Organic matter decomposition and carbon content in soil fractions as affected by a gradient of labile carbon input to a temperate forest soil

0531022 - BC 2021 RIV NL eng J - Článek v odborném periodiku
Jílková, Veronika - Jandová, K. - Cajthaml, Tomáš - Devetter, Miloslav - Kukla, J. - Starý, Josef - Vacířová, A.
Organic matter decomposition and carbon content in soil fractions as affected by a gradient of labile carbon input to a temperate forest soil.
Biology and Fertility of Soils. Roč. 56, č. 3 (2020), s. 411-421. ISSN 0178-2762. E-ISSN 1432-0789
Grant CEP: GA ČR(CZ) GA17-08717S; GA MŠMT(CZ) LM2015075; GA MŠMT(CZ) EF16_013/0001782
Grant ostatní: AV ČR(CZ) L200961602
Institucionální podpora: RVO:60077344 ; RVO:61388971
Klíčová slova: coniferous forest * litter bag * microbial activity * PLFA * soil fauna
Obor OECD: Ecology; Microbiology (MBU-M)
Impakt faktor: 6.432, rok: 2020
Způsob publikování: Omezený přístup
https://link.springer.com/article/10.1007/s00374-020-01433-4

Labile carbon (C) input to soils is expected to affect soil organic matter (SOM) decomposition and soil organic C (SOC) stocks in temperate coniferous forests. We hypothesized that the SOM decomposition rate, C content in soil fractions, and microbial and faunal abundance and activity were increased along the gradient in labile C input around wood ant nests. Three distances from the nest that differed in annual labile C input to soil were selected: 4 m with 6379 mg C m(-2), 30 m with 9060 mg C m(-2), and 70 m with 9215 mg C m(-2). Soil from the organic horizon (Oe+Oa), surface mineral horizon (A), and subsoil mineral horizon (B) was analyzed for C content in soil fractions and for activity and abundance of soil microorganisms and fauna. In addition, a 1-year litter-bag and soil-bag decomposition experiment was conducted. Although the rate of soil decomposition did not differ along the labile C input gradient, the rate of litter decomposition in the B horizon increased as labile C input increased with distance from the nest. Correspondingly, the C content in bulk soil and in the labile and less-protected soil fractions in the B horizon decreased as labile C input increased. We infer that, because the O and A horizons are less C-limited than the B horizon, the changes in the labile C input along the gradient affected the B horizon more than the surface O and A horizons. However, soil microbial and faunal activity and abundances were not consistently affected by the gradient. Apparently, C stocks in soil fractions are more important for microbial and faunal communities than labile C inputs. Although the results indicate that SOC content changes very slowly in the coniferous forest soil of the current study, increases in the input of natural labile C leads to decreases in the SOC stock in the B horizon. By increasing the labile C input to temperate forest soils, future increases in atmospheric CO2 concentration may therefore lead to a significant loss of SOC in deep soil layers.
Trvalý link: http://hdl.handle.net/11104/0310446