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Wiley, New Phytologist, 4(201), p. 1431-1439, 2013

DOI: 10.1111/nph.12578

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Fungal functioning in a pine forest: Evidence from a 15N-labeled global change experiment

This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Abstract

We used natural and tracer nitrogen (N) isotopes in a Pinus taeda free air CO2 enrichment (FACE) experiment to investigate functioning of ectomycorrhizal and saprotrophic fungi in N cycling. Fungal sporocarps were sampled in 2004 (natural abundance and (15) N tracer) and 2010 (tracer) and δ(15) N patterns were compared against litter and soil pools. Ectomycorrhizal fungi with hydrophobic ectomycorrhizas (e.g. Cortinarius and Tricholoma) acquired N from the Oea horizon or deeper. Taxa with hydrophilic ectomycorrhizas acquired N from the Oi horizon (Russula and Lactarius) or deeper (Laccaria, Inocybe, and Amanita). (15) N enrichment patterns for Cortinarius and Amanita in 2010 did not correspond to any measured bulk pool, suggesting that a persistent pool of active organic N supplied these two taxa. Saprotrophic fungi could be separated into those colonizing pine cones (Baeospora), wood, litter (Oi), and soil (Ramariopsis), with δ(15) N of taxa reflecting substrate differences. (15) N enrichment between sources and sporocarps varied across taxa and contributed to δ(15) N patterns. Natural abundance and (15) N tracers proved useful for tracking N from different depths into fungal taxa, generally corresponded to literature estimates of fungal activity within soil profiles, and provided new insights into interpreting natural abundance δ(15) N patterns.