Interactions and Self-Organization in the Soil-Microbe Complex

By Iain M. Young, John W. Crawford. Science, 2004

903 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Evolution, Behavior and Systematics, Oceanography

View Paper: https://www.semanticscholar.org/paper/2cc9bddea07f4adc73c843e8b11adb03ac9ec7ed

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Citations in the corpus

Bacterial-fungal interactions: ecology, mechanisms and challenges. (2018, background): “In addition, BFI tend to be dynamic (Young and Crawford 2004; Hennessy 2017b).”
Hydration and diffusion processes shape microbial community organization and function in model soil aggregates (2015, background): “Such small-scale interactions are crucial for capturing emergent soil profile responses and require modeling and process description at the pore scale where microbial cells interacts with their neighbors [Young and Crawford, 2004; Or et al., 2007].”
Rhizosphere processes and management in plant-assisted bioremediation (phytoremediation) of soils (2009, background): “Roots create pores which can improve connectivity and diffusivity of the soil (Young and Crawford 2004) thus facilitating mass flow and diffusion of water and pollutants.”
How Deep Can Surface Signals Be Traced in the Critical Zone? Merging Biodiversity with Biogeochemistry Research in a Central German Muschelkalk Landscape (2016, background): “These interfaces are organized in a complex, dynamic, and hierarchical system (Young and Crawford, 2004; Totsche et al., 2010) and can be conceived as a “biogeochemical reactor” that transforms the water, gases and other materials that pass through it.”
Modelling the rhizosphere: a review of methods for ‘upscaling’ to the whole‐plant scale (2006, background): “The networks of pores in which biological and chemical activity occurs and through which solutes and water move are complex three-dimensional structures (Young et al., 2001; Young & Crawford, 2004).”
Three-dimensional quantification of intra-aggregate pore-space features using synchrotron-radiation-based microtomography (2008, background): “First steps in relating physical and biological process in the microenvironment have been reported by Young and Crawford (2004) and Tokunaga et al. (2003).”
Dynamics of bacterial communities in relation to soil aggregate formation during the decomposition of 13C-labelled rice straw (2012, background): “structure, and therefore the functioning, of the resident microbial communities (Young and Crawford, 2004).”
Soil textural heterogeneity impacts bacterial but not fungal diversity (2020, background): “Soil heterogeneity both drives and is driven by microbial diversity and function (Young and Crawford, 2004).”
Embracing the unknown: disentangling the complexities of the soil microbiome (2017, background): “2) , far less than 1% of the available soil surface area is typically occupied by microorganisms 16 , which suggests that there are biotic or abiotic constraints on the microbial colonization of soil surfaces.”
Rhizosphere Spatiotemporal Organization–A Key to Rhizosphere Functions (2018, methodology): “To our knowledge, the self-organization concept has not been applied to the rhizosphere although it has been discussed for soils (Phillips, 1998; Young and Crawford, 2004; Lavelle et al., 2016), soil-microbe complexes (Young and Crawford, 2004), mycorrhizal networks (Simard, 2009), microbial biofilm”