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Where have all the sediments gone? The fate of sediments in the Taiwan Strait: A reassesment. Chih-Chieh Su, Man-Shan Chang, Horn-Ru Liao, Ho-Shing Yu Institute of Oceanography, NTU 20, Feb, 2008. Outline. Previous study Relict sediments? Short-term changes Chronology of sediment cores
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Where have all the sediments gone?The fate of sediments in the Taiwan Strait: A reassesment Chih-Chieh Su, Man-Shan Chang, Horn-Ru Liao, Ho-Shing Yu Institute of Oceanography, NTU 20, Feb, 2008
Outline • Previous study • Relict sediments? • Short-term changes • Chronology of sediment cores • Where have all the sediments gone? • What we know… • What we “don’t” know…
Kuanyin Depression Wuchu Depression Changyun Ridge Penghu Channel Taiwan Banks
Emery (1952; 1961) In general, any shelf sediment belongs to one or more of five main groups: • Authigenic (glauconite and phosphorite) • Organic (Foraminifera and shells) • Residual (weathered from underlying rocks) • Relict (remnant from a different earlier environment-such as a now-submerged beach or dune) • Detrital (presently supplied chiefly from adjacent river mouths, beaches, or sea cliffs)
Boggs ( 1975; 1979 ) • continued using Emery’s concept of relict sediments • mud belt along the coast of mainland China→modern sediments • sandy sediments in Taiwan Strait • in the nearshore area of Taiwan→Holocene to modern sand • central part of Taiwan Strait →relict sediments from mainland China • A large area of the Strait surrounding the Penghu Island was covered by palimpsest sediment formed by mixing of modern and relict sediment.
Chiu( 2000 ) Modern muddy sediment Relict sediment Palimpsest sediment Modern sandy sediment
Chang( 2002 ) Modern muddy sediment Relict sediment Palimpsest sediment Modern sandy sediment
Outline Previous study Relict sediments? Short-term changes Chronology of sediment cores Where have all the sediments gone? What we know… What we “don’t” know…
median sorting
Outline Previous study Relict sediments? Short-term changes Chronology of sediment cores Where have all the sediments gone? What we know… What we “don’t” know…
Location Map 790-1 790-2 790-3 790-4 790-7 790-5 790-6 (050705-07) (060406-09) (060721-24)
1.00 cm/a 0.12 cm/a 1.08 cm/a 0.18 cm/a 1.46 cm/a 0.18 cm/a 1.25 cm/a 0.21 cm/a 0.70 cm/a 1.06 cm/a 0.05 cm/a
OR542 BC9 (1999/3/9)
Outline Previous study Relict sediments? Short-term changes Chronology of sediment cores Where have all the sediments gone? What we know… What we “don’t” know…
What we know… • The sediments in the Taiwan Strait are not the so called “relict sediments”, they are the products of the action of modern tidal currents. • Taiwan is the major source of modern sediments in the Taiwan Strait.
What we don’t know… • Where did the “old” sediments in the Taiwan Strait (Chanyun Ridge) come from? • mainland China? • Taiwan? • Penghu Channel?
2008 Joint Hydrographic Survey • Grain Size Analysis • Clay Mineral Composition • Trace Element Distribution • Thermoluminescence Dating (TLD)