珠江口内伶仃洋晚第四纪黏土矿物组成特征及对源区气候变化的指示

张立雪, 陈爱清, 陈庆, 赖佩欣. 珠江口内伶仃洋晚第四纪黏土矿物组成特征及对源区气候变化的指示[J]. 海洋地质与第四纪地质, 2021, 41(5): 202-209. doi: 10.16562/j.cnki.0256-1492.2020121002
引用本文: 张立雪, 陈爱清, 陈庆, 赖佩欣. 珠江口内伶仃洋晚第四纪黏土矿物组成特征及对源区气候变化的指示[J]. 海洋地质与第四纪地质, 2021, 41(5): 202-209. doi: 10.16562/j.cnki.0256-1492.2020121002
ZHANG Lixue, CHEN Aiqing, CHEN Qing, LAI Peixin. Late Quaternary clay minerals in the inner Lingdingyang of the Pearl River Estuary, southern China: Implications for paleoclimate changes at the provenance[J]. Marine Geology & Quaternary Geology, 2021, 41(5): 202-209. doi: 10.16562/j.cnki.0256-1492.2020121002
Citation: ZHANG Lixue, CHEN Aiqing, CHEN Qing, LAI Peixin. Late Quaternary clay minerals in the inner Lingdingyang of the Pearl River Estuary, southern China: Implications for paleoclimate changes at the provenance[J]. Marine Geology & Quaternary Geology, 2021, 41(5): 202-209. doi: 10.16562/j.cnki.0256-1492.2020121002

珠江口内伶仃洋晚第四纪黏土矿物组成特征及对源区气候变化的指示

  • 基金项目: 南方海洋科学与工程广东省实验室(广州)人才团队引进重大专项 “粤港澳大湾区海岸线及滩涂湿地千年至十年尺度环境演变”(GML2019ZD0209)
详细信息
    作者简介: 张立雪(1990—),女,博士,工程师,从事海洋沉积物和结核结壳研究,E-mail:zhanglixue9782@163.com
  • 中图分类号: P736.2

Late Quaternary clay minerals in the inner Lingdingyang of the Pearl River Estuary, southern China: Implications for paleoclimate changes at the provenance

  • 黏土矿物组合和相对含量变化可反映源区地表风化过程,进而推断古气候的周期性变化,因此黏土矿物分析是古气候重建的重要手段之一。对珠江口内伶仃洋13-LD-ZK20钻孔晚第四纪沉积物中黏土矿物组成进行分析,结果显示黏土矿物主要为蒙脱石(含伊利石/蒙脱石无序混层),平均相对含量为49%,其次为伊利石、高岭石和绿泥石,平均相对含量分别为20%、19%和12%。伊利石化学指数较高(多数大于0.4),指示源区强烈的化学风化作用。珠江口内伶仃洋晚第四纪以来黏土矿物根据其相对含量变化和岩芯是否受成岩作用影响可分为4个阶段,指示西江源区气候总体暖-冷-暖的变化趋势。晚更新世第1阶段黏土矿物受成岩作用影响,不具古气候指示意义,第2阶段初期较为温暖,末期存在短期气候相对干冷阶段,可能与晚更新世末次冰盛期有关,第3阶段前期稍转暖。全新世(第3阶段后期和第4阶段)主要为温暖潮湿气候特征,并存在短期冷-暖波动。

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  • 图 1  珠江口内伶仃洋13-LD-ZK20钻孔位置图

    Figure 1. 

    图 2  13-LD-ZK20钻孔地层柱状图

    Figure 2. 

    图 3  13-LD-ZK20钻孔典型样品X射线衍射图

    Figure 3. 

    图 4  13-LD-ZK20钻孔黏土矿物相对含量变化柱状图

    Figure 4. 

    图 5  13-LD-ZK20钻孔黏土矿物含量和比值变化阶段划分图

    Figure 5. 

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收稿日期:  2020-12-10
修回日期:  2021-01-29
刊出日期:  2021-10-28

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