Linking vegetation change, carbon sequestration and biodiversity: insights from island ecosystems in a long‐term natural experiment
By David A. Wardle, M. Jonsson, Sheel Bansal, R. Bardgett, M. Gundale, D. Metcalfe. 2012
253 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/8ad5106bbcecebb39dcfe907b177971e39d617b3
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
In Global and Planetary Change
- W. H. van der Putten
- David A. Wardle
- James D. Bever
- R. Bardgett
- T. Martijn Bezemer
- B. Casper
- T. Fukami
- Paul Kardol
In Nature and Landscape Conservation
- W. H. van der Putten
- R. Bardgett
- David A. Wardle
- T. Martijn Bezemer
- T. Fukami
- Paul Kardol
- James D. Bever
- Tess F. J. van de Voorde
Citations in the corpus
- The Role of Plant Litter in Driving Plant-Soil Feedbacks (2019, background): “As a result, secondary metabolites can contribute to litter-mediated PSFs via impeding nutrient cycling (Wardle et al., 2012).”
- Plant–soil feedbacks: the past, the present and future challenges (2013, background): “Handley’s (1954) work on Calluna vulgaris in the UK and work on Swedish islands reported by Wardle et al. (2012) shows that plant species can impede rates of N mineralization by producing litter with high levels of polyphenols, which adversely affects earlier-successional plant species…”
- Bacterial communities in soil mimic patterns of vegetative succession and ecosystem climax but are resilient to change between seasons (2013, background): “It is not well-known, however, how these processes of long-term ecosystem development, vegetative succession, and pedogenesis are related to changes in soil microbial communities (Wardle et al., 2012).”
- Soil networks become more connected and take up more carbon as nature restoration progresses (2017, unknown): “Second, increased tightening could be due to declined nutrient availability in the soil along the successional gradient 19,29-30 , which may enhance the necessity of stronger cooperative and trophic interactions between functional groups of soil biota.”