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AM真菌在生态系统中的作用 J9 C1 ~" n; i9 h2 O5 Y
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Forests accumulate and store large amounts of carbon (C), and a sub4 p6 C `% D5 o" ~" P8 K
stantial fraction of this stock is contained in deadwood. This transient pool is subject ' O3 H- [ c* j0 U6 r! Fto decomposition by deadwood-associated organisms, and in this process it contrib , @/ y2 b& c4 f9 p V2 t$ l3 Wutes to CO2 ! o8 t5 ^7 |3 D, w$ e
emissions. Although fungi and bacteria are known to colonize dead5 e# [" X9 T% ?7 b2 j
wood, little is known about the microbial processes that mediate carbon and nitro+ ^! Q6 P/ K2 [- A. f
gen (N) cycling in deadwood. In this study, using a combination of metagenomics, 4 c }) i( o- e" ]. U7 mmetatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom 0 U* u- p R' N! P, Yposition of deadwood reflflects the complementary roles played by fungi and bacteria.! X4 V; n v# x' J- F9 q, n
Fungi were found to dominate the decomposition of deadwood and particularly its re6 ?8 n- V- O, _( q1 Q
calcitrant fractions, while several bacterial taxa participate in N accumulation in dead / _* w. c. S9 x1 P1 ^) ?1 F' Swood through N fifixation, being dependent on fungal activity with respect to deadwood 8 _: v! F ]% Dcolonization and C supply. Conversely, bacterial N fifixation helps to decrease the con # Z& e0 ~$ C5 w' t% Pstraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation ) O" [' P, y! c' H8 e( }4 ?$ \that are a result of a joint action of deadwood bacteria and fungi may be signifificant for1 o$ I* `$ g% B
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead/ }% F: y6 n& O
wood retention may help to improve the nutritional status and fertility of soils. ! S- F3 k$ M7 @. ?4 w: B; _2 ?, d5 y* z/ {1 c0 p& H, A) K
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