Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: Oct. 19, 2023
Calcium
(Ca)
can
contribute
to
soil
organic
carbon
(SOC)
persistence
by
mediating
physico-chemical
interactions
between
compounds
and
minerals.
Yet,
Ca
is
also
crucial
for
microbial
adhesion,
potentially
affecting
colonization
of
plant
mineral
surfaces.
The
importance
as
a
mediator
microbe-mineral-organic
matter
resulting
SOC
transformation
has
been
largely
overlooked.
We
incubated
44Ca
labeled
soils
with
13C15N
leaf
litter
study
how
affects
formation
associated
matter.
Here
we
show
that
additions
promote
hyphae-forming
bacteria,
which
often
specialize
in
colonizing
surfaces,
increase
incorporation
into
biomass
use
efficiency
approximately
45%
each.
reduce
cumulative
CO2
production
4%,
while
promoting
associations
minerals
byproducts
litter.
These
findings
expand
the
role
from
solely
driver
reactions
coupled
abiotic-biotic
cycling
SOC.
The ISME Journal,
Journal Year:
2019,
Volume and Issue:
14(1), P. 1 - 9
Published: Sept. 25, 2019
Microorganisms
are
critical
in
terrestrial
carbon
cycling
because
their
growth,
activity
and
interactions
with
the
environment
largely
control
fate
of
recent
plant
inputs
as
well
protected
soil
organic
[1,
2].
Soil
stocks
reflect
a
balance
between
microbial
decomposition
stabilisation
assimilated
carbon.
The
can
shift
under
altered
environmental
conditions
[3],
new
research
suggests
that
knowledge
physiology
may
be
for
projecting
changes
improving
prognosis
climate
change
feedbacks
[4–7].
Still,
predicting
ecosystem
implications
processes
remains
challenge.
Here
we
argue
this
challenge
met
by
identifying
life
history
strategies
based
on
an
organism’s
phenotypic
characteristics,
or
traits,
representing
these
models.
What
key
traits
change?
Microbial
growth
survival
impacted
multiple
determine
responses
to
varying
resource
availability
fluctuating
abiotic
[8].
Cellular
maintenance
activities
(those
do
not
produce
growth)
include
production
extracellular
enzymes
degrade
acquire
resources,
biomolecular
repair
mechanisms,
cellular
integrity,
osmotic
balance,
defence,
antagonism,
cell
signalling
motility
[9–11].
It
is
conceivable
investment
into
would
generally
high
soils,
highly
heterogeneous
temporally
variable
distribution
stressful
like
extremes
moisture,
temperature,
pH
salinity
[12,
13].
Selective
pressures
suboptimal
could
lead
greater
cellular-level
physiological
allocation
relative
(Fig. 1)
thereby
impacting
processes.
Open
separate
window
Fig.
1
Schematic
showing
C
flux
includes
depolymerisation,
substrate
uptake,
assimilation,
dissimilation,
biomass
synthesis
non-growth
production.
Extracellular
enzyme
represents
acquisition,
stress
protein
linked
tolerance
reflects
higher
yield.
Forked
arrows
signify
metabolic
points
where
hypothesised
tradeoffs
might
occur.
expected
empirical
relationships
among
also
shown
Nature,
Journal Year:
2023,
Volume and Issue:
618(7967), P. 981 - 985
Published: May 24, 2023
Abstract
Soils
store
more
carbon
than
other
terrestrial
ecosystems
1,2
.
How
soil
organic
(SOC)
forms
and
persists
remains
uncertain
1,3
,
which
makes
it
challenging
to
understand
how
will
respond
climatic
change
3,4
It
has
been
suggested
that
microorganisms
play
an
important
role
in
SOC
formation,
preservation
loss
5–7
Although
affect
the
accumulation
of
matter
through
many
pathways
4,6,8–11
microbial
use
efficiency
(CUE)
is
integrative
metric
can
capture
balance
these
processes
12,13
CUE
potential
act
as
a
predictor
variation
storage,
persistence
unresolved
7,14,15
Here
we
examine
relationship
between
SOC,
interactions
with
climate,
vegetation
edaphic
properties,
using
combination
global-scale
datasets,
microbial-process
explicit
model,
data
assimilation,
deep
learning
meta-analysis.
We
find
at
least
four
times
evaluated
factors,
such
input,
decomposition
or
vertical
transport,
determining
storage
its
spatial
across
globe.
In
addition,
shows
positive
correlation
content.
Our
findings
point
major
determinant
global
storage.
Understanding
underlying
their
environmental
dependence
may
help
prediction
feedback
changing
climate.
Nature Communications,
Journal Year:
2020,
Volume and Issue:
11(1)
Published: July 23, 2020
Abstract
Empirical
evidence
for
the
response
of
soil
carbon
cycling
to
combined
effects
warming,
drought
and
diversity
loss
is
scarce.
Microbial
use
efficiency
(CUE)
plays
a
central
role
in
regulating
flow
through
soil,
yet
how
biotic
abiotic
factors
interact
drive
it
remains
unclear.
Here,
we
combine
distinct
community
inocula
(a
factor)
with
different
temperature
moisture
conditions
(abiotic
factors)
manipulate
microbial
structure
within
model
soil.
While
composition
are
strongest
predictors
CUE,
modulated
relationship
between
CUE
being
positively
correlated
bacterial
only
under
high
moisture.
Altogether
these
results
indicate
that
×
ecosystem-function
can
be
impaired
non-favorable
soils,
understand
changes
C
need
account
multiple
facets
global
changes.
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
27(10), P. 2039 - 2048
Published: Feb. 10, 2021
Abstract
Optimal
methods
for
incorporating
soil
microbial
mechanisms
of
carbon
(C)
cycling
into
Earth
system
models
(ESMs)
are
still
under
debate.
Specifically,
whether
physiology
parameters
and
residual
materials
important
to
organic
C
(SOC)
content
is
unclear.
Here,
we
explored
the
effects
biotic
abiotic
factors
on
SOC
based
a
survey
soils
from
16
locations
along
~4000
km
forest
transect
in
eastern
China,
spanning
wide
range
climate,
conditions,
communities.
We
found
that
was
highly
correlated
with
biomass
(MBC)
amino
sugar
(AS)
concentration,
an
index
necromass.
Microbial
use
efficiency
(CUE)
significantly
related
variations
this
national‐scale
transect.
Furthermore,
effect
climatic
edaphic
mainly
via
their
regulation
physiological
properties
(CUE
MBC).
also
regression
explanation
AS
performed
better
than
without
them.
Our
results
provide
empirical
linkages
among
characteristics,
at
large
scale
confirm
necessity
necromass
pools
ESMs
global
change
scenarios.
Soil Biology and Biochemistry,
Journal Year:
2019,
Volume and Issue:
138, P. 107584 - 107584
Published: Sept. 4, 2019
The
microbial
partitioning
of
organic
carbon
(C)
into
either
anabolic
(i.e.
growth)
or
catabolic
respiration)
metabolic
pathways
represents
a
key
process
regulating
the
amount
added
C
that
is
retained
in
soil.
factors
use
efficiency
(CUE)
agricultural
soils,
however,
remain
poorly
understood.
aim
this
study
was
to
investigate
substrate
CUE
from
wide
range
soils
(n
=
970)
and
geographical
area
(200,000
km2)
determine
which
soil
properties
most
influenced
retention
within
community.
Using
14C-labeling
approach,
we
showed
average
across
all
0.65
±
0.003,
but
variation
relatively
high
sample
population
(CV
14.9%).
Of
major
measured
our
found
pH
exchangeable
aluminum
(Al)
were
highly
correlated
with
CUE.
We
identified
critical
transition
point
at
declined
(pH
5.5).
This
coincided
exactly
Al3+
started
become
soluble.
In
contrast,
other
[e.g.
total
nitrogen
(N),
dissolved
(DOC),
clay
content,
available
calcium,
phosphorus
(P)
sulfur
(S),
base
cations]
little
no
relationship
also
evidence
suggest
nutrient
stoichiometry
(C:N,
C:P
C:S
ratios)
these
soils.
Based
on
current
evidence,
postulate
decline
low
Al
reflects
greater
channeling
energy
intensive
involved
overcoming
H+/Al3+
stress
(e.g.
cell
repair
detoxification).
response
may
be
associated
shifts
community
structure,
are
known
tightly
pH.
conclude
maintaining
above
5.5
maximizes
efficiency.