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AM真菌在生态系统中的作用 9 R# S# O, e" O( w' `. ~4 P9 H/ @. M ; t6 ]+ Q5 F5 r1 z5 B6 a% \; y ) \, u/ g! o4 z4 O- Z7 C: u: e0 ?/ c! a- E6 _/ p
( ^* G! l# r) U8 uForests accumulate and store large amounts of carbon (C), and a sub 4 y F% p( O, q: Q& estantial fraction of this stock is contained in deadwood. This transient pool is subject# L$ p/ d" K: e6 A" W
to decomposition by deadwood-associated organisms, and in this process it contrib , x# ]2 C. S5 C# Z3 {$ \utes to CO2 / I {5 G# V0 I9 v/ {6 m
emissions. Although fungi and bacteria are known to colonize dead, y- o; ?- b' B. }* r
wood, little is known about the microbial processes that mediate carbon and nitro 2 w4 V0 x6 D3 b% s, [gen (N) cycling in deadwood. In this study, using a combination of metagenomics, & B- b x; W I! E; g4 Xmetatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom ) _% i. r6 E$ z) |2 A: e8 gposition of deadwood reflflects the complementary roles played by fungi and bacteria.' k4 P; C8 s( x5 u2 [$ b: _
Fungi were found to dominate the decomposition of deadwood and particularly its re ( E% l! d! I0 C: k" Scalcitrant fractions, while several bacterial taxa participate in N accumulation in dead g5 Z( o) U8 U3 L, u c7 a
wood through N fifixation, being dependent on fungal activity with respect to deadwood % J& p/ S* m5 t1 e' l& Acolonization and C supply. Conversely, bacterial N fifixation helps to decrease the con* v9 Z3 u# B0 v
straints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation( }, ?7 X& c6 H
that are a result of a joint action of deadwood bacteria and fungi may be signifificant for; j7 e4 m+ [8 M( |: r3 l
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead 0 P; U f7 P! c1 y: @wood retention may help to improve the nutritional status and fertility of soils. * p9 e" x$ D' @" b+ V: z+ w/ F* l3 Y$ R
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