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Bardgett, R.

Publications and source records attributed to Bardgett, R..

2 recordsLinked to original sources

Maximum entropy networks predict fluctuations and stability of food web energetics

A central goal of ecology is understanding how the architecture of food webs, which represent the structural backbone of ecosystems, affects their stability. The analysis of stability in the classical sense of population dynamics (i.e. return to equilibrium) can be successful for a single instance of an empirical food web but ignores the multiplicity of alternative states in which the system could be found as a result of intrinsic variability and fluctuations. Here we propose and test a new methodology to reconstruct, from single empirical observations of a food web, the viable ensemble of alternative realizations respecting the observed resource-consumer linkages and empirical ener-getics. The reconstruction can be handled analytically within a maximum-entropy framework which predicts how empirical food webs access a multitude of alternative states with comparable stability and reactivity. The (measurable) entropy of the reconstructed ensemble directly quantifies this multiplicity and serves as a novel proxy of system resilience, that is the rate of return to equilibrium in response to an external perturbation. We show that the associated ensemble fluctuations provide explicit predictions for the expected response of food webs to external perturbations, such as anthropogenic or climate-induced stresses. We do that by validating the proposed fluctuation-response relation on empirical soil food webs subjected to experimentally controlled perturbations, confirming that intrinsic fluctuations in the unperturbed state predict responses to subsequent stresses. The perturbed states are associated with higher entropy, indicating less likely spontaneous recovery.

ecology↗

No enhancement of soil carbon persistence by sheep grazing in a long-term calcareous grassland experiment

Soils hold a globally important carbon pool that is generally more persistent than the carbon stored in plant biomass. However, this carbon is becoming increasingly vulnerable to disturbances such as soil warming, fire, and erosion. Managing land to increase soil carbon sequestration and persistence may therefore improve long-term soil carbon storage and contribute to climate change mitigation. It has been hypothesized that grazing by large herbivores may enhance the persistence of soil carbon by increasing the amount of soil organic matter forming more stable associations with mineral particles (mineral-associated organic matter). We compared sheep-grazed and ungrazed plots within the Gibson Grazing and Successional Experiment located in the Upper Seeds calcareous grassland in Wytham Woods, Oxfordshire, using organic matter fractionation to estimate the surface (0-5 cm) carbon stocks in the mineral-associated and particulate organic matter fractions. Counter to predictions, after 35 years sheep grazing had not increased mineral-associated organic matter carbon stocks relative to ungrazed plots. We hypothesize that this indicates the saturation of mineral surfaces in both grazed and ungrazed treatments and the inability of grazing to increase soil nitrogen stocks and decrease pH to levels conducive for mineral-associated carbon sequestration. Only one of twelve soil properties examined showed statistically detectable responses to grazing: spring-grazing increased the C:N ratio in the mineral-associated organic matter. While the number of tests performed (24) means this may be a false-positive result, if genuine it would be consistent with a more direct pathway from plant exudates to mineral-associated organic matter formation due to compensatory growth in response to spring-grazing. Overall, the results of this long-term experiment do not support the hypothesis that grazing can improve the persistence of the soil carbon pool.

ecology↗