A temporal approach to linking aboveground and belowground ecology.
By R. Bardgett, W. Bowman, R. Kaufmann, S. K. Schmidt. Trends in Ecology & Evolution, 2005
868 citations recorded by the source corpus.
Subfields: Ecology, Ecology, Evolution, Behavior and Systematics, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/82b1379ec026b82bb1e1015286d96dbc1174f64c
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Ecology
- R. Bardgett
- Noah Fierer
- Y. Kuzyakov
- David A. Wardle
- D. Peltzer
- W. H. van der Putten
- S. Lavorel
- Jizhong Zhou
In Ecology, Evolution, Behavior and Systematics
- W. H. van der Putten
- Peter B. Reich
- R. Bardgett
- S. Lavorel
- David A. Wardle
- Fernando T. Maestre
- J. H. C. Cornelissen
- T. Martijn Bezemer
In Nature and Landscape Conservation
- Peter B. Reich
- W. H. van der Putten
- S. Lavorel
- David A. Wardle
- R. Bardgett
- J. H. C. Cornelissen
- D. Peltzer
- C. Violle
Citations in the corpus
- Adapt or disperse: understanding species persistence in a changing world (2010, background): “Interaction networks of terrestrial ecosystems extend to both aboveground and belowground components that are closely interlinked (Wardle et al., 2004; Bardgett et al., 2005; De Deyn & van der Putten, 2005).”
- Chemical and Biological Gradients along the Damma Glacier Soil Chronosequence, Switzerland (2011, neutral): “In addition, it is also necessary to consider different temporal fluctuations and conduct sampling at different timescales (daily to seasonal) to obtain a better understanding of the relationships between microbial groups and belowground and aboveground ecology (Bardgett et al., 2005).”
- Microbe-mediated plant-soil feedback causes historical contingency effects in plant community assembly (2007, background): “However, the role of such feedbacks in temporal plant community dynamics has received little attention (Bardgett et al. 2005, BarteltRyser et al. 2005, Kardol et al. 2006).”
- Biotic plant–soil feedbacks across temporal scales (2013, background): “from mutualists such as mycorrhizal fungi (Bardgett et al. 2005).”
- Bridging the gap between micro - and macro-scale perspectives on the role of microbial communities in global change ecology (2006, background): “We are increasing our understanding of the nested hierarchy of drivers acting at varying spatial and temporal scales that impact microbial communities, as well as beginning to quantify the potential role of microbial community composition as an independent controlling variable in ecosystem functioni”
- Temporal variation in plant-soil feedback controls succession. (2006, background): “Therefore, an integrated above-belowground approach will be required (Wardle 2002; Bardgett et al. 2005 ).”
- Stoichiometric imbalances between terrestrial decomposer communities and their resources: mechanisms and implications of microbial adaptations to their resources (2014, background): “Unlike C and P, N has no specific storage pool beside small, intermittent accumulation of essential amino acids, and no significant N storage in microbes has been reported to date (e.g., Banham and Whatley, 1991).”
- Soil microbial community under a nurse-plant species changes in composition, biomass and activity as the nurse grows (2013, background): “However, the role of such interactions in plant community dynamics with time has received little attention (Bardgett et al., 2005; Bartelt-Ryser et al., 2005; Kardol et al., 2006).”
- Inoculation with a Native Soil Community Advances Succession in a Grassland Restoration (2012, background): “Late successional species may suffer less from negative soil feedbacks and can benefit from 218 Restoration Ecology Vol. 20, No. 2, pp. 218–226 MARCH 2012 an increase in mycorrhizal densities (Janos 1980; Bever 2003; Bardgett et al. 2005; Kardol et al. 2007; Kulmatiski et al. 2008).”
- Is Tree Species Diversity or Species Identity the More Important Driver of Soil Carbon Stocks, C/N Ratio, and pH? (2016, background): “…can be a 354 result of higher variety of litter substrates to decomposers and thereby higher activities of soil organisms in 355 diverse forests (Bardgett et al., 2005; Wardle et al., 2006), but it remains to be further documented whether 356 higher decomposition rates in litter mixtures (Ball…”