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Recognition of the Minoan tephra in the Acigöl Basin, western Turkey: implications for inter‐archive correlations and fine ash dispersal

Identifieur interne : 000364 ( Istex/Corpus ); précédent : 000363; suivant : 000365

Recognition of the Minoan tephra in the Acigöl Basin, western Turkey: implications for inter‐archive correlations and fine ash dispersal

Auteurs : R. Sulpizio ; M. C. Alçiçek ; G. Zanchetta ; L. Solari

Source :

RBID : ISTEX:2EAC6FCB660158BF61F79B4EF9B4D0166910C2E2

English descriptors

Abstract

Here we report the recognition of the Minoan tephra layer in the Acigöl Basin (western Turkey), which represents the most eastward occurrence of this tephra on land and the first in continental deposits out of lacustrine sediments in mainland Turkey. The correlation is supported by glass and mineral geochemistry, which includes solution and laser‐ablation ICP‐MS data for trace and rare earth elements. Thickness and grain size data allow the extension of already described occurrences to an area of about 359 000 km2, from the eastern Mediterranean to Black Sea throughout central–western Turkey. Coupling dispersal area and grain‐size data suggests the joint influence of high and low atmosphere dynamics in dispersal of fine ash during volcanic eruptions. The thickness and lateral continuity of the Minoan tephra in the Acigöl Basin testifies to the widespread impact on the Late Bronze Age environment of mainland Turkey of this important ash deposit. Copyright © 2013 John Wiley & Sons, Ltd.

Url:
DOI: 10.1002/jqs.2630

Links to Exploration step

ISTEX:2EAC6FCB660158BF61F79B4EF9B4D0166910C2E2

Le document en format XML

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<p>Here we report the recognition of the Minoan tephra layer in the Acigöl Basin (western Turkey), which represents the most eastward occurrence of this tephra on land and the first in continental deposits out of lacustrine sediments in mainland Turkey. The correlation is supported by glass and mineral geochemistry, which includes solution and laser‐ablation ICP‐MS data for trace and rare earth elements. Thickness and grain size data allow the extension of already described occurrences to an area of about 359 000 km
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, from the eastern Mediterranean to Black Sea throughout central–western Turkey. Coupling dispersal area and grain‐size data suggests the joint influence of high and low atmosphere dynamics in dispersal of fine ash during volcanic eruptions. The thickness and lateral continuity of the Minoan tephra in the Acigöl Basin testifies to the widespread impact on the Late Bronze Age environment of mainland Turkey of this important ash deposit. Copyright © 2013 John Wiley & Sons, Ltd.</p>
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Details of the analytical methods.</p>
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Comparison of the EDS device used in this study with WDS microprobes from GeoForschungsZentrum, Germany and from Saclay, France.</p>
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EDS analyses of the T1 tephra layer sampled at sites AC1 and AC2.</p>
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EDS analyses of mineral phases from the T1 tephra.</p>
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ICP‐MS trace element data of the T1 tephra sampled at site AC1.</p>
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ICP‐MS REE data of the T1 tephra sampled at site AC1.</p>
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Single grain LAICP‐MS trace element data of the T1 tephra sampled at site AC1.</p>
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Single grain LAICP‐MS REE data of the T1 tephra sampled at site AC1.</p>
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<p>Here we report the recognition of the Minoan tephra layer in the Acigöl Basin (western Turkey), which represents the most eastward occurrence of this tephra on land and the first in continental deposits out of lacustrine sediments in mainland Turkey. The correlation is supported by glass and mineral geochemistry, which includes solution and laser‐ablation ICP‐MS data for trace and rare earth elements. Thickness and grain size data allow the extension of already described occurrences to an area of about 359 000 km
<sup>2</sup>
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<abstract lang="en">Here we report the recognition of the Minoan tephra layer in the Acigöl Basin (western Turkey), which represents the most eastward occurrence of this tephra on land and the first in continental deposits out of lacustrine sediments in mainland Turkey. The correlation is supported by glass and mineral geochemistry, which includes solution and laser‐ablation ICP‐MS data for trace and rare earth elements. Thickness and grain size data allow the extension of already described occurrences to an area of about 359 000 km2, from the eastern Mediterranean to Black Sea throughout central–western Turkey. Coupling dispersal area and grain‐size data suggests the joint influence of high and low atmosphere dynamics in dispersal of fine ash during volcanic eruptions. The thickness and lateral continuity of the Minoan tephra in the Acigöl Basin testifies to the widespread impact on the Late Bronze Age environment of mainland Turkey of this important ash deposit. Copyright © 2013 John Wiley & Sons, Ltd.</abstract>
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