by | Jun 25, 2024 | vol31

Corrigendum to “Sulfur solubility in a deep magma ocean and implications for the deep sulfur cycle” by Steenstra et al., 2022.

E.S. Steenstra1,2,

1Earth and Planets Laboratory, Carnegie Institution of Science, Washington DC, USA
2Institute of Mineralogy, University of Münster, Germany

O.T. Lord3,

3School of Earth Sciences, University of Bristol, UK

S. Vitale1,

1Earth and Planets Laboratory, Carnegie Institution of Science, Washington DC, USA

E.S. Bullock1,

1Earth and Planets Laboratory, Carnegie Institution of Science, Washington DC, USA

S. Klemme2,

2Institute of Mineralogy, University of Münster, Germany

M. Walter1

1Earth and Planets Laboratory, Carnegie Institution of Science, Washington DC, USA

Affiliations | Corresponding Author | Cite as

Geochemical Perspectives Letters v31 | https://doi.org/10.7185/geochemlet.2219cor
Received 15 May 2024 | Accepted 15 May 2024 | Published 25 June 2024

Copyright © 2024 The Authors

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


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Corrigendum

Corrigendum | Original article

The original version of this article contained an error in the funding acknowledgement. The correct information for the funding acknowledgement should be as follows: E.S.S. was funded through H2020 Marie Skłodowska-Curie Postdoctoral Fellowship 101020611 and by a Carnegie Postdoctoral Fellowship. O.T.L. acknowledges support from the Royal Society in the form of a University Research Fellowship (UF150057).

The authors would like to apologise for any inconvenience caused.

The corresponding text has now been corrected in the PDF and online versions of the original article.
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