Hidden biofilms in a far northern lake and implications for the changing Arctic

Abstract Shallow lakes are common across the Arctic landscape and their ecosystem productivity is often dominated by benthic, cyanobacterial biofilms. Many of these water bodies freeze to the bottom and are biologically inactive during winter, but full freeze-up is becoming less common with Arctic w...

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Main Authors: Vani Mohit, Alexander Culley, Connie Lovejoy, Frédéric Bouchard, Warwick F. Vincent
Format: Article
Language:English
Published: Nature Publishing Group 2017-07-01
Series:npj Biofilms and Microbiomes
Online Access:https://doi.org/10.1038/s41522-017-0024-3
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spelling doaj-2ada85fc09a84e2fbe1d89cdfbc13da52020-12-08T13:59:50ZengNature Publishing Groupnpj Biofilms and Microbiomes2055-50082017-07-01311410.1038/s41522-017-0024-3Hidden biofilms in a far northern lake and implications for the changing ArcticVani Mohit0Alexander Culley1Connie Lovejoy2Frédéric Bouchard3Warwick F. Vincent4Département de biologie & Centre d’études nordiques (CEN), Université LavalDépartement de biochimie, de microbiologie et de bio-informatique, & Centre d’études nordiques (CEN), Université LavalDépartement de biologie & Centre d’études nordiques (CEN), Université LavalCentre Eau Terre Environnement, Institut national de la recherche scientifique (INRS), Centre d’études nordiques (CEN)Département de biologie & Centre d’études nordiques (CEN), Université LavalAbstract Shallow lakes are common across the Arctic landscape and their ecosystem productivity is often dominated by benthic, cyanobacterial biofilms. Many of these water bodies freeze to the bottom and are biologically inactive during winter, but full freeze-up is becoming less common with Arctic warming. Here we analyzed the microbiome structure of newly discovered biofilms at the deepest site of a perennially ice-covered High Arctic lake as a model of polar microbial communities that remain unfrozen throughout the year. Biofilms were also sampled from the lake’s shallow moat region that melts out and refreezes to the bottom annually. Using high throughput small subunit ribosomal RNA sequencing, we found more taxonomic richness in Bacteria, Archaea and microbial eukaryotes in the perennially unfrozen biofilms compared to moat communities. The deep communities contained both aerobic and anaerobic taxa including denitrifiers, sulfate reducers, and methanogenic Archaea. The water overlying the deep biofilms was well oxygenated in mid-summer but almost devoid of oxygen in spring, indicating anoxia during winter. Seasonally alternating oxic-anoxic regimes may become increasingly widespread in polar biofilms as fewer lakes and ponds freeze to the bottom, favoring prolonged anaerobic metabolism and greenhouse gas production during winter darkness.https://doi.org/10.1038/s41522-017-0024-3
collection DOAJ
language English
format Article
sources DOAJ
author Vani Mohit
Alexander Culley
Connie Lovejoy
Frédéric Bouchard
Warwick F. Vincent
spellingShingle Vani Mohit
Alexander Culley
Connie Lovejoy
Frédéric Bouchard
Warwick F. Vincent
Hidden biofilms in a far northern lake and implications for the changing Arctic
npj Biofilms and Microbiomes
author_facet Vani Mohit
Alexander Culley
Connie Lovejoy
Frédéric Bouchard
Warwick F. Vincent
author_sort Vani Mohit
title Hidden biofilms in a far northern lake and implications for the changing Arctic
title_short Hidden biofilms in a far northern lake and implications for the changing Arctic
title_full Hidden biofilms in a far northern lake and implications for the changing Arctic
title_fullStr Hidden biofilms in a far northern lake and implications for the changing Arctic
title_full_unstemmed Hidden biofilms in a far northern lake and implications for the changing Arctic
title_sort hidden biofilms in a far northern lake and implications for the changing arctic
publisher Nature Publishing Group
series npj Biofilms and Microbiomes
issn 2055-5008
publishDate 2017-07-01
description Abstract Shallow lakes are common across the Arctic landscape and their ecosystem productivity is often dominated by benthic, cyanobacterial biofilms. Many of these water bodies freeze to the bottom and are biologically inactive during winter, but full freeze-up is becoming less common with Arctic warming. Here we analyzed the microbiome structure of newly discovered biofilms at the deepest site of a perennially ice-covered High Arctic lake as a model of polar microbial communities that remain unfrozen throughout the year. Biofilms were also sampled from the lake’s shallow moat region that melts out and refreezes to the bottom annually. Using high throughput small subunit ribosomal RNA sequencing, we found more taxonomic richness in Bacteria, Archaea and microbial eukaryotes in the perennially unfrozen biofilms compared to moat communities. The deep communities contained both aerobic and anaerobic taxa including denitrifiers, sulfate reducers, and methanogenic Archaea. The water overlying the deep biofilms was well oxygenated in mid-summer but almost devoid of oxygen in spring, indicating anoxia during winter. Seasonally alternating oxic-anoxic regimes may become increasingly widespread in polar biofilms as fewer lakes and ponds freeze to the bottom, favoring prolonged anaerobic metabolism and greenhouse gas production during winter darkness.
url https://doi.org/10.1038/s41522-017-0024-3
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