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.
In
macroecology,
the
concept
of
r-
and
K-strategy
has
been
widely
applied,
yet,
there
have
limited
studies
on
microbial
life-history
strategies
in
temperate
grasslands
using
multiple
sequencing
approaches.
Total
phospholipid
fatty
acid
(PLFA)
analysis,
high-throughput
meta-genomic
sequencing,
GeoChip
technologies
were
used
to
examine
changes
traits
a
chronosequence
restored
(1,
5,
10,
15,
25,
30
years
since
restoration).
Grassland
restoration
increased
relative
abundances
Actinobacteria,
Proteobacteria,
Bacteroidetes
but
reduced
Acidobacteria,
Planctomycetes,
Chloroflexi.
PLFA
analysis
revealed
that
grassland
fungi:bacteria
Gram-positive:Gram-negative
bacteria
ratios.
Combined
with
data,
we
found
shifted
microorganisms
from
oligotrophic
(K-)
copiotrophic
(r-)
groups,
consistent
rRNA
operon
copy
number
community.
Structural
equation
modeling
showed
soil
properties
positively
(
Global Change Biology,
Journal Year:
2022,
Volume and Issue:
28(13), P. 4194 - 4210
Published: April 21, 2022
Increasing
phosphorus
(P)
inputs
induced
by
anthropogenic
activities
have
increased
P
availability
in
soils
considerably,
with
dramatic
effects
on
carbon
(C)
cycling
and
storage.
However,
the
underlying
mechanisms
via
which
drives
plant
microbial
regulation
of
soil
organic
C
(SOC)
formation
stabilization
remain
unclear,
hampering
accurate
projection
sequestration
under
future
global
change
scenarios.
Taking
advantage
an
8-year
field
experiment
increasing
addition
levels
a
subalpine
forest
eastern
Tibetan
Plateau,
we
explored
inputs,
communities,
biomarkers,
as
well
SOC
physical
chemical
fractions.
We
found
that
continuous
reduced
fine
root
biomass,
but
did
not
affect
total
content.
decreased
lignin
contribution
to
SOC,
primarily
from
declined
vanillyl-type
phenols,
was
coincided
reduction
methoxyl/N-alkyl
2.1%-5.5%.
Despite
decline
decomposition
due
suppressed
oxidase
activity
addition,
content
lignin-derived
compounds
because
low
input
roots.
In
contrast,
(mainly
fungal)
necromass
its
slower
N-acquisition
enzyme
activity.
The
larger
corresponded
9.1%-12.4%
increase
carbonyl
abundance.
Moreover,
had
no
influence
slow-cycing
mineral-associated
pool,
stability
indicated
aliphaticity
recalcitrance
indices.
Overall,
over
8
years
influenced
composition
through
divergent
alterations
plant-
microbial-derived
contributions,
shape
stability.
Such
findings
may
aid
accurately
forecasting
dynamics
their
potential
feedbacks
climate
scenarios
Earth
system
models.
Our
results
reveal
different
responses
of
soil
multifunctionality
to
increased
and
decreased
precipitation.
By
linking
microbial
network
properties
functions,
we
also
show
that
complexity
potentially
competitive
interactions
are
key
drivers
multifunctionality.
Geoderma,
Journal Year:
2023,
Volume and Issue:
432, P. 116393 - 116393
Published: Feb. 22, 2023
Although
the
impact
of
land
conversion
on
carbon
mineralization
in
paddy
soils
has
received
increasing
attention,
coupled
roles
soil
microdiversity
and
chemodiversity
these
processes
are
largely
unknown.
To
address
this
issue,
use
from
fields
(PF)
to
vegetable
(VF),
rice-vegetable
rotation
(RV),
abandoned
(AL),
were
investigated
study.
The
relationships
between
characteristics
microbial
community,
metabolism
physiology
dissolved
organic
matter
(DOM)
analyzed.
After
conversion,
enhanced
AL
RV,
which
217.49%
183.02%
that
PF.
In
contrast,
no
significant
change
was
observed
VF,
although
anaerobic
environment
transformed
into
an
aerobic
one
fungal
richness/
diversity
increased
soil.
This
because
directly
regulated
by
DOM
quantity
labile
carbon,
indirectly
community.
Specifically,
largest
attributed
strongest
as
had
DOC
contents,
hydrophilic
substances
(e.g.,
carboxyl,
carbohydrate,
amino),
abundant
eutrophic
taxa
Actinobacteria
Proteobacteria).
VF
mainly
related
more
condensed
aromatics
oligotrophic
microbes,
fewer
soil,
resulting
dominance
recalcitrant
carbon.
also
prevailed
RV.
However,
RV
showed
moderate
due
having
proper
with
high
bioavailability.
Collectively,
results
provide
molecular
insights
a
micro-chemodiversity
perspective,
highlights
importance
nutrient
supply
strategy.