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
Global Change Biology,
Journal Year:
2019,
Volume and Issue:
25(12), P. 4369 - 4382
Published: July 17, 2019
Fine
root
litter
is
a
primary
source
of
soil
organic
matter
(SOM),
which
globally
important
pool
C
that
responsive
to
climate
change.
We
previously
established
~20
years
experimental
nitrogen
(N)
deposition
has
slowed
fine
decay
and
increased
the
storage
carbon
(C;
+18%)
across
widespread
northern
hardwood
forest
ecosystem.
However,
microbial
mechanisms
have
directly
are
unknown.
Here,
we
show
N
decreased
relative
abundance
Agaricales
fungi
(-31%)
partially
ligninolytic
Actinobacteria
(+24%)
on
decaying
roots.
Moreover,
lignin-derived
compounds
residing
in
SOM
(+53%),
this
biochemical
response
significantly
related
shifts
both
fungal
bacterial
community
composition.
Specifically,
accumulation
negatively
Mycena
Kuehneromyces
fungi,
positively
Microbacteriaceae.
Our
findings
suggest
by
altering
composition
communities
roots
such
their
capacity
for
lignin
degradation
reduced,
decay,
contribution
from
SOM.
The
responses
observed
may
explain
anthropogenic
increases
terrestrial
ecosystems.
More
broadly,
our
link
function
communities,
implicate
compositional
mediating
biogeochemical
processes
global
significance.
Soil Science Society of America Journal,
Journal Year:
2019,
Volume and Issue:
83(S1)
Published: May 30, 2019
Core
Ideas
N
additions
alter
soil
microbial
community
composition
and
reduce
forest
biomass
enzyme
activity.
Litter
decomposition
organic
matter
degradation
was
slowed
by
additions.
Reduced
increases
C,
but
long‐term
effects
on
productivity
are
unknown.
Eastern
North
American
forests
receive
anthropogenically
elevated
nitrogen
(N)
deposition
that
alters
processes
productivity.
We
examined
carbon
(C)
in
temperate,
N‐rich
plots
fertilized
annually
(100
kg
ha
−1
y
)
since
1993.
After
nearly
two
decades,
C
O,
A,
upper
50
cm
of
B
horizons
N‐addition
17%
greater
(14.2
±
0.7
m
−2
than
control
plots.
Aboveground
tree
growth
litterfall
were
not
affected
fertilization.
Fine
root
mass
(0–1
mm)
34%
plots,
did
explain
increases.
Rather,
reduced
litter
drove
Decomposition
rates
black
cherry,
sugar
maple,
mixed
leaf
43,
67,
36%,
greater,
respectively,
Light
fraction
due
to
either
enhanced
production
or
decreased
matter.
Soil
respiration
reduced,
upper‐B
lower
controls.
The
also
altered
dramatically
with
Recalcitrant
activity
(peroxidase)
the
O‐horizon
addition.
Available
Ca,
Mg,
K
O
A
These
results
suggest
chronic
atmospheric
inputs
can
increase
storage
decreasing
decomposition,
however
stability
this
additional
sequestration
is
Journal of Ecology,
Journal Year:
2022,
Volume and Issue:
110(6), P. 1376 - 1389
Published: March 26, 2022
Abstract
To
evaluate
how
increased
anthropogenic
nutrient
inputs
alter
carbon
cycling
in
grasslands,
we
conducted
a
litter
decomposition
study
across
20
temperate
grasslands
on
three
continents
within
the
Nutrient
Network,
globally
distributed
enrichment
experiment
We
determined
effects
of
addition
experimental
nitrogen
(N),
phosphorus
(P)
and
potassium
plus
micronutrient
(K
μ
)
common
tree
leaf
long‐term
(maximum
7
years;
exact
deployment
period
varied
sites).
The
use
higher
order
models
allowed
us
to
distinguish
between
nutrients
early‐
versus
late‐stage
decomposition.
Across
continents,
N
(but
not
other
nutrients)
accelerated
early‐stage
slowed
decomposition,
increasing
slowly
decomposing
fraction
by
28%
overall
mean
residence
time
58%.
Synthesis
.
Using
novel,
cross‐site
experiment,
found
widespread
evidence
that
enhances
early
stages
above‐ground
plant
diverse
grassland
sites
but
slows
These
findings
were
corroborated
fitting
data
multiple
have
implications
for
soil
organic
matter
formation.
For
example,
following
enrichment,
microbial
processing
substrates
could
promote
production
transfer
low
molecular
weight
compounds
soils
potentially
enhance
stabilization
mineral‐associated
matter.
By
contrast,
slowing
particulate
(POM)
accumulation.
Such
hypotheses
deserve
further
testing.
Proceedings of the National Academy of Sciences,
Journal Year:
2024,
Volume and Issue:
121(13)
Published: March 19, 2024
The
huge
carbon
stock
in
humus
layers
of
the
boreal
forest
plays
a
critical
role
global
cycle.
However,
there
remains
uncertainty
about
factors
that
regulate
below-ground
sequestration
this
region.
Notably,
based
on
evidence
from
two
independent
but
complementary
methods,
we
identified
exchangeable
manganese
is
factor
regulating
accumulation
forests
across
both
regional
scales
and
entire
latitudinal
range.
Moreover,
novel
fertilization
experiment,
addition
reduced
soil
stocks,
only
after
4
y
additions.
Our
results
highlight
an
underappreciated
mechanism
influencing
pool
forests.