| 渤海湾沿岸贝壳堤对潮滩有孔虫海面变化指示意义的影响 |
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| 引用本文： | 李建芬,商志文,姜兴钰,陈永胜,王福,田立柱,王宏.渤海湾沿岸贝壳堤对潮滩有孔虫海面变化指示意义的影响[J].地质通报,2016,35(10):1578-1583. |
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| 作者姓名： | 李建芬 商志文 姜兴钰 陈永胜 王福 田立柱 王宏 |
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| 作者单位： | 1. 中国地质调查局天津地质调查中心, 天津 300170;2. 中国地质调查局泥质海岸带地质环境重点实验室, 天津 300170 |
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| 基金项目： | 国家自然科学基金项目（批准号:41372173）和中国地质调查局项目（编号:1212011120169、12120113005800） |
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| 摘 要： | 通过对渤海湾沿岸有贝壳堤发育和无贝壳堤发育的2类现代开放潮滩有孔虫组合的对比,研究了该2类潮滩环境沉积物中有孔虫的海面指示意义。5个有孔虫组合带被MHWST(平均大潮高潮位)、MHW(平均高潮位)、MHWNT(平均大潮低潮位)和MSL(平均海面)分隔,分别对应潮滩的高盐沼、低盐沼、潮间带上部、潮间带中上部和潮间带中下部5个不同亚环境。不同亚环境沉积物因其所含的有孔虫群的独特性,均可作为高精度海面标志物,误差为各亚带高差的1/2。沿岸贝壳堤可对潮滩有孔虫的属种组成产生影响,影响程度从高潮位向低潮位逐渐降低。在MHWNT潮位之下,有孔虫组合不再受到沿岸贝壳堤的影响。
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| 关 键 词： | 有孔虫 贝壳堤 泥质潮坪 海面指示意义 渤海湾 |
| 收稿时间： | 2016/5/19 0:00:00 |
| 修稿时间： | 2016/8/22 0:00:00 |
Sea-level indicated by foraminifera assemblages liv-ing in the open muddy flats with or without influence of the chenier ridges in Bohai Bay coastal areas |
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| LI Jianfen,SHANG Zhiwen,JIANG Xingyu,CHEN Yongsheng,WANG Fu,TIAN Lizhu and WANG Hong.Sea-level indicated by foraminifera assemblages liv-ing in the open muddy flats with or without influence of the chenier ridges in Bohai Bay coastal areas[J].Geologcal Bulletin OF China,2016,35(10):1578-1583. |
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| Authors: | LI Jianfen SHANG Zhiwen JIANG Xingyu CHEN Yongsheng WANG Fu TIAN Lizhu and WANG Hong |
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| Institution: | 1. Tianjin Center, China Geological Survey, Tianjin 300170, China;2. Key Laboratory of Muddy Coast Geo-environment, China Geological Survey, Tianjin 300170, China |
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| Abstract: | Based on comparison of the two categories of foraminifera fauna living on the modern open muddy tidal flats in the west coast of Bohai Bay, with or without chenier ridge, the authors thoroughly studied the variability indicating sea level elevations by different foram assemblages in these two kinds of environment. Each category of forams, consisting of five assemblages and corresponding to five subzones, i.e., high salt marsh, low salt marsh, upper intertidal, upper-middle intertidal and middle-lower intertidal subenvironments, was separated successively by MHWST, MHW, MHWNT and MSL, and investigated in detail. As a result, the specific forams-attached sediment from each subzone on tidal surface can be recognized as a high-accuracy sea level indicator, of which the reconstructed elevation point lies in the middle of the subzone with an error of half of the vertical range. It is evident that the existence of the local chenier body can exert an influence on the composition of foram assemblages, and such an influence tends to decline gradually from high to low water, and finally fades out seaward beneath the MHWNT. |
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| Keywords: | foraminifera assemblages chenier muddy tidal flats sea level indication Bohai Bay |
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