The Chronological Characteristics of Bosten Lake Holocene Sediment Environment in Xinjiang, China

ZHANG Cheng-jun; CAO Jie; LEI Yan-bin; SHANG Hua-ming

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(3): 494-499

ZHANG Cheng-jun, CAO Jie, LEI Yan-bin, SHANG Hua-ming. The Chronological Characteristics of Bosten Lake Holocene Sediment Environment in Xinjiang, China[J]. Acta Sedimentologica Sinica, 2004, 22(3): 494-499.

Citation:

ZHANG Cheng-jun, CAO Jie, LEI Yan-bin, SHANG Hua-ming. The Chronological Characteristics of Bosten Lake Holocene Sediment Environment in Xinjiang, China[J]. Acta Sedimentologica Sinica, 2004, 22(3): 494-499.

The Chronological Characteristics of Bosten Lake Holocene Sediment Environment in Xinjiang, China

School of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000

Received Date: 2003-10-16
Rev Recd Date: 2003-01-02
Publish Date: 2004-09-10

Abstract

Cs and ¹⁴C AMS were analyzed for the Bosten Lake sediment cores in Xinjiang, arid China. In the BST-4 core ¹³⁷ Cs section, there are obvious 1986 Chemobyl nucleus accident peak and 1975, 1963 peaks, which are important age characteristics for the Bosten lake sediment. The sedimentation rate, which was average 0.13±0.01 g/cm ² .a, was stable in the Bosten Lake by analysing the mass depth and ages. It is very similar to that from the ¹⁴C age, 0.13±0.03cm/a for BSTC-1 core and 0.12±0.05cm/a for xb46 core, in Bosten Lake after middle Holocene and show that the depositional environment was stable and the ¹⁴C ages were accurate. From the ¹⁴C age of the samples in Bosten Lake, it can be calibrated the old carbon effect produced by the hard water in the lakes and old carbon effect can lead to the old age for the ¹⁴C age in analysing the lake organic matters in sediments. We obtained the result of about 650a old effect in Bosten lake from the ¹⁴C age and the sedimentation rate by the ¹³⁷ Cs data.
- Bosten lake,¹³⁷Cs,
- sedimentation rate,¹⁴C AMS age,

References

[1]	王苏民,李建仁.湖泊沉积-研究历史气候的有效手段--以青海湖、岱海为例.科学通报,1991,1:54～56[Wang Sumin, Li Jianren. Lake sediments-an effective way to research the palaeoclimate: as exampe of Qinghai lake and Daihai lake. Chinese Science Bulletim,1991,1:54～56]
[2]	Deevey E S, Jr Gross M S, Hutchinson G E, and Kraybill H L. The natural ¹⁴C contents of materials from hard water lakes. Proceedings of the National Academy of Sciences USA, 1954,40:285～288
[3]	Shotton F W. An example of hard-water error in radiocarbon dating of vegetable matter. Nature, 1972,240:460～461
[4]	Karrow P E, Warner B G, Fritz P. Corry Bog, Pennsylvania: A case study of the radiocarbon dating of marl. Quaternary Research, 1984,21:326～336
[5]	MacDonald G M, Beuken R P, Kieser W E, Vitt D H. Comparative radiocarbon dating of terrestrial plant macrofossils and aquatic moss from the "ice-free corridor" of western Canada. Geology, 1987,15:837～840
[6]	任国玉. 内蒙古湖相沉积14C年代测定中"硬水"影响的发现. 湖泊科学,1998,10(3):80～82[Ren Guoyu. A finding of the influence of "Hard Water" on radiocarbon dating for lake sediments in Inner Mongolia, China. Journal of Lake Sciences,1998,10(3):80～82]
[7]	Aravena R, Warner B G, MacDonald G M, Hanf k. Carbon isotope composition of lake sediments in relation to lake productivity and radiocarbon dating. Quaternary Research, 1992,37:333～345
[8]	许英勤.新疆博斯腾湖地区全新世以来的孢粉组合与环境.干旱区地理,1998,21(2):43～ 49[Xu Yingqing. The assemblage of Holocene spore pollen and its environment in Bosten lake area, Xinjiang. Arid Land Geography,1998,2(2):43～49]
[9]	严平,董光荣,张信宝,张一云. ¹³⁷Cs法测定青藏高原土壤侵蚀的初步结果.科学通报,2000a,45(2):199～204[Yan Ping, Dong Guangrong, Zhang Xinbao,et al. Preliminary results of using ¹³⁷Cs to study wind erosion in the Qinghai-Tibet Plateau. Chinese Science Bulletin,2000a,11:1019～1024]
[10]	Lomenick T F, Tamura T. Naturally occurring fixation of cesium-137 on sediments of lacustrine origin. Soil Science Society of American Proceeding, 1965, 29:383～386
[11]	Richie J C, MeHenry J R. Fallout cesium-137: A tool in conservation research. Journal Soil Water Conservation, 1975, 30:283～286
[12]	Collins A L, Walling D E, Leeks G J L. Using of the geochemical record preserved in floodplain deposits to reconstruct recent changes in river basin sediment sources. Geomorphology, 1997, 19:151～167
[13]	万国江.现代沉积物年分辨的¹³⁷Cs记年--以云南洱海和贵州红枫湖为例.第四纪研究,1999,(1):73～80[Wan Guojiang. 137Cs dating by annual distinguishment for recent sedimentation: samples from Erhai lake and Hongfeng lake. Quaternary Sciences,1999,(1):73～80]
[14]	万国江. ¹³⁷Cs及²¹⁰Pbex方法湖泊沉积物计年研究新进展. 地球科学进展,1995,10(2):198～192[Wang Guojiang. Progresses on ¹³⁷Cs and sup>210Pbex dating of lake sediments. Advance in Earth Sciences, 1995,10(2):198～192]
[15]	项亮,吴瑞金,吉磊. ¹³⁷Cs和²⁴¹在滇池、剑湖沉积孔柱中的蓄积分布及时标意义.湖泊科学,1996,8(1):27～34[Xiang Liang,Wu Ruijin, Ji Lei. ¹³⁷Cs and ²⁴¹Am profiles and dating of sediments from two lakes in Yunnan province, China. Journal of Lake Sciences,1996,8(1):27～34]
[16]	严平,董光荣,董治宝,等.青海共和盆地达连海湖积物¹³⁷Cs示踪的初步结果. 地球化学,2000b,29(5):469～474[Yan Ping., Dong Guangrong, Dong Zhibao, et al.137Cs tracing of lacustrine sediments from Dalianhai lake, Qinghai province, China. Geochimica,2000b,29(5):469～474]
[17]	林瑞芬,卫克勤,程致远,等.新疆博斯腾湖沉积岩芯的²¹⁰Pb、²²⁸Th、^239,240Pu和³H的分布及意义.地球化学,1992,1:63～69[Lin Ruifen, WeiKeqin, Cheng Zhiyuan, et al. Distributions of ²¹⁰Pb,²²⁸Th,^239,240Pu and ³H and their implications in sediment core from Bosten lake, Xinjiang, China. Geochimica,1992,1:63～69]
[18]	Krishnaswami S, Lai D, Martin J M, Meybeck M. Geochronology of lake sediments. Earth Planetary Science Letters, 1971,11:407～414
[19]	Pennington Cambrary W R S and Fisher E M. Observation on lake sediments using fallout ¹³⁷Cs as a tracer. Nature, 1973, 242:324～326
[20]	Ritchie J C, Mchenry J R and Gill A C. Dating recent reservoir sediments. Limnology Oceanography. 1973, 18:254～263
[21]	Robbins J A and Edgington D N. Determination of recent sedimentation rates in lake Michigan using ²¹⁰Pb and ¹³⁷Cs. Geochimica et Cosmochimica Acta, 1975,39:285～304
[22]	钟巍,舒强. 南疆博斯腾湖近12.0kaB.P.以来古气候与古水文状况的变化. 海洋与湖沼,2001,32(2):213～219[Zhong Wei, Shu Qiang. Palaeoclimatic and palaeohydrologic oscillations since about 12.0kaB.P. at Bosten lake, Southern Xinjiang. Oceanologia et Limnologia Sinica, 2001,32(2):213～219]
[23]	范德江,杨作升,郭志刚. 中国陆架210Pb测年应用现状与思考. 地球科学进展,2000,15(3):297～302[Fan Dejiang, Yang Zuosheng, Guo Zhigang. Review of 210Pb dating in the continental shelf of China. Advance in Earth Sciences,2000,15(3):297～302]
[24]	Regnell J. Preparing pollen concentrations for AMS dating-a methodological study from a hard-water lake in southern Sweden. Boreas, 1992, 21:373～377
[25]	孙湘君,杜乃秋,陈因硕, 等.西藏色林错湖相沉积物的花粉分析.植物学报,1993,35(12):943～ 950[Sun Xiangjun, Du Naiqiu, Chen Yinshun,et al. Holocene palynological resords in lake Selincuo, Northern Xizang. Acta Botanica Sinica,1993,35(12):943～950]

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The Chronological Characteristics of Bosten Lake Holocene Sediment Environment in Xinjiang, China

School of Resources and Environmental Sciences, Lanzhou University, Lanzhou 730000

Received Date: 2003-10-16

Rev Recd Date: 2003-01-02

Publish Date: 2004-09-10

Key words:

Abstract: Cs and ¹⁴C AMS were analyzed for the Bosten Lake sediment cores in Xinjiang, arid China. In the BST-4 core ¹³⁷ Cs section, there are obvious 1986 Chemobyl nucleus accident peak and 1975, 1963 peaks, which are important age characteristics for the Bosten lake sediment. The sedimentation rate, which was average 0.13±0.01 g/cm ² .a, was stable in the Bosten Lake by analysing the mass depth and ages. It is very similar to that from the ¹⁴C age, 0.13±0.03cm/a for BSTC-1 core and 0.12±0.05cm/a for xb46 core, in Bosten Lake after middle Holocene and show that the depositional environment was stable and the ¹⁴C ages were accurate. From the ¹⁴C age of the samples in Bosten Lake, it can be calibrated the old carbon effect produced by the hard water in the lakes and old carbon effect can lead to the old age for the ¹⁴C age in analysing the lake organic matters in sediments. We obtained the result of about 650a old effect in Bosten lake from the ¹⁴C age and the sedimentation rate by the ¹³⁷ Cs data.

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Reference (25)

[1]	王苏民,李建仁.湖泊沉积-研究历史气候的有效手段--以青海湖、岱海为例.科学通报,1991,1:54～56[Wang Sumin, Li Jianren. Lake sediments-an effective way to research the palaeoclimate: as exampe of Qinghai lake and Daihai lake. Chinese Science Bulletim,1991,1:54～56]
[2]	Deevey E S, Jr Gross M S, Hutchinson G E, and Kraybill H L. The natural ¹⁴C contents of materials from hard water lakes. Proceedings of the National Academy of Sciences USA, 1954,40:285～288
[3]	Shotton F W. An example of hard-water error in radiocarbon dating of vegetable matter. Nature, 1972,240:460～461
[4]	Karrow P E, Warner B G, Fritz P. Corry Bog, Pennsylvania: A case study of the radiocarbon dating of marl. Quaternary Research, 1984,21:326～336
[5]	MacDonald G M, Beuken R P, Kieser W E, Vitt D H. Comparative radiocarbon dating of terrestrial plant macrofossils and aquatic moss from the "ice-free corridor" of western Canada. Geology, 1987,15:837～840
[6]	任国玉. 内蒙古湖相沉积14C年代测定中"硬水"影响的发现. 湖泊科学,1998,10(3):80～82[Ren Guoyu. A finding of the influence of "Hard Water" on radiocarbon dating for lake sediments in Inner Mongolia, China. Journal of Lake Sciences,1998,10(3):80～82]
[7]	Aravena R, Warner B G, MacDonald G M, Hanf k. Carbon isotope composition of lake sediments in relation to lake productivity and radiocarbon dating. Quaternary Research, 1992,37:333～345
[8]	许英勤.新疆博斯腾湖地区全新世以来的孢粉组合与环境.干旱区地理,1998,21(2):43～ 49[Xu Yingqing. The assemblage of Holocene spore pollen and its environment in Bosten lake area, Xinjiang. Arid Land Geography,1998,2(2):43～49]
[9]	严平,董光荣,张信宝,张一云. ¹³⁷Cs法测定青藏高原土壤侵蚀的初步结果.科学通报,2000a,45(2):199～204[Yan Ping, Dong Guangrong, Zhang Xinbao,et al. Preliminary results of using ¹³⁷Cs to study wind erosion in the Qinghai-Tibet Plateau. Chinese Science Bulletin,2000a,11:1019～1024]
[10]	Lomenick T F, Tamura T. Naturally occurring fixation of cesium-137 on sediments of lacustrine origin. Soil Science Society of American Proceeding, 1965, 29:383～386
[11]	Richie J C, MeHenry J R. Fallout cesium-137: A tool in conservation research. Journal Soil Water Conservation, 1975, 30:283～286
[12]	Collins A L, Walling D E, Leeks G J L. Using of the geochemical record preserved in floodplain deposits to reconstruct recent changes in river basin sediment sources. Geomorphology, 1997, 19:151～167
[13]	万国江.现代沉积物年分辨的¹³⁷Cs记年--以云南洱海和贵州红枫湖为例.第四纪研究,1999,(1):73～80[Wan Guojiang. 137Cs dating by annual distinguishment for recent sedimentation: samples from Erhai lake and Hongfeng lake. Quaternary Sciences,1999,(1):73～80]
[14]	万国江. ¹³⁷Cs及²¹⁰Pbex方法湖泊沉积物计年研究新进展. 地球科学进展,1995,10(2):198～192[Wang Guojiang. Progresses on ¹³⁷Cs and sup>210Pbex dating of lake sediments. Advance in Earth Sciences, 1995,10(2):198～192]
[15]	项亮,吴瑞金,吉磊. ¹³⁷Cs和²⁴¹在滇池、剑湖沉积孔柱中的蓄积分布及时标意义.湖泊科学,1996,8(1):27～34[Xiang Liang,Wu Ruijin, Ji Lei. ¹³⁷Cs and ²⁴¹Am profiles and dating of sediments from two lakes in Yunnan province, China. Journal of Lake Sciences,1996,8(1):27～34]
[16]	严平,董光荣,董治宝,等.青海共和盆地达连海湖积物¹³⁷Cs示踪的初步结果. 地球化学,2000b,29(5):469～474[Yan Ping., Dong Guangrong, Dong Zhibao, et al.137Cs tracing of lacustrine sediments from Dalianhai lake, Qinghai province, China. Geochimica,2000b,29(5):469～474]
[17]	林瑞芬,卫克勤,程致远,等.新疆博斯腾湖沉积岩芯的²¹⁰Pb、²²⁸Th、^239,240Pu和³H的分布及意义.地球化学,1992,1:63～69[Lin Ruifen, WeiKeqin, Cheng Zhiyuan, et al. Distributions of ²¹⁰Pb,²²⁸Th,^239,240Pu and ³H and their implications in sediment core from Bosten lake, Xinjiang, China. Geochimica,1992,1:63～69]
[18]	Krishnaswami S, Lai D, Martin J M, Meybeck M. Geochronology of lake sediments. Earth Planetary Science Letters, 1971,11:407～414
[19]	Pennington Cambrary W R S and Fisher E M. Observation on lake sediments using fallout ¹³⁷Cs as a tracer. Nature, 1973, 242:324～326
[20]	Ritchie J C, Mchenry J R and Gill A C. Dating recent reservoir sediments. Limnology Oceanography. 1973, 18:254～263
[21]	Robbins J A and Edgington D N. Determination of recent sedimentation rates in lake Michigan using ²¹⁰Pb and ¹³⁷Cs. Geochimica et Cosmochimica Acta, 1975,39:285～304
[22]	钟巍,舒强. 南疆博斯腾湖近12.0kaB.P.以来古气候与古水文状况的变化. 海洋与湖沼,2001,32(2):213～219[Zhong Wei, Shu Qiang. Palaeoclimatic and palaeohydrologic oscillations since about 12.0kaB.P. at Bosten lake, Southern Xinjiang. Oceanologia et Limnologia Sinica, 2001,32(2):213～219]
[23]	范德江,杨作升,郭志刚. 中国陆架210Pb测年应用现状与思考. 地球科学进展,2000,15(3):297～302[Fan Dejiang, Yang Zuosheng, Guo Zhigang. Review of 210Pb dating in the continental shelf of China. Advance in Earth Sciences,2000,15(3):297～302]
[24]	Regnell J. Preparing pollen concentrations for AMS dating-a methodological study from a hard-water lake in southern Sweden. Boreas, 1992, 21:373～377
[25]	孙湘君,杜乃秋,陈因硕, 等.西藏色林错湖相沉积物的花粉分析.植物学报,1993,35(12):943～ 950[Sun Xiangjun, Du Naiqiu, Chen Yinshun,et al. Holocene palynological resords in lake Selincuo, Northern Xizang. Acta Botanica Sinica,1993,35(12):943～950]

The Chronological Characteristics of Bosten Lake Holocene Sediment Environment in Xinjiang, China

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