Relationships among fires, fungi, and soil dynamics in Alaskan Boreal Forests
By K. Treseder, Michelle C. Mack, Alison Cross. 2004
223 citations recorded by the source corpus.
Subfields: Insect Science, Plant Science, Soil Science
View Paper: https://www.semanticscholar.org/paper/4e3b821fb4470b4fc999dd11c44152b71c65d239
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Citations in the corpus
- Climate change feedbacks to microbial decomposition in boreal soils (2011, background): “Using a nearby set of fire chronosequence sites, Treseder et al. (2004) found that the diversity of bacteria and the abundance of ectomycorrhizal fungi required >15 yr to recover to preburn levels.”
- Global patterns of plant root colonization intensity by mycorrhizal fungi explained by climate and soil chemistry (2015, background): “, 2011; Veresoglou et al., 2012b). Here we take an essential step forward to obtain such quantifications, showing how the intensity of mycorrhizal colonization relates to soil fertility and climate. In 1990, based on expert knowledge, Read (1991) constructed the first qualitative global distribution”
- Low levels of nitrogen addition stimulate decomposition by boreal forest fungi (2009, methodology): “To accomplish this goal, we used substrates that comprise the major C inputs to mature black spruce forests (Treseder et al., 2004) and isolated fungi that are representative of the taxa present in clone libraries from field soils.”
- Soil fungal communities respond compositionally to recurring frequent prescribed burning in a managed southeastern US forest ecosystem (2015, background): “Despite the low intensity stripped head-fires used in our experimental implementation, our results are consistent with findings from other studies (Johnson and Curtis, 2001; Treseder et al., 2004; Mack et al., 2008; Amiro et al., 2010; Goulden et al., 2011; Dooley and Treseder, 2012; Holden et al., ”
- Nitrogen fertilization reduces diversity and alters community structure of active fungi in boreal ecosystems (2007, methodology): “We collected samples from two sites in east-central Alaska, USA (63 1 55 0 N, 145 1 44 0 W) described in detail by Treseder et al. (2004).”
- Influences of fire on forest soil fungal communities (2007, background): “Similarly, by comparing boreal forest stands that had been severely burned 3, 15, 45, or 80 years before sampling, Treseder et al. (2004) concluded that percent root colonization by ECM fungi was lower 3 years after fire, but had returned to preburn levels after 15 years.”
- Mycorrhizal responses to nitrogen fertilization in boreal ecosystems: potential consequences for soil carbon storage (2007, background): “N mineralization rates are highest in the middle-aged sites, and soil organic matter accumulates with site age (Treseder et al., 2004).”
- Fire severity influences the response of soil microbes to a boreal forest fire (2016, background): “Other studies have reported that ectomycorrhizal fungi are negatively affected by boreal forest fires, and this group can require up to 12–17 years to return to pre-fire abundance (Treseder et al 2004, Holden et al 2013).”
- Microbial activity and soil respiration under nitrogen addition in Alaskan boreal forest (2008, background): “We collected samples from a boreal forest site in central Alaska, USA (631550N, 1451440W), described in detail by Treseder et al. (2004).”