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A Holocene relative sea-level database for the Baltic Sea

机译:波罗的海的全新世相对海平数据库

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摘要

We present a compilation and analysis of 1099 Holocene relative shore-level (RSL) indicators located around the Baltic Sea including 867 relative sea-level data points and 232 data points from the Ancylus Lake and the following transitional phase. The spatial distribution covers the Baltic Sea and near-coastal areas fairly well, but some gaps remain mainly in Sweden. RSL data follow the standardized HOLSEA format and, thus, are ready for spatially comprehensive applications in, e.g., glacial isostatic adjustment (GIA) modelling. We apply a SQL database system to store the nationally provided data sets in their individual form and to map the different input into the HOLSEA format as the information content of the individual data sets from the Baltic Sea area differs. About 80% of the RSL data is related to the last marine stage in Baltic Sea history after 8.5 ka BP (thousand years before present). These samples are grouped according to their dominant RSL tendencies into three clusters: regions with negative, positive and complex (transitional) RSL tendencies. Overall, regions with isostatic uplift driven negative tendencies dominate and show regression in the Baltic Sea basin during the last marine stage. Shifts from positive to negative tendencies in RSL data from transitional regions show a mid-Holocene high-stand around 7.5-6.5 ka BP which is consistent with the end of the final melting of the Laurentide Ice Sheet. Comparisons of RSL data with GIA predictions including global ICE-5G and ICE-6G-C ice histories show good fit with RSL data from the regions with negative tendencies, whereas in the transitional areas in the eastern Baltic, predictions for the mid-Holocene clearly overestimate the RSL and fail to recover the mid-Holocene RSL highstand derived from the proxy reconstructions. These results motivate improvements of ice-sheet and Earth-structure models and show the potential and benefits of the new compilation for future studies.
机译:我们展示了位于波罗的海围绕波罗的海的1099个相对岸线(RSL)指示器的汇编和分析,包括867个相对海平数据点和来自ancylus湖的232个数据点和以下过渡阶段。空间分布覆盖了波罗的海和近沿海地地区,但一些差距主要是瑞典。 RSL数据遵循标准化的HOLSEA格式,因此,准备好用于空间综合应用,例如冰川等静态调整(GIA)建模。我们应用一个SQL数据库系统以将全国提供的数据集存储在各个形式,并将不同的输入映射到HOLSEA格式,因为来自波罗的海区域的各个数据集的信息内容不同。 80%的RSL数据与波罗的海历史上的最后一个海洋舞台有关,在8.5 ka BP(在场前千年)。这些样品根据其显性RSL倾向分组为三簇:具有负,阳性和复杂(过渡)RSL趋势的区域。总体而言,具有异位隆起的地区在最后的海洋阶段在波罗的海盆地中占据主导地位和显示回归。从过渡地区的RSL数据中从阳性到负倾向的变化显示,中全新世高级高于7.5-6.5 kA BP,这与LauRentide冰盖的最终熔化结束一致。与GIA预测的RSL数据的比较,包括全球ICE-5G和ICE-6G-C型凝固历史表现出与带有负面倾向的地区的RSL数据良好,而在东部波罗的海的过渡区,清楚地区的中东后的预测高估RSL并无法恢复从代理重建导出的中间全新世rsl高价。这些结果激发了冰纸和地球结构模型的改进,并显示了未来研究新汇编的潜力和益处。

著录项

  • 来源
    《Oceanographic Literature Review》 |2021年第9期|1886-1886|共1页
  • 作者单位

    Institute of Ecology and Earth Sciences University of Tartu Tartu 51014 Estonia;

    Institute of Ecology and Earth Sciences University of Tartu Tartu 51014 Estonia;

    Institute of Ecology and Earth Sciences University of Tartu Tartu 51014 Estonia;

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  • 正文语种 eng
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  • 入库时间 2022-08-19 03:07:53

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