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AM真菌在生态系统中的作用3 `9 j' W! T3 q9 i
2 u5 J) R9 u: {) P2 W& \ 6 P+ i) m0 ^: x: y- T8 R8 V, S% L $ W5 V# N/ C/ G 5 u" Q1 ?" }* sForests accumulate and store large amounts of carbon (C), and a sub, |4 v/ w( X8 l3 x$ W# x* N1 y p
stantial fraction of this stock is contained in deadwood. This transient pool is subject 9 P6 h. q2 ?. o7 \5 k# f3 j* ^to decomposition by deadwood-associated organisms, and in this process it contrib7 |5 J! ?, x' C* [
utes to CO2 , Y! c% y9 l" ]/ w
emissions. Although fungi and bacteria are known to colonize dead # i$ Q R) C& v2 j; Qwood, little is known about the microbial processes that mediate carbon and nitro( @- d+ h, { y: D/ u. M
gen (N) cycling in deadwood. In this study, using a combination of metagenomics, 7 |; ~% V' B+ Z6 @6 e" rmetatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom : d5 G! O# U/ s3 \/ oposition of deadwood reflflects the complementary roles played by fungi and bacteria. ' @. J" U9 o" s$ v; mFungi were found to dominate the decomposition of deadwood and particularly its re - E8 k4 { c# W+ r: W0 Y6 |calcitrant fractions, while several bacterial taxa participate in N accumulation in dead # k5 q9 W3 M% A4 J: X0 awood through N fifixation, being dependent on fungal activity with respect to deadwood5 R! _0 ~ k# i3 Y& m% @
colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con5 S, |+ u+ ]0 m) e8 N; v
straints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation & B! N+ Q; u7 I) h$ fthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for2 m/ g6 A" V4 G/ v; E
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead) j0 \, p o5 O/ r: o. C
wood retention may help to improve the nutritional status and fertility of soils.0 @) H, J5 c; t* L. A( K- O
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