Provenance discrimination of the clay sediment in the western Taiwan Strait and its implication for coastal current variability during the late-Holocene
Restricted accessResearch articleFirst published online January, 2017
Provenance discrimination of the clay sediment in the western Taiwan Strait and its implication for coastal current variability during the late-Holocene
This study aims to quantify the contribution of Yangtze clays to the sediment accumulation in the western Taiwan Strait and reconstruct the strength of Chinese Coastal Current (CCC) since middle-Holocene driven by East Asian Winter Monsoon (EAWM). Both down-core and surficial sediment samples were collected for grain size, radiocarbon, and clay mineral analyses. One 250-cm-long core was collected from the southern Yangtze distal mud wedge in western Taiwan Strait which receives Yangtze-derived clays transported by the Zhejiang-Fujian Coastal Current (ZFCC), the southern part of CCC. Clay minerals were examined in surficial sediment samples which were influenced by the Yangtze, Zhejiang-Fujian, western Taiwanese rivers, and the inner-shelf mud wedge. Ternary diagrams of smectite–kaolinite–chlorite revealed that three endmembers represented the Yangtze, Min, and western Taiwanese rivers, respectively. The estuaries seaward of the tidal current limits of Zhejiang-Fujian rivers, especially the Qiantang and Ou, were influenced by Yangtze-derived sediments through energetic tidal mixing. It was found that smectite can be used as a fingerprint of the Yangtze fine-grained sediment because among all the studied rivers, the Yangtze is the only one supplying smectite. Clay mineral results in core sediments revealed a dramatic provenance change at the depth of 113 cm, dated at ~4.0 cal. kyr BP. Smectite disappeared in the upper core, suggesting decreased contribution of Yangtze clays to the southern distal mud wedge. Decreased grain size of the fine population in the upper core also indicated that the ZFCC weakened during the late-Holocene. Such a decline also occurred in Subei Coast Current (northern part of CCC), revealed by the previous studies. The decline of CCC was related to the decreased EAWM of the late-Holocene, and it resulted in decreased sediment accumulation rate of the inner-shelf mud.
AnZPorterSC (1997) Millennial-scale climatic oscillations during the last interglaciation in central China. Geology25: 603–605.
2.
BeardsleyRCLimeburnerRYuH (1985) Discharging of the Changjiang (Yangtze River) into the East China Sea. Continental Shelf Research4: 57–76.
3.
BiLYangSLiC. (2015) Geochemistry of river-borne clays entering the East China Sea indicates two contrasting types of weathering and sediment transport processes. Geochemistry, Geophysics, Geosystems16: 3034–3052.
4.
BiscayePE (1965) Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans. Geological Society of America Bulletin76: 803–832.
5.
ChenJWangZHChenZY. (2009) Diagnostic heavy minerals in Plio-Pleistocene sediments of the Yangtze Coast, China with special reference to the Yangtze River connection into the sea. Geomorphology113: 129–136.
6.
DadsonSJHoviusNChenH. (2003) Links between erosion, runoff variability and seismicity in the Taiwan orogen. Nature426(6967): 648–651.
7.
DeMasterDJMcKeeBANittrouerCA. (1985) Rates of sediment accumulation and particle reworking based on radiochemical measurements from continental shelf deposits in the East China Sea. Continental Shelf Research4(1–2): 143–158.
8.
DiekmannBHofmannJHenrichR. (2008) Detrital sediment supply in the southern Okinawa Trough and its relation to sea-level and Kuroshio dynamics during the late Quaternary. Marine Geology255: 83–95.
9.
DouYGYangSYLiuZX. (2010) Clay mineral evolution in the central Okinawa Trough since 28 ka: Implications for sediment provenance and paleoenvironmental change. Palaeogeography, Palaeoclimatology, Palaeoecology288: 108–117.
10.
EberlDD (1984) Clay mineral formation and transformation in rocks and soils. Philosophical Transactions of the Royal Society of London: A311: 241–257.
11.
GeHZhangCLLiJ. (2014) Tetraether lipids from the southern Yellow Sea of China: Implications for the variability of East Asia Winter Monsoon in the Holocene. Organic Geochemistry70: 10–19.
12.
GibbsRJ (1977) Clay mineral segregation in the marine environment. Journal of Sedimentary Research47(1): 237–243.
13.
HoriKSaitoYWangP. (2002) Evolution of the coastal depositional systems of the Changjiang (Yangtze) River in response to Late Pleistocene–Holocene sea-level changes. Journal of Sedimentary Research72: 884–897.
14.
HorngCSHuhCA (2011) Magnetic properties as tracers for source-to-sink dispersal of sediments: A case study in the Taiwan Strait. Earth and Planetary Science Letters309: 141–152.
15.
HuBYangZZhaoM. (2012) Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China. Science China Earth Sciences55: 1656–1668.
16.
HuangETianJSteinkeS (2011) Millennial-scale dynamics of the winter cold tongue in the southern South China Sea over the past 26 ka and the East Asian winter monsoon. Quaternary Research75: 196–204.
17.
HuhCAChenWFHsuFH. (2011) Modern (<100 years) sedimentation in the Taiwan Strait: Rates and source-to-sink pathways elucidated from radionuclides and particle size distribution. Continental Shelf Research31: 47–63.
18.
JanSWangJChernCS. (2002) Seasonal variation of the circulation in the Taiwan Strait. Journal of Marine Systems35: 249–268.
19.
JiaGBaiYYangX. (2015) Biogeochemical evidence of Holocene East Asian summer and winter monsoon variability from a tropical maar lake in southern China. Quaternary Science Reviews111: 51–61.
20.
JianZWangPSaitoY. (2000) Holocene variability of the Kuroshio current in the Okinawa Trough, northwestern Pacific Ocean. Earth and Planetary Science Letters184: 305–319.
21.
KaoSLeeTMillimanJD (2005) Calculating highly fluctuated suspended sediment fluxes from mountainous rivers in Taiwan. Terrestrial Atmospheric and Oceanic Sciences16: 653–675.
22.
KatayamaHWatanabeY (2003) The Huanghe and Changjiang contribution to seasonal variability in terrigenous particulate load to the Okinawa Trough. Deep Sea Res II50: 475–485.
23.
LiCSShiXFGaoSJ. (2012) Clay minerals of the Taiwan rivers and their provenance implications. Chinese Science Bulletin57: 169–177 (in Chinese).
24.
LiJHuBWeiH. (2014) Provenance variations in the Holocene deposits from the southern Yellow Sea: Clay mineralogy evidence. Continental Shelf Research90: 41–51.
25.
LiuJSaitoYKongXH. (2010a) Sedimentary record of environmental evolution off the Yangtze River estuary East China Sea, during the last 13,000 years, with special reference to the influence of the Yellow River on the Yangtze River delta during the last 600 years. Quaternary Science Reviews29: 2424–2438.
26.
LiuJPLiACXuKH. (2006) Sedimentary features of the Yangtze River-derived along-shelf clinoform deposit in the East China Sea. Continental Shelf Research26: 2141–2156.
27.
LiuJPLiuCXuK. (2008) Flux and fate of small mountainous rivers derived sediments into the Taiwan Strait. Marine Geology256: 65–76.
28.
LiuJPXuKLiA. (2007) Flux and fate of Yangtze River sediment delivered to the East China Sea. Geomorphology85: 208–224.
29.
LiuSShiXFangX. (2014) Spatial and temporal distributions of clay minerals in mud deposits on the inner shelf of the East China Sea: Implications for paleoenvironmental changes in the Holocene. Quaternary International349: 270–279.
30.
LiuSFShiXFLiuYG. (2010b) East Asia winter monsoon records in the inner shelf mud of East China Sea since middle Holocene. Chinese Science Bulletin55: 1387–1396 (in Chinese).
31.
LiuZ (2010) Clay mineral assemblages in sediments of the South China Sea: East Asian monsoon evolution proxies?Acta Sedimentologica Sinica28: 1012–1019 (in Chinese with English abstract).
MaCZhouYChenJ. (2010) Clay minerals in the major Chinese coastal estuaries and their provenance implications. Frontiers of Earth Science in China4: 449–456.
34.
MillimanJDMeadeRH (1983) World-wide delivery of river sediment to the oceans. The Journal of Geology91: 1–21.
35.
MillimanJDSyvitskiJPM (1992) Geomorphic/tectonic control of sediment discharge to the ocean: The importance of small mountainous rivers. The Journal of Geology100: 525–544.
36.
MillimanJDShenHTYangZS. (1985) Transport and deposition of river sediment in the Changjiang estuary and adjacent continental shelf. Continental Shelf Research4: 37–45.
37.
QiaoSYangZLiuJ. (2011) Records of late-Holocene East Asian winter monsoon in the East China Sea: Key grain-size component of quartz versus bulk sediments. Quaternary International230: 106–114.
38.
QinYSZhengTM (1982) A study of distribution pattern of sediments on the continental shelf of the East China Sea. In: Institute of Oceanology, Academia Sinica (ed.) The Geology of the Yellow Sea and East China Sea. Beijing: Science Press, pp. 39–51.
39.
QinYSZhaoYYChenLR. (1987) Geology of the East China Sea. Beijing: Science Press (in Chinese).
40.
ReimerPJBardEBaylissA. (2013) IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon55(4): 1869–1887.
41.
SelvarajKChenCTA (2006) Moderate chemical weathering of subtropical Taiwan: Constraints from solid-phase geochemistry of sediments and sedimentary rocks. Journal of Geology114: 101–116.
42.
SingerAStoffersP (1980) Clay mineral diagenesis in two East African lake sediments. Clay Minerals15(3): 291–307.
43.
SongBLiZSaitoY. (2013) Initiation of the Changjiang (Yangtze) delta and its response to the mid-Holocene sea level change. Palaeogeography, Palaeoclimatology, Palaeoecology388: 81–97.
44.
SteinkeSGlatzCMohtadiM. (2011) Past dynamics of the East Asian monsoon: No inverse behaviour between the summer and winter monsoon during the Holocene. Global and Planetary Change78: 170–177.
45.
SuJL (2001) A review of circulation dynamics of the coastal oceans near china. Acta Oceanologica Sinica23: 1–16 (in Chinese with English abstract).
46.
SunYGaoSLiJ (2003) Primary analysis on the sensitive grain-size of terrigenous sediment to environments in marginal sea. Chinese Science Bulletin48: 83–87.
47.
UjiiéYUjiiéHTairaA. (2003) Spatial and temporal variability of surface water in the Kuroshio source region, Pacific Ocean, over the past 21,000 years: Evidence from planktonic foraminifera. Marine Micropaleontology49: 335–364.
48.
WangJGuoXXuS. (1981) Evolution of the Holocene Changjiang delta. Acta Geologica Sinica55: 67–81 (in Chinese with English abstract).
49.
WangKZhengHBPrinsM. (2008) High resolution paleoenvironmental record of the mud sediments of the East China Sea inner shelf. Marine Geology & Quaternary Geology28: 1–10 (in Chinese with English abstract).
50.
WangLLiJJLuHY. (2012) The East Asian winter monsoon over the last 15,000 years: Its links to high-latitudes and tropical climate systems and complex correlation to the summer monsoon. Quaternary Science Reviews32: 131–142.
51.
WangQYangS (2013) Clay mineralogy indicates the Holocene monsoon climate in the Changjiang (Yangtze River) Catchment, China. Applied Clay Science74: 28–36.
52.
WangZHXuHZhanQ. (2010) Lithological and palynological evidence of late Quaternary depositional environments in the subaqueous Yangtze delta, China. Quaternary Research73: 550–562.
53.
WhitehouseUGMcCarterRS (1958) Diagenetic modification of clay mineral types in artificial sea water. Proceedings of the Fifth National Conference on Clays and Clay Minerals566: 81–119.
54.
XiangRSunYLiT. (2007) Paleoenvironmental change in the middle Okinawa Trough since the last deglaciation: Evidence from the sedimentation rate and planktonic foraminiferal record. Palaeogeography, Palaeoclimatology, Palaeoecology243: 378–393.
55.
XiaoJPorterSAnZ. (1995) Grain-size of quartz as an indicator of winter monsoon strength on the Loess Plateau of central China during the last 130000 yr. Quaternary Research43: 22–29.
56.
XiaoS (2009) Comments on ‘High resolution paleoenvironmental record of the mud sediments of the East China Sea inner shelf’. Marine Geology & Quaternary Geology2009: 106–106 (in Chinese with English abstract).
57.
XiaoSLiAChenM. (2005) Recent 8 ka mud records of the East Asian Winter Monsoon from the inner shelf of the East China Sea. Earth Science: Journal of China University of Geosciences30: 573–581 (in Chinese with English abstract).
58.
XiaoSLiALiuJP. (2006) Coherence between solar activity and the East Asian winter monsoon variability in the past 8000 years from Yangtze River-derived mud in the East China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology237: 293–304.
59.
XuFJLiACXiaoSB. (2009a) Paleoenvironmental evolution in the inner shelf of the East China Sea since the last deglaciation. Acta Sedimentologyica Sinica27: 118–127 (in Chinese with English abstract).
60.
XuKHLiACLiuJP. (2012) Provenance, structure, and formation of the mud wedge along inner continental shelf of the East China Sea: A synthesis of the Yangtze dispersal system. Marine Geology291–294: 176–191.
61.
XuKHMillimanJDLiAC. (2009b) Yangtze- and Taiwan-derived sediments on the inner shelf of East China Sea. Continental Shelf Research29: 2240–2256.
62.
XuKHSangerDRiekerkG. (2014a) Seabed texture and composition changes offshore of Port Royal Sound, South Carolina before and after the dredging for beach nourishment. Estuarine, Coastal and Shelf Science149: 57–67.
63.
XuTWangGShiX. (2016) Sequence stratigraphy of the subaqueous Changjiang (Yangtze River) delta since the Last Glacial Maximum. Sedimentary Geology331: 132–147.
64.
XuZLiTChangF. (2014b) Clay-sized sediment provenance change in the northern Okinawa Trough since 22 kyr BP and its paleoenvironmental implication. Palaeogeography, Palaeoclimatology, Palaeoecology399: 236–245.
65.
YanchevaGNowaczykNRMingramJ. (2007) Influence of the intertropical convergence zone on the East Asian monsoon. Nature445: 74–77.
66.
YangSBelkinIBelkinaA. (2003) Delta response to decline in sediment supply from the Yangtze River: Evidence of the recent four decades and expectations for the next half-century. Estuarine, Coastal and Shelf Science57: 689–699.
67.
YangSMillimanJLiP. (2011a) 50,000 dams later: Erosion of the Yangtze River and its delta. Global and Planetary Change75: 14–20.
68.
YangSYLiCXYokoyamaK (2006) Elemental compositions and monazite age patterns of core sediments in the Changjiang delta: Implications for sediment provenance and development history of the Changjiang River. Earth and Planetary Science Letters245: 762–776.
69.
YangWZhouXXiangR. (2015) Reconstruction of winter monsoon strength by elemental ratio of sediments in the East China Sea. Journal of Asian Earth Sciences114: 467–475.
70.
YangZJiYBiN. (2011b) Sediment transport off the Huanghe (Yellow River) delta and in the adjacent Bohai Sea in winter and seasonal comparison. Estuarine, Coastal and Shelf Science93: 173–181.
71.
YonedaMUnoHShibataY. (2007) Radiocarbon marine reservoir ages in the western Pacific estimated by pre-bomb molluscan shells. Nuclear Instruments and Methods in Physics Research B259: 432–437.
72.
ZhaoQHJianZMZhangZX. (2009) Holocene benthic foraminifera and ostracoda from the shelf mud area of the East China Sea and their paleoenvironmental implications. Acta Micropalaeontologica Sinica26: 117–128 (in Chinese with English abstract).
73.
ZhengYKisselCZhengHB. (2010) Sedimentation on the inner shelf of the East China Sea: Magnetic properties, diagenesis and paleoclimate implications. Marine Geology268: 34–42.
74.
ZhouXJGaoSJiaJJ (2003) Preliminary evaluation of the stability of Changjiang clay minerals as fingerprints for material source tracing. Oceanologia ET Limnologia Sinica34(6): 683–692.
