Late Pleistocene and Holocene Stratigraphy and Paleo- environmental Evolution in the Western Taiwan Shoal

WANG Li-bo; LI Jun; CHEN Zheng-xing; ZHAO Jing-tao; BAI Feng-long; HU Bang-qi; DOU Yan-guang; ZHAI Bin

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2014 > 32(6): 1089-1099

WANG Li-bo, LI Jun, CHEN Zheng-xing, ZHAO Jing-tao, BAI Feng-long, HU Bang-qi, DOU Yan-guang, ZHAI Bin. Late Pleistocene and Holocene Stratigraphy and Paleo- environmental Evolution in the Western Taiwan Shoal[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1089-1099.

Citation:

WANG Li-bo, LI Jun, CHEN Zheng-xing, ZHAO Jing-tao, BAI Feng-long, HU Bang-qi, DOU Yan-guang, ZHAI Bin. Late Pleistocene and Holocene Stratigraphy and Paleo- environmental Evolution in the Western Taiwan Shoal[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1089-1099.

Late Pleistocene and Holocene Stratigraphy and Paleo- environmental Evolution in the Western Taiwan Shoal

WANG Li-bo^1,2,3,
LI Jun^{2,3
,},
CHEN Zheng-xing^2,3,
ZHAO Jing-tao^2,3,
BAI Feng-long^2,3,
HU Bang-qi^2,3,
DOU Yan-guang^2,3,
ZHAI Bin^2,3

1.
College of Marine Geosciences, Ocean University of China, Qingdao, Shandong 266100;
2.
Key Laboratory of Marine Hydrocarbon Resources and Environment Geology, Ministry of Land and Resources, Qingdao, Shandong 266071;
3.
Qingdao Institute of Marine Geology, Qingdao, Shandong 266071

Received Date: 2013-08-20
Rev Recd Date: 2014-04-04
Publish Date: 2014-12-10

Abstract

Sediment core and high-resolution subbottom profiles from the western Taiwan Shoal were analyzed to research stratigraphic sequence, paleo-environmental development of the Shoal. According to the analyses of sedimentary characteristics, grain-sizes and AMS ¹⁴C dating, three marine strata and two terrestrial strata were recovered in the core, which were confidently correlated with seismic units in the profiles. The bottom marine strata (DU6) were mainly composed of intertidal and subtidal deposits and were formed in the Marine Isotope Stage (MIS) 5.1; the middle marine strata (DU4) mainly consisted of littoral and intertidal deposits and were formed in the MIS 3; the top marine strata (DU2 and DU1) were transgressive sands and tidal sands in the last deglaciation, respectively. The two terrestrial strata (DU5 and DU3) were incised valley filling deposits, and were formed in the MIS 4 and MIS 2, respectively. Transgressive medium - coarse sands (DU2) constructed the base of sand waves. The main body of sand waves (DU1), which had been formed since the high sea-level stage in Holocene, mainly consisted of medium - coarse sands and gravelly medium - coarse sands, with stable grain-size and good sorting on the top. Grain-size frequency distribution curves of sand waves have a modal number of -1 to 3 Φ; probability cumulative curves are two-segment pattern generally, with leap composition more than 80% and suspension composition less than 20%.Correlative analysis shows that there is a positive correlative between mean grain-size and sorting coefficient of tidal sand deposits (DU1), indicating that the stronger tidal current scouring the coarser grain-size and the better sorting is the sandy deposits.
- Taiwan Shoal,
- tidal deposits,
- sedimentary environment,
- Late Pleistocene

References

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[20]	Cai A, Zhu X, Li Y,et al. Sedimentary environment in Taiwan Shoal [J]. Chinese Journal of Oceanology and Limnology, 1992, 10(4): 331-339
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Late Pleistocene and Holocene Stratigraphy and Paleo- environmental Evolution in the Western Taiwan Shoal

1. College of Marine Geosciences, Ocean University of China, Qingdao, Shandong 266100;

2. Key Laboratory of Marine Hydrocarbon Resources and Environment Geology, Ministry of Land and Resources, Qingdao, Shandong 266071;

3. Qingdao Institute of Marine Geology, Qingdao, Shandong 266071

Received Date: 2013-08-20

Rev Recd Date: 2014-04-04

Publish Date: 2014-12-10

Key words:

Abstract: Sediment core and high-resolution subbottom profiles from the western Taiwan Shoal were analyzed to research stratigraphic sequence, paleo-environmental development of the Shoal. According to the analyses of sedimentary characteristics, grain-sizes and AMS ¹⁴C dating, three marine strata and two terrestrial strata were recovered in the core, which were confidently correlated with seismic units in the profiles. The bottom marine strata (DU6) were mainly composed of intertidal and subtidal deposits and were formed in the Marine Isotope Stage (MIS) 5.1; the middle marine strata (DU4) mainly consisted of littoral and intertidal deposits and were formed in the MIS 3; the top marine strata (DU2 and DU1) were transgressive sands and tidal sands in the last deglaciation, respectively. The two terrestrial strata (DU5 and DU3) were incised valley filling deposits, and were formed in the MIS 4 and MIS 2, respectively. Transgressive medium - coarse sands (DU2) constructed the base of sand waves. The main body of sand waves (DU1), which had been formed since the high sea-level stage in Holocene, mainly consisted of medium - coarse sands and gravelly medium - coarse sands, with stable grain-size and good sorting on the top. Grain-size frequency distribution curves of sand waves have a modal number of -1 to 3 Φ; probability cumulative curves are two-segment pattern generally, with leap composition more than 80% and suspension composition less than 20%.Correlative analysis shows that there is a positive correlative between mean grain-size and sorting coefficient of tidal sand deposits (DU1), indicating that the stronger tidal current scouring the coarser grain-size and the better sorting is the sandy deposits.

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Reference (38)

[1]	秦蕴珊,赵一阳,赵松龄,等. 渤海地质[M]. 北京:科学出版社,1985:161-211 [Qin Yunshan, Zhao Yiyang, Zhao Songling, et al. Geology of the Baohai Sea [M]. Beijing: Science Press, 1985: 161-211]
[2]	Liu J, Saito Y, Wang H,et al. Stratigraphic development during the Late Pleistocene and Holocene offshore of the Yellow River delta, Bohai Sea [J]. Journal of Asian Earth Sciences, 2009, 36: 318-331
[3]	刘敏厚,吴世迎,王永吉,等. 黄海晚第四纪地质[M]. 北京:海洋出版社,1987:292-302 [Liu Minhou, Wu Shiying, Wang Yongji, et al. Late Quaternary Geology of the Yellow Sea [M]. Beijing: Ocean Press, 1987: 292-302]
[4]	秦蕴珊,赵一阳,陈丽蓉,等. 黄海地质[M]. 北京:海洋出版社,1989:39-180 [Qin Yunshan, Zhao Yiyang, Chen Lirong, et al. Geology of the Yellow Sea [M]. Beijing: Ocean Press, 1989: 39-180]
[5]	杨子赓. Olduvai亚期以来南黄海沉积层序及古地理变迁[J]. 地质学报,1993,67(4):357-366 [Yang Zigeng. The sedimentary sequence and palaeogeographic changes of the south Yellow Sea since the olduvai subchron [J]. Acta Geological Sinica, 1993, 67(4): 357-366]
[6]	葛淑兰,石学法,朱日祥,等. 南黄海EY02-2孔磁性地层及古环境意义[J]. 科学通报,2005,50(22):2531-2540 [Ge Shulan, Shi Xuefa, Zhu Rixiang, et al. Magnetostratigraphy of Borehole EY02-2 in the southern Yellow Sea and its paleoenvironmental significance [J]. Chinese Science Bulletin, 2005, 50(22): 2531-2540]
[7]	Liu J, Saito Y, Kong X,et al. Delta development and channel incision during marine isotope stages 3 and 2 in the western South Yellow Sea [J]. Marine Geology, 2010, 278(1): 54-76
[8]	Liu Z X, Berne S, Saito Y,et al. Quaternary seismic stratigraphy and paleoenvironments on the continental shelf of the East China Sea [J]. Journal of Asian Earth Sciences, 2000, 18(4): 441-452
[9]	葛淑兰,石学法,吴永华,等. 东海北部外陆架 EY02-1 孔磁性地层研究[J]. 海洋学报,2008,30(2):51-61 [Ge Shulan, Shi Xuefa, Wu Yonghua, et al. Magnetostratigraphy of Borehole EY02-1 in the northern outer continental shelf of the East China Sea [J]. Acta Oceanologica Sinica, 2008, 30(2): 51-61]
[10]	杨子赓,林和茂. 中国东部第四纪进程与国际对比[M]. 北京:地质出版社,1993:1-125 [Yang Zigeng, Lin Hemao. Quaternary Processes in East China and International Correlation [M]. Beijing: Geological Publishing House, 1993: 1-125]
[11]	Chen P P, Chen Z Y, Zhang Q M. Sequence stratigraphy and continental margin development of the northwestern shelf of the South China Sea [J]. AAPG Bulletin, 1993, 77(5): 842-862
[12]	Ludmann T, Kin W H, Wang P. Plio-Quaternary sedimentation processes and neotectonics of the northern continental margin of the South China Sea [J]. Marine Geology, 2001, 172(3/4): 331-358
[13]	葛黄敏,李前裕,钟广法,等. 南海北部第四纪高分辨率地震层序地层与古环境演化[J]. 海洋地质与第四纪地质,2012,32(4):49-60 [Ge Huangmin, Li Qianyu, Zhong Guangfa, et al. High resolution Quarternary seismic sequence stratigraphy and paleoenvironment evolution in the northern South China Sea [J]. Marine Geology and Quaternary Geology, 2012, 32(4): 49-60]
[14]	Liu J P, Liu C S, Xu K H,et al. Flux and fate of small mountainous rivers derived sediments into the Taiwan Strait [J]. Marine Geology, 2008, 256(1/2/3/4): 65-76
[15]	Liao H R, Yu H S, Su C C. Morphology and sedimentation of sand bodies in the tidal shelf sea of eastern Taiwan Strait [J]. Marine Geology, 2008, 248: 161-178
[16]	Huh C A, Chen W, Hsu F H,et al. Modern (<100 years) sedimentation in the Taiwan Strait: Rates and source-to-sink pathways elucidated from radionuclides and particle size distribution [J]. Continental Shelf Research, 2011, 31(1): 47-63
[17]	Liu Z, Xia D, Berne S,et al. Tidal deposition systems of China's continental shelf, with special reference to the eastern Bohai Sea [J]. Marine Geology, 1998, 145: 225-253
[18]	郑铁民,张君元. 台湾浅滩及其附近大陆架的地形和沉积特征的初步研究[M]//中国科学院海洋研究所. 黄东海地质. 北京:科学出版社,1982:52-66 [Zheng Tiemin, Zhang Junyuan. Preliminary Researches of Geomorphology and Sedimentary Characteristics in the Taiwan Shoal and Surrounding Shelf [M]//Institute of Oceanology, Chinese Academy of Sciences. Geology of the Yellow Sea and East China Sea. Beijing: Science Press, 1982: 52-66]
[19]	蓝东兆,张维林,陈承惠,等. 台湾浅滩中粗砂的时代与成因[J]. 台湾海峡,1991,10(2):156-161 [Lan Dongzhao, Zhang Weilin, Chen Chenghui, et al. Preliminary study on age and origin of medium-coarse sand in Taiwan Shoal [J]. Journal of Oceanography in Taiwan Strait, 1991, 10(2): 156-161]
[20]	Cai A, Zhu X, Li Y,et al. Sedimentary environment in Taiwan Shoal [J]. Chinese Journal of Oceanology and Limnology, 1992, 10(4): 331-339
[21]	廉耀康,李炎. 台湾浅滩沉积物粒度特征及输运趋势[J]. 台湾海峡,2011,30(1):122-127 [Lian Yaokang, Li Yan. Grain size characteristics and transport trend in the Taiwan Bank [J]. Journal of Oceanography in Taiwan Strait, 2011, 30(1): 122-127]
[22]	刘振夏,夏东兴. 中国近海潮流沉积沙体[M]. 北京:海洋出版社,2004:129-210 [Liu Zhenxia, Xia Dongxing. Tidal Sands in the China Seas [M]. Beijing: Ocean Press, 2004: 129-210]
[23]	陈承惠,蓝东兆,于永芬,等. 台湾海峡西部海域晚第四纪地层[J]. 第四纪研究,1990(4):301-307 [Chen Chenghui, Lan Dongzhao, Yu Yongfen, et al. Late Quarternary stratigraphy in the western Taiwan Strait [J]. Quaternary Sciences, 1990(4): 301-307]
[24]	蓝东兆,张维林,陈承惠,等. 晚更新世以来台湾海峡西部的海侵及海平面变化[J]. 海洋学报,1993,15(4):77-84 [Lan Dongzhao, Zhang Weilin, Chen Chenghui, et al. Transgression and sea-level change in western Taiwan Strait since the Late Pleiocene [J]. Acta Oceanologica Sinica, 1993, 15(4): 77-84]
[25]	伍伯瑜. 台湾海峡及其邻近水域的流型和水文特征[J]. 海洋通报,1983,2(4):1-8 [Wu Boyu. The current pattern and hydrologic character in the Taiwan Straits and its adjacent waters [J]. Marine Science Bulletin, 1983, 2(4): 1-8]
[26]	李立,郭小钢,吴日升. 台湾海峡南部的海洋锋[J]. 台湾海峡,2000,19(2):147-156 [Li Li, Guo Xiaogang, Wu Risheng. Oceanic fronts in southern Taiwan Strait [J]. Journal of Oceanography in Taiwan Strait, 2000, 19(2): 147-156]
[27]	Jan S, Chern C S, Wang J,et al. The anomalous amplification of M2 tide in the Taiwan Strait [J]. Geophysical Research Letters, 2004, 31: L07308
[28]	Wang Y H, Jan S, Wang D P. Transports and tidal current estimates in the Taiwan Strait from shipboard ADCP observations (1999-2001) [J]. Estuarine, Coastal and Shelf Science, 2003, 57: 193-199
[29]	杜晓琴,李炎,高抒. 台湾浅滩大型沙波、潮流结构和推移质输运特征[J]. 海洋学报,2008,30(5):124-136 [Du Xiaoqin, Li Yan, Gao Shu. Characteristics of the large scale sandwaves, tidal flow structure and bedload transport over the Taiwan Bank in southern China [J]. Acta Oceanologica Sinica, 2008, 30(5): 124-136]
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Late Pleistocene and Holocene Stratigraphy and Paleo- environmental Evolution in the Western Taiwan Shoal

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