Effect of increasing of water level during the middle of dry season on landscape pattern of the two largest freshwater lakes of China

被引:37
|
作者
Wu, Haipeng [1 ,2 ]
Hu, Xuyue [1 ,2 ]
Sun, Shiquan [1 ,2 ]
Dai, Juan [1 ,3 ]
Ye, Shujing [1 ,4 ]
Du, Chunyan [1 ,2 ]
Chen, Hong [1 ,2 ]
Yu, Guanlong [1 ,2 ]
Zhou, Lu [1 ,2 ]
Chen, Jing [1 ,2 ]
机构
[1] Changsha Univ Sci & Technol, Sch Hydraul Engn, Changsha 410114, Peoples R China
[2] Key Lab Dongting Lake Aquat Ecoenvironm Control &, Changsha 410114, Peoples R China
[3] Changjiang River Sci Res Inst, Wuhan 430072, Peoples R China
[4] Hunan Univ, Coll Environm Sci & Engn, Changsha 410082, Peoples R China
基金
中国国家自然科学基金;
关键词
Landscape; Dry season; Vegetation; Higher water level; Dongting Lake (DL); Poyang Lake (PL); BACTERIAL COMMUNITY STRUCTURE; SOIL MICROBIAL BIOMASS; LAND-USE CHANGE; 3 GORGES DAM; DRAMATIC INUNDATION CHANGES; POYANG LAKE; WETLAND CHANGES; CLIMATE-CHANGE; VEGETATION; BIODIVERSITY;
D O I
10.1016/j.ecolind.2020.106283
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
The hydrologic conditions of global wetlands are dramatically changed, and its ecological responses attract the great attention around the world. In recent decades, the water level of the middle of dry season had a tendency of significant increase in Dongting Lake and Poyang Lake (DL and PL, the two largest freshwater lake of China). Landscape pattern is sensitive to the local environmental changes and anthropogenic activity, and could influence the progresses and function of ecosystems. In this study, the landscape pattern between middle of dry season with increased water level (DIW) and that with normal water level (DNW) were compared to reveal the influence of the increasing of water level during the middle of dry season on landscape pattern of DL and PL. The results revealed that the increasing of water level during the middle of dry season caused expanding of deep water (cover increased from 14.40% to 18.36% of the total lake) to shallow water zone and expanding of shallow water (from 6.41% to 10.12%) to mudflat zone in DL; while it caused expanding of deep water (from 24.17% to 46.00%) to shallow water, sand, mudflat and grass zone and expanding of shallow water (from 12.18% to 19.51%) to sand, mudflat and grass zone in PL. In landscape metrics, it caused significant increase of the LPI in PL. In class metrics, it caused the some significant changes of landscape pattern indices (such as TA, LPI, MPS, AMPFDI, MNN and IJI) of the lakes. It had greater effects on the landscape pattern of PL than that of DL. And these changes of landscape pattern would affect birds, fish and mammals.
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页数:8
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