Resource partitioning for soil phosphorus: a hypothesis

By Benjamin L Turner. 2008

349 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Industrial and Manufacturing Engineering, Soil Science

View Paper: https://www.semanticscholar.org/paper/c971b638e433ff787d61e373648843def87341ef

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In Environmental Chemistry

In Industrial and Manufacturing Engineering

In Soil Science

Citations in the corpus

Linking vegetation change, carbon sequestration and biodiversity: insights from island ecosystems in a long‐term natural experiment (2012, background): “The chemical composition of the soil P pool is increasingly recognized as of ecological importance (Turner 2008); in this system, NaOH-extractable P (which is recalcitrant) increases with decreasing island size, while membraneextractable P (which has high biological availability) decreases (Lagerstr”
Contribution of interspecific interactions and phosphorus application to sustainable and productive intercropping systems (2013, background): “, 2008) or different fractions of each of these pools (Turner, 2008).”
Changes in coexistence mechanisms along a long‐term soil chronosequence revealed by functional trait diversity (2012, background): “adaptation for use of P sources requiring more or less investment for uptake) might also permit coexistence when P is limiting (Turner 2008), and this might not necessarily manifest itself in foliar or root trait divergence.”
Decreased soil organic P fraction associated with ectomycorrhizal fungal activity to meet increased P demand under N application in a subtropical forest ecosystem (2017, background): “Soil organic P turnover is thought to influence labile P. Turner (2008) summarized previous studies and concluded that organic P is abundant in soil and its turnover can supply a considerable fraction of the P taken up by natural vegetation.”
Strong plant-soil associations in a heterogeneous subtropical broad-leaved forest (2011, background): “tion of Fe-bound and Al-bound phosphorus or the partitioning of organic phosphorus may provide other ways for species to coexist by reducing competitions (Oluleye et al. 2008; Turner 2008).”
Does phosphorus limitation promote species-rich plant communities? (2011, neutral): “ Turner 2008 ). From this, I would predict a greater diversity of uptake mechanisms for P than for N, though this assumption requires to be confirmed with data.”
Nitrogen inputs accelerate phosphorus cycling rates across a wide variety of terrestrial ecosystems. (2012, neutral): “Where data were not presented in tables, DataThief (Tummers, 2006) was used to acquire numbers from figures.”
Contrasting effects of plant inter‐ and intraspecific variation on community‐level trait measures along an environmental gradient (2013, background): “in the intraspecific responses of LNC and LNP to elevation may reflect differences in plant species preferences for distinct forms of nutrients (McKane et al. 2002; Turner 2008) as shifts in the relative availability of different forms of N and P can occur with elevation (Sundqvist et al.”
Multiple phosphorus acquisition strategies adopted by fine roots in low-fertility soils in Central Amazonia (2019, positive): “Additionally, the lack of correlation (neither negative nor positive) between AM colonisation and root APase could suggest the possible complementary role of both strategies (Steidinger et al. 2015; Turner 2008).”
Nitrogen and phosphorus interact to control tropical symbiotic N2 fixation: a test in Inga punctata (2013, background): “Both mechanisms could allow the plant to access additional phosphorus (Robson et al. 1981; Joner et al. 2000; Wang et al. 2007; Houlton et al. 2008; Turner 2008; Baribault et al. 2012).”
Ectomycorrhizal fungi: the symbiotic route to the root for phosphorus in forest soils (2011, background): “Organic forms of P, largely refractory inositol phosphates (eg phytic acid), simple phosphomonoesters (eg mononucleotides and sugar phosphates) and phosphodiesters (eg nucleic acids and phospholipids), can constitute a large proportion of the P pool in forest soils (Paul and Clark 1989; Tibbett 2002”