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Wilmeth DT, Myers KD, Lalonde SV, Mänd K, Konhauser KO, Grandin P, van Zuilen MA. Evaporative silicification in floating microbial mats: patterns of oxygen production and preservation potential in silica-undersaturated streams, El Tatio, Chile. Geobiology 2022; 20:310-330. [PMID: 34676677 PMCID: PMC9298402 DOI: 10.1111/gbi.12476] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/21/2021] [Revised: 10/01/2021] [Accepted: 10/04/2021] [Indexed: 05/26/2023]
Abstract
Microbial mats floating within multiple hydrothermally sourced streams in El Tatio, Chile, frequently exhibit brittle siliceous crusts (~1 mm thick) above the air-water interface. The partially silicified mats contain a diverse assemblage of microbial clades and metabolisms, including cyanobacteria performing oxygenic photosynthesis. Surficial crusts are composed of several amorphous silica layers containing well-preserved filaments (most likely cyanobacteria) and other cellular textures overlying EPS-rich unsilicified mats. Environmental logs, silica crust distribution, and microbial preservation patterns provide evidence for crust formation via repeated cycles of evaporation and silica precipitation. Within the mats, in situ microelectrode profiling reveals that daytime oxygen concentrations and pH values are diminished beneath silica crusts compared with adjacent unencrusted communities, indicating localized inhibition of oxygenic photosynthesis due to light attenuation. As a result, aqueous conditions under encrusted mats have a higher saturation state with regard to amorphous silica compared with adjacent, more active mats where high pH increases silica solubility, likely forming a modest feedback loop between diminished photosynthesis and crust precipitation. However, no fully lithified sinters are associated with floating encrusted mats in El Tatio streams, as both subaqueous and subaerial silica precipitation are limited by undersaturated, low-SiO2 (<150 ppm) stream waters. By contrast, well-cemented sinters can form by evaporation in silica-undersaturated solutions above 200 ppm SiO2 . Floating mats in El Tatio therefore represent a specific sinter preservation window, where evaporation in silica-undersaturated microbial mats produces crusts, which preserve cells and affect mat chemistry, but low-silica concentrations prevent the formation of lasting sinter deposits. Patterns of silica precipitation in El Tatio microbial communities show that the preservation potential of silicifying mats in the rock record is strongly dependent on aqueous silica concentrations.
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Affiliation(s)
- Dylan T. Wilmeth
- Université de ParisInstitut de Physique du Globe de Paris, CNRSParisFrance
- CNRS‐UMR6538European Institute for Marine StudiesPlouzanéFrance
| | - Kimberly D. Myers
- Université de ParisInstitut de Physique du Globe de Paris, CNRSParisFrance
| | | | - Kaarel Mänd
- Department of GeologyUniversity of TartuTartuEstonia
- Department of Earth and Atmospheric SciencesUniversity of AlbertaEdmontonAlbertaCanada
| | - Kurt O. Konhauser
- Department of Earth and Atmospheric SciencesUniversity of AlbertaEdmontonAlbertaCanada
| | - Prisca Grandin
- CNRS‐UMR6538European Institute for Marine StudiesPlouzanéFrance
| | - Mark A. van Zuilen
- Université de ParisInstitut de Physique du Globe de Paris, CNRSParisFrance
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Gong J, Munoz-Saez C, Wilmeth DT, Myers KD, Homann M, Arp G, Skok JR, van Zuilen MA. Morphogenesis of digitate structures in hot spring silica sinters of the El Tatio geothermal field, Chile. Geobiology 2022. [PMID: 34590770 DOI: 10.6084/m9.figshare.12957797.v1] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Subscribe] [Scholar Register] [Indexed: 05/12/2023]
Abstract
In silica-rich hot spring environments, internally laminated, digitate sinter deposits are often interpreted as bio-mediated structures. The organic components of microbial communities (cell surfaces, sheaths and extracellular polymeric substances) can act as templates for silica precipitation, therefore influencing digitate sinter morphogenesis. In addition to biologic surface-templating effects, various microenvironmental factors (hydrodynamics, local pH and fluctuating wind patterns) can also influence silica precipitation, and therefore the morphology of resulting digitate sinters. Digitate sinter morphology thus depends on the dynamic interplay between microenvironmentally driven silica precipitation and microbial growth, but the relative contributions of both factors are a topic of continuing research. Here we present a detailed study of digitate silica sinters in distal, low-temperature regimes of the El Tatio geothermal field, Chile. This high-altitude geothermal field is extremely arid and windy, and has one of the highest silica precipitation rates found in the world. We find that digitate silica sinters at El Tatio always accrete into the prevailing eastward wind direction and exhibit laminar growth patterns coinciding with day-night cycles of wind- and thermally driven evaporation and rewetting. Subaerial parts of digitate sinters lack preserved organics and sinter textures that would indicate past microbial colonization, while filamentous cyanobacteria with resistant, silicified sheaths only inhabit subaqueous cavities that crosscut the primary laminations. We conclude that, although fragile biofilms of extremophile micro-organisms may have initially been present and templated silica precipitation at the tips of these digitate sinters, the saltation of sand grains and precipitation of silica by recurrent wind- and thermally driven environmental forcing at El Tatio are important, if not dominant factors shaping the morphology of these digitate structures. Our study sheds light on the relative contributions of biogenic and abiogenic factors in sinter formation in geothermal systems, with geobiological implications for the cautious interpretation of stromatolite-like features in ancient silica deposits on Earth and Mars.
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Affiliation(s)
- Jian Gong
- Université de Paris, Institut de Physique du Globe de Paris, CNRS, F-75005, Paris, France
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA
| | | | - Dylan T Wilmeth
- Université de Paris, Institut de Physique du Globe de Paris, CNRS, F-75005, Paris, France
- Equipe Géomicrobiologie, Institut Universitaire Européen de la Mer, Plouzané, France
| | - Kimberly D Myers
- Université de Paris, Institut de Physique du Globe de Paris, CNRS, F-75005, Paris, France
| | - Martin Homann
- Department of Earth Sciences, University College London, London, UK
| | - Gernot Arp
- Geobiology Division, Geoscience Centre, Georg-August-Universität Göttingen, Göttingen, Germany
| | - John R Skok
- SETI Institute, Mountain View, California, USA
| | - Mark A van Zuilen
- Université de Paris, Institut de Physique du Globe de Paris, CNRS, F-75005, Paris, France
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Gong J, Munoz‐Saez C, Wilmeth DT, Myers KD, Homann M, Arp G, Skok JR, van Zuilen MA. Morphogenesis of digitate structures in hot spring silica sinters of the El Tatio geothermal field, Chile. Geobiology 2022; 20:137-155. [PMID: 34590770 PMCID: PMC9292339 DOI: 10.1111/gbi.12471] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/18/2021] [Accepted: 09/02/2021] [Indexed: 05/19/2023]
Abstract
In silica-rich hot spring environments, internally laminated, digitate sinter deposits are often interpreted as bio-mediated structures. The organic components of microbial communities (cell surfaces, sheaths and extracellular polymeric substances) can act as templates for silica precipitation, therefore influencing digitate sinter morphogenesis. In addition to biologic surface-templating effects, various microenvironmental factors (hydrodynamics, local pH and fluctuating wind patterns) can also influence silica precipitation, and therefore the morphology of resulting digitate sinters. Digitate sinter morphology thus depends on the dynamic interplay between microenvironmentally driven silica precipitation and microbial growth, but the relative contributions of both factors are a topic of continuing research. Here we present a detailed study of digitate silica sinters in distal, low-temperature regimes of the El Tatio geothermal field, Chile. This high-altitude geothermal field is extremely arid and windy, and has one of the highest silica precipitation rates found in the world. We find that digitate silica sinters at El Tatio always accrete into the prevailing eastward wind direction and exhibit laminar growth patterns coinciding with day-night cycles of wind- and thermally driven evaporation and rewetting. Subaerial parts of digitate sinters lack preserved organics and sinter textures that would indicate past microbial colonization, while filamentous cyanobacteria with resistant, silicified sheaths only inhabit subaqueous cavities that crosscut the primary laminations. We conclude that, although fragile biofilms of extremophile micro-organisms may have initially been present and templated silica precipitation at the tips of these digitate sinters, the saltation of sand grains and precipitation of silica by recurrent wind- and thermally driven environmental forcing at El Tatio are important, if not dominant factors shaping the morphology of these digitate structures. Our study sheds light on the relative contributions of biogenic and abiogenic factors in sinter formation in geothermal systems, with geobiological implications for the cautious interpretation of stromatolite-like features in ancient silica deposits on Earth and Mars.
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Affiliation(s)
- Jian Gong
- Université de Paris, Institut de Physique du Globe de Paris, CNRSF‐75005ParisFrance
- Department of Earth, Atmospheric and Planetary SciencesMassachusetts Institute of TechnologyCambridgeMassachusettsUSA
| | | | - Dylan T. Wilmeth
- Université de Paris, Institut de Physique du Globe de Paris, CNRSF‐75005ParisFrance
- Equipe GéomicrobiologieInstitut Universitaire Européen de la MerPlouzanéFrance
| | - Kimberly D. Myers
- Université de Paris, Institut de Physique du Globe de Paris, CNRSF‐75005ParisFrance
| | - Martin Homann
- Department of Earth SciencesUniversity College LondonLondonUK
| | - Gernot Arp
- Geobiology DivisionGeoscience CentreGeorg‐August‐Universität GöttingenGöttingenGermany
| | | | - Mark A. van Zuilen
- Université de Paris, Institut de Physique du Globe de Paris, CNRSF‐75005ParisFrance
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Gong J, Myers KD, Munoz-Saez C, Homann M, Rouillard J, Wirth R, Schreiber A, van Zuilen MA. Formation and Preservation of Microbial Palisade Fabric in Silica Deposits from El Tatio, Chile. Astrobiology 2020; 20:500-524. [PMID: 31663774 PMCID: PMC7133459 DOI: 10.1089/ast.2019.2025] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/07/2019] [Accepted: 09/19/2019] [Indexed: 05/26/2023]
Abstract
Palisade fabric is a ubiquitous texture of silica sinter found in low temperature (<40°C) regimes of hot spring environments, and it is formed when populations of filamentous microorganisms act as templates for silica polymerization. Although it is known that postdepositional processes such as biological degradation and dewatering can strongly affect preservation of these fabrics, the impact of extreme aridity has so far not been studied in detail. Here, we report a detailed analysis of recently silicified palisade fabrics from a geyser in El Tatio, Chile, tracing the progressive degradation of microorganisms within the silica matrix. This is complemented by heating experiments of natural sinter samples to assess the role of diagenesis. Sheathed cyanobacteria, identified as Leptolyngbya sp., were found to be incorporated into silica sinter by irregular cycles of wetting, evaporation, and mineral precipitation. Transmission electron microscopy analyses revealed that nanometer-sized silica particles are filling the pore space within individual cyanobacterial sheaths, giving rise to their structural rigidity to sustain a palisade fabric framework. Diagenesis experiments further show that the sheaths of the filaments are preferentially preserved relative to the trichomes, and that the amount of water present within the sinter is an important factor for overall preservation during burial. This study confirms that palisade fabrics are efficiently generated in a highly evaporative geothermal field, and that these biosignatures can be most effectively preserved under dry diagenetic conditions.
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Affiliation(s)
- Jian Gong
- Equipe Géomicrobiologie, Université de Paris, Institut de physique du globe de Paris, CNRS, Paris, France
| | - Kimberly D. Myers
- Equipe Géomicrobiologie, Université de Paris, Institut de physique du globe de Paris, CNRS, Paris, France
| | - Carolina Munoz-Saez
- Departamento de Geologia, FCFM, Centro de Excelencia en Geotermia de los Andes (CEGA), Universidad de Chile, Santiago, Chile
| | - Martin Homann
- CNRS-UMR6538 Laboratoire Géosciences Océan, European Institute for Marine Studies, Technopôle Brest-Iroise, Plouzané, France
| | - Joti Rouillard
- Equipe Géomicrobiologie, Université de Paris, Institut de physique du globe de Paris, CNRS, Paris, France
| | - Richard Wirth
- GeoForschungsZentrum, Section 3.5 Interface Geochemistry, D-14473, Potsdam, Germany
| | - Anja Schreiber
- GeoForschungsZentrum, Section 3.5 Interface Geochemistry, D-14473, Potsdam, Germany
| | - Mark A. van Zuilen
- Equipe Géomicrobiologie, Université de Paris, Institut de physique du globe de Paris, CNRS, Paris, France
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Edwards BE, Couch NW, Myers KD, Blanchard SG, Chandra G, Parr AF. 125I aqueous waste volume reduction at a pharmaceutical research laboratory. Health Phys 1996; 71:379-383. [PMID: 8698582 DOI: 10.1097/00004032-199609000-00017] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/22/2023]
Abstract
A wide variety of radioactive waste is generated by pharmaceutical research. One particularly high volume low specific activity waste stream produced by a research and development facility is aqueous 125I waste. This waste is generally held for decay and released to the sanitary sewer when the activity is low enough to ensure that concentrations are well below the appropriate regulatory limits. However, the large volume of this particular waste stream rapidly exhausted available space to store it for decay. This study investigated safe, inexpensive, and efficient methods for removing 125I from the aqueous waste, with the goal of implementing a practical process for concentrating the activity and thus reducing the stored volume. The implemented treatment (volume reduction) process used commercially available low cost activated carbon/particulate filters and inexpensive resin beds manufactured in-house. The much smaller volumes of spent filters and resin beds are then held for decay and eventual incineration. This technique has proven an effective means for managing this high volume waste stream.
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Affiliation(s)
- B E Edwards
- Glaxo Wellcome Inc., Research Triangle Park, NC 27709, USA
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