Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain

LI Nan-nan; JIE Dong-mei; YANG Jin-xiu; CHEN Xue-song; CHEN Yu-jie; HU Chu-tian; QIAO Zhi-he

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2014 > 32(5): 873-883

LI Nan-nan, JIE Dong-mei, YANG Jin-xiu, CHEN Xue-song, CHEN Yu-jie, HU Chu-tian, QIAO Zhi-he. Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain[J]. Acta Sedimentologica Sinica, 2014, 32(5): 873-883.

Citation:

Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain

1.
School of Geographical Science, Northeast Normal University, Changchun 130024;
2.
Key Laboratory for Wetland Ecology and Vegetation Restoration, Ministry of Environmental Protection, Changchun 130024;
3.
Daqing Normal University, Daqing, Heilongjiang 163712

Received Date: 2013-07-15
Rev Recd Date: 2013-11-28
Publish Date: 2014-10-10

Abstract

In order to recognize the provenances, granularity characteristics of peat ash, and further reveal the paleo-enviromental significance of peat ash. Two peat cores in Hani and Gushantun Peat-land in the west foothill of Changbai Mountain are collected. The results of grain size analysis show that the dominant size of peat ash is 1~350 μm. Which means peat ash is mainly composed of different kinds of silt. What is more, the majority probability cumulative curves for particle size distribution are with two sections. At the same time, frequency distribution curves show unimodal type (10~100 μm), bimodal type (10~100 μm, 100~1 000 μm). These show that the transportation ways of peat ash is suspension and saltation. And the grain sizes changed with the hydrologic condition in the peat land. In the dry season, the water power is weak and the peat ash content is relatively fine. But in the wet season, surface runoff carries the coarse particle into the swamp and deposits. Therefore, the peat ash can be used for rebuilding the evolution of paleo-precipitation and it can be a proxy for the summer monsoon. In addition, 9.2 ka, 8ka and 5ka drought events in Holocene are recognized from the grain size changing curve and the curve also reveals a "dry-wet-dry" cycle in the precipitation history. Because these events correspond to the famous cold events, so we may draw the conclusion that dry and cold, warm and wet may be matched in the process of climate change.
- Changbai Mountain area,
- peat,
- grain-size,
- sedimentary facies,
- summer monsoon

References

[1]	刘东生, 等. 黄土与环境[M]. 北京:科学出版社, 1985[Liu Tungsheng, et al. Loess and Environment[M]. Beijing: Science Press, 1985]
[2]	胡邦琦, 杨作升, 赵美训, 等. 南黄海中部泥质区7200 年以来东亚冬季风变化的沉积记录[J]. 中国科学(D辑):地球科学, 2012, 42(10):1568-1581[Hu Bangqi, Yang Zuosheng, Zhao Meixun, et al. Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area[J]. China Science(Seri. D): Earth Science, 2012, 42(10): 1568-1581]
[3]	张洪岩, 王锡魁, 隋维国, 等. 图们江河口沼泽沉积物的粒度特征及碎屑源分析[J]. 世界地质, 2006, 25(2):147-159[Zhang Hongyan, Wang Xikui, Sui Weiguo, et al. Analysis on grain-size characteristics and fragment sources of deposits in swamps near debouchment of Tumen River[J]. Global Geology, 2006, 25(2): 147-159]
[4]	郑国璋, 岳乐平, 何军锋, 等. 疏勒河下游安西古沼泽全新世沉积物粒度特征及其古气候环境意义[J]. 沉积学报, 2006, 24(5):733-739[Zheng Guozhang, Yue Leping, He Junfeng, et al. Grain-size characteristics of the sediments at palaeoswamp in Anxi County in downstream of Shulehe River during Holocene and its paleoclimatic significance[J]. Acta Sedimentologica Sinica, 2006, 24(5): 733-739]
[5]	王心源, 张广胜, 张恩楼, 等. 巢湖湖泊沉积记录的早-中全新世环境演化研究[J]. 科学通报, 2008, 53(增刊Ⅰ):132-138[Wang Xinyuan, Zhang Guangsheng, Zhang Enlou, et al. Research on early-middle Holocene environment evolution from the records of sediment in Chaohu Lake[J]. Chinese Science Bulletin, 2008, 53(Suppl.Ⅰ): 132-138]
[6]	殷书柏, 吕宪国. "泥炭气候成因说"的探讨[J]. 地理科学, 2006, 26(3):321-326[Yin Shubai, Lü Xianguo. Discussion on "the theory on climate cause of peat forming"[J]. Scientia Geographica Sinica, 2006, 26(3): 321-326]
[7]	赵红艳, 冷雪天, 王升忠. 长白山地泥炭分布、沉积速率与全新世气候变化[J]. 山地学报, 2002, 20:513-518[Zhao Hongyan, Leng Xuetian, Wang Shengzhong. Distribution, accumulation rate of peat in the Changbaishan Mountains and climate change in Holocene[J]. Journal of Mountain Science, 2002, 20: 513-518]
[8]	刘金陵. 长白山区孤山屯沼泽地13000年以来的植被和气候变化[J]. 古生物学报, 1989, 28:495-509[Liu Jinling. Vegetational and climatic changes at Gushantun Bog in Jilin, NE China Since 13, 000 Y.B.P[J]. Acta Palaeontologica Sinica, 1989, 28: 495-509]
[9]	李荣麟, 介冬梅, 刘艳萍, 等. 东北长白山区北部虎山泥炭剖面植硅体的环境指示意义[J]. 微体古生物学报, 2011, 28:329-336[Li Ronglin, Jie Dongmei, Liu Yanpin, et al. Phytolith as an environment indicator of Hushan peat section from northern region in Changbai Mountain[J]. Acta Micropalaeontologica Sinica, 2011, 28: 329-336]
[10]	王金权, 刘金陵. 长白山区全新世大暖期的氨基酸和碳同位素记录[J]. 微体古生物学报, 2001, 18:392-398[Wang Jinquan, Liu Jinling. The records of amino acids and organic carbon isotope for Holocene megathermal in Changbaishan area[J]. Acta Micropalaeontologica Sinica, 2001, 18: 392-398]
[11]	李鸿凯, 卜兆君, 王升忠, 等. 长白山区泥炭地现代有壳变形虫环境意义探讨[J]. 第四纪研究, 2009, 29(4):817-824[Li Hongkai, Bu Zhaojun, Wang Shengzhong, et al. Environmental implications of the modern testate amoebae in the peatlands in Changbai Mountains[J]. Quaternary Sciences, 2009, 29(4): 817-824]
[12]	洪冰, 刘丛强, 林庆华, 等. 哈尼泥炭δ¹⁸O记录的过去14000年温度演变[J]. 中国科学(D 辑):地球科学, 2009, 39:626-637[Hong Bing, Liu Congqiang, Lin Qinghua, et al. Temperature evolution from the δ¹⁸O record of Hani peat, Northeast China, in the last 14000 years[J]. Science China(Seri. D): Earth Science, 2009, 39: 626-637]
[13]	Stuiver M, and Reimer, P J. Extended ¹⁴C database and revised CALIB radiocarbon calibration program[J]. Radiocarbon, 1993, 35: 215-230
[14]	国家海洋局. 海洋调查规范(第四分册——海洋地质调查)[M]. 北京:海洋出版社, 1975:9-88[State Oceanic Administration. Specifications for Oceanographic Survey (volume 4: Marine Geologic Survey)[M]. Beijing: Ocean Press, 1975: 9-88]
[15]	Link A G. Textural classification of sediments[J]. Sedimentology, 1966, 7(3): 249-254
[16]	SY/T 5434—1999, 中华人民共和国石油天然气行业标准:碎屑岩粒度分析方法[S][State Petroleum and Chemical Industry. Standards of petroleum and natural gas industry of the People's Republic of China, Method of grain-size analysis of clastic rocks[S]]
[17]	成都地质学院陕北队编. 沉积岩(物)粒度分析及其应用[M]. 北京:地质出版社, 1978[Chengdu College of Geology, Shanbei team. Sedimentary Rock (Material) Particle-size Analysis and Its Application[M]. Beijing: Geological Publishing House, 1978]
[18]	肖景义, 陈建强, 孙刚, 等. 河北邯郸HZ-S孔第四纪沉积物粒度特征分析[J]. 干旱区资源与环境, 2009, 23(1):54-59[Xiao Jingyi, Chen Jianqiang, Sun Gang, et al. Grain-size characteristics of HZ-S Core Quaternary sediments in Handan City, Hebei province[J]. Journal of Arid Land Resources and Environment, 2009, 23(1): 54-59]
[19]	雷国良, 张虎才, 张文翔, 等. 柴达木盆地察尔汗古湖贝壳堤剖面粒度特征及其沉积环境[J]. 沉积学报, 2007, 25(2):274-281[Lei Guoliang, Zhang Hucai, Zhang Wenxiang, et al. Characteristics of grain-size and sedimentation of shell bar section in salt Lake Qarhan, Qaidam Basin[J]. Acta Sedimentologica Sinica, 2007, 25(2): 274-281]
[20]	黄臻, 王建力, 王勇.长江三峡巫山第四纪沉积物粒度分布特征[J].热带地理, 2010, 30(1):30-39[Huang Zhen, Wang Jianli, Wang Yong. Grain-size features of Quaternary sediments in Changjiang Three Gorge Reservoir of the Wushan area[J]. Tropical Geography, 2010, 30(1): 30-39]
[21]	李敬卫, 乔彦松, 王燕, 等. 江西九江红土堆积的粒度特征及成因研究[J]. 地质力学学报, 2009, 15(1):95-103[Li Jingwei, Qiao Yansong, Wang Yan, et al. Aeolian origin of the red earth tormation in Jiujiang city of Jiangxi province, China: Evidence from grain-size analysis[J]. Journal of Geomechanics, 2009, 15(1): 95-103]
[22]	于学峰, 周卫健, 刘晓清, 等. 青藏高原东部全新世泥炭灰分的粒度特征及其古气候意义[J]. 沉积学报, 2006, 12(6):864-869[Yu Xuefeng, Zhou Weijian, Liu Xiaoqing, et al. Grain size characteristics of the Holocene peat sediment in eastern Tibetan Plateau and its paleoclimatic significance[J]. Acta Sedimentologica Sinica, 2006, 12(6): 864-869]
[23]	Lerman A. Lakes—Chemistry, Geology, Physics[M]. Berlin: Springer-Verlag, 1978
[24]	孙永传, 李惠生. 碎屑岩沉积相和沉积环境[M]. 北京:地质出版社, 1986[Sun Yongchuan, Li Huisheng. Clastic Sedimentary Facies and Sedimentary Environment[M]. Beijing: Geological Publishing House, 1986]
[25]	施雅风. 中国全新世大暖期气候与环境[M]. 北京:海洋出版社, 1992[Shi Yafeng. The Holocene Megathermal Climate and Environment in China[M]. Beijing: Ocean Press, 1992]
[26]	宋长青, 吕厚远, 孙湘君. 中国北方花粉—气候因子转换函数建立及应用[J]. 科学通报, 1997, 42:2182-2185[Song Changqing, Lü Houyuan, Sun Xiangjun. Construction of pollen-climate factor transfer function and its application in North China[J]. Chinese Science Bulletin, 1997, 42: 2182-2185]
[27]	崔美玲, 罗运利, 孙湘君. 吉林哈尼湖钻孔5 000 年以来的古植被气候变化指示[J]. 海洋地质与第四纪地质, 2006, 26(5):117-122[Cui Meiling, Luo Yunli, Sun Xiangjun. Paleoegetatinal and paleoclimatic changes in Ha'ni Lake, Jilin since 5 ka B.P.[J]. Marine Geology and Quaternary Geology, 2006, 26(5): 117-122]
[28]	喻春霞, 罗运利, 孙湘君. 吉林柳河哈尼湖13.1～4.15cal.ka B.P.古气候演化的高分辨率孢粉记录[J]. 第四纪研究, 2008, 28(5):929-938[Yu Chunxia, Luo Yunli, Sun Xiangjun. A high-resolution pollen records from Ha'ni Lake, Jilin, Northeast China showing climate changes between 13.1 cal.ka B.P. and 4.5 cal.ka B.P.[J]. Quaternary Sciences, 2008, 28(5): 929-938]
[29]	周卫建, 李小强, 董光荣, 等. 新仙女木期沙漠/黄土过渡带高分辨率泥炭记录——东亚季风气候颤动的实例[J]. 中国科学(D 辑):地球科学, 1996, 26(2):118-124[Zhou Weijian, Li Xiaoqiang, Dong Guangrong, et al. High-resolution peat record from the desert-loess transitional belt during the Younger Dryas Interval: An example of East Asian monsoon climatic fluctuations[J]. Science China(Seri. D): Earth Science, 1996, 26(2): 118-124]
[30]	沈吉, 吴瑞金, 羊向东, 等. 大布苏湖沉积剖面碳酸盐含量、氧同位素特征的古气候意义[J]. 湖泊科学, 1997, 9(3):217-222[Shen Ji, Wu Ruijin, Yang Xiangdong, et al. Paleoclimatic change inferred from δ¹⁸O and carbonate content of the section in Dabusu Lake[J]. Journal of Lake Sciences, 1997, 9(3): 217-222]
[31]	Dykoskia C A, Edwardsa R L, Cheng H, et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China[J]. Earth and Planetary Science Letters, 2005, 233(1/2): 71-86
[32]	萧家仪, 吕海波, 周卫健, 等. 末次盛冰期以来江西大湖孢粉植被与环境演变[J]. 中国科学(D 辑):地球科学, 2007, 37(6):789-797[Xiao Jiayi, Lü Haibo, Zhou Weijian, et al. Evolution of vegetation and climate since the last glacial maximum recorded at Dahu peat site, South China[J]. Science China(Seri. D): Earth Science, 2007, 37(6): 789-797]
[33]	王志国. 吉林金川泥炭纤维素稳定碳同位素组成序列与东北季风区五千多年来的环境变迁[J]. 矿物岩石地球化学通报, 1998, 17(1):52-54[Wang Zhiguo. Reconstruction of past 5 000-year humidity changes of Northeast China using δ¹³C values of peat cellulose in Jinchuan region, Jilin province[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 1998, 17(1): 52-54]
[34]	李秉成, 雷祥义, 李正泽, 等. 西安白鹿塬全新世黄土剖面磁化率的古气候特征[J]. 海洋地质与第四纪地质, 2008, 28(2):115-121[Li Bingcheng, Lei Xiangyi, Li Zhengze, et al. Paleoclimate character of susceptibility of Holocene Loess section in Xi'an Bailuyuan[J]. Marine Geology & Quaternary Geology, 2008, 28(2): 115-121]
[35]	竺可桢. 中国近五千年来气候变迁的初步研究[J]. 中国科学(B辑), 1973(2):226-256[Zhu Kezhen. Preliminary study on climate change over last 5000 years in China[J]. Science China(Seri. B), 1973(2): 226-256]
[36]	Mayewski, P A, Rohling E E, Stager J C, et al. Holocene climate variability[J]. Quaternary Research, 2004, 62(3): 243-255
[37]	Gupta A K, Anderson D M, Overpeck J T. Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean[J]. Nature, 421: 354-357
[38]	贾耀锋, 庞奖励. 关中盆地东部李湾剖面全新世高分辨率气候研究[J]. 干旱区资源与环境, 2003, 17(3):39-43[Jia Yaofeng, Pang Jiangli. The high resolution of the Holocene climatic study in Liwan profile in eastern Guanzhong Basin[J]. Journal of Arid Land Resources and Environment, 2003, 17(3): 39-43]
[39]	唐领余, 沈才明, 李春海, 等. 花粉记录的青藏高原中部中全新世以来植被与环境[J]. 中国科学(D 辑):地球科学, 2009, 39(5):615-625[Tang Lingyu, Shen Caiming, Li Chunhai, et al. Pollen-inferred vegetation and environmental changes in the central Tibetan Plateau since 8200 yr BP[J]. Science China(Seri. D): Earth Science, 2009, 39(5): 615-625]
[40]	Johnsen S, Dahl-Jensen D, Gundestrup N S, et al. Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye3, GRIP, GISP2, Renland and North GRIP[J]. Journal of Quaternary Science, 2001, 16(4): 299-307

Proportional views

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

Get Citation

PDF

XML

Article Metrics

Article views(1433) PDF downloads(1119) Cited by()

Proportional views

Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain

1. School of Geographical Science, Northeast Normal University, Changchun 130024;

2. Key Laboratory for Wetland Ecology and Vegetation Restoration, Ministry of Environmental Protection, Changchun 130024;

3. Daqing Normal University, Daqing, Heilongjiang 163712

Received Date: 2013-07-15

Rev Recd Date: 2013-11-28

Publish Date: 2014-10-10

Key words:

Abstract: In order to recognize the provenances, granularity characteristics of peat ash, and further reveal the paleo-enviromental significance of peat ash. Two peat cores in Hani and Gushantun Peat-land in the west foothill of Changbai Mountain are collected. The results of grain size analysis show that the dominant size of peat ash is 1~350 μm. Which means peat ash is mainly composed of different kinds of silt. What is more, the majority probability cumulative curves for particle size distribution are with two sections. At the same time, frequency distribution curves show unimodal type (10~100 μm), bimodal type (10~100 μm, 100~1 000 μm). These show that the transportation ways of peat ash is suspension and saltation. And the grain sizes changed with the hydrologic condition in the peat land. In the dry season, the water power is weak and the peat ash content is relatively fine. But in the wet season, surface runoff carries the coarse particle into the swamp and deposits. Therefore, the peat ash can be used for rebuilding the evolution of paleo-precipitation and it can be a proxy for the summer monsoon. In addition, 9.2 ka, 8ka and 5ka drought events in Holocene are recognized from the grain size changing curve and the curve also reveals a "dry-wet-dry" cycle in the precipitation history. Because these events correspond to the famous cold events, so we may draw the conclusion that dry and cold, warm and wet may be matched in the process of climate change.

HTML

Reference (40)

[1]	刘东生, 等. 黄土与环境[M]. 北京:科学出版社, 1985[Liu Tungsheng, et al. Loess and Environment[M]. Beijing: Science Press, 1985]
[2]	胡邦琦, 杨作升, 赵美训, 等. 南黄海中部泥质区7200 年以来东亚冬季风变化的沉积记录[J]. 中国科学(D辑):地球科学, 2012, 42(10):1568-1581[Hu Bangqi, Yang Zuosheng, Zhao Meixun, et al. Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area[J]. China Science(Seri. D): Earth Science, 2012, 42(10): 1568-1581]
[3]	张洪岩, 王锡魁, 隋维国, 等. 图们江河口沼泽沉积物的粒度特征及碎屑源分析[J]. 世界地质, 2006, 25(2):147-159[Zhang Hongyan, Wang Xikui, Sui Weiguo, et al. Analysis on grain-size characteristics and fragment sources of deposits in swamps near debouchment of Tumen River[J]. Global Geology, 2006, 25(2): 147-159]
[4]	郑国璋, 岳乐平, 何军锋, 等. 疏勒河下游安西古沼泽全新世沉积物粒度特征及其古气候环境意义[J]. 沉积学报, 2006, 24(5):733-739[Zheng Guozhang, Yue Leping, He Junfeng, et al. Grain-size characteristics of the sediments at palaeoswamp in Anxi County in downstream of Shulehe River during Holocene and its paleoclimatic significance[J]. Acta Sedimentologica Sinica, 2006, 24(5): 733-739]
[5]	王心源, 张广胜, 张恩楼, 等. 巢湖湖泊沉积记录的早-中全新世环境演化研究[J]. 科学通报, 2008, 53(增刊Ⅰ):132-138[Wang Xinyuan, Zhang Guangsheng, Zhang Enlou, et al. Research on early-middle Holocene environment evolution from the records of sediment in Chaohu Lake[J]. Chinese Science Bulletin, 2008, 53(Suppl.Ⅰ): 132-138]
[6]	殷书柏, 吕宪国. "泥炭气候成因说"的探讨[J]. 地理科学, 2006, 26(3):321-326[Yin Shubai, Lü Xianguo. Discussion on "the theory on climate cause of peat forming"[J]. Scientia Geographica Sinica, 2006, 26(3): 321-326]
[7]	赵红艳, 冷雪天, 王升忠. 长白山地泥炭分布、沉积速率与全新世气候变化[J]. 山地学报, 2002, 20:513-518[Zhao Hongyan, Leng Xuetian, Wang Shengzhong. Distribution, accumulation rate of peat in the Changbaishan Mountains and climate change in Holocene[J]. Journal of Mountain Science, 2002, 20: 513-518]
[8]	刘金陵. 长白山区孤山屯沼泽地13000年以来的植被和气候变化[J]. 古生物学报, 1989, 28:495-509[Liu Jinling. Vegetational and climatic changes at Gushantun Bog in Jilin, NE China Since 13, 000 Y.B.P[J]. Acta Palaeontologica Sinica, 1989, 28: 495-509]
[9]	李荣麟, 介冬梅, 刘艳萍, 等. 东北长白山区北部虎山泥炭剖面植硅体的环境指示意义[J]. 微体古生物学报, 2011, 28:329-336[Li Ronglin, Jie Dongmei, Liu Yanpin, et al. Phytolith as an environment indicator of Hushan peat section from northern region in Changbai Mountain[J]. Acta Micropalaeontologica Sinica, 2011, 28: 329-336]
[10]	王金权, 刘金陵. 长白山区全新世大暖期的氨基酸和碳同位素记录[J]. 微体古生物学报, 2001, 18:392-398[Wang Jinquan, Liu Jinling. The records of amino acids and organic carbon isotope for Holocene megathermal in Changbaishan area[J]. Acta Micropalaeontologica Sinica, 2001, 18: 392-398]
[11]	李鸿凯, 卜兆君, 王升忠, 等. 长白山区泥炭地现代有壳变形虫环境意义探讨[J]. 第四纪研究, 2009, 29(4):817-824[Li Hongkai, Bu Zhaojun, Wang Shengzhong, et al. Environmental implications of the modern testate amoebae in the peatlands in Changbai Mountains[J]. Quaternary Sciences, 2009, 29(4): 817-824]
[12]	洪冰, 刘丛强, 林庆华, 等. 哈尼泥炭δ¹⁸O记录的过去14000年温度演变[J]. 中国科学(D 辑):地球科学, 2009, 39:626-637[Hong Bing, Liu Congqiang, Lin Qinghua, et al. Temperature evolution from the δ¹⁸O record of Hani peat, Northeast China, in the last 14000 years[J]. Science China(Seri. D): Earth Science, 2009, 39: 626-637]
[13]	Stuiver M, and Reimer, P J. Extended ¹⁴C database and revised CALIB radiocarbon calibration program[J]. Radiocarbon, 1993, 35: 215-230
[14]	国家海洋局. 海洋调查规范(第四分册——海洋地质调查)[M]. 北京:海洋出版社, 1975:9-88[State Oceanic Administration. Specifications for Oceanographic Survey (volume 4: Marine Geologic Survey)[M]. Beijing: Ocean Press, 1975: 9-88]
[15]	Link A G. Textural classification of sediments[J]. Sedimentology, 1966, 7(3): 249-254
[16]	SY/T 5434—1999, 中华人民共和国石油天然气行业标准:碎屑岩粒度分析方法[S][State Petroleum and Chemical Industry. Standards of petroleum and natural gas industry of the People's Republic of China, Method of grain-size analysis of clastic rocks[S]]
[17]	成都地质学院陕北队编. 沉积岩(物)粒度分析及其应用[M]. 北京:地质出版社, 1978[Chengdu College of Geology, Shanbei team. Sedimentary Rock (Material) Particle-size Analysis and Its Application[M]. Beijing: Geological Publishing House, 1978]
[18]	肖景义, 陈建强, 孙刚, 等. 河北邯郸HZ-S孔第四纪沉积物粒度特征分析[J]. 干旱区资源与环境, 2009, 23(1):54-59[Xiao Jingyi, Chen Jianqiang, Sun Gang, et al. Grain-size characteristics of HZ-S Core Quaternary sediments in Handan City, Hebei province[J]. Journal of Arid Land Resources and Environment, 2009, 23(1): 54-59]
[19]	雷国良, 张虎才, 张文翔, 等. 柴达木盆地察尔汗古湖贝壳堤剖面粒度特征及其沉积环境[J]. 沉积学报, 2007, 25(2):274-281[Lei Guoliang, Zhang Hucai, Zhang Wenxiang, et al. Characteristics of grain-size and sedimentation of shell bar section in salt Lake Qarhan, Qaidam Basin[J]. Acta Sedimentologica Sinica, 2007, 25(2): 274-281]
[20]	黄臻, 王建力, 王勇.长江三峡巫山第四纪沉积物粒度分布特征[J].热带地理, 2010, 30(1):30-39[Huang Zhen, Wang Jianli, Wang Yong. Grain-size features of Quaternary sediments in Changjiang Three Gorge Reservoir of the Wushan area[J]. Tropical Geography, 2010, 30(1): 30-39]
[21]	李敬卫, 乔彦松, 王燕, 等. 江西九江红土堆积的粒度特征及成因研究[J]. 地质力学学报, 2009, 15(1):95-103[Li Jingwei, Qiao Yansong, Wang Yan, et al. Aeolian origin of the red earth tormation in Jiujiang city of Jiangxi province, China: Evidence from grain-size analysis[J]. Journal of Geomechanics, 2009, 15(1): 95-103]
[22]	于学峰, 周卫健, 刘晓清, 等. 青藏高原东部全新世泥炭灰分的粒度特征及其古气候意义[J]. 沉积学报, 2006, 12(6):864-869[Yu Xuefeng, Zhou Weijian, Liu Xiaoqing, et al. Grain size characteristics of the Holocene peat sediment in eastern Tibetan Plateau and its paleoclimatic significance[J]. Acta Sedimentologica Sinica, 2006, 12(6): 864-869]
[23]	Lerman A. Lakes—Chemistry, Geology, Physics[M]. Berlin: Springer-Verlag, 1978
[24]	孙永传, 李惠生. 碎屑岩沉积相和沉积环境[M]. 北京:地质出版社, 1986[Sun Yongchuan, Li Huisheng. Clastic Sedimentary Facies and Sedimentary Environment[M]. Beijing: Geological Publishing House, 1986]
[25]	施雅风. 中国全新世大暖期气候与环境[M]. 北京:海洋出版社, 1992[Shi Yafeng. The Holocene Megathermal Climate and Environment in China[M]. Beijing: Ocean Press, 1992]
[26]	宋长青, 吕厚远, 孙湘君. 中国北方花粉—气候因子转换函数建立及应用[J]. 科学通报, 1997, 42:2182-2185[Song Changqing, Lü Houyuan, Sun Xiangjun. Construction of pollen-climate factor transfer function and its application in North China[J]. Chinese Science Bulletin, 1997, 42: 2182-2185]
[27]	崔美玲, 罗运利, 孙湘君. 吉林哈尼湖钻孔5 000 年以来的古植被气候变化指示[J]. 海洋地质与第四纪地质, 2006, 26(5):117-122[Cui Meiling, Luo Yunli, Sun Xiangjun. Paleoegetatinal and paleoclimatic changes in Ha'ni Lake, Jilin since 5 ka B.P.[J]. Marine Geology and Quaternary Geology, 2006, 26(5): 117-122]
[28]	喻春霞, 罗运利, 孙湘君. 吉林柳河哈尼湖13.1～4.15cal.ka B.P.古气候演化的高分辨率孢粉记录[J]. 第四纪研究, 2008, 28(5):929-938[Yu Chunxia, Luo Yunli, Sun Xiangjun. A high-resolution pollen records from Ha'ni Lake, Jilin, Northeast China showing climate changes between 13.1 cal.ka B.P. and 4.5 cal.ka B.P.[J]. Quaternary Sciences, 2008, 28(5): 929-938]
[29]	周卫建, 李小强, 董光荣, 等. 新仙女木期沙漠/黄土过渡带高分辨率泥炭记录——东亚季风气候颤动的实例[J]. 中国科学(D 辑):地球科学, 1996, 26(2):118-124[Zhou Weijian, Li Xiaoqiang, Dong Guangrong, et al. High-resolution peat record from the desert-loess transitional belt during the Younger Dryas Interval: An example of East Asian monsoon climatic fluctuations[J]. Science China(Seri. D): Earth Science, 1996, 26(2): 118-124]
[30]	沈吉, 吴瑞金, 羊向东, 等. 大布苏湖沉积剖面碳酸盐含量、氧同位素特征的古气候意义[J]. 湖泊科学, 1997, 9(3):217-222[Shen Ji, Wu Ruijin, Yang Xiangdong, et al. Paleoclimatic change inferred from δ¹⁸O and carbonate content of the section in Dabusu Lake[J]. Journal of Lake Sciences, 1997, 9(3): 217-222]
[31]	Dykoskia C A, Edwardsa R L, Cheng H, et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China[J]. Earth and Planetary Science Letters, 2005, 233(1/2): 71-86
[32]	萧家仪, 吕海波, 周卫健, 等. 末次盛冰期以来江西大湖孢粉植被与环境演变[J]. 中国科学(D 辑):地球科学, 2007, 37(6):789-797[Xiao Jiayi, Lü Haibo, Zhou Weijian, et al. Evolution of vegetation and climate since the last glacial maximum recorded at Dahu peat site, South China[J]. Science China(Seri. D): Earth Science, 2007, 37(6): 789-797]
[33]	王志国. 吉林金川泥炭纤维素稳定碳同位素组成序列与东北季风区五千多年来的环境变迁[J]. 矿物岩石地球化学通报, 1998, 17(1):52-54[Wang Zhiguo. Reconstruction of past 5 000-year humidity changes of Northeast China using δ¹³C values of peat cellulose in Jinchuan region, Jilin province[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 1998, 17(1): 52-54]
[34]	李秉成, 雷祥义, 李正泽, 等. 西安白鹿塬全新世黄土剖面磁化率的古气候特征[J]. 海洋地质与第四纪地质, 2008, 28(2):115-121[Li Bingcheng, Lei Xiangyi, Li Zhengze, et al. Paleoclimate character of susceptibility of Holocene Loess section in Xi'an Bailuyuan[J]. Marine Geology & Quaternary Geology, 2008, 28(2): 115-121]
[35]	竺可桢. 中国近五千年来气候变迁的初步研究[J]. 中国科学(B辑), 1973(2):226-256[Zhu Kezhen. Preliminary study on climate change over last 5000 years in China[J]. Science China(Seri. B), 1973(2): 226-256]
[36]	Mayewski, P A, Rohling E E, Stager J C, et al. Holocene climate variability[J]. Quaternary Research, 2004, 62(3): 243-255
[37]	Gupta A K, Anderson D M, Overpeck J T. Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean[J]. Nature, 421: 354-357
[38]	贾耀锋, 庞奖励. 关中盆地东部李湾剖面全新世高分辨率气候研究[J]. 干旱区资源与环境, 2003, 17(3):39-43[Jia Yaofeng, Pang Jiangli. The high resolution of the Holocene climatic study in Liwan profile in eastern Guanzhong Basin[J]. Journal of Arid Land Resources and Environment, 2003, 17(3): 39-43]
[39]	唐领余, 沈才明, 李春海, 等. 花粉记录的青藏高原中部中全新世以来植被与环境[J]. 中国科学(D 辑):地球科学, 2009, 39(5):615-625[Tang Lingyu, Shen Caiming, Li Chunhai, et al. Pollen-inferred vegetation and environmental changes in the central Tibetan Plateau since 8200 yr BP[J]. Science China(Seri. D): Earth Science, 2009, 39(5): 615-625]
[40]	Johnsen S, Dahl-Jensen D, Gundestrup N S, et al. Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye3, GRIP, GISP2, Renland and North GRIP[J]. Journal of Quaternary Science, 2001, 16(4): 299-307

Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related