Genomic reconstruction of fossil and living microorganisms in ancient Siberian permafrost.

Adaptive strategy Ancient permafrost Asgard archaea Fossil and living microorganisms Long-term survivability Metagenome-assembled genome

Journal

Microbiome
ISSN: 2049-2618
Titre abrégé: Microbiome
Pays: England
ID NLM: 101615147

Informations de publication

Date de publication:
17 05 2021
Historique:
received: 20 12 2020
accepted: 22 03 2021
entrez: 18 5 2021
pubmed: 19 5 2021
medline: 21 5 2021
Statut: epublish

Résumé

Total DNA (intracellular, iDNA and extracellular, eDNA) from ancient permafrost records the mixed genetic repository of the past and present microbial populations through geological time. Given the exceptional preservation of eDNA under perennial frozen conditions, typical metagenomic sequencing of total DNA precludes the discrimination between fossil and living microorganisms in ancient cryogenic environments. DNA repair protocols were combined with high throughput sequencing (HTS) of separate iDNA and eDNA fraction to reconstruct metagenome-assembled genomes (MAGs) from ancient microbial DNA entrapped in Siberian coastal permafrost. Despite the severe DNA damage in ancient permafrost, the coupling of DNA repair and HTS resulted in a total of 52 MAGs from sediments across a chronosequence (26-120 kyr). These MAGs were compared with those derived from the same samples but without utilizing DNA repair protocols. The MAGs from the youngest stratum showed minimal DNA damage and thus likely originated from viable, active microbial species. Many MAGs from the older and deeper sediment appear related to past aerobic microbial populations that had died upon freezing. MAGs from anaerobic lineages, including Asgard archaea, however exhibited minimal DNA damage and likely represent extant living microorganisms that have become adapted to the cryogenic and anoxic environments. The integration of aspartic acid racemization modeling and metaproteomics further constrained the metabolic status of the living microbial populations. Collectively, combining DNA repair protocols with HTS unveiled the adaptive strategies of microbes to long-term survivability in ancient permafrost. Our results indicated that coupling of DNA repair protocols with simultaneous sequencing of iDNA and eDNA fractions enabled the assembly of MAGs from past and living microorganisms in ancient permafrost. The genomic reconstruction from the past and extant microbial populations expanded our understanding about the microbial successions and biogeochemical alterations from the past paleoenvironment to the present-day frozen state. Furthermore, we provided genomic insights into long-term survival mechanisms of microorganisms under cryogenic conditions through geological time. The combined strategies in this study can be extrapolated to examine other ancient non-permafrost environments and constrain the search for past and extant extraterrestrial life in permafrost and ice deposits on Mars. Video abstract.

Sections du résumé

BACKGROUND
Total DNA (intracellular, iDNA and extracellular, eDNA) from ancient permafrost records the mixed genetic repository of the past and present microbial populations through geological time. Given the exceptional preservation of eDNA under perennial frozen conditions, typical metagenomic sequencing of total DNA precludes the discrimination between fossil and living microorganisms in ancient cryogenic environments. DNA repair protocols were combined with high throughput sequencing (HTS) of separate iDNA and eDNA fraction to reconstruct metagenome-assembled genomes (MAGs) from ancient microbial DNA entrapped in Siberian coastal permafrost.
RESULTS
Despite the severe DNA damage in ancient permafrost, the coupling of DNA repair and HTS resulted in a total of 52 MAGs from sediments across a chronosequence (26-120 kyr). These MAGs were compared with those derived from the same samples but without utilizing DNA repair protocols. The MAGs from the youngest stratum showed minimal DNA damage and thus likely originated from viable, active microbial species. Many MAGs from the older and deeper sediment appear related to past aerobic microbial populations that had died upon freezing. MAGs from anaerobic lineages, including Asgard archaea, however exhibited minimal DNA damage and likely represent extant living microorganisms that have become adapted to the cryogenic and anoxic environments. The integration of aspartic acid racemization modeling and metaproteomics further constrained the metabolic status of the living microbial populations. Collectively, combining DNA repair protocols with HTS unveiled the adaptive strategies of microbes to long-term survivability in ancient permafrost.
CONCLUSIONS
Our results indicated that coupling of DNA repair protocols with simultaneous sequencing of iDNA and eDNA fractions enabled the assembly of MAGs from past and living microorganisms in ancient permafrost. The genomic reconstruction from the past and extant microbial populations expanded our understanding about the microbial successions and biogeochemical alterations from the past paleoenvironment to the present-day frozen state. Furthermore, we provided genomic insights into long-term survival mechanisms of microorganisms under cryogenic conditions through geological time. The combined strategies in this study can be extrapolated to examine other ancient non-permafrost environments and constrain the search for past and extant extraterrestrial life in permafrost and ice deposits on Mars. Video abstract.

Identifiants

pubmed: 34001281
doi: 10.1186/s40168-021-01057-2
pii: 10.1186/s40168-021-01057-2
pmc: PMC8130349
doi:

Types de publication

Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S. Video-Audio Media

Langues

eng

Sous-ensembles de citation

IM

Pagination

110

Subventions

Organisme : National Science Foundation
ID : DEB-1442059
Organisme : National Science Foundation
ID : EAR-1528492
Organisme : National Science Foundation
ID : DEB-1442262
Organisme : National Science Foundation
ID : IIA-1460058
Organisme : U.S. Department of Energy
ID : DE-SC0020369
Organisme : Russian Government Assignment
ID : AAAA-A18-118013190181-6
Organisme : Russian Government Assignment
ID : RFBR 19-29-05003

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Auteurs

Renxing Liang (R)

Princeton University, B88, Guyot Hall, Princeton, NJ, 08544, USA. rliang@princeton.edu.

Zhou Li (Z)

Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, USA.

Maggie C Y Lau Vetter (MCY)

Princeton University, B88, Guyot Hall, Princeton, NJ, 08544, USA.
Present address: Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya, China.

Tatiana A Vishnivetskaya (TA)

University of Tennessee, Knoxville, TN, USA.
Institute of Physicochemical and Biological Problems in Soil Science, Russian Academy of Sciences, Pushchino, Moscow Region, Russia.

Oksana G Zanina (OG)

Institute of Physicochemical and Biological Problems in Soil Science, Russian Academy of Sciences, Pushchino, Moscow Region, Russia.

Karen G Lloyd (KG)

University of Tennessee, Knoxville, TN, USA.

Susan M Pfiffner (SM)

University of Tennessee, Knoxville, TN, USA.

Elizaveta M Rivkina (EM)

Institute of Physicochemical and Biological Problems in Soil Science, Russian Academy of Sciences, Pushchino, Moscow Region, Russia.

Wei Wang (W)

Genomics Core Facility, Princeton University, Princeton, NJ, USA.

Jessica Wiggins (J)

Genomics Core Facility, Princeton University, Princeton, NJ, USA.

Jennifer Miller (J)

Genomics Core Facility, Princeton University, Princeton, NJ, USA.

Robert L Hettich (RL)

Biosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN, USA.

Tullis C Onstott (TC)

Princeton University, B88, Guyot Hall, Princeton, NJ, 08544, USA.

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