2001
DOI: 10.1098/rspb.2001.1844
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Reconstruction of the historical changes in mycorrhizal fungal communities under anthropogenic nitrogen deposition

Abstract: Archived soil samples (1937^1999) and historic air quality data from the Los Angeles Basin were used for reconstructing the record of change between atmospheric NO x loads, soil d 15 N values and the diversity of arbuscular mycorrhizae (AM), which are ubiquitous plant^fungus mutualists that control plant community productivity. A tripling of atmospheric NO x loads between 1937 and the 1970s was paralleled by soil nitrogen enrichment (d 15 N 3.18). From 1975 onwards, atmospheric NO x declined, but soils became… Show more

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Cited by 59 publications
(31 citation statements)
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“…Three previously common mycorrhizal genera disappeared from the mycorrhizal spore community in soil and one large-spored genus (Gigasopora) was no longer found in plant roots. N enrichment also enhanced the proliferation of potentially less-mutualistic species of small-spored genus Glomus, which may have implications for plant community succession in the face of chronic N deposition (Egerton-Warburton et al 2001).…”
Section: Mediterranean Vegetationmentioning
confidence: 99%
See 1 more Smart Citation
“…Three previously common mycorrhizal genera disappeared from the mycorrhizal spore community in soil and one large-spored genus (Gigasopora) was no longer found in plant roots. N enrichment also enhanced the proliferation of potentially less-mutualistic species of small-spored genus Glomus, which may have implications for plant community succession in the face of chronic N deposition (Egerton-Warburton et al 2001).…”
Section: Mediterranean Vegetationmentioning
confidence: 99%
“…& Arn. near Los Angeles was associated with dramatic changes in the mycorrhizal community (Egerton-Warburton et al 2001). Diversity, species richness, and productivity of the arbuscular mycorrhizal community had deteriorated severely by 1969.…”
Section: Mediterranean Vegetationmentioning
confidence: 99%
“…Soil nitrogen varies because of natural and anthropogenic inputs into soils and since the industrial revolution atmospheric deposition has dramatically polluted some soils with reactive forms of nitrogen [35][36][37][38][39]. Assuming that host-control traits are costly to express [12,40], similar to other plant defences against bacteria [41,42], we predict that host control will be downregulated in nitrogen-rich soils, where hosts can gain nitrogen primarily from less costly mineral sources [43] rather than symbionts.…”
Section: Introductionmentioning
confidence: 99%
“…Most atmospheric N r deposition into terrestrial ecosystems likely occurs on historically nitrogen-limited soils (Vitousek et al 1997;Padgett et al 1999;Egerton-Warburton et al 2001). N r deposition and the resultant fertilization of soils can reduce plant species richness (Roem et al 2002;Carroll et al 2003;Maskell et al 2006;Clark and Tilman 2008;Maskell et al 2010) by altering outcomes of competitive interactions among plants, and by making the environment unfavorable for nitrogen-sensitive species (Bobbink et al 2010).…”
Section: Introductionmentioning
confidence: 99%