The evolution of river systems under the influence of climate change and human activities in the endorheic zones during the Holocene

被引：1

作者：

Gao, Mingjun ^{[1
]}

Li, Yu ^{[1
,2
,3
]}

Zhang, Zhansen ^{[1
]}

Duan, Junjie ^{[1
]}

Xue, Yaxin ^{[1
]}

Peng, Simin ^{[1
]}

Shang, Hao ^{[1
]}

Liu, Shiyu ^{[1
]}

机构：

[1] Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou, Peoples R China

[2] Minist Educ, Key Lab Western Chinas Environm Syst, Lanzhou, Peoples R China

[3] Minist Educ, Key Lab Western Chinas Environm Syst, 222 South Tianshui Rd, Lanzhou 730000, Gansu, Peoples R China

来源：

HOLOCENE | 2024年 / 34卷 / 07期

基金：

中国国家自然科学基金;

关键词：

accumulation; erosion; human-river relationship; lake sediment; the Hexi Corridor; the historical period; ARID CENTRAL-ASIA; LAKE TITICACA; HEXI CORRIDOR; ENVIRONMENTAL-CHANGES; NW CHINA; LOP NUR; MOISTURE EVOLUTION; MONGOLIAN PLATEAU; HIGH-RESOLUTION; DRAINAGE-BASIN;

D O I：

10.1177/09596836241236344

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

Endorheic river basins and their terminal lakes are highly sensitive to climate change and human activities. Based on chemical and pollen indicators, lake level, and erosion/accumulation rates of rivers, we explore the phasing of the evolution of the river system in the Hexi Corridor during the Holocene. The results suggest that climate change dominated the evolution of the river system during the early-Mid-Holocene. Entering the historical period, humans began to have an impact on runoff, water resources, and lake evolution, and since 1000 BP, anthropogenic perturbations recorded by regional proxies increased and humans dominated the migrations of river . In addition, we discuss the widespread erosion of rivers in the global endorheic zone and the impact of human activities in this context and found the timing of human influence on river evolution is not the same in different regions.

引用

页码：795 / 805

页数：11

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