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Deep subsurface mine stalactites trap endemic fissure fluid Archaea, Bacteria, and Nematoda possibly originating from ancient seas
Stalactites (CaCO(3) and salt) from water seeps are frequently encountered in ceilings of mine tunnels whenever they intersect water-bearing faults or fractures. To determine whether stalactites could be mineralized traps for indigenous fracture water microorganisms, we analyzed stalactites collecte...
Autores principales: | , , , , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Frontiers Media S.A.
2015
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4585192/ https://www.ncbi.nlm.nih.gov/pubmed/26441844 http://dx.doi.org/10.3389/fmicb.2015.00833 |
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author | Borgonie, Gaëtan Linage-Alvarez, Borja Ojo, Abidemi Shivambu, Steven Kuloyo, Olukayode Cason, Errol D. Maphanga, Sihle Vermeulen, Jan-G Litthauer, Derek Ralston, Colin D. Onstott, Tullis C. Sherwood-Lollar, Barbara Van Heerden, Esta |
author_facet | Borgonie, Gaëtan Linage-Alvarez, Borja Ojo, Abidemi Shivambu, Steven Kuloyo, Olukayode Cason, Errol D. Maphanga, Sihle Vermeulen, Jan-G Litthauer, Derek Ralston, Colin D. Onstott, Tullis C. Sherwood-Lollar, Barbara Van Heerden, Esta |
author_sort | Borgonie, Gaëtan |
collection | PubMed |
description | Stalactites (CaCO(3) and salt) from water seeps are frequently encountered in ceilings of mine tunnels whenever they intersect water-bearing faults or fractures. To determine whether stalactites could be mineralized traps for indigenous fracture water microorganisms, we analyzed stalactites collected from three different mines ranging in depth from 1.3 to 3.1 km. During sampling in Beatrix gold mine (1.4 km beneath the surface), central South Africa, CaCO(3) stalactites growing on the mine tunnel ceiling were collected and observed, in two cases, to contain a living obligate brackish water/marine nematode species, Monhystrella parvella. After sterilization of the outer surface, mineral layers were physically removed from the outside to the interior, and DNA extracted. Based upon 16S and 18S rRNA gene sequencing, Archaea, Bacteria, and Eukarya in different combinations were detected for each layer. Using CT scan and electron microscopy the inner structure of CaCO(3) and salt stalactites were analyzed. CaCO(3) stalactites show a complex pattern of lamellae carrying bacterially precipitated mineral structures. Nematoda were clearly identified between these layers confirming that bacteria and nematodes live inside the stalactites and not only in the central straw. Salt stalactites exhibit a more uniform internal structure. Surprisingly, several Bacteria showing highest sequence identities to marine species were identified. This, together with the observation that the nematode M. parvella recovered from Beatrix gold mine stalactite can only survive in a salty environment makes the origin of the deep subsurface colonization enigmatic. The possibility of a Permian origin of fracture fluids is discussed. Our results indicate stalactites are suitable for biodiversity recovery and act as natural traps for microorganisms in the fissure water long after the water that formed the stalactite stopped flowing. |
format | Online Article Text |
id | pubmed-4585192 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2015 |
publisher | Frontiers Media S.A. |
record_format | MEDLINE/PubMed |
spelling | pubmed-45851922015-10-05 Deep subsurface mine stalactites trap endemic fissure fluid Archaea, Bacteria, and Nematoda possibly originating from ancient seas Borgonie, Gaëtan Linage-Alvarez, Borja Ojo, Abidemi Shivambu, Steven Kuloyo, Olukayode Cason, Errol D. Maphanga, Sihle Vermeulen, Jan-G Litthauer, Derek Ralston, Colin D. Onstott, Tullis C. Sherwood-Lollar, Barbara Van Heerden, Esta Front Microbiol Microbiology Stalactites (CaCO(3) and salt) from water seeps are frequently encountered in ceilings of mine tunnels whenever they intersect water-bearing faults or fractures. To determine whether stalactites could be mineralized traps for indigenous fracture water microorganisms, we analyzed stalactites collected from three different mines ranging in depth from 1.3 to 3.1 km. During sampling in Beatrix gold mine (1.4 km beneath the surface), central South Africa, CaCO(3) stalactites growing on the mine tunnel ceiling were collected and observed, in two cases, to contain a living obligate brackish water/marine nematode species, Monhystrella parvella. After sterilization of the outer surface, mineral layers were physically removed from the outside to the interior, and DNA extracted. Based upon 16S and 18S rRNA gene sequencing, Archaea, Bacteria, and Eukarya in different combinations were detected for each layer. Using CT scan and electron microscopy the inner structure of CaCO(3) and salt stalactites were analyzed. CaCO(3) stalactites show a complex pattern of lamellae carrying bacterially precipitated mineral structures. Nematoda were clearly identified between these layers confirming that bacteria and nematodes live inside the stalactites and not only in the central straw. Salt stalactites exhibit a more uniform internal structure. Surprisingly, several Bacteria showing highest sequence identities to marine species were identified. This, together with the observation that the nematode M. parvella recovered from Beatrix gold mine stalactite can only survive in a salty environment makes the origin of the deep subsurface colonization enigmatic. The possibility of a Permian origin of fracture fluids is discussed. Our results indicate stalactites are suitable for biodiversity recovery and act as natural traps for microorganisms in the fissure water long after the water that formed the stalactite stopped flowing. Frontiers Media S.A. 2015-08-11 /pmc/articles/PMC4585192/ /pubmed/26441844 http://dx.doi.org/10.3389/fmicb.2015.00833 Text en Copyright © 2015 Borgonie, Linage-Alvarez, Ojo, Shivambu, Kuloyo, Cason, Maphanga, Vermeulen, Litthauer, Ralston, Onstott, Sherwood-Lollar and Van Heerden. http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. |
spellingShingle | Microbiology Borgonie, Gaëtan Linage-Alvarez, Borja Ojo, Abidemi Shivambu, Steven Kuloyo, Olukayode Cason, Errol D. Maphanga, Sihle Vermeulen, Jan-G Litthauer, Derek Ralston, Colin D. Onstott, Tullis C. Sherwood-Lollar, Barbara Van Heerden, Esta Deep subsurface mine stalactites trap endemic fissure fluid Archaea, Bacteria, and Nematoda possibly originating from ancient seas |
title | Deep subsurface mine stalactites trap endemic fissure fluid Archaea, Bacteria, and Nematoda possibly originating from ancient seas |
title_full | Deep subsurface mine stalactites trap endemic fissure fluid Archaea, Bacteria, and Nematoda possibly originating from ancient seas |
title_fullStr | Deep subsurface mine stalactites trap endemic fissure fluid Archaea, Bacteria, and Nematoda possibly originating from ancient seas |
title_full_unstemmed | Deep subsurface mine stalactites trap endemic fissure fluid Archaea, Bacteria, and Nematoda possibly originating from ancient seas |
title_short | Deep subsurface mine stalactites trap endemic fissure fluid Archaea, Bacteria, and Nematoda possibly originating from ancient seas |
title_sort | deep subsurface mine stalactites trap endemic fissure fluid archaea, bacteria, and nematoda possibly originating from ancient seas |
topic | Microbiology |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4585192/ https://www.ncbi.nlm.nih.gov/pubmed/26441844 http://dx.doi.org/10.3389/fmicb.2015.00833 |
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