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The South China Sea: Paleoceanography and Sedimentology [Paperback]

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  • Category: Books (Science)
  • ISBN-10:  9400796595
  • ISBN-10:  9400796595
  • ISBN-13:  9789400796591
  • ISBN-13:  9789400796591
  • Publisher:  Springer
  • Publisher:  Springer
  • Binding:  Paperback
  • Binding:  Paperback
  • Pub Date:  01-Feb-2014
  • Pub Date:  01-Feb-2014
  • SKU:  9400796595-11-SPRI
  • SKU:  9400796595-11-SPRI
  • Pages:  506
  • Pages:  506
  • Item ID: 100997113
  • List Price: $169.99
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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).Oceanographical and Geological Background.- Stratigraphy and Sea Level Changes.- Sedimentology.- Upper Water Structure and Paleo-Monsoon5.- Deep Waters and Oceanic Connection.- Biogeochemistry and the Carbon Reservoir.- History of the South China Sea  A Synthesis.

Pinxian Wang was born in Shanghai in 1936. He graduated from the Moscow State University in 1960, majoring in paleontology, and was Alexander von Humboldt Fellow in 1981-82 in Kiel, Germlsï

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