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@ARTICLE{deSosa:859359,
author = {de Sosa, Laura L. and Glanville, Helen C. and Marshall,
Miles R. and Schnepf, Andrea and Cooper, David M. and Hill,
Paul W. and Binley, Andrew and Jones, Davey L.},
title = {{S}toichiometric constraints on the microbial processing of
carbon with soil depth along a riparian hillslope},
journal = {Biology and fertility of soils},
volume = {54},
number = {8},
issn = {1432-0789},
address = {Heidelberg},
publisher = {Springer},
reportid = {FZJ-2019-00227},
pages = {949 - 963},
year = {2018},
abstract = {Soil organic matter (SOM) content is a key indicator of
riparian soil functioning and in the provision of ecosystem
services such as water retention, flood alleviation,
pollutant attenuation and carbon (C) sequestration for
climate change mitigation. Here, we studied the importance
of microbial biomass and nutrient availability in regulating
SOM turnover rates. C stabilisation in soil is expected to
vary both vertically, down the soil profile and laterally
across the riparian zone. In this study, we evaluated the
influence of five factors on C mineralisation (Cmin): (i)
substrate quantity, (ii) substrate quality, (iii) nutrient
(C, N and P) stoichiometry, (iv) soil microbial activity
with proximity to the river (2 to 75 m) and (v) as a
function of soil depth (0–3 m). Substrate quality,
quantity and nutrient stoichiometry were evaluated using
high and low molecular weight 14C-labelled dissolved organic
(DOC) along with different nutrient additions. Differences
in soil microbial activity with proximity to the river and
soil depth were assessed by comparing initial (immediate)
Cmin rates and cumulative C mineralised at the end of the
incubation period. Overall, microbial biomass C (MBC),
organic matter (OM) and soil moisture content (MC) proved to
be the major factors controlling rates of Cmin at depth.
Differences in the immediate and medium-term response (42
days) of Cmin suggested that microbial growth increased and
carbon use efficiency (CUE) decreased down the soil profile.
Inorganic N and/or P availability had little or no effect on
Cmin suggesting that microbial community growth and activity
is predominantly C limited. Similarly, proximity to the
watercourse also had relatively little effect on Cmin. This
work challenges current theories suggesting that areas
adjacent to watercourse process C differently from upslope
areas. In contrast, our results suggest that substrate
quality and microbial biomass are more important in
regulating C processing rates rather than proximity to a
river.},
cin = {IBG-3},
ddc = {640},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000447917800006},
pubmed = {pmid:30956377},
doi = {10.1007/s00374-018-1317-2},
url = {https://juser.fz-juelich.de/record/859359},
}