Biotic interactions mediate soil microbial feedbacks to climate change
Jazyk angličtina Země Spojené státy americké Médium print-electronic
Typ dokumentu časopisecké články, práce podpořená grantem, Research Support, U.S. Gov't, Non-P.H.S.
PubMed
26038557
PubMed Central
PMC4460469
DOI
10.1073/pnas.1502956112
PII: 1502956112
Knihovny.cz E-zdroje
- Klíčová slova
- biotic interaction, bottom-up control, global change, soil feedback, top-down control,
- MeSH
- analýza rozptylu MeSH
- dusík metabolismus MeSH
- houby fyziologie MeSH
- Isopoda fyziologie MeSH
- klimatické změny * MeSH
- potravní řetězec * MeSH
- půdní mikrobiologie * MeSH
- teoretické modely * MeSH
- zpětná vazba * MeSH
- zvířata MeSH
- Check Tag
- zvířata MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Research Support, U.S. Gov't, Non-P.H.S. MeSH
- Geografické názvy
- Massachusetts MeSH
- Názvy látek
- dusík MeSH
Decomposition of organic material by soil microbes generates an annual global release of 50-75 Pg carbon to the atmosphere, ∼7.5-9 times that of anthropogenic emissions worldwide. This process is sensitive to global change factors, which can drive carbon cycle-climate feedbacks with the potential to enhance atmospheric warming. Although the effects of interacting global change factors on soil microbial activity have been a widespread ecological focus, the regulatory effects of interspecific interactions are rarely considered in climate feedback studies. We explore the potential of soil animals to mediate microbial responses to warming and nitrogen enrichment within a long-term, field-based global change study. The combination of global change factors alleviated the bottom-up limitations on fungal growth, stimulating enzyme production and decomposition rates in the absence of soil animals. However, increased fungal biomass also stimulated consumption rates by soil invertebrates, restoring microbial process rates to levels observed under ambient conditions. Our results support the contemporary theory that top-down control in soil food webs is apparent only in the absence of bottom-up limitation. As such, when global change factors alleviate the bottom-up limitations on microbial activity, top-down control becomes an increasingly important regulatory force with the capacity to dampen the strength of positive carbon cycle-climate feedbacks.
Department of Environmental Sciences University of Helsinki FI 00014 Finland;
Department of Natural Resources and the Environment University of New Hampshire Durham NH 03824
Yale School of Forestry and Environmental Studies Yale University New Haven CT 06511;
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