Correction to: Nature Geoscience https://doi.org/10.1038/s41561-023-01234-y, published online 31 July 2023.
In the version of the article originally published, a reference was missing from the seventh paragraph of the “A global shift towards enhanced clay formation” section and the first paragraph of the “Further information on the successful model Scenario 8” section (in the latter instance, the reference is cited in the added text “although a global reorganisation of the silicon cycle may have also played a part”). The reference—Dunlea, A. G. et al. Cenozoic global cooling and increased seawater Mg/Ca via reduced reverse weathering. Nat. Commun. 8, 844 (2017)—has now been inserted as new ref. 54. In the “Data treatment and availability section”, the isotopic data, which can be found in the Figshare data repository at https://doi.org/10.5522/04/23749197, were incorrectly said to be found in the PANGAEA data repository. These corrections have been made in the HTML and PDF versions of the article.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
About this article
Cite this article
Krause, A.J., Sluijs, A., van der Ploeg, R. et al. Publisher Correction: Enhanced clay formation key in sustaining the Middle Eocene Climatic Optimum. Nat. Geosci. (2023). https://doi.org/10.1038/s41561-023-01280-6
Published:
DOI: https://doi.org/10.1038/s41561-023-01280-6
