Microbial responses to experimental soil warming: Five testable hypotheses
Abstract
Soil microbes are key regulators of Earth's biogeochemical cycles, and their growth, turnover, and efficiency are important controls of organic matter decay and soil carbon (C) storage. A central roadblock to scaling microbial activity is explaining the incongruence between long- and short-term warming responses. In addition to the well-described kinetics which dominate the short-term warming response, the long-term response is also subject to indirect effects, such as substrate availability, soil moisture, and shifts in plant community composition, that influence microbial activity and community dynamics. Here we discuss possible mechanisms of this attenuation, synthesized in the context of five testable hypotheses, presented in order of decreasing current empirical support.
Department
Soil Biogeochemistry and Microbial Ecology
Publication Date
4-19-2019
Journal Title
Ecosystem Consequences of Soil Warming: Microbes, Vegetation, Fauna and Soil Biogeochemistry
Publisher
Elsevier
Digital Object Identifier (DOI)
Document Type
Book Chapter
Recommended Citation
Kristen M. DeAngelis, Priyanka Roy Chowdhury, Grace Pold, Adriana Romero-Olivares, Serita Frey, Chapter 6 - Microbial responses to experimental soil warming: Five testable hypotheses, Editor(s): Jacqueline E. Mohan, Ecosystem Consequences of Soil Warming, Academic Press, 2019, Pages 141-156, ISBN 9780128134931, https://doi.org/10.1016/B978-0-12-813493-1.00007-7.
Rights
© 2019 Elsevier Inc. All rights reserved.