Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
52(1)
Published: Dec. 28, 2024
Abstract
Protection
by
metal
(hydr)
oxides
is
one
of
the
key
mechanisms
for
long‐term
stabilization
soil
organic
carbon
(SOC).
However,
source
and
turnover
(metal‐)
bound
(OC)
in
soils
are
poorly
constrained.
Here
we
present
first
large‐scale
study
on
13
C
14
characteristics
OC
15
wetland
upland
profiles.
We
find
that
has
similar
δ
as
SOC,
suggesting
no
preference
plant‐
or
microbe‐derived
carbon.
Δ
more
negative
than
SOC
but
not
mineral
soils,
decreases
with
increasing
reactive
minerals.
Hence,
contrast
to
conventional
assumption,
better
preserved
relative
wetlands
high
contents
metals.
Our
finding
highlights
dynamic
exchange
calls
a
recognition
metals
stabilizing
wetlands.
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.
Functional Ecology,
Journal Year:
2024,
Volume and Issue:
38(7), P. 1510 - 1522
Published: April 29, 2024
Abstract
Microbial
carbon
use
efficiency
(CUE),
a
key
parameter
to
characterize
microbial
conversion
efficiency,
is
assumed
be
similar
in
soil
models
for
different
functional
pools
with
varied
organic
matter
composition
and
nutrient
availability,
that
is,
particulate
(POM)
mineral‐associated
(MAOM).
However,
empirical
studies
comparing
CUE
POM
versus
MAOM
are
largely
lacking.
It
not
known
whether
variance
may
underpin
the
variant
behaviour
(i.e.
turnover
composition)
of
pools.
Here
we
collected
surface
soils
from
25
natural
forests
grasslands
divergent
edaphic
properties,
compared
their
using
fractionation
combination
incubation
18
O‐labelled
water.
We
also
quantified
composition,
community
structures
stoichiometric
imbalance
nitrogen
(N)
phosphorus
(P)
relative
based
on
dissolved
pool
biomass
(Im
N
Im
P
)
investigate
variables
regulating
its
variation
(CUE
/CUE
).
In
contrast
our
expectation,
did
consistently
differ
between
across
sites,
albeit
large
inter‐sample
variations
(from
0.3
4.4).
Although
had
higher
substrate
quality,
indicated
by
lower
ratios
total
(C/N
OM
N‐compounds/aromatic
ratios,
proportions
r‐strategists
fast‐growing
bacteria
than
POM,
degrees
limitation
),
which
was
best
predictor
all
samples.
Therefore,
although
harboured
more
N‐containing
compounds
necessarily
lower,
leading
an
overall
MAOM.
Nevertheless,
decreased
increasing
Overall,
paper
presents
comprehensive,
study
diverse
soils,
results
support
models,
but
highlight
potential
contrasts
under
strong
limitation.
Such
inferences
deserve
attention
potentially
induced
deposition.
This
advances
mechanistic
understanding
ecological
patterns
processes
organismic
ecosystem
scale
physiology
Read
free
Plain
Language
Summary
this
article
Journal
blog.
Scientific Reports,
Journal Year:
2025,
Volume and Issue:
15(1)
Published: March 10, 2025
Peatlands
are
vital
for
global
carbon
storage,
but
drainage
significantly
disrupts
their
natural
cycling.
Drainage
alters
peatland
soil
environments
in
complex
ways,
affecting
factors
such
as
water
table,
temperature,
organic
(SOC),
pH,
and
microbial
communities.
However,
how
these
interact
to
influence
GHG
emissions
remains
unclear.
In
this
study,
we
compared
properties,
community
structure,
across
three
zones
of
a
Northeast
China
undergoing
drainage:
drained,
transition,
areas.
The
average
table
the
drained
area
was
lower
than
(from
11.45
cm
-13.47
cm),
shifting
from
waterlogged
unsaturated
conditions.
Deep
temperatures
decreased
by
1
~
3
°C.
pH
upper
layer
higher
(5.05
5.29
vs.
4.64
4.71),
while
SOC
(197.31
374.75
g/kg
437.05
512.71
g/kg).
Aerobic
bacteria
(mainly
Solibacter)
were
more
abundant
area,
methanogens
hydrogenotrophic)
declined
significantly.
Fungal
diversity
increased
with
negative
interactions
enhanced
network
modularity.
reduced
CH4
CO2
N2O
emissions,
resulting
significant
rise
net
(8.86
10.65
22.27
24.26
t
CO2-eq·ha⁻¹·season⁻¹),
primarily
driven
CO2.
positively
correlated
aerobic
bacteria,
facultatively
anaerobic
negatively
moisture
C/N
ratio.
flux
pH.
effects
pronounced
near
ditches,
particularly
highlighting
localized
impacts
on
fluxes.
Global Change Biology,
Journal Year:
2025,
Volume and Issue:
31(4)
Published: April 1, 2025
Soil
organic
carbon
(SOC)
decomposition
underpins
soil-atmosphere
exchange
and
is
regulated
by
climate
change-mediated
variations
in
soil
redox
conditions.
Periodic
anoxia,
commonly
occurring
following
precipitation,
flooding,
erosion
events,
assumed
to
preserve
SOC.
Yet,
water
saturation
may
also
increase
SOC
relative
unsaturated
conditions,
contradictory
findings
among
previous
studies
remain
unexplained.
Here,
using
incubation
experiments
on
20
soils
collected
across
a
24°
latitude
gradient
China,
we
show
that
70%
of
the
showed
higher
or
similar
anoxic
rate
compared
oxic
treatment,
indicating
fast
loss
under
relatively
short
anoxia.
Methane
production
was
far
lower
than
CO2
due
presence
alternative
terminal
electron
acceptors
(TEAs).
Variation
TEAs
microbial
community
shows
primarily
driven
iron
(Fe)
reduction,
which
accounted
for
up
90%
production.
Meanwhile,
positive
relationships
water-extractable
(OC),
hydrochloric
acid-extractable
ferrous
Fe,
abundance
Fe-reducing
prokaryotes,
suggest
release
readily
metabolized
substrates
Fe
reduction.
This
provided
metabolism
potentially
led
OC
protected
(Fe-bound
OC;
slow-cycling
pool
conditions).
Mass
balance
calculation
confirms
Fe-bound
mostly
elevated
magnitude,
random
forest
modeling
indicates
rich
reducible
SOC,
prokaryotes
most
likely
experience
periodic
Overall,
our
demonstrate
important
pathway
stimulate
intense
hydrologic
regimes,
particularly
Plant and Soil,
Journal Year:
2024,
Volume and Issue:
unknown
Published: July 5, 2024
Abstract
Background
and
aims
Most
studies
of
the
relationships
between
composition
soil
organic
matter
plant
cover
have
been
carried
out
at
genera
level.
However,
they
largely
overlooked
potential
effects
that
varieties,
belonging
to
same
genus,
can
on
matter.
Methods
We
investigated
whether
varieties
different
Salix
species
(
S.
dasyclados
viminalis)
impacted
using
mid-infrared
spectroscopy
pyrolysis
GC/MS.
Top-soils
were
taken
from
an
18
year-old
long-term
field
trial
where
six
grown
as
short-rotation
coppice
under
two
fertilisation
regimes.
Results
Significant
differences
in
molecular
diversity
observed
fertilised
plots.
The
mostly
visible
level,
i.e.
had
higher
lignin
content
than
viminalis
,
potentially
due
amount
their
litter
inputs.
Smaller
among
also
observed.
No
significant
unfertilised
relatively
high
degree
spatial
variability
several
properties
found
these
plots
may
masked
variety
and/or
effects.
Conclusion
This
study
provides
evidence
identity
or
affect
corresponding
traits
should
be
considered
breeding
programmes
enhance
C
accumulation
persistence.
Scientific Reports,
Journal Year:
2024,
Volume and Issue:
14(1)
Published: Oct. 10, 2024
The
replacement
of
farmland
by
native
hygro-plants
is
increasingly
common
globally
within
the
context
wetland
ecosystem
restoration.
Understanding
long-term
effects
this
on
abundance
and
persistence
soil
organic
carbon
(SOC)
in
mountain
marshes
important
for
management.
Here,
restored
plateau
Duliu
River
Wetland
Provincial
Nature
Reserve,
China
was
selected.
properties,
moisture
content
(SMC),
pH,
texture,
free-form
iron
oxides
(
$$\:{\text{F}\text{e}}_{\text{d}}$$
),
amorphous
$$\:{\text{F}\text{e}}_{\text{o}}$$
mineral-associated
(MAOC),
iron-bound
(Fe-OC)
were
analyzed
topsoil
samples
(0
~
20
cm)
during
restoration
rice
paddies
to
Sphagnum
palustre
L.
wetlands
0,
2,
10,
years.
Natural
also
used
as
control.
We
found
that
marsh
increased
SMC,
,
/
SOC,
MAOC,
Fe-OC,
Fe-OC/SOC,
but
decreased
MAOC/SOC
ratio.
ratio
expectedly
lower
than
proportion
labile
SOC
total
period.
MAOC
higher
natural
other
habitats.
Both
Fe-OC/SOC
positively
correlated
with
negatively
pH.
.
These
results
emphasized
significance
reconverting
increasing
sequestration
Fe-OC.
Further
studies
are
required
identify
quantify
organo-mineral
stabilization
mechanisms
at
different
fractionations
throughout