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Joshua P. Schimel

Researcher at University of California, Santa Barbara

Publications -  197
Citations -  34815

Joshua P. Schimel is an academic researcher from University of California, Santa Barbara. The author has contributed to research in topics: Soil water & Tundra. The author has an hindex of 83, co-authored 187 publications receiving 29476 citations. Previous affiliations of Joshua P. Schimel include University of Alaska Fairbanks & United States Geological Survey.

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Nitrogen mineralization: challenges of a changing paradigm

TL;DR: A complete new conceptual model of the soil N cycle needs to incorporate recent research on plant–microbe competition and microsite processes to explain the dynamics of N across the wide range of N availability found in terrestrial ecosystems.
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Microbial stress‐response physiology and its implications for ecosystem function

TL;DR: It is suggested that more effectively integrating microbial ecology into ecosystem ecology will require a more complete integration of microbial physiological ecology, population biology, and process ecology.
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Variations in microbial community composition through two soil depth profiles

TL;DR: Using PLFAs as biomarkers, it is shown that Gram-positive bacteria and actinomycetes tended to increase in proportional abundance with increasing soil depth, while the abundances of Gram-negative bacteria, fungi, and protozoa were highest at the soil surface and substantially lower in the subsurface.
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The implications of exoenzyme activity on microbial carbon and nitrogen limitation in soil: a theoretical model

TL;DR: A simple theoretical model is built to explore the behavior of the decomposition–microbial growth system when the fundamental kinetic assumption is changed from first order kinetics to exoenzymes catalyzed decomposition (dC/dt=KC×Enzymes).
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Role of Land-Surface Changes in Arctic Summer Warming

TL;DR: It is shown that terrestrial changes in summer albedo contribute substantially to recent high-latitude warming trends and the continuation of current trends in shrub and tree expansion could further amplify this atmospheric heating by two to seven times.