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苏北平原MIS3阶段海侵事件的沉积记录

, PP. 883-891

Keywords: 苏北平原,海侵事件,沉积环境,氧同位素3阶段(MIS,3)

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Abstract:

MIS3阶段的气候与环境是古气候与古环境研究的热点,该阶段中国沿海地区的海侵过程是沿海平原环境演化的重要事件。根据苏北平原宝应By1钻孔的14C年代结果和沉积特征、微体生物组合特点,确认苏北平原MIS3阶段存在明显的海侵事件,潮滩与泻湖相沉积层的厚度约7m,深度在By1孔19~26m,海相层位于长江三角洲地区的典型末次冰盛期的硬粘土层之下,14C年代在距今26~39ka之间,属于MIS3阶段的沉积,岩芯沉积物的沉积构造以水平的薄层砂质粉砂沉积为主。沉积物中大量的海相有孔虫壳体在研究的岩芯段中是最丰富的;此外,还发现咸水环境下的Sinocytherideaimpressa(Brady),Spinileberispulchra与Spinileberisfuruyaensis,NeomonoceratinachenaeZhao,Keijellabisanensis(Okubo)等形类壳体;该段岩芯中的植物残体、碳屑也很丰富,有机质含量丰富,显示比较封闭的弱动力环境,指示了潮滩、泻湖沉积环境。

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