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The Holocene, Vol. 13, No. 2, 277-283 (2003)
DOI: 10.1191/0959683603hl617rr

Rhyolitic tephra horizons in northwestern Europe and Iceland from the AD 700s–800s: a potential alternative for dating first human impact

Stefan Wastegård

Department of Physical Geography and Quaternary Geology, Stockholm University, S-106 91 Stockholm, Sweden; stefan.wastegard{at}geo.su.se

Valerie A. Hall

Palaeoecology Centre and Institute of Irish Studies, Queen's University, Belfast BT7 1NN, Northern Ireland, UK

Gina E. Hannon

Southern Swedish Forest Research Centre, SLU, S-230 53 Alnarp, Sweden

Christel van den Bogaard

GEOMAR, Research Center for Marine Geosciences, Wischhofstrasse 1–3, D-24148 Kiel, Germany

Jonathan R. Pilcher

Palaeoecology Centre and Institute of Irish Studies, Queen's University, Belfast BT7 1NN, Northern Ireland, UK

Magnús Á. Sigurgeirsson

Icelandic Radiation Protection Institute, RauDarárstíg 10, IS-150 Reykjavík, Iceland

Margrét Hermanns-Auoardóttir

The Reykjavík Academy, Hringbraut 121, IS-107 Reykjaviík, Iceland

The distribution and geochemistry of four rhyolitic tephra horizons from Iceland dated to the ad 700s–800s is assessed. These include the rhyolitic phase of the Landnám tephra (ad 870s), the ad 860 layer, a previously unrecorded tephra called the GA4–85 layer (c. ad 700–800) and the Tjïrnuvík tephra (c. ad 800s). The ad 860 and GA4–85 layers were first found in peat bogs in north Ireland. They are here correlated with equivalent horizons on Iceland which were found below the Landnám tephra (c. ad 870s). This time period is considered important in the North Atlantic region, because it coincides with a phase of human settlement in Iceland and the Faroe Islands. The establishment of a detailed tephrochronology may provide a tool for exact dating of sediment successions and sediments associated with archaeological excavations. Caution must be taken especially on Iceland where the Landnám tephra is often used for dating archaeological sites. This investigation show that several rhyolitic tephra horizons occur close in time to the Landnám tephra, and that mistakes can be made if detailed geochemical analyses are not carried out, especially in areas which are distal to the source of the Landnám tephra (the Veidivötn and Torfajökull volcanic systems, southern Iceland).

Key Words: Iceland • Ireland • Faroe Islands • Germany • tephra • Landnám • human impact


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