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.

Geoarchaeology reveals development of terrace farming in the Northern Apennines during the Medieval Climate Anomaly / F. Brandolini, T.C. Kinnaird, A. Srivastava, S. Costanzo, C. Compostella, S. Turner. - In: SCIENTIFIC REPORTS. - ISSN 2045-2322. - 15:1(2025 Jul 10), pp. 24989.1-24989.19. [10.1038/s41598-025-08396-2]

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

F. Brandolini
Primo
;
S. Costanzo;C. Compostella
Penultimo
;
2025

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.
Anthropogenic Geomorphology; Canossa; Dantean Anomaly; Encastellation; Geochronology; Isotopic analysis; Land-Use change; Landscape Archaeology; Little Ice Age; OSL-PD
Settore GEOS-03/A - Geografia fisica e geomorfologia
   Historic Landscape and Soil Sustainability
   HiLSS
   European Commission
   Horizon 2020 Framework Programme
   890561
10-lug-2025
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/1177675
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