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Microbial Potential for Carbon Fixation and Stabilization

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26310%2F21%3APU150951" target="_blank" >RIV/00216305:26310/21:PU150951 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://link.springer.com/chapter/10.1007/978-981-33-6765-4_4" target="_blank" >https://link.springer.com/chapter/10.1007/978-981-33-6765-4_4</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/978-981-33-6765-4_4" target="_blank" >10.1007/978-981-33-6765-4_4</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Microbial Potential for Carbon Fixation and Stabilization

  • Popis výsledku v původním jazyce

    Research on microbial diversity, interaction between microbes and soil physiochemical properties, role of microbes in biogeochemical cycles, and climate change have guided the scientific community to understand the soil and environmental health. Carbon is one of the essential elements of the soil, oceans, atmosphere, crustal rocks, kerogen (solid hydrocarbon for the formation of fuels), and reserve in various forms called carbon sink. Carbon-containing organic molecules flux between all these ecosystems (reservoirs) for the balance and sustainable function of the ecosystems via active carbon cycle. Carbon is the prime element for building a life on Earth which is fixed in various forms in the terrestrial and marine plants through photosynthesis. Microorganisms play regulatory role in biogeochemical cycles and shaping any kind of ecosystems. There are huge diversity of soil and aquatic microbes like Acetobacterium woodii, Aquifex aeolicus, Archaebacteria brierleyi, Ignicoccus hospitalis, Chlorobium limicola, C. tepidum, C. thiosulfatophilum, C. phaeobacteroides, Chloroflexus aurantiacus, C. aggregans, Chromatium vinosum, Clostridium thermoaceticum, Crenarchaeota, Desulfobacter hydrogenophilus, Desulfurobacterium crinifex, D. thermolithotrophum, Halobacterium salinarum, Thiobacillus ferrooxidans, Hydrogenobacter hydrogenophilus, H. thermophilus, Metallosphaera sedula, Moorella thermoacetica, Pyrobaculum aerophilum, Pyrobaculum islandicum, Pyrolobus fumarii, Rhodobacter sphaeroides, Rhodopseudomonas viridis, Rhodospirillum rubrum, Stygiolobusa zoricus, Sulfolobus metallicus, Sulfurihydrogenibium subterraneum, Thermocrinis ruber, Thermoproteus neutrophilus, Thermovibrio ammonificans, T. ruber, and Thiomicrospira denitrificans, and also order Rhizobiales are able to fix the various forms of carbon through numerous pathways such as Calvin cycle, reductive acetylcoenzyme A pathway, reductive citric acid cycle, dicarboxylate/4-hydroxybutyrate cycle (DC/HB), hydroxypropionat

  • Název v anglickém jazyce

    Microbial Potential for Carbon Fixation and Stabilization

  • Popis výsledku anglicky

    Research on microbial diversity, interaction between microbes and soil physiochemical properties, role of microbes in biogeochemical cycles, and climate change have guided the scientific community to understand the soil and environmental health. Carbon is one of the essential elements of the soil, oceans, atmosphere, crustal rocks, kerogen (solid hydrocarbon for the formation of fuels), and reserve in various forms called carbon sink. Carbon-containing organic molecules flux between all these ecosystems (reservoirs) for the balance and sustainable function of the ecosystems via active carbon cycle. Carbon is the prime element for building a life on Earth which is fixed in various forms in the terrestrial and marine plants through photosynthesis. Microorganisms play regulatory role in biogeochemical cycles and shaping any kind of ecosystems. There are huge diversity of soil and aquatic microbes like Acetobacterium woodii, Aquifex aeolicus, Archaebacteria brierleyi, Ignicoccus hospitalis, Chlorobium limicola, C. tepidum, C. thiosulfatophilum, C. phaeobacteroides, Chloroflexus aurantiacus, C. aggregans, Chromatium vinosum, Clostridium thermoaceticum, Crenarchaeota, Desulfobacter hydrogenophilus, Desulfurobacterium crinifex, D. thermolithotrophum, Halobacterium salinarum, Thiobacillus ferrooxidans, Hydrogenobacter hydrogenophilus, H. thermophilus, Metallosphaera sedula, Moorella thermoacetica, Pyrobaculum aerophilum, Pyrobaculum islandicum, Pyrolobus fumarii, Rhodobacter sphaeroides, Rhodopseudomonas viridis, Rhodospirillum rubrum, Stygiolobusa zoricus, Sulfolobus metallicus, Sulfurihydrogenibium subterraneum, Thermocrinis ruber, Thermoproteus neutrophilus, Thermovibrio ammonificans, T. ruber, and Thiomicrospira denitrificans, and also order Rhizobiales are able to fix the various forms of carbon through numerous pathways such as Calvin cycle, reductive acetylcoenzyme A pathway, reductive citric acid cycle, dicarboxylate/4-hydroxybutyrate cycle (DC/HB), hydroxypropionat

Klasifikace

  • Druh

    C - Kapitola v odborné knize

  • CEP obor

  • OECD FORD obor

    10500 - Earth and related environmental sciences

Návaznosti výsledku

  • Projekt

  • Návaznosti

    S - Specificky vyzkum na vysokych skolach

Ostatní

  • Rok uplatnění

    2021

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název knihy nebo sborníku

    Soil Carbon Stabilization to Mitigate Climate Change

  • ISBN

    978-981-33-6765-4

  • Počet stran výsledku

    44

  • Strana od-do

    125-168

  • Počet stran knihy

    332

  • Název nakladatele

    Springer Nature

  • Místo vydání

    Neuveden

  • Kód UT WoS kapitoly