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. 2023 Jan 19;1(1):60–73. doi: 10.1038/s44221-022-00001-4

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© The Author(s) 2023

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. 4 — a–b, Triple tracer correlations between V, He and archaeal eDNA contributed by YLA114 + WCHD3-30 (a) and by YLA114 only (b). c, Triple tracer correlation between V, He and the alpha diversity of Archaea. d, Triple tracer correlation between V, Na⁺ and the alpha diversity of Archaea (d). He concentrations represent measurements taken on site with the new portable GE-MIMS instrument. STP, standard temperature and pressure (T = 0 °C, P = 1 atm). H′_A is Shannon’s diversity index^160,168 evaluated for Archaea. Data for Fujinishiki in d represent data from Fujinishiki brewery well (site id: F1), except for the Na⁺ concentration, which represents the average measured Na⁺ concentration in Fujinishiki spring (site id: 7) located next to the Fujinishiki brewery well.