by | Oct 16, 2023 | vol27

Corrigendum to “Inferred pyrite growth via the particle attachment pathway in the presence of trace metals” by Domingos et al., 2023

J.M. Domingos1,

1Sedimentology & Organic Geochemistry, Center for Applied Geosciences, University of Tuebingen, 72076 Tuebingen, Germany

E. Runge1,

1Sedimentology & Organic Geochemistry, Center for Applied Geosciences, University of Tuebingen, 72076 Tuebingen, Germany

C. Dreher2,

2Geomicrobiology, Center for Applied Geosciences, University of Tuebingen, 72076 Tuebingen, Germany

T.-H. Chiu2,

2Geomicrobiology, Center for Applied Geosciences, University of Tuebingen, 72076 Tuebingen, Germany

J. Shuster3,

3Tuebingen Structural Microscopy Core Facility, University of Tuebingen, 72076 Tuebingen, Germany

S. Fischer3,

3Tuebingen Structural Microscopy Core Facility, University of Tuebingen, 72076 Tuebingen, Germany

A. Kappler2,4,

2Geomicrobiology, Center for Applied Geosciences, University of Tuebingen, 72076 Tuebingen, Germany
4Cluster of Excellence: EXC 2124: Controlling Microbes to Fight Infection, 72076 Tuebingen, Germany

J.-P. Duda1,

1Sedimentology & Organic Geochemistry, Center for Applied Geosciences, University of Tuebingen, 72076 Tuebingen, Germany

J. Xu5,6,

5NanoGeoBio, Department of Geological Sciences, The University of Texas at El Paso, TX 79968, El Paso, USA
6School of Molecular Sciences, Arizona State University, 85278, Tempe, USA

M. Mansor2,5

2Geomicrobiology, Center for Applied Geosciences, University of Tuebingen, 72076 Tuebingen, Germany
5NanoGeoBio, Department of Geological Sciences, The University of Texas at El Paso, TX 79968, El Paso, USA

Affiliations | Corresponding Author | Cite as

Geochemical Perspectives Letters v27 | https://doi.org/10.7185/geochemlet.2318cor
Received 28 September 2023 | Accepted 3 October 2023 | Published 18 October 2023

Copyright © 2023 The Authors

Published by the European Association of Geochemistry
under Creative Commons License CC BY-NC-ND 4.0

 

top

Corrigendum

Corrigendum | Correction to Elemental Sulphur Concentrations | Fe Sulphide Transformation Sequence | Original article

Correction to: Geochemical Perspectives Letters 26, 14-19, doi: 10.7185/geochemlet.2318cor, published 9 June 2023.


top

Correction to Elemental Sulphur Concentrations

Corrigendum | Correction to Elemental Sulphur Concentrations | Fe Sulphide Transformation Sequence | Original article


The concentration of elemental sulphur used in the experiments was incorrectly reported as “30 mM elemental sulphur” instead of “10 mM elemental sulphur”, due to an error in calculation and converting between mg to mM (see the Fe Sulphide Transformation Sequence section in the main article, also the Methods, Pyrite synthesis section and Table S-1 in the Supplementary Information). The corrected text is shown below. The corrected Supplementary Information is also available for download.

top

Fe Sulphide Transformation Sequence

Corrigendum | Correction to Elemental Sulphur Concentrations | Fe Sulphide Transformation Sequence | Original article


Iron sulphides were synthesised in the presence of 3 mM Fe2+, 6 mM Na2S and 10 mM elemental sulphur (S0) in 50 mM HEPES buffer (pH 7). Two sets of experiments were performed and termed Set-1 (97 % N2, 3 % H2 headspace) and Set-2 (100 % N2), respectively (details in SI Methods, Table S-1).

In the first paragraph of ‘Pyrite synthesis’ (Methods) in the Supplementary Information, the reagents were incorrectly written to include “30 mM S0 ” instead of “10 mM S0” in the following sentence, now corrected:

“The final mixture contained approximately 3 mM Fe, 6 mM Na2S, 10 mM S0 and either 30 μM (high-metal) or 30 nM trace metals (low-metal experiments).”

In Table S-1 the cells describing the synthesis conditions for “This study” on pages 7-9 have also been corrected to give 10 mM S0.
top