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AM真菌在生态系统中的作用 8 o# H8 u3 U4 i0 K5 V# n: b! a 7 V( y7 @/ f- x1 I+ |/ R % v# G- y9 W! {# W5 N. y4 C# x( |" N( _8 O2 D; r( _
0 J4 L# G. Y0 l C) X" R- d5 U8 EForests accumulate and store large amounts of carbon (C), and a sub " K- H q9 O. ?stantial fraction of this stock is contained in deadwood. This transient pool is subject& V) j6 e, m: L E& U/ ?
to decomposition by deadwood-associated organisms, and in this process it contrib+ y' |! a! l7 f+ g
utes to CO2 ' t: y2 {, X7 r1 C! iemissions. Although fungi and bacteria are known to colonize dead* Z4 n1 P! l- k2 e6 i
wood, little is known about the microbial processes that mediate carbon and nitro / Q; ^5 V: I6 s& g( J7 _% E) T8 k6 h Jgen (N) cycling in deadwood. In this study, using a combination of metagenomics, 7 E/ o3 x' T w r3 ~metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom# M" N/ F: A' D) S/ K* t g- O, w5 i
position of deadwood reflflects the complementary roles played by fungi and bacteria." q0 m7 b( Y P6 g9 b9 |- _$ o
Fungi were found to dominate the decomposition of deadwood and particularly its re& L ^3 h& g5 ~/ Y9 A
calcitrant fractions, while several bacterial taxa participate in N accumulation in dead6 w* R4 [6 `0 Z( k
wood through N fifixation, being dependent on fungal activity with respect to deadwood c/ Q! b' e5 R; g' S# |colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con 0 ?( n9 A" v `* c; r* x$ t6 Rstraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation 6 x( z* F. e6 C' y& Y; y+ Bthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for, c+ |# |- X3 }
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead ! ~4 ]! s& R6 `0 P, L0 p" `$ W3 J- lwood retention may help to improve the nutritional status and fertility of soils.0 c( a* I. d; G b2 B
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