9 @% ^: i: p, x1 ]- G 9 P$ X. ]( \3 s, w 9 f! Y( T: N& {# m' F3 O) MForests accumulate and store large amounts of carbon (C), and a sub 7 W# H3 U# S4 b }5 k0 [stantial fraction of this stock is contained in deadwood. This transient pool is subject 5 D+ e9 Y" j+ y. A8 f) f ^4 Nto decomposition by deadwood-associated organisms, and in this process it contrib+ P* x6 {: T& i) P9 w W
utes to CO2 h* {' q+ z9 F! U) J& V" A J
emissions. Although fungi and bacteria are known to colonize dead # F- H( q0 }7 [$ I3 u) Twood, little is known about the microbial processes that mediate carbon and nitro . w3 o1 r1 V) ^# M2 y. Wgen (N) cycling in deadwood. In this study, using a combination of metagenomics,2 p0 H# W9 u. x) D8 q% U, p8 b# P
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom ; B& \& K: `- K9 l5 j% ]position of deadwood reflflects the complementary roles played by fungi and bacteria. 6 ?2 y" K; W% z" [. B. VFungi were found to dominate the decomposition of deadwood and particularly its re + ]4 w& N1 D/ S1 B: i6 y. ~- ~calcitrant fractions, while several bacterial taxa participate in N accumulation in dead% |! n* r$ ^' J* b
wood through N fifixation, being dependent on fungal activity with respect to deadwood$ N% D Z7 H- l5 S' g6 ~6 [
colonization and C supply. Conversely, bacterial N fifixation helps to decrease the con0 a) v2 R; g/ p$ T5 J
straints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation/ g4 T8 J Z; f* ~4 I. m
that are a result of a joint action of deadwood bacteria and fungi may be signifificant for / F) _( z' o& |' u) ?" n& hnutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead 4 [ }8 ^4 k- qwood retention may help to improve the nutritional status and fertility of soils. ) g% u# H) ]+ ^9 |3 y, w; n5 i) k4 y9 }0 A8 l' h1 x4 e5 t& C
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