Cosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano

The assessment of soil sustainability in prehistoric times requires comparing millennium-scale erosion rates with geological background rates. Here, the authors apply in situ cosmogenic 14C, 10Be, and 26Al to reveal rapid soil erosion on the Andean Altiplano in response to Late Holocene climate chan...

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Autores principales: Kristina Hippe, John D. Jansen, Daniel Søndergaard Skov, Maarten Lupker, Susan Ivy-Ochs, Florian Kober, Gerold Zeilinger, José Mariano Capriles, Marcus Christl, Colin Maden, Christof Vockenhuber, David Lundbek Egholm
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Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/8f0d25383aa849ae936acef1ada210b7
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spelling oai:doaj.org-article:8f0d25383aa849ae936acef1ada210b72021-12-02T14:49:41ZCosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano10.1038/s41467-021-22825-62041-1723https://doaj.org/article/8f0d25383aa849ae936acef1ada210b72021-05-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-22825-6https://doaj.org/toc/2041-1723The assessment of soil sustainability in prehistoric times requires comparing millennium-scale erosion rates with geological background rates. Here, the authors apply in situ cosmogenic 14C, 10Be, and 26Al to reveal rapid soil erosion on the Andean Altiplano in response to Late Holocene climate change and the onset of agropastoralism.Kristina HippeJohn D. JansenDaniel Søndergaard SkovMaarten LupkerSusan Ivy-OchsFlorian KoberGerold ZeilingerJosé Mariano CaprilesMarcus ChristlColin MadenChristof VockenhuberDavid Lundbek EgholmNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-9 (2021)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Kristina Hippe
John D. Jansen
Daniel Søndergaard Skov
Maarten Lupker
Susan Ivy-Ochs
Florian Kober
Gerold Zeilinger
José Mariano Capriles
Marcus Christl
Colin Maden
Christof Vockenhuber
David Lundbek Egholm
Cosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano
description The assessment of soil sustainability in prehistoric times requires comparing millennium-scale erosion rates with geological background rates. Here, the authors apply in situ cosmogenic 14C, 10Be, and 26Al to reveal rapid soil erosion on the Andean Altiplano in response to Late Holocene climate change and the onset of agropastoralism.
format article
author Kristina Hippe
John D. Jansen
Daniel Søndergaard Skov
Maarten Lupker
Susan Ivy-Ochs
Florian Kober
Gerold Zeilinger
José Mariano Capriles
Marcus Christl
Colin Maden
Christof Vockenhuber
David Lundbek Egholm
author_facet Kristina Hippe
John D. Jansen
Daniel Søndergaard Skov
Maarten Lupker
Susan Ivy-Ochs
Florian Kober
Gerold Zeilinger
José Mariano Capriles
Marcus Christl
Colin Maden
Christof Vockenhuber
David Lundbek Egholm
author_sort Kristina Hippe
title Cosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano
title_short Cosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano
title_full Cosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano
title_fullStr Cosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano
title_full_unstemmed Cosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano
title_sort cosmogenic in situ 14c-10be reveals abrupt late holocene soil loss in the andean altiplano
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/8f0d25383aa849ae936acef1ada210b7
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