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Icelandic volcanic ash from the Late-glacial open-air archaeological site of Ahrenshoft LA 58 D, North Germany

机译:来自德国北部Ahrenshoft LA 58 D的晚冰川露天考古现场的冰岛火山灰

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Cryptotephra of Icelandic origin from the open-air archaeological site of Ahrensh?ft LA 58 D(Kr. Nordfriesland, Schleswig-Holstein), northern Germany overlies a Late-glacial Havelte lithic assemblage,hitherto dated by ~(14)C and biostratigraphy to the earliest part of the Late-glacial interstadial (GI-1eto GI-1c_3). Peaks in ash shards are observed in two profiles. Major and minor element geochemistryindicates volcanic ash originating in the Katla system. Precise correlation to previously described tephrais uncertain due to overlapping chemical characteristics. The Ahrenshft ~(14)C determinations, litho- andbio-stratigraphy encompass a broad age-span for the cryptotephra bearing sediments, from the end ofthe Aller?d to the Preboreal. The most plausible volcanic eruption correlates are the Vedde Ash(wYounger Dryas), already known from the European mainland, tephra AF555 (late Younger Dryas) andthe Suduroy tephra (wPreboreal/Boreal), hitherto recorded only in the North Atlantic region. These threeash horizons have been dated to, respectively, 12,171 57 yr b2k in the NGRIP ice-core, c.11,500 cal BP, inScotland and c.8000 cal BP, by radiocarbon from the Faroe Isles. Ongoing research on deposits from thetype sites for the tephra layers may in the future differentiate these markers leading to betterdiscrimination of the chemistries and a resolution of this question.
机译:冰岛的隐球藻起源于德国北部的Ahrensh?ft LA 58 D(Kr。Nordfriesland,石勒苏益格-荷尔斯泰因州)的露天考古现场,其上覆有晚冰川的哈维德石器组合,迄今可追溯到〜(14)C和生物地层晚冰川间期的最早部分(GI-1eto GI-1c_3)。在两个轮廓中观察到了碎屑的峰值。主要和次要元素地球化学指示源自卡特勒系统的火山灰。由于重叠的化学特征,与之前描述的特非莱不明原因的精确相关性。 Ahrenshft〜(14)C的测定,岩石和生物地层学涵盖了从Aller?d到Preboreal的含隐孢子岩沉积物的较宽年龄范围。可能与火山喷发有关的最合理的是欧洲大陆已知的Vedde Ash(wYounger Dryas),tephra AF555(Younger Dryas晚期)和Suduroy tephra(wPreboreal / Boreal),迄今为止仅在北大西洋地区记录。在法罗群岛的放射性碳中,这三个灰烬层位在NGRIP冰芯,约11,500 cal BP(苏格兰)和约8000 cal BP中分别可追溯到12,171 57 y b2k。正在进行的对特发拉层典型位点沉积物的研究将来可能会区分这些标记物,从而更好地区分化学物质并解决这个问题。

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