Holocene vegetation variations and the associated environmental changes in the western part of the Chinese Loess Plateau

被引:63
作者
Feng, Z. -D. [1 ]
Tang, L. Y.
Wang, H. B.
Ma, Y. Z.
Liu, K. -b.
机构
[1] Montclair State Univ, Dept Earth & Environm Studies, Montclair, NJ 07043 USA
[2] Lanzhou Univ, MOE Key Lab Western Chinas Environm Syst, Lanzhou 730000, Peoples R China
[3] Lanzhou Univ, Coll Resource & Environm Sci, Lanzhou 730000, Peoples R China
[4] Chinese Acad Sci, Nanjing Inst Geol & Paleontol, Nanjing 210008, Peoples R China
[5] Beijing Normal Univ, Coll Resource Sci & Technol, Beijing 100875, Peoples R China
[6] Louisiana State Univ, Dept Geog & Anthropol, Baton Rouge, LA 70803 USA
基金
中国国家自然科学基金; 美国国家科学基金会;
关键词
Holocene climate; Chinese Loess Plateau; vegetation history;
D O I
10.1016/j.palaeo.2006.04.009
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The western part of the Chinese Loess Plateau has experienced a series of environmental changes during the Holocene. A desert-steppe of late glacial was succeeded by a forest-steppe from 8850 to 7540 C-14 years BP, and a Pinus-dominated forest occupied the landscape from 7540 to 6560 C-14 years BP. A deciduous forest of high density and diversity existed from 6560 to 5790 C-14 years BP. Afterwards the vegetation changed to a Pinus-dominated forest-steppe (5790-4950 14C years BP) and then to an Ulmus-dominated forest-steppe (4950 to similar to 4000 C-14 years BP). The vegetation subsequently changed to a steppe from similar to 4000 to 3120 C-14 years BP and further to a desert-steppe from 3120 to 2900 C-14 years BP. After a period of vegetation improvement (steppe) from 2900 to 2460 C-14 years BP, a desert-steppe resumed (2460-2020 C-14 years BP). Steppe vegetation was re-established around 2020 C-14 years BP and seems to have then deteriorated again around 1000 C-14 years BP. The general trend of aforementioned climatic changes is proposed here to have been modulated by the insolation changes. Specifically, the insolation started to increase around 15,000 years BP and peaked around 9000 years BP when the obliquity-driven seasonality reached a maximum with the summer insolation being about 8% more than the present. As a result, tropical Holocene SST increased steadily from similar to 10,000 to similar to 6,000 years BP, thus effectively strengthening the East Asian summer monsoon. In addition, the documented high temperatures from 10,000 to 4000 years BP in high northern latitudes might have weakened the strength of the winter monsoon and thus enhanced the strength of the summer monsoon probably via lengthening of the rainy season, directly contributing to the "megahumid" climate between 10,000 and 4000 years BP in the western part of the Chinese Loess Plateau. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:440 / 456
页数:17
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