Deep microbial proliferation at the basalt interface in 33.5–104 million-year-old oceanic crust
The upper oceanic crust is mainly composed of basaltic lava that constitutes one of the largest habitable zones on Earth. However, the nature of deep microbial life in oceanic crust remains poorly understood, especially where old cold basaltic rock interacts with seawater beneath sediment. Here we s...
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| Veröffentlicht in: | Communications biology 2020-04, Vol.3 (1), p.136-136, Article 136 |
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| creator | Suzuki, Yohey Yamashita, Seiya Kouduka, Mariko Ao, Yutaro Mukai, Hiroki Mitsunobu, Satoshi Kagi, Hiroyuki D’Hondt, Steven Inagaki, Fumio Morono, Yuki Hoshino, Tatsuhiko Tomioka, Naotaka Ito, Motoo |
| description | The upper oceanic crust is mainly composed of basaltic lava that constitutes one of the largest habitable zones on Earth. However, the nature of deep microbial life in oceanic crust remains poorly understood, especially where old cold basaltic rock interacts with seawater beneath sediment. Here we show that microbial cells are densely concentrated in Fe-rich smectite on fracture surfaces and veins in 33.5- and 104-million-year-old (Ma) subseafloor basaltic rock. The Fe-rich smectite is locally enriched in organic carbon. Nanoscale solid characterizations reveal the organic carbon to be microbial cells within the Fe-rich smectite, with cell densities locally exceeding 10
10
cells/cm
3
. Dominance of heterotrophic bacteria indicated by analyses of DNA sequences and lipids supports the importance of organic matter as carbon and energy sources in subseafloor basalt. Given the prominence of basaltic lava on Earth and Mars, microbial life could be habitable where subsurface basaltic rocks interact with liquid water.
Yohey Suzuki, Seiya Yamashita et al. discover the presence of bacterial cells in the iron-rich smectite on aged subseafloor basaltic rock using nanoscale solid characterizations. Analysis of their lipid profiles and DNA sequences reveals the dominance of heterotrophic bacteria, suggesting the presence of organic matter resources in the subsea basalt. |
| doi_str_mv | 10.1038/s42003-020-0860-1 |
| format | Article |
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10
cells/cm
3
. Dominance of heterotrophic bacteria indicated by analyses of DNA sequences and lipids supports the importance of organic matter as carbon and energy sources in subseafloor basalt. Given the prominence of basaltic lava on Earth and Mars, microbial life could be habitable where subsurface basaltic rocks interact with liquid water.
Yohey Suzuki, Seiya Yamashita et al. discover the presence of bacterial cells in the iron-rich smectite on aged subseafloor basaltic rock using nanoscale solid characterizations. Analysis of their lipid profiles and DNA sequences reveals the dominance of heterotrophic bacteria, suggesting the presence of organic matter resources in the subsea basalt.</description><identifier>ISSN: 2399-3642</identifier><identifier>EISSN: 2399-3642</identifier><identifier>DOI: 10.1038/s42003-020-0860-1</identifier><identifier>PMID: 32242062</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>13 ; 14 ; 14/34 ; 45 ; 45/22 ; 45/23 ; 631/158/47/4113 ; 631/1647/245/2225 ; 631/326/171/1818 ; Biology ; Biomedical and Life Sciences ; Carbon ; Carbon sources ; Deoxyribonucleic acid ; DNA ; Dominance ; Heterotrophic bacteria ; Lava ; Life Sciences ; Lipids ; Nucleotide sequence ; Organic carbon ; Organic matter</subject><ispartof>Communications biology, 2020-04, Vol.3 (1), p.136-136, Article 136</ispartof><rights>The Author(s) 2020</rights><rights>The Author(s) 2020. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c536t-efc1bb785cdbdd6cfefb6daf863514fd1b72e06ecb37b028175ffa461c25c45c3</citedby><cites>FETCH-LOGICAL-c536t-efc1bb785cdbdd6cfefb6daf863514fd1b72e06ecb37b028175ffa461c25c45c3</cites><orcidid>0000-0002-8713-9368 ; 0000-0001-5686-0243 ; 0000-0001-8928-4254 ; 0000-0003-2887-6525 ; 0000-0001-5725-9513 ; 0000-0001-9915-1148</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC7118141/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC7118141/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,864,885,27924,27925,41120,42189,51576,53791,53793</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/32242062$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Suzuki, Yohey</creatorcontrib><creatorcontrib>Yamashita, Seiya</creatorcontrib><creatorcontrib>Kouduka, Mariko</creatorcontrib><creatorcontrib>Ao, Yutaro</creatorcontrib><creatorcontrib>Mukai, Hiroki</creatorcontrib><creatorcontrib>Mitsunobu, Satoshi</creatorcontrib><creatorcontrib>Kagi, Hiroyuki</creatorcontrib><creatorcontrib>D’Hondt, Steven</creatorcontrib><creatorcontrib>Inagaki, Fumio</creatorcontrib><creatorcontrib>Morono, Yuki</creatorcontrib><creatorcontrib>Hoshino, Tatsuhiko</creatorcontrib><creatorcontrib>Tomioka, Naotaka</creatorcontrib><creatorcontrib>Ito, Motoo</creatorcontrib><title>Deep microbial proliferation at the basalt interface in 33.5–104 million-year-old oceanic crust</title><title>Communications biology</title><addtitle>Commun Biol</addtitle><addtitle>Commun Biol</addtitle><description>The upper oceanic crust is mainly composed of basaltic lava that constitutes one of the largest habitable zones on Earth. However, the nature of deep microbial life in oceanic crust remains poorly understood, especially where old cold basaltic rock interacts with seawater beneath sediment. Here we show that microbial cells are densely concentrated in Fe-rich smectite on fracture surfaces and veins in 33.5- and 104-million-year-old (Ma) subseafloor basaltic rock. The Fe-rich smectite is locally enriched in organic carbon. Nanoscale solid characterizations reveal the organic carbon to be microbial cells within the Fe-rich smectite, with cell densities locally exceeding 10
10
cells/cm
3
. Dominance of heterotrophic bacteria indicated by analyses of DNA sequences and lipids supports the importance of organic matter as carbon and energy sources in subseafloor basalt. Given the prominence of basaltic lava on Earth and Mars, microbial life could be habitable where subsurface basaltic rocks interact with liquid water.
Yohey Suzuki, Seiya Yamashita et al. discover the presence of bacterial cells in the iron-rich smectite on aged subseafloor basaltic rock using nanoscale solid characterizations. 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10
cells/cm
3
. Dominance of heterotrophic bacteria indicated by analyses of DNA sequences and lipids supports the importance of organic matter as carbon and energy sources in subseafloor basalt. Given the prominence of basaltic lava on Earth and Mars, microbial life could be habitable where subsurface basaltic rocks interact with liquid water.
Yohey Suzuki, Seiya Yamashita et al. discover the presence of bacterial cells in the iron-rich smectite on aged subseafloor basaltic rock using nanoscale solid characterizations. Analysis of their lipid profiles and DNA sequences reveals the dominance of heterotrophic bacteria, suggesting the presence of organic matter resources in the subsea basalt.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><pmid>32242062</pmid><doi>10.1038/s42003-020-0860-1</doi><tpages>1</tpages><orcidid>https://orcid.org/0000-0002-8713-9368</orcidid><orcidid>https://orcid.org/0000-0001-5686-0243</orcidid><orcidid>https://orcid.org/0000-0001-8928-4254</orcidid><orcidid>https://orcid.org/0000-0003-2887-6525</orcidid><orcidid>https://orcid.org/0000-0001-5725-9513</orcidid><orcidid>https://orcid.org/0000-0001-9915-1148</orcidid><oa>free_for_read</oa></addata></record> |
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| subjects | 13 14 14/34 45 45/22 45/23 631/158/47/4113 631/1647/245/2225 631/326/171/1818 Biology Biomedical and Life Sciences Carbon Carbon sources Deoxyribonucleic acid DNA Dominance Heterotrophic bacteria Lava Life Sciences Lipids Nucleotide sequence Organic carbon Organic matter |
| title | Deep microbial proliferation at the basalt interface in 33.5–104 million-year-old oceanic crust |
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