0 f8 v5 A- v+ @( c1 _6 s) {$ u+ y/ T T) x: V# B3 _7 a
Forests accumulate and store large amounts of carbon (C), and a sub+ b) q6 D" G1 o* z
stantial fraction of this stock is contained in deadwood. This transient pool is subject : l6 V, J0 j7 b( f, g& tto decomposition by deadwood-associated organisms, and in this process it contrib & }! { F f+ A, g( xutes to CO2 $ }: g( n4 N3 C# H2 {# [' Demissions. Although fungi and bacteria are known to colonize dead ) \5 o/ _. [ p/ o0 E) jwood, little is known about the microbial processes that mediate carbon and nitro / Y. \- X* X7 c! s" Cgen (N) cycling in deadwood. In this study, using a combination of metagenomics,# a- @! R9 e: Y
metatranscriptomics, and nutrient flflux measurements, we demonstrate that the decom& G! Q* `8 F# c/ T3 ?+ q
position of deadwood reflflects the complementary roles played by fungi and bacteria. # d+ E* R5 |$ ?4 Z: l; T6 m+ U, J5 OFungi were found to dominate the decomposition of deadwood and particularly its re V5 m5 i' ~! d* H2 o/ o
calcitrant fractions, while several bacterial taxa participate in N accumulation in dead ' q3 q3 P5 {, ]5 Swood through N fifixation, being dependent on fungal activity with respect to deadwood / _: c5 ? M, K, B' ?, K3 Kcolonization and C supply. Conversely, bacterial N fifixation helps to decrease the con) B# H X% f9 M; P8 W$ T# O$ Z
straints of deadwood decomposition for fungi. Both the CO2 efflflux and N accumulation5 f* p( U" c" i! H2 q
that are a result of a joint action of deadwood bacteria and fungi may be signifificant for. X! Q: P! [/ @% b
nutrient cycling at ecosystem levels. Especially in boreal forests with low N stocks, dead, p: C- s( D* h# F* g
wood retention may help to improve the nutritional status and fertility of soils. 5 W8 K& S# l$ ~1 P e8 j- N* O* C5 K1 N$ x
+ L* B! ]1 g3 X* Z' B