宁绍平原东部新石器遗址地层碱土金属元素地球化学特征以及对海水入侵事件的指示

潘昱, 孙国平, 雷少, 吴莹莹, 王张华. 宁绍平原东部新石器遗址地层碱土金属元素地球化学特征以及对海水入侵事件的指示[J]. 海洋地质与第四纪地质, 2023, 43(6): 169-180. doi: 10.16562/j.cnki.0256-1492.2022112202
引用本文: 潘昱, 孙国平, 雷少, 吴莹莹, 王张华. 宁绍平原东部新石器遗址地层碱土金属元素地球化学特征以及对海水入侵事件的指示[J]. 海洋地质与第四纪地质, 2023, 43(6): 169-180. doi: 10.16562/j.cnki.0256-1492.2022112202
PAN Yu, SUN Guoping, LEI Shao, WU Yingying, WANG Zhanghua. Geochemical characteristics of alkaline earth metals in the sediments of Neolithic sites in the eastern Ningshao Plain and implications for the saltwater intrusion[J]. Marine Geology & Quaternary Geology, 2023, 43(6): 169-180. doi: 10.16562/j.cnki.0256-1492.2022112202
Citation: PAN Yu, SUN Guoping, LEI Shao, WU Yingying, WANG Zhanghua. Geochemical characteristics of alkaline earth metals in the sediments of Neolithic sites in the eastern Ningshao Plain and implications for the saltwater intrusion[J]. Marine Geology & Quaternary Geology, 2023, 43(6): 169-180. doi: 10.16562/j.cnki.0256-1492.2022112202

宁绍平原东部新石器遗址地层碱土金属元素地球化学特征以及对海水入侵事件的指示

  • 基金项目: 浙江省重点研发计划“杭州湾沿岸文化遗存与全新世古地貌复原耦合及其三维可视化系统应用”(2022C03141)
详细信息
    作者简介: 潘昱(1998—),女,硕士研究生,主要从事第四纪地质学研究,E-mail:875588348@qq.com
    通讯作者: 王张华(1973—),女,教授,博士生导师,主要从事河口海岸带古环境演变和新石器时代人地关系研究,E-mail:zhwang@geo.ecnu.edu.cn
  • 中图分类号: P531

Geochemical characteristics of alkaline earth metals in the sediments of Neolithic sites in the eastern Ningshao Plain and implications for the saltwater intrusion

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  • 宁绍平原东部地区孕育了丰富灿烂的新石器时代文化,但目前发现的遗址地层中普遍存在着不同时期文化堆积中断现象。选择井头山遗址和鱼山遗址两个剖面进行AMS14C测年、有机地球化学和碱土金属元素分析,探讨稀醋酸提取的碱土金属元素含量变化的特征和原因,同时通过与研究区其他新石器遗址地层记录对比,识别区域性的水文环境变化事件。研究结果显示,稀醋酸提取的碱土金属元素Sr和Ca含量对海岸带低地环境的海水入侵事件十分敏感,是海陆过渡带有效的水文环境代用指标;而Ba含量的变化更加复杂,在两个遗址的中全新世地层中普遍呈现为低值,显示其不仅受水体盐度影响,而且与本地河流输入的泥沙量密切相关。通过区域性地层对比,认为宁绍平原东部新石器时代中晚期存在3次大范围海水入侵事件,分别发生于大约6300、5300和4500 cal. aBP,主要由相对海平面上升或极端风暴事件造成,是新石器遗址文化堆积中断的主要原因。

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  • 图 1  杭州湾沿岸地貌概况与采样点分布

    Figure 1. 

    图 2  井头山剖面(a)与鱼山遗址T0213S(b)年龄深度模型

    Figure 2. 

    图 3  井头山剖面(a)、鱼山遗址T0213S(b)地层及地球化学元素含量变化

    Figure 3. 

    图 4  多个遗址剖面和良渚古城ZK07孔Sr(a)、Ba(b)与TOC含量对比下王渡、乌龟山遗址及ZK07孔数据分别引自[21-22,32]

    Figure 4. 

    图 5  杭州湾沿岸典型新石器遗址地层及海水入侵事件对比

    Figure 5. 

    表 1  井头山剖面、鱼山遗址T0213S 的AMS14C测年数据及校正结果

    Table 1.  AMS14C ages and their calibrations of the profiles JTS and T0213S

    剖面深度/cm测年材料14C年龄 /aBP校正年龄
    /cal. aBP
    实验室编号数据
    来源
    2σ置信
    水平
    中值
    井头山
    剖面
    JTS
    23富有机质泥3960±304295~452014430Beta-629556本研究
    95植物碎屑4660±305317~546515400Beta-629557
    143*炭屑6060±306835~69950.9256915Beta-629558
    185植物碎屑6020±306784-~69470.9886860Beta-629559
    鱼山
    遗址T0213S
    125~130种子4300±254830~48830.9334855BA151805He等[30]
    150~155种子4525±255051~531015155BA151806
    180~185种子4785±255476~558415525BA151807
    215~220种子5495±256211~639016295BA151808
    230~235种子5665±256394~64990.9846440BA151809
    245~250种子5860±256626~67450.9856690BA151810
    260~265种子6225±257011~724917105BA151811
    注:*代表年龄倒置,不参与年龄深度模型计算。
    下载: 导出CSV
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收稿日期:  2022-11-22
修回日期:  2022-12-09
录用日期:  2022-12-09
刊出日期:  2023-12-28

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