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Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter
J. Frouz, T. Cajthaml, B. Kříbek, P. Schaeffer, M. Bartuška, R. Galertová, P. Rojík, V. Krištůfek
Jazyk angličtina Země Česko
Typ dokumentu časopisecké články, práce podpořená grantem
- MeSH
- aerobióza MeSH
- Bacteria metabolismus MeSH
- biomasa MeSH
- extrakce na pevné fázi MeSH
- fosfolipidy analýza MeSH
- glukosa metabolismus MeSH
- houby metabolismus MeSH
- kyslík metabolismus MeSH
- mastné kyseliny analýza MeSH
- mikrobiální společenstva fyziologie MeSH
- plynová chromatografie s hmotnostně spektrometrickou detekcí MeSH
- půda analýza MeSH
- půdní mikrobiologie MeSH
- silikáty hliníku analýza klasifikace MeSH
- zkameněliny MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
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.
Biogeochemistry Group Université de Strasbourg UMR 7177 du CNRS ECPM
Institute for Environmental Studies Charles University
Institute of Soil Biology BC ASCR
Institute of Soil Biology BC ASCR Na Sádkách 7 CZ37005 České Budějovice Czech Republic
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