Human and climate impacts on the alpine Critical Zone over the past 10,000 y
成果类型:
Article
署名作者:
Rapuc, William; Guinoiseau, Damien; Arnaud, Fabien; Dellinger, Mathieu; Sabatier, Pierre; Gaillardet, Jerome; Poulenard, Jerome; Bouchez, Julien
署名单位:
Universite Savoie Mont Blanc; Centre National de la Recherche Scientifique (CNRS); Durham University; Centre National de la Recherche Scientifique (CNRS); Universite Paris Cite; Universite Paris Saclay
刊物名称:
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
ISSN/ISSBN:
0027-14998
DOI:
10.1073/pnas.2506030122
发表日期:
2025-07-22
关键词:
lake le-bourget
soil-erosion
french alps
holocene treeline
lithium isotopes
western alps
land-use
DYNAMICS
river
reconstruction
摘要:
Agropastoral activities have impacted the habitable part of our planet-the Critical Zone-for thousands of years, triggering a major increase in soil erosion in mountain environments. Understanding and quantifying the impact of these activities on soil is central to the well-being of our societies. Here, we investigate the isotope ratios of the trace element lithium in detrital sediments of Lake Bourget, European Alps, and provide a reconstruction of the impact of human activities on the evolution of alpine soil during the Holocene. We demonstrate that during the Early Holocene, soil formation was altered by the development of pastoralism followed by tillage. This led to three major erosive surges (3.8 to 3.0, 2.8 to 1.6, and 1.6 ky cal BP to modern times), thinning soils down to a state close to that of their early development 10,000 y ago. The detailed study of the lithium detrital signal reveals the appearance of an altitudinal decoupling in the response of the Critical Zone in the Alps following the development of the agropastoral activities during the Iron Age. The onset of agropastoral activities disrupted the balance between soil formation and erosion, leading to erosion rates 3 to 10 times faster than soil production since the end of the Ice Age.