Quantitative reconstruction of Holocene sediment sources contributing to the central Jiangsu coast,China: New insights into source-to-sink processes |
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| Authors: | Yang Yang Jianjun Jia Liang Zhou Jianhua Gao Wenhua Gao Benwei Shi Zhanhai Li Ya Ping Wang Shu Gao |
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| Affiliation: | 1. State Key Laboratory for Estuarine and Coastal Research, East China Normal University, Shanghai, 200062 China;2. Ministry of Education, Key Laboratory for Coast and Island Development, Nanjing University, Nanjing, 210093 China;3. Department of Environmental Science, Henan University, Kaifeng, 475001 China |
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| Abstract: | Coastal deltaic deposits are the primary locations for sediment storage on Earth, and quantifying their source contributions is a critical prerequisite for delineating S2S patterns in marginal seas. In most cases, quantification for the contribution by fine-grained sediments (i.e. particle size < 63 μm) is considered to be representative to constrain the overall sediment supply. However, this approach may be inappropriate because large differences exist between the two quantities. Here we propose an approach to solve the problem, which is based on the maximum number of tracers from multiple sediment size fractions incorporating the content of all size fractions of sediment. Using this approach, absolute source contributions during the Holocene are reconstructed that provide a first-order model for the S2S pattern of the central Jiangsu coast, China. The Huanghe River is the strongest driver for the Holocene sedimentation, with a mean contribution of ~72 ± 6% (1417 × 108 t). The absolute contributions from the Changjiang and offshore areas were of secondary importance, (i.e. ~17 ± 1% (330 × 108 t) and ~11 ± 5% (217 × 108 t), respectively). The results show that a large difference between the relative and absolute source contributions and the assumption that the relative contribution represents the absolute contribution is invalid in a coastal setting. The impact of the Huanghe is mainly based on episodic events, such as the event of 1128–1855 AD . The model also reveals that the offshore sediments are as important as the Changjiang sediments for the central Jiangsu coast during the Holocene. Thus, the model provides both the time series and overall quantities of sediment supply during the formation and evolution of the Holocene tidal flats on the Jiangsu coast. Our findings shed new light on quantitative analysis of sediment sources applicable to future S2S studies of marginal seas. © 2020 John Wiley & Sons, Ltd. |
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| Keywords: | sediment supply quantitative tracing mixing model source-to-sink processes Holocene Jiangsu coast |
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