Microbial Survival Strategies In Ancient Permafrost: Insights From Metagenomics

In permafrost (perennially frozen ground) microbes survive oligotrophic conditions, sub-zero temperatures, low water availability and high salinity over millennia. Viable life exists in permafrost tens of thousands of years old but we know little about the metabolic and physiological adaptations to...

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Published in:The ISME Journal
Main Authors: Mackelprang, Rachel, Burkert, Alexander, Haw, Monica, Mahendrarajah, Tara, Conaway, Christopher H, Douglas, Thomas A, Waldrop, Mark P
Format: Article in Journal/Newspaper
Language:English
Published: Natural Publishing Group 2017
Subjects:
Online Access:http://hdl.handle.net/10211.3/204654
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record_format openpolar
spelling ftcalifstateuniv:oai:dspace.calstate.edu:10211.3/204654 2023-05-15T17:55:52+02:00 Microbial Survival Strategies In Ancient Permafrost: Insights From Metagenomics Mackelprang, Rachel Burkert, Alexander Haw, Monica Mahendrarajah, Tara Conaway, Christopher H Douglas, Thomas A Waldrop, Mark P 2017 http://hdl.handle.net/10211.3/204654 en eng Natural Publishing Group International Society for Microbial Ecology doi.org/10.1038/ismej.2017.93 The ISME Journal 11, 2305-2318. (2017) 1751-7362 http://hdl.handle.net/10211.3/204654 Bacteria Freezing Metagenomics Microbial Viability Permafrost Phylogeny Salinity Temperature Article 2017 ftcalifstateuniv https://doi.org/10.1038/ismej.2017.93 2022-04-13T11:41:11Z In permafrost (perennially frozen ground) microbes survive oligotrophic conditions, sub-zero temperatures, low water availability and high salinity over millennia. Viable life exists in permafrost tens of thousands of years old but we know little about the metabolic and physiological adaptations to the challenges presented by life in frozen ground over geologic time. In this study we asked whether increasing age and the associated stressors drive adaptive changes in community composition and function. We conducted deep metagenomic and 16 S rRNA gene sequencing across a Pleistocene permafrost chronosequence from 19 to 33 years before present (kyr). We found that age markedly affected community composition and reduced diversity. Reconstruction of paleovegetation from metagenomic sequence suggests vegetation differences in the paleo record are not responsible for shifts in community composition and function. Rather, we observed shifts consistent with long-term survival strategies in extreme cryogenic environments. These include increased reliance on scavenging detrital biomass, horizontal gene transfer, chemotaxis, dormancy, environmental sensing and stress response. Our results identify traits that may enable survival in ancient cryoenvironments with no influx of energy or new materials. Article in Journal/Newspaper permafrost California State University (CSU): DSpace The ISME Journal 11 10 2305 2318
institution Open Polar
collection California State University (CSU): DSpace
op_collection_id ftcalifstateuniv
language English
topic Bacteria
Freezing
Metagenomics
Microbial Viability
Permafrost
Phylogeny
Salinity
Temperature
spellingShingle Bacteria
Freezing
Metagenomics
Microbial Viability
Permafrost
Phylogeny
Salinity
Temperature
Mackelprang, Rachel
Burkert, Alexander
Haw, Monica
Mahendrarajah, Tara
Conaway, Christopher H
Douglas, Thomas A
Waldrop, Mark P
Microbial Survival Strategies In Ancient Permafrost: Insights From Metagenomics
topic_facet Bacteria
Freezing
Metagenomics
Microbial Viability
Permafrost
Phylogeny
Salinity
Temperature
description In permafrost (perennially frozen ground) microbes survive oligotrophic conditions, sub-zero temperatures, low water availability and high salinity over millennia. Viable life exists in permafrost tens of thousands of years old but we know little about the metabolic and physiological adaptations to the challenges presented by life in frozen ground over geologic time. In this study we asked whether increasing age and the associated stressors drive adaptive changes in community composition and function. We conducted deep metagenomic and 16 S rRNA gene sequencing across a Pleistocene permafrost chronosequence from 19 to 33 years before present (kyr). We found that age markedly affected community composition and reduced diversity. Reconstruction of paleovegetation from metagenomic sequence suggests vegetation differences in the paleo record are not responsible for shifts in community composition and function. Rather, we observed shifts consistent with long-term survival strategies in extreme cryogenic environments. These include increased reliance on scavenging detrital biomass, horizontal gene transfer, chemotaxis, dormancy, environmental sensing and stress response. Our results identify traits that may enable survival in ancient cryoenvironments with no influx of energy or new materials.
format Article in Journal/Newspaper
author Mackelprang, Rachel
Burkert, Alexander
Haw, Monica
Mahendrarajah, Tara
Conaway, Christopher H
Douglas, Thomas A
Waldrop, Mark P
author_facet Mackelprang, Rachel
Burkert, Alexander
Haw, Monica
Mahendrarajah, Tara
Conaway, Christopher H
Douglas, Thomas A
Waldrop, Mark P
author_sort Mackelprang, Rachel
title Microbial Survival Strategies In Ancient Permafrost: Insights From Metagenomics
title_short Microbial Survival Strategies In Ancient Permafrost: Insights From Metagenomics
title_full Microbial Survival Strategies In Ancient Permafrost: Insights From Metagenomics
title_fullStr Microbial Survival Strategies In Ancient Permafrost: Insights From Metagenomics
title_full_unstemmed Microbial Survival Strategies In Ancient Permafrost: Insights From Metagenomics
title_sort microbial survival strategies in ancient permafrost: insights from metagenomics
publisher Natural Publishing Group
publishDate 2017
url http://hdl.handle.net/10211.3/204654
genre permafrost
genre_facet permafrost
op_relation doi.org/10.1038/ismej.2017.93
The ISME Journal 11, 2305-2318. (2017)
1751-7362
http://hdl.handle.net/10211.3/204654
op_doi https://doi.org/10.1038/ismej.2017.93
container_title The ISME Journal
container_volume 11
container_issue 10
container_start_page 2305
op_container_end_page 2318
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