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Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter
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SYSNO ASEP 0367392 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Deep, 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) RIDSource Title Folia Microbiologica. - : Springer - ISSN 0015-5632
Roč. 56, č. 5 (2011), s. 389-396Number of pages 8 s. Language eng - English Country CZ - Czech Republic Keywords microflora ; biomass ; fossil organic matter Subject RIV EH - Ecology, Behaviour R&D Projects GA206/09/1642 GA ČR - Czech Science Foundation (CSF) CEZ AV0Z60660521 - UPB-H, BC-A (2005-2011) AV0Z50200510 - MBU-M (2005-2011) UT WOS 000295681100004 DOI 10.1007/s12223-011-0062-9 Annotation Three 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. Workplace Biology Centre (since 2006) Contact Dana Hypšová, eje@eje.cz, Tel.: 387 775 214 Year of Publishing 2012
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