Number of the records: 1  

Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter

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    SYSNO ASEP0367392
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleDeep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter
    Author(s) Frouz, Jan (BC-A) RID, ORCID
    Cajthaml, Tomáš (MBU-M) RID, ORCID
    Kříbek, B. (CZ)
    Schaeffer, P. (FR)
    Bartuška, Martin (BC-A) RID, ORCID
    Galertová, R. (CZ)
    Rojík, P. (CZ)
    Krištůfek, Václav (BC-A) RID
    Source TitleFolia Microbiologica. - : Springer - ISSN 0015-5632
    Roč. 56, č. 5 (2011), s. 389-396
    Number of pages8 s.
    Languageeng - English
    CountryCZ - Czech Republic
    Keywordsmicroflora ; biomass ; fossil organic matter
    Subject RIVEH - Ecology, Behaviour
    R&D ProjectsGA206/09/1642 GA ČR - Czech Science Foundation (CSF)
    CEZAV0Z60660521 - UPB-H, BC-A (2005-2011)
    AV0Z50200510 - MBU-M (2005-2011)
    UT WOS000295681100004
    DOI10.1007/s12223-011-0062-9
    AnnotationThree types of Miocene claystones (amorphous, lamellar, and transitional) were aseptically sampled from depths of 30 m and 150 m below the soil surface. Respiration of these sediments was measured under conditions that prevented inoculation by other microorganisms not indigenous to the claystones in situ. Microbial respiration was higher in lamellar than amorphous claystones and was not affected by sampling depth. During cultivation, microbial biomass (as indicated by PLFA) significantly increased. Microbial biomass after cultivation was significantly higher in sediments from 30 m than from 150 m depth. Both microbial respiration and biomass increased after glucose addition.
    WorkplaceBiology Centre (since 2006)
    ContactDana Hypšová, eje@eje.cz, Tel.: 387 775 214
    Year of Publishing2012
Number of the records: 1  

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