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AM真菌在生态系统中的作用9 r# g! e7 {8 P) o6 V2 F7 J" \8 L) j
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' ^! }" H' v% T8 X- _1 n3 E : O! [3 _7 d, Q! @Forests accumulate and store large amounts of carbon (C), and a sub7 \; [% O4 V+ h( A9 m
stantial fraction of this stock is contained in deadwood. This transient pool is subject + X3 H/ z: B$ k' T1 i' o+ @* j) ato decomposition by deadwood-associated organisms, and in this process it contrib2 @( }2 n* U5 s
utes to CO2 - W& q1 \+ g3 Y
emissions. Although fungi and bacteria are known to colonize dead # C& V8 P5 ^. C6 r/ _% Rwood, little is known about the microbial processes that mediate carbon and nitro" b: N* z+ K+ B8 ~
gen (N) cycling in deadwood. In this study, using a combination of metagenomics, 1 `& O8 r% k7 y5 R& F, _1 [metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom " V- T0 _4 G7 b- [) W2 [# H; s) i$ cposition of deadwood reflflects the complementary roles played by fungi and bacteria." L" G* [0 d' o5 S' e/ T! B
Fungi were found to dominate the decomposition of deadwood and particularly its re / |& ~% }) o' d0 t% a5 _calcitrant fractions, while several bacterial taxa participate in N accumulation in dead 2 C( w* E# t. J- H% a9 |2 cwood through N fifixation, being dependent on fungal activity with respect to deadwood 5 W) F/ c3 ]4 C3 }; I0 V. ncolonization and C supply. Conversely, bacterial N fifixation helps to decrease the con % p0 e7 M1 j3 T, r" wstraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation 1 s, _% I" v. pthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for ' Y( ~9 I8 P) Z7 [2 `3 ynutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead8 }$ C! S. [- b
wood retention may help to improve the nutritional status and fertility of soils. 2 ~- ]2 s7 P; w( l4 C: ^ ' _( k* R+ t& |* f& M8 w5 @2 r1 J- c1 A y) C