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AM真菌在生态系统中的作用( W) X Y e$ u4 m8 x( R7 x9 k
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Forests accumulate and store large amounts of carbon (C), and a sub 8 }+ d9 l0 B$ K) d' ^7 g. Pstantial fraction of this stock is contained in deadwood. This transient pool is subject! b( U: O D1 `6 W6 k; t" l
to decomposition by deadwood-associated organisms, and in this process it contrib ]4 I% i1 E. u6 U3 A+ |utes to CO2 . M2 A$ h1 n, N* K6 `
emissions. Although fungi and bacteria are known to colonize dead; j% q9 g' y2 ~) u7 {: y+ S% u5 M
wood, little is known about the microbial processes that mediate carbon and nitro1 j4 q2 A( d& e9 Z9 O4 [* t) i& Z
gen (N) cycling in deadwood. In this study, using a combination of metagenomics,& O! m+ \1 l+ u* E+ ]( v2 s
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom # O! ^: d9 w" M: P) m% Vposition of deadwood reflflects the complementary roles played by fungi and bacteria. 6 r E3 |/ ?$ C' `( M- z$ T; [Fungi were found to dominate the decomposition of deadwood and particularly its re 0 t, a! g) A. b- J5 [ qcalcitrant fractions, while several bacterial taxa participate in N accumulation in dead6 h E7 O M& F6 I y# Q/ _
wood through N fifixation, being dependent on fungal activity with respect to deadwood . B; n+ j0 z8 M5 C) Ccolonization and C supply. Conversely, bacterial N fifixation helps to decrease the con , r/ i7 H& l- R! ^2 o, Wstraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation * Y% T/ x( u+ y" ethat are a result of a joint action of deadwood bacteria and fungi may be signifificant for/ p$ `7 C( W1 }
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead* I3 }/ E3 ~ {0 b# W! {: n( K
wood retention may help to improve the nutritional status and fertility of soils. 3 y6 y5 a6 Y+ ^+ C% k8 W& N7 ^- p+ f1 O) ]