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
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: June 15, 2023
Much
research
focuses
on
increasing
carbon
storage
in
mineral-associated
organic
matter
(MAOM),
which
may
persist
for
centuries
to
millennia.
However,
MAOM-targeted
management
is
insufficient
because
the
formation
pathways
of
persistent
soil
are
diverse
and
vary
with
environmental
conditions.
Effective
must
also
consider
particulate
(POM).
In
many
soils,
there
potential
enlarging
POM
pools,
can
over
long
time
scales,
be
a
direct
precursor
MAOM.
We
present
framework
context-dependent
strategies
that
recognizes
soils
as
complex
systems
conditions
constrain
MAOM
formation.
Global Change Biology,
Journal Year:
2023,
Volume and Issue:
29(7), P. 1971 - 1983
Published: Jan. 6, 2023
Abstract
Nitrogen
(N)
availability
has
been
considered
as
a
critical
factor
for
the
cycling
and
storage
of
soil
organic
carbon
(SOC),
but
effects
N
enrichment
on
SOC
pool
appear
highly
variable.
Given
complex
nature
pool,
recent
frameworks
suggest
that
separating
this
into
different
functional
components,
example,
particulate
(POC)
mineral‐associated
(MAOC),
is
great
importance
understanding
predicting
dynamics.
Importantly,
little
known
about
how
these
N‐induced
changes
in
components
(e.g.,
ratios
among
fractions)
would
affect
functionality
given
differences
nutrient
density,
resistance
to
disturbance,
turnover
time
between
POC
MAOC
pool.
Here,
we
conducted
global
meta‐analysis
803
paired
observations
from
98
published
studies
assess
effect
addition
fractions.
We
found
addition,
average,
significantly
increased
pools
by
16.4%
3.7%,
respectively.
In
contrast,
both
were
remarkably
decreased
(4.1%
10.1%,
respectively).
Increases
positively
correlated
with
aboveground
plant
biomass
hydrolytic
enzymes.
However,
positive
responses
increases
microbial
biomass.
Our
results
although
reactive
deposition
could
facilitate
C
sequestration
some
extent,
it
might
decrease
time,
disturbance
study
provides
mechanistic
insights
its
at
scale,
which
pivotal
dynamics
especially
future
scenarios
more
frequent
severe
perturbations.
Global Change Biology,
Journal Year:
2023,
Volume and Issue:
29(16), P. 4662 - 4669
Published: June 4, 2023
Abstract
Soil
organic
carbon
(SOC)
sequestration
is
a
promising
climate
change
mitigation
option.
In
this
context,
the
formation
of
relatively
long‐lived
mineral‐associated
(MAOC)
key.
To
date,
soils
are
considered
to
be
limited
in
their
ability
accumulate
MAOC,
mainly
by
amount
clay
and
silt
particles
present.
Using
comprehensive
German
Agricultural
Inventory,
we
selected
189
samples
with
wide
range
SOC
(5–118
g
kg
−1
)
contents
(30–770
test
whether
there
detectable
upper
limit
MAOC
content.
We
found
that
proportion
was
surprisingly
stable
for
under
cropland
grassland
use
across
whole
bulk
contents.
texture
influenced
slope
relationship
between
but
no
observed
any
class.
Also,
C
content
fine
fraction
(g
fraction)
negatively
correlated
soil).
Both
findings
challenge
notion
accumulation
soil
per
se.
Carbon Neutrality,
Journal Year:
2023,
Volume and Issue:
2(1)
Published: Feb. 7, 2023
Abstract
The
large-scale
vegetation
restoration
project
on
the
Loess
Plateau
increased
ecosystem
carbon
(C)
stocks
and
affected
C
budget
in
arid
semi-arid
ecosystems.
specific
details
affecting
stocks,
their
distribution,
dependence
land
use
climate
were
never
presented
generalized.
We
assessed
effects
of
factors
soil
properties
through
field
investigation
across
Plateau.
total
four
ecosystems:
forestlands
[0.36],
shrublands
[0.24],
grasslands
[1.18],
farmlands
[1.05]
was
2.84
Pg
(1
=
10
15
g),
among
which
30%
stored
topsoil
(0–20
cm),
53%
above-ground
biomass,
17%
roots.
density
decreased
according
to
from
southeast
(warm
dry)
northwest
(cold
moist)
with
increasing
temperature
(from
5
°C),
but
precipitation
200
700
mm).
Variation
partitioning
analysis
structural
equation
models
indicated
that
more
explained
by
compared
properties.
This
supports
theory
empirical
findings
large
scale
pattern
is
predominantly
regulated
Our
results
highlight
are
predestined
store
other
ecosystems,
roots
substantial
should
be
considered
when
assessing
strongly
contributes
organic
matter
formation.
suggest
investing
can
an
effective
strategy
for
meeting
part
reduction
goals
mitigate
change,
necessary
validating
parameterizing
worldwide.
Proceedings of the National Academy of Sciences,
Journal Year:
2023,
Volume and Issue:
120(21)
Published: May 15, 2023
Sustainability
of
agricultural
production
and
mitigation
global
warming
rely
on
the
regeneration
soil
organic
carbon
(SOC),
in
particulate
(POC)
mineral-associated
(MAOC)
forms.
We
conducted
a
systematic
meta-analysis
effects
regenerative
management
practices
SOC,
POC,
MAOC
cropland,
finding:
1)
no-till
(NT)
cropping
system
intensification
increase
SOC
(11.3%
12.4%,
respectively),
(8.5%
7.1%,
POC
(19.7%
33.3%,
respectively)
topsoil
(0
to
20
cm),
but
not
subsoil
(>20
cm);
2)
experimental
duration,
tillage
frequency,
type,
rotation
diversity
moderate
management;
3)
NT
synergized
with
integrated
crop-livestock
(ICL)
systems
greatly
(38.1%)
ICL
(33.1
53.6%).
This
analysis
shows
that
agriculture
is
key
strategy
reduce
C
deficit
inherent
promote
both
health
long-term
stabilization.
Annual Review of Ecology Evolution and Systematics,
Journal Year:
2023,
Volume and Issue:
54(1), P. 375 - 401
Published: Aug. 22, 2023
Over
70%
of
soil
organic
carbon
(SOC)
is
stored
at
a
depth
greater
than
20
cm
belowground.
A
portion
this
deep
SOC
actively
cycles
on
annual
to
decadal
timescales
and
sensitive
global
change.
However,
responses
change
likely
differ
from
surface
because
biotic
controls
cycling
become
weaker
as
mineral
predominate
with
depth.
Here,
we
synthesize
the
current
information
drivers
warming,
shifting
precipitation,
elevated
CO
2
,
land
use
cover
Most
can
only
be
hypothesized
few
studies
measure
soils,
even
fewer
experiments
manipulate
soils.
We
call
scientists
incorporate
soils
into
their
manipulations,
measurements,
models
so
that
response
accounted
for
in
projections
nature-based
climate
solutions
terrestrial
feedbacks
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 Geoscience,
Journal Year:
2024,
Volume and Issue:
17(3), P. 205 - 212
Published: Feb. 20, 2024
Abstract
Soil
organic
matter
decomposition
and
its
interactions
with
climate
depend
on
whether
the
is
associated
soil
minerals.
However,
data
limitations
have
hindered
global-scale
analyses
of
mineral-associated
particulate
carbon
pools
their
benchmarking
in
Earth
system
models
used
to
estimate
cycle–climate
feedbacks.
Here
we
analyse
observationally
derived
global
estimates
quantify
relative
proportions
compute
climatological
temperature
sensitivities
as
decline
increasing
temperature.
We
find
that
sensitivity
average
28%
higher
than
carbon,
up
53%
cool
climates.
Moreover,
distribution
between
these
underlying
drives
emergent
bulk
stocks.
vary
widely
predictions
pool
distributions.
show
proportion
model
are
conceptually
similar
mineral-protected
ranges
from
16
85%
across
Coupled
Model
Intercomparison
Project
Phase
6
offline
land
models,
implications
for
ages
ecosystem
responsiveness.
To
improve
projections
feedbacks,
it
imperative
assess
accurately
predict
vulnerability
carbon.