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| 1 | Climatology and Interannual Variability of the Southeast Asian Summer Monsoon显示文摘ClimatologyandInterannualVariabilityoftheSoutheastAsianSummerMonsoonK.-M.LauLaboratoryforAtmospheres,Code913,NASA-GoddardSpac... | K. M. Lau Song Yang | 1997 | Advances in Atmospheric Sciences1997，14，2： | 123 |
| 2 | The first offshore natural gas hydrate production test in South China Sea显示文摘Natural gas hydrates (NGH)is one of key future clean energy resources.Its industrialized development will help remit the huge demand of global natural gas,relieve the increasing pressure of the environment, and play a vital role in the green sustainable growth of human societies.Based on nearly two decades' studying on the reservoir characteristics in the South China Sea (SCS)and the knowledge of reservoir system,the China Geological Survey (CGS)conducted the first production test on an optimal target selected in Shenhu area SCS in 2017.Guided by the 'three-phase control'exploitation theory which focused on formation stabilization,technologies such as formation fluid extraction,well drilling and completing, reservoir stimulating,sand controlling,environmental monitoring,monitoring and preventing of secondary formation of hydrates were applied.The test lasted for 60 days from May 10^th when starting to pump, drop pressure and ignite to well killing on July 9^th,with gas production of 3.09×10^5 m^3 in total,which is a world record with the longest continuous duration of gas production and maximal gas yield.This successful test brings a significant breakthrough on safety control of NGH production. | Jin-fa Li Jian-liang Ye Xu-wen Qin Hai-jun Qiu Neng-you Wu Hai-long Lu Wen-wei Xie Jing-an Lu Fei Peng Zhen-qiang Xu Cheng Lu Zeng-gui Kuang Jian-gong Wei Qian-yong Liang Hong-feng Lu Bei-bei Kou | 2018 | China Geology2018，1，1： | 117 |
| 3 | 战略环境评价(SEA)及其研究进展显示文摘战略环境评价 ( SEA)是目前环境评价领域中令人关注的前沿课题 .本文对 SEA的提出和发展进行了回顾 ,对国外开展SEA的实践进行了归纳分析 ,探讨了 SEA的作用、区域特征、评价因素、基本程序、技术方法和机制 ,论述了 SEA与项目 EIA的关系 ,并介绍了香港和内地 SEA的初步实践 . | 马蔚纯 林健枝 陈立民 余澍滨 | 2000 | 环境科学2000，21，5： | 65 |
| 4 | 城市化进程中的战略环境评价(SEA)初探显示文摘城市化是中国现代化进程中面临的一个重要问题。21世纪初期,中国城市化发展将进入快速发展的关键时期。开展城市化进程中的SEA,即在城市化决策的各个层次前瞻性地考虑政策、规划、计划及其替代方案的环境影响,有助于提高决策质量和实施可持续发展。文章对城市化进程中SEA的概念、对象、评价目标、评估指标体系和评价方法进行了初步探讨,并提出城市化进程中SEA的基本程序。 | 车秀珍 尚金城 陈冲 | 2001 | 地理科学2001，21，6： | 52 |
| 5 | Deep water bottom current deposition in the northern South China Sea显示文摘There are some active bottom currents on the northern continental slope of the South China Sea (SCS). Reflection seismic profiles show that the bottom current channels occur in the water depth range of 1000 to 2700 m,extending from the NE to the SW,leading to accumulation of discontinuous drifts with higher sedimentation rates on the eastern side of the channel. The stacking pattern of the layers sug-gests that these drifts propagated southwestward,following the direction of the bottom currents. One sedimentary drift to the southeast of the Dongsha Islands has the highest sedimentation rate of 97cm/ka in the last 12 ka. The sedimentary characteristics of the sediment layers indicate that these bottom currents are most likley caused by the water movement of a branch of the West Pacific Ocean Current,which enters the northern SCS via the Bashi Strait. Once formed,the bottom currents trans-port sediments along the northern slope of SCS southwestward and finally disappear into the central basin of the SCS. Due to the bottom current activity,the deep-sea sedimentary process in the northern SCS is complex. | SHAO Lei LI XueJie GENG JianHua PANG Xiong LEI YongChang QIAO PeiJun WANG LiaoLiang WANG HongBin | 2007 | Science China Earth Sciences2007，50，7： | 43 |
| 6 | Phytoplankton community structure and environmental parameters in aquaculture areas of Daya Bay,South China Sea显示文摘Environmental characteristics and phytoplankton community structure were investigated in two aquaculture areas in Dapeng Cove of Daya Bay,South China Sea,between April 2005 and June 2006.Phytoplankton abundance ranged between 5.0 and 8877.5 cells/mL,with an average of 751.8 cells/mL.The seasonal cycle of phytoplankton were demonstrated by frequent oscillations,with recurrent high abundances from late spring to autumn and a peak stage in late winter.Diatoms were the predominant phytoplankton group,accounting for 93.21%of the total abundance.The next most abundant group was the dinoflagellates,which made up only 1.24%of total abundance. High concentrations of Alexandrium tamarense(Lebour) Balech with a maximum of 603.0 cells/mL were firstly recorded in this area known for high rates of paralytic shellfish poisoning(PSP) contamination.Temperatures and salinities were within the suitable values for the growth of phytoplankton,and were important in phytoplankton seasonal fluctuations.The operation of the Daya Bay Nuclear Power Station(DNPS) exerts influences on the phytoplankton community and resulted in the high abundances of toxic dinoflagellate species during the winter months.Dissolved inorganic nitrogen(DIN) and dissolved silicate(DSi) were suffcient,and rarely limited for the growth of phytoplankton.Dissolved inorganic phosphorus(DIP) was the most necessary element for phytoplankton growth. The enriched environments accelerated the growth of small diatoms,and made for the shift in predominant species from large diatom Rhizosolenia spp.to chain-forming diatoms such as Skeletonema costatum,Pseudo-nitzschia spp.and Thalassiosira subtilis. | WANG Zhaohui ZHAO Jiangang ZHANG Yujuan CAO Yu | 2009 | Journal of Environmental Sciences2009，21，9： | 44 |
| 7 | Arctic Sea Ice Decline Intensified Haze Pollution in Eastern China显示文摘Air quality in eastern China has becoming more and more worrying in recent years, and haze is now No.1 air pollution issue. Results in this study show the decreasing Arctic sea ice(ASI) is an important contributor to the recent increased haze days in eastern China. The authors find that the number of winter haze days(WHD) in eastern China is strongly negatively correlated with the preceding autumn ASI during 1979–2012, and about 45%– 67% of the WHD interannual to interdecadal variability can be explained by ASI variability. Following previous studies on the impact of ASI loss on the northern hemisphere climate, the authors' studies further reveal that the reduction of autumn ASI leads to positive sea-level pressure anomalies in mid-latitude Eurasia, northward shift of track of cyclone activity in China, and weak Rossby wave activity in eastern China south of 40N during winter season. These atmospheric circulation changes favor less cyclone activity and more stable atmosphere in eastern China, leading to more haze days there. Furthermore, the patterns of circulation changes associated with autumn ASI and WHD are in very good agreement over the East Asia, particularly in eastern China. The authors suggest that haze pollution may continue to be a serious issue in the near future as the decline of ASI continues under global warming. | WANG Hui-Jun CHEN Huo-Po LIU Jiping | 2015 | Atmospheric and Oceanic Science Letters2015，8，1： | 43 |
| 8 | A three-dimensional variational ocean data assimilation system:Scheme and preliminary results显示文摘A new 3DVAR-based Ocean Variational Analysis System (OVALS) is developed. OVALS is capable of assimilating in situ sea water temperature and salinity observations and satellite altimetry data. As a component of OVALS, a new variational scheme is proposed to assimilate the sea surface height data. This scheme considers both the vertical correlation of background errors and the nonlinear temperature-salinity relationship which is derived from the generalization of the linear balance constraints to the nonlinear in the 3DVAR. By this scheme, the model temperature and salinity fields are directly adjusted from the altimetry data. Additionally, OVALS can assimilate the temperature and salinity profiles from the ARGO floats which have been implemented in recent years and some temperature and salinity data such as from expendable bathythermograph, moored ocean buoys, etc. A 21-year assimilation experiment is carried out by using OVALS and the Tropical Pacific circulation model. The results show that the assimilation system may effectively improve the estimations of temperature and salinity by assimilating all kinds of observations. Moreover, the root mean square errors of temperature and salinity in the upper depth less than 420 m reach 0.63℃ and 0.34 psu. | ZHU Jiang1,2, ZHOU Guangqing1, YAN Changxiang1, FU Weiwei1 & YOU Xiaobao1,3 1. International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China 2. Jiangsu Key Laboratory of Meteorological Disaster, Nanjing University of Information Science and Technology, Nanjing 210044, China 3. Beijing Institute of Applied Meteorology, Beijing 100029, China | 2006 | Science China Earth Sciences2006，49，11： | 35 |
| 9 | A numerical study of the South China Sea deep circulation and its relation to the Luzon Strait transport显示文摘A fine-resolution MOM code is used to study the South China Sea basin-scale circulation and its relation to the mass transport through the Luzon Strait. The modal domain includes the South China Sea, part of the East China Sea, and part of the Philippine Sea so that the currents in the vicinity of the Luzon Strait are free to evolve. In addition, all channels between the South China ,Sea and the Indonesian seas are closed so that the focus is on the Luzon Strait transport. The model is driven by specified Philippine Sea currents and by surface heat and salt flux conditions. For simplicity, no windstress is applied at the surface.The simulated Luzon Strait transport and the South China Sea circulation feature a sandwich vertical structure from the surface to the bottom. The Philippine Sea water is simulated to enter the South China Sea at the surface and in the deep ocean and is carried to the southern basin by western boundary currents. At the intermediate depth, the net Luzon Strait transport is out of the South China Sea and is fed by a western boundary current flowing to the north at the base of the thermocline. Corresponding to the western boundary currents, the basin circulation of the South China Sea is cyclonic gyres at the surface and in the abyss but an anti-cyclonic gyre at the intermediate depth. The vorticity balance of the gyre circulation is between the vortex stretching and the meridional change of the planetary vorticity.Based on these facts, it is hypothesized that the Luzon Strait transports are determined by the diapycnal mixing inside the entire South China Sea. The South China Sea plays the role of a 'mixing mill' that mixes the surface and deep waters to return them to the Luzon Strait at the intermediate depth. The gyre structures are consistent with the Stommel and Arons theory (1960), which suggests that the mixlng-induced circulation inside the South China Sea should be cyclonic gyres at the surface and at the bottom but an anti-cyclonic gyre at the intermediate depth. The simulated gyre circulation at the intermediate depth has been confirmed by the dynamic height calculation based on the Levitns hydrography data.The sandwich transports in the Luzon Strait are consistent with recent hydrographic, al observations.Model results suggest that the Kuroshio tends to form a loop current in the northeastern South China Sea. The simulated Kuroshio Loop Current is generated by the pressure head at the Pacific side of the Luzon Strait and is enhanced by theβ- plane effects. The β- plane appears to be of paramount importance to the South China Sea circulation and to the Luzon Strait translports. Without theβ-plane, the Luzon Strait transports would be greatly reduced and the South China Sea circulation would be complete-ly different. | Yuan Dongliang1. Goddard Earth Science and Technology Center, University of Maryland, Baltimore County Code 971, Laboratory for Hydrospheric Processes, NASA/Goddard Space Flight Center, Greenbelt, MD 20771, USA | 2002 | Acta Oceanologica Sinica2002，21，2： | 37 |
| 10 | Influence of interannual variability of Antarctic oscillation on mei-yu along the Yangtze and Huaihe River valley and its importance to prediction显示文摘Both correlation analysis and case study indi-cate that Antarctic oscillation (AAO) is closely related withsummer rainfall in eastern China. When AAO is stronger inboreal spring, especially in May, there is more mei-yu rain-fall in summer with a longer period along the Yangtze andHuaihe River valley. In contrast, there is less rainfall with ashorter period corresponding to a weaker AAO. Besides, ananomalous AAO changes the position and intensity of severalcirculation systems, which are important to summer rainfallalong the Yangtze and Huaihe River valley. Furthermore, theAntarctic sea ice is negatively correlated with the intensity ofAAO with a 6-month leading time. The result in this studyprovides a new method for the prediction of mei-yu. | GAO Hui~(1,2), XUE Feng~1 WANG Huijun~1 1. Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China 2. Department of Atmospheric Sciences, Nanjing Institute of Meteorology, Nanjing 210044. China | 2003 | Chinese Science Bulletin2003，48，S2： | 34 |
| 11 | Influence of South China Sea SST and the ENSO on Winter Rainfall over South China显示文摘The present study investigates the influence of South China Sea (SCS) SST and ENSO on winter (January-February-March; JFM) rainfall over South China and its dynamic processes by using station observations for the period 1951-2003, Met Office Hadley Center SST data for the period 1900-2008, and ERA-40 reanalysis data for the period 1958-2002. It is found that JFM rainfall over South China has a sig- nificant correlation with Nio-3 and SCS SST. Analyses show that in El Nio or positive SCS SST anomaly years, southwesterly anomalies at 700 hPa dominate over the South China Sea, which in turn transports more moisture into South China and favors increased rainfall. A partial regression analysis indicates that the independent ENSO influence on winter rainfall occurs mainly over South China, whereas SCS SST has a larger independent influence on winter rainfall in northern part of South China. The temperature over South China shows an obvious decrease at 300 hPa and an increase near the surface, with the former induced by Nio-3 and the latter SCS SST anomalies. This enhances the convective instability and weakens the potential vorticity (PV), which explains the strengthening of ascending motion and the increase of JFM rainfall over South China. | 周连童 Chi-Yung TAM 周文 Johnny C. L. CHAN | 2010 | Advances in Atmospheric Sciences2010，27，4： | 34 |
| 12 | Major element,trace element,and Sr,Nd and Pb iso-tope studies of Cenozoic basalts from the South China Sea显示文摘The whole rock K-Ar ages of basalts from the South China Sea basin vary from 3.8 to 7.9 Ma, which suggest that intra-plate volcanism after the cessation of spreading of the South China Sea (SCS) is comparable to that in adjacent regions around the SCS, i.e., Leiqiong Peninsula, northern margin of the SCS, Indochina block, and so on. Based on detailed petrographic studies, we selected many fresh ba-saltic rocks and measured their major element, trace element, and Sr-Nd-Pb isotope compositions. Geochemical characteristics of major element and trace element show that these basaltic rocks belong to alkali basalt magma series, and are similar to OIB-type basalt. The extent of partial melting of mantle rock in source region is very low, and magma may experience crystallization differentiation and cu-mulation during the ascent to or storing in the high-level magma chamber. Sr-Nd-Pb isotopic data of these basaltic rocks imply an inhomogeneous mantle below the South China Sea. The nature of magma origin has a two end-member mixing model, one is EM2 (Enriched Mantle 2) which may be originated from mantle plume, the other is DMM (Depleted MORB Mantle). Pb isotopic characteristics show the Dupal anomaly in the South China Sea, and combined with newly found Dupal anomaly at Gakkel ridge in Arctic Ocean, this implies that Dupal anomaly is not only limited to South Hemisphere. In variation diagrams among Sr, Nd and Pb, the origin nature of mantle below the SCS is similar to those below Leiqiong peninsula, northern margin of the SCS and Indochina peninsula, and is different from those below north and northeast China. This study provides geochemical constraints on Hainan mantle plume. | YAN QuanShu SHI XueFa WANG KunShan BU WenRui XIAO Long | 2008 | Science China Earth Sciences2008，51，4： | 33 |
| 13 | 战略环境影响评价(SEA)在中国的开展—区域环境评价(REA)显示文摘实践和研究表明 :传统的环境影响评价 (EIA) ,即在项目层次上开展的EIA ,不尽完美。而包含有战略环境影响评价的新一代EIA体系将很好的弥补项目EIA的不足 ,并且将可持续发展的思想真正贯彻到实际中去。中国在开展环境影响评价方面 ,也逐渐注重两个层次上EIA的开展 ,特别是结合当前发展的新特点 ,开展了区域环境影响评价。文章论证了区域环境评价 ,无论从层次上 ,还是从评价的对象、内容上都是属于战略环境影响的形式。并基于这个观点 ,介绍了区域环评在中国的开展及今后发展应注意的一些问题。 | 徐鹤 朱坦 贾纯荣 | 2000 | 城市环境与城市生态2000，13，3： | 32 |
| 14 | 海参的营养成分介绍显示文摘 | 李春艳 常亚青 | 2006 | 科学养鱼2006，28，2： | 30 |
| 15 | Episodic rifting of continental marginal basins and tectonic events since 10 Ma in the South China Sea显示文摘Integrated study on the tectonic, basin filling and thermal evolution of the Tertiary basins on the northern margin of the South China Sea has indicated that the rift continental margin on the northern South China Sea is not a passive margin and that the western margin is characteristic of the transformextension. Episodic rifting and the thermal events since 10 Ma in the area have been documented by the integrated analysis of dynamic process. It has been clarified that the tectono-thermal events have exerted a significant influence on basin features and hydrocarbon accumulation, and particularly, the westward collision of the Lusong Island Arc, the generation of densely spaced faults in the Pearl River Mouth Basin, the rapid subsidence, high heat flow and large-scale over pressure and thermal-fluid breakthrough in the Yinggehai and the Qiongdongnan basins have proved to be the important factors determining the formation of oil and gas in these basins. | Sitian Li Changsong Lin Qiming Zhang Shigong Yang Peikan Wu | 1999 | Chinese Science Bulletin1999，44，1： | 27 |
| 16 | 日本血吸虫成虫及虫卵可溶性抗原的早期诊断分子筛选显示文摘为获取有效的日本血吸虫病早期诊断靶抗原分子。以感染前和感染后2周、4周、6周兔混合血清以及急性、慢性日本血吸虫病人和正常人血清,用Westernblot对日本血吸虫成虫可溶性抗原(AWA)和虫卵可溶性抗原(SEA)进行了全面的分析与筛选。SEA140kDa和AWA54kDa、21kDa、20kDa分子出现最早,能被感染后2周兔血清所识别;SEA69kDa、50kDa、45kDa、38kDa和AWA72kDa、45kDa、34kDa、15kDa相继能被感染后4周兔血清所识别;其中SEA140kDa、50kDa、45kDa、38kDa和AWA34kDa、21kDa、54kDa、15kDa与病人血清反应同6周兔血清反应效果相仿,均为免疫反应主带,且在SDS-PAGE上有对应的蛋白主带,具有潜在的早期诊断价值。进一步对SEA进行抗体类型的分析,发现SEA能刺激机体产生IgG、IgM和IgA反应,其中SEA50kDa、45kDa、38kDa三个抗原分子均能被IgG、IgM、IgA三种抗体所识别,且均为反应主带;SEA140kDa以IgM反应带最深;SEA100kDa反应带仅出现于病人血清,以IgM反应最强,且其与IgM反应带在急性病人血清明显深于慢性病人血清,表明针对IgM的SEA100kDa分子也具有一定的早期诊断和区分病程的价值。SEA140kDa、50kDa、45kDa、38kDa和AWA34kDa、21kDa、54kDa、15kDa和针对IgM的SEA100kDa分子是具有潜在早期诊断价值的优势靶抗原分子。 | 周晓红 陈晓光 冯明钊 李华 刘国章 | 2000 | 寄生虫与医学昆虫学报2000，7，1： | 27 |
| 17 | HbH病患儿临床表现与基因型相关性的研究显示文摘目的 探讨血红蛋白H(HbH)病患儿的基因型在预测该病临床表现中的价值以及影响该病进程的因素。方法 采用已建立的技术和方法检测 4 3例珠海市户籍HbH病患儿的基因型 ,测定其所有的血液学指标并详细记录其临床资料 ,分析其基因型与临床表现的关系。结果 4 3例HbH病患儿中 ,检出 6种α 地中海贫血基因并相互组合产生 5种HbH病基因型 ,其中 α3 7/ SEA(2 6例 ,6 0 % )、 α4 2 / SEA(8例 ,19% )和αCSα/ SEA(5例 ,12 % )是该地区人群中 3种主要的HbH病分子缺陷类型。与 α3 7/ SEA相比 ,非缺失型 (αTα/ SEA)HbH病患儿的红细胞计数 (RBC)、血红蛋白 (Hb)、红细胞平均血红蛋白浓度 (MCHC)和血红蛋白A2 (HbA2 )值偏低 (P <0 0 5、0 0 1、0 0 1和 0 0 1) ,而红细胞平均体积 (MCV)和HbH水平则偏高 (P <0 0 1) ,且有较严重的临床表现。而与 α4 2 / SEA组相比 ,αTα/ SEA无论在血液学指标上 ,还是临床表现上的差异均不及与 α3 7/ SEA组比较为显著。并发现HbH水平与红细胞计数呈负相关 (r=- 0 39,P <0 0 0 1)。结论 HbH病患儿的临床表现主要与α 珠蛋白的基因型有关 ,αTα/ SEA型HbH病患儿有更严重的临床和血液学表现 , α4 2 / SEA次之 , α3 7/ SEA居末。 | 周玉球 肖奇志 黄丽娟 肖鸽飞 李文典 朱兰芳 陈紫霞 张玉梅 | 2004 | 中华儿科杂志2004，42，9： | 25 |
| 18 | North Pacific sea ice cover, a predictor for the Western North Pacific typhoon frequency?显示文摘The relationship between the sea ice cover in the North Pacific and the typhoon frequency has been studied in this paper. It follows that the index for the sea ice cover in the North Pacific (ISA) both in December-January-February (DJF) and in March-April-May (MAM) is negatively correlated with annual typhoon number over the western North Pacific (TNWNP) during 1965―2004, with correlation coeffi-cients of -0.42 and -0.49 respectively (above 99% significant level). Large sea ice cover in the North Pacific tends to decrease TNWNP. Positive ISA (MAM) is associated with the tropical circulation and SST anomalies in the North Pacific, which may lead to unfavorable dynamic and thermal conditions for typhoon genesis over WNP from June to October (JJASO). The variability of the atmospheric circula-tion over the North Pacific, associated with the ISA anomaly in MAM is connected to the tropical at-mospheric circulation variability in MAM via the teleconnection wave train. Besides, as the tropical circulation has strong seasonal persistency from the MAM to JJASO, thus, the ISA in MAM-related variability of the tropical atmospheric circulation as well as the SST can affect the typhoon activity over the western North Pacific. | FAN Ke Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China Department of Atmospheric Science, Yun-nan University, Kunming 650091, China | 2007 | Science China Earth Sciences2007，50，8： | 25 |
| 19 | Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene显示文摘AMS14C dating and analysis of grain size,major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea.Based on the environmentally sensitive grain size,clay mineral and major element assemblages,the history of the East Asia winter monsoon since the mid-Holocene could be reconstructed.These three proxies,mean grain size(>9.71μm),chemical index of alteration(CIA)and ratio of smectite to kaolinite in particular,show similar fluctuation patterns. Furthermore,10 extreme values corresponding to the contemporary cooling events could be recognized since the mid-Holocene;these extreme values are likely to have been caused by the strengthening of the East Asia winter monsoon.The cooling events correlated well with the results of theδ18O curves of the Dunde ice core and GISP2,which therefore revealed a regional response to global climate change.Four stages of the East Asia winter monsoon were identified,i.e.8300-6300 a BP,strong and unstable;6300-3800 a BP,strong but stable;3800-1400 a BP,weak and unstable;after 1400 a BP,weak but stable. | LIU ShengFa SHI XueFa LIU YanGuang QIAO ShuQing YANG Gang FANG XiSheng WU YongHua LI ChaoXin LI XiaoYan ZHU AiMei GAO JingJing | 2010 | Chinese Science Bulletin2010，55，21： | 25 |
| 20 | Late Quaternary clay minerals off Middle Vietnam in the western South China Sea: Implications for source analysis and East Asian monsoon evolution显示文摘High-resolution clay mineral records combined with oxygen isotopic stratigraphy over the past 450 ka during late Quaternary from Core MD05-2901 off Middle Vietnam in the western South China Sea are re-ported to reconstruct a history of East Asian monsoon evolution. Variations in Illite, chlorite, and kaolinite contents indicate a strong glacial-interglacial cyclicity, while changes in smectite content present a higher frequency cyclicity. The provenance analysis indicates a mixture of individual clay minerals from various sources surrounding the South China Sea. Smectite derived mainly from the Sunda shelf and its major source area of the Indonesian islands. Illite and chlorite originated mainly from the Mekong and Red rivers. Kaolinite was provided mainly by the Pearl River. Spectral analysis of the kaolin-ite/(illite+chlorite) ratio displays a strong eccentricity period of 100 ka, implying the ice sheet-forced win-ter monsoon evolution; whereas higher frequency changes in the smectite content show an ice sheet-forced obliquity period of 41 ka, and precession periods of 23 and 19 ka and a semi-precession period of 13 ka as well, implying the tropical-forced summer monsoon evolution. The winter monsoon evolution is generally in coherence with the glacial-interglacial cyclicity, with intensified winter monsoon winds during glacials and weakened winter monsoon winds during interglacials; whereas the summer monsoon evolution provides an almost linear response to the summer insolation of low latitude in the Northern Hemisphere, with strengthened summer monsoon during higher insolation and weakened summer monsoon during lower insolation. The result suggests that the high-latitude ice sheet and low-latitude tropical factor could drive the late Quaternary evolution of East Asian winter and summer monsoons, respectively, implying their diplex and self-contained forcing mechanism. | Christophe COLIN | 2007 | Science China Earth Sciences2007，50，11： | 24 |
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