Restricted accessResearch articleFirst published online 2021-7
Source-to-sink and evolutionary processes of the East China Sea inner-shelf mud belt and its response to environmental changes since the Holocene: New evidence from the distal mud belt
During the past decades, the elongated mud belt, 1000 km length, in the inner shelf of the East China Sea (ECS), has been extensively studied. Previous studies mainly focused on the northern part of the mud belt. There are still many arguments on various issues of the mud belt, including the provenance discrimination, the formation mechanism, and its evolution response to climate and environmental changes. In this paper, a borehole acquired from the distal southern mud belt which penetrated the Holocene strata with the collected data was analyzed. According to the parameters of (La/Sm)UCC versus (Gd/Yb)UCC and the ternary diagram of smectite-illite-(kaolinite + chlorite), sediments from the top section of Core ECS1601 originated from the Yangtze River since 13.7 ka. Sediments from upper and lower reaches of the Yangtze River can be clearly distinguished by (Gd/Yb)UCC value. The provenance of the distal mud belt shifted from upper reaches to lower valley since 5 ka and returned to the upper reaches again since 2.5 ka, which was related to the asynchronous evolution of Asian monsoon system and anthropogenic activities. The high sedimentation rates occurring in the distal mud belt between 5 and 2.5 ka were related to the decreased sediment supply of the upper reaches and the strengthened Zhejiang-Fujian Coastal Current (ZFCC) caused by the intensified East Asian Winter Monsoon (EAWM).
AnZPorterSCKutzbachJE, et al. (2000) Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews19(8): 762.
2.
BentleySJBlumMDMaloneyJ, et al. (2016) The Mississippi River source-to-sink system: Perspectives on tectonic, climatic, and anthropogenic influences, Miocene to Anthropocene. Earth-Science Reviews153(1): 139–174.
3.
BiLYangSLiC, et al. (2015) Geochemistry of river-borne clays entering the East China Sea indicates two contrasting types of weathering and sediment transport processes. Geochemistry Geophysics Geosystems16(9): 3034–3052.
4.
BiLYangSYZhaoY, et al. (2017) Provenance study of the Holocene sediments in the Changjiang (Yangtze River) estuary and inner shelf of the East China sea. Quaternary International441: 147–161.
5.
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.
6.
CalvoEGrimaltJJansenE (2002) High resolution U37K sea surface temperature reconstruction in the Norwegian Sea during the Holocene. Quaternary Science Reviews21(12–13): 1385–1394.
7.
ChenJLiuYWeiTY (2016) Provenance discrimination of the clay sediment in the western Taiwan strait and its implication for coastal current variability during the late-Holocene. The Holocene27: 110–121.
8.
ChenJYanJXieZ, et al. (2001) Nd and Sr isotopic compositions of igneous rocks from the lower Yangtze Region in Eastern China: Constraints on sources. Physics and Chemistry of the Earth Part A Solid Earth and Geodesy26(9–10): 719–731.
9.
ChenYSyvitskiJPMGaoS, et al. (2012) Socio-economic impacts on flooding: A 4000-year history of the Yellow River, China. Ambio41: 682–698.
10.
CongJYYuanZPHuG, et al. (2020) Sedimentary differentiation and hydrodynamic environment of multi-sourced sediment in the Changjiang distal delta. Acta Sedimentologica Sinica38(3): 528–553.
11.
DengBWuHYangSL, et al. (2017) Longshore suspended sediment transport and its implications for submarine erosion off the Yangtze River Estuary. Estuarine, Coastal and Shelf Science190: 1–10.
12.
DingYHKrishnamurtiTN (1987) Heat budget of Siberian high and the winter monsoon. Monthly Weather Review, 115: 2428–2449.
13.
DongJLiACLiuXT, et al. (2018) Sea-level oscillations in the east china sea and their implications for global seawater redistribution during 14.0–10.0 kyr BP. Palaeogeography, Palaeoclimatology, Palaeoecology511: 298–308.
14.
DouYGYangSYLiuZX, et al. (2010) Clay mineral evolution in the central Okinawa Trough since 28 ka: Implications for sediment provenance and paleoenvironmental change. Palaeogeography Palaeoclimatology Palaeoecology288(1): 108–117.
15.
DouYGYangSYLiuZX, et al. (2010) Provenance discrimination of siliciclastic sediments in the middle Okinawa Trough since 30 ka: Constraints from rare earth element compositions. Marine Geology275(1–4): 212–220.
16.
DuJLYangSLChenDC (2012) Preliminary study on the effect of three gorges reservoir on the evolution of landform of the Yangtze Estuary delta. Marine Science Bulletin31(5): 489–495.
17.
GaoJ HShiYShengH, et al. (2019) Rapid response of the Changjiang (Yangtze) River and East China Sea source-to-sink conveying system to human induced catchment perturbations. Marine Geology414: 1–17.
18.
GaoSCollinsMB (2014) Holocene sedimentary systems on continental shelves. Marine Geology352(3): 268–294.
19.
GaoSWangDYangY, et al. (2015) Holocene sedimentary systems on a broad continental shelf with abundant river input: Process-product relationships. Geological Society London Special Publications429: 223–259.
20.
GarzantiEAndoSFrance-LanordC, et al. (2010) Mineralogical and chemical variability of fluvial sediments 1. Bedload sand (Ganga-Brahmaputra, Bangladesh). Earth Planetary Science Letters299(3–4): 368–381.
21.
HanebuthTJJLantzschHNizouJ (2015) Mud depocenters on continental shelves—appearance, initiation times, and growth dynamics. Geo-Marine Letters35(6): 487–503.
22.
HarlavanYErelY (2002) The release of Pb and REE from granitoids by the dissolution of accessory phases. Geochimica et Cosmochimica Acta66: 837–848.
23.
HeMYZhengHBCliftPD, et al. (2015) Geochemistry of fine-grained sediments in the Yangtze River and the implications for provenance and chemical weathering in East Asia. Progress in Earth & Planetary Science2: 32.
24.
HongYTHongBLinQH, et al. (2009) Synchronous climate anomalies in the western North Pacific and North Atlantic regions during the last 14,000 years. Quaternary Science Reviews28(9–10): 840–849.
25.
HoriKSaitoYZhaoQ, et al. (2001) Sedimentary facies of the tidal-dominated paleo-Changjiang (Yangtze) estuary during the last transgression. Marine Geology177: 331–351.
26.
HoriKSaitoYZhaoQ, et al. (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(6): 884–897.
27.
HuDKCliftPDBningP, et al. (2013) Holocene evolution in weathering and erosion patterns in the Pearl River delta. Geochemistry Geophysics Geosystems14(7): 2349–2368.
28.
HuDX (1984) Upwelling and sedimentation dynamics: 1. The role of upwelling in sedimentation in the Huanghai Sea and East China Sea: A description of general features. Chinese Journal of Oceanologia and Limnologia2(1): 12–19.
29.
HuDXYangZS (2001) Margin Flux in the East China Sea. Beijing, China: Ocean Press.
30.
HuhCASuCC (1999) Sedimentation dynamics in the East China Sea elucidated from 210Pb, 137Cs and 239,240Pu. Marine Geology160: 183–196.
31.
LanXHZhangZXTianZX, et al. (2013) Content distributions and source analysis of rare earth elements in surface sediment off Changjiang River estuary. Journal of Applied Oceanography32(1): 13–19.
32.
LiCWangPSunH, et al. (2002) Late quaternary incised-valley fill of the Yangtze delta (China): Its stratigraphic framework and evolution. Sedimentary Geology152(1–2): 133–158.
33.
LiGLiPYongL, et al. (2014) Sedimentary system response to the global sea level change in the East China Seas since the last glacial maximum. Earth-Science Reviews139: 390–405.
34.
LiJYDodsonJYanH, et al. (2017) Quantitative Holocene climatic reconstructions for the lower Yangtze region of China. Climate Dynamics50(3–4): 1101–1113.
35.
LiXYJianZMShiXF, et al. (2012). Holocene foraminifera from the mud area of the inner shelf, East China Sea and their paleoenvironmental significance. Marine Geology & Quaternary Geology32(4): 61–71.
36.
LiYYangS (2010) A dynamical index for the east Asian winter monsoon. Journal of Climate23(15): 4255–4262.
37.
LiYQiaoLWangA, et al. (2013) Seasonal variation of water column structure and sediment transport in a mud depo-center off the Zhejiang-Fujian coast in China. Ocean Dynamics63(6): 679–690.
38.
LiYH (1976) Denudation of Taiwan Island Since Pliocene Epoch. Geology4(2): 105–108.
39.
LiuJSaitoYKongX, et al. (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(17–18): 2438.
40.
LiuJPLiACXuKH, et al. (2006) Sedimentary features of the Yangtze River-derived along-shelf clinoform deposit in the East China Sea. Continental Shelf Research26: 2141–2156.
41.
LiuJPLiuCSXuKH, et al. (2008) Flux and fate of small mountainous rivers derived sediments into the Taiwan Strait. Marine Geology256(1–4): 65076.
42.
LiuJPXuKHLiAC, et al. (2007) Flux and fate of Yangtze River sediment delivered to the East China Sea. Geomorphology85(3–4): 208–224.
43.
LiuJTHuhCAYouCF (2009) Fate of terrestrial substances in the Gaoping (Kaoping) shelf/slope and in the Gaoping Submarine Canyon off SW Taiwan. Journal of Marine System76(4): 367–368.
44.
LiuJTKaoSJHuhCA, et al. (2013) Gravity flows associated with flood events and carbon burial: Taiwan as instructional source area. Annual Review of Marine Science5: 47–68.
45.
LiuSFMiBBFangXS, et al. (2017). A preliminary study of a sediment core drilled from the mud area on the inner shelf of the East China Sea: Implications for paleoclimatic changes during the fast transgression period (13 ka B.P.–8 ka B.P.). Quaternary International441: 35–50.
46.
LiuSFShiXFFangXS, et al. (2014) Spatial and temporary 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.
47.
LiuSFShiXFLiuYG, et al. (2010b) Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene. Chinese Science Bulletin55(21): 2306–2314.
48.
LiuXTLiACDongJ, et al. (2018) Nonevaporative origin for gypsum in mud sediments from the East China Sea shelf. Marine Chemistry205: 90–97.
49.
LiuYDLiCAYuanSY (2011) Geochemistry of REE and provenance of sediments from 0-108 m Zhoulao borehole in Jianghan Plain. Geological Science and Technology Information30(1): 47–50.
50.
LiuZFZhaoYLColinC, et al. (2016) Source-to-sink transport processes of fluvial sediments in the South China Sea. Earth-Science Review153: 238–273.
51.
MaherBA (2008) Holocene variability of the East Asian summer monsoon from Chinese cave records: A re-assessment. The Holocene18(6): 861–866.
52.
MaoCPChenJYuanXY, et al. (2011) Seasonal variations in the Sr-Nd isotopic compositions of suspended particulate matter in the lower Changjiang River: Provenance and erosion constraints. Chinese Science Bulletin22: 2371–2378.
53.
MaoHGanZLanS (1963) Preliminary study on the Changjiang diluted water and its mixing natures. Oceanologia Et Limnologia Sinca5(3): 183–206.
54.
MiBBLiuSFShiXF, et al. (2017) A high resolution record of rare earth element compositional changes from the mud deposit on the inner shelf of the East China Sea: Implications for paleoenvironmental changes. Quaternary International447: 35–45.
55.
MillimanJDFarnsworthKL (2011) River Discharge to the Coastal Ocean: A Global Synthesis. Cambridge: Cambridge University Press.
56.
MillimanJDMeadeRH (1983) World-wide delivery of sediment to the oceans. Journal of Geology91(1): 1–21.
57.
MillimanJDSyvitskiJPM (1992) Geomorphic/tectonic control of sediment discharge to the ocean: The importance of small mountainous rivers. Journal of Geology100(5): 525–544.
58.
MillimanJDLinSWKaoSJ, et al. (2007) Shortterm changes in seafloor character due to flood-derived hyperpycnal discharge: Typhoon Mindulle, Taiwan, July 2004. Geology35: 779.
59.
MillimanJDQinYSRenME, et al. (1987) Man’s influence on the erosion and transport of sediment by Asian rivers: The Yellow River (Huanghe) example. The Journal of Geology95(6): 751–762.
60.
MillimanJDShenHTYangZS, et al. (1985) Transport and deposition of river sediment in the Changjiang estuary and adjacent continental shelf. Continental Shelf Research4(1–2): 37–45.
61.
MoyCMSeltzerGORodbellDT, et al. (2002) Variability of El Nino/southern Oscillation activity at millennial timescales during the Holocene epoch. Nature420(6912): 162–165.
62.
PanYQXuDRXuJP (1985) Frontal structure, change and reason of upwelling zone along the Zhejiang coast. Acta Oceanologica Sinica4: 401–411.
63.
PangCLiKHuD (2016). Net accumulation of suspended sediment and its seasonal variability dominated by shelf circulation in the Yellow and East China Seas. Marine Geology371: 33–43.
64.
QinYSZhaoYYChenSL, et al. (1987) Geology in the East China Sea. Beijing, China: Science Press.
65.
QuTDHuDX (1984) Upwelling and sedimentation dynamics II. A simple model. Chinese Journal of Oceanology & Limnology2(1): 12–19.
66.
SandeepKShankarRWarrierAK, et al. (2017) A multi-proxy lake sediment record of Indian summer monsoon variability during the Holocene in southern India. Palaeogeography, Palaeoclimatology, Palaeoecology476: 1–14.
67.
SuNYangSGuoY, et al. (2017) Revisit of rare earth element fractionation during chemical weathering and river sediment transport. Geochemistry Geophysics Geosystems18(3): 935–955.
68.
SuJL (2001) A review of circulation dynamics of the coastal oceans near china. Acta Oceanologica Sinica23(4): 1–16 (in Chinese with English abstract).
69.
SunSSMcDonoughWF (1989) Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes. In: SaudersADNorryMJ (eds.) Magmatism in the Ocean Basins. London: Geological Society London Special Publications, pp.313–345.
70.
TaylorSRMcLennanSM (1985) The Continental Crust: Its Composition and Evolution. Oxford: Blackwell, p.1e190.
71.
WanSMToucanneSCliftPD, et al. (2015) Human impact overwhelms long term climate control of weathering and erosion in southwest China. Geology43(5): 439–442.
72.
WangB (2006) The Asian Monsoon. Chichester: Praxis Publishing, p. 787.
73.
WangLM (2014) Paleoenvironmental Sedimentary Records Since the Holocene in the Central Mud Area of the South Yellow Sea and Its Response to the East Asian Monsoon. Beijing, China: Ocean University of China.
74.
WangPXZhangJJZhaoQH, et al. (1988) Foraminifera and Ostracoda in the Sediment of the East China Sea. Beijing, China: Ocean Press.
75.
WangQYangSY (2013) Clay mineralogy indicates the Holocene monsoon climate in the Changjiang (Yangtze River) catchment. China Applied Clay Science74(4): 28–36.
76.
WangYLiuXHerzschuhU (2010a) Asynchronous evolution of the Indian and East Asian Summer Monsoon indicated by Holocene moisture patterns in monsoonal central Asia. Earth Science Reviews103(3): 135–153.
77.
WangZLiMZhangR, et al. (2011) Impacts of human activity on the late-Holocene development of the subaqueous Yangtze delta, China, as shown by magnetic properties and sediment accumulation rates. The Holocene21(3): 393–407.
78.
WangZLiuJZhaoB (2008) Holocene depocenter shift in the middle-lower Changjiang River basins and coastal area in response to sea level change. Frontiers of Earth Science in China2(1): 17–26.
79.
WangZSaitoYZhanQ, et al. (2018) Three-dimensional evolution of the Yangtze River mouth, China during the Holocene: Impacts of sea level, climate and human activity. Earth-Science Reviews185: 938–955.
80.
WangZWeiGChenJ, et al. (2017) El Niño–Southern oscillation variability recorded in estuarine sediments of the Changjiang River, China. Quaternary International441: 18–28.
81.
WangZXuHZhanQ, et al. (2010b) Lithological and palynological evidence of late quaternary depositional environments in the subaqueous Yangtze delta, China. Quaternary Research73(3): 550–562.
82.
WeiWChangYPDaiZJ (2014) Streamflow changes of the Changjiang (Yangtze) River in the recent 60 years: impacts of the East Asian summer monsoon, ENSO, and human activities. Quaternary International336(12): 98–107.
83.
WuCKuoY (1999) Typhoons affecting Taiwan: Current understanding and future challenges. American Meteorological Society80: 67–80.
84.
WuHDengBYuanR, et al. (2013) Detiding measurement on transport of the Changjiang-derived buoyant coastal current. Journal of Physical Oceanography43: 2388–2399.
85.
WuJRenJLiuH, et al. (2015) Trapping and escaping processes of Yangtze River-derived sediments to the East China Sea. Geological Society, London, Special Publications429: 153–169.
86.
WuTNWuH (2018) Tidal mixing sustains a bottom-trapped river plume and buoyant coastal current on an energetic continental shelf. Journal of Geophysical Research: Oceans123: 8026–8051.
87.
XiaoSLiAChenM, et al. (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(5): 573–581.
88.
XiaoSLiALiuJ, et al. (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(2–4): 304.
89.
XuFJLiACLiTG, et al. (2010) Geochemical characteristics of sediments on the inner shelf of the East China Sea: Implications for paleoenvironment since the last deglaciation. Geochimica39(3): 240–250.
90.
XuFJLiACLiTG, et al. (2011) Rare earth element geochemistry in the inner shelf of the East China Sea and its implication to sediment provenances. Journal of Rare Earths29: 702–709.
91.
XuFJLiACXiaoSB, et al. (2009a) Paleoenvironmental evolution in the inner shelf of the East China Sea since the last deglaciation. Acta Sedimentologica Sinica27(1): 118–127.
92.
XuKHLiACLiuJP, et al. (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.
93.
XuKHMillimanJDLiAC, et al. (2009b) Yangtze- and Taiwan-derived sediments on the inner shelf of East China Sea. Continental Shelf Research29: 2240–2256.
94.
XuTWangGShiX, et al. (2016) Sequence stratigraphy of the subaqueous Changjiang (Yangtze river) delta since the last glacial maximum. Sedimentary Geology331: 132–147.
95.
YangSYWangZB (2011) Rare earth element compositions of the sediments from the major tributaries and the main stream of the Changjiang River. Bulletin of Mineralogy Petrology and Geochemistry30(1): 31–39.
96.
YangSYJungHSLiCX (2004) Two unique weathering regimes in the Changjiang and Huanghe drainage basins: Geochemical evidence from river sediments. Sedimentary Geology164(1): 19–34.
97.
YangSYJungHSChoiMS, et al. (2002) The rare earth element compositions of the Changjiang (Yangtze) and Huanghe (Yellow) river sediments. Earth and Planetary Science Letters201(2): 407–419.
98.
YangSYLiCWangZB, et al. (2013) Heterogeneity of geochemical compositions of the Changjiang river sediments and provenance indication. Quaternary Science33(4): 645–655.
99.
YangSYWangZBDouYG, et al. (2014) A review of sedimentation since the last glacial maximum on the continental shelf of eastern China. Geological Society London Memoirs41(1): 293–303.
100.
YangSYWeiGJXiaXP, et al. (2007) Provenance study of the late Cenozoic sediments in the Changjiang Delta: REE and Nd isotopic constraints. Quaternary Science27(3): 339–346.
101.
YankovskyAEChapmanDC (1997) A simple theory for the fate of buoyant coastal discharges. Journal of Physical Oceanography27(7): 1386–1401.
102.
YonedaMUnoHShibataY, et al. (2007) Radiocarbon marine reservior ages in the western pacific estimated by pre-bomb molluscan shells. Nuclear Instruments and Methods in Physics Research B259: 432–437.
103.
YuanZXiaoXWangF, et al. (2018) Spatiotemporal temperature variations in the East China Sea shelf during the Holocene in response to surface circulation evolution. Quaternary International482: 46–55.
104.
ZhangDX (2000) The effect of population activity on the changes in vegetation of Yangtze River Valley since the ancient period of Spring and Autumn-Warring States (770~221 B. C.). Journal of Plant Resources and Environment9(1): 47–53 (in Chinese with English abstract).
105.
ZhangXDalrympleRWYangSY, et al. (2015) Provenance of Holocene sediments in the outer part of the Paleo-Qiantang River estuary, China. Marine Geology366: 1–15.
106.
ZhaoQHJianZMZhangZX, et al. (2009) Holocene paleoenvironmental changes of the inner-shelf mud area of the East China Sea: Evidence from foraminifera faunas. Marine Geology & Quaternary Geology29(2): 75–82.
107.
ZhaoYZouXGaoJ, et al. (2018) Clay mineralogy and source-to-sink transport processes of Changjiang River sediments in the estuarine and inner shelf areas of the East China Sea. Journal of Asian Earth Sciences152: 91–102.
108.
ZhengXLiAWanS, et al. (2015) Formation of the modern current system in the East China Sea since the early Holocene and its relationship with sea level and the monsoon system. Chinese Journal of Marine Limnology33(4): 1062–1071.
109.
ZhengYKisselCZhengHB, et al. (2010a) Sedimentation on the inner shelf of the east china sea: Magnetic properties, diagenesis and paleoclimate implications. Marine Geology268(1–4): 34–42.
110.
ZhengYZhengHBWangK (2010b) History of sea level change since last glacial reflected by sedimentology of core from East China Sea Inner Shelf. Journal of Tongji University38(9): 1381–1386.
111.
ZhouXSunLGHuangW, et al. (2012) Precipitation in the yellow river drainage basin and East Asian monsoon strength on a decadal time scale. Quaternary Research78: 486–491.
112.
ZhuZFeinbergJMXieS, et al. (2017) Holocene ENSO-related cyclic storms recorded by magnetic minerals in speleothems of central China. Proceedings of the National Academy of Sciences of the United States of America114(5): 852–857.
113.
ZouLWeiGJ (2007) Distribution of major elements in sediment by sequential extraction procedures. Marine Geology Quaternary Geology27(2): 133–140.
