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Sedimentology

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The South China Sea

Part of the book series: Developments in Paleoenvironmental Research ((DPER,volume 13))

The South China Sea (SCS) receives approximately 700 million tons of deposits annually in modern times, including about 80% of terrigenous matters provided by surrounding rivers and 20% of biogenic carbonate and silicates and volcanic ash. A similar scenario has been indentified also in the geological past. Since the early Oligocene, the sea has accumulated about 14.4 thousand trillion tons of deposits, which contain 63% terrigenous matters and 37% biogenic carbonate with negligible biogenic silicates and volcanic materials (Huang 2004). Most of these deposits accumulated on the SCS shelf (43% of total sediment mass) and slope (52%). Such a huge deposition cover makes the SCS an ideal place to study terrigenous input, paleoceanograhy, and regional and global climate evolution as well as sedimentary evolution of the SCS.

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Liu, Z. et al. (2009). Sedimentology. In: Wang, P., Li, Q. (eds) The South China Sea. Developments in Paleoenvironmental Research, vol 13. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-9745-4_4

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