Download - Where have all the sediments gone? The fate of sediments in the Taiwan Strait: A reassesment
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Where have all the
sediments gone?The fate of sediments in the
Taiwan Strait: A reassesment
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
Chih-Chieh Su, Man-Shan Chang, Horn-Ru Liao, Ho-
Shing Yu Institute of Oceanography, NTU
20, Feb, 2008
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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…
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Changyun Ridge
Wuchu Depression
Kuanyin Depression
Taiwan Banks
Penghu Channel
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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)
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Emery ( 1968 )
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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.
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Boggs et al. ( 1979 )
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Chiu ( 2000 )
Modern muddy sediment
Relict sediment
Palimpsest sediment
Modern sandy sediment
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Chang ( 2002 )
Modern muddy sediment
Relict sediment
Palimpsest sediment
Modern sandy sediment
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Liu et al., 1998
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Liao ( 2005 ); Liao et al. (2008)
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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…
![Page 13: Where have all the sediments gone? The fate of sediments in the Taiwan Strait: A reassesment](https://reader035.vdocuments.net/reader035/viewer/2022062409/56814cd8550346895db9dd5e/html5/thumbnails/13.jpg)
Location map of the surface sediment
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median sorting
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Milliman et al., 2007
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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…
![Page 17: Where have all the sediments gone? The fate of sediments in the Taiwan Strait: A reassesment](https://reader035.vdocuments.net/reader035/viewer/2022062409/56814cd8550346895db9dd5e/html5/thumbnails/17.jpg)
Location Map
(060721-24)(060406-09)(050705-07)
790-1
790-2
790-3
790-4
790-5
790-6
790-7
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1.00 cm/a0.12 cm/a
1.46 cm/a0.18 cm/a
1.06 cm/a
1.25 cm/a0.21 cm/a
1.08 cm/a0.18 cm/a
0.05 cm/a
0.70 cm/a
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OR542 BC9(1999/3/9)
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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…
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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.
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-1 0 1 2 3 4 5 6 7 8 9 10Partic le d iam eter (Ph i)
0123456789
1011
Vo
lum
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%)
O R II-1294
Liao, 2005
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0 1 2 3 4 5 6 7 8 9 10Partic le d iam eter (Phi)
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%)
OR790-BC2
0 1 2 3 4 5 6 7 8 9 10Partic le d iam eter (Phi)
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OR790-BC5
0 1 2 3 4 5 6 7 8 9 10Partic le d iam eter (Phi)
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0 1 2 3 4 5 6 7 8 9 10Partic le d iam eter (Phi)
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OR790-BC7
0 1 2 3 4 5 6 7 8 9 10Partic le d iam eter (Phi)
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OR790-BC1
0 1 2 3 4 5 6 7 8 9 10Partic le d iam eter (Phi)
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OR790-BC4
0 1 2 3 4 5 6 7 8 9 10Partic le d iam eter (Phi)
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OR790-BC3
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What we don’t know…
• Where did the “old” sediments in the Taiwan Strait (Chanyun Ridge) come from?– mainland China?– Taiwan?– Penghu Channel?
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2008 Joint Hydrographic Survey
• Grain Size Analysis• Clay Mineral
Composition• Trace Element
Distribution• Thermoluminesce
nce Dating (TLD)
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It’s not complicated, but “VERY” dynamic!