, H$ f, ^' f! m: eAM真菌在生态系统中的作用 ( J, u& `8 t( F9 d7 a5 e: T k6 g: t
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Forests accumulate and store large amounts of carbon (C), and a sub, }2 A% b1 s$ m& Z0 v: u6 o
stantial fraction of this stock is contained in deadwood. This transient pool is subject & [: J. Z: J6 c0 nto decomposition by deadwood-associated organisms, and in this process it contrib7 m- ], z4 {) F3 p3 a
utes to CO2 ! O4 s. `% |5 _5 ~
emissions. Although fungi and bacteria are known to colonize dead: @* `8 F I, [
wood, little is known about the microbial processes that mediate carbon and nitro) W4 e' a0 O. O' `0 Y, ~! B
gen (N) cycling in deadwood. In this study, using a combination of metagenomics, " X: R. Q2 I3 q- t5 emetatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom 7 P4 V2 @. U- ? A" `position of deadwood reflflects the complementary roles played by fungi and bacteria.: I3 Z/ a9 X D+ c: I4 d C/ q
Fungi were found to dominate the decomposition of deadwood and particularly its re - j: W. v. o( w+ u% u$ Vcalcitrant fractions, while several bacterial taxa participate in N accumulation in dead 8 W. a! i7 p5 W" b2 Bwood through N fifixation, being dependent on fungal activity with respect to deadwood 1 W& v9 ?1 p0 H6 c& ?, z4 u: C) I3 k$ ccolonization and C supply. Conversely, bacterial N fifixation helps to decrease the con 8 u; k/ Z$ o% y- a* h bstraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation + Z) g6 ~$ a3 G8 R" uthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for ( I6 f; b* D1 H& Fnutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead - l, t% g' n: _. m& W- O2 E8 E& i8 pwood retention may help to improve the nutritional status and fertility of soils./ S; b. M/ W% t
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