山岳地帯における土壌侵食が3800年前から農牧活動により加速(Soil erosion in mountain environments accelerated by agro-pastoral activities for 3,800 years)

2025-07-14 フランス国立科学研究センター(CNRS)

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CNRSの研究で、アルプス山岳地帯の土壌侵食が過去3,800年間に農牧業の影響で自然の4~10倍に加速していたことが判明。湖底堆積物のリチウム同位体分析とDNA解析により、植生変化や家畜放牧・森林伐採の影響が特定された。高地では早期に放牧による影響が顕在化し、山麓ではローマ期以降に農耕技術の普及で侵食が拡大。本研究は土壌保全や気候・生態系への影響理解に重要な科学的基盤を提供する。

<関連情報>

青銅器時代以降のヨーロッパアルプスにおける侵食速度の人為的な拡大 Human-triggered magnification of erosion rates in European Alps since the Bronze Age

William Rapuc,Charline Giguet-Covex,Julien Bouchez,Pierre Sabatier,Jérôme Gaillardet,Kévin Jacq,Kim Genuite,Jérôme Poulenard,Erwan Messager & Fabien Arnaud
Nature Communications  Published:10 February 2024
DOI:https://doi.org/10.1038/s41467-024-45123-3

山岳地帯における土壌侵食が3800年前から農牧活動により加速(Soil erosion in mountain environments accelerated by agro-pastoral activities for 3,800 years)

Abstract

A major feature of the Anthropocene is the drastic increase in global soil erosion. Soil erosion is threatening Earth habitability not only as soils are an essential component of the Earth system but also because societies depend on soils. However, proper quantification of the impact of human activities on erosion over thousands of years is still lacking. This is particularly crucial in mountainous areas, where the highest erosion rates are recorded. Here we use the Lake Bourget catchment, one of the largest in the European Alps, to estimate quantitatively the impact of human activities on erosion. Based on a multi-proxy, source-to-sink approach relying on isotopic geochemistry, we discriminate the effects of climate fluctuations from those of human activities on erosion over the last 10,000 years. We demonstrate that until 3800 years ago, climate is the only driver of erosion. From that time on, climate alone cannot explain the measured rates of erosion. Thanks to an unprecedented regional paleoenvironmental reconstruction, we highlight that the development of pastoralism at high altitudes from the Bronze Age onwards and the extension of agriculture starting in the Middle Ages were key factors in the drastic increase in erosion observed in the Alps.

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