DRY-HOT CLIMATE CHANGES FROM 210 TO 120 kaBP BY LACUSTRINE SEDIMENTS IN YUANMOU BASIN, YUNNAN

LI Hua-yong; MING Qing-zhong; ZHANG Hu-cai; SU Huai; ZHANG Zi-qiang; DUAN Li-zeng

Volume 19 Issue 1

Mar. 2013

Turn off MathJax

Article Contents

Article Navigation > Journal of Geomechanics > 2013 > 19(1): 14-25

LI Hua-yong, MING Qing-zhong, ZHANG Hu-cai, et al., 2013. DRY-HOT CLIMATE CHANGES FROM 210 TO 120 kaBP BY LACUSTRINE SEDIMENTS IN YUANMOU BASIN, YUNNAN. Journal of Geomechanics, 19 (1): 14-25.

Citation:

LI Hua-yong, MING Qing-zhong, ZHANG Hu-cai, et al., 2013. DRY-HOT CLIMATE CHANGES FROM 210 TO 120 kaBP BY LACUSTRINE SEDIMENTS IN YUANMOU BASIN, YUNNAN. Journal of Geomechanics, 19 (1): 14-25.

Citation:

LI Hua-yong, MING Qing-zhong, ZHANG Hu-cai, et al., 2013. DRY-HOT CLIMATE CHANGES FROM 210 TO 120 kaBP BY LACUSTRINE SEDIMENTS IN YUANMOU BASIN, YUNNAN. Journal of Geomechanics, 19 (1): 14-25.

PDF( 1614 KB)

DRY-HOT CLIMATE CHANGES FROM 210 TO 120 kaBP BY LACUSTRINE SEDIMENTS IN YUANMOU BASIN, YUNNAN

LI Hua-yong^{1, 2
,},
MING Qing-zhong^{1, 2
,
,},
ZHANG Hu-cai^{1, 2},
SU Huai^{1, 2},
ZHANG Zi-qiang^{1, 2},
DUAN Li-zeng^{1, 2}

1.
Laboratory of Plateau Lake Ecology and Global Change, Key Laboratory of Plateau Geographic Process and Environment Changes, Kunming 650500, China
2.
College of Tourism & Geography Science, Yunnan Normal University, Kunming 650500, China

More Information

Received: 2012-11-30
Published: 2013-06-01

Abstract

Abstract

Langbapu Palaeolake is located in the west of Yuanmou Basin. A complete lacustrine sediments stratum (27m-thick) was preserved and the ESR dating was accomplished in this paper. The research results showed that Langbapu Lake existed from 216±20 to 121±10 kaBP, which covered the end of the penultimate interglacial, the penultimate glaciation as well as the beginning of the last interglacial. Based on the analysis of grain size, magnetic susceptibility and pollen, the palaeoclimatic changes during 216±20 and 121±10 kaBP of Yuanmou Basin has been reconstructed. During 216~185 kaBP, the mean pollen concentration was the highest and Cycadaceae and Cyperaceae, as well as Sedge vegetation appeared, which indicated that the climate was relatively hygrothermal. During 185~150 kaBP, the pollen concentration decreased rapidly. In the 160 kaBP, the pollen concentration was only 8.67 grain/100 g, which was corresponding to the glacial maximum of penultimate glaciation. During 150~122 kaBP, several sandy gravel layers appeared. The proportion of herb increased. The palaeoclimate became warmer but drier, which was very similar to today's climate. The Langbapu Lake shrank and disappeared at last. The mean pollen concentration of lake sediments was only 34.35 grain/100 g, so we thought that dry-hot climate was already significantly before the penultimate interglacial. The characteristics of dry-hot climate were very similar to modern status after the last interglacial.
- Yuanmou Basin,
- penultimate glaciations,
- pollen,
- grain size,
- climate change,
- dry-hot valley

FullText(HTML)

References(50)

References

[1]	浦庆余, 钱方.对元谋人化石地层——元谋组的研究[J].地质学报, 1977, (1):89~100. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197701007.htm PU Qing-yu, QIAN Fang. Study on the fossil human strata:The Yuanmou Formation[J]. Acta Geologica Sinica, 1977, (1):89~100. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE197701007.htm
[2]	尹济云, 梁其中, 江能人.元谋盆地晚新生代古地磁地层年代学及其古生物意义[J].云南地质, 1994, 13(3):306~311. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD403.007.htm YIN Ji-yun, LIANG Qi-zhong, JIANG Neng-ren. The late Cenozoic palaeomagnetic chronostratigraphy of Yuanmou Basin and its paleontologic significance[J]. Yunnan Institute of Geological Sciences, 1994, 13(3):306~311. http://www.cnki.com.cn/Article/CJFDTOTAL-YNZD403.007.htm
[3]	邱铸鼎.云南禄丰、元谋晚中新世古猿地点始鼠科化石[J].古脊椎动物学报, 2006, 44(4):307~319. http://www.cnki.com.cn/Article/CJFDTOTAL-GJZD200604003.htm QIU Zhu-ding. Eomyids (Mammalia:Rodentia) from the Late Miocene Lufeng and Yuanmou hominoid localities, Yunnan[J]. Vertebrata Palasiatica, 2006, 44(4):307~319. http://www.cnki.com.cn/Article/CJFDTOTAL-GJZD200604003.htm
[4]	张云翔, 邱占祥, 郑良, 等.云南元谋小河盆地含古猿化石地层的沉积特点与对比[J].沉积学报, 2001, 19(1):85~89. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200101014.htm ZHANG Yun-xiang, QIU Zhan-xiang, ZHENG Liang, et al. Sedimentary feature and correlation of Hominoid fossil stratigraphy of Xiaohe Basin, Yuanmou, Yunnan[J]. Acta Sedimentologica Sinica, 2001, 19(1):85~89. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200101014.htm
[5]	张云翔, 郑良, 吉学平, 等.云南元谋古猿动物群化石埋藏学[J].地质学报, 2002, 76(1):45~49. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200201007.htm ZHANG Yun-xiang, ZHENG Liang, JI Xue-ping, et al. Taphonomy of the Hominoid Faunain the Yuanmou Basin Yunnan[J]. Acta Geologica Sinica, 2002, 76(1):45~49. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200201007.htm
[6]	刘东生, 丁梦林.关于元谋人化石地质时代的讨论[J].人类学学报, 1983, 2(1):40~48. http://www.cnki.com.cn/Article/CJFDTOTAL-RLXB198301004.htm LIU Dong-sheng, DING Meng-lin. Discussion on the age of "Yuanmou Man"[J]. Acta Anthropologica Sinica, 1983, 2(1), 40~48. http://www.cnki.com.cn/Article/CJFDTOTAL-RLXB198301004.htm
[7]	刘泽纯, 李庆辰.关于元谋盆地的沉积特征与地层划分[J].海洋地质与第四纪地质, 1988, 8(4):66~77. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198804012.htm LIU Ze-chun, LI Qing-chen. On the stratigraphical classification of the deposits in the yuanmou sedimentary basin[J]. Marine Geology & Quaternary Geology, 1988, 8(4):66~77. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ198804012.htm
[8]	Zhu Ri-xiang, An Zhi-sheng, Richard Potts, et al. Magnetostratigraphic dating of humans in China[J]. Earth-Science Reviews, 2003, 61:341~359. doi: 10.1016/S0012-8252(02)00132-0
[9]	Masayuki Hyodo, Hideo Nakaya, Atsushi Urabe, et al. Paleomagnetic dates of hominid remains from Yuanmou, China, and other Asian sites[J]. Journal of Human Evolution, 2002, 43:27~41. doi: 10.1006/jhev.2002.0555
[10]	Atsushi Urabe, Hideo Nakaya, Tetsuji Muto, et al. Lithostratigraphy and depositional history of the Late Cenozoic hominid-bearing successions in the Yuanmou Basin, southwest China[J]. Quaternary Science Review, 2001, (20):1671~1681.
[11]	Chang Zhi-gang, Xiao Ju-le, Lv Liang-qing, et al. Abrupt shift in the Indian monsoon during the Pliocene marked by high-resolution terrestrial records from the Yuanmou Basin in southwest China[J]. Journal of Asian Earth Sciences, 2010, (37):166~175.
[12]	Zhu R X, Potts R, Pan Y X, et al. Paleomagnetism of the Yuanmou Basin near the southeastern margin of the Tibetan Plateau and its constraints on late Neogene sedimentation and tectonic rotation[J]. Earth and Planetary Science Letters, 2008, 272(1-2):97~104. doi: 10.1016/j.epsl.2008.04.016
[13]	张虎才, 钱方, 陈怀录.元谋盆地元谋组地层的裂变径迹年代数据[J].兰州大学学报:自然科学版, 1994, 30(1):147~148. http://www.cnki.com.cn/Article/CJFDTOTAL-LDZK401.030.htm ZHAN GHu-cai, QIAN Fang, CHEN Huailu. Fission track of Yuanmou Formation in Yuanmou Basin dates[J]. Journal of Lanzhou university (nature sciences), 1994, 30(1):147~148. http://www.cnki.com.cn/Article/CJFDTOTAL-LDZK401.030.htm
[14]	张宗祜, 刘平贵, 钱方, 等.元谋盆地晚新生代地质研究的新进展[J].海洋地质与第四纪地质, 1994, 14(2):1~18. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ402.000.htm ZHANG Zong-hu, LIU Ping-gui, QIAN Fang, et al. New development in research of late cenozoic stratigraphy in Yuanmou Basin[J]. Marine Geology & Quaternary Geology, 1994, 14(12):1~18. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ402.000.htm
[15]	闵隆瑞, 尹占国, 张金起.龙街粉砂层形成时代及其古环境[J].第四纪研究, 1990, (4):354~362. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199004007.htm MIN Long-rui, YIN Zhan-guo, ZHANG Jin-qi. The formation time and paleoenvironment of the Longjie silt bed[J]. Quarternary Sciences, 1990, (4):354~362. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199004007.htm
[16]	吕金福, 曹家欣.云南龙街盆地第四纪沉积及环境演化[J].第四纪研究, 1992, (8):216~223. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199203002.htm LÜ Jin-fu, CAO Jia-xin. Quarternary sediments and environmental evolution of the Longjie basin, Yunnan province[J]. Quarternary Sciences, 1992, (8):216~223. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199203002.htm
[17]	张宗祜.川滇南北构造带中段晚新生代地质研究[M].北京:石油工业出版社, 1994:1~258. ZHANG Zong-hu. Research on the late Cenozoic geological in the middle of Sichuan-Yunnan north-south tectonic belt[M]. Bei jing:Petroleum Industry Press, 1994:1~258.
[18]	CHENG Ye-ming, LI Cheng-sen, JIANG Xiao-mei, et al. A new species of Lagerstroemioxylon (Lythraceae) from the Pliocene of Yuanmou, Yunnan, China[J]. Acta Phytotaxonomica Sinica, 2007, 45(3):315~320. doi: 10.1360/aps050119
[19]	程业明, 王宇飞, 李承森, 等.云南元谋上新统秋枫化石木的首次发现及古环境意义[J].古地理学报, 2005, 7(1):107~112. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200501011.htm CHENG Ye-ming, WANG Yu-fei, LI Cheng-sen, et al. Fossil woods of bischofia javanica BI. from the Pliocene and palaeoenvironmental implication in Yuanmou Basin, Yunnan Province[J]. Journal of Palaeogeaphy, 2005, 7(1):107~112. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200501011.htm
[20]	刘耕武, 李代芸, 黄翡, 等.云南元谋盆地上新世甘棠组植物和孢粉组合及其古气候意义[J].古生物学报, 2002, 41(1):1~9. http://www.cnki.com.cn/Article/CJFDTOTAL-GSWX200201001.htm LIU Geng-wu, LI Dai-yun, HUANG Fei, et al. A Pliocene flora from the gantang formation of Yuanmou Basin, Yunnan Province, southwestern China and its paleoclimate significance[J]. Acta palaeontologica sinica, 2002, 41(1):1~9. http://www.cnki.com.cn/Article/CJFDTOTAL-GSWX200201001.htm
[21]	黄成敏, 王成善, 何毓蓉, 等.元谋盆地古红土的土壤发生学特征及古环境意义[J].土壤通报, 2004, 35(3):251~256. http://www.cnki.com.cn/Article/CJFDTOTAL-TRTB200403003.htm HUANG Cheng-min, WANG Cheng-shan, HE Yu-rong, et al. Pedogenetic properties and paleo-environmental implication of Paleo-Krasnosems in the Yuanmou Basin[J]. Chinese Journal of Soil Science, 2004, 35(3):251~256. http://www.cnki.com.cn/Article/CJFDTOTAL-TRTB200403003.htm
[22]	张叶春, 李吉均, 朱俊杰, 等.晚新生代元谋盆地演化与河谷发育研究[J].兰州大学学报:自然科学版, 1999, 35(1):199~205. http://www.cnki.com.cn/Article/CJFDTOTAL-LDZK901.037.htm ZHANG Ye-chun, LI Ji-jun, ZHU Jun-jie, et al. Studies on development of Yuanmou Basin and valley during Late Cenozoic[J]. Journal of Lanzhou University:Nature Sciences, 1999, 35(1):199~205. http://www.cnki.com.cn/Article/CJFDTOTAL-LDZK901.037.htm
[23]	李华勇, 明庆忠.金沙江石鼓-宜宾段河谷-水系演化研究综述与讨论[J].地理与地理信息科学, 2011, 27(2):50~55. http://www.cnki.com.cn/Article/CJFDTOTAL-DLGT201102013.htm LI Hua-yong, MING Qing-zhong. Summary and prospects for the valley & drainage evolution of the Shigu-Yibin Section of the Jinsha River[J]. Geography and Geo-Information Science, 2011, 27(2):50~55. http://www.cnki.com.cn/Article/CJFDTOTAL-DLGT201102013.htm
[24]	云南省元谋县志编纂委员会.元谋县志[M].昆明:云南人民出版社, 1993:30~62. Compiling Committee of Yunnan Yuanmou County Annals. Yuanmou County Annals[M]. Kunming:Yunnan People's Press, 1993:30~62.
[25]	陈敬安, 万国江, 张峰, 等.不同时间尺度下的湖泊沉积物环境记录——以沉积物粒度为例[J].中国科学:D辑, 2003, 33(6):563~568. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200306009.htm CHEN Jing-an, WAN Guo-jiang, ZHANG Feng, et al. Environmental records of lacustrine sediments in different time scales:Sediment grain size as an example[J]. Science in China:Series D, 2003, 33(6):536~568. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200306009.htm
[26]	王君波, 朱立平.藏南沉错沉积物的粒度特征及其古环境意义[J].地理科学进展, 2002, 21(5):459~467. doi: 10.11820/dlkxjz.2002.05.007 WANG Jun-bo, ZHU Li-ping. Grain-size characteristics and their paleo-environmental significance of ChenCo Lake Sediments in Southern Tibet[J]. Progress in Geography, 2002, 21(5):459~467. doi: 10.11820/dlkxjz.2002.05.007
[27]	孙千里, 周杰, 肖举乐.岱海沉积物粒度特征及其古环境意义[J].海洋地质与第四纪地质, 2001, 21(1):93~95. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200101018.htm SUN Qian-li, ZHOU Jie, XIAO Ju-le. Grain-size characteristics of lake Daihai sediments and its paleaoenvironment significance[J]. Marine Geology & Quaternary Geology, 2001, 21(1):93~95. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ200101018.htm
[28]	刘兴起, 王苏民, 沈吉.青海湖QH-2000钻孔沉积物粒度组成的古气候古环境意义[J].湖泊科学, 2003, 15(2):112~117. doi: 10.18307/2003.0203 LIU Xing-qi, WANG Su-min, SHEN Ji. The grain size of the core QH-2000 in Qinghai Lake and its implication for paleoclimate and paleoenvironment[J]. Journal of Lake Sciences, 2003, 15(2):112~117. doi: 10.18307/2003.0203
[29]	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):274~282. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200702015.htm LEI Guo-liang, ZHANG Hu-cai, ZHANG Wen-xiang, 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):274~282. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200702015.htm
[30]	陈碧珊, 潘安定, 张元芳.柴达木盆地尕海湖沉积物粒度特征及其古气候意义[J].海洋地质与第四纪地质, 2010, 30(2):111~119. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201002023.htm CHEN Bi-shan, PAN An-ding, ZHANG Yuan-fang. Grain-size characteristics and their environmental significance of Gahai lake sediments in Qaidam Basin[J]. Marine Geology & Quaternary Geology, 2010, 30(2):111~119. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201002023.htm
[31]	陈敬安, 万国江, 徐经意.洱海沉积物粒度记录与气候干湿变迁[J].沉积学报, 2000, 18(3):341~345. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200003002.htm CHEN Jing-an, WAN Guo-jiang, XU Jing-yi. Sediment particle sizes and the dry-humid transformation of the regional climate in Erhai Lake[J]. Acta Sedimentologica Sinica, 2000, 18(3):341~345. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200003002.htm
[32]	王永波, 刘兴起, 羊向东, 等.可可西里库塞湖揭示的青藏高原东北部近4000年来的干湿变化[J].湖泊科学, 2008, 20(5):605~612. doi: 10.18307/2008.0509 WANG Yong-bo, LIU Xing-qi, YANG Xiang-dong, et al. A 4000-year moisture evolution recorded by sediments of Lake Kusai in the Hoh Xil area, northern Tibetan Plateau[J]. Journal of Lake Sciences, 2008, 20(5):605~612. doi: 10.18307/2008.0509
[33]	朱立平, 王君波, 林晓, 等.西藏纳木错深水湖芯反映的8.4 ka以来气候环境变化[J].第四纪研究, 2007, 27(4):588~597. ZHU Li-ping, WANG Jun-bo, LIN Xiao, et al. Environmental changes reflected by core sediments since 8.4 ka in Namco, central Tibet of China[J]. Quarternary Sciences, 2007, 27(4):588~597.
[34]	吴健, 沈吉.兴凯湖沉积物粒度特征揭示的27.7 kaBP以来区域古气候演化[J].湖泊科学, 2010, 22(1):110~118. http://www.cnki.com.cn/Article/CJFDTOTAL-FLKX201001018.htm WU Jian, SHEN Ji. Paleoclimate evolution since 27.7 kaBP reflected by grain size variation of a sediment core from lake Xingkai, northeastern Asia[J]. Journal of Lake Sciences, 2010, 22(1):110~118. http://www.cnki.com.cn/Article/CJFDTOTAL-FLKX201001018.htm
[35]	明庆忠, 苏怀, 史正涛, 等.云南小中甸盆地湖相沉积记录的最近5次Heinrich事件[J].地理学报, 66(1):123~130. doi: 10.11821/xb201101012 MING Qing-zhong, SU Huai, SHI Zheng-tao, et al. Last five heinrich events revealed by lacustrine sediments from Xiaozhongdian Basin in Yunnan Province[J]. Acta Geographica Sinica, 66(1):123~130. doi: 10.11821/xb201101012
[36]	朱立平, 鞠建廷, 王君波, 等.湖芯沉积物揭示的末次冰消期开始时期普莫雍错湖区环境变化[J].第四纪研究, 2006, 26(5):772~780. ZHU Li-ping, JU Jian-ting, WANG Jun-bo, et al. Environmental changes recorded in core sediments from the Pumoyum Co Lake of the Tibetan Plateau during the initial stage of the last deglacial period[J]. Quaternary Sciences, 2006, 26(5):772~780.
[37]	蒋庆丰, 刘兴起, 沈吉.乌伦古湖沉积物粒度特征及其古气候环境意义[J].沉积学报, 2006, 24(6):877~882. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200606013.htm JIANG Qing-feng, LIU Xing-qi, SHEN Ji. Grain-size characteristics of Wulungu lake sediments and its palaeo climate and palaeoenvironment implication[J]. Acta Sedimentologica Sinica, 2006, 24(6):877~882. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200606013.htm
[38]	黄小忠, 陈发虎, 肖舜, 等.新疆博斯腾湖沉积物粒度的古环境意义初探[J].湖泊科学, 2008, 20(3):291~297. doi: 10.18307/2008.0305 HUANG Xiao-zhong, CHEN Fa-hu, XIAO shun, et al. Primary study on the environmental significances of grain-size changes of the Lake Bosten sediments[J]. Journal of Lake Sciences, 2008, 20(3):291~297. doi: 10.18307/2008.0305
[39]	王心源, 吴立, 张广胜, 等.安徽巢湖全新世湖泊沉积物磁化率与粒度组合的变化特征及其环境意义[J].地理科学, 2008, 28(4):548~553. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX200804015.htm WANG Xin-yuan, WU Li, ZHANG Guang-sheng, et al. Characteristics and environmental significance of magnetic susceptibility and grain size of lake sediments since Holocene in Chaohu Lake, Anhui Province[J]. Scientia Geographica Sinica, 2008, 28(4):548~553. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX200804015.htm
[40]	张振克, 吴瑞金, 王苏民.岱海湖泊沉积物频率磁化率对历史时期环境变化的反映[J].地理研究, 1998, 17(3):297~302. http://www.cnki.com.cn/Article/CJFDTOTAL-DLYJ803.010.htm ZHANG Zhen-ke, WU Rui-jin, WANG Su-min. Implication of magnetic frequency dependent susceptibility on environmental variation from lacustrine sediment in Daihai Lake[J]. Geographical Research, 1998, 17(3):297~302. http://www.cnki.com.cn/Article/CJFDTOTAL-DLYJ803.010.htm
[41]	舒强, 李才林, 赵志军, 等.苏北盆地浅钻沉积物磁化率与粒度记录的末次冰消期以来的环境变化[J].沉积学报, 2009, 27(1):111~117. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200901016.htm SHU Qiang, LICai-lin, ZHAO Zhi-jun, et al. The records of mass susceptibility and grain size for climate changes in Subei Basin during the Last Deglaciation[J]. Acta Sedimentologica Sinica, 2009, 27(1):111~117. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200901016.htm
[42]	殷勇, 方念乔, 王倩, 等.云南中甸纳帕海湖泊沉积物的磁化率及环境意义[J].地理科学, 2002, 22(4):413~419. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX200204005.htm YIN Yong, FANGNian-qiao, WANG Qian, et al. Magnetic susceptibility of lacustrine sediments and its environmental significance:Evidence from Napahai Lake, northwestern Yunnan, China[J]. Scientia Geographica Sinica, 2002, 22(4):413~419. http://www.cnki.com.cn/Article/CJFDTOTAL-DLKX200204005.htm
[43]	Xiao Xiayun, Shen Ji, Wang Sumin. Spatial variation of modern pollen from surface lake sediments in Yunnan and southwestern Sichuan Province, China[J]. Review of Palaeobotany and Palynology, 2011, 165(3-4):224~234. doi: 10.1016/j.revpalbo.2011.04.001
[44]	Kataoka H, Miyoshi N, Hase Y, et al. Pollen analysis of a sediment core (BDP96-1) from Lake Baikal[J]. Acta Palaeontologica Sinica, 41(4):534~538.
[45]	Norio FUJI. Palaeovegetation and palaeoclimate during the Quaternary period based on the long cores from lake Biwa, central Japan, and global correlation of the palaeoclimate records[J]. Acta Palaeontologica Sinica, 42(1):138~147.
[46]	于革.高分辨湖泊沉积和孢粉记录对气候、水文变化的响应[J].沉积学报, 2011, 29(1):118~124. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201101014.htm YU Ge.High-resolution records of lacustrine sedimentology and palynology responding to changes in climate and hydrology[J]. Acta Sedimentologica Sinica, 2011, 29(1):118~124. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201101014.htm
[47]	吕厚远, 刘嘉麒, 储国强, 等.末次冰期以来湛江湖光岩玛珥湖孢粉记录及古环境变化[J].古生物学报, 2003, 42(2):284~291. http://www.cnki.com.cn/Article/CJFDTOTAL-GSWX200302015.htm LÜHou-yuan, LIU Jia-qi, CHU Guo-qiang, et al. A study of pollen and environment in the Huguangyan Maar Lake since the Last Glaciation[J]. Acta Palaeontologica Sinica, 2003, 42(2):284~291. http://www.cnki.com.cn/Article/CJFDTOTAL-GSWX200302015.htm
[48]	羊向东, 王苏民, 童国榜, 等.云南鹤庆古湖晚更新世的孢粉记录及其古气候学意义[J].第四纪研究, 1998, (4):335~343. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199804005.htm YANG Xiang-dong, WANG Su-min, TONG Guo-bang, et al. The late pleistocene pollen record in the lake sediments from ancient Heqing lake and its significance for palaeoclimate[J]. Quarternary Sciences, 1998, (4):335~343. http://www.cnki.com.cn/Article/CJFDTOTAL-DSJJ199804005.htm
[49]	肖霞云, 沈吉, 肖海丰, 等.云南鹤庆盆地中更新世以来的孢粉记录及其植被与气候变化[J].湖泊科学, 2006, 18(4):369~376. doi: 10.18307/2006.0408 XIAO Xia-yun, SHEN Ji, XIAO Hai-feng, et al. Pollen records and vegetation and climate changes in Heqing Basin, Yunnan Province since middle Pleistocene[J]. Journal of Lake Sciences, 2006, 18(4):369~376. doi: 10.18307/2006.0408
[50]	许哲平, 陈建强, 肖景义.云南昆明盆地中更新世晚期以来的孢粉记录及古气候演化[J].地质学报, 2009, 83(1):65~77. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200901007.htm XU Zhe-ping, CHEN Jian-qiang, XIAO Jing-yi. Pollen records since late Middle Pleistocene in the Kunming Basin, Yunnan Province and paleoclimate evolution[J]. Acta Geologica Sinica, 2009, 83(1):65~77. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200901007.htm