Analysis on the Holocene sediment supply to the Shikoku Basin, northern Philippine Sea

Han Zhuochen; Gao Shu; Li Yanping

doi:10.3969/j.issn.0253-4193.2015.02.002

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Han Zhuochen, Gao Shu, Li Yanping. Analysis on the Holocene sediment supply to the Shikoku Basin, northern Philippine Sea[J]. Haiyang Xuebao, 2015, 37(2): 11-24. doi: 10.3969/j.issn.0253-4193.2015.02.002

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Han Zhuochen, Gao Shu, Li Yanping. Analysis on the Holocene sediment supply to the Shikoku Basin, northern Philippine Sea[J]. Haiyang Xuebao, 2015, 37(2): 11-24. doi: 10.3969/j.issn.0253-4193.2015.02.002

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Analysis on the Holocene sediment supply to the Shikoku Basin, northern Philippine Sea

doi: 10.3969/j.issn.0253-4193.2015.02.002

1.
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210023, China
2.
School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210023, China;Ministry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing 210023, China
3.
Ministry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing 210023, China

Received Date: 2014-04-02
Rev Recd Date: 2014-05-19

Abstract

Abstract

Grain size and Sr-Nd isotope analyses are carried out for the core C0011 samples, the northern Shikoku Basin, obtained from the IODP Expedition 333. The results are used for a comparative study with the isotope data obtained from adjacent areas. The Holocene sediment in the Shikoku Basin shows the characteristics of two-end member mixing processes, i.e., the terrestrial constituent and the volcanic source. In terms of the geographical location, the material supply to the Shikoku Basin mainly consists of volcanic materials from the Izu-Bonin Arc, the mixing-type sediment from the northwest Japanese islands, and terrestrial sediment transported by the prevailing westerly winds, monsoon or rivers from the Asian mainland. In general, the materials from the northwest Japanese islands represent the largest contribution. In comparison with the sediment from the central Shikoku Basin and the Japan Sea, the sedimentary materials from the northern Basin display a relatively large contribution by terrestrial sources. Based upon the negative correlation between ⁸⁷Sr/⁸⁶Sr and ε_Nd, together with the ⁸⁷Sr/⁸⁶Sr ratio and mean grain size, the relative contribution of terrestrial sources indicates a multi-periodic variation pattern as increase, decrease, increase, decrease, according to the chronological sequence.
- Holocene deposits,
- Sr-Nd isotope characteristics,
- grain size,
- sediment supply,
- Shikoku Basin

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