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AM真菌在生态系统中的作用 7 `. v9 y1 A/ Q8 A 5 P6 P) N, G4 S+ `& Z5 i' @' p ) L7 e4 X7 W3 e# d3 |$ B0 q* H' P W( N3 m* ^1 V; \' H
: Q- z- O+ N( V; m9 g/ q1 QForests accumulate and store large amounts of carbon (C), and a sub - m. Q7 z; i5 ]$ ]. p: f- ustantial fraction of this stock is contained in deadwood. This transient pool is subject h+ `: K% I8 X( c zto decomposition by deadwood-associated organisms, and in this process it contrib% S6 Q' g# j3 \ x
utes to CO2 & F" Y* O' p9 D$ _& Y
emissions. Although fungi and bacteria are known to colonize dead + I( i0 V9 w5 V) W V. h6 pwood, little is known about the microbial processes that mediate carbon and nitro - {4 u9 f, B2 V# ggen (N) cycling in deadwood. In this study, using a combination of metagenomics, % M. K, `# R' F; ~metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom - q# k0 W- k3 S/ c4 i. {, c! c7 Zposition of deadwood reflflects the complementary roles played by fungi and bacteria.* Z7 D. }0 i( E P1 g
Fungi were found to dominate the decomposition of deadwood and particularly its re 5 }' S" x, O5 x6 Mcalcitrant fractions, while several bacterial taxa participate in N accumulation in dead 8 h- i) O0 s' zwood through N fifixation, being dependent on fungal activity with respect to deadwood( o! R) r) L1 y/ n# r
colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con ) V/ w3 b, k( E( Ostraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation + Z! O' P7 _. ~( H4 Rthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for7 |! c0 k: _5 [& Y$ ~
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead! a7 L$ E( H |! d M: K
wood retention may help to improve the nutritional status and fertility of soils. : K/ ]& q3 s+ g: q. z$ P" v& l2 R
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