An archaeobotanical and stable isotope approach to changing agricultural practices in the NW Mediterranean region around 4000 BC

Author:

Antolín Ferran12ORCID,Jacomet Stefanie2,Soteras Raül1,Gerling Claudia23,Bernasconi Stefano M4,Follmann Franziska15,Hajdas Irka6,Jaggi Madalina4,Jesus Ana2ORCID,Martínez-Grau Héctor2,Oms Francesc Xavier78,Röder Brigitte3,Steiner Bigna L2,van Willigen Samuel9

Affiliation:

1. German Archaeological Institute, Natural Sciences Unit, Germany

2. Department of Environmental Sciences, Integrative Prehistory and Archaeological Science (IPAS), Basel University, Switzerland

3. Departement Altertumswissenschaften, Ur- und Frühgeschichtliche und Provinzialrömische Archäologie, Basel University, Switzerland

4. Department of Earth Sciences, Geological Institute, ETH Zurich, Switzerland

5. Institut für Prähistorische Archäologie, Freie Universität Berlin, Germany

6. Laboratory of Ion Beam Physics (LIP), Swiss Federal Institute of Technology (ETH) Zurich, Switzerland

7. Seminari d’Estudis i Recerques Prehistòriques (SERP). Secció de Prehistòria i Arqueologia, Dept. d’Història i Arqueologia, Facultat de Geografia i Història. Universitat de Barcelona, Spain

8. Institut d’Arqueologia de la Universitat de Barcelona. Facultat de Geografia i Història. Universitat de Barcelona, Spain

9. InSitu Archéologie, Switzerland

Abstract

It has recently been observed, that a change in the crop spectrum happened during the so-called Middle Neolithic in France at ca. 4000 BC. An agricultural system based on free-threshing cereals (naked wheat and naked barley) seems to shift to one based on glume wheats. This is a major change for traditional farmers and this paper aims to shed light on its possible causes. Here we describe the results of new investigations in a key area for the understanding of this process: the NW Mediterranean arch, where free-threshing cereals are the main cultivars since ca. 5100 BC. New data confirm that the shift towards glume wheats is also observed in some sites of the NE of the Iberian Peninsula and that among the glume wheats that spread at ca. 4000 BC we should not only consider emmer and einkorn but also Timopheevi’s wheat. Stable isotope analyses indicate no major decrease in soil fertility or alterations in local precipitation regimes. The agricultural change may be the result of a combination of the spread of damaging pests for free-threshing cereals and presumably new networks being developed with the North-eastern part of Italy and the Balkans.

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

SAGE Publications

Subject

Paleontology,Earth-Surface Processes,Ecology,Archeology,Global and Planetary Change

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