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@ARTICLE{DeFeudis:829704,
author = {De Feudis, M. and Cardelli, V. and Massaccesi, L. and
Hofmann, D. and Berns, A. E. and Bol, R. and Cocco, S. and
Corti, G. and Agnelli, A.},
title = {{A}ltitude affects the quality of the water-extractable
organic matter ({WEOM}) from rhizosphere and bulk soil in
{E}uropean beech forests},
journal = {Geoderma},
volume = {302},
issn = {0016-7061},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2017-03348},
pages = {6 - 13},
year = {2017},
abstract = {Water-extractable organic matter (WEOM) is the most dynamic
and bioavailable fraction of the soil organicmatter pool.
Although the litterfloor is considered the main source of
WEOM, roots also release a great amountof labile organic
compounds through rhizodeposition processes. This makes the
rhizosphere, the small soilvolume in proximity to the roots,
a soil compartment relatively enriched in WEOM. Since both
the rhizosphereand the labile organic C pool are highly
sensitive to the environmental conditions we evaluated
thecharacteristics of WEOM from rhizosphere and bulk soil
collected from the A horizons of European beech(Fagus
sylvaticaL.) forest soils of Apennines mountains (central
Italy) at two altitudes (800 and 1000 m), usingelevation as
a proxy for temperature change. Specifically, we tested ifi)
the rhizosphere contains higher amountsof WEOM with a
greater diversity of compounds with respect to the bulk
soil, andii) this effect is morepronounced at higher
altitude. At both 800 m and 1000 m above sea level, the main
distinction between WEOMfrom rhizosphere and bulk soil was
the larger amounts of sugars in the soil close to the roots.
Further, our resultsindicated an influence of altitude on
rhizospheric processes as suggested by the larger
concentrations of organicC and soluble phenols, and richness
of tannins in the rhizosphere WEOM than in the bulk soil at
1000 m. Weattributed this influence to environmental
constraints which enhanced the release of labile organics
andsecondary metabolites by rhizodeposition and humification
processes in the rhizosphere. As a whole, our datadraw a
picture where the roots are able to affect the
characteristics of WEOM and environmental constraintsenhance
the differentiation between rhizosphere and bulk soil. This
view confirms the influence of therhizosphere on the soil C
cycle, and the importance of the rhizospheric processes when
environmental conditionsbecome harsher.},
cin = {IBG-3},
ddc = {550},
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:000403522800002},
doi = {10.1016/j.geoderma.2017.04.015},
url = {https://juser.fz-juelich.de/record/829704},
}