Abstract
This study applied end-member mixing analysis (EMMA) to clay minerals in Taiwan Strait sediments to determine the proportional contributions from known riverine sources, which are called end-members. Three end-members were thus determined: the rivers of Taiwan (TW), the rivers of Zhu and Min (ZM), and the rivers of Luzon (LZ). The EMMA model yielded strong and unbiased estimates of the clay mineral contents and end-member proportions. The TW end-member dominates the entire strait except for the western coastal area, the ZM end-member dominates the western coastal area, and the LZ end-member dominates the southern strait and the western coastal area. The spatial trends of end-member proportions are comparable with the directions of marine currents.
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Acknowledgments
We would like to thank the crew of the marine survey cruise of the western Taiwan Strait for their assistance with collecting samples. Special thanks are due to Weiguo Wang of the Third Institute of Oceanography, Ministry of Natural Resources, for his help in the clay mineral analysis.
Funding
This work was funded by the National Natural Science Foundation of China (41776112) and the Chinese Special Survey of Marine Geology (DD20190627, DD20191002, GZH201400208, GZH201400207).
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Tao Li, Guanqiang Cai, Kai Liang, Shengzhong Ma, and Weidong Luo designed the research; Tao Li analyzed the data and wrote the paper; Chaoweng Wang revised the paper.
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Li, T., Cai, G., Wang, C. et al. Quantifying clay mineral sources in marine sediments by using end-member mixing analysis. Geo-Mar Lett 41, 6 (2021). https://doi.org/10.1007/s00367-020-00674-4
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DOI: https://doi.org/10.1007/s00367-020-00674-4