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松林中的真菌功能:来自一项¹⁵N标记的全球变化实验的证据。

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

作者信息

Hobbie Erik A, van Diepen Linda T A, Lilleskov Erik A, Ouimette Andrew P, Finzi Adrien C, Hofmockel Kirsten S

机构信息

Earth Systems Research Center, University of New Hampshire, Durham, NH, 03824, USA.

Department of Natural Resources and the Environment, University of New Hampshire, Durham, NH, 03824, USA.

出版信息

New Phytol. 2014 Mar;201(4):1431-1439. doi: 10.1111/nph.12578. Epub 2013 Nov 7.

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.

摘要

• 我们在火炬松自由空气CO₂ 浓度增加(FACE)实验中使用天然氮和示踪氮同位素来研究外生菌根真菌和腐生真菌在氮循环中的功能。

• 2004年(天然丰度和¹⁵N示踪)和2010年(示踪)采集了真菌子实体,并将δ¹⁵N模式与凋落物和土壤库进行了比较。

• 具有疏水外生菌根的外生菌根真菌(如丝膜菌属和口蘑属)从Oea层或更深层获取氮。具有亲水外生菌根的分类群从Oi层(红菇属和乳菇属)或更深层(蜡壳耳属、丝盖伞属和鹅膏菌属)获取氮。2010年丝膜菌属和鹅膏菌属的¹⁵N富集模式与任何测量的总体库都不对应,这表明存在一个持续的活性有机氮库为这两个分类群提供氮源。腐生真菌可分为定殖在松果(小孢霉属)、木材、凋落物(Oi)和土壤(拟枝瑚菌属)上的真菌,分类群的δ¹⁵N反映了底物差异。不同分类群的源与子实体之间的¹⁵N富集情况各不相同,并导致了δ¹⁵N模式的差异。

• 天然丰度和¹⁵N示踪剂被证明有助于追踪不同深度的氮进入真菌分类群,总体上与土壤剖面内真菌活性的文献估计相符,并为解释天然丰度δ¹⁵N模式提供了新的见解。

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