About: Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter     Goto   Sponge   NotDistinct   Permalink

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  • 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.
  • 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. (en)
Title
  • Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter
  • Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter (en)
skos:prefLabel
  • Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter
  • Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter (en)
skos:notation
  • RIV/61388971:_____/11:00367392!RIV12-AV0-61388971
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(GA206/09/1642), Z(AV0Z50200510), Z(AV0Z60660521), Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika
  • 5
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 193086
http://linked.open...ai/riv/idVysledku
  • RIV/61388971:_____/11:00367392
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • microflora; biomass; fossil organic matter (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [7F9664D23A8C]
http://linked.open...i/riv/nazevZdroje
  • Folia Microbiologica
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 56
http://linked.open...iv/tvurceVysledku
  • Cajthaml, Tomáš
  • Frouz, Jan
  • Krištůfek, Václav
  • Rojík, P.
  • Bartuška, Martin
  • Galertová, R.
  • Kříbek, B.
  • Schaeffer, P.
http://linked.open...ain/vavai/riv/wos
  • 000295681100004
http://linked.open...n/vavai/riv/zamer
issn
  • 0015-5632
number of pages
http://bibframe.org/vocab/doi
  • 10.1007/s12223-011-0062-9
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