In recent years, light isotope analysis in sediments has been used to reconstruct climatic variations in continental contexts. The aim of this study is to verify the usefulness of this analytical methodology in archaeological deposits, especially in the absence of other proxies. Sediments from different contexts (fluvial, colluvial and cave-fill), from the Pleistocene and Holocene, were analysed, in order to have better stratigraphic and chronological control, and were collected from sites with archaeological evidence. The results are compared with the best-known marine isotope data.
ANÁLISE ISOTÓPICA ESTÁVEL (δ13C) EM SEDIMENTOS DE SÍTIOS ARQUEOLÓGICOS
Virginia Lattao
Primo
Project Administration
;Elena MarrocchinoMembro del Collaboration Group
;Pierluigi Rosina
Membro del Collaboration Group
;Carmela VaccaroUltimo
Membro del Collaboration Group
2023
Abstract
In recent years, light isotope analysis in sediments has been used to reconstruct climatic variations in continental contexts. The aim of this study is to verify the usefulness of this analytical methodology in archaeological deposits, especially in the absence of other proxies. Sediments from different contexts (fluvial, colluvial and cave-fill), from the Pleistocene and Holocene, were analysed, in order to have better stratigraphic and chronological control, and were collected from sites with archaeological evidence. The results are compared with the best-known marine isotope data.File in questo prodotto:
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