Soil Biology & Biochemistry 39 si b H
orm e 1 o a atio ive s). fertilization, from 67 to 52 OTUs. Fungal community structure in litter differed significantly with N fertilization, primarily because fungi impacts on ecosystem processes and biological commu-nities. For example, N deposition increases N leaching and Lilleskov et al., 2001)...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.689.4193 http://allison.bio.uci.edu/publications/allison2007b.pdf |
| Summary: | orm e 1 o a atio ive s). fertilization, from 67 to 52 OTUs. Fungal community structure in litter differed significantly with N fertilization, primarily because fungi impacts on ecosystem processes and biological commu-nities. For example, N deposition increases N leaching and Lilleskov et al., 2001). However, climate change may lead to changes in N availability in these ecosystems. The IPCC Especially in arctic and boreal ecosystems, fungi play a major role in the decomposition and mineralization of N fertilization reduces mycorrhizal abundance by 15% (Treseder, 2004). However, mycorrhizal fungi are not believed to play a major role in organic carbon decom-ARTICLE IN PRESSposition (Read, 1991; Dighton, 2003), and the responses of decomposer fungi to N deposition remain largely untested. |
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