Influence of balsam poplar tannin fractions on carbon and nitrogen dynamics in Alaskan taiga floodplain soils
By Noah Fierer, J. Schimel, R. Cates, Jiping Zou. 2001
290 citations recorded by the source corpus.
Subfields: Environmental Chemistry, Health, Toxicology and Mutagenesis, Soil Science
View Paper: https://www.semanticscholar.org/paper/f96d6a571b3b5b2ce697217318579c9642150d3b
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Citations in the corpus
- Plant secondary metabolites: a key driver of litter decomposition and soil nutrient cycling (2016, background): “At the genetic level, Schweitzer et al. (2004) found marked differences among cottonwood hybrids (Populus fremontii L. 9 P. angustifolia James) in terms of foliar levels of condensed tannins, which ranged from 1% to 10% of leaf dry matter.”
- Tannins in nutrient dynamics of forest ecosystems - a review (2003, background): “Fierer et al. (2001) reported that poplar tannins added to several soils did not inhibit the extracellular enzymes endocellulase, phenol oxidase, peroxidase and β-glucosidase, although any effects may have been masked by high variability.”
- Microbial N immobilization is of great importance in acidified mountain spruce forest soils (2013, background): “Simple organic N molecules have been shown to be the major source of N while mineral N forms usually account for a smaller proportion of N uptake (Fierer et al., 2001; Schimel and Bennett, 2004; Finzi and Berthrong, 2005).”
- Biological, ecological and agronomic significance of plant phenolic compounds in rhizosphere of the symbiotic legumes (2007, background): “…2000); increase of microbial activity when used as carbon source (Sparling et al., 1981; Schimel et al., 1996; Schmidt et al., 1997; Blum, 1998; Fierer et al., 2001); N immobilization (Shafer and Blum, 1991; Sugai and Schimel, 1993; Schimel et al., 1996; Blum, 1998) and direct inhibition of…”
- Secondary metabolites of Pinus halepensis alter decomposer organisms and litter decomposition during afforestation of abandoned agricultural zones (2014, background): “…added to microcosms and mainly concern the impact of tannins (Schimel et al. 1996; Bradley, Titus & Preston 2000; H€attenschwiler & Vitousek 2000; Fierer et al. 2001; Schofield, Mbugua & Pell 2001; Kraus, Dahlgren & Zasoski 2003) or monoterpenoids (White 1986, 1991, 1994; Bremner & McCarty…”
- Bacterial and fungal contributions to soil nitrogen cycling under Douglas fir and red alder at two sites in Oregon (2008, result): “These results suggest that heterotrophic bacteria and fungi in forest systems may rely primarily on organic N for building biomass (Fierer et al., 2001; Schimel and Bennett, 2004).”
- Soil nitrogen cycling rates in low arctic shrub tundra are enhanced by litter feedbacks (2010, background): “For instance, it has been suggested that the isotope pool dilution procedure for determining gross N cycling rates may be recording microbial recycling of small pools of labile N, and thus may not be a good indication of soil organic matter decomposition processes (Fierer et al. 2001).”
- Nitrogen cycling in a northern hardwood forest: Do species matter? (2004, background): “1995), acting as general microbial inhibitors or as sources of labile C (Schimel et al. 1998; Fierer et al. 2001), or specifically inhibiting nitrification (Baldwin et al.”