Sustainability,
Journal Year:
2024,
Volume and Issue:
16(19), P. 8408 - 8408
Published: Sept. 27, 2024
In
the
Bamen
Bay
area
of
Qinglan
Harbor
Mangrove
Provincial
Nature
Reserve
in
Wenchang,
Hainan
Province,
China,
mangrove
aboveground
biomass
(AGB)
was
estimated
using
high-resolution
UAV
ortho-imagery
and
LiDAR
data.
The
spatial
distribution
characteristics
AGB
were
studied
global
Moran’s
I
index
hotspot
analysis.
Optimal
geographic
detectors
regression
models
employed
to
analyze
relationship
between
key
environmental
factors.
results
indicate
that
(1)
average
study
141.22
Mg/ha,
with
significant
variation.
High
values
concentrated
southwestern
northeastern
regions,
while
low
mainly
found
central
southeastern
regions.
(2)
Plant
species,
water
pH,
soil
total
potassium,
salinity,
dissolved
oxygen,
elevation,
organic
matter,
phosphorus,
nitrogen
identified
as
major
factors
influencing
AGB.
interaction
either
bifactor
enhancement
or
nonlinear
enhancement,
showing
a
significantly
higher
impact
compared
single
(3)
Comprehensive
model
reveal
primary
factor
affecting
AGB,
followed
by
pH
having
least
impact.
Factors
positively
correlated
promoted
growth,
elevation
negatively
affected
inhibiting
accumulation.
findings
provide
critical
insights
can
guide
targeted
conservation
efforts
management
strategies
aimed
at
enhancing
ecosystem
health
resilience,
particularly
focusing
on
areas
for
potential
improvement
addressing
complex
interactions
among
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
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.
Geoderma,
Journal Year:
2024,
Volume and Issue:
446, P. 116904 - 116904
Published: May 7, 2024
The
global
warming-driven
poleward
expansion
of
mangrove
habitats
(e.g.,
Avicennia
germinans
and
Rhizophora
mangle)
into
temperate
salt
marshes
Spartina
alterniflora
Juncus
roemerianus)
has
been
shown
to
alter
coastal
soil
organic
carbon
(SOC)
storage.
However,
the
taxa-specific
consequences
this
vegetation
shift
on
origin
size
SOC
sub-fractions
(particulate
OC
(POC);
mineral-associated
(MAOC);
reactive
iron-associated
(FeR-MAOC))
remain
largely
unexplored.
In
study,
we
used
a
particle
size-based
fractionation
method
compare
quantity
δ13C
composition
bulk
each
in
cores
collected
from
Apalachicola
Bay
barrier
islands
Florida,
USA,
highest
latitude
where
monospecific
communities
all
four
aforementioned
plants
co-occur.
Depth-dependent
variation
clearly
showed
replacement
S.
by
mangroves,
as
well
reciprocal
substitutions
J.
roemerianus,
probably
driven
changes
wetland
elevation.
Higher
burial
rates
suggested
that
soils
were
principally
developed
deposition.
contrast,
comparatively
lower
but
higher
stocks
marsh
illustrated
subsurface
input
roots.
POC
was
primarily
derived
contemporary
plant
detritus;
its
concentration
(58.8
±
9.0
%
SOC)
relative
mangroves
(38.4
6.0
SOC).
MAOC
content
did
not
vary
across
(53.5
10.9
SOC),
originated
microbially-transformed
pre-existing
plants.
FeR-MAOC
essentially
absent
R.
mangle
(2.9
3.6
while
representing
minor
fraction
three
other
(7.8
7.0
more
like
present-day
surface
plants,
highlighting
situ
formation
their
active
oxidizing
rhizospheres.
Soil Science Society of America Journal,
Journal Year:
2025,
Volume and Issue:
89(2)
Published: March 1, 2025
Abstract
Scientists
are
increasingly
exploring
soil
carbon
(C)
stabilization
processes
that
protect
organic
C
from
microbial
decomposition.
Mineral‐associated
matter
(MAOM)
is
considered
one
of
the
most
protected
pools
C,
but
remains
understudied
in
wetland
soils
relative
to
upland
soils.
Using
complementary
intact
core
and
bottle
incubation
studies,
this
research
investigated
how
fine
sediment
addition,
form
dredged
sediment,
impacts
respiration
MAOM
coastal
vary
by
(SOM)
content
particle
size.
We
hypothesized
additions
would
reduce
increase
pools,
with
greatest
response
addition
being
high
SOM
soil.
Contrary
our
prediction,
sediments
cores
did
not
change
rate,
CO
2
production
rate
decreased
21%
low
cores,
mass
MAOM‐C
increased
23%
after
receiving
additions.
In
study
only,
varied
initial
Specifically,
largest
particles
(>2
mm)
showed
a
1727%
MAOM‐C,
which
coincides
49%
decrease
CH
4
rate.
Overall,
protection
resulting
differed
type
texture,
suggesting
properties
(e.g.,
existing
mineral
content,
nutrient
availability,
degree
decomposition)
influence
through
these
should
be
when
choosing
potential
restoration
sites.