Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene

Taoyu Xu; Xuefa Shi; Guoqing Wang; Shuqing Qiao; Gang Yang; Shengfa Liu; Xuchen Wang; Quanhong Zhao

doi:10.1007/s00343-013-2281-1

Your Location：

Home >

Browse articles >

Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene

OriginalPaper | Updated：2023-05-16

- Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene
- Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene
- 海洋湖沼学报（英文） 2013年31卷第5期页码：1107-1119
- Affiliations：
  
  1. Institute of Oceanology Chinese Academy of Sciences
  2. First Institute of Oceanography State Oceanic Administration and Key Laboratory of State Oceanic Administration for Marine Sedimentology and Environmental Geology
  3. China University of Geosciences,Wuhan
  4. University of Massachusetts
  5. Laboratory of Marine Geology Tongji University
- Author bio：
- Funds：
  
  Supported by the Marine Public Welfare Research Project (No. 200805063), the National Natural Science Foundation of China (Nos. 41076023 and 41106065), the Basic Fund Project of National Science and Technology Ministry (No. 2008FY220300), and the Coastal Investigation and Research Project of China (No. 908-02-02-05)
- DOI：10.1007/s00343-013-2281-1
  中图分类号：
- 网络首发：2013-09-07，
  
  纸质出版：2013
- Accepted：
Scan QR Code
Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene[J]. 海洋湖沼学报（英文）, 2013,31(5):1107-1119.

Xu, T., Shi, X., Wang, G. et al. Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene., Chin. J. Ocean. Limnol. 31, 1107–1119 (2013). https://doi.org/10.1007/s00343-013-2281-1
Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene[J]. 海洋湖沼学报（英文）, 2013,31(5):1107-1119. DOI： 10.1007/s00343-013-2281-1.

Xu, T., Shi, X., Wang, G. et al. Sedimentary facies of the subaqueous Changjiang River delta since the late Pleistocene., Chin. J. Ocean. Limnol. 31, 1107–1119 (2013). https://doi.org/10.1007/s00343-013-2281-1 DOI：

摘要

Abstract

The sedimentary facies of the subaqueous Changjiang (Yangtze) River delta since the late Pleistocene was studied based on lithology and foraminifera analysis for two boreholes

CJK07 and CJK11

along with 14C dating. Four sedimentary facies were identified

namely fluvial

tidal flat

offshore

and prodelta facies. The fluvial sedimentary facies is comprised of fluvial channel lag deposits

fluvial point bar deposits

and floodplain deposits

showing a fining-upward sequence in general with no benthic foraminifera. A layer of stiff clay overlies the fluvial deposits in core CJK07

indicating a long-term exposure environment during the Last Glacial Maximum (LGM). During the postglacial sea-level rise around 13-7.5 cal ka BP

the tidal flat facies was deposited in core CJK11

characterized by abundant silt-clay couplets. Euryhaline species dominate the subtidal flat foraminiferal assemblages

while almost no foraminifera was found in the intertidal flat. The offshore environment was the major sedimentary environment when the sea level reached its highest level around 7.5 cal ka BP

with a maximum accumulation rate of 10 mm/a found in core CJK11. Prodelta sediments have been deposited in core CJK11 since ∼3 cal ka BP

after the formation of the Changjiang River delta. The difference in sedimentary facies between core CJK07 and CJK11 is due to their location: core CJK07 was in an interfluve while core CJK11 was in an incised valley during the LGM. Furthermore

AMS 14 C dating of core CJK07 shows poor chronological order

indicating that the sediments were reworked by strong tidal currents and that sediment deposited since ∼7.7 cal ka BP in core CJK07 was eroded away by modern hydrodynamic forces caused by the southward shift of the Changjiang River delta depocenter.

关键词

Keywords

references

Chen Z Y, Saito Y, Hori K, Zhao Y W, Kitamura A. 2003. Early Holocene mud-ridge formation in the Yangtze offshore China: a tidal-controlled estuarine pattern and sea-level implications. Marine Geology, 198: 245–257.

Chen Z Y, Song B P, Wang Z H, Cai Y L. 2000. Late Quaternary evolution of the sub-aqueous Yangtze Delta, China: sedimentation, stratigraphy, palynology, and deformation. Marine Geology, 162: 423–441.

Chen Z Y, Stanley D J. 1993. Yangtze Delta, eastern China: Late Quaternary subsidence and deformation. Marine Geology, 112: 13–21.

Hori K, Saito Y, Zhao Q H, Cheng X R, Wang P X, Sato Y, Li C X. 2001a. Sedimentary facies and Holocene progradation rates of the Changjiang (Yangtze) delta, China. Geomorphology, 41: 233–248.

Hori K, Saito Y, Zhao Q H, Cheng X R, Wang P X, Sato Y, Li C X. 2001b. Sedimentary facies of the tide-dominated paleo-Changjiang (Yangtze) estuary during the last transgression. Marine Geology, 177: 331–351.

Hori K, Saito Y, Zhao Q H, Wang P X. 2002a. Control of incised-valley fill stacking patterns by accelerated and decelerated sea-level rise: the Changjiang example during the last deglaciation. Geo-Marine Letters, 22: 127–132.

Hori K, Saito Y, Zhao Q H, Wang P X. 2002b. Architecture and evolution of the tide-dominated Changjiang (Yangtze) River delta, China. Sedimentary Geology, 146: 249–264.

Hori K, Saito Y. 2007. An early Holocene sea-level jump and delta initiation. Geophysical Research Letters, 34: L18401, http://dx.doi.org/10.1029/2007GL031029.

Huang H Z, Shen B P, Hu Q S. 1985. Geological implication of geophysical data in Holocene Changjiang subaqueous delta. Marine Geology and Quaternary Geology, 5 (4): 81–94. (in Chinese with English abstract)

Huang H Z, Tang B G. 1996. Sedimentological Geology in the Yangtze River Delta Area. Geology Publishing Company, Beijing, China. 239p. (in Chinese)

Li C X, Wang P X. 1998. The Study on Stratigraphy in Changjiang River Estuary in the Late Quaternary. Science Press, Beijing, China. 197p. (in Chinese)

Li C X, Wang P, Sun H P, Zhang J Q, Fan D D, Deng B. 2002. Late Quaternary incised-valley fill of the Yangtze delta (China): its stratigraphic framework and evolution. Sedimentary Geology, 152: 133–158.

Li C X, Zhang G J. 1996a. Process on high resolution sequence stratigraphy in incised paleovalley. Advances in Earth Science, 11(2): 13–24. (in Chinese with English abstract)

Li C X, Zhang G J. 1996b. Sequence boundaries and depositional intermittent in the region of Yangtze River and Qiantang River Delta during the late Quaternary. Progress in Nature Science, 6 (4): 461–469. (in Chinese with English abstract)

Li C X, Zhang G J. 1996c. A primary study on high-resolution sequence stratigraphy of late quaternary in the Yangtze River Delta area. Marine Geology and Quaternary Geology, 16 (3): 13–24. (in Chinese with English abstract)

Li T G, Cao Q Y, Li A C, Qin Y S. 2003. Source to sink: Sedimentation in the continental margins. Advances in Earth Science, 18 (5): 713–721. (in Chinese with English abstract)

Liu J P, Xu K H, Li A C, Milliman J D, Velozzi D M, Xiao S B, Yang Z S. 2007. Flux and fate of Yangtze River sediment delivered to the East China Sea. Geomorphology, 85: 208–224.

Liu J, Saito Y, Kong X H, Wang H, Xiang L H, Wen C, Nakashima R. 2010. 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 Reviews, 29: 2 424–2 438.

McManus J. Grain size determination and interpretation. 1988. In: Tucker M E ed. Techniques in Sedimentology. Oxford: Blackwell Scientific Publications. p.63–85.

Qin J X, Yang Z S, Liang W, Zeng F G. 1998. High-resolution sequence stratigraphy of the Holocene strata on the East China Sea shelf. Sedimentary Facies and Palaeogeography, 18 (6): 11–26. (in Chinese with English abstract)

Saito Y, Yang Z S, Hori K. 2001. The Huanghe (Yellow River) and Changjiang (Yangtze River) deltas: a review on their characteristics, evolution and sediment discharge during the Holocene. Geomorphology, 41: 219–231.

Saito Y. 1998. Sea levels of the last glacial in the East China Sea continental shelf. The Quaternary Research, 37 (3): 235–242. (in Japanese with English abstract)

Wang G Q, Shi X F, Li C X. 2006. A review on Late Quaternary sedimentary geology of the Yangtze River Delta. Marine Geology and Quaternary Geology, 26 (6): 131–137. (in Chinese with English abstract)

Wang P X, Zhang J J, Min Q B. 1985. Distribution of foraminifera in surface sediments of the East China Sea. In: Wang P X ed. Marine Micropaleontology of China. China Ocean Press, Beijing, China. p.34–69.

Wang P X, Zhang J J, Zhao Q H. 1988. Foraminifera and Ostracods in Bottom Sediments of the East China Sea. China Ocean Press, Beijing, China. 438p. (in Chinese)

Wang Z H, Xu H, Zhan Q, Saito Y, He Z F, Xie J L, Li X, Dong Y H. 2010. Lithological and palynological evidence of late Quaternary depositional environments in the subaqueous Yangtze delta. China Quaternary Research, 73(3): 550–562.

Wang Z Y, Saito Y, Hori K, Kitamura A, Chen Z Y. 2005. Highly laminated sediments from the transition zone between subaqueous delta and the continental shelf. Estuarine, Coastal and Shelf Science, 62: 161–168.

Yuan Y R. 1986. Shallow seismic sequences in the sea area of Yangtze River delta. Acta Sedimentologica Sinica, 4 (4): 65–72. (in Chinese with English abstract)

Zhang J Q, Zhang G J, Li C X. 1998. Characteristics of the Late Quaternary stratigraphic sequence in the Changjiang River delta area. Journal of Tongji University (Natural Science), 26: 438–442. (in Chinese with English abstract)

浏览量

Downloads

CSCD

文章被引用时，请邮件提醒。

Submit

工具集

关联资源

The components of the saline lake in Xizang and an approach to their origin

大涵道比风扇/增压级进气畸变数值模拟研究

离子推力器放电室阳极壁面电流密度分布特性研究

基于模态频率的V型缺口梁裂纹扩展速率模型

压电阻抗法表征固体推进剂老化的研究