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. 2021 Oct 12;11:20603. doi: 10.1038/s41598-021-00215-8

Author Correction: Iron oxides and aluminous clays selectively control soil carbon storage and stability in the humid tropics

Maximilian Kirsten 1,, Robert Mikutta 2, Cordula Vogel 1, Aaron Thompson 3, Carsten W Mueller 4, Didas N Kimaro 5, Huig L T Bergsma 6, Karl-Heinz Feger 1, Karsten Kalbitz 1
PMCID: PMC8511147  PMID: 34642374

Correction to: Scientific Reports 10.1038/s41598-021-84777-7, published online 03 March 2021

The original version of this Article contained errors in Figure 3, where the bar showing the mineralogical combination of “high clay-low Fe (0-10 cm)” was incorrectly given.

The original Figure 3 and accompanying legend appear below.

Figure 3.

Figure 3

Bulk OC stocks related to soil density fractions (fLF and oLF = free and occluded light fraction; HF = heavy fraction) in mineralogical combinations under forest and cropland separated by soil depth. Sample numbers for the combinations are as follows: ‛low clay‒low Fe’ under forest (n = 4), ‛low clay‒high Fe’ under forest (n = 4), ‛high clay‒low Fe’ under forest (n = 3), ‛high clay‒high Fe’ under forest (n = 7); all cropland combinations (n = 3).

The original Article has been corrected.


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