Arbuscular mycorrhizal fungi contribute to 13C and 15N enrichment of soil organic matter in forest soils

被引:30
作者
Etcheverria, Paulina [2 ]
Huygens, Dries [1 ]
Godoy, Roberto [3 ]
Borie, Fernando [2 ]
Boeckx, Pascal [4 ]
机构
[1] Univ Austral Chile, Fac Ciencias Agr, Inst Ingn Agr & Suelos, Valdivia, Chile
[2] Univ La Frontera, Dept Ciencias Quim, Temuco, Chile
[3] Univ Austral Chile, Fac Ciencias, Inst Bot, Valdivia, Chile
[4] Univ Ghent, Fac Biosci Engn, Lab Appl Phys Chem, ISOFYS, B-9000 Ghent, Belgium
关键词
Glomalin-related soil protein (GRSP); Arbuscular mycorrhizal fungi; Pristine forest; delta N-15; delta C-13; Isotope enrichment; Chile; NATURAL-ABUNDANCE; ISOTOPIC FRACTIONATION; NITROGEN; GLOMALIN; PROTEIN; CARBON; DECOMPOSITION; POOLS; DISCRIMINATION; EXTRACTION;
D O I
10.1016/j.soilbio.2009.01.018
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Increasing evidence suggests that accretion of microbial turnover products is an important driver for isotopic carbon (C) and nitrogen (N) enrichment of soil organic matter (SOM). However, the exact contribution of arbuscular mycorrhizal fungi (AMF) to soil isotopic patterns remains unknown. in this study, we compared C-13 and N-15 patterns of glomalin-related soil protein (GRSP), which includes a main fraction derived from AMF, litter, and bulk soil in four temperate rainforests. GRSP was an abundant C and N pool in these forest soils, showing significant C-13 and N-15 enrichment relative to litter and bulk soil. Hence, cumulative accumulation of recalcitrant AMF turnover products in the soil profile likely contributes to C-13 and N-15 enrichment in forest soils. Further research on the relationship between GRSP and AMF should clarify the exact extent of this process. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:858 / 861
页数:4
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