! v' { X$ w4 G5 D( A" J$ `! y& xForests accumulate and store large amounts of carbon (C), and a sub $ _8 ~( a+ F! fstantial fraction of this stock is contained in deadwood. This transient pool is subject / d: E2 ^, z4 L) K! N$ pto decomposition by deadwood-associated organisms, and in this process it contrib7 B3 ^4 i4 f* C @; A) R0 d. Z
utes to CO2 2 K' C0 e- K0 C4 `emissions. Although fungi and bacteria are known to colonize dead 6 u$ N/ X3 E& y2 Y- L2 mwood, little is known about the microbial processes that mediate carbon and nitro 8 R4 Z; U3 `' V2 P/ l+ rgen (N) cycling in deadwood. In this study, using a combination of metagenomics,0 e& r( s( ]3 R' ^$ n7 r
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom; Y# P' x% u7 z6 I+ E
position of deadwood reflflects the complementary roles played by fungi and bacteria. 7 b% `& M& x/ a' s& u, aFungi were found to dominate the decomposition of deadwood and particularly its re# s# w! B: e/ ~! u' k
calcitrant fractions, while several bacterial taxa participate in N accumulation in dead ; Z; Z" Q' j, R0 g$ L* M2 mwood through N fifixation, being dependent on fungal activity with respect to deadwood7 p8 J) _( \5 \$ [# z9 |0 i# z5 s* t
colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con 6 m! S! c1 T/ O& I7 l& Pstraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation4 i& p$ e3 Y) V f. M
that are a result of a joint action of deadwood bacteria and fungi may be signifificant for ], `% v# n0 i' ^: h. [! Anutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead- @4 m# a( o1 n1 R7 I! k% a
wood retention may help to improve the nutritional status and fertility of soils., M, u, @/ _2 X. I' v( O. A, ~
& ?% x1 g4 g- [. G: X+ H