Global Change Biology,
Journal Year:
2025,
Volume and Issue:
31(3)
Published: March 1, 2025
ABSTRACT
Separating
soil
organic
carbon
(SOC)
into
mineral‐associated
(MAOC)
and
particulate
(POC)
enables
accurate
prediction
of
SOC
vulnerability
to
land
use
change
(LUC).
Here,
we
synthesize
the
responses
MAOC
POC
LUC,
including
restoration
degradation,
from
693
observations
globally.
We
observed
a
large
increase
in
after
greater
decline
but
magnitude
proportion
these
two
fractions
(fMAOC
fPOC)
varied
with
LUC.
POC,
comparison
MAOC,
responded
more
sensitively
suggesting
that
was
vulnerable
environmental
change.
Using
duration
relationships,
found
fraction
(fPOC)
higher
at
early
stage
lower
late
stage,
projecting
stability
declined
short‐term
gradually
increased
long‐term
restoration.
Further
analysis
showed
context‐dependent
effects
LUC
on
fractions:
arid
or
carbon‐poor
topsoil,
greatly
fPOC,
while
humid
carbon‐rich
degradation
resulted
decreases
especially
POC.
Overall,
highlight
importance
fractions,
particularly
predicting
suggest
incorporating
climate
initial
status
models
dynamics
helps
accurately
predict
future
sink
potential.
Global Change Biology,
Journal Year:
2025,
Volume and Issue:
31(1)
Published: Jan. 1, 2025
ABSTRACT
Coastal
wetlands
contain
very
large
carbon
(C)
stocks—termed
as
blue
C—and
their
management
has
emerged
a
promising
nature‐based
solution
for
climate
adaptation
and
mitigation.
The
interactions
among
sources,
pools,
molecular
compositions
of
soil
organic
C
(SOC)
within
ecosystems
(BCEs)
remain
elusive.
Here,
we
explore
these
along
an
18,000
km
long
coastal
line
salt
marshes,
mangroves,
seagrasses
in
China.
We
found
that
mineral‐associated
(MAOC)
is
enriched
BCEs
dominated
by
allochthonous
inputs
abundant
active
minerals,
leading
to
increased
proportion
persistent
molecules.
Specifically,
soils
with
(>
50%)
are
characterized
substantial
contribution
MAOC
70%)
total
SOC
notable
preservation
lipids
(36%)
across
seagrasses.
burial
particles,
derived
from
external
sources
such
rivers
or
tidal
influxes,
facilitates
the
formation
stable
through
binding
mineral
surfaces
occlusion
microaggregates.
proportions
particulate
(POC)
important
predictors
matter.
Lipid
composition
decrease
POC
autochthonous
increase.
These
findings
provide
new
insights
into
coupled
control
over
sequestration
BCEs,
emphasizing
role
inputs,
components.
Forests,
Journal Year:
2025,
Volume and Issue:
16(2), P. 197 - 197
Published: Jan. 22, 2025
Under
global
warming,
vegetation
composition
changes
induced
by
plant
encroachment
have
a
significant
impact
on
the
carbon
balance
of
tundra
ecosystems.
The
herbaceous
plants
into
indigenous
shrub
communities
has
changed
aboveground
and
belowground
litter
input
characteristics
in
Changbai
Mountains.
However,
variations
dynamics
soil
organic
(SOC)
pool
concentrations
SOC
stability
remains
ambiguous.
In
this
study,
samples
were
collected
for
lab
experiments.
Our
results
showed
that
increase
due
to
Deyeuxia
purpurea
increased
concentration.
Simultaneously,
D.
decreased
C/N
decreasing
components
both
resistant
decomposition
(C/N
lignin/N)
mineralization
ability
available
N
concentrations,
CO2
release
rate,
ultimately
enhanced
capacity
increasing
concentration
molecular
structures,
such
as
carbohydrates,
litter,
thereby
decomposable
structures
active
soil,
while
simultaneously
reducing
recalcitrant
carbon.
Even
more,
reduced
capability
nitrogen
concentration,
which
collectively
oxidation
state
(COX)
stability.
general,
warming
led
encroachment,
inputs
properties
tundra,
turn
stability,
enhancing
emission
capacity,
atmospheric
forming
vicious
cycle.
Global Change Biology,
Journal Year:
2025,
Volume and Issue:
31(3)
Published: March 1, 2025
ABSTRACT
Separating
soil
organic
carbon
(SOC)
into
mineral‐associated
(MAOC)
and
particulate
(POC)
enables
accurate
prediction
of
SOC
vulnerability
to
land
use
change
(LUC).
Here,
we
synthesize
the
responses
MAOC
POC
LUC,
including
restoration
degradation,
from
693
observations
globally.
We
observed
a
large
increase
in
after
greater
decline
but
magnitude
proportion
these
two
fractions
(fMAOC
fPOC)
varied
with
LUC.
POC,
comparison
MAOC,
responded
more
sensitively
suggesting
that
was
vulnerable
environmental
change.
Using
duration
relationships,
found
fraction
(fPOC)
higher
at
early
stage
lower
late
stage,
projecting
stability
declined
short‐term
gradually
increased
long‐term
restoration.
Further
analysis
showed
context‐dependent
effects
LUC
on
fractions:
arid
or
carbon‐poor
topsoil,
greatly
fPOC,
while
humid
carbon‐rich
degradation
resulted
decreases
especially
POC.
Overall,
highlight
importance
fractions,
particularly
predicting
suggest
incorporating
climate
initial
status
models
dynamics
helps
accurately
predict
future
sink
potential.