Global Change Biology,
Journal Year:
2022,
Volume and Issue:
28(8), P. 2527 - 2540
Published: Jan. 6, 2022
Associations
between
soil
minerals
and
microbially
derived
organic
matter
(often
referred
to
as
mineral-associated
or
MAOM)
form
a
large
pool
of
slowly
cycling
carbon
(C).
The
rhizosphere,
immediately
adjacent
roots,
is
thought
control
the
spatial
extent
MAOM
formation
because
it
dominant
entry
point
new
C
inputs
soil.
However,
emphasis
on
rhizosphere
implicitly
assumes
that
microbial
redistribution
into
bulk
(non-rhizosphere)
soils
minimal.
We
question
this
assumption,
arguing
extensive
fungal
exploration
rapid
hyphal
turnover,
from
common,
encourages
formation.
First,
we
summarize
published
estimates
length
density
turnover
rates
demonstrate
are
high
throughout
rhizosphere-bulk
continuum.
Second,
colonization
surfaces
common
dispersal
mechanism
for
bacteria,
argue
allows
non-random
mineral
by
hyphae-associated
taxa.
Third,
these
bacterial
communities
their
hosts
determine
chemical
deposited
colonized
surfaces.
Collectively,
our
analysis
demonstrates
omission
hyphosphere
conceptual
models
flow
overlooks
key
mechanisms
in
soils.
Moving
forward,
there
clear
need
spatially
explicit,
quantitative
research
characterizing
environmental
drivers
community
composition
across
systems,
important
controls
over
rate
chemistry
minerals.
Global Change Biology,
Journal Year:
2022,
Volume and Issue:
28(10), P. 3426 - 3440
Published: Jan. 29, 2022
Global
changes
can
alter
plant
inputs
from
both
above-
and
belowground,
which,
thus,
may
differently
affect
soil
carbon
microbial
communities.
However,
the
general
patterns
of
how
input
them
in
forests
remain
unclear.
By
conducting
a
meta-analysis
3193
observations
166
experiments
worldwide,
we
found
that
alterations
aboveground
litter
and/or
root
had
profound
effects
on
communities
forest
ecosystems.
Litter
addition
stimulated
organic
(SOC)
pools
biomass,
whereas
removal
litter,
roots
or
(no
inputs)
decreased
them.
The
increased
SOC
under
suggested
benefit
sequestration
despite
accelerated
decomposition.
Unlike
removal,
no
altered
particulate
carbon,
all
detrital
treatments
did
not
significantly
change
mineral-associated
carbon.
In
addition,
contrastingly
community,
with
shifting
it
toward
fungi,
bacteria.
Furthermore,
responses
biomass
to
positively
correlated
rate
total
input,
suggesting
quantity
is
critical
controller
belowground
processes.
Taken
together,
these
findings
provide
insights
into
understanding
productivity
allocation
affects
cycling,
functioning
ecosystems
global
changes.
Future
studies
take
full
advantage
existing
detritus
should
focus
relative
roles
forming
its
fractions.
Nature Communications,
Journal Year:
2022,
Volume and Issue:
13(1)
Published: March 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
Functional Ecology,
Journal Year:
2022,
Volume and Issue:
36(6), P. 1411 - 1429
Published: March 7, 2022
Abstract
Soil
organic
matter
(SOM)
is
the
largest
actively
cycling
reservoir
of
terrestrial
carbon
(C),
and
majority
SOM
in
Earth's
mineral
soils
(~65%)
mineral‐associated
(MAOM).
Thus,
formation
fate
MAOM
can
exert
substantial
influence
on
global
C
cycle.
To
predict
future
changes
to
climate,
it
critical
mechanistically
understand
processes
by
which
formed
decomposed,
accurately
represent
this
process‐based
understanding
biogeochemical
Earth
system
models.
In
review,
we
use
a
trait‐based
framework
synthesize
interacting
roles
plants,
soil
micro‐organisms,
matrix
regulating
decomposition.
Our
proposed
differentiates
between
plant
microbial
traits
that
total
OM
inputs
(‘feedstock
traits’)
versus
proportion
are
ultimately
incorporated
into
(‘MAOM
traits’).
We
discuss
how
these
feedstock
may
be
altered
warming,
precipitation
elevated
dioxide.
At
planetary
scale,
help
shape
distribution
across
biomes,
modulate
biome‐specific
responses
climate
change.
leverage
synthesis
measurements
provide
estimates
amount
MAOM‐C
globally
(~840–1540
Pg
C;
34%–51%
C),
its
biomes.
show
concentration
highest
temperate
forests
grasslands,
lowest
shrublands
savannas.
Grasslands
croplands
have
(SOC)
fraction
(i.e.
MAOM‐C:SOC
ratio),
while
boreal
tundra
ratio.
Drawing
our
trait
framework,
then
review
experimental
data
posit
effects
change
pools
different
conclude
discussing
integrated
models,
included
also
summarize
projected
under
scenarios
(Representative
Concentration
Pathways
4.5
8.5)
key
model
uncertainties.
Read
free
Plain
Language
Summary
for
article
Journal
blog.
Global Change Biology,
Journal Year:
2022,
Volume and Issue:
28(24), P. 7167 - 7185
Published: Aug. 31, 2022
Predicting
and
mitigating
changes
in
soil
carbon
(C)
stocks
under
global
change
requires
a
coherent
understanding
of
the
factors
regulating
organic
matter
(SOM)
formation
persistence,
including
knowledge
direct
sources
SOM
(plants
vs.
microbes).
In
recent
years,
conceptual
models
have
emphasized
primacy
microbial-derived
inputs,
proposing
that
microbial
physiological
traits
(e.g.,
growth
efficiency)
are
dominant
controls
on
quantity.
However,
quantitative
studies
challenged
this
view,
suggesting
plants
make
larger
contributions
to
than
is
currently
recognized
by
paradigm.
review,
we
attempt
reconcile
these
perspectives
highlighting
variation
across
estimates
plant-
versus
may
arise
part
from
methodological
limitations.
We
show
all
major
methods
used
estimate
plant
substantial
shortcomings,
uncertainty
our
current
estimates.
demonstrate
there
significant
overlap
chemical
signatures
compounds
produced
microbes,
roots,
through
extracellular
decomposition
litter,
which
introduces
into
use
common
biomarkers
for
parsing
SOM,
especially
mineral-associated
(MAOM)
fraction.
Although
review
contributed
deeper
limitations
with
constrain
light
advances,
suggest
now
critical
time
re-evaluate
long-standing
methods,
clearly
define
their
limitations,
develop
strategic
plan
improving
quantification
SOM.
From
synthesis,
outline
key
questions
challenges
future
research
mechanisms
stabilization
pathways.
Ecological Applications,
Journal Year:
2020,
Volume and Issue:
31(3)
Published: Dec. 20, 2020
Increasing
the
quantity
and
quality
of
plant
biomass
production
in
space
time
can
improve
capacity
agroecosystems
to
capture
store
atmospheric
carbon
(C)
soil.
Cover
cropping
is
a
key
practice
increase
system
net
primary
productivity
(NPP)
high-quality
residues
available
for
integration
into
soil
organic
matter
(SOM).
crop
management
local
environmental
conditions,
however,
influence
magnitude
C
stock
change.
Here,
we
used
comprehensive
meta-analysis
approach
quantify
effect
cover
crops
on
stocks
from
0-30
cm
depth
temperate
climates
identify
ecological
factors
that
impact
variation
this
response.
A
total
40
publications
with
181
observations
were
included
representing
six
countries
across
three
different
continents.
Overall,
had
strong
positive
(P
<
0.0001)
leading
12%
increase,
averaging
1.11
Mg
C/ha
more
relative
no
control.
The
strongest
predictors
SOC
response
planting
termination
date
(i.e.,
growing
window),
annual
production,
clay
content.
planted
as
continuous
or
autumn
terminated
led
20-30%
greater
other
windows.
Likewise,
high
(>7
Mg·ha-1
·yr-1
)
resulted
30%
higher
than
lower
levels
production.
Managing
NPP
by
improving
synchronization
windows
climate
will
enhance
drawdown
dioxide
(CO2
atmosphere
agroecosystems.
window
(potentially
proxy
growth),
climate,
decision-support
tools
are
relevant
quantification
change
under
crops,
particularly
expansion
terrestrial
markets.
Crop Science,
Journal Year:
2019,
Volume and Issue:
59(2), P. 441 - 459
Published: Feb. 21, 2019
Ecosystem
services
(ES)
are
the
direct
and
indirect
contributions
of
ecosystems
to
human
well‐being.
Grassland
cover
>40%
Earth's
ice‐free
terrestrial
surface,
grassland
management
affects
ES
provided.
Our
objective
was
synthesize
existing
literature
assessing
effects
on
regulating
supporting
provided
by
grasslands,
explore
related
mechanisms,
determine
which
practices
favor
delivery.
Current
supports
following
conclusions.
Increasing
intensity
grasslands
through
planting
more
productive
species
or
increasing
fertilizer
inputs
generally
increases
soil
organic
C
(SOC)
accumulation.
number
plant
functional
groups,
especially
when
legumes
added,
often
SOC
Grazed
accumulate
rapidly
than
undefoliated
grasslands.
Low
moderate
stocking
rates
accumulation
relative
high
rates,
in
lower‐rainfall
environments.
Short‐term
observed
after
conversion
cropland
perennial
do
not
continue
indefinitely.
More
digestible
forages
defoliated
at
optimal
maturity
may
decrease
CH
4
emitted
per
unit
feed
consumed
animal
product.
Substituting
for
N
reducing
livestock
excretion
diet
manipulation
reduce
2
O
emissions.
Managing
grazing
increase
uniformity
excreta
deposition
efficiency
nutrient
cycling.
Species‐rich
with
flower‐rich
forbs
foraging
opportunities
pollinators.
Finally,
optimize
delivery
ES,
that
sustain
ecosystem
function
likely
need
replace
those
maximize
short‐term
resource
utilization
economic
return.
To
encourage
adoption,
such
be
incentivized.