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GAO Maosheng, GUO Fei, HOU Guohua, QIU Jiandong, KONG Xianghuai, LIU Sen, HUANG Xueyong, ZHUANG Haihai. 2018. The evolution of sedimentary environment since late Pleistocene in Laizhou Bay, Bohai Sea[J]. Geology in China, 45(1): 59-68. doi: 10.12029/gc20180106
Citation: GAO Maosheng, GUO Fei, HOU Guohua, QIU Jiandong, KONG Xianghuai, LIU Sen, HUANG Xueyong, ZHUANG Haihai. 2018. The evolution of sedimentary environment since late Pleistocene in Laizhou Bay, Bohai Sea[J]. Geology in China, 45(1): 59-68. doi: 10.12029/gc20180106
shu

The evolution of sedimentary environment since late Pleistocene in Laizhou Bay, Bohai Sea

  • 1.

    Qingdao Institute of Marine Geology, China Geological Survey, Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao 266071, Shandong, China

  • 2.

    Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, Shandong, China

  • 3.

    Institute of Earth Environment, CAS, Xi'an 710061, Shaanxi, China

  • 4.

    China University of Geoscience, Wuhan 430074, Hubei, China

  • 5.

    Liaoning Normal University, Dalian 116000, Liaoning, China

  • 6.

    Qingdao University, Qingdao 266071, Shandong, China

    • Fund Project: Supported by the program of China Geological Survey (No. DD20160144), the National Key Research and Development Program of China (No. 2016YFC0402801) and National Science and Technology Basic Project (No. 2014FY210600)
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  • Author Bio: GAO Maosheng, male, born in 1966, doctor, senior researcher, engages in the study of marine sedimentary environment and coastal geology; E-mail:gms532@163.com
Received Date:  05 December 2017
Revised Date:  23 January 2018
Publish Date:  25 February 2018
    Abstract

  • There have existed three transgression-regression events and sedimentary evolution processes by sea level changes since late Pleistocene in the southern coast of Laizhou Bay, Bohai Sea. It is obvious that a multi-source fluvial delta sedimentary system may be more dominant for the sedimentary environment. Based on previous researchers' survey and collected data, the authors carried out research work such as division of sedimentary units, sedimentary facies analysis and stratigraphic division and correlation, with the purpose of establishing sedimentary stratigraphic framework of the Laizhou Bay. Besides, the authors focused on analyzing the sedimentary processes of the Laizhou Bay since Late Pleistocene. It is concluded that the main provenance of borehole 07 is Bailang River and the Yellow River, which have played an important role in the multi-source fluvial delta sedimentary system of the southern coast of Laizhou Bay since Late Pleistocene. The evolution can be divided into two glacial periods and three interglacial periods, corresponding to three transgression events and two regression events in Laizhou Bay since late Pleistocene. By geochemistry and provenance analysis, sediments have the characteristics of generation, segment and correlation. In 124.6-72.0 ka B.P., 60.0-24.4 ka B.P. and 10.2-4.0 ka B.P., there occurred three warm-wet periods, respectively corresponding to Cangzhou transgression, Xianxian transgression, and Huanghua transgression; In 72.0-60.0 ka B.P. and 24.4-10.2 ka B.P., which were two dry and cold periods, there was a continental sedimentary environment, corresponding to Wurm early glacier age and Wurm late glacial age. During the transgression period, there always developed littoral-neritic facies in marine area, which was gradually transitional to delta and fluvial facies in the land field, with sediments showing retrogradation superposition pattern. Contribution of short runoff rivers (Bailang river) was reduced gradually from land to sea. During the regression period, fluvial and delta facies were formed in most areas of Laizhou Bay. Terrigenous input of short runoff rivers increased, with sediments showing progradational sequences. From late Pleistocene to Holocene, the region went through sedimentary evolution of neritic facies-delta-continental facies-tidal flat-neritic facies-delta-continental facies.

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