首页> 外文期刊>Journal of quaternary science: JQS >Holocene tephra horizons at Klocka Bog, west-central Sweden: aspects of reproducibility in subarctic peat deposits
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Holocene tephra horizons at Klocka Bog, west-central Sweden: aspects of reproducibility in subarctic peat deposits

机译:瑞典中西部Klocka沼泽的全新世Tephra地层:弧下泥炭沉积物的可再现性方面

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This paper presents one of the most extensive Holocene tephra records found to date in Scandinavia. Microtephra horizons originating from Icelandic eruptions were recorded in two ca. 2 m thick peat profiles at Klocka Bog in west-central Sweden. Five of the microtephra horizons were geochemically correlated to the Askja-1875, Hekla-3, Kebister, Hekla-4 and Lairg A tephras respectively. Radiocarbon-based dating of these tephras broadly agree with previously published ages from Iceland, Sweden, Germany and the British Isles. The identification of the Lairg A tephra demonstrates a more widespread distribution than previously thought, extending the usefulness of Icelandic Holocene tephrochronology further north into west-central Scandinavia. Long-lasting snow cover and seasonal wind distribution in the lower stratosphere are suggested as factors that may be responsible for fragmentary tephra deposition patterns in peat deposits of subarctic Scandinavia.
机译:本文介绍了迄今为止在斯堪的纳维亚半岛发现的最广泛的全新世特非拉记录之一。在大约两个月的时间里,记录了源自冰岛喷发的微尘暴层位。瑞典中西部Klocka沼泽的2 m厚泥炭轮廓。在地球化学上,有5个微触角层分别与Askja-1875,Hekla-3,Kebister,Hekla-4和Lairg A特菲拉斯相关。这些以特弗拉为基础的放射性碳测年法与冰岛,瑞典,德国和不列颠群岛先前发表的年龄基本一致。对Lairg A tephra的识别显示出比以前认为的更为广泛的分布,从而将冰岛全新世年代学向北延伸到斯堪的纳维亚半岛的中西部。建议在平流层下部长期积雪和季节性风向分布,作为可能导致斯堪的纳维亚半岛南北泥炭沉积中的分段性特非拉沉积模式的因素。

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