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Geoarchaeology reveals development of terrace farming in the northern Apennines during the Medieval Climate Anomaly

Lookup NU author(s): Dr Filippo Brandolini, Dr Tim Kinnaird, Professor Sam Turner

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This work is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0).


Abstract

This study employs Optically Stimulated Luminescence Profiling and Dating (OSL-PD) to address the challenge of synchronizing social changes with natural events, a significant limitation in existing studies on the resilience and vulnerability of pre-modern societies to ecological stress. By uncovering the construction dates of terrace farming systems in the northern Apennines region, the research reveals a distinct temporal framework, indicating that the establishment of agricultural terraces predominantly occurred during the 11th to 13th centuries CE. This crucial time frame aligns directly with complex socio-economic factors, including the encastellation process, alongside the climatic shifts characterising the Medieval Climate Anomaly. Isotopic fractionation of the Total Organic Carbon confirms that different agricultural choices were made in coincidence with the establishment of terrace farming. The resultant historical rural landscape underwent continuous enhancements in the centuries that followed. Notably, the main phases of (re)construction correspond to the coldest periods of the Little Ice Age, offering new insights into the historical interactions between human activities and the environment during the Late Holocene in the area.


Publication metadata

Author(s): Brandolini F, Kinnaird T, Srivastava A, Costanzo S, Compostella C, Turner S

Publication type: Article

Publication status: Published

Journal: Scientific Reports

Year: 2025

Volume: 15

Online publication date: 10/07/2025

Acceptance date: 20/06/2025

Date deposited: 11/07/2025

ISSN (electronic): 2045-2322

Publisher: Nature Publishing Group

URL: https://doi.org/10.1038/s41598-025-08396-2

DOI: 10.1038/s41598-025-08396-2

Data Access Statement: The results of the geochronological analysis are available as supplementary materials attached to this paper


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Funding

Funder referenceFunder name
AH/T000104/1Arts & Humanities Research Board-AHRB (now AHRC)
the Italian Min- istry of Education, University, and Research (MIUR) through the ‘Dipartimenti di Eccellenza 2023–2027’ award
the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 890561

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