Weathering and soil production under trees growing on sandstones – The role of tree roots in soil formation

Rock weathering drives both landform formation and soil production/evolution. The less studied biological component of weathering and soil production caused by tree root systems is the main focus of the present study. Weathering by trees, which likely has been important in soil formation since the f...

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Published in:The Science of the total environment 2023-12, Vol.902, p.166002-166002, Article 166002
Main Authors: Pawlik, Łukasz, Gruba, Piotr, Gałązka, Anna, Marzec-Grządziel, Anna, Kupka, Dawid, Szopa, Krzysztof, Buma, Brian, Šamonil, Pavel
Format: Article
Language:English
Subjects:
Bioweathering
Carpathians
Microbial biodiversity
Soil evolution
Sudety
Tree roots
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Summary:Rock weathering drives both landform formation and soil production/evolution. The less studied biological component of weathering and soil production caused by tree root systems is the main focus of the present study. Weathering by trees, which likely has been important in soil formation since the first trees emerged in the middle and late Devonian, is accomplished through both physical and biological means, like acids excreted by plants and exudates from associated bacterial communities. However, these processes are relatively poorly known. We assessed the impact of tree roots and associated microbiota on the potential level of biological weathering. Three research plots were selected in two sandstone regions in Poland. Two plots were in the Stołowe Mountains (Złotno, Batorów), a tableland built of Cretaceous sandstones. The third plot (Żegiestów) was in the Sącz Beskidy Mountains, the Carpathians. Soil samples were taken from tree root zones of Norway spruces from predefined sampling positions. Soils from non-tree control positions were also sampled. Soil samples were a subject of laboratory analyses which included the content of Fe and Al (amorphous and labile forms), carbon (C), nitrogen (N), and soil pH. The microbial functional diversity of soil microorganisms was determined using the Biolog (EcoPlate) system. Rock fragments were collected for mineralogical and a subject of optical microscopy and cathodoluminescence analyses in order to examine their mineralogical composition. Significant differences (pHolm-corrected 
ISSN:0048-9697
1879-1026
DOI:10.1016/j.scitotenv.2023.166002