首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Identification of the Askja-S Tephra in a rare turlough record from Pant-y-Llyn,south Wales
Institution:1. Department of Geography, College of Science, Swansea University, Singleton Park, Abertawe, Cymru SA2 8PP, UK;2. British Geological Survey, Cardiff University, Main Building, Park Place, Caerdydd, Cymru CF10 3AT, UK;3. Natural Resources Wales, Maes Newydd, Britannic Way West, Llandarcy, Neath Port Talbot, Cymru SA10 6JQ, UK;1. Department of Geography, Royal Holloway University of London, Egham, TW20 0EX Surrey, UK;2. W. Szafer Institute of Botany, Polish Academy of Sciences, ul. Lubicz 46, 31-512 Kraków, Poland;3. Institute of Archaeology, University of Wrocław, ul. Szewska 48, 50-139 Wrocław, Poland;4. Research Laboratory for Archaeology and the History of Art, University of Oxford, Dyson Perrins, South Parks Road, Oxford OX1 3QY, UK;5. Faculty of Humanities (Archaeology), Building 65A, Avenue Campus, University of Southampton, Southampton SO17 1BF, UK;6. Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada;1. Research Laboratory for Archaeology, University of Oxford, Dyson Perrins Building, South Parks Road, Oxford, OX1 3QY, UK;2. Department of Geography, Royal Holloway University of London, Egham, Surrey, TW20 0EX, UK;3. Department of Geography, The University of Manchester, Arthur Lewis Building, Oxford Road, Manchester, M13 9PL, UK;1. Research Laboratory for Archaeology and the History of Art, University of Oxford, Dyson Perrins, South Parks Road, Oxford, UK;2. Archaeology, University of Southampton, Avenue Campus, Highfield, Southampton SO17 1BF, UK;1. GFZ German Research Centre for Geosciences, Section 5.2 – Climate Dynamics and Landscape Evolution, Telegrafenberg, D-14473 Potsdam, Germany;2. Senckenberg Research Institute and Natural History Museum, BIK-F, TSP6 Evolution and Climate, Senckenberganlage 25, D-60325 Frankfurt a.M., Germany;3. GFZ German Research Centre for Geosciences, Section 3.3 – Chemistry and Physics of Earth Materials, Telegrafenberg, D-14473 Potsdam, Germany;4. Faculty of Earth Sciences, Institute of Earth Sciences, University of Iceland, Strulugata 7, 101 Reykjavík, Iceland;5. Helmholtz Centre for Ocean Research Kiel, GEOMAR, Wischhofstrasse 1-3, D-24148 Kiel, Germany;6. Polish Academy of Sciences, Institute of Geography and Spatial Organization, Department of Environmental Resources and Geohazards, Kopernika 19, Torun 87-100, Poland;1. Research Laboratory for Archaeology, University of Oxford, Dyson Perrins Building, South Parks Road, Oxford, OX1 3QY, UK;2. Department of Geography, Royal Holloway University of London, Egham, Surrey, TW20 0EX, UK;3. Department of Geography, The University of Manchester, Arthur Lewis Building, Oxford Road, Manchester, M13 9PL, UK;1. Nordic Volcanological Center, Institute of Earth Sciences, University of Iceland, Iceland;2. Institute of Earth Sciences, University of Iceland, Iceland;3. Department of Arctic Geology, The University Center in Svalbard, Svalbard and Jan Mayen;4. Department of Geology, Quaternary Sciences, Lund University, Sweden
Abstract:Tephrochronology and especially crypto-tephrochronology is an established chronological technique employed in a range of depositional environments in Europe and beyond. During the late Quaternary, Icelandic cryptotephra deposits are widely found in palaeorecords across northern latitudes of Europe e.g. Scotland, Ireland, Norway, Sweden and the Faroe Islands but are sporadic in southerly latitudes as distance from Iceland increases. As yet, very few Icelandic cryptotephras have been identified in Wales or southern England which may well reflect the geographical limit of Icelandic tephra distribution. Here, however, we report the discovery of an Icelandic cryptotephra deposit within a sediment sequence retrieved from the Pant-y-Llyn turlough (Carmarthenshire, south Wales), the only known turlough in Britain. Turloughs are groundwater-fed ephemeral lakes associated with limestone bedrock and can accumulate sediments that may yield records suitable for palaeoreconstructions. A discrete peak of glass shards originating from the Askja-S eruption is identified in the sediment record. This discovery extends the distribution of this early Holocene eruption giving new insight into its dispersal patterns and also indicates that sedimentary sequences from sites in these more southerly latitudes are valuable repositories for ash preservation. Furthermore, its discovery within a carbonate-rich sequence provides a minimum age constraint on the timing of sediment accumulation and provides an alternative tool for what is typically a problematic dating environment.
Keywords:Cryptotephra  Askja-S Tephra  Turlough  Tephra dispersal  Radiocarbon dating  Carbonates
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号