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. 2024 Jan 2;15:179. doi: 10.1038/s41467-023-43960-2

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© The Author(s) 2024

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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 5 — a A map of the Taupō Volcanic Zone (TVZ), with geothermal fields where Venenivibrio 16S rRNA genes were detected highlighted in yellow. Geothermal fields are scaled in size according to average relative abundance of Venenivibrio-assigned sequencing reads across spring communities in each field, with the number of springs containing Venenivibrio displayed in brackets. b The proportion of the 20 most abundant Venenivibrio 16S rRNA gene operational taxonomic units (OTUs) per geothermal field are displayed in colour, where 100% equals the total relative abundance of Venenivibrio reads within each field. Geothermal fields are ordered north to south. A breakdown of this relative abundance in reads per spring can be found in Fig. S5. Map data ©2022 Google.