琼北盆地晚新生代沉积环境变迁的孢粉记录

Palynological records of sedimentary environmental changes during the late Cenozoic in Qiongbei Basin, Hainan Island

  • 摘要: 孢粉是近海沉积环境研究中的重要微体化石,为进一步了解琼北盆地新生代沉积环境演化,支撑区域统一地层格架的建立,在碎屑石英电子自旋共振(Electron Spin Resonance,简称ESR)测年的基础上,对琼北盆地QJD10孔岩芯进行了系统的孢粉鉴定,并结合沉积特征重建了琼北盆地的沉积环境变迁。QJD10孔共鉴定花粉和孢子121科属,并根据分布特征将其分为3个组合带、6个亚带。QJD10孔近岸地层以高孢粉浓度和孢粉组合中常绿栎属、松属等热带亚热带木本植物花粉组分占绝对优势,而远岸地层以低孢粉浓度和高蕨类植物孢子含量的特征,结合测年数据、地层沉积特征和沟鞭藻、有孔虫海相微体化石的分布,揭示晚新生代以来琼北盆地经历了由三角洲至无障壁海岸、再到湖泊和暴露风化环境的海陆变迁。QJD10孔孢粉的变化还记录了水动力环境的变迁,238.30~123.40 m段的高蕨类植物孢子含量和总体孢粉浓度的明显下降,以及199.90~189.00 m段孢粉浓度的突然升高指示了一个受水流影响的高能沉积环境,可能还受到琼州海峡古洋流的作用。QJD10孔的孢粉记录了琼北盆地晚新生代的沉积环境演化,为区域地层的对比提供了重要参考。

     

    Abstract: Palynological analysis plays an important role in paralic paleoenvironment reconstruction. For further understanding of the Cenozoic sedimentary environment changes, and supporting the establishment of regional stratigraphic framework, the pollen and spore assemblages were identified systemically from core QJD10 in Qiongbei Basin, Hainan Island. Based on clastic quartz ESR (electron spin resonance) dating, the sedimentary environmental evolution was reconstructed with the sedimentary characteristics and the palynological record. A total of 121 families and genera of pollen and spores were identified from core QJD10. There are 3 assemblage zones and 6 subzones categorized according to its variation. With the dating data, sedimentary characteristics, and the distribution of marine microfossils dinoflagellates and foraminifera, the fluctuations of pollen and spores from core QJD10 recorded the sedimentary environment changes from marine to continental facies, which experienced from delta to unbarriered coast, and then to lake, and finally exposed to erosion in Qiongbei Basin during the late Cenozoic. In the nearshore environment, the palynological concentration is relatively high, with an absolute dominance of tropical and subtropical woody plant pollen components such as Quercus-evergreen and Pinus, whereas in the offshore environment, the palynological concentration is much lower, and featured with higher fern spores components. Moreover, the palynological record in core QJD10 could reflect the changes of hydrodynamic environment. The high content of fern spores and the dramatic decline of general palynological concentration in 238.30~123.40 m, as well as the abrupt increase of palynological concentration in 199.90~189.00 m indicates a high-energy hydrodynamic environment, which might be affected by the paleocurrent across the Qiongzhou Strait. The palynological records from core QJD10 reflect the sedimentary environmental evolution during the late Cenozoic in Qiongbei Basin, and provid an important reference for the regional stratigraphic work.

     

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