+ E) b& i. o/ W& ^% CAM真菌在生态系统中的作用 7 b/ p! k2 {6 s5 M2 g. q& z % [" B. i. Z* J! t$ U 8 Q7 |& ~. T3 ~# R I; W- ~- N; L3 X$ _6 R$ c) z
1 Q/ z* e, }9 G- U1 I6 X, S) TForests accumulate and store large amounts of carbon (C), and a sub ! U2 R6 j3 M' b; H) G6 vstantial fraction of this stock is contained in deadwood. This transient pool is subject 3 Q3 u7 |+ l; O- g+ d! ] m+ nto decomposition by deadwood-associated organisms, and in this process it contrib& f6 Z, \# |3 S& }) K7 ~ m
utes to CO2 5 \' g# U2 O3 R# ]' d# H. |emissions. Although fungi and bacteria are known to colonize dead 7 E6 N. Y7 ?4 U, Ewood, little is known about the microbial processes that mediate carbon and nitro 4 B4 M, y& F6 L/ hgen (N) cycling in deadwood. In this study, using a combination of metagenomics, O; G4 u8 w4 D3 Y' v8 s; S
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom ' Z3 }$ m% w) r( S6 K6 C% q2 Xposition of deadwood reflflects the complementary roles played by fungi and bacteria. ) z. }8 s. H- g) Q, `2 oFungi were found to dominate the decomposition of deadwood and particularly its re. c4 I3 E0 q- A# j7 x
calcitrant fractions, while several bacterial taxa participate in N accumulation in dead : o" d8 b6 d- J- W7 Hwood through N fifixation, being dependent on fungal activity with respect to deadwood, Q2 k7 _: r+ d$ l9 e: u
colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con 2 C8 R, t& {- A0 z m ]7 Q' ]straints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation+ l& _2 d/ q/ B7 d/ ?0 t, L* z
that are a result of a joint action of deadwood bacteria and fungi may be signifificant for: ~8 |* A8 y! O! V: A
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead : e7 H2 n9 P0 W2 Q+ \9 Pwood retention may help to improve the nutritional status and fertility of soils. 4 y& U9 S$ x3 } 2 f- S) F7 d8 o# W1 `, h4 ?& }' Y: x3 p5 ~. z