Fog controls biological cycling of soil phosphorus in the Coastal Cordillera of the Atacama Desert

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  • Xiaolei Sun
    Forschungszentrum Jülich GmbH
  • Wulf Amelung
    Forschungszentrum Jülich GmbH
  • Erwin Klumpp
    Forschungszentrum Jülich GmbH
  • Janek Walk
    University of Vienna
  • Ramona Mörchen
    Rheinische Friedrich-Wilhelms University, Bonn
  • Christoph Böhm
    University of Cologne
  • Ghazal Moradi
    Forschungszentrum Jülich GmbH
  • Simon Matthias May
    University of Cologne
  • Federica Tamburini
    ETH Zürich
  • Ye Wang
    Rheinische Friedrich-Wilhelms University, Bonn
  • Roland Bol
Abstract Soils in hyper-arid climates, such as the Chilean Atacama Desert, show indications of past and present forms of life despite extreme water limitations. We hypothesize that fog plays a key role in sustaining life. In particular, we assume that fog water is incorporated into soil nutrient cycles, with the inland limit of fog penetration corresponding to the threshold for biological cycling of soil phosphorus (P). We collected topsoil samples (0?10?cm) from each of 54 subsites, including sites in direct adjacency (

Keywords

  • Atacama Desert, fog, hyper-aridity, oxygen isotopes ratio in phosphates, soil P cycle
Original languageEnglish
Pages (from-to)e17068
JournalGlobal Change Biology
Volume30
Issue number1
Early online date8 Dec 2023
DOIs
Publication statusPublished - 1 Jan 2024
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