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  • 1
    Online Resource
    Online Resource
    Singapore :Springer Singapore Pte. Limited,
    Keywords: Geomicrobiology-Japan. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (181 pages)
    Edition: 1st ed.
    ISBN: 9789811313370
    Series Statement: Springer Geology Series
    Language: English
    Note: Intro -- Preface -- Contents -- Chapter 1: Introduction -- References -- Chapter 2: Basic Knowledge of Geochemical Processes -- 2.1 Subsurface Processes and Basic Requirement for Travertine Formation -- 2.2 Geochemistry of Carbonic Acid Species -- 2.3 Activity Coefficient and Ion Pair -- 2.4 Precipitation Kinetics of Calcium Carbonate -- 2.5 Stable Isotopes -- 2.5.1 Oxygen Isotopes of Carbonate and Water -- 2.5.2 Carbon Isotopes of Carbonate and DIC -- 2.5.3 Downstream Change in Travertine Stable Isotope -- 2.5.4 Isotopic Non-equilibrium in the Travertine System -- 2.6 Mineral Polymorphs -- References -- Chapter 3: Sedimentology of Travertine -- 3.1 Geomorphology of Travertine Bodies -- 3.2 Travertines as Microbialites -- 3.3 Fabrics of Microbial Carbonate -- 3.4 Microscopic Fabrics -- 3.4.1 Inorganic Fabrics -- 3.4.2 Microbe-Associated Fabrics -- 3.5 Non-carbonate Structures -- 3.5.1 Black Layer by Sulfate Reduction -- 3.5.2 Iron Deposits Near the Vent -- References -- Chapter 4: Methods -- 4.1 Water Chemistry -- 4.2 Microelectrode -- 4.2.1 Importance of Chemical Profiles at the Sediment/Water Interface -- 4.2.2 Structure of Microelectrodes -- 4.2.3 Semi-In Situ Measurement -- 4.2.4 Examples of Microelectrode Measurement -- 4.3 Stable Isotope Measurement -- 4.4 Textural Observation -- 4.4.1 Thin Section -- 4.4.2 Scanning Electron Microscopy (SEM) -- 4.4.3 Fluorescence In Situ Hybridization (FISH) -- 4.5 Microbial Analysis -- 4.5.1 Phylogenetic Analysis of 16S rRNA Gene -- 4.5.2 PCR-DGGE -- 4.5.3 Analysis for Extracellular Polymeric Substance -- References -- Chapter 5: Geomicrobiological Processes for Laminated Textures -- 5.1 Annual Lamination in Tufas -- 5.2 Daily Lamination in Travertines -- 5.3 Travertines as a Modern Analog of Ancient Stromatolites -- References. , Chapter 6: Geochemical Model for Rapid Carbonate Precipitation of Travertines -- 6.1 Background -- 6.2 Laminated Travertines and Tufa -- 6.3 Precipitation Rate Observed the Laminated Deposits -- 6.3.1 Methods to Quantify Precipitation Rate -- 6.3.2 Observed Precipitation Rate of Travertines and Tufas -- 6.4 Water Chemistry of Travertine and Tufa Sites -- 6.4.1 Travertine -- 6.4.2 Tufa -- 6.5 Correlation Between the OPR and Chemical Properties of the Water -- 6.6 Other Factors Controlling Carbonate Precipitation -- 6.7 Conclusions -- References -- Chapter 7: Travertines in Japan -- 7.1 Futamata -- 7.1.1 Background -- 7.1.2 Water Chemistry -- 7.1.3 Travertine Occurrence -- 7.2 Okuokuhachikuro -- 7.2.1 Geological Settings -- 7.2.2 Water Chemistry and Travertine Occurrence -- 7.3 Yunomata -- 7.3.1 General Settings -- 7.3.2 Water Chemistry -- 7.4 Shionoha -- 7.4.1 Geological Settings -- 7.4.2 Hydrochemistry and Travertine Occurrence -- 7.5 Kibedani -- 7.5.1 Overview of Hot Springs in Shimane Prefecture -- 7.5.2 Kibedani -- 7.6 Nagayu -- 7.6.1 Hydrothermal Settings -- 7.6.2 Geochemistry of Water -- 7.6.3 Travertine -- 7.7 Shiobitashi -- 7.7.1 Background -- 7.7.2 Water Chemistry and Travertine Occurrence -- 7.8 Myoken -- 7.8.1 Hydrothermal Settings and Geochemistry of Water -- 7.8.2 Travertine Textures -- References -- Chapter 8: Concluding Remarks.
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  • 2
    Keywords: Bacteriology ; Mineralogy ; Sedimentology ; Sedimentology ; Bacteriology ; Mineralogy ; Geobiology. ; Japan ; Travertin ; Mikrobiologie ; Geomikrobiologie ; Sedimentologie
    Description / Table of Contents: This book presents basic knowledge and key objectives of research of geological, geochemical, and microbial properties and processes in travertines, carbonate deposits precipitated from calcareous hot springs. Much of the contents are based on the authors’ researches performed in Japan and Indonesia over the last decade. Travertine is one of the most active sedimentary systems, which have a potential impact on the Earth’s environment. It is also an accessible epitome of the Earth’s history, cultivating ancestral bacteria and representing a modern analog for ancient stromatolites. Readers can learn how integration of various scopes and methods unveils mysterious phenomena in travertine and can find cues for considering the early history of the Earth and life. This book includes a monographic chapter on Japanese onsens, or hot springs, which may help tourists to select the best places to enjoy the unique features of travertine
    Type of Medium: Online Resource
    Pages: Online-Ressource (IX, 176 p. 79 illus., 63 illus. in color, online resource)
    Edition: Springer eBook Collection. Earth and Environmental Science
    ISBN: 9789811313370
    Series Statement: Springer Geology
    Language: English
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  • 3
    Publication Date: 2018-11-07
    Description: Cyanobacteria-dominated biofilms in a CO2-degassing karst-water creek (Westerhöfer Bach, Germany) were investigated with regard to the effects of microbial activity on CaCO3 precipitation, water chemistry of micro- and macroenvironments, stable isotopic records, and tufa fabric formation. Ex situ microelectrode measurements of pH, O2, Ca2+ and CO32− revealed that annually laminated calcified biofilms composed mainly of filamentous cyanobacteria (tufa stromatolites) strongly induced CaCO3 precipitation by photosynthesis under illumination, but inhibited precipitation by respiration in the dark. In contrast, endolithic cyanobacterial biofilms and mosses did not cause photosynthesis-induced precipitation under experimental conditions. No spontaneous precipitation occurred on bare limestone substrates, despite high calcite supersaturation of the ambient water. Mass balance calculations suggest that biofilm photosynthesis was responsible for 10–20% of Ca2+ loss in the creek, while the remaining Ca2+ loss derived from physicochemical precipitation on branches, leaves and as fine-grained calcite particles. Neither analysis of bulk water chemistry nor oxygen nor carbon stable isotopic records of the tufa stromatolites confirmed photosynthetic effects, despite the evident photosynthesis-induced calcite precipitation. Oxygen stable isotopic values reflected seasonal changes in water temperature, and carbon stable isotope values probably recorded carbon isotopic composition of dissolved inorganic carbon in the creek water. Annual lamination and fabric formation of the tufa stromatolites is suggested to vary with photosynthesis-induced calcite precipitation rates that are affected by temperature dependency of diffusion coefficients. Photosynthesis-induced precipitation resulted in encrusted cyanobacterial sheaths, reflecting syntaxial overgrowth of microcrystalline cyanobacterial tubes by microspar, instead of microcrystalline sheath impregnation, which was previously suggested as an indicator of photosynthesis-induced precipitation. Therefore, sheath impregnation or encrustation by CaCO3 cannot be used to distinguish photosynthesis-induced from physicochemically-induced CaCO3 precipitation.
    Type: Article , PeerReviewed
    Format: text
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