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Surface chemistry allows for abiotic precipitation of dolomite at low temperature
by
Moore, David S.
, González, Luis A.
, Fowle, David A.
, Roberts, Jennifer A.
, Kenward, Paul A.
, Goldstein, Robert H.
in
"Earth, Atmospheric, and Planetary Sciences"
/ Aragonite
/ Bacteria - growth & development
/ Bacteria - metabolism
/ biofilm
/ Biofilms
/ Biological Sciences
/ Bioreactors - microbiology
/ Calcite
/ Calcium Carbonate - chemistry
/ Calcium Carbonate - metabolism
/ carbon
/ carbon dioxide
/ Carbon Dioxide - metabolism
/ Carbonates
/ carbonation
/ Chemical analysis
/ Chemical Precipitation
/ death
/ Dolomite
/ Earth sciences
/ Earth, ocean, space
/ energy
/ Environmental Microbiology
/ Exact sciences and technology
/ Geology
/ Hydrogen-Ion Concentration
/ ions
/ laboratory experimentation
/ Low temperature
/ magnesium
/ Magnesium - chemistry
/ Magnesium - metabolism
/ microbial biomass
/ Microbiology
/ Microorganisms
/ Microscopy, Electron, Scanning
/ Mineral precipitation
/ mixing
/ Models, Chemical
/ Nucleation
/ Organic carbon
/ Organic matter
/ Physical Sciences
/ Polystyrene
/ polystyrenes
/ Precipitation
/ Reaction kinetics
/ Salinity
/ Seawater
/ Seawater - microbiology
/ Spectrometry, X-Ray Emission
/ Stratigraphy
/ Surface chemistry
/ Surface Properties
/ Temperature
/ Water analysis
/ X-Ray Diffraction
2013
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Surface chemistry allows for abiotic precipitation of dolomite at low temperature
by
Moore, David S.
, González, Luis A.
, Fowle, David A.
, Roberts, Jennifer A.
, Kenward, Paul A.
, Goldstein, Robert H.
in
"Earth, Atmospheric, and Planetary Sciences"
/ Aragonite
/ Bacteria - growth & development
/ Bacteria - metabolism
/ biofilm
/ Biofilms
/ Biological Sciences
/ Bioreactors - microbiology
/ Calcite
/ Calcium Carbonate - chemistry
/ Calcium Carbonate - metabolism
/ carbon
/ carbon dioxide
/ Carbon Dioxide - metabolism
/ Carbonates
/ carbonation
/ Chemical analysis
/ Chemical Precipitation
/ death
/ Dolomite
/ Earth sciences
/ Earth, ocean, space
/ energy
/ Environmental Microbiology
/ Exact sciences and technology
/ Geology
/ Hydrogen-Ion Concentration
/ ions
/ laboratory experimentation
/ Low temperature
/ magnesium
/ Magnesium - chemistry
/ Magnesium - metabolism
/ microbial biomass
/ Microbiology
/ Microorganisms
/ Microscopy, Electron, Scanning
/ Mineral precipitation
/ mixing
/ Models, Chemical
/ Nucleation
/ Organic carbon
/ Organic matter
/ Physical Sciences
/ Polystyrene
/ polystyrenes
/ Precipitation
/ Reaction kinetics
/ Salinity
/ Seawater
/ Seawater - microbiology
/ Spectrometry, X-Ray Emission
/ Stratigraphy
/ Surface chemistry
/ Surface Properties
/ Temperature
/ Water analysis
/ X-Ray Diffraction
2013
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Surface chemistry allows for abiotic precipitation of dolomite at low temperature
by
Moore, David S.
, González, Luis A.
, Fowle, David A.
, Roberts, Jennifer A.
, Kenward, Paul A.
, Goldstein, Robert H.
in
"Earth, Atmospheric, and Planetary Sciences"
/ Aragonite
/ Bacteria - growth & development
/ Bacteria - metabolism
/ biofilm
/ Biofilms
/ Biological Sciences
/ Bioreactors - microbiology
/ Calcite
/ Calcium Carbonate - chemistry
/ Calcium Carbonate - metabolism
/ carbon
/ carbon dioxide
/ Carbon Dioxide - metabolism
/ Carbonates
/ carbonation
/ Chemical analysis
/ Chemical Precipitation
/ death
/ Dolomite
/ Earth sciences
/ Earth, ocean, space
/ energy
/ Environmental Microbiology
/ Exact sciences and technology
/ Geology
/ Hydrogen-Ion Concentration
/ ions
/ laboratory experimentation
/ Low temperature
/ magnesium
/ Magnesium - chemistry
/ Magnesium - metabolism
/ microbial biomass
/ Microbiology
/ Microorganisms
/ Microscopy, Electron, Scanning
/ Mineral precipitation
/ mixing
/ Models, Chemical
/ Nucleation
/ Organic carbon
/ Organic matter
/ Physical Sciences
/ Polystyrene
/ polystyrenes
/ Precipitation
/ Reaction kinetics
/ Salinity
/ Seawater
/ Seawater - microbiology
/ Spectrometry, X-Ray Emission
/ Stratigraphy
/ Surface chemistry
/ Surface Properties
/ Temperature
/ Water analysis
/ X-Ray Diffraction
2013
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Surface chemistry allows for abiotic precipitation of dolomite at low temperature
Journal Article
Surface chemistry allows for abiotic precipitation of dolomite at low temperature
2013
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Overview
Although the mineral dolomite is abundant in ancient low-temperature sedimentary systems, it is scarce in modern systems below 50 °C. Chemical mechanism(s) enhancing its formation remain an enigma because abiotic dolomite has been challenging to synthesize at low temperature in laboratory settings. Microbial enhancement of dolomite precipitation at low temperature has been reported; however, it is still unclear exactly how microorganisms influence reaction kinetics. Here we document the abiotic synthesis of low-temperature dolomite in laboratory experiments and constrain possible mechanisms for dolomite formation. Ancient and modern seawater solution compositions, with identical pH and pCO ₂, were used to precipitate an ordered, stoichiometric dolomite phase at 30 °C in as few as 20 d. Mg-rich phases nucleate exclusively on carboxylated polystyrene spheres along with calcite, whereas aragonite forms in solution via homogeneous nucleation. We infer that Mg ions are complexed and dewatered by surface-bound carboxyl groups, thus decreasing the energy required for carbonation. These results indicate that natural surfaces, including organic matter and microbial biomass, possessing a high density of carboxyl groups may be a mechanism by which ordered dolomite nuclei form. Although environments rich in organic matter may be of interest, our data suggest that sharp biogeochemical interfaces that promote microbial death, as well as those with high salinity may, in part, control carboxyl-group density on organic carbon surfaces, consistent with origin of dolomites from microbial biofilms, as well as hypersaline and mixing zone environments.
Publisher
National Academy of Sciences
Subject
"Earth, Atmospheric, and Planetary Sciences"
/ Bacteria - growth & development
/ biofilm
/ Biofilms
/ Calcite
/ Calcium Carbonate - chemistry
/ Calcium Carbonate - metabolism
/ carbon
/ death
/ Dolomite
/ energy
/ Exact sciences and technology
/ Geology
/ ions
/ Microscopy, Electron, Scanning
/ mixing
/ Salinity
/ Seawater
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