% h/ n7 c% ]9 Y6 I( m1 J) OForests accumulate and store large amounts of carbon (C), and a sub 6 F+ r I" Y( ]( estantial fraction of this stock is contained in deadwood. This transient pool is subject 4 R! V- ?8 F7 V5 q" Vto decomposition by deadwood-associated organisms, and in this process it contrib4 C0 m: g- t0 d! D5 r8 |
utes to CO2 ( l3 n! {% m; Zemissions. Although fungi and bacteria are known to colonize dead 0 l# q$ T) p' u- r) T8 ?wood, little is known about the microbial processes that mediate carbon and nitro0 L d* a- O5 @0 g% B- Y8 [9 G
gen (N) cycling in deadwood. In this study, using a combination of metagenomics,/ f; v& p# V! A& S/ W' ^
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom 3 F7 A3 A9 D. O2 _3 f7 i0 Pposition of deadwood reflflects the complementary roles played by fungi and bacteria.- R: _# f( f0 M q3 y) R3 f W
Fungi were found to dominate the decomposition of deadwood and particularly its re' `& G( D6 |& L1 j
calcitrant fractions, while several bacterial taxa participate in N accumulation in dead6 C( b4 z5 H8 W5 d, ]
wood through N fifixation, being dependent on fungal activity with respect to deadwood/ E! _' G6 ~4 X) ^
colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con1 a6 Z# }/ l% t
straints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation + u4 x$ w% N$ Vthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for4 X* l+ \) X( r& w3 p% H
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead# n/ \ |+ S+ r+ F9 i6 t) h/ e
wood retention may help to improve the nutritional status and fertility of soils.. n ~& Q: e' R# I2 f7 S/ r
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3 x0 e C- n7 i. E5 _, i$ i