Evolution of integrated lake status since the last deglaciation: A high-resolution sedimentary record from Lake Gonghai, Shanxi, China

被引:16
|
作者
Chen, Shengqian [1 ]
Liu, Jianbao [1 ]
Xie, Chengling [1 ]
Chen, Jianhui [1 ]
Wang, Haipeng [1 ]
Wang, Zongli [1 ]
Rao, Zhiguo [1 ]
Xu, Qinghai [2 ]
Chen, Fahu [1 ]
机构
[1] Lanzhou Univ, Key Lab West Chinas Environm Syst, Minist Educ, 222 South Tianshui Rd, Lanzhou 730000, Gansu, Peoples R China
[2] Hebei Normal Univ, Inst Nihewan Archaeol Res, Coll Resources & Environm, Shijiazhuang 050024, Hebei, Peoples R China
基金
中国国家自然科学基金;
关键词
Alpine lake; Climate change; East Asian summer monsoon; Local humidity; NORTH CHINA; LOESS PLATEAU; ALPINE LAKE; HOLOCENE; CLIMATE; PRECIPITATION; CATCHMENT; CARBON; AGE;
D O I
10.1016/j.palaeo.2018.01.035
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Alpine lakes not only provide internationally important habitats for endangered species, they also play a crucial role in the regional water balance. Unfortunately, a rapid loss of alpine lakes in China has occurred in recent decades; however, intensive human activities, together with regional differences in the responses of lakes to climate change, has impeded our understanding of the contribution of climate change to the loss of these lakes. To better understand how alpine lakes will evolve with continuing global warming, we used the analysis of new sedimentary proxies from Lake Gonghai, an undisturbed alpine lake, together with a review of published records, to reconstruct variations in integrated lake status since the last deglaciation. From 14,660-11,890 cal. yr BP the lake was in the most unstable state, indicated by the highest amplitude fluctuations in lake level and the within lake environment. The lake status experienced clear millennial-scale changes. During the early and middle Holocene (11,890-3200 cal. yr BP), the most stable lake status occurred, consistent with the highest precipitation levels. Owing to the highest level of freshwater influx in the middle Holocene (8-5 ka), the lake water was the deepest and most acidic. At this time, the dense vegetation cover resulted in maximum catchment stability and the lowest level of soil erosion, and hence the lowest sediment accumulation rate. From 3200 cal. yr BP, decreasing mean annual precipitation resulted in a moderately stable lake status, a shallow water depth and more alkaline lake water. The sparse vegetation cover caused a dramatic increase in the erosion rate and hence in the sediment accumulation rate. We infer that variations in local humidity were the major control on the integrated lake status during the last similar to 14,600 cal. yr BP. With the anticipated progression of global warming, the status of the alpine lakes in the region may continue to deteriorate and appropriate mitigation strategies are imperative.
引用
收藏
页码:175 / 182
页数:8
相关论文
共 50 条
  • [31] A Dam Construction Event Recorded by High-Resolution Sedimentary Grain Size in an Outflow-Controlled Lake (Hulun Lake, China)
    Gao, Hongbin
    Zhang, Rui
    Wang, Gang
    Fan, Yanru
    Zhu, Xinfeng
    Wu, Junfeng
    Wu, Li
    WATER, 2022, 14 (23)
  • [32] The Huguang maar lake - a high-resolution record of palaeoenvironmental and palaeoclimatic changes over the last 78,000 years from South China
    Mingram, J
    Schettler, G
    Nowaczyk, N
    Luo, XJ
    Lu, HY
    Liu, JQ
    Negendank, JFW
    QUATERNARY INTERNATIONAL, 2004, 122 : 85 - 107
  • [33] A high-resolution palaeoclimate record for the last 4800 years from lake la Brava, SE pampas plains, Argentina
    Irurzun, Maria A.
    Gogorza, Claudia S. G.
    Sinito, Ana M.
    Chaparro, Marcos A. E.
    Prieto, Aldo R.
    Laprida, Cecilia
    Lirio, Juan M.
    Navas, Ana M.
    Nunez, Hector
    GEOFISICA INTERNACIONAL, 2014, 53 (04): : 365 - 383
  • [34] A high resolution record of the last deglaciation in the southern Tyrrhenian Sea: environmental and climatic evolution
    Buccheri, G
    Capretto, G
    Di Donato, V
    Esposito, P
    Ferruzza, G
    Pescatore, T
    Ermolli, ER
    Senatore, MR
    Sprovieri, M
    Bertoldo, M
    Carella, D
    Madonia, G
    MARINE GEOLOGY, 2002, 186 (3-4) : 447 - 470
  • [35] The early Holocene optimum inferred from a high-resolution pollen record of Huguangyan Maar Lake in southern China
    Wang ShuYun
    Lue HouYuan
    Liu JiaQi
    Negendank, Joerg F. W.
    CHINESE SCIENCE BULLETIN, 2007, 52 (20): : 2829 - 2836
  • [36] The early Holocene optimum inferred from a high-resolution pollen record of Huguangyan Maar Lake in southern China
    Jrg F. W. NEGENDANK
    Chinese Science Bulletin, 2007, (20) : 2829 - 2836
  • [37] Sedimentary Evolution and Coastal Currents Variations of the Yangtze River Mouth(East China Sea) since Last Deglaciation
    Zhan Q.
    Wang Z.
    Zhao B.
    Wang H.
    Shi Y.
    He Z.
    Xie J.
    Diqiu Kexue - Zhongguo Dizhi Daxue Xuebao/Earth Science - Journal of China University of Geosciences, 2020, 45 (07): : 2697 - 2708
  • [38] High-resolution climate evolution derived from the sediment records of Erlongwan Maar Lake since 14 ka BP
    You HaiTao
    Liu JiaQi
    CHINESE SCIENCE BULLETIN, 2012, 57 (27): : 3610 - 3616
  • [39] High-resolution climate evolution derived from the sediment records of Erlongwan Maar Lake since 14 ka BP
    YOU HaiTao 1 & LIU JiaQi 2 1 Key Laboratory of Computational Geodynamics of Chinese Academy of Sciences
    College of Earth Science
    2 Institute of Geology and Geophysics
    Science Bulletin, 2012, (27) : 3610 - 3616
  • [40] High-resolution climate evolution derived from the sediment records of Erlongwan Maar Lake since 14 ka BP
    YOU HaiTao LIU JiaQi Key Laboratory of Computational Geodynamics of Chinese Academy of Sciences
    College of Earth ScienceGraduate University of the Chinese Academy of SciencesBeijing China Institute of Geology and GeophysicsChinese Academy of SciencesBeijing China
    Chinese Science Bulletin, 2012, 57 (27) : 3610 - 3616