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. 2017 Aug 21;7:8987. doi: 10.1038/s41598-017-09344-5

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© The Author(s) 2017

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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Aragonite growth normal to calcification interface. Inverse pole figure (IPF) map of the crystallization lamella highlighted in Fig. 2, along with aragonite [001] pole figures corresponding to the sectors delimited by dashed lines. Projection and contouring parameters as in Figs 4 and 5, except that the Gaussian half-width has been set to 20° to avoid non-representative peaks in sectors with poor statistics (i.e. small n). The orientation of the calcification interface is indicated by black lines. R and L are shown only for the pole figure at the top centre. IPF map colour code as in Fig. 2.