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The South China Sea - Paleoceanography and Sedimentology (Paperback, 2009 ed.)
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The South China Sea - Paleoceanography and Sedimentology (Paperback, 2009 ed.)
Series: Developments in Paleoenvironmental Research, 13
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Pinxian Wang and Qianyu Li The South China Sea (SCS) (Fig. 1. 1)
offers a special attraction for Earth scientists world-wide because
of its location and its well-preserved hemipelagic sediments. As
the largest one of the marginal seas separating Asia from the
Paci?c, the largest continent from the largest ocean, the SCS
functions as a focal point in land-sea int- actions of the Earth
system. Climatically, the SCS is located between the Western Paci?c
Warm Pool, the centre of global heating at the sea level, and the
Tibetan Plateau, the centre of heating at an altitude of 5,000m.
Geomorphologically, the SCS lies to the east of the highest peak on
earth, Zhumulangma or Everest in the Himalayas (8,848m elevation)
and to the west of the deepest trench in the ocean, Philippine
Trench (10,497m water depth) (Wang P. 2004). Biogeographically, the
SCS belongs to the so-called "East Indies Triangle" where modern
marine and terrestrial biodiversity reaches a global maximum
(Briggs 1999). Among the major marginal sea basins from the west
Paci?c, the SCS presents some of the best conditions for
accumulating complete paleoclimatic records in its hemipelagic
deposits. These records are favorable for high-resolution pa-
oceanographic studies because of high sedimentation rates and good
carbonate preservation. It may not be merely a coincidence that two
cores from the southern 14 SCS were among the ?rst several cores in
the world ocean used by AMS C dating for high-resolution
stratigraphy (Andree et al. 1986; Broecker et al. 1988).
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