Correction to “The Stonesphere in Agricultural Soils: A Microhabitat Associated With Rock Fragments Bridging Rock and Soil”

The caption for Figure 2 is incorrect.The correct caption for Figure 2 is: Relationships between chemical weathering and element mobility, OM accumulation and the production of noncrystalline Fe-(hydr)oxides pointing towards the evolution of a microhabitat in weathered rocks and soils.(a) Physical accumulation of heavy minerals and element depletion through chemical weathering as indicated by Zr concentrations and Ba:Nb ratios.(b) Fe o concentrations and 13 C values indicate an enrichment in noncrystalline Fe-(hydr)oxides with increasing OM content.Typical 13 C ranges for CaCO 3 and OM-sourced carbon (C3 plants) are inserted (Hoefs 2009).Variations in 13 C and mass transfer coefficients ( Zr ) depict the fractional loss of Fe (c) and Si (d) with increasing OM content and turnover rates.We apologize for this error.

Publication Details

Journal
European Journal of Soil Science
Published
2025-02-28
DOI
https://doi.org/10.1111/ejss.70066
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

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article

Correction to “The Stonesphere in Agricultural Soils: A Microhabitat Associated With Rock Fragments Bridging Rock and Soil”

European Journal of Soil Science
Geology and Paleoclimatology Research
article

Correction to “The Stonesphere in Agricultural Soils: A Microhabitat Associated With Rock Fragments Bridging Rock and Soil”

article en

Abstract

The caption for Figure 2 is incorrect.The correct caption for Figure 2 is: Relationships between chemical weathering and element mobility, OM accumulation and the production of noncrystalline Fe-(hydr)oxides pointing towards the evolution of a microhabitat in weathered rocks and soils.(a) Physical accumulation of heavy minerals and element depletion through chemical weathering as indicated by Zr concentrations and Ba:Nb ratios.(b) Fe o concentrations and 13 C values indicate an enrichment in noncrystalline Fe-(hydr)oxides with increasing OM content.Typical 13 C ranges for CaCO 3 and OM-sourced carbon (C3 plants) are inserted (Hoefs 2009).Variations in 13 C and mass transfer coefficients ( Zr ) depict the fractional loss of Fe (c) and Si (d) with increasing OM content and turnover rates.We apologize for this error.

European Journal of Soil ScienceVol. 76(2)
European Commission
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Geology and Paleoclimatology Research
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