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首页> 外文期刊>Progress in Oceanography >Large-scale pollen distribution in marine surface sediments from the Bohai Sea, China: Insights into pollen provenance, transport, deposition, and coastal-shelf paleoenvironment
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Large-scale pollen distribution in marine surface sediments from the Bohai Sea, China: Insights into pollen provenance, transport, deposition, and coastal-shelf paleoenvironment

机译:中国渤海海表沉积物的大规模花粉分布:对花粉起源,运输,沉积和沿海陆架古环境的认识

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摘要

To elucidate the mechanisms responsible for pollen and spore transportation and deposition in the Bohai Sea, fully covered seafloor-surface sediment samples were collected for palynological and grain size analysis. The results reveal that the pollen and spore concentrations were higher in the head of Liaodong Bay and in the muddy area of the Bohai Sea. The Yellow River was the main source of pollen and spores in the Bohai Sea. The sediments with relatively high pollen concentrations consisted mainly of clay and fine silt, whereas sediment with lower pollen concentrations was mostly fine sand. In addition, the percentages of Firms pollen and pteridophyte spores increased with increasing sea water depth, while other arboreal (excluding Pinus) and herbaceous pollen generally decreased with increasing distance from the shore. The relationship between the pollen taxa and the water depth of the sampling points shows that the fluvial water plays a predominant role in pollen transmission within 20 m of water depth, while the wind is the main driving force for pollen transmission when the water depth exceeds 20 m. Although Pinus pollen and pteridophyte spores were over-represented, there was good correlation between marine pollen signals and terrestrial vegetation. Apart from the influence of rivers and wind on pollen and spore deposition, the tidal currents and circulation were also main force responsible for transporting sediment and determining the differentiation of pollen and spores in the Bohai Sea. The comparison of pollen and spore percentages between surface sediment and fossil records from sedimentary cores made it possible to identify changes in pollen sources and transport mechanisms. Meanwhile, the percentage fluctuations of fossil Pinus and herbaceous pollen revealed concomitant changes of the sea level and climate. These findings are of paramount importance to the interpretation of Quaternary marine pollen data from the Bohai Sea, China.
机译:为了阐明造成花粉和孢子在渤海中运输和沉积的机制,收集了全覆盖的海底表层沉积物样本,以进行孢粉学和粒度分析。结果表明,辽东湾海域顶部和渤海浑浊地区的花粉和孢子浓度较高。黄河是渤海地区花粉和孢子的主要来源。花粉浓度较高的沉积物主要由粘土和细粉砂组成,而花粉浓度较低的沉积物主要是细砂。此外,牢固的花粉和蕨类植物孢子的百分比随着海水深度的增加而增加,而其他树木(不包括松树)和草本花粉通常随着距岸距离的增加而减少。花粉类群与采样点水深的关系表明,河流水在水深20 m以内的花粉传播中起主要作用,而当水深超过20 m时,风是花粉传播的主要驱动力。米尽管松花粉和蕨类植物孢子的含量过高,但海洋花粉信号与陆地植被之间存在良好的相关性。除了河流和风对花粉和孢子沉积的影响外,潮汐流和环流也是决定沉积物运输和决定渤海花粉和孢子分化的主要力量。通过比较表层沉积物和沉积岩中化石记录的花粉和孢子百分比,可以发现花粉来源和运输机制的变化。同时,化石松和草本花粉的百分比波动揭示了海平面和气候的伴随变化。这些发现对于解释来自中国渤海的第四纪海洋花粉数据至关重要。

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  • 来源
    《Progress in Oceanography》 |2019年第11期|102183.1-102183.17|共17页
  • 作者单位

    China Geol Survey Key Lab Coastal Wetland Biogeosci Qingdao Inst Marine Geol Qingdao 266071 Shandong Peoples R China|Qingdao Natl Lab Marine Sci & Technol Lab Marine Geol Qingdao 266061 Shandong Peoples R China;

    Chinese Acad Sci Nanjing Inst Geog & Limnol State Key Lab Lake Sci & Environm Nanjing 210008 Jiangsu Peoples R China;

    China Geol Survey Key Lab Coastal Wetland Biogeosci Qingdao Inst Marine Geol Qingdao 266071 Shandong Peoples R China|Louisiana State Univ Sch Coast & Environm Dept Environm Sci Baton Rouge LA 70803 USA;

    China Geol Survey Key Lab Coastal Wetland Biogeosci Qingdao Inst Marine Geol Qingdao 266071 Shandong Peoples R China;

    Minist Nat Resources Inst Oceanog 1 Qingdao 266061 Shandong Peoples R China;

    Univ Goettingen Dept Palynol & Climate Dynam D-37073 Gottingen Germany;

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