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首页> 外文期刊>Quaternary International >Early Holocene history of the Baltic Sea, as reflected in coastal sediments in Blekinge, southeastern Sweden
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Early Holocene history of the Baltic Sea, as reflected in coastal sediments in Blekinge, southeastern Sweden

机译:波罗的海的全新世早期历史,反映在瑞典东南部布莱金厄的沿海沉积物中

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摘要

Integrated palacoecological studies of two fiord sediment sequences in the province of Blekinge, SE Sweden, covering the time span 11,000-5000 cal BP, reveal the timing and the environment for the Ancylus Lake/Littorina Sea transition 9800-8500 cal BP. The first ingression of saline water into the Baltic Sea through the Danish Straits occurred earlier than formerly assumed. New evidence, particularly mineral magnetic and palaeobotanical analyses, demonstrate that on the general trend of the ecstatically caused Littorina transgression several minor fluctuations of the water level can be identified between 8500 and 5000 cal years BP. A distinct regression phase around 8100 cal BP is correlated with the Greenland ice-core cold event dated to 8200 ice-core years BP. This is described as a regional climatic catastrophe for the Baltic Sea region. The coastul stratigraphy is compared with the offshore stratigraphy earlier studied. A tentative shore displacement curve for Early and Middle Holocene is presented.
机译:瑞典东南部布雷金厄省两个峡湾沉积序列的综合古生态学研究涵盖了11,000-5000 cal BP的时间跨度,揭示了Ancylus湖/ Littorina海过渡9800-8500 cal BP的时间和环境。盐水首先通过丹麦海峡进入波罗的海,发生的时间比以前设想的要早。新的证据,特别是矿物磁性和古植物学分析表明,在狂喜引起的立陶宛海侵的总体趋势下,可以确定在8500到5000 cal BP之间水位有一些细微的波动。大约在8100 cal BP附近有一个明显的回归阶段,它与日期为8200 BP的格陵兰冰芯寒冷事件有关。这被描述为波罗的海地区的区域性气候灾难。将沿海地层与先前研究的海上地层进行比较。给出了全新世早期和中期的暂定海岸位移曲线。

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