Počet záznamů: 1

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

SYSNO ASEP	0367392
Druh ASEP	J - Článek v odborném periodiku
Zařazení RIV	J - Článek v odborném periodiku
Poddruh J	Článek ve WOS
Název	Deep, subsurface microflora after excavation respiration and biomass and its potential role in degradation of fossil organic matter
Tvůrce(i)	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
Zdroj.dok.	Folia Microbiologica. - : Springer - ISSN 0015-5632 Roč. 56, č. 5 (2011), s. 389-396
Poč.str.	8 s.
Jazyk dok.	eng - angličtina
Země vyd.	CZ - Česká republika
Klíč. slova	microflora ; biomass ; fossil organic matter
Vědní obor RIV	EH - Ekologie - společenstva
CEP	GA206/09/1642 GA ČR - Grantová agentura ČR
CEZ	AV0Z60660521 - UPB-H, BC-A (2005-2011)
	AV0Z50200510 - MBU-M (2005-2011)
UT WOS	000295681100004
DOI	10.1007/s12223-011-0062-9
Anotace	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.
Pracoviště	Biologické centrum (od r. 2006)
Kontakt	Dana Hypšová, eje@eje.cz, Tel.: 387 775 214
Rok sběru	2012

Počet záznamů: 1