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. 2021 Jul 14;12:4311. doi: 10.1038/s41467-021-24533-7

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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. 2 — Solubility is reported as a function of pressure and temperature in water or aqueous solutions of different ionic strength: a present data, b literature data. Only studies at pressures of 1 GPa or more are included. Full symbols indicate upper limits for solubility. The solid line represents a solubility line for dolomite at 400 °C in 1 m NaCl aqueous solution. Since no magnesite crystals dissolved, the dashed line represents an upper solubility limit for magnesite at 400 °C. All solubility lines are guides to the eye. Error bars shown for our data represent estimated standard deviation. Note the log scale.