Mycorrhizal fungi have a potential role in soil carbon storage under elevated CO2 and nitrogen deposition

By K. Treseder, M. Allen. 2000

415 citations recorded by the source corpus.

Subfields: Ecology, Plant Science, Soil Science

View Paper: https://www.semanticscholar.org/paper/7bedfea47436109bfffb470e974a52a139a0fe5d

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Citations in the corpus

Progressive N limitation of plant response to elevated CO2: a microbiological perspective (2006, background): “Mycorrhizal responses to elevated CO2 can be of special significance because mycorrhizae enhance plant nutrient acquisition and mycorrhizal biomass represents a significant C input (Treseder and Allen 2000; Staddon et al. 2003; Rillig 2004).”
Chronic nitrogen enrichment affects the structure and function of the soil microbial community in temperate hardwood and pine forests (2004, background): “Most studies examining the effects of N deposition on the microbial community have focused on mycorrhizal fungi (e.g., Arnolds, 1991; Dighton and Jansen, 1991; Egerton-Warburton and Allen, 2000; Treseder and Allen, 2000; Lilleskov et al., 2002a,b).”
Mycorrhizal mediation of plant N acquisition and residue decomposition: Impact of mineral N inputs (2006, background): “(Treseder & Allen, 2000), and glomalin, a glycoprotein produced by AM fungi, may contribute to C retention in soil because they can remain relatively undegraded in the soil for several years and even decades (Rillig et al., 2001).”
Community shifts and carbon translocation within metabolically-active rhizosphere microorganisms in grasslands under elevated CO 2 (2007, background): “…for ecosystem functioning as fungi are believed to play a positive role in soil structural stabilization (Bossuyt et al., 2001; Rillig et al., 2002), C sequestration (Treseder and Allen, 2000; Bailey et al., 2002) and N immo- bilization through hyphal translocation (Beare, 1997; Frey et al., 2000).”
The response of two Glomus mycorrhizal fungi and a fine endophyte to elevated atmospheric CO2, soil warming and drought (2004, background): “The available evidence, reviewed several times over the last few years, suggests that there is no direct effect of eCO2 on AM fungi (Staddon & Fitter, 1998; Rillig & Allen, 1999; Fitter et al., 2000; Treseder & Allen, 2000; Staddon et al., 2002).”
Arbuscular mycorrhizae and terrestrial ecosystem processes (2004, background): “AMF mycelium is frequently a dominant fraction of soil microbial biomass (Allen 1991; Miller et al. 1995; Rillig & Allen 1999; Treseder & Allen 2000; Zhu & Miller 2003).”
Dynamics of Fine Root, Fungal Rhizomorphs, and Soil Respiration in a Mixed Temperate Forest: Integrating Sensors and Observations (2008, background): “Rhizomorphs largely consist of newly fi xed carbon directly allocated from the leaves and only passing through the fi ne roots (Treseder and Allen, 2000; Olsson and Johnson, 2005; Godbold et al., 2006).”
Mycorrhizal fungi mediation of terrestrial ecosystem responses to global change: mini-review (2014, background): “Increasing atmospheric CO2 will impact functioning of mycorrhizal plants and their fungal associates with potential implications for ecosystem functioning (Rillig et al., 2000; Treseder and Allen, 2000; Parrent et al., 2006; Antoninka et al., 2011; Zavalloni et al., 2012).”
Linking soil process and microbial ecology in freshwater wetland ecosystems (2006, background): “While ecosystem ecologists have traditionally approached soils as a black box in which nutrient transformations are conducted by an uncharacterized community of microbes (Tiedje et al. 1999; Treseder and Allen 2000; Balser et al. 2001), this approach limits our ability to predict how or why belowgro”
Nitrogen addition alters ectomycorrhizal fungal communities and soil enzyme activities in a tropical montane forest (2017, background): “, 2011), mycelial growth rate (Wallander and Nylund, 1992), and colonization of root tips (Treseder and Allen, 2000; Peter et al., 2001), while nitrophilic species tend to increase in abundance.”