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. 2020 Jul 13;20:207. doi: 10.1186/s12866-020-01884-7

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© The Author(s) 2020

Open AccessThis 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/. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated in a credit line to the data.

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Fig. 3 — iOTUs retrieved from photic-layer and deep-sea waters. a Venn diagram representing the percentages of the sequences shared between photic and mesopelagic only from vertical profile samples of the station 39. Numbers inside brackets indicate the number of shared iOTUs corresponding to that percentage of sequences. b Venn diagram showing the percentages of the sequences shared between photic, mesopelagic and bathypelagic layers. Numbers inside brackets indicate the number of shared iOTUs corresponding to that percentage of sequences. Numbers displayed in all Venn diagrams are extracted from the rarefied iOTU-abundance tables