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作 者:李保华[1] 王晓燕[1] 孔晓敏[1] 林春明[2] 李艳丽[2] 张霞[2]
机构地区:[1]中国科学院南京地质古生物研究所,南京210008 [2]南京大学地球科学与工程学院,南京210093
出 处:《微体古生物学报》2012年第2期121-129,共9页Acta Micropalaeontologica Sinica
基 金:中国科学院知识创新工程重要方向项目(kzcx2-yw-155-2);中国科学院战略性先导科技专项(XDA05120601);国家自然科学基金(40872075;40876020)资助
摘 要:本研究对浙江萧山SE2钻孔近50m沉积物岩心进行了详细的有孔虫定量统计分析,并结合测年资料重建了冰后期以来钱塘江沉积河谷的环境演化过程。有孔虫群落特征反映的古环境变化与沉积相分析结果一致。有孔虫资料显示:大约1万年以来该地区受到海水的影响、以胶结质壳Textularia-Reophax组合为特征,并在中全新世海水深度到达最大、以近岸浅水组合Ammonia beccarii-Elphidium magellanicum为代表,而晚全新世以来在全球海平面下降的影响下、该地区海水变浅的同时,却由于狭窄的特殊河口地形,水动力相对较强,显示强潮型河口地区特有的近岸分子Ammonia beccarii,Elphidium advenum和相对较深水分子Ammonia compressiuscula共存的底栖有孔虫群落特征。A 50 m sedimentary core (SE2) from Xiaoshan, southern Qiantang River estuary was taken for the study of paleoenvironmental changes. Quantitative foraminiferal analyses were performed for more than 90 samples. AMS14 C dates indicate that the foraminiferal fauna records the post-glacial environmental evolution of the Qiantang River val- ley. With the global sea-level rise, the valley was affected by the marine water since 10 kaBP, but only few species first occurred, such as the agglutinated Textularia spp. and Reophax donghaiensis, and euryhaline Ammonia becca- rii in a lower abundance, possibly from the low-salinity intertidal zone. Both the benthic and planktic foraminifera then increased to a higher abundance and diversity during the middle Holocene, with Ammonia beccarii and Elphidi um magellanicum as dominant species, which suggests coastal shallow water. However, the late Holocene foramini- feral assemblage was characterized by the nearshore Ammonia beccarii and Elphidium advenum mixed with the relatively deeper-water species Ammonia compressiuscula, which implies a shallow but high-energy water influence, pos sibly resulted from the narrowing estuary with the global sea-level drop, which performs as a macro-tidal estuary environment today.
分 类 号:Q915[天文地球—古生物学与地层学]
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