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The shifting of buffer crop repertoires in pre-industrial north-eastern Europe.

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Peer-reviewed

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Authors

Abdrakhmanov, Meiirzhan  ORCID logo  https://orcid.org/0009-0000-0722-2747

Abstract

This study explores how major climatic shifts, together with socioeconomic factors over the past two millennia, influenced buffer crop selection, focusing on five crops: rye, millet, buckwheat, oat, and hemp. For this study, we analyzed archaeobotanical data from 135 archaeological contexts and historical data from 242 manor inventories across the northeastern Baltic region, spanning the period from 100 to 1800 AD. Our findings revealed that rye remained a main staple crop throughout the studied periods reflecting environmental adaptation to northern latitudes. The drought-tolerant and thermophilic millet crop exhibited resilience during the adverse dry climatic conditions of the Medieval Climatic Anomaly while showing a significant decline during the Little Ice Age. During the period of post-1500 AD, a significant shift towards cold-resilient summer crops such as buckwheat and hemp is recorded. This study enhances our understanding of how historical agricultural systems responded to both socioeconomic factors and climatic change in northern latitudes, offering notable potential solutions for modern agricultural practices in the face of future climate variability trends.

Description

Acknowledgements: This research was funded by the European Union with a Consolidator Grant awarded to Giedre Motuzaite Matuzeviciute (ERC-CoG, MILWAYS, 101087964). Views and opinions expressed are those of the authors only and do not necessarily reflect those of the European Union or the European Research Council Executive Agency. Neither the European Union nor the granting authority can be held responsible for them. We appreciate the very constructive and insightful comments of two anonymous reviewers. We are also grateful to National Museum of Lithuania for providing access to archaeobotanical collections and for allowing to conduct AMS dating on some of the plant remains. We would like to thank Dr. Krystof Pleskot for providing chironomid inferred temperature data from the northern Polish site of Lake Spore for our climatic comparison. MK’s research at Basel and Cambridge is financed by the Swiss National Science Foundation (SNSF/SNF) and his project EXOCHAINS - Exploring Holocene Climate Change and Human Innovations across Eurasia, Grant number TMPFP2_217358.

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Sci Rep

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Journal ISSN

2045-2322
2045-2322

Volume Title

15

Publisher

Springer Science and Business Media LLC

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Except where otherwised noted, this item's license is described as http://creativecommons.org/licenses/by/4.0/
Sponsorship
the European Research Council Executive Agency, European Union (ERC-CoG, MILWAYS, 101087964)