Microbial Selection and Survival in Subseafloor Sediment

Many studies have examined relationships of microorganisms to geochemical zones in subseafloor sediment. However, responses to selective pressure and patterns of community succession with sediment depth have rarely been examined. Here we use 16S rDNA sequencing to examine the succession of microbial...

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Published in:Frontiers in Microbiology
Main Authors: John B. Kirkpatrick, Emily A. Walsh, Steven D’Hondt
Format: Article
Language:English
Published: Frontiers Media S.A. 2019-05-01
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fmicb.2019.00956/full
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author John B. Kirkpatrick
John B. Kirkpatrick
Emily A. Walsh
Steven D’Hondt
author_facet John B. Kirkpatrick
John B. Kirkpatrick
Emily A. Walsh
Steven D’Hondt
author_sort John B. Kirkpatrick
collection DOAJ
container_title Frontiers in Microbiology
description Many studies have examined relationships of microorganisms to geochemical zones in subseafloor sediment. However, responses to selective pressure and patterns of community succession with sediment depth have rarely been examined. Here we use 16S rDNA sequencing to examine the succession of microbial communities at sites in the Indian Ocean and the Bering Sea. The sediment ranges in depth from 0.16 to 332 m below seafloor and in age from 660 to 1,300,000 years. The majority of subseafloor taxonomic diversity is present in the shallowest depth sampled. The best predictor of sequence presence or absence in the oldest sediment is relative abundance in the near-seafloor sediment. This relationship suggests that perseverance of specific taxa into deep, old sediment is primarily controlled by the taxonomic abundance that existed when the sediment was near the seafloor. The operational taxonomic units that dominate at depth comprise a subset of the local seafloor community at each site, rather than a grown-in group of geographically widespread subseafloor specialists. At both sites, most taxa classified as abundant decrease in relative frequency with increasing sediment depth and age. Comparison of community composition to cell counts at the Bering Sea site indicates that the rise of the few dominant taxa in the deep subseafloor community does not require net replication, but might simply result from lower mortality relative to competing taxa on the long timescale of community burial.
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spelling doaj-art-e1598cd51b644e04acd5016e6ebacd3d2025-08-19T20:19:40ZengFrontiers Media S.A.Frontiers in Microbiology1664-302X2019-05-011010.3389/fmicb.2019.00956443494Microbial Selection and Survival in Subseafloor SedimentJohn B. Kirkpatrick0John B. Kirkpatrick1Emily A. Walsh2Steven D’Hondt3Graduate School of Oceanography, The University of Rhode Island, Narragansett, RI, United StatesThe Evergreen State College, Olympia, WA, United StatesGraduate School of Oceanography, The University of Rhode Island, Narragansett, RI, United StatesGraduate School of Oceanography, The University of Rhode Island, Narragansett, RI, United StatesMany studies have examined relationships of microorganisms to geochemical zones in subseafloor sediment. However, responses to selective pressure and patterns of community succession with sediment depth have rarely been examined. Here we use 16S rDNA sequencing to examine the succession of microbial communities at sites in the Indian Ocean and the Bering Sea. The sediment ranges in depth from 0.16 to 332 m below seafloor and in age from 660 to 1,300,000 years. The majority of subseafloor taxonomic diversity is present in the shallowest depth sampled. The best predictor of sequence presence or absence in the oldest sediment is relative abundance in the near-seafloor sediment. This relationship suggests that perseverance of specific taxa into deep, old sediment is primarily controlled by the taxonomic abundance that existed when the sediment was near the seafloor. The operational taxonomic units that dominate at depth comprise a subset of the local seafloor community at each site, rather than a grown-in group of geographically widespread subseafloor specialists. At both sites, most taxa classified as abundant decrease in relative frequency with increasing sediment depth and age. Comparison of community composition to cell counts at the Bering Sea site indicates that the rise of the few dominant taxa in the deep subseafloor community does not require net replication, but might simply result from lower mortality relative to competing taxa on the long timescale of community burial.https://www.frontiersin.org/article/10.3389/fmicb.2019.00956/fullmarine sediment bacteriamarine sediment archaeadeep biospheremicrobial selection16S rDNAU1343
spellingShingle John B. Kirkpatrick
John B. Kirkpatrick
Emily A. Walsh
Steven D’Hondt
Microbial Selection and Survival in Subseafloor Sediment
marine sediment bacteria
marine sediment archaea
deep biosphere
microbial selection
16S rDNA
U1343
title Microbial Selection and Survival in Subseafloor Sediment
title_full Microbial Selection and Survival in Subseafloor Sediment
title_fullStr Microbial Selection and Survival in Subseafloor Sediment
title_full_unstemmed Microbial Selection and Survival in Subseafloor Sediment
title_short Microbial Selection and Survival in Subseafloor Sediment
title_sort microbial selection and survival in subseafloor sediment
topic marine sediment bacteria
marine sediment archaea
deep biosphere
microbial selection
16S rDNA
U1343
url https://www.frontiersin.org/article/10.3389/fmicb.2019.00956/full
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