CARBON ISOTOPE COMPOSITION OF ARCHAEOBOTANICAL REMAINS FOR THE PALAEOCLIMATIC RECONSTRUCTION

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Published: Jan 14, 2011
DOI: https://doi.org/10.26382/
Keywords:
plant macroremains, isotopes, archaeological site, climate change

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Alessia Masi
Dipartimento di Biologia Ambientale - Università “Sapienza”, Roma
Ilaria Baneschi
Istituto di Geoscienze e Georisorse – CNR, Pisa
Laura Sadori
Dipartimento di Biologia Ambientale - Università “Sapienza”, Roma
Giovanni Zanchetta
Dipartimento di Scienze della Terra - Università di Pisa, Pisa

Abstract

Masi A. et al., Carbon isotope composition of archaeobotanical remains for the palaeoclimatic reconstruction (IT ISSN 0394-3356, 2011) 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. 

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How to Cite
Masi, Alessia, Ilaria Baneschi, Laura Sadori, and Giovanni Zanchetta , trans. 2011. “CARBON ISOTOPE COMPOSITION OF ARCHAEOBOTANICAL REMAINS FOR THE PALAEOCLIMATIC RECONSTRUCTION”. Alpine and Mediterranean Quaternary 24 (Extended Abstract): 215-16. https://doi.org/10.26382/.
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Vol. 24 No. Extended Abstract (2011): IL QUATERNARIO
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Articles
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How to Cite

Masi, Alessia, Ilaria Baneschi, Laura Sadori, and Giovanni Zanchetta , trans. 2011. “CARBON ISOTOPE COMPOSITION OF ARCHAEOBOTANICAL REMAINS FOR THE PALAEOCLIMATIC RECONSTRUCTION”. Alpine and Mediterranean Quaternary 24 (Extended Abstract): 215-16. https://doi.org/10.26382/.