Ecosystem Properties and Forest Decline in Contrasting Long-Term Chronosequences
By David A. Wardle, L. Walker, R. Bardgett. Science, 2004
1,045 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/56bb75c03bc9be1ffb401f5dcffb8834b92dc05d
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Global and Planetary Change
- D. Peltzer
- David A. Wardle
- Nicholas A. J. Graham
- G. Yeates
- Han Y. H. Chen
- Jens Kattge
- Benjamin L Turner
- R. Bardgett
In Nature and Landscape Conservation
- David A. Wardle
- D. Peltzer
- J. H. C. Cornelissen
- R. Bardgett
- G. T. Freschet
- Rien Aerts
- G. Yeates
- Benjamin L Turner
Citations in the corpus
- Tamm Review: On the nature of the nitrogen limitation to plant growth in Fennoscandian boreal forests (2017, background): “It has been speculated that boreal forests should develop a P deficiency also on mineral soils, like the tropical forests, if they are allowed to develop for a long time without major disturbances (Wardle et al., 2004).”
- Changes in the community structure and diversity of soil invertebrates across the Franz Josef Glacier chronosequence (2008, methodology): “…previously been shown that tree community composition varies strongly with ratios of C to N, C to P and N to P in the soil across the sequence (Richardson et al., 2004; Wardle et al., 2004b), and the present study shows that this is also largely true for the soil invertebrate community (Table 5).”
- Species‐ and community‐level patterns in fine root traits along a 120 000‐year soil chronosequence in temperate rain forest (2011, background): “This is a key area of research given the increasing awareness of the role that below-ground processes play in regulating plant–soil interactions and determining ecosystem responses to global change (Coomes & Grubb 2000;Wardle et al. 2004; Orwin et al. 2010).”
- Linking vegetation change, carbon sequestration and biodiversity: insights from island ecosystems in a long‐term natural experiment (2012, background): “A key emerging trend is that there is a greater level of specificity between the plant and associated soil communities than has historically been assumed (Wardle et al. 2004a; Bezemer et al. 2010; Eisenhauer et al. 2010).”
- Quantifying photosynthetic capacity and its relationship to leaf nitrogen content for global‐scale terrestrial biosphere models (2009, background): “Thus, leaf nitrogen content should only have a minor impact on photosynthetic capacity (Wardle et al., 2004).”
- Priming and microbial nutrient limitation in lowland tropical forest soils of contrasting fertility (2012, background): “4) and with later retrogressional and therefore less fertile stages of soil development (Allison et al. 2007; Wardle et al. 2008).”
- The hare, the tortoise and the crocodile: the ecology of angiosperm dominance, conifer persistence and fern filtering (2005, neutral): “P depletion contributed to the substantial changes in the stoichiometry of C : N : P in plants and soils (Tables 1 & 2), and the resulting increase in P limitation is likely to have had major consequences (Koerselman & Meuleman 1996; Elser et al. 2000; Tessier & Raynal 2003; Wardle et al. 2004).”
- Soil acidification and adaptations of plants and microorganisms in Bornean tropical forests (2014, background): “Several studies on soil weathering sequences have shown that nutrient deficiency can eventually limit net primary production (NPP) in most tropical forests (Schuur and Matson 2001; Austin 2002; Wardle et al. 2004).”
- Hurricane disturbance accelerates invasion by the alien tree Pittosporum undulatum in Jamaican montane rain forests (2005, background): “In the extensive plots, its invasion (Pittosporum basal area in 2004) was negatively related to soil N concentration, and its growth rates were positively related to soil N:P; five of the nine plots from which Pittosporum growth data could be calculated had soil N:P that exceeded the Redfield ratio ”