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AM真菌在生态系统中的作用* F3 u& x7 B6 P
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Forests accumulate and store large amounts of carbon (C), and a sub 9 r8 t& A( H0 A( h/ p/ _9 ?stantial fraction of this stock is contained in deadwood. This transient pool is subject . _; p# W; J9 A& Dto decomposition by deadwood-associated organisms, and in this process it contrib& v/ W. H) n. L m! ~
utes to CO2 2 K/ j3 _; g% q
emissions. Although fungi and bacteria are known to colonize dead - O. u, ]) R& N5 i: t2 m/ Vwood, little is known about the microbial processes that mediate carbon and nitro , w# ^1 m/ }5 Z- zgen (N) cycling in deadwood. In this study, using a combination of metagenomics,0 O. ~- u0 a: O) \( N
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom : R/ [ s$ C# X* k& y* ]6 jposition of deadwood reflflects the complementary roles played by fungi and bacteria.8 I4 L9 m% m# s: r
Fungi were found to dominate the decomposition of deadwood and particularly its re ) L3 V# ?2 W: I6 P8 Xcalcitrant fractions, while several bacterial taxa participate in N accumulation in dead) J: G6 k5 E* w+ d! e: g
wood through N fifixation, being dependent on fungal activity with respect to deadwood 2 `/ d+ B5 L" T" u5 Ucolonization and C supply. Conversely, bacterial N fifixation helps to decrease the con* q6 R" {$ u( V1 c( y* D: i2 ?2 E
straints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation % Q$ L% |3 P& R0 f& Bthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for # h# T8 a3 A* j' `; y1 U' Enutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead4 K3 G m" S7 u" A. J# G! u
wood retention may help to improve the nutritional status and fertility of soils. - K6 T% W3 r4 z! @ * t9 a5 _; o' S ( J2 A. Z. R( t2 K, O