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. 2022 Nov 29;12:20118. doi: 10.1038/s41598-022-24206-5

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© The Author(s) 2022

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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Locations and types of mat samples used for this study. (a) Map of the Lake Fryxell Basin in Taylor Valley, Antarctica with exact sampling sites (white squares) along streams (red lines: 1. Canada Stream, 2. Bowles Creek, 3. Delta Stream, 4. Von Guerard Stream). Blue lines indicate other streams not included in this study. Types of mats included in this study: (b) black type and (c) orange type with orange type showing regrowth 12 months post sampling. Photo credit: Josh Darling and Mike Gooseff. Map was created with ArcGIS Desktop 10.8.2 (http://www.esri.com).