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Research article

A sedimentary evolvement record and its response to anthropogenic-driven pressure in the shallow Honghu Lake over a century

ORCID Icon, , &
Pages 1-12 | Received 07 Jan 2024, Accepted 25 Jun 2024, Published online: 01 Jul 2024

Figures & data

Figure 1. The Map of Hong Lake and the sampling site.

Figure 1. The Map of Hong Lake and the sampling site.

Figure 2. Vertical profile distribution of 210Pbex in sediment cores HH-A and HH-B in Honghu Lake: (a) HH-A (b) HH-B.

Figure 2. Vertical profile distribution of 210Pbex in sediment cores HH-A and HH-B in Honghu Lake: (a) HH-A (b) HH-B.

Figure 3. (Grain size or content) change of each group in sediment cores HH-A and HH-B in Honghu Lake: (a) HH-A (b) HH-B.

Figure 3. (Grain size or content) change of each group in sediment cores HH-A and HH-B in Honghu Lake: (a) HH-A (b) HH-B.

Figure 4. Sedimentation rate changes in sediment cores HH-A and HH-B in Honghu Lake: (a) HH-A (b) HH-B.

Figure 4. Sedimentation rate changes in sediment cores HH-A and HH-B in Honghu Lake: (a) HH-A (b) HH-B.

Table 1. Comparison of sedimentation rate among typical lakes in the Yangtze River Basin.

Figure 5. Variation of TN, TP, TOC percentage and the value of C/N, N/P along with the HH-B depth.

Figure 5. Variation of TN, TP, TOC percentage and the value of C/N, N/P along with the HH-B depth.

Table 2. Correlation efficiency of HH-B sediments.

Data availability statement

Data will be made available on reasonable request.