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Science china Earth Sciences 2005年第10期48卷 1698-1707页

作者： wang rujian1.& chen ronghua2 1. state key laboratory of marine geology,{1., shanghai 200092, china 2. The key laboratory of Submarine Geoscience, state Oceanic Administration, Hangzhou 31.01., china state {1. laboratory of marine geology tongji university shanghai china The key {1. of Submarine Geoscience state Oceanic Administration Hangzhou china

Cycladophora davisiana (Radiolarian) contents are counted in two cores of the Ber-ing Sea and correlated well with the oxygen isotopic records of ice in the deep core obtained by the Greenland Ice Sheet Project II (GISP 2) and deep-sea sediments (SPECMAP) of the world oceans. Millennial scale climatic events, for example, Younge Dryas and B?lling/Aller?d events, Heinrich1.and Dansgaard-Oeschger1.vents, recorded by C. davisiana percents are distin-guished from Core B4-2. C. davisiana events b, c1. c2, d, e1.and e2, respectively, corresponding to oxygen isotopic 2.0, 3.1. 3.3, 4.0, 5.1.and 5.3, are identified from Core B2-9. High resolution re-cords of C. davisian are tuned to the oxygen isotopic records in GISP 2 and SPECMAP and the depth-age frameworks are established in the two cores, supplying a stratigraphic base for future paleoceanographic and paleoclimatic studies. High C. davisiana during the glacial periods in the two cores indicate that they can serve as a proxy of the glacial Subarctic Pacific Intermediate Water, which verifies the glacial Subarctic Pacific Intermediate Water brought from the Bering Sea.

关键词： Cycladophora davisiana, stratigraphic tool, YD and B/A events, Heinrich 1 and D/O1 events, proxy of glacial Subarctic Pacific Intermediate Water, late Quaternary, Bering Sea.

Forcing mechanism of the Pleistocene east Asian monsoon variations in a phase perspective

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Science china Earth Sciences 2005年第10期48卷 1708-1717页

作者： TIAN Jun1,2, wang Pinxian1, chenG Xinrong1, wang rujian1.& SUN Xiangjun1,3 1. state key laboratory of marine geology, tongji university, shanghai 200092, china 2. Institute of geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, china 3. Institute of Botany, Chinese Academy of Sciences, Beijing 100093, china state {1. laboratory of marine geology tongji university shanghai china Institute of geology and Geophysics Chinese Academy of Sciences Beijing{1. Institute of Botany Chinese Academy of Sciences Beijing china

The deep sea records from the ODP Sites 1.43 and 1.44 in the northern and southern South china Sea (SCS), including foraminiferal δ 1.O and δ 1.C, Opal% and pollen percentage, reveal that the variations of the east Asian monsoon have been closely correlated with the variations of the Earth’s orbital parameters (eccentricity, obliquity and precession) and the global ice volume on orbital scale. All the monsoonal proxies show strong 1.0 ka, 41.ka and 23 ka cycles. Although G. ruber δ 1.C of Site 1.43 is coherent with the ETP (ETP= normalized (eccentricity + obliquity-precession) at eccentricity, obliquity and precession bands, most of the coherent relationship focuses on the precession band, and the other monsoonal proxies are coherent with the ETP only at the precession band, which indicate that precession dominates the Pleistocene tropical climate changes. The phase relationship of the monsoonal proxies with the foraminiferal δ 1.O implies that the global ice volume changes have played a significant role in modulating the east Asian monsoon climate, at least dominating the winter monsoon. This forcing mechanism of the east Asian monsoon is apparently different from that of the Indian ocean mon-soon. The variations of the east Asian monsoon at the precession band, at least that of the winter monsoon, have been controlled not only by the sensible heating but also by the latent heating of the surface water in the South china Sea.

关键词： South china Sea, ODP, east Asian monsoon, orbital forcing, global ice volume.

Microfossils, carbonate lysocline and compensation depth in surface sediments of the northeastern South china Sea

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Acta Oceanologica Sinica 2003年第4期22卷 597-606页

作者： chen ronghua1, Xu Jian2, Meng Yi3, wang Dongjun1 Liu Chuanlian2, Huang Baoqi2, Zhang Fuyuan1 1. key laboratory of Submarine Geosciences of state Oceanic Administration, Hangzhou 310012, china 2. laboratory of marine geology, tongji university, shanghai 200092, china 3. Institute of Estuarine and Coastal Research, East china Normal university, shanghai 200062, china key Lab Sub{1. Geosci state Ocean Adm Hangzhou 310012 Peoples R China tongji Univ Lab Marine Geol Shanghai 200092 Peoples R China E china Normal Univ Inst Estuarine & Coastal Res Shanghai 200062 Peoples R China

Based on the quantitative analyses of abundance of planktonic foraminifera, benthic foraminifera, calcareous nannofossils, the ratios of calcareous to siliceous microfossils, and the determination of carbonate contents in the surface sediments of the northeastern South china Sea, it has been found that the carbonate contents, the abundance of planktonic foraminifera and calcareous nannoplankton, and the ratio of calcareous microfossils decrease rapidly while the ratio of the benthic foraminifera to the total foraminiferal fauna, specific value of siliceous microfossils, and the percentage of the agglutinated tests in the benthic foraminiferal fauna increase with the water depth. The results indicate that the microfossils abundance and ratio, and the carbonate content are closely related to the carbonate lysocline and carbonate compensation depth (CCD) in the study area. In addition, the carbonate lysocline and the CCD are different between the southern and northern parts of the South china Sea. Both the lysocline and the CCD are deeper in the south with 2 600 and 3 600 m than in the north with 2 200 and 3 400 m, respectively.

关键词： microfossils carbonate lysocline depth carbonate compensation depth (CCD) surface sediments South china Sea (SCS)

Siliceous microplankton fluxes and seasonal variations in the central South china Sea during 1.93-1.95: monsoon climate and ? Nino responses

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Chinese Science Bulletin 2000年第23期45卷 2168-2172页

作者： wang rujian, LIN Jun, ZHENG Lianfu, chen ronghua & chen Jianfanglaboratory of marine geology of MOE, tongji university, shanghai 200092, china The key laboratory of Submarine Geoscience, state Oceanic Administration, Hangzhou 310012, china Correspondence should be addressed to wang rujian laboratory of {1. geology of MOE Tongji University Shanghai China The key {1. of Submarine Geoscience State Oceanic Administration Hangzhou China

Seasonal variations of radiolarian and diatom fluxes in the central South china Sea during 1.93-1.95 were overwhelmingly controlled by monsoon climate. Radiolarian and diatom increased obviously during the Northeast (from November to February) and Southwest (from June to September) monsoons and decreased during the periods between the monsoons. The change of circulation driven by the monsoons improved water exchange in the different areas that brought rich nutrient materials for the surface microplankton, thereby enhancing radiolarian and diatom fluxes. Variation of radiolarian flux coincided with organic carbon flux, surface primary and export productivities. High radiolarian flux corresponded to high surface primary productivity. Radiolarian and diatom fluxes raised abnormally during 1.94-1.95 could be attributed to the El Nino event during the period.

关键词： siliceous microplankton fluxes seasonal variations monsoon climate El Nino event central South china Sea.

Denitrification in Qi'ao Island coastal zone,the Zhujiang Estuary in china

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Acta Oceanologica Sinica 2009年第1期28卷 37-46页

作者： wang Hu ZHOU Huaiyang PENG Xiaotong YANG Qunhui QIN Chaomei YIN Xijie {1. Guangqian Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou 510640 China state {1. laboratory. of marine geology Tongji University Shanghai 200092 China Graduate university of Chinese Academy of Sciences Beijing 100049 China

Samples of sediments and the overlying water were collected in the Qi＇ao Island coastal zone,the Zhujiang（Pearl River） Estuary（ZE）.Denitrification rates,sediment oxygen demand（SOD）,and fluxes of inorganic nitrogen compounds were investigated with N2 flux method,using a self-designed continuous flow through and auto-sampling *** results indicate that the denitrification rates varied between 222 and 908 μmol/（m2·h） with an average of 499 μmol /（m2·h）.During incubation,the sediments absorbed dissolved oxygen in the overlying water with SOD ranging from 300 to 2 363 μmol/（m2·h）.The denitrification rates were highly correlated with the SOD（r2=0.77） regardless of the NO-3＋NO-2 concentrations in the overlying water,organic carbon contents in sediments and water temperature,suggesting that the SOD was probably the main environmental factor controlling the denitrification in the Qi＇ao Island coastal *** was a net flux of NO-3＋NO-2 into the sediments from the overlying *** NH＋4 flux from sediments into water as the result of mineralization was between 1..3 and 21..3 μmol/（m2·h）,which seems limited by both organic carbon content in sediment and dissolved oxygen concentration in the overlying water.

关键词： denitrification N2 flux SOD inorganic nitrogen compound Qi' ao Island coastal zone Zhu-jiang Estuary

Quantitative prediction model for the depth limit of oil accumulation in the deep carbonate rocks:A case study of Lower Ordovician in Tazhong area of Tarim Basin

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Petroleum Science 2024年第1期21卷 115-124页

作者： Wen-Yang wang Xiong-Qi Pang Ya-Ping wang Zhang-Xin chen Fu-Jie Jiang Ying chen state {1. laboratory of Lithospheric Evolution Institute of Geology and GeophysicsChinese Academy of SciencesBeijing100029China state {1. laboratory of Petroleum Resources and Prospecting China University of Petroleum(Beijing)Beijing102249China College of Geosciences China University of Petroleum(Beijing)Beijing102249China Research Institute of Exploration and Development PetroChina Southwest Oil&Gas Field CompanyChengdu610041SichuanChina Chemical and Petroleum Engineering Schulich School of EngineeringUniversity of CalgaryCalgaryT2N 1N4Canada

With continuous hydrocarbon exploration extending to deeper basins,the deepest industrial oil accumulation was discovered below 8,200 m,revealing a new exploration ***,the extent to which oil exploration can be extended,and the prediction of the depth limit of oil accumulation(DLOA),are issues that have attracted significant attention in petroleum *** it is difficult to characterize the evolution of the physical properties of the marine carbonate reservoir with burial depth,and the deepest drilling still cannot reach the ***,the DLOA cannot be predicted by directly establishing the relationship between the ratio of drilling to the dry layer and the *** this study,by establishing the relationships between the porosity and the depth and dry layer ratio of the carbonate reservoir,the relationships between the depth and dry layer ratio were obtained *** depth corresponding to a dry layer ratio of 1.0%is the *** on this,a quantitative prediction model for the DLOA was finally *** results indicate that the porosity of the carbonate reservoir,Lower Ordovician in Tazhong area of Tarim Basin,tends to decrease with burial depth,and manifests as an overall low porosity reservoir in deep *** critical porosity of the DLOA was 1.8%,which is the critical geological condition corresponding to a 1.0%dry layer ratio encountered in the *** depth of the DLOA was 9,000 *** study provides a new method for DLOA prediction that is beneficial for a deeper understanding of oil accumulation,and is of great importance for scientific guidance on deep oil drilling.

关键词： Deep layer Tarim Basin Hydrocarbon accumulation Depth limit of oil accumulation Prediction model

Nd isotope as the tracer of seawater evolution of early Miocene in the eastern Pacific Ocean

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Chinese Science Bulletin 2003年第B06期48卷 106-110页

作者： LIU Jihua~(1.2,3), chen Lirong~1. {1. Yingxi~4 & HAN Jianxiu~5 1. Institute of Oceanology, Chinese Acadcmy of ences, Qingdao 266071. china 2. key Lab of marine Sedimentology and Environmental geology, First Institute of Oceanograpgy, state Oceanic Administration, Qingdao 266061. china 3. Graduate School, Chinese Academy of Sciences, Beijing 1.0039. china 4. Modern Analysis Center, Nanjing university. Nanjing 21.093. china 5. Guangzhou marine Investigation Bureau, Guangzhou 51.760. china 1. Institute of Oceanology Chinese Academy of Sciences 266071 Qingdao China 2. key Lab of {1. Sedimentology and Environmental geology First Institute of Oceanograpgy State Oceanic Administration 266061 Qingdao China 3. Graduate School Chinese Academy of Sciences 100039 Beijing China 4. Modern Analysis Center Nanjing University 210093 Nanjing China 5. Guangzhou marine Investigation Bureau 510760 Guangzhou China

Fifty-six samples of nannofossil ooze were collected from Core PC5794 in the northern equatorial Pacific at 5 cm intervals. With the methods of mass spectrometer (VG354) and ICP, the Nd isotopic compositions (εNd(t)), Mn contents and Mg/Sr ratios of carbonate phase have been analyzed. CaCO3 contents of bulk sediments were obtained by dissolution of 0.5 mol/L HCl. Based on these data, the high-resolution εNd(t) profile of seawater in early Miocene with core depth(or time) have been established. The values of εNd(t) range from -6.2 to -2.97 and 4 fluctuation cycles existed during 24.06-22.02 Ma. 4 low εNd(t) values (about -6.4) correspond to high CaCO3 contents, which implicates that there were 4 cold epochs or 4 times of Antarctic Bottom Water activity. They occurred at the time of 24.06 Ma, 23.85 Ma,22.88 Ma and 22.26 Ma, respectively. High εNd(t) values correspond to the high Mn contents and high values of Mg/Sr ratio, which indicates the existence of 4 intense hydrothermal activity periods during 24.06-22 Ma, the durations of them are 4.05-23.98 Ma, 23.69-23.1. Ma, 22.74-22.37 Ma and 22.06-22.02 Ma, respectively.

关键词：同位素钕示踪原子海水演化中新世太平洋微化石分光计持续期海水样品

Paleoceanographic records and sea ice extension history on the slope of the northern Bering Sea over the last 1.0 ka B.P.

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Acta Oceanologica Sinica 2005年第6期24卷 117-126页

作者： wang {1. LI Xia XIAO Wenshen XIA Peifen chen ronghua state {1. laboratory of marine geology Tongji University Shanghai 200092China State Key Laboratory of Marine Geology Tongji University Shanghai 200092China State Key Laboratory of Marine Geology Tongji University Shanghai 200092China State Key Laboratory of Marine Geology Tongji University Shanghai 200092China Key Laboratory of Submarine Geoscience State Oceanic Administration Hangzhou 310012China

Quantitative analytic results of the biogenic components in Core B2-9 fromthe northern Bering Sea slope indicate that the coarse fraction and opal content, serving as proxiesof surface productivity, have increased stepwise since the marine isotope stageCMISJS.S, reflectingperiodic enhancement in surface *** surface productivity attained its highest levelduring the Holocene, followed by MIS 3.2 to 2 and then MIS 5.3 to 3.3 with a lowest level. Hightotal organic carbon(TOC) contents, together with high C/N ratios, which stand mostly between 7 and20, show that the TOC was deposited from mixing sources. Therefore,one has to be cautious to use TOCas a proxy of surface *** high TOC and C/N ratio during MIS 5.1. 3.3 to 3.2 and theHolocene reflect that the terrigenous organic matter input increased during *** in the fine- and silt-grained terrigenous components from MIS 5.3 to the middleHolocene imply that with the cooling climate, sea ice on the Bering Sea slope extended ***-rafted and charcoal detritus increased during glacial, interstadial and the last deglaciationperiods and decreased during interglacial periods, suggesting that sea ice on the slope increasedand melted, respectively, during glacial and interglacial periods. The extension of sea ice duringglacial *** was linked with the climate over the North American Continent, responded toglobal climate change during late Quaternary glacial and interglacial cycles.

关键词： surface productivity ice-rafted detritus sea ice extension history latequaternary bering sea

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海相碳酸盐岩烃源岩的研究进展

天然气工业 2004年第8期24卷 21-23页

作者：王杰陈践发中国科学院兰州地质研究所气体地球化学重点实验室

文章就碳酸盐岩烃源岩有机质丰度下限标准、有机质的赋存形式、生烃机制与生烃模式等方面的研究现状、主要进展进行讨论。目前对有机质丰度下限认识不一 ,石油勘探部门所采用的标准也很低 ,应用效果不理想 ,进而提出以 0 .5 %作为下限标... 详细信息

文章就碳酸盐岩烃源岩有机质丰度下限标准、有机质的赋存形式、生烃机制与生烃模式等方面的研究现状、主要进展进行讨论。目前对有机质丰度下限认识不一 ,石油勘探部门所采用的标准也很低 ,应用效果不理想 ,进而提出以 0 .5 %作为下限标准 ,现场应用效果很好。在成岩演化过程中 ,不同赋存形式的有机质相互转变 ,在不同演化阶段的生烃量和生烃类型也存在较大差异。生烃模式的研究主要采用干法、加水以及小玻管热模拟实验 ,提出了“三段式”生烃模式 ,发现不同赋存状态的有机质地球化学特征不同。文章对于一些碳酸盐岩生烃研究热点问题的讨论希冀引起人们对碳酸盐岩生烃问题的关注 ,进而推动我国海相碳酸盐岩的基础理论研究。

关键词：海相碳酸盐岩烃源岩丰度有机质油气勘探含油气盆地

High-resolution carbon isotope record for the Paleocene-Eocene thermal maximum from the Nanyang Basin,Central china

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High-resolution carbon isotope record for the Paleocene-Eoce...