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dc.contributor.authorKim, J. W.
dc.contributor.authorKogure, T.
dc.contributor.authorYang, Kiho
dc.contributor.authorKim, S. T.
dc.contributor.authorJang, Y. N.
dc.contributor.authorBalik, H. S.
dc.contributor.authorGeesey, Gill G.
dc.date.accessioned2017-01-31T20:47:01Z
dc.date.available2017-01-31T20:47:01Z
dc.date.issued2012-10
dc.identifier.citationKim J-W, Kogure T, Yang K, Kim S-T, Jang Y-N, Baik H-S, Geesey G, "The characterization of CaCo3 in a geothermal environment: A SEM/TEM-EELS study," Clays and Clay Minerals, October 2012 60(5):484–495.en_US
dc.identifier.issn0009-8604
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/12490
dc.description.abstractMineralization of microbial biomass is a common phenomenon in geothermal habitats, but knowledge of the structure of the minerals formed in these environments is limited. A combination of spectroscopic, microscopic, and stable isotopic methods, as well as the chemical analysis of spring water, were employed in the present study to characterize calcium carbonate minerals deposited in filamentous cyanobacterial mats in different locations of La Duke hot spring, a circumneutral thermal feature near the north entrance of Yellowstone National Park, Montana, USA. Calcite was the primary crystalline mineral phase associated with biofilm-containing deposits closest to the source of the spring and the suspended microbial biomass in a pool further from the source. The carbonate minerals at all sites occurred as aggregated granules, ~2 mm in diameter, in close association with the microbial biomass. Only in the deposits closest to the source were the granules organized as laminated structures interspersed with microbial biomass. The calcium carbonate grains contained two distinct regions: a dense monolithic calcite core and a porous dendritic periphery containing organic matter (OM). Electron energy loss spectroscopy (EELS) indicated that the voids were infilled with OM and carbonates. The EELS technique was employed to distinguish the source of carbon in the organic matter and carbonate mixture. The studies of carbon isotope compositions of the calcium carbonates and the saturation indices for calcite in the spring waters suggest that processes (abiotic vs. biotic) controlling the carbonate formation may vary among the sampling sites.en_US
dc.titleThe characterization of CaCo3 in a geothermal environment: A SEM/TEM-EELS studyen_US
dc.typeArticleen_US
mus.citation.extentfirstpage484en_US
mus.citation.extentlastpage495en_US
mus.citation.issue5en_US
mus.citation.journaltitleClays and Clay Mineralsen_US
mus.citation.volume60en_US
mus.identifier.categoryChemical & Material Sciencesen_US
mus.identifier.categoryEngineering & Computer Scienceen_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1346/ccmn.2012.0600505en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.collegeCollege of Engineeringen_US
mus.relation.collegeCollege of Letters & Scienceen_US
mus.relation.departmentCenter for Biofilm Engineering.en_US
mus.relation.departmentChemical & Biological Engineering.en_US
mus.relation.departmentChemical Engineering.en_US
mus.relation.departmentChemistry & Biochemistry.en_US
mus.relation.departmentEcology.en_US
mus.relation.departmentEnvironmental Engineering.en_US
mus.relation.departmentLand Resources & Environmental Sciences.en_US
mus.relation.departmentMicrobiology & Immunology.en_US
mus.relation.universityMontana State University - Bozemanen_US
mus.relation.researchgroupCenter for Biofilm Engineering.en_US
mus.data.thumbpage8en_US


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