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AM真菌在生态系统中的作用9 L; k% b* C! V- J+ {
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/ w2 ^8 d c4 E# F ~* n3 s6 }Forests accumulate and store large amounts of carbon (C), and a sub 8 W1 A3 s2 W3 j( D$ A# W( tstantial fraction of this stock is contained in deadwood. This transient pool is subject 7 A; g" E! Z7 Dto decomposition by deadwood-associated organisms, and in this process it contrib # r' r l0 [$ Y; K1 z) t& s5 Nutes to CO2 1 b5 o4 B8 i4 k, w+ oemissions. Although fungi and bacteria are known to colonize dead 9 }; G$ A. `" X/ \1 w' K3 kwood, little is known about the microbial processes that mediate carbon and nitro ' F7 T; V1 J7 v# lgen (N) cycling in deadwood. In this study, using a combination of metagenomics,; V/ ?, P! L, U3 r1 c$ n$ P- X
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom / G ^( w0 |* k. e7 xposition of deadwood reflflects the complementary roles played by fungi and bacteria.# C& u; p& [- @; V! c) p" a: k
Fungi were found to dominate the decomposition of deadwood and particularly its re . ~% `( R4 ^5 y0 z% M, c, ^calcitrant fractions, while several bacterial taxa participate in N accumulation in dead( l; C5 z3 O+ c# B: O# G4 l: L }
wood through N fifixation, being dependent on fungal activity with respect to deadwood' n8 {( S3 W2 J' P
colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con7 M- m2 W1 g2 d: K
straints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation2 t' ~/ n! t* X; t
that are a result of a joint action of deadwood bacteria and fungi may be signifificant for 7 X: y9 i! l; Q$ y& snutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead 6 r1 x% T1 A" I# w$ L J0 h B$ bwood retention may help to improve the nutritional status and fertility of soils. 1 m; `8 U8 Q: h) P$ N2 A: p4 I , t d+ i2 N) [- ~% e 7 e/ m6 [) A# e