长江中游湖泊沉积微结构特征与沉积环境

易朝路; 吴显新; 刘会平; 王柏轩; 许厚泽

长江中游湖泊沉积微结构特征与沉积环境

1.
南京大学城市与资源学系南京 210093;
2.
中国科学院水生生物研究所东湖生态实验站武汉 430073;
3.
华中师范大学地理系武汉 430071;

基金项目: 国家自然科学基金(批准号:49501003和49971081);中国科学院水生生物研究所东湖生态实验站(200105);中国科学院‘九五'重大项目ZK951A12020103资助

详细信息

作者简介:
易朝路,男,1959年出生,博士,研究,员第四纪地质与地貌

中图分类号: P512.2

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Microfabric Properties of Lacustrine Sediments and Sedimentary Environments

1.
Nanjing university, Nanjing 210093;
2.
Donghu experi mental station of ecology, Chinese academy of sciences, Wuhan 430073;
3.
Depart ment of geography, Central China Nor mal university, Wuhan 430071;
4.
Instit ute of environmental geosciences, China university of geosciences, Wuhan 430073

摘要

摘要: 在长江中游的洪湖、东湖、网湖和大九湖等四个地点取得湖沼沉积物的钻孔样品,用偏光显微镜下和电子显微镜观察微结构特征并以此解释三种湖相粘土的成因和沉积环境的变化。在长江沿岸湖泊中,0.4~ 0.5kaBP以来形成的浅色粘土的微结构类型主要有 :显微层理构造、颗粒的定向性、较大的微孔隙和颗粒粒径,面与面或边与边接触方式。物源主要来自河流带来的泥沙.当时河湖相通,河流入湖水沙量大。 1~ 2.5kaBP期间形成的青色粘土的典型微结构是 :凝胶结构、絮凝结构、细颗粒粒径和小孔隙、低球度和淡水中心冈硅藻。主要是有机质胶体与粘土胶体相互作用形成的。此期间,河流带入湖泊的泥沙少,江汉平原拥有一个开阔、稳定、浮游生物较多的淡水湖泊环境。 0.4~ 1kaBP期间形成的黑色粘土的主要微结构类型是 :凝胶结构、大的圆孔隙和植物纤维的生物框架结构、呈双峰分布的孔隙。它主要是由于维管束植物残体大量积累形成的。当时江汉平原湖泊湖水变浅,大量挺水植物生长,有些湖泊沼已经沼泽化了。鱼骨框架结构证明,在 2.9~ 4kaBP的全新世温暖期山间盆地大九湖出现大量鱼类,但并没有导致喜温鱼类向上游明显迁徙。
- 微结构 /
- 湖相粘土的成因 /
- 环境变化 /
- 长江中游 /
- 东湖 /
- 洪湖 /
- 网湖 /
- 大九湖
Abstract: Mircrofabrics from core sediments were observed in polarizing microscope and scanning microscope and used in interpreting the origin of three types of clay as well as the changes of sedimentary environments in four sites-the Honghu Lake,the Donghu Lake,the Wanghu Lake and the Dajiuhu Lake along the middle reach of the Yangtze River.Micro-beddings,orientation of particles and large sizes of micro-voids and particles with contacting patterns of face to face or edge to edge occurred in the light-colored clay formed since 0.4～0.5ka BP in the lakes.Their origin was ascirbed to clastic sediments from rivers surrounding the lakes.It was suggested that the lakes were connected with rivers and large amount of sedimens came from rivers into the lakes during that period.The typical microfabrics in the blue clay formed in 1～2.5ka BP were gelatinous texture,agglutinational texture,small sizes of particles and voids,low sphericity and diatoms of freshwater Class Centrium .Their origin was ascribed to the result of the interaction between organic colloids and clay colloids.It was suggested that the lakes in the Jianghan plain were of open and stable fresh water lake environments rich in planktons and with small amount of clay carried by rivers during this period.The main microfabrics in the black clay formed during 0.4～1ka Bp were gelatinous texture,large circular voids and plant fiber.The voids had a bimodal distribution.The sediment was formed mainly due to the accumulation of large amount of aquatic vascular bundle plants.It was suggested that the lakes were shallow and rich in aquatic vascular bundle plants,and some of them were swamping.The framework of fish bone in the sediments indicated that there was large number of fish in the Dajiuhu area during the Holocene warm period of 2.9～4ka BP,but the thermophilous fish did not migrate upwards apparently.
- microfabric /
- origin of lacustrine clay /
- environmental changes /
- the middle reach of the Yangtze River /
- Donghu Lake /
- Honghu Lake /
- Wanghu Lake /
- Dajiuhu Lake

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参考文献(1)

[1]

1. Gilbert J E.Study of the fabric of fine-grained sediments with the scanning electron microscope[J].Journal of Sedimentary Petrology,1969,39（1）: 90～105

2. Bennett R H,Bryant W R,Kller G H.Clay fabric of selected submarine sediment: fundamental properties and models[J].Journal of Sedimentary Petrology,1981,51: 217～232

3. Kuehl S A,Nittrouer C A,Demaster D J.Microfabric study of fine grained sediments: observations from the Amazon subaqueous delta[J].Journal of Sedimentary Petrology,1988,58（1）: 12～23

4. Reynolds S,Gorsline D S.Clay microfabric of deep-sea detrital mudstones,California continental borderland[J].Journal of Sedimentary of Petrology,1991,62（1）: 41～53

5. 方小敏，沈明智，牟昀智。武都泥石头流显微构造极其形成机制初探[J].中国科学（B辑），1991,21（2）:198～204 [ Fang Xiaomin,Shen Mingzhi,Mou Yunzhi.Preliminary studies on the microstructures of mud-rock flow and its formation mechanism in Wudou[J].Science in China （B series）。1991,21（2）: 198～204]

6. Van der Meer J J M.Microscopic evidence of subglacial deformation[J].Quaternary Science Reviews,1993,12: 553～587

7. C -L Yi.Subglacial comminution in till-evidence from microfabric studies and grain size analysis[J].Journal of Glaciology,1997,43（14）:1～7

8. Tang Z H,Parnell J,Ruffell A H.Deposition and diagenesis of the lacustrine-fluvial Cangfanggou Group （uppermost Permian to Lower Triassic），southern Junggar Basin,NW China: a contribution from sequence stratigraphy[J].Journal of Paleolimnology,1994,11: 67～90

9. Peter A G,et al.The Holocene history of West Basin Lake,Victoria,Australia; chemical changes based on fossil biota and sediment mineralogy[J].Journal of Paleolimnology,1994,12（3）: 235～258

10. Sack A,Last W M.Lithostratigraphy and recent sedimentation history of Little Manitoba Lake,Saskatchewan,Canada[J].Journal of Paleolimnology,1994,10: 199～212

11. Edund M B,Stoermer E F.Resting spores of the freshwater diatoms Acanthoceras and Urosolenia[J] .Journal of Paleolimnology,1993,9: 95～61

12. Valero-Garc e′ s B L,Kelts K R.A sedimentary facies for perennial and meromictic saline lakes: Holocene Medicine Lake Basin,South Dakota,USA[J].Journal of Paleolimnology,1995,14: 123～149

13. George H.Characteristics of varved clays of the Elk valley,British Columbian,Canada[J].Engineering Geology,1986,23: 59～74

14. Defarge C,et al.Texture of microbial sediments revealed by cryo-scanning electron microscopy[J].Journal of Paleolimnology,1996,66（5）: 935～947.

15. Lamoureuxand S F,Bradley R S.A late Holocene varved sediment record of environmental change from northern Ellesmere Island,Canada[J].Journal of Paleolimnology,1996,16: 239～255

16. 李世杰，郑本新，焦克勤。西昆仑山区湖泊初探[J].海洋与湖沼，1993,24（1）: 37～44 [ Li Shijie,Zheng Benxin,Jiao Keqin.Priliminary study on the lakes in western Kunlun Mountains[J].Oceanology and Limnology,1993,24（1）: 37～44]

17. 王苏民，薛滨。中国全新世以来若尔盖盆地环境演化与黄土高原比较研究[J].中国科学，1996,26（2）: 323～328 [Wang Sumin,Xue Bin.Comparative study of the evolution of Ruoergai basin and Huangtu Plateau since the Holocene[J].Science in China （D series），1996,26（2）:323～328]

18. 王苏民，薛滨，夏威岚。希门错2000多年来气候变化的湖泊记录[J].第四纪研究，1997,2:62～69 [Wang Sumin,Xue Bin,Xia Weilan.Lake record of climatic change in the past 2000 years of Ximen Cuo （lake）[J].Quaternary Research,1997,2:62～69]

19. 吴敬禄，王苏民，施雅风等。若尔盖盆地200ka以来氧同位素记录的古温度定量研究[J].中国科学（D辑），2000,30（1）:73～80 [ Wu Jinlu,Wang Sumin,Shi Yafeng,et al.Quantitative study of oxygen isotope record in Ruoergai basin since 200ka[J].Science in China （D series），2000,30（1）:73～80]

20. 蔡述明，官子和。第四纪跨江南北的古云梦泽是不能成立的[J].海洋与湖沼，1981,13（2）: 130～142 [Cai Shuming,Guan Zihe.Impossible establishment of integrated Yunmen swamp-lake in Jianghan-dongtin basin[J].Oceanology and Limnology,1981,13（2）: 130～142]

21. 王苏民，窦鸿身。中国湖泊志[M].北京: 科学出版社，1998 [Wang Sumin,Du Hongsheng.Record of lakes in China[M].Beijing: Science Press,1998]

22. Cai S M,Yi C L.Sedimentary features and evolution of Honghu Lake,central China[J].Hydrobiologica,1991,214:341～345

23. 杨汉东等。武汉东湖沉积物环境地球化学[J].水生生物学报，1994,18（3）: 208～214 [Yang Handong,et al.Environmental geochemistry of lacustrine sediment in Donghu lake,Wuhan[J].Acta Hydrobiologica,1994,18（3）: 208～214]

24. H-D Yang,B-Y He,S-M Cai et al.Environmental impicatons of magnetic measurements on recent sediments from lake Donghu[J].Water,Air and Soil Pollution,1997,98:187～195

25. 刘会平。神农架地区第四纪植被与古环境[D].同济大学海洋地质与地球物理系。1998 [Liu Huipin.Quaternary vegetation and paleoenvironment in Shenlongjia mountain[D].Department of Geology and Geophysics,Tongji University,Shanghai,1998]

26. Leemann A,Niessen F.Varve formation and the climatic record in an Alpine proglacial lake: calibration annually-laminated sediments against hydrological and meteorological data[J].The Holocene,1994,4: 1～8.

27. Deslodges J R.Varve deposition and sediment record at three small lakes of the southern Canadian Cordillera[J].Arctic and Alpine Research,1994,26: 130～130

28. Pike J,Kemp A E S.Early Holocene decadal-scale ocean variability recorded in Gulf of California laminated sediments[J].Paleoceonography,1997,12（2）: 227～238

29. Pilskaln C H,Johnson T C.Seasonal signals in lake Malavi sediments[J].Limnology and Oceanography,1991,36（3）: 544～557

30. 曹家欣，黄润华，石宁等。上新世湖相纹泥极其环境信息与时间标尺记录[J].第四纪研究。1998,4:353～357 [Cao Jiaxin,Huang Runhua,Shi Ning,Luo Yunli.Late Pliocene lacustrine varves and its environmental information and time mark record[J].Quaternary Research,1998,4:353～357]

31. 王正瑛等。沉积岩结构和构造图谱[M].北京: 地质出版社。1988 [ Wang Zhengying,et al.Atlas of textures and structures of sedimentary rocks[M].Bejing:Geological Publishing House,1988]

32. 濮培民等。三峡工程与长江中游湖泊洼地环境[M].北京:科学出版社，1994[ Pu Peimin,et al.Three Gorges Construction and depression environment in the middle reach of the Yangtze River[M].Beijing: Science Press,1994]

33. 周明明，李文漪 ,姚祖驹。神龙架大九湖全新世植被与环境[A].中国北亚热带晚第四纪植被与环境研究[C].北京: 海洋出版社，1993.33～45 [ Zhou Mingming,Li Wenyi.Holocene vegetation and environment in Dajiuhu,Shenlongjia mountain[A].In: Li Wenyi andYao Zhuju,et al.eds.Research on late Quaternary vegetation and environment in north subtropical of China[C].Beijing:Ocean Publishing House,1993.33～45]

34. Hakanson L,Bottom dynamics in lakes[A].In:Sly PG,ed.Sediment/freshwater interaction [C].The Hugue,1982.1～22

35. 刘家麒，刘东生，储国强等。玛珥湖与纹泥年代学[J].第四纪研究，1996,（4）: 353～358 [Liu Jiaqi,Liu Dongsheng,Chu Guoqiang,Xiao Jule.Mara lake and varve geochronology[J].Quaternary Research,1996,（4）: 353～358]

36. Dell C I.A special mechanism for varve-formation in a glacial lake[J].Journal of Sedimentary Petrology,1973,43: 466～488

37. Ludlam S D.The role of turbidity currents in lakes sedimentation[J].Limnology and Oceanography,1974,19: 656～664

38. Wartel S,Singh S P,Faas R W.The nature and significance of gas-generated microvoids as "secondary" microfabric features in modern and Pleistocene marine and estuarine sediments[A].In: Bennett R H,Bryant W R and Hulbert M H,eds.Microstructure of fine grained sediments from mud to shale[C].Springer,1991.55～59

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长江中游湖泊沉积微结构特征与沉积环境

作者简介:
易朝路,男,1959年出生,博士,研究,员第四纪地质与地貌

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Microfabric Properties of Lacustrine Sediments and Sedimentary Environments

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长江中游湖泊沉积微结构特征与沉积环境

1. 南京大学城市与资源学系南京 210093;

2. 中国科学院水生生物研究所东湖生态实验站武汉 430073;

3. 华中师范大学地理系武汉 430071;

作者简介:
易朝路,男,1959年出生,博士,研究,员第四纪地质与地貌

English Abstract

Microfabric Properties of Lacustrine Sediments and Sedimentary Environments

1. Nanjing university, Nanjing 210093;

2. Donghu experi mental station of ecology, Chinese academy of sciences, Wuhan 430073;

3. Depart ment of geography, Central China Nor mal university, Wuhan 430071;

4. Instit ute of environmental geosciences, China university of geosciences, Wuhan 430073

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长江中游湖泊沉积微结构特征与沉积环境

作者简介: 易朝路,男,1959年出生,博士,研究,员第四纪地质与地貌

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Microfabric Properties of Lacustrine Sediments and Sedimentary Environments

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长江中游湖泊沉积微结构特征与沉积环境

1. 南京大学城市与资源学系 南京 210093; 2. 中国科学院水生生物研究所东湖生态实验站 武汉 430073; 3. 华中师范大学地理系 武汉 430071;

作者简介: 易朝路,男,1959年出生,博士,研究,员第四纪地质与地貌

English Abstract

Microfabric Properties of Lacustrine Sediments and Sedimentary Environments

1. Nanjing university, Nanjing 210093; 2. Donghu experi mental station of ecology, Chinese academy of sciences, Wuhan 430073; 3. Depart ment of geography, Central China Nor mal university, Wuhan 430071; 4. Instit ute of environmental geosciences, China university of geosciences, Wuhan 430073

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作者简介:
易朝路,男,1959年出生,博士,研究,员第四纪地质与地貌

1. 南京大学城市与资源学系南京 210093;

2. 中国科学院水生生物研究所东湖生态实验站武汉 430073;

3. 华中师范大学地理系武汉 430071;

作者简介:
易朝路,男,1959年出生,博士,研究,员第四纪地质与地貌

1. Nanjing university, Nanjing 210093;

2. Donghu experi mental station of ecology, Chinese academy of sciences, Wuhan 430073;

3. Depart ment of geography, Central China Nor mal university, Wuhan 430071;

4. Instit ute of environmental geosciences, China university of geosciences, Wuhan 430073