2 O n2 h# `( h6 y. |AM真菌在生态系统中的作用4 C, `0 z% s8 x( W
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Forests accumulate and store large amounts of carbon (C), and a sub 8 m" t/ g4 e( c5 {- ~$ t( zstantial fraction of this stock is contained in deadwood. This transient pool is subject 5 k! {# ^4 }$ Vto decomposition by deadwood-associated organisms, and in this process it contrib: P- A3 r( Z S$ L
utes to CO2 ; }6 }' r8 m a5 S9 A% U
emissions. Although fungi and bacteria are known to colonize dead ( a E" A6 z- W& m8 |wood, little is known about the microbial processes that mediate carbon and nitro2 i* x. a, f& E: \. G/ T. [
gen (N) cycling in deadwood. In this study, using a combination of metagenomics, & q2 U* |: [1 l' G4 m4 s; \; wmetatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom " C, c! Q, c. X/ E8 bposition of deadwood reflflects the complementary roles played by fungi and bacteria.9 V, u; l4 t; U! Z& ?
Fungi were found to dominate the decomposition of deadwood and particularly its re . k7 ?, e9 A. E) E- s3 S' Ecalcitrant fractions, while several bacterial taxa participate in N accumulation in dead # q/ ]+ i H% m0 U& U0 Y0 Rwood through N fifixation, being dependent on fungal activity with respect to deadwood. R1 J: ]4 w- ?! x& C& e9 T3 I; k
colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con " b L4 i7 |% g0 rstraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation : W) \& A, P8 S1 ]5 i; j8 C7 Lthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for9 a% g: g. g: v
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead" R# [* T/ Y, U Y
wood retention may help to improve the nutritional status and fertility of soils. 1 m( E) R% Y- W/ o # H7 M3 T, |. m- R* J' r4 ^8 ?/ q3 g5 ?) z5 A5 h1 Q