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Article

Grain Size and Pollen of Sediments in Wanghu Lake (Central China) Linked to Hydro-Environmental Changes

by 1,2, 1,*, 3 and 4
1
College of Earth Science and Engineering, Hohai Univ., Nanjing 210098, China
2
Key Laboratory of Hydrology and Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
3
Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
4
Editorial Department of Journal, Ningbo University, Ningbo 315211, China
*
Author to whom correspondence should be addressed.
Water 2020, 12(1), 45; https://doi.org/10.3390/w12010045
Received: 14 November 2019 / Revised: 16 December 2019 / Accepted: 18 December 2019 / Published: 20 December 2019
(This article belongs to the Section Hydrology)
Grain size of lake sediments is often measured in paleolimnological studies, especially investigations of past paleoclimatic and paleohydrologic changes. The implications of such measures, however, remain unclear, since watershed hydrology and the related transfer of materials to the lake are affected by local climate variables, hydrological shifts, and vegetation cover variables. Sediment from Wanghu Lake in the middle reaches of the Yangtze River have apparently been affected by land cover changes and lake-river system transitions caused by a sluice gate built at Fuchi in 1967. These changes influenced the watershed hydrology, thereby confounding paleoclimatic and paleohydrologic interpretations by proxy records in sediment cores. We collected sediment cores from the center of Wanghu Lake and analyzed trends in pollen and physical properties through sedimentary records to investigate land cover changes and hydrological transitions during the past 90 years. The grain size of the sediment core increased with precipitation and the significant relationships between pollen and grain size after 1967 indicated that sediment transfer to the lake was controlled by rainfall and land cover changes due to human-induced deforestation and farming in the lake catchment. Interestingly before 1967, there was no significant relationship between the pollen and grain size or between the precipitation and grain size, indicating that the sediment of WanghuLake was not simply from the lake catchment. The different relationships patterns before and after 1967 indicated that the sediments in the lake were not only transported following precipitation and discharge from the lake catchment but also came from the Yangtze River draining back into the lake during the flood seasons before 1967. These results highlight matters needing attention and the potential application of grain size of sediments for reconstructions of past hydro-environmental changes. View Full-Text
Keywords: pollen; grain size; hydrological transitions; sedimentation processes; sediment core; China pollen; grain size; hydrological transitions; sedimentation processes; sediment core; China
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MDPI and ACS Style

Shen, H.; Yu, Z.; Yu, G.; Shi, X. Grain Size and Pollen of Sediments in Wanghu Lake (Central China) Linked to Hydro-Environmental Changes. Water 2020, 12, 45. https://doi.org/10.3390/w12010045

AMA Style

Shen H, Yu Z, Yu G, Shi X. Grain Size and Pollen of Sediments in Wanghu Lake (Central China) Linked to Hydro-Environmental Changes. Water. 2020; 12(1):45. https://doi.org/10.3390/w12010045

Chicago/Turabian Style

Shen, Huadong, Zhongbo Yu, Ge Yu, and Xiaoli Shi. 2020. "Grain Size and Pollen of Sediments in Wanghu Lake (Central China) Linked to Hydro-Environmental Changes" Water 12, no. 1: 45. https://doi.org/10.3390/w12010045

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