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

Xiaolei Sun; Wulf Amelung; Erwin Klumpp; Janek Walk; Ramona Mörchen; Christoph Böhm; Ghazal Moradi; Simon Matthias May; Federica Tamburini; Ye Wang; Roland Bol

doi:10.1111/gcb.17068

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

Xiaolei Sun
, Wulf Amelung
, Erwin Klumpp
, Janek Walk
, Ramona Mörchen
, Christoph Böhm
, Ghazal Moradi
, Simon Matthias May
, Federica Tamburini
, Ye Wang
, Roland Bol

Ysgol Gwyddorau Amgylcheddol a Naturiol

Forschungszentrum Jülich GmbH
University of Vienna
Rheinische Friedrich-Wilhelms University, Bonn
University of Cologne
ETH Zürich

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

40 Wedi eu Llwytho i Lawr (Pure)

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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 (

Iaith wreiddiol	Saesneg
Tudalennau (o-i)	e17068
Cyfnodolyn	Global Change Biology
Cyfrol	30
Rhif cyhoeddi	1
Dyddiad ar-lein cynnar	8 Rhag 2023
Dynodwyr Gwrthrych Digidol (DOIs)	https://doi.org/10.1111/gcb.17068
Statws	Cyhoeddwyd - 1 Ion 2024

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10.1111/gcb.17068Trwydded: CC BY-NC-ND

Global Change Biology - 2023 - Sun - Fog controls biological cycling of soil phosphorus in the Coastal Cordillera of theFersiwn derfynol wedi’i chyhoeddi, 25.2 MBTrwydded: CC BY-NC-ND

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title = "Fog controls biological cycling of soil phosphorus in the Coastal Cordillera of the Atacama Desert",

abstract = "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",

author = "Xiaolei Sun and Wulf Amelung and Erwin Klumpp and Janek Walk and Ramona M{\"o}rchen and Christoph B{\"o}hm and Ghazal Moradi and May, \{Simon Matthias\} and Federica Tamburini and Ye Wang and Roland Bol",

year = "2024",

month = jan,

day = "1",

doi = "10.1111/gcb.17068",

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T1 - Fog controls biological cycling of soil phosphorus in the Coastal Cordillera of the Atacama Desert

AU - Sun, Xiaolei

AU - Amelung, Wulf

AU - Klumpp, Erwin

AU - Walk, Janek

AU - Mörchen, Ramona

AU - Böhm, Christoph

AU - Moradi, Ghazal

AU - May, Simon Matthias

AU - Tamburini, Federica

AU - Wang, Ye

AU - Bol, Roland

PY - 2024/1/1

Y1 - 2024/1/1

N2 - 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 (

AB - 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 (

KW - Atacama Desert

KW - fog

KW - hyper-aridity

KW - oxygen isotopes ratio in phosphates

KW - soil P cycle

U2 - 10.1111/gcb.17068

DO - 10.1111/gcb.17068

M3 - Article

SN - 1354-1013

VL - 30

SP - e17068

JO - Global Change Biology

JF - Global Change Biology

IS - 1

ER -

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

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