Soil Biology and Biochemistry,
Journal Year:
2024,
Volume and Issue:
197, P. 109535 - 109535
Published: July 14, 2024
Microbial
processes
mediating
the
cycling
of
carbon
and
nutrients
in
soils
are
complex
thus
difficult
to
predict
with
mathematical
models.
Such
complexity
arises
because
biological
ecological
dynamics
interact
physical
soil
shape
patterns
resource
acquisition
use,
ultimately
organic
matter
stabilization
soil.
In
article
collection
"Advances
Modelling
Soil
Dynamics"
(https://www.sciencedirect.com/special-issue/10DG8MTGCCF),
novel
approaches
tackle
these
complexities
presented.
This
perspective
summarizes
their
findings
by
highlighting
theoretical
advances
outstanding
challenges
modelling
microbial
constraints.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: April 27, 2024
Abstract
Delineation
of
microbial
habitats
within
the
soil
matrix
and
characterization
their
environments
metabolic
processes
are
crucial
to
understand
functioning,
yet
experimental
identification
remains
persistently
limited.
We
combined
single-
triple-energy
X-ray
computed
microtomography
with
pore
specific
allocation
13
C
labeled
glucose
subsequent
stable
isotope
probing
demonstrate
how
long-term
disparities
in
vegetation
history
modify
spatial
distribution
patterns
particulate
organic
matter
drivers
habitats,
probe
bacterial
communities
populating
such
habitats.
Here
we
show
striking
differences
between
large
(30-150
µm
Ø)
small
(4-10
pores
(i)
diversity,
composition,
life-strategies,
(ii)
responses
added
substrate,
(iii)
pathways,
(iv)
processing
fate
labile
C.
propose
a
habitat
classification
concept
based
on
biogeochemical
mechanisms
localization
also
suggests
interventions
mitigate
environmental
consequences
agricultural
management.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: Feb. 8, 2024
Abstract
Unravelling
biosphere
feedback
mechanisms
is
crucial
for
predicting
the
impacts
of
global
warming.
Soil
priming,
an
effect
fresh
plant-derived
carbon
(C)
on
native
soil
organic
(SOC)
decomposition,
a
key
mechanism
that
could
release
large
amounts
C
into
atmosphere.
However,
climate
warming
priming
remain
elusive.
Here,
we
show
experimental
accelerates
by
12.7%
in
temperate
grassland.
Warming
alters
bacterial
communities,
with
38%
unique
active
phylotypes
detected
under
The
functional
genes
essential
decomposition
are
also
stimulated,
which
be
linked
to
effects.
We
incorporate
lab-derived
information
ecosystem
model
showing
parameter
uncertainty
can
reduced
32–37%.
Model
simulations
from
2010
2016
indicate
increase
warming,
9.1%
rise
priming-induced
CO
2
emissions.
If
our
findings
generalized
other
ecosystems
over
extended
period
time,
play
important
role
terrestrial
cycle
feedbacks
and
change.
Nature Microbiology,
Journal Year:
2024,
Volume and Issue:
9(2), P. 421 - 433
Published: Feb. 5, 2024
Abstract
Soil
microbiomes
are
highly
diverse,
and
to
improve
their
representation
in
biogeochemical
models,
microbial
genome
data
can
be
leveraged
infer
key
functional
traits.
By
integrating
genome-inferred
traits
into
a
theory-based
hierarchical
framework,
emergent
behaviour
arising
from
interactions
of
individual
predicted.
Here
we
combine
theory-driven
predictions
substrate
uptake
kinetics
with
genome-informed
trait-based
dynamic
energy
budget
model
predict
life-history
trade-offs
soil
bacteria.
When
applied
plant
microbiome
system,
the
accurately
predicted
distinct
substrate-acquisition
strategies
that
aligned
observations,
uncovering
resource-dependent
between
growth
rate
efficiency.
For
instance,
inherently
slower-growing
microorganisms,
favoured
by
organic
acid
exudation
at
later
stages,
exhibited
enhanced
carbon
use
efficiency
(yield)
without
sacrificing
(power).
This
insight
has
implications
for
retaining
root-derived
soils
highlights
power
data-driven,
approaches
improving
models.
New Phytologist,
Journal Year:
2024,
Volume and Issue:
243(3), P. 866 - 880
Published: Feb. 11, 2024
Summary
A
large
fraction
of
plant
litter
comprises
recalcitrant
aromatic
compounds
(lignin
and
other
phenolics).
Quantifying
the
fate
is
difficult,
because
oxidative
degradation
carbon
(C)
a
costly
but
necessary
endeavor
for
microorganisms,
we
do
not
know
when
gains
from
decomposition
C
outweigh
energetic
costs.
To
evaluate
these
tradeoffs,
developed
model
in
which
rate
optimized
dynamically
to
maximize
microbial
growth
given
costs
maintaining
ligninolytic
activity.
We
tested
performance
against
>
200
datasets
collected
published
literature
assessed
effects
climate
chemistry
on
decomposition.
The
predicted
time‐varying
oxidation
rate,
was
used
calculate
lag
time
before
initiated.
Warmer
conditions
increased
rates,
shortened
oxidation,
improved
C‐use
efficiency
by
decreasing
oxidation.
Moreover,
higher
initial
content
promoted
an
earlier
start
under
any
climate.
With
this
contribution,
highlight
application
eco‐evolutionary
approaches
based
life
strategies
as
alternative
parametrization
scheme
models.
SOIL,
Journal Year:
2025,
Volume and Issue:
11(1), P. 149 - 174
Published: Feb. 5, 2025
Abstract.
Land
planning
projects
aiming
to
maximize
soil
organic
carbon
(SOC)
stocks
are
increasing
in
number
and
scope,
often
line
with
the
objective
reach
neutrality
by
2050.
In
response,
a
rising
of
studies
assesses
where
additional
SOC
could
be
stored
over
regional
global
spatial
scales.
order
provide
realistic
values
transferrable
beyond
scientific
community,
providing
targets
accrual
should
consider
timescales
needed
them,
taking
into
consideration
effects
C
inputs,
type,
depth
on
dynamics.
This
research
was
conducted
320
km2
territory
north-eastern
France,
eight
contrasted
types
have
been
identified,
characterized,
mapped
thanks
high
density
fully
described
profiles.
Continuous
profiles
were
interpolated
for
each
type
land
use
(cropland,
grassland,
or
forest).
We
defined
potential
using
percentile
boundary
lines
used
linear
model
depth-dependent
dynamics
explore
inputs
necessary
those
within
25
years.
also
from
literature
input
scenarios
provided
maps
stocks,
maximum
accrual,
highly
heterogenous
region
study.
Median
range
78–333
tC
ha−1.
Maximum
varies
19
ha−1
forested
Leptosols
197
grassland
Gleysols.
The
simulated
years
whole
study
one-fifth
accrual.
Further
different
is
therefore
storage
relevant
public
policies
approach
Biology and Fertility of Soils,
Journal Year:
2024,
Volume and Issue:
60(3), P. 263 - 306
Published: March 11, 2024
Abstract
Essential
soil
functions
such
as
plant
productivity,
C
storage,
nutrient
cycling
and
the
storage
purification
of
water
all
depend
on
biological
processes.
Given
this
insight,
it
is
remarkable
that
in
modeling
these
functions,
various
actors
usually
do
not
play
an
explicit
role.
In
review
perspective
paper
we
analyze
state
art
how
processes
could
more
adequately
be
accounted
for.
We
for
six
different
biologically
driven
clusters
are
key
understanding
namely
i)
turnover
organic
matter,
ii)
N
cycling,
iii)
P
dynamics,
iv)
biodegradation
contaminants
v)
disease
control
vi)
structure
formation.
A
major
conclusion
development
models
to
predict
changes
at
scale
profiles
(i.e.
pedons)
should
better
rooted
underlying
known
a
large
extent.
This
prerequisite
arrive
predictive
urgently
need
under
current
conditions
Global
Change.
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
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