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. 2018 Jun 6;12(9):2129–2141. doi: 10.1038/s41396-018-0176-z

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© International Society for Microbial Ecology 2018

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 — Potential aerobic respiration of soils from different depths in control and decadal in situ deep-thaw plots during laboratory incubation at 11 °C, measured for 1 week after 1 month pre-incubation, expressed per gram soil dry weight (a) and per gram soil organic matter (b); samples to the right of the dotted line are from permanently frozen soil layers; means ± SE (n = 6). Asterisks denote significant effects (*P < 0.05; ***P < 0.001; n.s. non significant), letters denote significant differences between depths