ausblenden:
Schlagwörter:
Compound-specific c-14
Compound-specific c-13
Gram-negative bacteria
Gram-positive bacteria
C3/C4 vegetation change
Natural isotope
Labeling
Microbial community structure
Methane-oxidizing bacteria
Fatty-acid profiles
Organic-matter
Individual compounds
C-14 analysis
Biomass
Ratios
Lipids
Transformation
Zusammenfassung:
In this study we used compound specific C-13 and C-14 isotopic signatures to determine the degree to which recent plant material and older soil organic matter (SOM) served as carbon substrates for microorganisms in soils. We determined the degree to which plant-derived carbon was used as a substrate by comparison of the C-13 content of microbial phospholipid fatty acids (PLFA) from soils of two sites that had undergone a vegetation change from C3 to C4 plants in the past 20-30 years. The importance of much older SOM as a substrate was determined by comparison of the radiocarbon content of PLFA from soils of two sites that had different C-14 concentrations of SOM. The C-13 shift in PLFA from the two sites that had experienced different vegetation history indicated that 40-90% of the PLFA carbon had been fixed since the vegetation change took place. Thus PLFA were more enriched in 13C from the new C4 vegetation than it was observed for bulk SOM indicating recent plant material as preferentially used substrate for soil microorganisms. The largest C-13 shift of PLFA was observed in the soil that had high C-14 Concentrations of bulk SOM. These results reinforce that organic carbon in this soil for the most part cycles rapidly. The degree to which SOM is incorporated into microbial PLFA was determined by the difference in C-14 concentration of PLFA derived from two soils one with high C-14 concentrations of bulk SOM and one with low. These results showed that 0-40% of SOM carbon is used as substrate for soil microorganisms. Furthermore a different substrate usage was identified for different microorganisms. Gram-negative bacteria were found to prefer recent plant material as microbial carbon source while Gram-positive bacteria use substantial amounts of SOM carbon. This was indicated by C-13 as well as C-14 signatures of their PLFA. Our results find evidence to support 'priming' in that PLFA indicative of Gram-negative bacteria associated with roots contain both plant- and SOM-derived C. Most interestingly, we find PLFA indicative of archeobacteria (methanothrophs) that may indicate the use of other carbon sources than plant material and SOM to a substantial amount suggesting that inert or slow carbon pools are not essential to explain carbon dynamics in soil. (c) 2006 Elsevier Ltd. All rights reserved. [References: 58]
