基于沉积成因地化元素指标的闽北海湾晚更新世海侵地层辨识及其意义<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2022.01.011

古地理学报 ›› 2022, Vol. 24 ›› Issue (1): 139-151. doi: 10.7605/gdlxb.2022.01.011

基于沉积成因地化元素指标的闽北海湾晚更新世海侵地层辨识及其意义^*

孙丹丹¹, 刘平¹, 张杰¹, 于俊杰², 岳伟³, 王继龙², 彭博², 刘演¹, 李月¹, 陈静¹

1 华东师范大学河口海岸学国家重点实验室,上海 200241;
2 中国地质调查局南京地质调查中心,江苏南京 210016;
3 江苏师范大学地理测绘与规划学院,江苏徐州 221116

收稿日期:2021-07-16 修回日期:2021-09-08 出版日期:2022-01-01 发布日期:2022-01-24
通讯作者: 陈静,女,1977年生,华东师范大学河口海岸学国家重点实验室研究员,主要从事自然地理学研究。E-mail: jchen@geo.ecnu.edu.cn。
作者简介:孙丹丹,女,1996年生,华东师范大学河口海岸学国家重点实验室硕士研究生,自然地理学专业。E-mail: 51193904002@stu.ecnu.edu.cn。
基金资助:
*国家自然科学基金项目(编号: 41771226,41620104004)与中国地质调查局宁德海岸陆海统筹项目(编号: DD20189505)联合资助;

Identification and significance of the Late Pleistocene transgressive strata in the bays of northern Fujian Province based on geochemical element indicators of sedimentary origin

Sun Dan-Dan¹, Liu Ping¹, Zhang Jie¹, Yu Jun-Jie², Yue Wei³, Wang Ji-Long², Peng Bo², Liu Yan¹, Li Yue¹, Chen Jing¹

1 State Key Laboratory of Estuarine and Coastal Research,East China Normal University,Shanghai 200241,China;
2 Nanjing Center,China Geological Survey,Nanjing 210016,China;
3 School of Geography,Geomatics and Planning,Jiangsu Normal University,Jiangsu Xuzhou 221116,China

Received:2021-07-16 Revised:2021-09-08 Online:2022-01-01 Published:2022-01-24
Contact: Chen Jing,born in 1977, is a professor at State Key Laboratory of Estuarine and Coastal Research,East China Normal University. She is mainly engaged in research on physical geography. E-mail: jchen@geo.ecnu.edu.cn.
About author:Sun Dan-Dan,born in 1996, is a master degree candidate majoring in physical geography at East China Normal University. E-mail:51193904002@stu.ecnu.edu.cn.
Supported by:
Co-funded by the National Natural Science Foundation of China(Nos. 41771226,41620104004)and the Integrated Geological Survey on Land and Sea of the Ningde Coast(No. DD20189505)

摘要/Abstract

摘要： 福建沿岸晚更新世地层中微体古生物化石较为缺乏,极大限制了对该区晚第四纪海侵过程的深入研究。针对这一问题,本研究以闽北2个海湾内的第四纪钻孔为研究对象,通过有孔虫化石以及沉积成因的地球化学元素(Sr/Ba、Mn/Fe)分析,结合三沙湾表层沉积物相应指标,探讨沉积成因的地球化学元素指示海侵地层的可行性。结果显示,2个海湾钻孔的晚第四纪地层中均发育3套疑似海相深灰色黏土层,其中开放海湾霞浦湾钻孔底部黏土层中缺失有孔虫,半封闭海湾三沙湾钻孔中有孔虫仅出现于顶部黏土层中。这3层黏土层的Sr/ Ba值远大于1,和现代潮滩—河口湾体系相近,且出现的海相沟鞭藻和自生黄铁矿为典型的海相地层特征。基于已有的OSL和AMS¹⁴C年龄框架,这3层海侵层分别对应于MIS5、MIS3和MIS1期,Sr/Ba和Mn/Fe均值从MIS5到MIS1期不断增大,结合现代潮滩-河口湾体系指标,表明从MIS5到MIS1期海侵强度的增加。由此可见,沉积成因地球化学元素指标可以有效辨识闽北海湾晚更新世海侵地层,这将有助于进一步了解该区晚第四纪海侵过程及其控制因素。

关键词: 元素比值, 有孔虫, 海侵地层, 福建沿岸, 晚更新世

Abstract: The lack of micropaleontological records in the Late Pleistocene strata along the Fujian coasts has greatly restricted the further understanding on the regional land-sea interaction. This study aims to identify the transgressive strata of the Late Pleistocene in the two bays of northern Fujian,by using geochemical elements of sedimentary origin. Based on the analysis of the foraminifera and surficial sediments of Sansha Bay,the Sr/ Ba and Mn/ Fe are used as proxies to identify the possibility of transgression in the study area. The results suggest that there are three sets of dark grey layers in the two late Quaternary cores might be formed in a marine environment. Foraminifera are missed at the bottom of drilling cores in the open Xiapu Bay,while foraminifera are only observed in the upper drilling cores of semi-closed Sansha Bay. However,the sedimentary Sr/ Ba ratios in the three clay layers are much higher than 1 and similar to the modern tidal flat and bay system,indicating typical marine origins. This is also supported by the occurrence of marine dinoflagellates and abundant authigenic pyrites in these layers. Based on the existing chronology of the core(NDGK2),the three transgressive layers are possibly corresponding to the high-stands of the MIS5,MIS3 and MIS1,respectively. The mean ratios of Sr/ Ba and Mn/ Fe show an increase trend from MIS5 to MIS1,indicating marine influence is enhanced compared with the ratios of modern ti dal flat-bay system. This study shows geochemical elements of sedimentary origin can be used as an effective proxy to identify the Late Pleistocene transgression strata along the Fujian coast,which will help to further understand the process and controlling factors of the late Quaternary transgression in this area.

Key words: element ratios, foraminifera, transgression strata, Fujian coast, Late Pleistocene

中图分类号:

P512.2

孙丹丹, 刘平, 张杰, 于俊杰, 岳伟, 王继龙, 彭博, 刘演, 李月, 陈静. 基于沉积成因地化元素指标的闽北海湾晚更新世海侵地层辨识及其意义^*[J]. 古地理学报, 2022, 24(1): 139-151.

Sun Dan-Dan, Liu Ping, Zhang Jie, Yu Jun-Jie, Yue Wei, Wang Ji-Long, Peng Bo, Liu Yan, Li Yue, Chen Jing. Identification and significance of the Late Pleistocene transgressive strata in the bays of northern Fujian Province based on geochemical element indicators of sedimentary origin[J]. JOPC, 2022, 24(1): 139-151.

http://www.gdlxb.cn/CN/Y2022/V24/I1/139

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基于沉积成因地化元素指标的闽北海湾晚更新世海侵地层辨识及其意义^*

Identification and significance of the Late Pleistocene transgressive strata in the bays of northern Fujian Province based on geochemical element indicators of sedimentary origin

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基于沉积成因地化元素指标的闽北海湾晚更新世海侵地层辨识及其意义*

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基于沉积成因地化元素指标的闽北海湾晚更新世海侵地层辨识及其意义^*