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CORRECTION article

Front. Microbiol., 29 January 2021
Sec. Biology of Archaea
Volume 12 - 2021 | https://doi.org/10.3389/fmicb.2021.633015
This article is part of the Research Topic Archaea in the Environment: Views on Archaeal Distribution, Activity, and Biogeography View all 10 articles

Corrigendum: High Representation of Archaea Across All Depths in Oxic and Low-pH Sediment Layers Underlying an Acidic Stream

This article is a correction to:

  1. High Representation of Archaea Across All Depths in Oxic and Low-pH Sediment Layers Underlying an Acidic Stream

    1. Read original article
\nMarco A. Distaso,&#x;Marco A. Distaso1,2†Rafael Bargiela&#x;Rafael Bargiela1†Francesca L. Brailsford,,Francesca L. Brailsford1,2,3Gwion B. Williams,Gwion B. Williams1,2Samuel Wright,Samuel Wright1,2Evgenii A. LunevEvgenii A. Lunev4Stepan V. ToshchakovStepan V. Toshchakov5Michail M. YakimovMichail M. Yakimov6David L. Jones,,David L. Jones1,2,3Peter N. Golyshin,Peter N. Golyshin1,2Olga V. Golyshina, Olga V. Golyshina1,2*
  • 1School of Natural Sciences, Bangor University, Bangor, United Kingdom
  • 2Centre for Environmental Biotechnology, Bangor University, Bangor, United Kingdom
  • 3School of Agriculture and Environment, The University of Western Australia, Perth, WA, Australia
  • 4Institute of Living Systems, Immanuel Kant Baltic Federal University, Kaliningrad, Russia
  • 5National Research Centre “Kurchatov Institute”, Moscow, Russia
  • 6Institute for Biological Resources and Marine Biotechnology, CNR, Messina, Italy

A Corrigendum on
High Representation of Archaea Across All Depths in Oxic and Low-pH Sediment Layers Underlying an Acidic Stream

by Distaso, M. A., Bargiela, R., Brailsford, F. L., Williams, G. B., Wright, S., Lunev, E. A., et al. (2020). Front. Microbiol. 11:576520. doi: 10.3389/fmicb.2020.576520

In the original article, there was a mistake. The incorrect Figure 1 was published. The caption is correct as published. The correct Figure 1 appears below.

FIGURE 1
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Figure 1. PCA including all chemical parameters analysis by principal components analysis (PCA) of the influence of all chemical properties measured on the three cores. Contribution of each variable (chemical properties) to this graphical representation is shown by a color key from medium gray (less contribution) to violet (highest contribution). Ellipses and open dots represent the variance and mean for each core, respectively. Anion concentrations are showing the highest percentages of contribution due to the higher figures on these values for measured on layer 1.3.2, which is disrupting the variance (ellipse) corresponding to Core 1.

The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.

Keywords: acidophilic archaea and bacteria, Thermoplasmatales, “Candidatus Micrarchaeota”, unclassified Euryarchaeota/Terrestrial Miscellaneous Euryarchaeotal Group, acid mine drainage systems, mine-impacted environments, sediment microbiome

Citation: Distaso MA, Bargiela R, Brailsford FL, Williams GB, Wright S, Lunev EA, Toshchakov SV, Yakimov MM, Jones DL, Golyshin PN and Golyshina OV (2021) Corrigendum: High Representation of Archaea Across All Depths in Oxic and Low-pH Sediment Layers Underlying an Acidic Stream. Front. Microbiol. 12:633015. doi: 10.3389/fmicb.2021.633015

Received: 24 November 2020; Accepted: 08 January 2021;
Published: 29 January 2021.

Edited and reviewed by: Ricardo Amils, Autonomous University of Madrid, Spain

Copyright © 2021 Distaso, Bargiela, Brailsford, Williams, Wright, Lunev, Toshchakov, Yakimov, Jones, Golyshin and Golyshina. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Olga V. Golyshina, o.golyshina@bangor.ac.uk

†These authors have contributed equally to this work

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