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Direct terrestrial–marine correlation demonstrates surprisingly late onset of the last interglacial in central Europe
Quaternary Research ( IF 1.7 ) Pub Date : 2010-12-09 , DOI: 10.1016/j.yqres.2010.11.003
Mark J Sier 1 , Wil Roebroeks 2 , Corrie C Bakels 2 , Mark J Dekkers 3 , Enrico Brühl 4 , Dimitri De Loecker 2 , Sabine Gaudzinski-Windheuser 5 , Norbert Hesse 6 , Adam Jagich 2 , Lutz Kindler 7 , Wim J Kuijper 2 , Thomas Laurat 4 , Herman J Mücher 8 , Kirsty E H Penkman 9 , Daniel Richter 10 , Douwe J J van Hinsbergen 11
Affiliation  

An interdisciplinary study of a small sedimentary basin at Neumark Nord 2 (NN2), Germany, has yielded a high-resolution record of the palaeomagnetic Blake Event, which we are able to place at the early part of the last interglacial pollen sequence documented from the same section. We use this data to calculate the duration of this stratigraphically important event at 3400 ± 350 yr. More importantly, the Neumark Nord 2 data enables precise terrestrial–marine correlation for the Eemian stage in central Europe. This shows a remarkably large time lag of ca. 5000 yr between the MIS 5e ‘peak’ in the marine record and the start of the last interglacial in this region.

中文翻译:

直接的陆地-海洋相关性表明,中欧最后一次间冰期出现的时间出人意料地晚

一项对德国诺伊马克北 2 (NN2) 小型沉积盆地的跨学科研究产生了古地磁布莱克事件的高分辨率记录,我们能够将其放置在上一次间冰期花粉序列的早期部分。同一节。我们使用这些数据来计算这个具有重要地层意义的事件在 3400 ± 350 年的持续时间。更重要的是,Neumark Nord 2 数据为中欧 Eemian 阶段提供了精确的陆地-海洋相关性。这显示了一个非常大的时间滞后。海洋记录中的 MIS 5e“峰值”与该地区最后一次间冰期开始之间的 5000 年。
更新日期:2010-12-09
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