Abstract
The analysis of the sediment 14C dating, grain sizes, sporopollen and micropaleontology in the BZK01 borehole in the Yangtze River Delta Plain was carried out. The sporopollen assemblages, the sedimentary environment evolution, the sedimentary facies and the paleoclimate characteristics revealed by the borehole since the Pliocene were discussed in combination with the gamma logging and the lithologic stratigraphy, and the quaternary multiple stratigraphic division of the borehole was established. The results show that the study area has undergone many environmental changes since Pliocene due to the influence of the primitive topography, the sea level changes, the land-sea changes, the paleoclimate changes and the Neotectonic movement. From bottom to top, the drilling holes reveal that the lithology and the strata are bedrock Changhe Formation, the Neogene-Quaternary sedimentary Jiaxing Formation, the Qiangang Formation, the Dongpu Formation, the Ningbo Formation and the Zhenhai Formation in turn. The sporopollen assemblage can be divided into 16 sporopollen belts. According to the periodic variation of the paleoclimate cycle during the warm, the humid and the cold and the dry periods, BZK01 drilling reflects that in the total area there are seven paleoclimatic cycles. The multi-stratigraphic division and correlation of the boreholes revealed that 151.9–278.0 m is the Pliocene-Early Pleistocene period of the alternating fluvial and lacustrine deposits, and there are two climatic cycles; 83.5–151.9 m is the Middle Pleistocene of the fluvial-lacustrine-shallow lacustrine depositional environment, which includes two climatic cycles. 15.4–83.5 m is the Late Pleistocene and sinks. From bottom to top, the sedimentary environment is the estuarine-fluvial-tidal-flat-littoral-fluvial facies, corresponding to Wangdian-Hangzhou transgression period, including two climatic cycles. 0–15.4 m is Holocene of the estuarine-fluvial-lagoon facies sedimentary environment, corresponding to Fuyang transgression, including one climatic cycle.
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References
Li J, Yulan Z (2006) Palynological and paleoenvironmental studies of the late neogene sediments in the eastern margin of the Yangtze river delta. J Micropaleont (01):70–76
Liu Z et al (2014) Genesis and spatial characteristics of the marine-terrestrial sedimentary soils in the Yangtze Estuary. J. Undergr Space Eng (01):102–108
Wang Z et al (2008) A preliminary study of the late quaternary chronostratigraphic framework and two transgressions in the Yangtze river delta. J Palaeogeogr (01):99–110
Liu D, Ye Y (2005) Relative sea level rise and the land subsidence in the Yangtze river delta. J Geol Hazards Environ Prot (04):400–404
Sun Q et al (1997) Impact assessment of the sea level rise on the Yangtze river delta. Resour Environ Yangtze River Basin (01):59–65
Zheng Q (2015) Review of the Holocene sea level reconstruction in the Yangtze river delta. Shanghai Land Resour (01):80–85+94
Zhu J, et al (1994) The impact of the sea level rise on the Yangtze river delta and adjacent areas. Geogr Sci (02):109–117+199
Zhang Y (2005) Palynological and environmental studies of the late quaternary sediments in the front area of the Yangtze river delta. J Ocean (Chin Ed) (04):82–87
Zhao B (2013) Late quaternary sequence characteristics in the front of the Yangtze river delta and responses to the post-glacial sea level fluctuations and sediments, Shanghai Land Resour (02):50–54+63
Bai X, et al (2016) Magnetic characteristics of the tidal flat sediments in the Holocene strata of the Yangtze river delta and their paleoenvironmental significance. J Sediment (06):1165–1175
Liu J, et al (2007) Paleovegetation and paleoclimate since the Holocene on both sides of the Qiantang river and the Hangzhou bay. Earth Sci Front (05):235–245
Zhong S (2012) Late quaternary calcareous nannofossils of core Dy03 in the Yangtze river delta and their sedimentary environmental significance. Acta Micropalaeontologica Sinica 29(2):137–144
Zhang R et al (2011) Palaeoenvironmental evolution of subaqueous Yangtze delta inferred from sedimentary records. Mar Geol Quat Geol 31(1):1–10
Miao WD, et al (2016) Stratigraphic division of NB5 core in the Yangtze delta area and its environmental change information. Geology in China
Miao Y et al (2015) Late quaternary pollen records from the Yangtze river delta, east China, and its implications for the Asian monsoon evolution. Arab J Geosci 8(10):7845–7854
Zhao XT, et al (2017) Reviews on the research of late Cenozoic geology and environment of the Yangtze river delta area. J Geomech
Wu SJ (2008) Nanjing and Nanjing, sedimentary characteristics of the palaeochannel and environment evolution during the Holocene in the NW Taihu plain, Yangtze river delta. J Strat
Su J et al (2017) Postglacial sequence stratigraphy and sedimentary environment evolution of the Yangtze river subaqueous delta. J Palaeogeogr
Li B, et al (2011) Quaternary sedimentary records and paleoenvironment response in the Yangtze river delta. Quat Sci (02):316–328
Wei T, et al (2006) Distribution characteristics of the geochemical elements in the quaternary sediments of the Yangtze estuary and their palaeoenvironmental significance. Quat Sci (03):397–405
Wu YH (2013) Sedimentary characteristics and environmental implications of PJ core in the South Wing of the Yangtze river delta. J Guangxi Teach Educ Univ (2013)
Zhuang C, et al (2013) PRD16 pore microorganism records and paleoenvironment reconstruction in the Pearl river delta since the late pleistocene. J Sun Yat-Sen Univ (Nat Sci Ed) (3):128–132+138
Wu J, et al (2014) Palaeoenvironmental significance of the late quaternary microfauna in the eastern pearl river delta. J Sun Yat-Sen Univ (Nat Sci Ed) (6):45–52
Xue MA, et al (2015) Grain-size analysis of the quaternary sediments in Borehole ZKA4 in The Yangtze river delta and its paleoenvironment and paleoclimate implications. J Strat
Chen J, et al (2009) Paleoclimate changes and its coupling with sea level reflected by the sporopollen records since 120kaB.P. in the Yangtze river delta. Mar Sci (02):68–73
Liu C, et al (2008) High resolution ostracodal records and the late quaternary paleoenvironment reconstruction of PRD05 hole in the pearl river delta. J Paleogeography (3):313–322
Acknowledgment
Foundation Projects: China Geological Survey “Geological Survey of Zhejiang Marine Economic Development Demonstration Zone (Jiaxing) Urban Agglomeration” (1212011220008) and “Zhejiang 1/50000 Regional Survey Project of Jiaxing, Pinghu, Jiashan, Shengze and Xinfeng Towns” (1212011220538).
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Lin, Z., Jin, X., Zhu, Z., Pan, S., Zhao, X. (2020). Sedimentary Facies and Paleoenvironment Significance of Hole BZK01 in the Yangtze River Delta Plain Since Pliocene Based on Big Data Analytics. In: Xu, Z., Choo, KK., Dehghantanha, A., Parizi, R., Hammoudeh, M. (eds) Cyber Security Intelligence and Analytics. CSIA 2019. Advances in Intelligent Systems and Computing, vol 928. Springer, Cham. https://doi.org/10.1007/978-3-030-15235-2_41
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