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:
2023,
Volume and Issue:
30(1)
Published: Dec. 25, 2023
Abstract
Identifying
controls
on
soil
organic
carbon
(SOC)
storage,
and
where
SOC
is
most
vulnerable
to
loss,
are
essential
managing
soils
for
both
climate
change
mitigation
global
food
security.
However,
we
currently
lack
a
comprehensive
understanding
of
the
drivers
especially
with
regards
particulate
(POC)
mineral‐associated
(MAOC).
To
better
understand
hierarchical
POC
MAOC,
applied
path
analyses
fractions,
(i.e.,
mean
annual
temperature
[MAT]
precipitation
minus
potential
evapotranspiration
[MAP‐PET]),
(C)
input
net
primary
production
[NPP]),
property
data
synthesized
from
72
published
studies,
along
generated
National
Ecological
Observatory
Network
pits
(
n
=
901
total
observations).
assess
utility
investigating
MAOC
separately
in
storage
controls,
then
compared
these
results
another
analysis
predicting
bulk
storage.
We
found
that
negatively
related
MAT
pH,
while
positively
NPP
MAP‐PET,
but
%
sand.
Our
revealed
similar
trends
explained
less
variation
C
than
our
analyses.
Given
pH
impose
constraints
microbial
decomposition,
this
indicates
primarily
controlled
by
loss
processes.
In
contrast,
strong
relationships
variables
plant
productivity
constraints,
moisture,
mineral
surface
availability
sorption
indicate
climate‐driven
variations
inputs
soil,
as
well
stabilization
mechanisms.
Altogether,
demonstrate
separate
environmental
variables,
further
justifying
need
quantify
model
fractions
forecast
responses
change.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: June 17, 2024
Fauna
is
highly
abundant
and
diverse
in
soils
worldwide,
but
surprisingly
little
known
about
how
it
affects
soil
organic
matter
stabilization.
Here,
we
review
the
ecological
strategies
of
a
multitude
faunal
taxa
can
affect
formation
persistence
labile
(particulate
matter,
POM)
stabilized
(mineral-associated
MAOM).
We
propose
three
major
mechanisms
-
transformation,
translocation,
grazing
on
microorganisms
by
which
fauna
alters
factors
deemed
essential
POM
MAOM,
including
quantity
decomposability
mineralogy,
abundance,
location,
composition
microbial
community.
Determining
relevance
these
to
MAOM
cross-disciplinary
studies
that
cover
individual
more
complex
communities,
employ
physical
fractionation,
isotopic,
microbiological
approaches
advance
concepts,
models,
policies
focused
effectively
manage
as
carbon
sinks,
nutrient
stores,
providers
food.
Global Change Biology,
Journal Year:
2024,
Volume and Issue:
30(6)
Published: June 1, 2024
Understanding
the
mechanisms
of
soil
organic
carbon
(SOC)
sequestration
in
forests
is
vital
to
ecosystem
budgeting
and
helps
gain
insight
functioning
sustainable
management
world
forests.
An
explicit
knowledge
driving
global
SOC
still
lacking
because
complex
interplays
between
climate,
soil,
forest
type
influencing
pool
size
stability.
Based
on
a
synthesis
1179
observations
from
292
studies
across
forests,
we
quantified
relative
importance
property,
total
content
specific
contents
physical
(particulate
vs.
mineral-associated
SOC)
chemical
(labile
recalcitrant
pools
upper
10
cm
mineral
soils,
as
well
stock
O
horizons.
The
variability
soils
was
better
explained
by
climate
(47%-60%)
factors
(26%-50%)
than
NPP
(10%-20%).
particulate
(POC)
(ROC)
all
decreased
with
increasing
mean
annual
temperature
decomposition
overrides
C
replenishment
under
warmer
climate.
(MAOC)
influenced
temperature,
which
directly
affected
microbial
activity.
Additionally,
presence
clay
iron
oxides
physically
protected
forming
MAOC.
horizons
larger
temperate
zone
Mediterranean
regions
boreal
sub/tropical
zones.
Mixed
had
64%
either
broadleaf
or
coniferous
(i)
higher
productivity
(ii)
litter
input
different
tree
species
resulting
diversification
molecular
composition
community.
While
jointly
determine
formation
stability
SOC,
predominantly
controls
patterns
ecosystems.
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(6)
Published: March 18, 2024
Abstract
Mineral
preservation
and
microbial
residue
production
are
vital
for
the
accumulation
of
mineral‐associated
organic
carbon
(MAOC)
in
soils.
However,
their
relative
importance
interactive
effects
remain
unclear.
Here
MAOC
content
composition
analyzed
tandem
with
soil
mineral
attributes
along
a
weathering
gradient
on
volcanic
sequence.
We
find
that
increases
increasing
states,
accompanied
by
contribution
to
MAOC.
rather
than
physiological
traits
strongly
related
contents,
suggesting
weathering‐enhanced
capacity
overrides
governing
reactive
minerals.
Furthermore,
have
strong
effect
composition,
likely
fungal
abundance
community
weathering.
These
findings
highlight
may
effectively
boost
persistent
SOC
synergy
conversion
long
term.
Global Change Biology,
Journal Year:
2025,
Volume and Issue:
31(1)
Published: Jan. 1, 2025
Soil
microorganisms
transform
plant-derived
C
(carbon)
into
particulate
organic
(POC)
and
mineral-associated
(MAOC)
pools.
While
microbial
carbon
use
efficiency
(CUE)
is
widely
recognized
in
current
biogeochemical
models
as
a
key
predictor
of
soil
(SOC)
storage,
large-scale
empirical
evidence
limited.
In
this
study,
we
proposed
experimentally
tested
two
predictors
POC
MAOC
pool
formation:
necromass
(using
amino
sugars
proxy)
CUE
(by
18O-H2O
approach).
sampling
(0-10
10-20
cm
depth)
was
conducted
along
climatic
transect
900
km
on
the
Loess
Plateau,
including
cropland,
grassland,
shrubland,
forest
ecosystems,
to
ensure
homogeneous
parent
material.
We
found
highest
accumulation
occurred
zones
MAT
between
5°C
10°C
or
MAP
300
500
mm.
Microbial
more
positively
related
than
(p
<
0.05),
suggesting
that
residues
may
improve
strongly
compared
pool.
Random
linear
regression
analyses
showed
increased
with
fungal
C,
whereas
bacterial
drove
MAOC.
coupled
0.05)
but
decoupled
SOC
>
0.05).
The
have
faster
turnover
rate
due
lack
clay
protection,
which
lead
rapid
thus
their
decoupling
from
CUE.
sense,
driven
by
necromass,
explains
dynamics.
Our
findings
highlight
insufficiency
relying
solely
predict
bulk
storage.
Instead,
propose
should
be
used
together
explain
dynamics,
each
influencing
distinct
npj Materials Sustainability,
Journal Year:
2023,
Volume and Issue:
1(1)
Published: Nov. 27, 2023
Abstract
Reactive
primary
and
secondary
minerals
play
a
critical
role
in
the
transformation
stabilization
of
organic
matter
(OM)
soil,
aspect
that
has
been
largely
overlooked
existing
literature.
In
this
regard,
we
propose
new
model
known
as
“reactive
mineral
sink”
(RMS)
to
illustrate
three
mechanisms
through
which
these
drive
bioprocessing,
transformation,
transport
OM
soil.
Firstly,
from
biological
perspective,
reactive
influence
enzymatic
microbial
processing
binding
proteins
or
influencing
structure
communities.
Secondly,
chemical
standpoint,
have
capacity
adsorb
and/or
coprecipitate
with
it,
leading
more
diverse
distribution
This
distribution,
turn,
triggers
catalysis
redox
reactions.
Thirdly,
on
physical
level,
substantial
impact
soil
architecture,
aggregate
dynamics,
porosity
development,
hydrological
processes.
These
changes
then
affect
transport,
reprocessing
OM.
The
RMS
provides
conceptual
framework
underscores
fundamental
driving
dynamics
carbon
(C)
sequestration
natural
Furthermore,
it
promotes
restoration
biogeochemical
processes
ecological
resilience.
We
advocate
for
implementation
strategies
based
enhance
C
soils
purposes
rejuvenating
health
mitigating
CO
2
emission.
Soil Biology and Biochemistry,
Journal Year:
2024,
Volume and Issue:
190, P. 109323 - 109323
Published: Jan. 19, 2024
Microbial
necromass
carbon
(C)
can
substantially
contribute
to
stabilized
soil
organic
matter
(SOM),
and
effective
management
of
this
C
may
help
mitigate
climate
change.
However,
factors
important
the
formation
microbial
are
only
partly
understood.
While
bioavailable
plant
inputs
induce
by
boosting
growth
use
efficiency,
other
traits,
such
as
those
related
secretion
systems
or
adhesion
motility,
also
be
relevant.
These
traits
independent
bioavailability
modulated
environmental
depth
site
age.
Such
links,
however,
have
hardly
been
studied.
Here,
we
used
replicated
plots
European
alder
(more
inputs)
Scots
pine
(less
investigate
links
among
inputs,
depth,
age,
community
composition,
in
SOM,
i.e.,
particulate
occluded
within
aggregates
(oPOM)
mineral-associated
(MAOM).
We
did
not
find
evidence
that
nor
were
major
drivers
formation.
Instead,
certain
taxa,
diversity
particular,
most
tightly
MAOM.
contributed
oPOM
(up
∼57%
stored
fraction),
a
pool
considered
largely
derive
from
biomolecules.
Combined,
MAOM
accounted
for
∼23%
bulk
contents.
Our
results
imply
C-focused
research
consider
constraints
on
composition
diversity,
pools
than
MAOM,
plant-derived
SOM.