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. 2021 Nov 2;12:6295. doi: 10.1038/s41467-021-26668-z

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© The Author(s) 2021

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/.

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Fig. 7 — a Average olivine rim δ¹⁸O versus average olivine core δ¹⁸O in the kimberlites (and lamproites) from this study. Error bars are one SD of the mean. The blue line is the linear regression through the data points (excluding the Notre Dâme du Nord outlier). b Covariation diagram showing a broad direct correlation between δ¹⁸O and Mg# in olivine rims from the examined samples. Error bars indicate the 2σ of each analysis.