and Sr, Nd, Pb isotopic compositions show that the regional mantle source was metasomatized shortly before the partial melting. The alkali basalt and tholeiitic basalt might be 3%\5% and 10%\15% of the partial melting of the enriched mantle source respectively. Obviously the enrichment of the regional mantle played an important role in formation of the large and super\|large deposits in southern Hunan Province. | 赵振华 包志伟 张伯友 | 1998 | Science China Earth Sciences1998，41，S1： | 13 |
| 5 | 湖南各地市农业全要素生产率变动实证分析显示文摘运用非参数Malmquist指数法,测算了1985—2008年湖南省各地市农业全要素生产率水平及其变动趋势。结果显示:湖南省农业全要素生产率平均变动值为1.014,技术进步指数为1.015,技术效率变化指数为0.999,说明湖南省农业全要素生产率的增长主要依靠农业的技术进步,而整个农业规模效率基本保持在一个较稳定的常态;湖南全要素生产率呈现波段性周期变化,当出现重大技术创新时,其技术效率往往不高,说明技术创新的配套体系建立尚不够完善;各地市年均Malmquist指数相差较大,呈现出严重的东、中、西部梯度效应;西部地区的农业尚属传统农业,生产效率问题并非造成其生产力低下的主因,关键的问题在于促进其农业技术进步。 | 李立清 周贤君 | 2010 | 湖南农业大学学报(社会科学版)2010，11，6： | 12 |
| 6 | 湖南永顺烟区土壤养分状况的综合评价显示文摘对湖南省永顺县烟区的239个土壤样品、19项土壤养分指标进行了测定,确定了各指标所属的隶属度函数类型及其阈值,采用主成分分析法求得各指标的权重,用加乘法算出各土样的土壤肥力综合指标值(IFI),进而对永顺县植烟土壤适宜性进行了综合评价。结果表明:永顺县烟区土壤肥力存在较大的差异,其IFI值平均为0.541,变幅为0.341~0.730,变异系数5.14%。采用聚类分析法将土壤肥力分为高、较高、中等、较低4类,各类土样所占比例依次为15.86%、21.61%、44.17%、18.36%。 | 朱续熹 宋文峰 刘国顺 杨永锋 周琳 | 2010 | 江西农业学报2010，22，8： | 9 |
| 7 | A New Species of the Genus Tylototriton(Amphibia,Salamandridae) from Hunan,China显示文摘A new species of the genus Tylototriton is described in this article based on morphological and genetic evidence. The new species is identified belonging to the T. asperrimus group and is similar to T. wenxianensis. The diagnostic characters of the new species are as follows: dorsal ridge broad and thick,its width approximately equal to eye diameter(P < 0.001); tail height greater than width at base of tail(P < 0.001); no villous genital papilla found inside the male anal fissure; nodule-like warts,along lateral margin of the trunk,bulge and forming tubercles,and thin and transverse striae present between the tubercles. | Youhui SHEN Jianping JIANG Xiaoyang MO | 2012 | Asian Herpetological Research2012，3，1： | 7 |
| 8 | Middle and Late Devonian brachiopod assemblages,sea level change and paleogeography of Hunan,China显示文摘Givetian through middle Famennian brachiopods of Hunan are used to define five biozones,comprising,in ascending order,the Stringocephalus Abundance Zone,the Ambocoeliid-Leiorhynchid Assemblage Zone,the Cyrtospiriferid Assemblage Zone,the Yunnanellina-Sinospirifer Assemblage Zone,and the Yunnanella-Hunanospirifer Assemblage Zone.They correspond approximately to the Po.hemiansatus Zone to Po.varcus Zone,S.hermanni Zone to Pa.punctata Zone,Pa.hassi Zone to Pa.linguiformis Zone,Pa.triangularis Zone to Upper Pa.crepida Zone,and Uppermost Pa.crepida Zone to Pa.marginifera Zone,respectively.Intensified rifting activity in South China during the Devonian began in the middle of the Lower Po.varcus Zone(a level marked by the first appearance of Po.rhenanus),which is consistent with the Lower-Middle Givetian substage boundary suggested by the International Subcommission on Devonian Stratigraphy(SDS).This assumed that rifting activity in the Lower Po.varcus Zone was signified by the deposition of the Baqi Formation in Guangxi and was marked largely by the extensive deposition of the Qiziqiao Formation in central Hunan,which probably led to an opposite pattern of relative sea level change-rising in deeper water trough areas and lowering in carbonate platform areas.The previously recognized S.hermanni Zone sea level rise in platform margin areas of Guangxi can be identified not only in the trough areas but also in platform areas,which probably indicates an overall marine transgression at this time,rather than tectonically induced sea level change.Similarly,this level coincides with the Middle-Upper Givetian substage boundary suggested by the SDS.Although the sea level rise may have occurred in the deeper water trough areas of South China towards the end of the Givetian,platformal areas experienced uplifting at various degrees,especially in the central and northern regions of Hunan where Early Frasnian deposits were apparently absent in many places.Similarly,the end-Frasnian regression led to exposure of many places and absence of early Famennian deposits,which probably accounts for the restricted distribution of the Yunnanellina brachiopod fauna. | XuePing Ma Pu Zong | 2010 | Science China Earth Sciences2010，53，12： | 7 |
| 9 | 组织理论视角的知识共享影响因素整合模型研究——基于湖南省IT企业的实证分析显示文摘以湖南省内21家IT企业知识管理实践活动为研究对象,基于组织理论分析框架,从组织结构特征、组织文化和组织互动关系构建并检验了知识共享影响因素模型。研究发现,组织正式化程度、复杂化程度和集权化程度对企业知识共享行为都有负向影响;官僚型文化不利于知识共享行为的产生,虽然支持型文化和创新型文化都有利于知识共享,但创新型文化的影响更大;跨部门或个体之间的信任和组织承诺对知识共享行为有积极影响作用。 | 雷志柱 丁长青 | 2010 | 软科学2010，24，12： | 7 |
| 10 | Spatial and temporal patterns of amphibian species richness on Tianping Mountain,Hunan Province,China显示文摘DEAR EDITOR,Exploring species richness patterns across space and time can help in understanding species distribution and in formulating conservation strategies.Among taxa,amphibians are of utmost importance as they are highly sensitive to environmental changes due to their unique life histories(Zhong et al.,2018).Here,we investigated the spatial and temporal patterns of amphibian species richness on Tianping Mountain in China.Specifically,we established 10 transects at low to high elevations,and sampled amphibians in April,June,August,and October 2017.Our results demonstrated that amphibian species composition and richness varied significantly at both spatial and temporal scales and were associated with gradients of environmental change in microhabitats on Tianping Mountain. | Wen-Bo Zhu Chun-Lin Zhao Chun-Lin Liao Bei Zou Dan Xu Wei Zhu Tian Zhao Jian-Ping Jiang | 2020 | Zoological Research2020，41，2： | 5 |
| 11 | Contribution to the taxonomy of the genus Lycodon H.Boie in Fitzinger,1827(Reptilia:Squamata:Colubridae)in China,with description of two new species and resurrection and elevation of Dinodon septentrionale chapaense Angel,Bourret,1933显示文摘While considerable progress has been made in the taxonomic studies of the genus Lycodon in Asia,questions remain to be clarified regarding the taxonomy of certain groups,particularly those containing species in China.Not only do many regions in China remain overlooked by herpetologists,resulting in the possibility of undiscovered new species,but the surveyed areas also have suspicious records of recognized congeners that require taxonomic confirmations.Combining both morphological and genetic data,we tackle these outstanding issues in the taxonomy of Lycodon in China.In particular,we discover two new species of Lycodon:one from the previously neglected hot-dry valley in the northern Hengduan Mountain Region close to Tibet,and another recluse and cryptic species from the L.fasciatus complex in the downtown park of a major city in southern Sichuan Province.Additionally,we clarify the distribution of L.septentrionalis in China and resurrect and elevate its junior synonym subspecies,Dinodon septentrionale chapaense,as a full,valid species,and we synonymize the recently described L.namdongensis to the resurrected L.chapaensis comb.nov..Lycodon chapaensis comb.nov.thus represents a new national record of reptilian fauna of China.Lastly,based on literature review,we also correct some of the erroneous records of L.fasciatus and L.ruhstrati in China,point out remaining taxonomic issues of the genus for future research,and update the dichotomous key and distribution of the 20 species of Lycodon currently recorded from China. | Kai Wang Zhong-Bin Yu Gernot Vogel Jing Che | 2021 | Zoological Research2021，42，1： | 5 |
| 12 | Two new species of Vestrogothia (Phosphatocopina, Crustacea) of Orsten-type preservation from the Upper Cambrian in western Hunan, South China显示文摘Although fossils of Orsten-type preservation represented by Skaracarida and Phosphatocopina were first reported from the Middle and Upper Cambrian in western Hunan, South China in 2005, diversified phosphatocopine species have never been appropriately described and elucidated in terms of their evolutionary relationships. Here, we described two new species of Phosphatocopina, Vestrogothia anterispinata sp. nov. and V. bispinata sp. nov. The evolutionary relationship among all the valid species of Phosphatocopina is discussed and the phylogeny of Phosphatocopina is reestablished using cladistic analysis. Accordingly, phosphatocopines primitively evolved along two lineages: one evolved towards the emergence of lobes; the other evolved towards the emergence of dorsal spines. Respectively, lobes originated independently three times, and dorsal spines originated only once. With regard to the dorsal rims, interdorsum originated first, whereas dorsal furrow originated independently twice on the basis of interdorsum. Probably Hesslandona may represent a polyphyletic group, whereas Vestrogothia a monophyletic group. | ZHANG HuaQiao1,2 & DONG XiPing1,2 1 School of Earth and Space Sciences,Peking University,Beijing 100871,China 2 State Key Laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing 210008,China | 2009 | Science China Earth Sciences2009，52，6： | 5 |
| 13 | A Potential Candidate For the Middle-Upper Cambrian Boundary Stratotype——An Introduction to the Paibi Section in Huayuan,Hunan显示文摘The Middle-Upper Cambrian boundary is one of the current stratigraphical problems which remain openin the geological world, since there have been no universally acknowledged delimiting standard and stratotype.Acting on the instruction of Profs. Lu Yanhao and An Taixiang the author studied in details the Paibi Section,which is well exposed as a continuous sequence at an easily accessible locality. The Middle-Upper Cambrianboundary strata are composed of biocalcimicrosparite, indicating the sedimentary environment of anunderwater upheaval on the gentle slope along the frontal margin of the Yangtze carbonate platform. For the upper Middle and lower Upper Cambrian agnostid trilobite zones and conodont zones are erected,and a more accurate correlation between the trilobite and conodont sequences is established. Based on these,the Middle-Upper Cambrian boundary is drawn more reasonably and precisely than what was done before. Inshort, the section studied is superior to other known sections of Middle-Upper Cambrian. and it will probablybe an ideal candidate for the Middle-Upper Cambrian boundary stratotype. | Dong Xiping Department of Geology, Peking University, Beijing | 1990 | Acta Geologica Sinica(English Edition)1990，64，3： | 4 |
| 14 | Characteristics of Shale Reservoir and Sweet Spot Identification of the Lower Cambrian Niutitang Formation in Northwestern Hunan Province, China显示文摘The accumulation and productivity of shale gas are mainly controlled by the characteristics of shale reservoirs;study of these characteristics forms the basis for the shale gas exploitation of the Lower Cambrian Niutitang Formation(Fm),Southern China.In this study,core observation and lithology study were conducted along with X-ray diffraction(XRD)and electronic scanning microscopy(SEM)examinations and liquid nitrogen(N2)adsorption/desorption and CH4 isothermal adsorption experiments for several exploration wells in northwestern Hunan Province,China.The results show that one or two intervals with high-quality source rocks(TOC>2 wt%)were deposited in the deep-shelf facies.The source rocks,which were mainly composed of carbonaceous shales and siliceous shales,had high quartz contents(>40 wt%)and low clay mineral(<30 wt%,mainly illites)and carbonate mineral(<20 wt%)contents.The SEM observations and liquid nitrogen(N2)adsorption/desorption experiments showed that the shale is tight,and nanoscale pores and microscale fractures are well developed.BJH volume(VBJH)of shale ranged from 2.144×10^-3 to 20.07×10^-3 cm^3/g,with an average of 11.752×10^-3 cm3/g.Pores mainly consisted of opened and interconnected mesopores(2–50 nm in diameter)or macropores(>50 nm in diameter).The shale reservoir has strong adsorption capacity for CH4.The Langmuir volume(VL)varied from 1.63 to 7.39 cm^3/g,with an average of 3.95 cm^3/g.The characteristics of shale reservoir are controlled by several factors:(1)A deep muddy continental shelf is the most favorable environment for the development of shale reservoirs,which is controlled by the development of basic materials.(2)The storage capacity of the shale reservoir is positively related to the TOC contents and plastic minerals and negatively related to cement minerals.(3)High maturity or overmaturity leads to the growth of organic pores and microfractures,thereby improving the reservoir storage capacity.It can be deduced that the high percentage of residual gas in Niutitang Fm results from the strong reservoir storage capacity of adsorbed gas.Two layers of sweet spots with strong storage capacity of free gas,and they are characterized by the relatively high TOC contents ranging from 4 wt%to 8 wt%. | QIN Mingyang CAO Zheng GUO Jianhua HUANG Yanran SUN Lianpu DONG Li | 2019 | Acta Geologica Sinica(English Edition)2019，93，3： | 3 |
| 15 | A new cave-dwelling blind loach, Triplophysa erythraea sp. nov.(Cypriniformes: Nemacheilidae), from Hunan Province, China显示文摘DEAR EDITOR, A new blind loach species, Triplophysa erythraea sp. nov., from a karst cave in Hunan Province, central south China, is described based on morphology and cyt b gene sequencing. It can be distinguished from other species of Triplophysa by the following combi nation of characters: eyes absent;body scaleless and colorless;caudal-fin 17;maxillary barbel Ion gest;fins tran sparent, compressed pectoral-fin reachi ng 2/3 distanee between pectoral-fin and pelvic-fin origins;pelvicfin and dorsal-fin origins relative;posterior chamber of airbladder well developed, Iong, oval, and dissociative. | Tai-Fu Huang Pei-Ling Zhang Xing-Long Huang Tao Wu Xiao-Yan Gong You-Xiang Zhang Qing-Zhong Peng Zhi-Xiao Liu | 2019 | Zoological Research2019，40，4： | 3 |
| 16 | NATURAL DISASTERS AND DISASTER RELIEF IN PARTS OF CHINA IN 2003 | Chen Hongling (The Ministry of Civil Affairs, P.R.C, Beijing 100721)) An earthquake of 6.6 magnitudes occurred in Delingha,Qinghai Province | 2003 | Natural Disaster Reduction in China2003，，4： | 2 |
| 17 | 湖南方言“得+V”和“V+得”结构的发展(英文)显示文摘得 DE ' to obtain' is a linguistic sign which has a long history and has very complex usages. This paper will focus on the development of [DE + V] and [V + DE] constructions in which both the DE are claimed to be used as modal auxiliaries and indicate the notion of possibilities in Chinese throughout the history. [DE + V] appeared earlier than [V + DE] (Yue Junfa, 1984, Yang Ping, 1989, Sun Chaofen 1996, among others). Both constructions are rarely used in Mandarin but are till active in the Hunan dialects. | Yunji WuThe University of Melbourne Hunan Normal University The Melbourne Institute of Asian Languages and Societies The University of Melbourne 3010 Australia | 2001 | 语言研究2001，，3： | 2 |
| 18 | Study of Noble Metal Elements in Lower Cambrian Black Rock Series of Guizhou-Hunan Provinces, China显示文摘INTRODUCTIONLowerCambrianblackrockseriesexistsbroadlyinmorethan10provincesinSouthChina(Chenetal.,1990).Thebotomoftheseriesspo... | Li Shengrong Department of Geology and Mineral Resources, China University of Geosciences, Beijing 100083 Gao Zhenmin Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002 | 1999 | Journal of Earth Science1999，18，1： | 2 |
| 19 | MICROFOSSILS FROM LATE PROTEROZOIC MANGANESE ORE DEPOSITS IN WESTERN HUNAN PROVINCE AND EASTERN GUIZHOU PROVINCE, SOUTH CHINA显示文摘Abundant microfossils and organic residuals have been discovered by SEM and normal palynological maceration from manganese ore beds intercalated in late Proterozoic glacial rock units in western Hunan Province and eastern Guizhou Province. Taking isotopic dating into consideration, the age of manganese ore deposits in both regions is suggested to be about 750 Ma. A distinct character is that a great quantity of colonial microfossil——Sphaerocongregus (or Bavlinella) and their degradational variants have been obtained from rhodochrosite. Their biological and biochemical functions, combined with the geochemical effect of manganese in different ways, may play an important role in the manganese cycle. | 尹磊明 | 1990 | Science China Chemistry1990，33，6： | 2 |
| 20 | 基于抽样调查的湖南四地区农村民居震害预测显示文摘作者组织人员在湖南长沙、娄底、湘潭和邵阳对483户农村民居进行抗震性能调查,得到湖南省农村住宅在建筑年代、结构形式、建筑材料、地基基础及构造连接等方面的统计数据。在此基础上,运用建筑物地震易损性的概率分析法,对所调查的民居进行震害预测。分析表明:所调查地区农村民居在基本设防烈度作用下,不会发生毁坏,但可能发生中等破坏。 | 赵世伟 罗奇峰 | 2010 | 结构工程师2010，26，5： | 2 |
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