PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

王瑜; 宋长青; 孙湘君

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

王瑜, 宋长青, 孙湘君

文章导航 > Chinese Geographical Science > 1999 > 9(1): 87-91

王瑜, 宋长青, 孙湘君. PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA[J]. 中国地理科学, 1999, 9(1): 87-91.

引用本文:

王瑜, 宋长青, 孙湘君. PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA[J]. 中国地理科学, 1999, 9(1): 87-91.

Wang Fengyu, Song Changqing, Sun Xiangjun. PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA[J]. Chinese Geographical Science, 1999, 9(1): 87-91.

Citation:

Wang Fengyu, Song Changqing, Sun Xiangjun. PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA[J]. Chinese Geographical Science, 1999, 9(1): 87-91.

PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

1.
The Research Institute of Forest Resources Information and Technique, the Chinese Academy of Forestry, Beijing 100091, P. R. China;
2.
Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, P. R. China

基金项目: the National Natural Science Foundation of China (No.39600114)

PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

1.
The Research Institute of Forest Resources Information and Technique, the Chinese Academy of Forestry, Beijing 100091, P. R. China;
2.
Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, P. R. China

摘要: In this paper, the Holocene paleoenvironment change sequence in middle Inner Mongolia was primarily reconstructed on the basis of palynological analysis at the resolution of 70 years on a peat profile, which was located in thenorthern part of Tumd Plain with its oldest age of 9100 a. B. P. As the consequence indicated, the Holocene climatechange in the middle Inner Mongolia had undergone cool→temperate→ warm→ temperate→ cool series, and the historycould be divided into 5 epochs: 9100-7400 a B. P., with slightly arid and cold climate;7400-5000 a B. P., transitoryclimate with dynamic fluctuation, earlier period temperate and slightly arid, and later period temperate and slightly humid; 5000 - 4100 a B. P., with warm and humid climate; 4100-1350 a B. P., with transitory climate getting arid, asthe result of human being's growing influence; 1350 a B. P.-present, with temperate and slightly arid climate, understrong influence of human being. The warm period of Holocene occurred in 7400-4000 a B. P., while the optimal periodoccurred in 5000-4100 a B. P.
- Inner Mongolia /
- paleoenvironment change /
- Holocene
Abstract: In this paper, the Holocene paleoenvironment change sequence in middle Inner Mongolia was primarily reconstructed on the basis of palynological analysis at the resolution of 70 years on a peat profile, which was located in thenorthern part of Tumd Plain with its oldest age of 9100 a. B. P. As the consequence indicated, the Holocene climatechange in the middle Inner Mongolia had undergone cool→temperate→ warm→ temperate→ cool series, and the historycould be divided into 5 epochs: 9100-7400 a B. P., with slightly arid and cold climate;7400-5000 a B. P., transitoryclimate with dynamic fluctuation, earlier period temperate and slightly arid, and later period temperate and slightly humid; 5000 - 4100 a B. P., with warm and humid climate; 4100-1350 a B. P., with transitory climate getting arid, asthe result of human being's growing influence; 1350 a B. P.-present, with temperate and slightly arid climate, understrong influence of human being. The warm period of Holocene occurred in 7400-4000 a B. P., while the optimal periodoccurred in 5000-4100 a B. P.
- Inner Mongolia /
- paleoenvironment change /
- Holocene

[1]	Bo HU, Qingke WEN, Fengjiang XI, Mengyao LI, Libing WANG, Yuejuan REN. Effects of Enclosure on Grassland Ecological and Economic Benefits in Northern China . Chinese Geographical Science, 2024, 34(1): 67-78. doi: 10.1007/s11769-023-1404-7
[2]	Xuelian GUO, Lusheng HE, Guoyong ZHAO, Weibin WANG, Huairen CAO, Hao WU. Spatial-temporal Characteristics of Holocene Paleosols in the Chinese Loess Plateau and Paleoclimatic Significance . Chinese Geographical Science, 2022, 32(6): 1110-1118. doi: 10.1007/s11769-022-1285-1
[3]	WANG Chunling, ZHAO Hongyan, WANG Guoping. Vegetation Development and Water Level Changes in Shenjiadian Peatland in Sanjiang Plain, Northeast China . Chinese Geographical Science, 2015, 25(4): 451-461. doi: 10.1007/s11769-015-0768-8
[4]	WANG Shaowu, GE Quansheng, WANG Fang, WEN Xinyu, HUANG Jianbin. Abrupt Climate Changes of Holocene . Chinese Geographical Science, 2013, 23(1): 1-12.
[5]	ZHU Likai, MENG Jijun, MAO Xiyan. Analyzing Land-use Change in Farming-pastoral Transitional Region Using Autologistic Model and Household Survey Approach . Chinese Geographical Science, 2013, 23(6): 716-728. doi: 10.1007/s11769-013-0642-5
[6]	JIANG Weiguo, ZHU Xiaohua, WU Jianjun, et al. Retrieval and Analysis of Coal Fire Temperature in Wuda Coalfield, Inner Mongolia, China . Chinese Geographical Science, 2011, 21(2): 159-166.
[7]	LU Yingxia, LI Baosheng, WEN Xiaohao, QIU Shifan, WANG Fengnian, NIU Dongfeng, LI Zhiwen. Millennial-centennial Scales Climate Changes of Holocene Indicated by Magnetic Susceptibility of High-resolution Section in Salawusu River Valley, China . Chinese Geographical Science, 2010, 20(3): 243-251. doi: 10.1007/s11769-010-0243-5
[8]	ZHENG Yinghua, WU Yongqiu, LI Sen, TAN Lihua, GOU Shiwei, ZHANG Hongyan. Grain-size Characteristics of Sediments Formed Since 8600 yr B.P. in Middle Reaches of Yarlung Zangbo River in Tibet and Their Paleoenvironmental Significance . Chinese Geographical Science, 2009, 19(2): 113-119. doi: 10.1007/s11769-009-0113-1
[9]	XUE Jibin, ZHONG Wei, ZHENG Yanming, MA Qiaohong, CAI Ying, OUYANG Jun. A New High-resolution Late Glacial-Holocene Climatic Record from Eastern Nanling Mountains in South China . Chinese Geographical Science, 2009, 19(3): 274-282. doi: 10.1007/s11769-009-0274-y
[10]	XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China . Chinese Geographical Science, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
[11]	LONG Hao, TAN Hongbin, WANG Naiang, TAN Liangcheng, LI Yu. Mid-Holocene Climate Variations Recorded by Palaeolake in Marginal Area of East Asian Monsoon: A Multi-proxy Study . Chinese Geographical Science, 2007, 17(4): 325-332. doi: 10.1007/s11769-007-0325-1
[12]	HAN Mei, LI Dao-gao, ZHAO Ming-hua, JIANG Ai-xia. A STUDY OF THE SURFACE EMERGING PALAEOCHANNELS ON THE SOUTH COAST PLAIN OF LAIZHOU BAY . Chinese Geographical Science, 2000, 10(3): 245-253.
[13]	王乃昂, 高顺尉. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS . Chinese Geographical Science, 1999, 9(4): 335-341.
[14]	钟巍, 熊黑钢. ISOTOPIC EVIDENCE FOR HOLOCENE CLIMATIC CHANGES IN BOSTEN LAKE, SOUTHERN XINJIANG, CHINA . Chinese Geographical Science, 1998, 8(2): 176-182.
[15]	张虎才. CLIMATIC CHANGE AND HUMAN ACTIVITIES OF NORTHEASTERN SAHARA IN HOLOCENE . Chinese Geographical Science, 1998, 8(4): 377-382.
[16]	吴敬禄, 王苏民, 吴艳宏. THE HOLOCENE SEDIMENTAL CHARACTERISTIC AND PALEOCLIMATIC EVOLUTION OF EBINUR LAKE, XINJIANG . Chinese Geographical Science, 1996, 6(1): 78-88.
[17]	钟巍, 王建民. PRELIMINARY STUDY ON THE HOLOCENE ENVIRONMENT CHANGES IN XINJIANG──GEOLOGIC RECORDS AND SEQUENCE . Chinese Geographical Science, 1996, 6(2): 166-176.
[18]	周子康, 夏越炯, 刘为纶, 吴维棠. RECONSTRUCTION OF PALEOVEGETATION AND PALEOCLIMATE OF HOLOCENE HYPSITHERMAL IN THE HEMUDU REGION . Chinese Geographical Science, 1995, 5(3): 232-241.
[19]	翁齐浩. THE RELATIONSHIP BETWEEN THE ENVIRONMENTAL CHANGE OF THE ZHUJIANG RIVER DELTA IN HOLOCENE AND ITS CULTURAL ORIGINS AND PROPAGATION . Chinese Geographical Science, 1994, 4(4): 303-309.
[20]	张仲英, 刘瑞华. THE HOLOCENE ALONG THE COAST OF HAINAN ISLAND, CHINA . Chinese Geographical Science, 1991, 1(2): 188-196.

点击查看大图

计量

文章访问数: 1129
HTML全文浏览量: 49
PDF下载量: 697
被引次数: 0

PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

1. The Research Institute of Forest Resources Information and Technique, the Chinese Academy of Forestry, Beijing 100091, P. R. China;

2. Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, P. R. China

基金项目: the National Natural Science Foundation of China (No.39600114)

收稿日期: 1998-05-11
刊出日期: 1999-03-20

关键词:

Inner Mongolia /

paleoenvironment change /

Holocene

摘要: In this paper, the Holocene paleoenvironment change sequence in middle Inner Mongolia was primarily reconstructed on the basis of palynological analysis at the resolution of 70 years on a peat profile, which was located in thenorthern part of Tumd Plain with its oldest age of 9100 a. B. P. As the consequence indicated, the Holocene climatechange in the middle Inner Mongolia had undergone cool→temperate→ warm→ temperate→ cool series, and the historycould be divided into 5 epochs: 9100-7400 a B. P., with slightly arid and cold climate;7400-5000 a B. P., transitoryclimate with dynamic fluctuation, earlier period temperate and slightly arid, and later period temperate and slightly humid; 5000 - 4100 a B. P., with warm and humid climate; 4100-1350 a B. P., with transitory climate getting arid, asthe result of human being's growing influence; 1350 a B. P.-present, with temperate and slightly arid climate, understrong influence of human being. The warm period of Holocene occurred in 7400-4000 a B. P., while the optimal periodoccurred in 5000-4100 a B. P.

English Abstract

王瑜, 宋长青, 孙湘君. PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA[J]. 中国地理科学, 1999, 9(1): 87-91.

引用本文:

王瑜, 宋长青, 孙湘君. PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA[J]. 中国地理科学, 1999, 9(1): 87-91.

Citation:

全文HTML

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

留言板

PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

计量

出版历程

PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

1. The Research Institute of Forest Resources Information and Technique, the Chinese Academy of Forestry, Beijing 100091, P. R. China; 2. Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, P. R. China

English Abstract

PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA

1. The Research Institute of Forest Resources Information and Technique, the Chinese Academy of Forestry, Beijing 100091, P. R. China; 2. Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, P. R. China

全文HTML

目录

1. The Research Institute of Forest Resources Information and Technique, the Chinese Academy of Forestry, Beijing 100091, P. R. China;

2. Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, P. R. China

1. The Research Institute of Forest Resources Information and Technique, the Chinese Academy of Forestry, Beijing 100091, P. R. China;

2. Institute of Botany, the Chinese Academy of Sciences, Beijing 100093, P. R. China