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Carbon and Oxygen Stable Isotope Values and Microfossils at 41.4-4.5ka BP in Tai Co,Tibet,China,and Their Paleoclimatic Significance

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Acta Geologica Sinica(English Edition) 2011年第5期85卷 1036-1050+1052-1056+1051页

作者： ZHENG Mianping~(1,2.*),LIU Junying~(1,3.,MA Zhibang~(1,4),WANG Hailei~(1,2. and MA Nina~(1,2. 1 MLR {3. laboratory of {2. lake {3. and environment,Institute of Mineral {3.,CAGS, beijing 10003.,China 2.Research and Development Center for {2. lakes and Epithermal Deposits,chinese academy of {12. sciences,beijing 10003.,China 3.Institute of Geology,chinese academy of {12. sciences,beijing 10003.,China 4 {3. laboratory of Cenozoic Geology and environment,chinese academy of sciences,beijing 10002., China MLR key laboratory of {2. {3. {3. and environment Institute of Mineral Resources CAGS Beijing 100037 China Research and Development Center for saline lakes and Epithermal Deposits Chinese Academy of Geological Sciences Beijing 100037 China Institute of Geology Chinese Academy of Geological Sciences Beijing 100037 China key laboratory of Cenozoic Geology and {2. Chinese Academy of Sciences Beijing 100029 China

Two sedimentary sections were measured at Tai Co(Co means lake in Tibetan) in western Tibet,*** two sections are almost all composed of clay carbonate beds except in their lower parts where there are carbonized plants at>10 cm depths and dark-colored carbonate clay and clay at 50-70 cm depths,yielding abundant gastropods,ostracods,and *** carbon and oxygen stable isotope values of carbonate,ostracods,and charophytes and ecological features of microfossil communities indicate the following climatic change in the area from 41.4 to 4.5 ka BP:at 41.4-2..2.ka BP,the climate was relatively wet;at 2..2.2..5 ka BP,it was slightly warm-dry;at 2..5-2..5 ka BP,it was warm-wet;at 2..5-2..0 ka BP,it was slightly cold-wet;at 2..5-17.5 ka BP,it became cold abruptly and slightly wet,implying the climate of the last glacial maximum;at 17.5-16.0 ka BP,it was slightly cold-dry;at 16.0-11.8 ka BP,it was slightly warm-wet;at 11.8-10.4 ka BP,it was relatively cold-dry, roughly equivalent to the climate of the Younger Dryas,and at 10.4 ka BP,the temperatures began to rise again;at 10.4-9.4 ka BP,it was slightly warm-wet;at 9.4-8.5 ka BP,there occurred short warm-wet oscillations;at 8.5-7.9 ka BP,it was slightly dry-cold,representing a strong temperature-lowering and drying event in the postglacial stage;at 7.8-6.3.ka BP,it was slightly warm-wet;at 6.3.4.5 ka BP,the climate tended to be cold-dry.4.5 ka BP recorded the maximum aridity since the late part of the late Pleistocene.

关键词： sedimentary environment index paleoclimatic changes late Pleistocene-Holocene(41.4-4.5 ka BP) Tai Co Tibet

Cesium accumulation by bacterium Thermus sp. TibetanG7:hints for biomineralization of cesium-bearing geyserite in hot springs in Tibet,China

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chinese Science Bulletin 2007年第19期52卷 2680-2686页

作者： WANG HaiLei1,2.3. ZHENG MianPing1,2.3.& HUANG XiaoXing4 1 Institute of Mineral resources,{3. (CAGS),{2., China 2.R&D Center for {3. lake and Epithermal Deposits, CAGS,{2., China 3.open laboratory of {3. lake Resourses and {13., CAGS,{2., China 4 laboratory of Microbial resources, Institute of Microbiology, chinese academy of sciences, beijing 100081, China Institute of Mineral resources Chinese Academy of Geological Sciences (CAGS) Beijing China R&D Center for saline lake and Epithermal Deposits CAGS Beijing China open laboratory of {2. {3. Resourses and environment CAGS Beijing China laboratory of Microbial resources Institute of Microbiology Chinese Academy of Sciences Beijing China

The bacterium Thermus sp. TibetanG7, isolated from hot springs in Tibet, China, was examined for the ability to accumulate cesium from solutions. environmental conditions were simulated and the effects of pH, K+, Na+ and K+-regimes were then studied to determine the possible role of the bacterium in the formation of cesium-bearing geyserite around these hot springs. In despite of the inhibition of K+ and Na+, the bacterium Thermus sp. TibetanG7 revealed noticeable accumulation of cesium from solutions, with maximum accumulations of 53.49 and 40.41 μmol Cesium/g cell dry weight in Na+ and K+ inhibition experiments, respectively. The accumulation of cesium by this microorganism is rapid, with 40%―50% accumulated within the first 5 min. K+-deficient cells showed a much higher capacity of cesium accu- mulation compared with K+-sufficient cells. It is evident that the bacteria within the genus thermus play a significant role in the cesium assembly. The formation of cesium-bearing geyserite is also considered.

关键词：铯元素沉积物硅华生物矿化

Primary Study on Quantitative Reconstruction of Middle-Late Eocene Climate in Jianghan Basin

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Journal of China University of Geosciences 2002年第3期13卷 252-259页

作者： Tong Guobang Liu Zhiming Institute of Hydrogeology and environmental Geology, chinese academy of geological sciences, Zhengding 050803.{2. {3. of saline lake resources and environment, chinese academy of geological sciences, beijing 10003. Zheng Mianping Institute of Mineral resources, chinese academy of geological sciences, beijing 10003. Research & Development Center of saline lake and Epithermal Deposit, chinese academy of geological sciences, beijing 10003. Wang Weiming Nanjing Institute of Geology and Palaeontology, chinese academy of sciences, Nanjing 2.0008 Institute of Hydrogeology and environmental Geology Chinese Academy of Geological Sciences Zhengding 050803 open laboratory of {2. {3. resources and environment Chinese Academy of Geological Sciences Beijing 100037 Institute of Mineral resources Chinese Academy of Geological Sciences Beijing 100037 Research & Development Center of saline lake and Epithermal Deposit Chinese Academy of Geological Sciences Beijing 100037 Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences Nanjing 210008

This paper reports our primary effort in the quantitative reconstruction ofpaleoclimate based on the thrine in phytoecology of the affinity parent plants in the stratigraphicpollen records. The Eocene pollen data come from our former study on the Mingjia borehole 1 in theJianghan basin. The fluctuating trend in the parameter curve of climate shows that the climate inthe Middle Eocene in the Jianghan basin was more or less comparable with that of the present2.°―2.°N, characteristic of a humid, semi-humid central-southern subtropical climate. The annualtemperature at that time dropped by 1 ℃― 4 ℃ in the Late Eocene, approximately equal to that ofthe present 2.°―2.°N of northern-central subtropical climate. However, the climate composite atthat time, characterized by higher temperature, small annual range and big fluctuation inprecipitation, was quite different from the present one. The average temperature in January in theMiddle Eocene, higher than that of today, ranged between 5 ℃ and 9 ℃, indicating that no effect ofwinter monsoon occurred in the Middle Eocene, though such an effect may have occurred occasionallyin the Late Eocene. Major temperature decline is recognized at the depth of 2.100 m in the borehole,as was indicated by the decline in average January temperature, the increase in annual range, andthe increase in the deciduous broad-leaved types of trees in the spore-pollen assemblage. The sharpfluctuation in the annual precipitation, usually raging from 3.0 to 1 700 mm, was favorable for themigration and accumulation of salty deposit. When the precipitation was lower than 1 000 mm,ephemera shrub increased at the same depth as that of the salty deposit. It is, therefore, deducedthat the formation of the salty deposit was attributed mainly to the dry and hot environment in thehigh mountains and deep basins. The small annual precipitation and the intense fluctuation arefavorable for the sustainable accumulation of the salts, which is different from the present

关键词： quantitative reconstruction of paleoclimate annual range function ofthrine in phytoecology fuzzy mathematics eocene jianghan basin

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西藏台错晚第四纪轮藻类的新类型

微体古生物学报 2011年第2期28卷 145-168页

作者：刘俊英王海雷国土资源部盐湖资源与环境重点实验室北京100037 中国地质科学院盐湖与热水资源研究中心北京100037 中国地质科学院地质研究所北京100037 中国地质科学院矿产资源研究所北京100037

本文的研究材料来自西藏羌塘高原西部台错古湖一个3.69 m的天然剖面,其地层测年为3.0}6—4.5ka。从其156个样品中获取大量的轮藻类、介形类和腹足类及少量有孔虫等微体化石。据轮藻类藏卵器外形,顶部结构、螺旋细胞钙化式样等特征,该剖... 详细信息

本文的研究材料来自西藏羌塘高原西部台错古湖一个3.69 m的天然剖面,其地层测年为3.0}6—4.5ka。从其156个样品中获取大量的轮藻类、介形类和腹足类及少量有孔虫等微体化石。据轮藻类藏卵器外形,顶部结构、螺旋细胞钙化式样等特征,该剖面的轮藻类应归属于轮藻科Characeae之轮藻属Chara。经研究得知,台错古湖在大约2. ka的时期内,曾生长过2.种轮藻,其中新类型7个,包括新种4个:Chara platea,***,***和***;新型2.:***,***;新变种1个:***。其余是曾产于国内外第四系的Chara其它分子。其中有5个新联合种:Chara alba(Madler et Staesche),***(Tang et Di),***(Tang et Di),***(Tang etDi)和***。该剖面轮藻类、介形类、腹足类等多门类微体化石的紧密共生,对轮藻植物群生态学研究具重要意义。

关键词：轮藻类新类型晚第四纪台错西藏

Cymbella Agardh属(硅藻门Bacillariophyta)的一个新化石种的发现及其微细构造

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微体古生物学报 2003年第4期20卷 435-438页

作者：李家英魏乐军郑绵平中国地质科学院地质研究所北京100037 中国地质科学院矿产资源研究所

新化石种 Cymbella taicuonensis L i et Zheng ***.是在研究西藏西北部日土县台错古湖剖面沉积物中硅藻植物群时发现的 ,剖面沉积物中保存了非常丰富的硅藻化石 ,Cymbella taicuonensis就是这些硅藻化石中的一个新化石种。对标本采用... 详细信息

新化石种 Cymbella taicuonensis L i et Zheng ***.是在研究西藏西北部日土县台错古湖剖面沉积物中硅藻植物群时发现的 ,剖面沉积物中保存了非常丰富的硅藻化石 ,Cymbella taicuonensis就是这些硅藻化石中的一个新化石种。对标本采用光学镜 (L M)和扫描电镜 (SEM)观察和照相。

关键词：硅藻分类台错西藏

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西藏扎布耶盐湖太阳池的建造与运行试验

太阳能学报 2010年第2期31卷 163-167页

作者：黄维农王学魁孙之南乜贞沙作良天津科技大学海洋科学与工程学院天津300457 西藏扎布耶锂业高科技有限公司拉萨850000 中国地质科学院矿产资源研究所北京100037 国土资源部盐湖与环境开放研究实验室北京100037

介绍了西藏扎布耶盐湖面积为3.88m^2.阳池的建造与运行试验,获得了扎布耶盐湖太阳池运行过程中的温度和盐度分布情况,找到了不同时期简单实用的梯度层构建方法。基于当地条件,扎布耶盐湖太阳池的构建费用低,使用淡水量小,梯度层薄(3.～... 详细信息

介绍了西藏扎布耶盐湖面积为3.88m^2.阳池的建造与运行试验,获得了扎布耶盐湖太阳池运行过程中的温度和盐度分布情况,找到了不同时期简单实用的梯度层构建方法。基于当地条件,扎布耶盐湖太阳池的构建费用低,使用淡水量小,梯度层薄(3.～50cm);下对流层(LCZ)较厚,直接使用盐田日晒卤水,一般达2.0～2.0cm;运行周期短(约1个半月～2.月);升温幅度低(约3.～40℃);不需要复杂的辅助和维护设施。其成功运行为扎布耶盐湖锂资源的开发提供了热源。

关键词：扎布耶盐湖太阳池运行试验

HOLOCENE saline SEDIMENTARY RECORD IN TIBETAN DONG CO(lake) AND ITS SIGNIFICANCE ON PALAEOCLIMATE

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地学前缘 2000年第S1期7卷 378-378页

作者： Wei Lejun 1,2.,Zheng Mianping 2.3.[WT5,5”BX](1 China University of Geosciences,{3. 100083.China 2.{2. {3. of saline lake resources & environment ,chinese academy of {13. sciences,{3. 10003.,China 3.Institute of Min

Based on the sedimentary characteristics study of Holocene borax\|bearing mirabilite beds of Dong Co(lake) two sections, DZ01 and DZ02. in the center of North\|Tibetan Plateau,combined with dating of 14 C, applied theory and method of comparative salinology, it is determined that the palaeoclimate framework of Dong Co during early\|middle Holocene, and reckoned the range of the temperature variation. Furthermore, after completing regional analogue, discovered that the palaeoclimate environment is fully comparative and consistent with the synchronous lake\|water retreating trace of Zhaduixiong spits in Zabuye lake basin, with palaeoclimate changes recorded by pollen in adjacent Zabuye lake, with Holocene plaeoclimate environment indicated by drilling\|hole in Bangong Co,with palaeoclimate significance traced by δ 18 O value in Qinghai lake and Siling Co and with the palaeoclimate framework during the 5th Level Arid (Salinization) Extension Period of Quaternary arid center of Western China.

关键词： Dong Co Tibet Holocene sedimentary record palaeoclimate change s

Sequence stratigraphic framework and distribution of depositional systems for the Paleogene in Liaodong Bay area

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Science China Earth sciences 2008年第S2期51卷 1-10页

作者： ZHU XiaoMin1,DONG YanLei1,YANG JunSheng1,ZHANG Qin1,LI DeJiang2.XU ChangGui3.& YU Shui3.1 National key laboratory of Petroleum {2. and Prospecting,China University of Petroleum,beijing 102.49,China 2.Research Institute of Petroleum Exploration and Development——Langfang,PetroChina,Langfang 065007,China 3.Technology Department of CNOOC Tianjin Company,Tianjin 3.0452.China National key laboratory of Petroleum {2. and Prospecting China University of Petroleum Beijing China Research Institute of Petroleum Exploration and Development—Langfang PetroChina Langfang China Technology Department of CNOOC Tianjin Company Tianjin China

With a comprehensive geological and geophysical data base,the Paleogene in the Liaodong Bay area,which consists of the Kongdian,Shahejie and Donghying Formations from the base to top,was divided into 4 second-order sequences and 8 third-order sequences based on the characteristics of the se-quence boundaries. Each third-order sequence is subdivided into the lowstand,lake transgressive and highstand systems tracts. The Lowstand systems tract (LST) is mainly composed of progradational parasequence sets,while the lake transgressive systems tract (TST) largely consists of the retrograda-tional parasequence sets and the highstand systems tract (HST) is dominated by the progradational parasequence sets. The main types of depositional systems include the shallow lake,semi-deep lake,deep lake,delta,fan delta,braided fluvial delta and nearshore subaqueous fan. The braided fluvial delta and fan delta depositional systems are mainly confined to the sequences of the lower SEs4-Ek,SEs3.and SEs1+2.while the sequences of SEd3.SEd2.and SEd1 are dominated by the delta and nearshore subaqueous fan depositional systems with the latter being developed at the downthrown side of the basin-bounding fault in each sequence. The evolution of the depositional systems is always con-trolled by the paleo-tectonic setting and the ancient landform in the space and geological time. It is concluded that the most favorable reservoirs are distributed in the Liaoxi low uplift and the central Liaozhong sag.

关键词： Liaodong Bay area Paleogene sequence stratigraphy sequence boundary depositional system

Depositional characteristics and petroleum geological significance of wetland

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Petroleum Science 2009年第4期6卷 347-353页

作者： Jin Zhenkui Gu Junfeng Su Nina Wang Zhaofeng Huang Xiaoping State key laboratory of Hydrocarbon {2. and Exploration China University of PetroleumBeijing 102249China Research Institute of Petroleum Exploration and Development Xinjiang Oilfield CompanyPetroChinaKaramayXinjiang 834000China

Wetland is a new type of sedimentary facies proposed for the first time in this paper. It is a type of sedimentary environment, transitional between land facies and water (sea or lake) facies. In this paper, wetland is redefined as “a type of sedimentary environments whose ground surface is flat and wet throughout the year, which may be covered with very shallow water (less than {3.m deep), and is covered with lush plant growth”. Wetland is reclassified into two types, swamp wetland (swamp in brief) and wet plain wetland (wet plain in brief). Swamp deposits are coal, while wet plain deposits are dark colored mudstones or silty mudstones rich in plant fossils and carbon debris. The deposits of wet plain are different from those of lake and floodplain in the abundance of plant fossils, color, resistivity well logging curve, and other sedimentary characteristics. In boreholes, resistivity logging can be used to distinguish between wet plain mudstones and lake mudstones. Understanding the sedimentary characteristics of wet plain wetland can help to identify wet plain deposits which were formerly classified as floodplain or lake deposits. This will help to reconstruct the palaeogeography and to understand the history of basin and climate evolution accurately, and is especially important in evaluation of the hydrocarbon generating potential of a basin. With the Jurassic Sangonghe Formation of the Yanqi Basin as an example, the identification characteristics of wetland are described.

关键词： Wetland wet plain Yanqi Basin Sangonghe Formation of Jurassic braided river delta