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长江中下游水阳江流域BZK0402孔多重地层划分及其冰后期海平面变化的沉积响应

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陈忠良, 张晋喆, 沈仕豪, 黄蒙, 徐锦龙, 葛海影, SimonM. Jowitt. 2022. 长江中下游水阳江流域BZK0402孔多重地层划分及其冰后期海平面变化的沉积响应[J]. 中国地质, 49(2): 655-666. doi: 10.12029/gc20220221
引用本文: 陈忠良, 张晋喆, 沈仕豪, 黄蒙, 徐锦龙, 葛海影, SimonM. Jowitt. 2022. 长江中下游水阳江流域BZK0402孔多重地层划分及其冰后期海平面变化的沉积响应[J]. 中国地质, 49(2): 655-666. doi: 10.12029/gc20220221
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CHEN Zhongliang, ZHANG Jinzhe, SHEN Shihao, HUANG Meng, XU Jinglong, GE Haiying, Simon M. Jowitt. 2022. Multi-stratigraphic study and response to sea-level fluctuations since the last deglaciation detected from BZK0402 core in the Shuiyang River basin, Yangtze River[J]. Geology in China, 49(2): 655-666. doi: 10.12029/gc20220221
Citation: CHEN Zhongliang, ZHANG Jinzhe, SHEN Shihao, HUANG Meng, XU Jinglong, GE Haiying, Simon M. Jowitt. 2022. Multi-stratigraphic study and response to sea-level fluctuations since the last deglaciation detected from BZK0402 core in the Shuiyang River basin, Yangtze River[J]. Geology in China, 49(2): 655-666. doi: 10.12029/gc20220221
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长江中下游水阳江流域BZK0402孔多重地层划分及其冰后期海平面变化的沉积响应

  • 1.

    安徽省地质调查院，安徽 合肥 230001

  • 2.

    合肥工业大学 资源与环境工程学院，安徽 合肥 230009

  • 3.

    内华达大学拉斯维加斯分校地球科学学院，内华达州 拉斯维加斯 89154-4010

  • 基金项目:
    中国地质调查局地质调查项目（DD20160036，DD20190043）和安徽省自然科学基金青年项目（1808085QD116）联合资助
详细信息
    作者简介: 陈忠良，男，1984年生，博士生，高级工程师，长期从事区域地质调查和地学信息技术研究; E-mail: c_mulder@163.com

  • 中图分类号: P534.63

Multi-stratigraphic study and response to sea-level fluctuations since the last deglaciation detected from BZK0402 core in the Shuiyang River basin, Yangtze River

  • 1.

    Geological Survey of Anhui Province, Hefei 230001, Anhui, China

  • 2.

    School of Resources and Environment Engineering, Hefei University of Technology, Hefei 230009, Anhui, China

  • 3.

    Department of Geoscience, University of Nevada Las Vegas, Las Vegas 89154-4010, Nevada, USA

  • Fund Project: Supported by the project of China Geological Survey (No.DD20160036, DD20190043) and Anhui Provincial Natural Science Foundation (No.1808085QD116)
More Information
    Author Bio: CHEN Zhongliang, male, born in 1984, doctor candidate, senior engineer, mainly engaged in the regional geological survey and information technology research on geosciences; E-mail: c_mulder@163.com .

    摘要
  • 研究目的

    开展水阳江流域标准孔BZK0402孔多重地层划分，探讨长江支流水阳江流域冰后期海平面变化的沉积响应以及古丹阳湖的成因和形成时代。

     研究方法

    以岩石地层为基础，在磁性地层和年代地层的双重约束下，对BZK0402孔进行多重地层划分。对比分析BZK0402孔和长江河谷、长江三角洲等邻区钻孔。

     研究结果

    BZK0402孔第四纪地层可划分为中—下更新统大桥镇组、全新统芜湖组。钻孔所属的长江三角洲西缘河湖环境沉积物对末次盛冰期以来海平面升降和气候变化存在沉积响应：末次盛冰期，长江中下游河流比降大，区内河流侵蚀作用强烈，沉积物以砂砾石层为主; 全新世早期，区内受冰后期海侵影响，沉积物粒度逐渐变细，沉积环境由河漫滩相向湖相过渡。植被覆盖类型以针叶林为主，林下蕨类植物生长茂盛。平原地区发育湖泊沼泽; 全新世中期，海侵逐渐至最大，区内发育湖相淤泥质黏土。森林面貌以针叶-落叶阔叶混交林为主; 全新世晚期至今，区内沉积物有扰动现象。

     结论

    长江支流水阳江河谷中不仅是全新世沉积，还发育更新世沉积。水阳江流域内古丹阳湖形成于全新世早期，其形成与全新世海侵在时间上存在一致性。

    This paper is the result of environmental geological survey engineering.

     Objective

    To carry out multi-stratigraphic research on the borehole BZK0402 located in the Shuiyang River basin, and explore the sea-level fluctuations since the last deglaciation and the origin of the Paleo-Danyang Lake formation.

     Methods

    Based on the lithostratigraphical classification and the magnetostratigraphic and chronostratigraphical constraints, the multi-stratigraphic study on the BZK0402 core was carried out. Comparative analysis was also been made between the BZK0402 core and the cores which located in the Yangtze River valley and the Yangtze River delta.

     Results

    The analysis divided the BZK0402 core within Quarternary era into two units, namely the Middle-Upper Pelistocene Daqiaozhen Formation and the Holocene Wuhu Formation. The sediments through the western margin of the Yangtze River delta where the BZK0402 core lies in, also furthers our understanding of the general pattern of sea-level change since the Last Glacial Maximum (LGM), with these changes divided into four stages as follows: (1) The LGM was associated with a period of gravel and sand dominated deposition as a result of steep slopes and significant strong fluvial erosion within the Middle and Lower Reaches of the Yangtze River. (2) The Early Holocene saw a decrease in the grainsize of the sediments being deposited, with sedimentary facies changing from fluvial to lacustrine environments as a result of post-glacial transgression. This period also saw the development of pteridophyte undergrowth-dominated coniferous forest vegetation along with lakes and bog and swamp areas. (3) The Middle Holocene transgressive maximum was associated with the deposition of lacustrine clays that contain coniferous broad-leaved mixed forest vegetation. (4) These sediments are overlain by disturbed Late Holocene to present sediments, with this disturbance caused by uncertain factors.

     Conclusions

    The sediments in the Shuiyang River, which is a tributary of Yangzte River, not only formed within Holecene, but also formed in Pleistocene. The Paleo-Danyang Lake located within the Shuiyang River Valley formed during the Early Holocene, and the period of the lake formation consistent with the Holocene transgression.
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  • 图 1  研究区及BZK0402孔位置图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  BZK0402孔岩性剖面、古地磁曲线图及测年结果

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  BZK0402孔主要孢粉百分比图

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  BZK0402孔与固城湖孔、秦淮河流域N06S6孔、镇江B09孔岩性和沉积环境对比

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    图 5  BZK0402孔湖相沉积物岩心照片

    Figure 5. 

    下载: 全尺寸图片 幻灯片

    表 1  BZK0402孔AMS 14C年代序列及OxCal v4.4.2校正结果

    Table 1.  Results of the radiocarbon dating of the BZK0402 core

    下载: 导出CSV

    表 2  BZK0402孔OSL定年结果

    Table 2.  Results of the optically stimulated luminescence dating of the BZK0402 core

    下载: 导出CSV

    表 3  BZK0402孔与固城湖孔、N06S6孔、B09孔基本信息

    Table 3.  Essential information about the BZK0402 (this study), Gucheng Lake, N06S6, and B09 cores

    下载: 导出CSV
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收稿日期:  2019-04-04
修回日期:  2019-10-05
刊出日期:  2022-04-25

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