Microbial stress-response physiology and its implications for ecosystem function.

By J. Schimel, T. Balser, M. Wallenstein. Ecology, 2007

2,385 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/f7ab2c8324b0aaa08bf53f16b7bd68c716185f60

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In Soil Science

Citations in the corpus

Effects of past and current drought on the composition and diversity of soil microbial communities (2019, background): “Taken together, this could suggest important changes in the future functioning of the bacterial community in soils exposed to water stress, for example relating to carbon and nutrient cycling (Schimel et al., 2007; Frank et al., 2015).”
Responses of soil bacterial and fungal communities to extreme desiccation and rewetting (2013, background): “…strategies to survive desiccation and rewetting (Potts, 1994; Griffin, 1977), including: (i) the accumulation of compatible solutes (see review by Schimel et al., 2007); (ii) exopolysaccharide production, extensively studied in Pseudomonas sp. (Roberson and Firestone, 1992; Chang et al., 2007)…”
Impacts of multiple extreme winter warming events on sub‐Arctic heathland: phenology, reproduction, growth, and CO2 flux responses (2011, background): “Increased freeze–thaw cycles are assumed to have large impacts on soil microbial communities of these ecosystems that affect N cycling (Grogan et al., 2004; Schimel et al., 2007; Yergeau & Kowalchuk, 2008).”
Responses of ammonia-oxidizing bacteria and archaea to nitrogen fertilization and precipitation increment in a typical temperate steppe in Inner Mongolia (2013, background): “Microorganisms have evolved different strategies to adapt to oisture stresses, depending on their evolutionary adaptations and hysiological acclimation mechanisms (Schimel et al., 2007).”
Microbial control over carbon cycling in soil (2012, background): “Stress response compounds It has been argued that microorganisms physiologically acclimate to survive stresses such as low water potential or freezing by accumulating cytoplasmic constituents such as osmolytes or cryoprotectants (Schimel et al., 2007).”
Fungal communities are more sensitive indicators to non-extreme soil moisture variations than bacterial communities (2015, background): “Indeed, it is well documented that when soil 317 water potential decreases, the metabolic activity of some microbial species is decreased 318 (Schimel et al., 2007; Manzoni et al., 2012).”