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Forests accumulate and store large amounts of carbon (C), and a sub # X2 G$ m" e! C, [) ^% Lstantial fraction of this stock is contained in deadwood. This transient pool is subject . K7 H3 k- Q8 w4 D: F, Ato decomposition by deadwood-associated organisms, and in this process it contrib$ g+ y7 s9 I" k; C. J
utes to CO2 , Z \/ y$ R' O/ c& Pemissions. Although fungi and bacteria are known to colonize dead & d) \& D& V6 U! e+ twood, little is known about the microbial processes that mediate carbon and nitro8 d* ]( A! F, t( J8 l* a% O
gen (N) cycling in deadwood. In this study, using a combination of metagenomics,. o8 a# Z4 I+ ^$ {. P( k
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom" K0 _7 d7 Q H! h" Z% u; s
position of deadwood reflflects the complementary roles played by fungi and bacteria. 3 b( B/ e0 I# j* f0 N' UFungi were found to dominate the decomposition of deadwood and particularly its re( R% l0 f$ L+ V7 ]7 K) F' Y: B
calcitrant fractions, while several bacterial taxa participate in N accumulation in dead+ `/ i% O) F; v- I
wood through N fifixation, being dependent on fungal activity with respect to deadwood ; P6 a, C9 d; K+ s2 Ccolonization and C supply. Conversely, bacterial N fifixation helps to decrease the con " `* ^. @8 u5 G5 I* i, ystraints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation 2 V! y- v7 v, H s; g$ s; \% lthat are a result of a joint action of deadwood bacteria and fungi may be signifificant for, H, M7 n/ o5 \: {1 x
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead: \3 N* ~3 v( j7 }
wood retention may help to improve the nutritional status and fertility of soils.! Z% p0 h+ B, c
. ], {6 P. Z9 y% p0 k% ]7 x! i1 f3 P. p# \% o& S0 z, [