Variable use of plant- and soil-derived carbon by microorganisms in agricultural soils

By C. Kramer, G. Gleixner. 2006

307 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/222fe6aabadd67de38289feca99d36c5888eb13e

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Citations in the corpus

Grazing triggers soil carbon loss by altering plant roots and their control on soil microbial community (2009, methodology): “PLFA and their d13C signature were analysed according to Zelles (1999) and Kramer & Gleixner (2006).”
Soil-carbon preservation through habitat constraints and biological limitations on decomposer activity (2008, unknown): “This suggests a preferential incorporation of modern C derived from root residues and root exudates (Rethemeyer et al., 2004, 2005; Kramer and Gleixner, 2006).”
Mechanisms of real and apparent priming effects and their dependence on soil microbial biomass and community structure: critical review (2008, background): “Only few studies have shown that PEs initiated by different substrates are accompanied by changes in composition of soil microbial community (Bell et al. 2003; Blagodatskaya et al. 2007; Falchini et al. 2003; Kramer and Gleixner 2006; Landi et al. 2006).”
Temperature and substrate controls on microbial phospholipid fatty acid composition during incubation of grassland soils contrasting in organic matter quality. (2009, background): “, 2003), whilst Gram-negative bacteria are more dependent on the input of fresh organic material to create ‘‘hot spots’’ of decomposition in soils (Griffiths et al., 1999; Kramer and Gleixner, 2006; Potthoff et al., 2006).”
Stimulation of Plant Growth through Interactions of Bacteria and Protozoa: Testing the Auxiliary Microbial Loop Hypothesis (2012, background): “Kramer and Gleixner (2006) and later Nottingham et al. (2009) used the change in stable-C isotopic signature in natural field soils after a change from C3 to C4 plants to investigate the change in carbon signature in rhizosphere microorganisms.”
Soil organic matter dynamics: a biological perspective derived from the use of compound-specific isotopes studies (2013, methodology): “This was recently done using two field sites differing in the 14C content of soil organic matter (Kramer and Gleixner 2006).”
Plant species influence microbial diversity and carbon allocation in the rhizosphere (2010, methodology): “All d 13C values were corrected for the addition of the extra C atom introduced to the molecule during methylation, using the mass balance equation of Kramer and Gleixner (2006).”
Active microorganisms in soil: Critical review of estimation criteria and approaches (2013, background): “Phospholipid fatty acids (PLFA) are found only in living cells and thus are characteristic biomarkers for living microorganisms (Zelles,1999; Kramer and Gleixner, 2006; Denef et al., 2009).”
Seasonal differences in tree species influence on soil microbial communities (2013, background): “Gram-negative bacteria are associated with root activity (Kramer and Gleixner, 2006), a relationship that has been confirmed by several 13C-labeling studies showing a particular association of specific monounsaturated fatty acids such as PLFA 16:1u5, 16:1u7, 16:1u9, 17:1u8 and 18:1u7 with highly enr”