吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (1): 170-184.doi: 10.13278/j.cnki.jjuese.20180337

• 地质与资源 • 上一篇    

植硅体记录的敦化北部山地近2 ka泥炭沼泽演化气候背景

杜玉1,2,3, 张新荣1,2,3, 平帅飞1,2,3, 焦洁钰1,2,3, 马春梅4   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 吉林大学东北亚生物演化与环境教育部重点实验室, 长春 130026;
    3. 吉林省油页岩与共生能源矿产重点实验室, 长春 130061;
    4. 南京大学地理与海洋科学学院, 南京 210023
  • 收稿日期:2018-12-20 发布日期:2020-02-11
  • 通讯作者: 张新荣(1975-),女,副教授,博士,主要从事沉积学与第四纪地质学研究,E-mail:zhangxr@jlu.edu.cn E-mail:zhangxr@jlu.edu.cn
  • 作者简介:杜玉(1994-),女,硕士研究生,主要从事沉积学与第四纪地质学研究,E-mail:m15546115261@163.com
  • 基金资助:
    国家自然科学基金项目（41371202）

Climate Background of Peat Swamp Evolution Recorded by Phytolith over Past 2 ka in Northern Mountainous Area in Dunhua

Du Yu1,2,3, Zhang Xinrong1,2,3, Ping Shuaifei1,2,3, Jiao Jieyu1,2,3, Ma Chunmei4   

  1. 1. College of Earth Science, Jilin University, Changchun 130061, China;
    2. Key-Laboratory for Evolution of Past Life and Environment in Northeast Asia, Ministry of Education, Changchun 130026, China;
    3. Key Laboratory of Oil Shale and Coexistent Enerny Minerals of Jilin Province, Changchun 130061, China;
    4. School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China
  • Received:2018-12-20 Published:2020-02-11
  • Supported by:
    Supported by National Natural Science Foundation of China (41371202)

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摘要： 对敦化北部山地205 cm深泥炭剖面中的植硅体进行提取、鉴定和分析，结合AMS14C测年，重建研究区近2 ka的古气候环境过程，探讨其变化规律及影响因素。植硅体组合、有序聚类和植硅体指数变化趋势显示，研究区泥炭沼泽经历了4个显著阶段：即45-680 A.D.暖湿阶段；680-1340 A.D.温暖偏干阶段；1340-1870 A.D.由干转湿的寒冷阶段；1870-2017 A.D.转暖、干湿波动阶段。其中，680-1225 A.D.对应中世纪暖期（MWP），1340-1870 A.D.对应小冰期（LIA）。在此气候变化背景下，泥炭沼泽发展经历了由缓慢逐渐加快的过程。对比太阳辐射和太阳活动的变化、石笋δ18O序列、重建的东北地区古温度以及Niño3.4重建曲线，泥炭剖面的植硅体分析显示MWP和LIA期间的古气候过程受到太阳活动、太阳辐射、季风环流和ENSO（El Niño-Southern Oscillation）的控制。

关键词: 植硅体, 泥炭演化, 气候变迁, 区域差异, 敦化山地

Abstract: Based on the AMS14C dating and the phytoliths extracted from the 205 cm peat profile in the northern part of Dunhua, the paleoclimate environmental progresses of the study area near 2 ka were reconstructed,and the changing rules and influencing factors were discussed. The phytolith assemblages, ordered cluster analysis, and phytolith indexes showed that the peat swamp in the studied profile had experienced four significant stages:45-680 A. D. warm and wet stage; 680-1340 A. D. warm and dry stage; 1340-1870 A. D. cold and dry to wet stage; 1870-2017 A. D. warm, dry, and wet fluctuation stage. The paleoclimate condition in 680-1225 A. D. was similar to that in the Medieval Warm Period (MWP), and the condition in 1340-1870 A. D. was similar to that in the Little Ice Age (LIA). In such a climate context, the peat swamp developed a slow to gradually accelerated period. Compared with solar irradiation, stalagmite δ18O sequence,Niño3.4, and the paleotemperature reconstruction in Northeast China, the phytolith analysis in the studied peat profile indicated that the paleoclimate process during MWP and LIA was controlled by solar activity, solar irradiation, monsoon circulation, and ENSO (El Niño-Southern Oscillation).

Key words: phytolith, peat swamp evolution, climate changes, regional differences, moutainous area in Dunhua

中图分类号: 

  • P532
[1] de Menocal P B. Cultural Responses to Climate Change During the Late Holocene[J]. Science, 2001, 292:667-673.
[2] 李亮, 马春梅, 鹿化煜, 等.江西中部玉华山沼泽泥炭记录的过去两千年气候变化初步研究[J].第四纪研究,2017,37(3):548-559. Li Liang, Ma Chunmei, Lu Huayu, et a1. A Preliminary Study of the Climate Change Since 2 ka Archived by a Peat Core from Yuhua Mountain in the Middle Jiangxi Province[J]. Quaternary Sciences, 2017, 37(3):548-559.
[3] 王绍武.中世纪暖期与小冰期[J].气候变化研究进展,2010,6(5):388-390. Wang Shaowu. Medieval Warm Period and Little Ice Age[J]. Advances in Climate Change Research, 2010, 6(5):388-390.
[4] 陈建徽,陈发虎,冯松, 等.中世纪暖期和小冰期亚洲大陆水文气候变化:空间格局和可能机制[C]//第二届深海研究与地球系统科学学术研讨会论文集.上海:同济大学,2012:150-151. Chen Jianhui, Chen Fahu, Feng Song, et al. Hydrological and Climatic Changes in the Asian Continent During MWP and LIA:Spatial Patterns and Possible Mechanisms[C]//Proceedings of the 2nd Symposium on Deep Sea Research and Earth System Science. Shanghai:Tongji University, 2012:150-151.
[5] 张东良,兰波,杨运鹏.不同时间尺度的阿尔泰山北部和南部降水对比研究[J].地理学报,2017,72(9):1569-1579. Zhang Dongliang, Lan Bo, Yang Yunpeng. Comparison of Precipitation Variations at Diferent Time Scales in the Northern and Southern Altai Mountains[J]. Acta Geographica Sinica, 2017, 72(9):1569-1579.
[6] 田立德,姚檀栋.青藏高原冰芯高分辨率气候环境记录研究进展[J].科学通报,2016,61(9):926-937. Tian Lide, Yao Tandong. High-Resolution Climatic and Environmental Records from the Tibetan Plateau Ice Cores[J]. Chinese Science Bulletin, 2016, 61(9):926-937.
[7] 李明慧,康世昌.青藏高原湖泊沉积物对古气候环境变化的响应[J].盐湖研究,2007,15(1):63-72. Li Minghui, Kang Shichang. Responses of Lake Sediments to Paleoenvironmental and Paleoclimatic Changes in Tibetan Plateau[J]. Journal of Salt Lake Research, 2007, 15(1):63-72.
[8] 葛全胜,刘健,方修琦,等.过去2000年冷暖变化的基本特征与主要暖期[J].地理学报,2013,68(5):579-592. Ge Quansheng, Liu Jian, Fang Xiuqi, et al. General Characteristics of Temperature Change and Centennial Warm Periods During the Past 2000 Years[J]. Acta Geographica Sinica, 2013, 68(5):579-592.
[9] 迟宏,张振华,赵倩.近千年来洞穴沉积物的古气候及古环境记录的研究进展[J].鲁东大学学报(自然科学版),2016,32(3):278-283. Chi Hong, Zhang Zhenhua, Zhao Qian. Paleoclimate and Paleoenvironment Records of the Karst Sendiment in the Past 1000 Years[J]. Journal of Ludong University (Natural Science Edition), 2016, 32(3):278-283.
[10] 郑景云,王绍武.中国过去2000年气候变化的评估[J].地理学报,2005,60(1):21-31. Zheng Jingyun, Wang Shaowu. Assessment on Climate Change in China for the Last 2000 Years[J]. Acta Geographica Sinica, 2005, 60(1):21-31.
[11] 张娴.近2000年中国年代际-百年尺度气候特征及其全球对比[D].南京:南京信息工程大学,2012. Zhang Xian. The Decadal to Centennial Variability of China Climate in the Last 2000 Years and Its Relationship with Global Climate[D]. Nanjing:Nanjing University of Information Science & Technology, 2012.
[12] 柳中晖, 周爱锋, 刘卫国.近千年来青海湖水热变化再重建[J].第四纪研究,2017,37(5):974-981. Liu Zhonghui, Zhou Aifeng, Liu Weiguo. Further Reconstruction of Temperature and Salinity Changes in Lake Qinghai over the Past Millennium[J]. Quaternary Sciences, 2017, 37(5):974-981.
[13] 陈建徽, 陈发虎, 张家武, 等.中国西北干旱区小冰期的湿度变化特征[J].地理学报,2008,63(1):23-33. Chen Jianhui, Chen Fahu, Zhang Jiawu, et al. Humidity Vaiability in the Arid Northwest China During LIA Derived from Different Proxy Records[J]. Acta Geographica Sinica, 2008, 63(1):23-33.
[14] 任维鹤,易桂田,李泉.中国东部季风区小冰期干湿变化及影响机制[J].安徽师范大学学报(自然科学版),2017,40(5):479-483. Ren Weihe, Yi Guitian, Li Quan. Spatial and Possible Mechanisms of Hydroclimatic Changes in Eastern China During the Little Ice Age[J]. Journal of Anhui Normal University (Natural Science), 2017, 40(5):479-483.
[15] Peng Youbing, Xu Ying, Jin Liya. Climate Changes over Eastern China During the Last Millennium in Simulations and Reconstructions[J]. Quaternary International, 2009, 208:11-18.
[16] 左昕昕,靳鹤龄.中世纪暖期气候研究综述[J].中国沙漠,2009,29(1):136-142. Zuo Xinxin, Jin Heling. An Overview of Studies on Medieval Warm Period[J]. Journal of Desert Research, 2009, 29(1):136-142.
[17] 靳春寒,刘健,王志远.中国中世纪暖期温度年代际变化特征及成因分析[J].第四纪研究,2016,36(4):970-982. Jin Chunhan, Liu Jian, Wang Zhiyuan.Study on the Characteristics and Cause of on Interdecadal Temperature Changes in China During the MWP[J]. Quaternary Research, 2016, 36(4):970-982.
[18] 龚道溢.全球大气涛动[J].地学前缘,2000,7(增刊2):208. Gong Daoyi. Global Atmospheric Oscillation[J]. Earth Science Frontiers, 2000, 7(Sup. 2):208.
[19] Chen Jianhui, Chen Fahu, Feng Song, et al. Hydroclimatic Changes in China and Surroundings During the Medieval Climate Anomaly and Little Ice Age:Spatial Patterns and Possible Mechanisms[J]. Quaternary Science Reviews, 2015, 107:98-111.
[20] 张礼平,张乐飞,曾凡平.ENSO与中国东部夏季降水的关联[J].热带气象学报,2012,28(2):177-186. Zhang Liping, Zhang Lefei, Zeng Fanping. The Relationship Between ENSO and JJA Rainfall over the East of China[J]. Journal of Tropical Meteorology, 2012, 28(2):177-186.
[21] 周秀骥,赵平,刘舸,等.中世纪暖期、小冰期与现代东亚夏季风环流和降水年代-百年尺度变化特征分析[J].科学通报,2011, 56(25):2060-2067. Zhou Xiuji, Zhao Ping, Liu Ge, et al. Characteristics of Decadal-Centennial-Scale Changes in East Asian Summer Monsoon Circulation and Precipitation During the Mediveal Warm Period and Little Ice Age and in the Present Day[J]. Chinese Science Bulletin, 2011, 56(25):2060-2067.
[22] 夏玉梅,汪佩芳.密山杨木3000多年来气候变化的泥炭记录[J].地理研究,2000,19(1):53-59. Xia Yumei, Wang Peifang. Peat Record of Climate Change Sincce 3000 Years in Yangmu, Mishan Region[J]. Geographical Resarch, 2000, 19(1):53-59.
[23] Chu G Q, Sun Q, Wang X H, et al.A 1600 Year Multiproxy Record of Paleoclimatic Change from Varved Sediments in Lake Xiaolongwan, Northeastern China[J]. Journal of Geophysical Research Atmospheres, 2009, 114(114):2191-2196.
[24] Li J, Mackay A W, Zhang Y, et al. A 1000 Year Record of Vegetation Change and Wildfire from Maar Lake Erlongwan in Northeast China[J]. Quaternary International, 2013, 290/291:313-321.
[25] Chu G Q, Sun Q, Wang X H, et al.Snow Anomaly Events from Historical Documents in Eastern China During the Past Two Millennia and Implication for Low-Frequency Variability of AO/NAO and PDO[J]. Geophysical Research Letters, 2008, 35(14):63-72.
[26] 林庆华,冷雪天,洪冰.大兴安岭近1000年来气候变化的泥炭记录[J].矿物岩石地球化学通报,2004,23(1):15-18. Lin Qinghua, Leng Xuetian, Hong Bing. The Peat Record of 1 ka of Climate in Daxing Anling[J]. Bulletin of Mineralogy Petrology and Geochemistry, 2004, 23(1):15-18.
[27] 王芳. 辽宁水洞高分辨率石笋记录的近1000年来东亚夏季风变化[D]. 北京:中国地质大学(北京),2016. Wang Fang. East Asian Summer Monsoon Variability over the Last Millennium Recorded by Stalagmite in Cave Shuidong, Liaoning Province[D]. Beijing:China University of Geosciences (Beijing), 2016.
[28] 鲍锟山,赵红梅,于晓菲,等.大气环境变化的泥炭地质档案[J].地质论评,2011,57(2):234-242. Bao Kunshan, Zhao Hongmei, Yu Xiaofei, et al. Atmospheric Environmental Changes Records from Peat Bogs:A Review[J]. Geological Review, 2011, 57(2):234-242.
[29] 多洛雷斯-派潘诺.植硅石分析:在考古学和地质学中的应用[M].姜钦华, 王宪曾, 邓平,译. 北京:北京大学出版社, 1994:1. Pipemo Dolores. Phytolith Analysis:An Archaeological and Geological Perspective[M]. Translated by Jiang Qinhua, Wang Xianzeng, Deng Ping. Beijing:Peking University Press, 1994:1.
[30] Rovner I. Potential of Opal Phytoliths for Use in Paleoecological Reconstruction[J]. Quaternary Research, 1971, 1(3):343-359.
[31] 张新荣. 东北地区晚全新世泥炭沉积的植硅体气候指示意义研究[D]. 长春:吉林大学,2006:1-10. Zhang Xinrong. Phytolith Research as an Indicator of Paleo-Climate in the Late-Holoncene Peat Deposits of Northeast China[D]. Changchun:Jilin University, 2006:1-10.
[32] 赵红艳, 王升忠, 何春光. 吉林省敦化地区泥炭成矿类型及性质[J]. 东北师范大学学报(自然科学版), 2001, 33(2):93-96. Zhao Hongyan, Wang Shengzhong, He Chunguang. Types and Properties of Peat Mineralization in Dunhua Area, Jilin Province[J]. Journal of Northeast Normal University (Natural Science Edition), 2001, 33(2):93-96.
[33] 温大成. 敦化市志[M]. 北京:新华出版社, 1991:20-50. Wen Dacheng.Dunhua Chronicles[M]. Beijing:Xinhua Publishing House, 1991:20-50.
[34] 郭梅娥, 介冬梅, 葛勇, 等. 长白山区湿地表土植硅体特征及其环境意义[J]. 古地理学报, 2012, 14(5):639-650. Guo Meie, Jie Dongmei, Ge Yong, et al. Phytolith Characteristics and Their Significance of Environment in Surface Soils from Wetlands of Changbai Shan Area[J]. Journal of Palaeogeography, 2012, 14(5):639-650.
[35] 李建东. 吉林植被[M]. 长春:吉林科学技术出版社,2001:220-253. Li Jiandong.Jilin Vegetation[M]. Changchun:Jilin Science and Technology Press, 2001:220-253.
[36] 张新荣,胡克,刘莉莉.吉林敦化地区全新世泥炭沉积中植硅体分析[J].微体古生物学报,2005,22(2):202-207. Zhang Xinrong, Hu Ke, Liu Lili.Phytolith Analysis in Holocene Peat Deposits in Dunhua Area, Jilin Province[J]. Acta Micropalaeontologica Sinica, 2005, 22(2):202-207.
[37] 王永吉,吕厚远,植物硅酸体研究及应用[M]. 北京:海洋出版社,1993:50-124. Wang Yongji, Lü Houyuan. Phytolith Study and Its Application[M]. Beijing:China Ocean Press, 1993:50-124.
[38] 吕厚远,贾继伟,王伟铭,等."植硅体"含义和禾本科植硅体的分类[J].微体古生物学报,2002,19(4):389-396. Lü Houyuan, Jia Jiwei, Wang Weiming, et al. On the Meaning of Phytolith and Its Classification in Gramineae[J]. Acta Micropalaeontologica Sinica, 2002, 19(4):389-396.
[39] Gu Y S, Pearsall D M, Xie S C, et al. Vegetation and Fire History of a Chinese Site in Southern Tropical Xishuangbanna Derivedfrom Phytolith and Charcoal Records from Holocene Sediments[J]. Journal of Biogeography, 2008, 35(2):325-341.
[40] 张新荣,胡克,王东坡.东北地区泥炭表土中植硅体的形态特征[J].地理科学,2007,22(6):831-836. Zhang Xinrong, Hu Ke, Wang Dongpo. Morphological Characteristics of Phytolith in Surface Peat Deposits of Northeast China[J]. Scientia Geographica Sinica, 2007, 22(6):831-836.
[41] 舒军武,黄小忠,徐德克,等.新版Tilia软件:中文指南和使用技巧[J].古生物学报,2018,57(2):260-272. Shu Junwu,Huang Xiaozhong, Xu Deke, et al. The Latest TILIA Softwares:Chinese Manual and Practise Skills[J]. Acta Palaeontologica Sinica, 2018, 57(2):260-272.
[42] Diester-Haass L, Schrader H, Thiede J. Sedimentological and Palaeoclimatological Investigations of Two Pelagic-Ooze Cores off Cape Barbas, North-West Africa[J]. Meteor, Forschung-Ergebnisse, 1973, 16:19-66.
[43] Wang W M, Liu J L, Zhou X D. Climate Indexes of Phytoliths from Homo Erectus'Cave Deposits in Nanjing[J]. Chinese Science Bulletin, 2003, 48(18):2005-2009.
[44] Blaauw M, Christen J A. Flexible Paleoclimate Age-Depth Models Using an Autoregressive Gamma Process[J]. Bayesian Analysis, 2011, 6:457-474.
[45] Knezevic S Z, Streibig J C, Ritz C. Utilizing R Software Package for Dose-Response Studies:The Concept and Data Analysis[J]. Weed Technology, 2007, 21(3):840-848.
[46] Blaauw M,Christen J A. Bacon Manual-v2.2[EB/OL].[2018-11-15]. www.chrono.qub.ac.uk/blaauw/manualBacon_2.2.pdf.
[47] Madella M, Alexandre A, Ball T. International Code for Phytolith Nomenclature 1.0[J]. Annals of Botany, 2005, 96(2):253-260.
[48] Cordova C E,Johnson W C, Mandel R D, et al. Late Quaternary Environmental Change Inferred from Phytoliths and Other Soil-Related Proxies:Case Studies from the Central and Southern Great Plains, USA[J]. Catena, 2011, 185(2):87-108.
[49] Albert R M, Shahack-Gross R, Cabanes D. Phytolith-Rich Layers from the Late Bronze and Iron Ages at Tel Dor (Israel):Mode of Formation and Archaeological Significance[J]. Journal of Archaeological Science, 2008, 35(1):57-75.
[50] Parr J F. Effect of Fire on Phytolith Coloration[J]. Geoarchaeology, 2006, 21(2):171-185.
[51] Piperno D R. Phytoliths:A Comprehensive Guide for Archaeologists and Paleoecologists[M].[S. l.]:Alta Mira Press, 2006:135.
[52] Lehndorff E,Linstädter J, Kehl M, et al. Fire History Reconstruction from Black Carbon Analysis in Holocene Cave Sediments at Ifri Oudadane, Northeastern Morocco[J]. The Holocene, 2015, 25(2):398-402.
[53] 董进国.过去3000年季风降水变化与突变事件的洞穴石笋记录对比[J].干旱区资源与环境,2012,26(11):36-41. Dong Jinguo.Summer Monsoon Precipitation Variations and Abrupt Climate Events During the 3000 Years:Records from Stalagmites in China[J]. Journal of Arid Land Resources and Environment, 2012, 26(11):36-41.
[54] 柴岫. 泥炭地学[M]. 北京:地质出版社,1990. Chai Xiu. Study of Peafland[M]. Beijing:Geological Publishing House, 1990.
[55] Bauer E, Claussen M, Brovkin V. Assessing Climate Forcings of the Earth System for the Past Millennium[J]. Geophycical Research Letters, 2003, 30(6):1276.
[56] Bard E, Raisbeck G, Yiou F, et al. Solar Irradiance During the Last 1200 Years Based on Cosmogenic Nuclides[J]. Tellus Series B:Chemical and Physical Meteorlogy, 2000, 52(3):985-992.
[57] Dai X G, Wang P, Zhang P Q, et al.Rainfall Spectrum Change in North China and Its Possible Mechanism[J]. Progress in Natural Science, 2004, 14(7):598-604.
[58] Emile-Geay J, Cobb K M, Mann M E, et al. Estimating Central Equatorial Pacific SST Variability over the Past Millennium:Part II:Reconstructions and Implications[J]. Journal of Climate, 2013, 26(7):2329-2352.
[59] 葛全胜,郑景云,郝志新,等.过去2000年中国气候变化的若干重要特征[J].中国科学:地球科学,2012,42(6):934-942. Ge Quansheng,Zheng Jingyun,Hao Zhixin, et a1. General Characteristics of Climate Changes During the Past 2000 Years in China[J]. Science China:Earth Sciences, 2012, 42(6):934-942.
[60] Ge Q S, Zheng J Y, Hao Z X, et al. Temperature Variation Through 2000 Years in China:An Uncertainty Analysis of Reconstruction and Regional Difference[J]. Geophysical Research Letters, 2010, 37(3):1-5.
[61] 丁大林,张训华,于俊杰,等.浙闽泥质区全新世物源和古气候演化研究进展[J].吉林大学学报(地球科学版),2019,49(1):178-195. Ding Dalin, Zhang Xunhua, Yu Junjie, et al. Progressin Sedimentary Sourcesand Palaeoclimate Evolution in Zhejiang-Fujian Mud Areain Holocene[J]. Journal of Jilin University (Earth Science Edition), 2019, 49(1):178-195.
[62] 葛全胜,刘璐璐,郑景云,等.过去千年太阳活动异常期的中国东部旱涝格局[J].地理学报,2016,71(5):707-717. Ge Quansheng, Liu Lulu, Zheng Jingyun, et al. Spatial Patterns of Drought/Flood over Eastern China in the Periods of Anomalous Solar Activity During the Past Millennium[J]. Acta Geographica Sinica, 2016, 71(5):707-717.
[63] 中央气象局气象科学研究院. 中国近五百年旱涝分布图集[M]. 北京:地图出版社, 1981. Chinese Academy of Meteorological Sciences. Yearly Charts of Dryness/Wetness in China for the Last 500 Years Period[M]. Beijing:Map Publishing House, 1981.
[64] 张德二,刘传志.《中国近五百年旱涝分布图集》续补(1980-1992年)[J]. 气象杂志, 1993,19(11):41-45. Zhang De'er, Liu Chuanzhi. Continuation (1980-1992) of the Yearly Charts of Dryness/Wetness in China for the Last 500 Years Period[J]. Meteorological Monthly, 1993, 19(11):41-45.
[65] 张德二,李小泉,梁有叶. 《中国近五百年旱涝分布图集》的再续补(1993-2000年)[J]. 应用气象学报, 2003, 14(3):379-384. Zhang De'er, Li Xiaoquan, Liang Youye. Continuation (1993-2000) of the Yearly Charts of Dryness/Wetness in China for the Last 500 Years Period[J]. Journal of Applied Meteorological Science, 2003, 14(3):379-384.
[66] 夏杨,孙旭光,闫燕,等.全球变暖背景下ENSO特征的变化[J].科学通报,2017,62(16):1738-1751. Xia Yang, Sun Xuguang,Yan Yan, et al. ENSO Characteristics in the Context of Global Warming[J]. Chinese Science Bulletin, 2017, 62(16):1738-1751.
[67] 王志远,刘健.过去2000年全球典型暖期特征与机制的模拟研究[J].第四纪研究,2014,34(6):1136-1145. Wang Zhiyuan, Liu Jian. Modeling Study on the Characteristics and Mechanisms of Global Typical Warm Periods over the Past 2000 Years[J]. Quaternary Sciences, 2014, 34(6):1136-1145.
[68] 谭明. 近千年气候格局的环流背景:ENSO态的不确定性分析与再重建[J]. 中国科学:地球科学, 2016, 46(5):657-673. Tan Ming. Circulation Background of Climate Patterns in the Past Millennium:Uncertainty Analysis and Re-Reconstruction of ENSO-Like State[J]. Science China:Earth Sciences, 2016, 46(5):657-673.
[69] 周琳.东北气候[M].北京:中国气象出版社,1991. Zhou Lin. The Northeast Climate[M]. Beijing:China Meteorological Press, 1991.
[70] 钱代丽,管兆勇.超强与普通厄尔尼诺海-气特征差异及对西太平洋副热带高压的不同影响[J].气象学报,2018,763):394-407. Qian Daili,Guan Zhaoyong. Different Features of Super and Regular El Niño Events and Their Impacts on the Variation of the West Pacific Subtropical High[J]. Acta Meteorological Sinica, 2018, 76(3):394-407.
[71] 蔡学湛,温珍治,吴滨.西太平洋副高与ENSO的关系及其对福建雨季降水分布的影响[J].热带气象学报,2003,19(1):36-42. Cai Xuezhan, Wen Zhenzhi,Wu Bin. Relationship Between West Pacific Subtropical High and ENSO and Its Influence on Rainfall Distribution of Rainy Season in Fujian[J]. Journal of Tropical Meteorology, 2003, 19(1):36-42.
[72] 李仁成,樊俊,高崇辉.植硅体现代过程研究进展[J].地球科学进展,2013,28(12):1287-1295. Li Rencheng, Fan Jun,Gao Chonghui. Advance in Modern Phytolith Reserch[J]. Advances in Earth Science, 2013, 28(12):1287-1295.
[73] 顾延生,刘胡玫,曾佐勋,等.腾格里沙漠东缘26 ka来环境演化的植硅体记录[J].地球科学,2016,41(4):605-611. Gu Yansheng, Liu Humei, Zeng Zuoxun, et al. Environmental Change Documented by Pluvial Phytolith Records in the Past 26 ka on East Edge of Tengger Desert[J]. Earth Science, 2016, 41(4):605-611.
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