A long-lived Anatolian archaeological site (Arslantepe, Malatya plain) was investigated under a palaeoclimate perspective. Identified plant charred macroremains underwent an isotopic analysis to determine carbon isotope composition. The results obtained are used to assess the degree of climate changes in the site and its surroundings.

Carbon isotope composition of archaeobotanical remains for the palaeoclimatic reconstruction

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2011

Abstract

A long-lived Anatolian archaeological site (Arslantepe, Malatya plain) was investigated under a palaeoclimate perspective. Identified plant charred macroremains underwent an isotopic analysis to determine carbon isotope composition. The results obtained are used to assess the degree of climate changes in the site and its surroundings.
2011
Istituto di Geoscienze e Georisorse - IGG - Sede Pisa
plant macroremains; isotopes; archaeological site; climate change
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/448849
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