Half of the soil erosion in the Alps during the Holocene is explained by transient erosion crises as a consequence of rapid human land clearing
Human land use changes have altered soil erosion for millennia with extensive consequences on terrestrial and aquatic ecosystems as well as on biogeochemical cycles along the land-ocean continuum. Despite their great importance, past erosion trends have high uncertainties limiting quantitative estim...
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Veröffentlicht in: | Holocene (Sevenoaks) 2024-09, Vol.34 (9), p.1290-1303 |
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Sprache: | eng |
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