Global Change Biology,
Год журнала:
2024,
Номер
30(6)
Опубликована: Июнь 1, 2024
Priming
of
soil
organic
matter
(SOM)
decomposition
by
microorganisms
is
a
key
phenomenon
global
carbon
(C)
cycling.
Soil
pH
main
factor
defining
priming
effects
(PEs)
because
it
(i)
controls
microbial
community
composition
and
activities,
including
enzyme
(ii)
defines
SOM
stabilization
destabilization
mechanisms,
(iii)
regulates
intensities
many
biogeochemical
processes.
In
this
critical
review,
we
focus
on
prerequisites
mechanisms
PE
depending
assess
the
change
consequences
for
PE.
The
highest
PEs
were
common
in
soils
with
between
5.5
7.5,
whereas
low
molecular
weight
compounds
triggered
mainly
slightly
acidic
soils.
Positive
up
to
20
times
before
C
input
at
around
6.5.
Negative
below
4.5
or
above
7
reflecting
suboptimal
environment
specific
high
pH.
Short-term
acidification
(in
rhizosphere,
after
fertilizer
application)
affects
by:
mineral-SOM
complexation,
oxidation
iron
reduction,
enzymatic
depolymerization,
pH-dependent
changes
nutrient
availability.
Biological
processes
metabolism
shift
over
short-term,
long-term
adaptations
slow
are
common.
nitrogen
fertilization
induced
land
use
intensification
strongly
decrease
thus
boost
Concluding,
one
strongest
but
now
disregarded
factors
PE,
through
short-term
metabolic
adaptation
groups
communities.
Nature Communications,
Год журнала:
2022,
Номер
13(1)
Опубликована: Фев. 11, 2022
Abstract
Microbial
composition
and
functions
in
the
rhizosphere—an
important
microbial
hotspot—are
among
most
fascinating
yet
elusive
topics
ecology.
We
used
557
pairs
of
published
16S
rDNA
amplicon
sequences
from
bulk
soils
rhizosphere
different
ecosystems
around
world
to
generalize
bacterial
characteristics
with
respect
community
diversity,
composition,
functions.
The
selects
microorganisms
soil
function
as
a
seed
bank,
reducing
diversity.
is
enriched
Bacteroidetes,
Proteobacteria,
other
copiotrophs.
Highly
modular
but
unstable
networks
(common
for
r
-strategists)
reflect
interactions
adaptations
dynamic
conditions.
Dormancy
strategies
are
dominated
by
toxin–antitoxin
systems,
while
sporulation
common
soils.
Functional
predictions
showed
that
genes
involved
organic
compound
conversion,
nitrogen
fixation,
denitrification
were
strongly
(11–182%),
nitrification
depleted.
GCB Bioenergy,
Год журнала:
2021,
Номер
13(11), С. 1731 - 1764
Опубликована: Июль 27, 2021
Abstract
We
synthesized
20
years
of
research
to
explain
the
interrelated
processes
that
determine
soil
and
plant
responses
biochar.
The
properties
biochar
its
effects
within
agricultural
ecosystems
largely
depend
on
feedstock
pyrolysis
conditions.
describe
three
stages
reactions
in
soil:
dissolution
(1–3
weeks);
reactive
surface
development
(1–6
months);
aging
(beyond
6
months).
As
ages,
it
is
incorporated
into
aggregates,
protecting
carbon
promoting
stabilization
rhizodeposits
microbial
products.
Biochar
persists
for
hundreds
thousands
years.
By
increasing
pH,
porosity,
water
availability,
biochars
can
create
favorable
conditions
root
functions.
Biochars
catalyze
biotic
abiotic
reactions,
particularly
rhizosphere,
increase
nutrient
supply
uptake
by
plants,
reduce
phytotoxins,
stimulate
development,
resilience
disease
environmental
stressors.
Meta‐analyses
found
that,
average,
P
availability
a
factor
4.6;
decrease
tissue
concentration
heavy
metals
17%–39%;
build
organic
through
negative
priming
3.8%
(range
−21%
+20%);
non‐CO
2
greenhouse
gas
emissions
from
12%–50%.
show
average
crop
yield
increases
10%–42%
with
addition,
greatest
low‐nutrient
P‐sorbing
acidic
soils
(common
tropics),
sandy
drylands
due
retention
holding
capacity.
Studies
report
wide
range
diversity
contexts
which
have
been
applied.
Crop
yields
strongly
if
site‐specific
constraints
limitations
are
mitigated
appropriate
formulations.
be
tailored
address
site
selection,
modifying
conditions,
pre‐
or
post‐production
treatments,
co‐application
mineral
fertilizers.
demonstrate
how,
when
used
wisely,
mitigates
climate
change
supports
food
security
circular
economy.
Global Change Biology,
Год журнала:
2021,
Номер
27(12), С. 2763 - 2779
Опубликована: Март 12, 2021
Abstract
Temperature
sensitivity
(Q
10
)
of
soil
organic
matter
(SOM)
decomposition
is
a
crucial
parameter
to
predict
the
fate
carbon
(C)
under
global
warming.
Nonetheless,
response
pattern
Q
continuous
warming
and
underlying
mechanisms
are
still
debate,
especially
considering
complex
interactions
between
,
SOM
quality,
microorganisms.
We
examined
across
mean
annual
temperature
(MAT)
gradient
from
−1.9
5.1°C
in
temperate
mixed
forest
ecosystems
parallel
with
quality
bioavailability,
microbial
taxonomic
composition,
functional
genes
responsible
for
decomposition.
Within
this
7.0°C,
values
increased
MAT,
but
decreased
bioavailability.
The
prevalence
K‐strategy
community,
which
was
characterized
by:
(i)
high
ratios
oligotrophic
copiotrophic
taxa,
(ii)
ectomycorrhizal
saprotrophic
fungi,
(iii)
degradation
recalcitrant
that
labile
C,
(iv)
low
average
16S
rRNA
operon
copy
number.
Because
mainly
utilized
by
K‐strategists,
these
findings
independently
support
quality‐temperature
theory
perspective
composition
functions.
A
year‐long
incubation
experiment
performed
determine
C
pools
based
on
two‐pool
model.
more
sensitive
southern
warm
regions,
might
attribute
dominance
K‐selected
communities.
It
implies
climate
would
mobilize
larger
exacerbating
positive
feedback
MAT
CO
2
efflux.
This
first
attempt
link
eco‐strategies
incorporating
genetic
information
disentangling
relationship
Nature Communications,
Год журнала:
2022,
Номер
13(1)
Опубликована: Март 9, 2022
Abstract
Conceptual
and
empirical
advances
in
soil
biogeochemistry
have
challenged
long-held
assumptions
about
the
role
of
micro-organisms
organic
carbon
(SOC)
dynamics;
yet,
rigorous
tests
emerging
concepts
remain
sparse.
Recent
hypotheses
suggest
that
microbial
necromass
production
links
plant
inputs
to
SOC
accumulation,
with
high-quality
(i.e.,
rapidly
decomposing)
litter
promoting
use
efficiency,
growth,
turnover
leading
more
mineral
stabilization
necromass.
We
test
this
hypothesis
experimentally
observations
across
six
eastern
US
forests,
using
stable
isotopes
measure
traits
dynamics.
Here
we
show,
both
studies,
are
negatively
(not
positively)
related
mineral-associated
SOC.
In
experiment,
stimulation
growth
by
enhances
decomposition,
offsetting
positive
effect
quality
on
stabilization.
is
not
primary
driver
persistence
temperate
forests.
Factors
such
as
origin,
alternative
formation
pathways,
priming
effects,
abiotic
properties
can
strongly
decouple
from
Global Change Biology,
Год журнала:
2022,
Номер
28(7), С. 2169 - 2182
Опубликована: Янв. 3, 2022
In
this
concept
paper,
we
propose
a
new
view
on
soil
organic
matter
(SOM)
formation:
microorganisms
use
most
of
the
organics
entering
as
energy
rather
than
source
carbon
(C),
while
SOM
accumulates
residual
by-product
because
microbial
investment
in
its
decomposition
exceeds
gain.
During
initial
stages
decomposition,
nominal
oxidation
state
C
(NOSC)
remaining
litter
decreases,
and
content
increases.
This
reflects
rapid
mineralization
available
compounds
with
positive
neutral
NOSC
(carboxylic
acids,
sugars,
some
amino
acids).
Consequently,
drops
to
-0.3
units,
rate
decreases
due
relative
accumulation
aromatic
aliphatic
(which
are
hydrolized
later)
entombment
necromass.
Ultimately,
incompletely
decomposed
plant
residues
will
have
1%-2.5%
more
per
unit
litter.
The
linear
decrease
density
broad
range
substances
by
106
kJ
mol-1
upon
is
supported
experimental
data
decomposition.
Preferential
recycling
energy-rich
reduced
(lipids,
aromatics,
certain
sugars)
degradation
oxidized
acids)
also
energetically
enrich
SOM.
Despite
high
content,
availability
stored
lower
explains
why
not
fully
mineralized
(thermodynamically
unfavorable),
especially
absence
provide
(e.g.,
bare
soil).
Energy
from
activates
decomposers
mine
nutrients
(the
main
ecological
function
priming
effects)
nutrient
2-5
times
higher
that
results
only
0.4%-5%
year-1
litter-derived
being
sequestered
SOM,
whereas
stores
1%-10%
total
energy.
Thus,
captured
photosynthesis
reason
utilize
matter,
whereby
merely
storage
mediator
fluxes.
Communications Earth & Environment,
Год журнала:
2021,
Номер
2(1)
Опубликована: Авг. 6, 2021
Abstract
Rice
paddies
account
for
~9%
or
the
world’s
cropland
area
and
are
characterized
by
environmental
conditions
promoting
soil
organic
carbon
storage,
methane
emissions
to
a
lesser
extent
nitrous
oxide
emissions.
Here,
we
synthesize
data
from
612
sites
across
51
countries
estimate
global
stocks
in
paddy
soils
determine
main
factors
affecting
storage.
Paddy
(0–100
cm)
contain
18
Pg
worldwide.
decrease
with
increasing
mean
annual
temperature
pH,
whereas
precipitation
clay
content
had
minor
impacts.
Meta-analysis
shows
that
can
be
increased
through
several
management
practices.
However,
greenhouse
gas
mitigation
storage
is
generally
outweighed
increases
Our
results
emphasize
key
role
of
cycle,
importance
minimizing
anthropogenic
Biology and Fertility of Soils,
Год журнала:
2020,
Номер
56(8), С. 1093 - 1107
Опубликована: Май 14, 2020
Stoichiometric
control
of
input
substrate
(glucose)
and
native
soil
organic
C
(SOC)
mineralization
was
assessed
by
performing
a
manipulation
experiment
based
on
N
or
P
fertilization
in
paddy
soil.
Glucose
increased
with
nutrient
addition
up
to
11.6%
combined
application
compared
that
without
addition.
During
100
days
incubation,
approximately
4.5%
SOC
mineralized
stimulated
glucose
exponentially
dissolved
(DOC):NH4+-N,
DOC:Olsen
P,
microbial
biomass
(MB)C:MBN
ratios.
The
relative
abundances
Clostridia
β-Proteobacteria
(r-strategists)
were
NP
at
the
beginning
experiment,
while
Acidobacteria
(K-strategists)
enhanced
exhaustion
available
resource
end
incubation.
bacteria
abundance
diversity
negatively
related
DOC:NH4+-N
which
had
direct
positive
effects
(+
0.63)
mineralization.
Combined
decreased
network
density
bacterial
community.
Moreover,
significantly
negative
associations
among
taxa,
suggested
competition
for
nutrients
alleviated.
keystone
species
showed
significant
correlations
soils
application,
revealing
microbes
their
activity
mining
limited
from
matter.
Hence,
shifted
community
composition
interactions
acquire
necessary
elements
increasing
maintain
C:N:P
stoichiometric
balance
response
changes
stoichiometry.