Journal of Ecology,
Journal Year:
2022,
Volume and Issue:
111(1), P. 198 - 213
Published: Oct. 28, 2022
Abstract
Litters
of
leaves
and
roots
different
qualities
occur
naturally
above‐
below‐ground,
respectively,
where
they
decompose
in
contrasting
abiotic
biotic
environments.
Therefore,
ecosystem
carbon
(C)
nitrogen
(N)
dynamics
can
be
strongly
affected
by
the
combination
litter
position
quality.
However,
it
is
poorly
understood
how
C
versus
N
turnover
litters
depend
on
interplay
among
plant
functional
type
(PFT),
organs,
traits
position.
In
a
semi‐arid
inland
dune,
soil
surface
buried
leaf
fine
25
species
across
three
PFTs
(herbs,
legume
shrubs
nonlegume
shrubs)
were
incubated
for
3,
6,
9,
12,
18
24
months
to
investigate
decomposition
dynamics.
Morphological
chemical
(nutrient
NMR
carbon)
initial
determined.
The
rates
(
k
values)
did
not
differ,
but
decomposed
faster
than
litter.
Ratios
values
decreased
with
C:N
ratio.
Herbs
roots,
leaves.
At
given
loss,
had
higher
loss
litters;
relatively
or
lower
ratio
shrubs.
Stronger
positive
relationships
between
losses
shown
respectively.
Synthesis.
generality
release
at
highlights
importance
legumes
cycling
ecosystems
limiting
factor.
coordination
as
function
quality
are
modulated
PFT.
These
findings
have
important
implications
development
process‐based
models
cycles
context
on‐going
global
change
potentially
altering
composition
communities
relative
quantities
above‐ground
below‐ground
Soil Biology and Biochemistry,
Journal Year:
2019,
Volume and Issue:
136, P. 107521 - 107521
Published: June 26, 2019
Microorganisms
are
critical
in
mediating
carbon
(C)
and
nitrogen
(N)
cycling
processes
soils.
Yet,
it
has
long
been
debated
whether
the
underlying
biogeochemical
cycles
affected
by
composition
diversity
of
soil
microbial
community
or
not.
The
communities
can
be
influenced
various
environmental
factors,
which
turn
known
to
impact
processes.
objectives
this
study
were
test
effects
multiple
edaphic
drivers
individually
represented
as
multivariate
environment
interacting
with
diversity,
concomitantly
on
functions
(i.e.
enzyme
activities,
C
N
processes).
We
employed
high-throughput
sequencing
(Illumina
MiSeq)
analyze
bacterial/archaeal
fungal
targeting
16S
rRNA
gene
ITS1
region
soils
collected
from
three
land
uses
(cropland,
grassland
forest)
deriving
two
bedrock
forms
(silicate
limestone).
Based
data
set
we
explored
single
combined
variables
structure
well
activities
several
found
that
both
shaped
same
most
representation
exerting
stronger
than
communities,
demonstrated
(partial)
Mantel
tests.
also
similar
controls
bacterial/archaeal/fungal
richness
diversity.
Soil
only
directly
but
not
composition.
In
contrast,
significantly
related
richness/diversity
environment.
This
indicates
direct
control
indirect
structuring
communities.
further
highlights
importance
diversity)
important
Environmental Science & Technology,
Journal Year:
2021,
Volume and Issue:
55(18), P. 12136 - 12152
Published: Sept. 1, 2021
Manganese
(Mn)
is
a
biologically
important
and
redox-active
metal
that
may
exert
poorly
recognized
control
on
carbon
(C)
cycling
in
terrestrial
ecosystems.
influences
ecosystem
C
dynamics
by
mediating
biochemical
pathways
include
photosynthesis,
serving
as
reactive
intermediate
the
breakdown
of
organic
molecules,
binding
and/or
oxidizing
molecules
through
organo-mineral
associations.
However,
potential
for
Mn
to
influence
storage
remains
unresolved.
Although
substantial
research
has
demonstrated
ability
Fe-
Al-oxides
stabilize
matter,
there
scarcity
similar
information
regarding
Mn-oxides.
Furthermore,
Mn-mediated
reactions
regulate
litter
decomposition
pathways,
but
these
processes
are
constrained
across
diverse
Here,
we
discuss
ecological
roles
environments
synthesize
existing
knowledge
multiple
which
biogeochemical
intersect.
We
demonstrate
high
degrade
abiotic
microbially
mediated
oxidation
at
least
temporarily,
outline
priorities
needed
advance
understanding
Mn-C
interactions,
highlighting
gaps
address
key
uncertainties
soil
predictions.
Global Change Biology,
Journal Year:
2020,
Volume and Issue:
27(7), P. 1349 - 1364
Published: Nov. 7, 2020
Abstract
Fungal
decomposition
of
soil
organic
matter
depends
on
nitrogen
(N)
availability.
This
ecosystem
process
is
being
jeopardized
by
changes
in
N
inputs
that
have
resulted
from
a
tripling
atmospheric
deposition
the
last
century.
Soil
fungi
are
impacted
due
to
higher
availability,
as
soils
acidified,
or
micronutrients
become
increasingly
limiting.
communities
persist
with
chronic
may
be
enriched
traits
enable
them
tolerate
environmental
stress,
which
trade‐off
enabling
decomposition.
We
hypothesized
fungal
would
respond
shifting
community
composition
and
functional
gene
abundances
toward
those
stress
but
weak
decomposers.
sampled
at
seven
eastern
US
hardwood
forests
where
ambient
varied
3.2
12.6
kg
ha
−1
year
,
five
also
experimental
plots
was
simulated
through
fertilizer
application
treatments
(25–50
).
responses
across
gradient.
biomass
richness
increased
sites
low
decreased
high
deposition.
genes
involved
hydrolysis
while
oxidation
decreased.
One
four
generalized
abiotic
tolerance
In
summary,
we
found
divergent
response
depended
levels.
biomass,
richness,
oxidative
enzyme
potential
were
reduced
suggesting
pushed
beyond
an
threshold.
structure
function
enrichment
regional
scale.
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: Dec. 20, 2023
The
relationship
between
metallic
micronutrients
and
soil
microorganisms,
thereby
functioning,
has
been
little
explored.
Here,
we
investigate
the
(Fe,
Mn,
Cu,
Zn,
Mo
Ni)
abundance,
diversity
function
of
microbiomes.
In
a
survey
across
180
sites
in
China,
covering
wide
range
conditions
structure
microbiome
are
highly
correlated
with
micronutrients,
especially
Fe,
followed
by
Cu
Zn.
These
results
robust
to
controlling
for
pH,
which
is
often
reported
as
most
important
predictor
microbiome.
An
incubation
experiment
Fe
Zn
additions
five
different
types
also
shows
that
increased
micronutrient
concentration
affects
microbial
community
composition
functional
genes.
addition,
structural
equation
models
indicate
positively
contribute
ecosystem
productivity,
both
directly
(micronutrient
availability
plants)
and,
lesser
extent,
indirectly
(via
affecting
microbiome).
Our
findings
highlight
importance
explaining
functioning.
New Phytologist,
Journal Year:
2020,
Volume and Issue:
229(1), P. 296 - 307
Published: Aug. 7, 2020
Summary
The
continuing
nitrogen
(N)
deposition
observed
worldwide
alters
ecosystem
nutrient
cycling
and
functioning.
Litter
decomposition
is
a
key
process
contributing
to
these
changes,
but
the
numerous
mechanisms
for
altered
remain
poorly
identified.
We
assessed
different
with
experiment
using
litter
from
four
abundant
species
(
Achnatherum
sibiricum
,
Agropyron
cristatum
Leymus
chinensis
Stipa
grandis
)
mixtures
representing
treatment‐specific
community
composition
in
semi‐arid
grassland
under
long‐term
simulation
of
six
rates
N
deposition.
Decomposition
increased
consistently
increasing
addition
all
types.
Higher
soil
manganese
(Mn)
availability,
which
apparently
was
consequence
addition‐induced
lower
pH,
most
important
factor
faster
decomposition.
Soil
C
:
ratios
were
that
subsequently
led
markedly
higher
bacterial
fungal
ratios,
also
stimulated
Several
factors
contributed
jointly
response
Shifts
plant
quality
played
minor
role
compared
N‐driven
reductions
pH
N,
Mn
availability
microbial
structure.
soil‐driven
effect
on
reported
here
may
have
long‐lasting
impacts
cycling,
organic
matter
dynamics
Journal of Ecology,
Journal Year:
2020,
Volume and Issue:
108(6), P. 2283 - 2297
Published: June 25, 2020
Abstract
At
broad
spatial
scales,
the
factors
regulating
litter
decomposition
remain
ambiguous,
with
understanding
of
these
largely
based
on
studies
investigating
site‐specific
single
species,
whereas
using
multi
species
mixtures
across
sites
are
rare.
We
exposed
in
microcosms
containing
and
all
possible
four
leaf
differing
widely
initial
chemical
physical
characteristics
from
a
temperate
forest
to
climatic
conditions
different
forests
Northern
Hemisphere
for
1
year.
Calcium,
magnesium
condensed
tannins
predicted
mass
loss
types
biomes,
regardless
richness
microarthropod
presence.
However,
relative
mixture
effects
differed
among
varied
access
by
microarthropods.
Access
microarthropods
modified
individual
within
mixtures,
which
independent
composition
mixtures.
soil
generally
only
little
affected
decomposition.
Synthesis
.
conclude
that
identity
is
dominant
driver
non‐additive
vary
biomes
despite
identical
chemistry.
These
results
suggest
large
scales
environmental
context
decomposing
including
communities,
determine
besides
strong
trait‐based
effects.
Frontiers in Ecology and Evolution,
Journal Year:
2020,
Volume and Issue:
8
Published: June 30, 2020
Past
research
on
plant-soil
feedbacks
(PSF),
largely
undertaken
in
highly
controlled
greenhouse
conditions,
has
established
that
plant
species
differentially
alter
abiotic
and
biotic
soil
conditions
turn
affect
growth
of
other
conspecific
heterospecific
individuals
soil.
Yet,
whether
under
reflect
natural
environments
where
plants
are
exposed
to
a
range
pressures
is
still
unresolved.
To
address
how
environmental
context
affects
PSF,
we
conducted
meta-analysis
previously
published
studies
examined
responses
multiple
forms
competition,
stress,
disturbance
across
various
PSF
methodology.
We
asked
the
following
questions:
1)
Can
direction
and/or
strength
PSF?
2)
Do
particular
types
or
more
than
others?
3)
methods
conducting
(i.e.,
vs.
field
experiments
source
inoculum
conditioning
from
greenhouse)
disturbance,
their
interactions?
discovered
four
patterns
may
be
predictive
what
future
realistic
might
reveal.
First,
relatively
little
known
about
responds
stress
compared
plant-plant
competition.
Second,
specific
competition
enhanced
negative
effects
microbes
growth,
stressors
positive
growth.
Third,
can
change
responses.
And,
fourth,
phase
With
detail
shown,
these
results
confirm
writ
large
experiments.
These
data
should
aid
theory
predictions
for
conservation
restoration
applications
by
showing
relative
importance
over
time.
Lastly,
demonstrate
variation
experimental
interpretation
conclusions
studies.
Environmental Science & Technology,
Journal Year:
2021,
Volume and Issue:
55(11), P. 7741 - 7751
Published: May 11, 2021
Manganese
(Mn)
oxides
can
oxidize
dissolved
organic
matter
(DOM)
and
alter
its
chemical
properties
microbial
degradability,
but
the
compound
selectivity
for
oxidation
oxidative
alterations
remain
to
be
determined.
We
applied
ultrahigh
mass
spectrometry
catalog
macromolecular
composition
of
Suwannee
River
fulvic
acid
(SRFA)
before
after
by
a
Mn
oxide
(δ-MnO2)
at
pH
4
or
6.
Polycyclic
aromatic
hydrocarbons,
polyphenols,
carbohydrates
were
more
reactive
in
reducing
δ-MnO2
than
highly
unsaturated
phenolic
(HuPh)
compounds
aliphatics,
abundant
HuPh
contributed
most
(∼50%)
overall
reduction
δ-MnO2.
On
average,
oxidized
species
had
higher
molecular
weights,
aromaticity,
carbon
unsaturation
degree,
nominal
state
carbon,
oxygen
nitrogen
contents
lower
hydrogen
content
compared
unoxidized
species.
The
decreased
these
indices
increased
content,
with
stronger
changes
pH.
This
DOM
on
polar
mineral
surfaces
was
selective
shared
similar
rules
adsorption.
abiotic
resembles
degradation
matter,
oxide-oxidizable
may
useful
index
detection
identification
labile
carbon.
Ecology Letters,
Journal Year:
2021,
Volume and Issue:
24(4), P. 802 - 811
Published: Feb. 14, 2021
Abstract
Plant
litter
decomposition
is
a
central
process
in
the
carbon
(C)
cycle
and
sensitive
to
ongoing
anthropogenic
nitrogen
(N)
fertilisation.
Previous
syntheses
evaluating
effect
of
N
fertilisation
on
relied
largely
models
that
define
constant
rate
mass
loss
throughout
decomposition,
which
may
mask
hypothesised
shifts
dynamics.
In
this
meta‐analysis,
we
compared
performance
four
empirical
showed
consistently
accelerates
early‐stage
but
slows
late‐stage
when
model
structure
allows
for
flexibility
rates
through
time.
Within
particular
substrate,
N‐stimulation
was
associated
with
reduced
decay.
Because
products
early‐
vs.
are
stabilised
soils
distinct
chemical
physical
mechanisms,
N‐induced
changes
influence
formation
cycling
soil
C,
largest
terrestrial
C
pool.