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The effect of experimental warming and precipitation change on proteolytic enzyme activity: positive feedbacks to nitrogen availability are not universal
Author(s) -
Brzostek Edward R.,
Blair John M.,
Dukes Jeffrey S.,
Frey Serita D.,
Hobbie Sarah E.,
Melillo Jerry M.,
Mitchell Robert J.,
Pendall Elise,
Reich Peter B.,
Shaver Gaius R.,
Stefanski Artur,
Tjoelker Mark G.,
Finzi Adrien C.
Publication year - 2012
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2012.02685.x
Subject(s) - tundra , environmental science , climate change , evapotranspiration , nitrogen cycle , precipitation , temperate climate , nitrogen , water cycle , taiga , atmospheric sciences , arctic , global change , global warming , climatology , ecology , chemistry , biology , geography , meteorology , organic chemistry , geology
Nitrogen regulates the E arth's climate system by constraining the terrestrial sink for atmospheric CO 2 . Proteolytic enzymes are a principal driver of the within‐system cycle of soil nitrogen, yet there is little to no understanding of their response to climate change. Here, we use a single methodology to investigate potential proteolytic enzyme activity in soils from 16 global change experiments. We show that regardless of geographical location or experimental manipulation (i.e., temperature, precipitation, or both), all sites plotted along a single line relating the response ratio of potential proteolytic activity to soil moisture deficit, the difference between precipitation and evapotranspiration. In particular, warming and reductions in precipitation stimulated potential proteolytic activity in mesic sites – temperate and boreal forests, arctic tundra – whereas these manipulations suppressed potential activity in dry grasslands. This study provides a foundation for a simple representation of the impacts of climate change on a central component of the nitrogen cycle.