Types and Origin of Diatomaceous Laminaeof the Miocene Shanwang Formationin Linqu,Shandong Province

QIN Wen-sheng; LIU Jian-bo; HAN Bao-fu; WANG Xian-zeng; LI Fu-chang

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(2): 267-275

QIN Wen-sheng, LIU Jian-bo, HAN Bao-fu, WANG Xian-zeng, LI Fu-chang. Types and Origin of Diatomaceous Laminaeof the Miocene Shanwang Formationin Linqu,Shandong Province[J]. Acta Sedimentologica Sinica, 2004, 22(2): 267-275.

Citation:

Types and Origin of Diatomaceous Laminaeof the Miocene Shanwang Formationin Linqu,Shandong Province

1.
Key Laboratory of Orogenic Belts and Crustal Evolution, Department of Geology, Peking University, Beijing 100871;
2.
Fossil Museum of Shanwang, Linqu, Shandong 262600

Received Date: 2003-03-31
Publish Date: 2004-06-10

Abstract

The Miocene Shanwang Formation in Linqu of Shandong Province consists mainly of lacustrine diatomaceous sediments. Detailed sedimentary study on the laminated diatomites in the Shanwang Formation is necessary for the furtherwork on reconstruction of high-frequency climatic cycle. Based on the major mineral composition and their ratios, the diatomaceous sediments in the Shanwang Formation are distinguished as three distinct laminae (clay laminae, diatomaceous laminae and organic matter laminae) and three lamina couplet types (organic matter-clay couplet, organic matter-diatomaceous couplet and diatomaceous couplet- clay couplet). The formation of diatomaceous laminae and lamina couples in the Shanwang Formation was controlled by sedimentary rate of terrigenous clays, diatom growth, and deposition and preservation of organic matters in the basin.
- diatomite,
- laminae,
- lamina couplet,
- Shanwang formation,
- miocene

References

[1]	Duplessy J C,Overpeck J.The PAGES/CLIVAR Intersection: Coordinated Research Objectives of the International Geoshpere-Biosphere (IGBP) and World Climate Research (WCRP) Programs.Venice: Report of a Joint IGBP-WCRP Workshop, 1994. 1～40
[2]	Anderson R Y, Dean W E.Lacustrine varve formation through time. Paleogeography Paleoclimatology Paleoecology, 1988, 62: 215～235
[3]	霍坎松,等.湖泊沉积学原理.北京:科学出版社,1992[Hakanson L, et al. Principles of Lake Sedimentology. Beijing: Science Press, 1992]
[4]	莱尔曼.湖泊化学、地质学的物理学.北京:地质出版社,1978 [Lerman. Lakes Chemistry Geology Physics.Beijing: Geological Publishing House, 1978]
[5]	刘春华,魏仪芳,王生.硅藻岩的岩石学特征和形成环境.长春地质学院学报,1995,25(2):138～143[Liu Chunhua, Wei Yifang, Wang Sheng. Petrology and the producing environment of diatomite.Journal of Changchun University of Earth Science, 1995, 25(2):138～143 ]
[6]	李承森,王宇飞,孙启高,等.山东省临朐县山旺组硅藻土层的划分.植物学报,2000,17(IOPC-VI古植物学专辑):247～251 [Li Chengsen, Wang Yufei, Sun Qigao, et al.The stratigraphical sequence of the diatomaceous earth from the Shanwang Formation, Linqu County, Shandong Province[J]. Chinese Bulletin of Botany, 2000, 17(Special volume for palaeobotany): 247～251]
[7]	阎德发,邱铸鼎,孟振亚.山东山旺中新世地层及哺乳动物化石.古脊椎动物与古人类,1983, 12(3):211～221[Yan Defa, Qiu Zhuding, Meng Zhenya.Miocene stratigraphy and mammals from Shanwang, Shandong.Vertebrata Palasiantica, 1983, 12(3): 211～221]
[8]	李风麟.山东临朐山旺组的再认识.地层学杂志,1991,15(2):123～129[Li Fenglin, Reconsideration of the Shandong Formation, Linqu, Shandong.Journal of Stratigraphy, 1991, 15(2): 123～129]
[9]	梁明媚,阎际兴,宋书银,等.山东山旺中新世植物群研究进展.植物学通报,1998,15(增刊):32～40 [Liang Mingmei, Yan Jixing, Song Shuyin, et al. Wang Qin.Advance of research on Miocene flora from Shanwang in Shandong Province.Chinese Bulletin of Botany,15(Supplement): 32～40]
[10]	张俊峰.山旺昆虫化石.济南:山东科学技术出版社,1989. 1～459, pls.1～92 [Zhang Junfeng.Fossil Insects from Shanwang, Shandong, China.Ji'Nan: Shandong Science and Technology Publishing House, 1989. 1～459, pls. 1～92]
[11]	孙博主编.山旺植物化石.济南:山东科学技术出版社, 1999. 1～167,pls. 62 [Sun Bo (Editor-in-Chief).Fossil Plants of Shanwang. Ji'nan: Shandong Science and Technology Press, 1999. 1～167, pls. 62 ]
[12]	侯连海,周忠和,张福成,等.山东山旺发现中新世大型猛禽化石.古脊椎动物学报,2000,38(2):104～110 [Hou Lianhai, Zhou Zhonghe, Zhang Fucheng, et al.A new vulture from the Miocene of Shandong, eastern China.Vertebrata Palasiatica, 2000, 38(2): 104～110]
[13]	杨式溥.山东山旺中新世硅藻页岩中的遗迹化石.地质论评,1996,42(2):187～190[Yang Shipu. Trace fossils from the Miocene diatomites of Shanwang, Shandong, China.Geological Review, 1996, 42(2): 187～190]
[14]	王宪曾.山东临朐山旺组真菌化石的发现及其意义.见:岩石圈地质科学论文集.北京:北京大学出版社,1989. 19～26 [Wang Xianzeng. Discovery of fungus fossils from Shanwang Formation, Linqu, Shandong and its implication. In: Geological Sciences of Lithosphere. Beijing: Beijing University Press,1989. 19～26]
[15]	山东区域地层表编写组.华东地区区域地质表山东分册5,潍坊地层小区.北京:地质出版社,1987. 34～37[Compiling Group of Shandong Stratigraphical Sequence. A stratigraphical sequence of Weifang region.In: Stratigraphical Tables of East China (Volume 5 for Shandong). Beijing: Geological Publishing House, 1987. 34～37]
[16]	张明书,单莲芳.旺盆地沉积地质学.北京:地质出版社,1994. 1-83[Zhang Mingshu, Shan Lianfang.Sedimentary Geology of Shanwang Basic.Beijing: Geological Publishing House, 1994. 1-83]
[17]	金隆裕.郯庐断裂带中段新生代火山岩的K-Ar年龄值和分期.地质论评,1985,31(4):309～315 [Jin Longyu.K-Ar ages of Cenozoic volcanic rocks in the middle segment of the Tancheng-Lujiang fault belt and stages of related volcanic activity.Geological Review, 1985, 31(4): 309～315]
[18]	Garrison R E, Douglas R G, Pisoctiotto K A, Isaacs C M,et al.The Monterey Formation and related siliceous rocks of California.Society of Economic Paleontologists and Mineralogists, Pacific Section, Special Publication, 1981, 15: 327
[19]	Brodie I, Kemp A E S.Variation in biogenic and clay fluxes and formation of laminae in late Quaternary sediments from the Peruvian coastal upwelling zone.Marine Geology, 1994, 116: 385～398
[20]	Grimm K A, Lange C B, Gill A S.Biological forcing of hemipelagic sedimentary laminae: Evidence from ODP Site 893, Santa Barbara Basin, California.Journal of Sedimentary Research, 1996, 66: 613～624
[21]	Pike J, Kemp A E S.Early Holocene decadal-scale ocean variability recorded in Gulf of California laminated sediments.Paleoceanography, 1997, 12: 227～238
[22]	Kemp A E S.Sedimentary fabrics and variation in lamination style in Peru continental upwelling sediments.Proceedings of the Ocean Drilling Program, Scientific Results, 1990, 112(Ocean Drilling Program, College Station, Texas), 43～58
[23]	Alices S C, Kurt A G, Lisa D, White diatomaceous Sediments from the Miocene Monterey formation, California: A Lamina-scale investigation of biological, ecological, and sedimentary Processes.Palaios, 1998, 13: 439～458
[24]	李万春,李世杰,濮培民.高分辨率古环境指示器--湖泊纹泥研究综述.地球科学进展.1999,14(2):172～176[Li Wangchun, Li Shijie, Pu Peimin.Review on the high resolution varved lake sediments as a proxy of paleoenvironment.Advance in Earth Science, 1999, 14(2): 172～176]
[25]	O'Sullivan P E.Annually laminated lake sediments and the study of Quaternary environmental changes-a review.Quaternary Science Review,1983, 1: 245～313
[26]	石玲.山东山旺中新世硅藻及其环境的模糊数学的聚类分析.植物学报,1990,32(11):888～895[Shi Ling.Miocene diatoms from the Shanwang Basin of Shandong Province and analysis by fuzzy mathematics of the paleoenvironment.Acta Botania Sinica, 1990,32(11): 888～895]
[27]	杨洪.古生物的全息生活型复原及山旺中新世植物群的古气候指示.大自然探索,1988,7(1):127～133[Yang Hong.Reconstruction of Holographic life form in palaeobotany and paleoclimatic indication of Shanwang Miocence flora.Exploration of Nature, 1988,7(1):127～133]
[28]	王宪曾.山东临朐中新世山旺湖古环境初探.北京大学学报(自然科学),1981,4:100～111[Wang Xianzeng. An introductory survey of the paleoenvironment of Miocene Shanwang Lake in Linqu, Shantung Province.Acta Scientiarum Naturalium Universitatis Pekinensis, Issue, 1981, 4:100～111]
[29]	陈富平.山东山旺中新世鱼化石埋藏学及古湖泊环境.植物学通报,2000,17(IOPC-VI古植物学专辑):264～271[Chen Pingfu.Fish taponomy and its paleoclimatological significance from the Miocene Shanwang Formation, Shandong, eastern China.Chinese Bulletin of Botany, 2000, 17(Special Issue): 264～271]
[30]	Wetzel R G.Limnology.Saunders Philadelphia, 1975. 243
[31]	Lindell T, Hydrographic characteristics. In: Welch, ed. Ecological effects of waste water.Cambridge University Press, 1980
[32]	Eppley R W.The growth and culture of diatoms. In: Werner D, ed. The Biology of Diatoms.California: University of California Press, 1978. 24～64
[33]	Zolitschka B.High resolution lacustrine sediments and their potential for paleoclimatic reconstruction. In: Jones P D, Bradley R S, Jouzel J, eds. Climatic Science.1996, 166: 1191～1194

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Types and Origin of Diatomaceous Laminaeof the Miocene Shanwang Formationin Linqu,Shandong Province

1. Key Laboratory of Orogenic Belts and Crustal Evolution, Department of Geology, Peking University, Beijing 100871;

2. Fossil Museum of Shanwang, Linqu, Shandong 262600

Received Date: 2003-03-31

Publish Date: 2004-06-10

Key words:

Abstract: The Miocene Shanwang Formation in Linqu of Shandong Province consists mainly of lacustrine diatomaceous sediments. Detailed sedimentary study on the laminated diatomites in the Shanwang Formation is necessary for the furtherwork on reconstruction of high-frequency climatic cycle. Based on the major mineral composition and their ratios, the diatomaceous sediments in the Shanwang Formation are distinguished as three distinct laminae (clay laminae, diatomaceous laminae and organic matter laminae) and three lamina couplet types (organic matter-clay couplet, organic matter-diatomaceous couplet and diatomaceous couplet- clay couplet). The formation of diatomaceous laminae and lamina couples in the Shanwang Formation was controlled by sedimentary rate of terrigenous clays, diatom growth, and deposition and preservation of organic matters in the basin.

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Reference (33)

[1]	Duplessy J C,Overpeck J.The PAGES/CLIVAR Intersection: Coordinated Research Objectives of the International Geoshpere-Biosphere (IGBP) and World Climate Research (WCRP) Programs.Venice: Report of a Joint IGBP-WCRP Workshop, 1994. 1～40
[2]	Anderson R Y, Dean W E.Lacustrine varve formation through time. Paleogeography Paleoclimatology Paleoecology, 1988, 62: 215～235
[3]	霍坎松,等.湖泊沉积学原理.北京:科学出版社,1992[Hakanson L, et al. Principles of Lake Sedimentology. Beijing: Science Press, 1992]
[4]	莱尔曼.湖泊化学、地质学的物理学.北京:地质出版社,1978 [Lerman. Lakes Chemistry Geology Physics.Beijing: Geological Publishing House, 1978]
[5]	刘春华,魏仪芳,王生.硅藻岩的岩石学特征和形成环境.长春地质学院学报,1995,25(2):138～143[Liu Chunhua, Wei Yifang, Wang Sheng. Petrology and the producing environment of diatomite.Journal of Changchun University of Earth Science, 1995, 25(2):138～143 ]
[6]	李承森,王宇飞,孙启高,等.山东省临朐县山旺组硅藻土层的划分.植物学报,2000,17(IOPC-VI古植物学专辑):247～251 [Li Chengsen, Wang Yufei, Sun Qigao, et al.The stratigraphical sequence of the diatomaceous earth from the Shanwang Formation, Linqu County, Shandong Province[J]. Chinese Bulletin of Botany, 2000, 17(Special volume for palaeobotany): 247～251]
[7]	阎德发,邱铸鼎,孟振亚.山东山旺中新世地层及哺乳动物化石.古脊椎动物与古人类,1983, 12(3):211～221[Yan Defa, Qiu Zhuding, Meng Zhenya.Miocene stratigraphy and mammals from Shanwang, Shandong.Vertebrata Palasiantica, 1983, 12(3): 211～221]
[8]	李风麟.山东临朐山旺组的再认识.地层学杂志,1991,15(2):123～129[Li Fenglin, Reconsideration of the Shandong Formation, Linqu, Shandong.Journal of Stratigraphy, 1991, 15(2): 123～129]
[9]	梁明媚,阎际兴,宋书银,等.山东山旺中新世植物群研究进展.植物学通报,1998,15(增刊):32～40 [Liang Mingmei, Yan Jixing, Song Shuyin, et al. Wang Qin.Advance of research on Miocene flora from Shanwang in Shandong Province.Chinese Bulletin of Botany,15(Supplement): 32～40]
[10]	张俊峰.山旺昆虫化石.济南:山东科学技术出版社,1989. 1～459, pls.1～92 [Zhang Junfeng.Fossil Insects from Shanwang, Shandong, China.Ji'Nan: Shandong Science and Technology Publishing House, 1989. 1～459, pls. 1～92]
[11]	孙博主编.山旺植物化石.济南:山东科学技术出版社, 1999. 1～167,pls. 62 [Sun Bo (Editor-in-Chief).Fossil Plants of Shanwang. Ji'nan: Shandong Science and Technology Press, 1999. 1～167, pls. 62 ]
[12]	侯连海,周忠和,张福成,等.山东山旺发现中新世大型猛禽化石.古脊椎动物学报,2000,38(2):104～110 [Hou Lianhai, Zhou Zhonghe, Zhang Fucheng, et al.A new vulture from the Miocene of Shandong, eastern China.Vertebrata Palasiatica, 2000, 38(2): 104～110]
[13]	杨式溥.山东山旺中新世硅藻页岩中的遗迹化石.地质论评,1996,42(2):187～190[Yang Shipu. Trace fossils from the Miocene diatomites of Shanwang, Shandong, China.Geological Review, 1996, 42(2): 187～190]
[14]	王宪曾.山东临朐山旺组真菌化石的发现及其意义.见:岩石圈地质科学论文集.北京:北京大学出版社,1989. 19～26 [Wang Xianzeng. Discovery of fungus fossils from Shanwang Formation, Linqu, Shandong and its implication. In: Geological Sciences of Lithosphere. Beijing: Beijing University Press,1989. 19～26]
[15]	山东区域地层表编写组.华东地区区域地质表山东分册5,潍坊地层小区.北京:地质出版社,1987. 34～37[Compiling Group of Shandong Stratigraphical Sequence. A stratigraphical sequence of Weifang region.In: Stratigraphical Tables of East China (Volume 5 for Shandong). Beijing: Geological Publishing House, 1987. 34～37]
[16]	张明书,单莲芳.旺盆地沉积地质学.北京:地质出版社,1994. 1-83[Zhang Mingshu, Shan Lianfang.Sedimentary Geology of Shanwang Basic.Beijing: Geological Publishing House, 1994. 1-83]
[17]	金隆裕.郯庐断裂带中段新生代火山岩的K-Ar年龄值和分期.地质论评,1985,31(4):309～315 [Jin Longyu.K-Ar ages of Cenozoic volcanic rocks in the middle segment of the Tancheng-Lujiang fault belt and stages of related volcanic activity.Geological Review, 1985, 31(4): 309～315]
[18]	Garrison R E, Douglas R G, Pisoctiotto K A, Isaacs C M,et al.The Monterey Formation and related siliceous rocks of California.Society of Economic Paleontologists and Mineralogists, Pacific Section, Special Publication, 1981, 15: 327
[19]	Brodie I, Kemp A E S.Variation in biogenic and clay fluxes and formation of laminae in late Quaternary sediments from the Peruvian coastal upwelling zone.Marine Geology, 1994, 116: 385～398
[20]	Grimm K A, Lange C B, Gill A S.Biological forcing of hemipelagic sedimentary laminae: Evidence from ODP Site 893, Santa Barbara Basin, California.Journal of Sedimentary Research, 1996, 66: 613～624
[21]	Pike J, Kemp A E S.Early Holocene decadal-scale ocean variability recorded in Gulf of California laminated sediments.Paleoceanography, 1997, 12: 227～238
[22]	Kemp A E S.Sedimentary fabrics and variation in lamination style in Peru continental upwelling sediments.Proceedings of the Ocean Drilling Program, Scientific Results, 1990, 112(Ocean Drilling Program, College Station, Texas), 43～58
[23]	Alices S C, Kurt A G, Lisa D, White diatomaceous Sediments from the Miocene Monterey formation, California: A Lamina-scale investigation of biological, ecological, and sedimentary Processes.Palaios, 1998, 13: 439～458
[24]	李万春,李世杰,濮培民.高分辨率古环境指示器--湖泊纹泥研究综述.地球科学进展.1999,14(2):172～176[Li Wangchun, Li Shijie, Pu Peimin.Review on the high resolution varved lake sediments as a proxy of paleoenvironment.Advance in Earth Science, 1999, 14(2): 172～176]
[25]	O'Sullivan P E.Annually laminated lake sediments and the study of Quaternary environmental changes-a review.Quaternary Science Review,1983, 1: 245～313
[26]	石玲.山东山旺中新世硅藻及其环境的模糊数学的聚类分析.植物学报,1990,32(11):888～895[Shi Ling.Miocene diatoms from the Shanwang Basin of Shandong Province and analysis by fuzzy mathematics of the paleoenvironment.Acta Botania Sinica, 1990,32(11): 888～895]
[27]	杨洪.古生物的全息生活型复原及山旺中新世植物群的古气候指示.大自然探索,1988,7(1):127～133[Yang Hong.Reconstruction of Holographic life form in palaeobotany and paleoclimatic indication of Shanwang Miocence flora.Exploration of Nature, 1988,7(1):127～133]
[28]	王宪曾.山东临朐中新世山旺湖古环境初探.北京大学学报(自然科学),1981,4:100～111[Wang Xianzeng. An introductory survey of the paleoenvironment of Miocene Shanwang Lake in Linqu, Shantung Province.Acta Scientiarum Naturalium Universitatis Pekinensis, Issue, 1981, 4:100～111]
[29]	陈富平.山东山旺中新世鱼化石埋藏学及古湖泊环境.植物学通报,2000,17(IOPC-VI古植物学专辑):264～271[Chen Pingfu.Fish taponomy and its paleoclimatological significance from the Miocene Shanwang Formation, Shandong, eastern China.Chinese Bulletin of Botany, 2000, 17(Special Issue): 264～271]
[30]	Wetzel R G.Limnology.Saunders Philadelphia, 1975. 243
[31]	Lindell T, Hydrographic characteristics. In: Welch, ed. Ecological effects of waste water.Cambridge University Press, 1980
[32]	Eppley R W.The growth and culture of diatoms. In: Werner D, ed. The Biology of Diatoms.California: University of California Press, 1978. 24～64
[33]	Zolitschka B.High resolution lacustrine sediments and their potential for paleoclimatic reconstruction. In: Jones P D, Bradley R S, Jouzel J, eds. Climatic Science.1996, 166: 1191～1194

Types and Origin of Diatomaceous Laminaeof the Miocene Shanwang Formationin Linqu,Shandong Province

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