Biological reviews/Biological reviews of the Cambridge Philosophical Society,
Год журнала:
2019,
Номер
95(1), С. 167 - 183
Опубликована: Окт. 18, 2019
ABSTRACT
Soil
organic
carbon
(SOC)
is
a
valuable
resource
for
mediating
global
climate
change
and
securing
food
production.
Despite
an
alarming
rate
of
plant
diversity
loss,
uncertainties
concerning
the
effects
on
SOC
remain,
because
not
only
stimulates
litter
inputs
via
increased
productivity,
thus
enhancing
SOC,
but
also
microbial
respiration,
reducing
SOC.
By
analysing
1001
paired
observations
mixtures
corresponding
monocultures
from
121
publications,
we
show
that
both
content
stock
are
average
5
8%
higher
in
species
than
monocultures.
These
positive
mixture
increase
over
time
more
pronounced
deeper
soils.
Microbial
biomass
carbon,
indicator
release
formation,
increases,
proportion
lower
mixtures.
Moreover,
these
species‐mixture
consistent
across
forest,
grassland,
cropland
systems
independent
background
climates.
Our
results
indicate
converting
50%
forests
to
would
2.70
Pg
C
soil
annually
period
20
years:
about
30%
annual
fossil‐fuel
emissions.
study
highlights
importance
preservation
maintenance
sequestration
discussions
policy.
Science,
Год журнала:
2022,
Номер
377(6606), С. 603 - 608
Опубликована: Авг. 4, 2022
Grasslands
store
approximately
one
third
of
the
global
terrestrial
carbon
stocks
and
can
act
as
an
important
soil
sink.
Recent
studies
show
that
plant
diversity
increases
organic
(SOC)
storage
by
elevating
inputs
to
belowground
biomass
promoting
microbial
necromass
contribution
SOC
storage.
Climate
change
affects
grassland
modifying
processes
catabolism
anabolism.
Improved
grazing
management
biodiversity
restoration
provide
low-cost
and/or
high-carbon-gain
options
for
natural
climate
solutions
in
grasslands.
The
achievable
sequestration
potential
grasslands
is
2.3
7.3
billion
tons
dioxide
equivalents
per
year
(CO2e
year-1)
restoration,
148
699
megatons
CO2e
year-1
improved
management,
147
sown
legumes
pasturelands.
In
the
effort
to
achieve
Sustainable
Development
Goals
(SDGs)
related
food,
health,
water,
and
climate,
an
increase
in
pressure
on
land
is
highly
likely.
To
avoid
further
degradation
promote
restoration,
multifunctional
use
of
needed
within
boundaries
soil-water
system.
addition,
awareness-raising,
a
change
stakeholders’
attitudes,
economics
are
essential.
The
attainment
balance
between
economy,
society,
biosphere
calls
for
holistic
approach.
this
paper,
we
introduce
four
concepts
that
consider
be
conducive
realizing
LDN
more
integrated
way:
systems
thinking,
connectivity,
nature-based
solutions,
regenerative
economics.
We
illustrate
application
these
through
three
examples
agricultural
settings.
Systems
thinking
lies
at
base
others,
stressing
feedback
loops
but
also
delayed
responses.
Their
simultaneous
will
result
robust
which
sustainable
from
environmental,
societal,
economic
point
view.
Solutions
need
take
into
account
level
scale
(global,
national,
regional,
local),
interests
culture,
availability
financial
natural
capital.
Furthermore,
solutions
embed
short-term
management
long-term
landscape
planning.
conclusion,
paradigm
shifts
needed.
First,
it
necessary
move
excessive
exploitation
combination
with
environmental
protection,
accomplish
this,
new
business
models
based
thinking;
approach
integrates
social,
interests.
Second,
shift
“system
follows
function”
towards
“function
system”
one.
Only
by
making
transition
socio-economical-ecological
analysis,
using
such
as
do
stand
chance
Land
Degradation
Neutrality
2030.
make
shifts,
awareness-raising
relation
different
type
governance,
economy
land-use
planning
Forest Ecology and Management,
Год журнала:
2020,
Номер
466, С. 118127 - 118127
Опубликована: Апрель 8, 2020
Almost
half
of
the
total
organic
carbon
(C)
in
terrestrial
ecosystems
is
stored
forest
soils.
By
altering
rates
input
or
release
C
from
soils,
management
activities
can
influence
soil
stocks
forests.
In
this
review,
we
synthesize
current
evidence
regarding
influences
13
common
practices
on
stocks.
Afforestation
former
croplands
generally
increases
stocks,
whereas
grasslands
and
peatlands,
are
unchanged
even
reduced
following
afforestation.
The
conversion
primary
forests
to
secondary
reduces
particularly
if
land
converted
an
agricultural
land-use
prior
reforestation.
Harvesting,
clear-cut
harvesting,
results
a
reduction
floor
upper
mineral
soil.
Removal
residues
by
harvesting
whole-trees
stumps
negatively
affects
Soil
disturbance
site
preparation
decreases
top
soil,
however
improved
growth
tree
seedlings
may
outweigh
losses
over
rotation.
Nitrogen
(N)
addition
has
overall
positive
effect
across
wide
range
ecosystems.
Likewise,
higher
faster
accumulation
occur
under
species
with
N-fixing
associates.
Stocks
also
differ
different
species,
coniferous
accumulating
more
broadleaved
tending
store
There
some
that
increased
diversity
could
positively
affect
temperate
subtropical
forests,
but
identity,
seems
have
stronger
impact
than
diversity.
Management
stand
density
thinning
small
effects
high
populations
ungulate
herbivores,
herbivory
levels
increase
plant
biomass
for
fodder
fuel
related
Fire
such
as
prescribed
burning
reduce
less
so
wildfires
which
intense.
For
each
practice,
identify
existing
gaps
knowledge
suggest
research
address
gaps.
Global Change Biology,
Год журнала:
2018,
Номер
25(1), С. 12 - 24
Опубликована: Окт. 19, 2018
To
predict
the
behavior
of
terrestrial
carbon
cycle,
it
is
critical
to
understand
source,
formation
pathway,
and
chemical
composition
soil
organic
matter
(SOM).
There
emerging
consensus
that
slow-cycling
SOM
generally
consists
relatively
low
molecular
weight
substrates
enter
mineral
as
dissolved
associate
with
surfaces
(referred
"mineral-associated
OM,"
or
MAOM).
However,
much
debate
contradictory
evidence
persist
around:
(a)
whether
C
within
MAOM
pool
primarily
originate
from
aboveground
vs.
belowground
plant
sources
(b)
directly
sorb
undergo
microbial
transformation
prior
their
incorporation
into
MAOM.
Here,
we
attempt
reconcile
disparate
views
on
by
proposing
a
spatially
explicit
set
processes
link
source
pathway.
Specifically,
because
distinct
regions
soil,
propose
fine-scale
differences
in
abundance
should
determine
probability
substrate-microbe
substrate-mineral
interaction.
Thus,
areas
high
density
(e.g.,
rhizosphere
other
hotspots)
occur
through
an
vivo
turnover
pathway
favor
are
first
biosynthesized
carbon-use
efficiency
pool.
In
contrast,
certain
bulk
soil),
direct
sorption
intact
partially
oxidized
compounds
uncolonized
surfaces,
minimizing
importance
efficiency,
favoring
strong
"sorptive
affinity."
Through
this
framework,
thus
describe
how
primacy
biotic
abiotic
controls
dynamics
not
mutually
exclusive,
but
rather
dictated.
Such
understanding
may
be
integral
more
accurately
modeling
across
different
spatial
scales.
New Phytologist,
Год журнала:
2020,
Номер
229(5), С. 2413 - 2445
Опубликована: Авг. 13, 2020
Atmospheric
carbon
dioxide
concentration
([CO2
])
is
increasing,
which
increases
leaf-scale
photosynthesis
and
intrinsic
water-use
efficiency.
These
direct
responses
have
the
potential
to
increase
plant
growth,
vegetation
biomass,
soil
organic
matter;
transferring
from
atmosphere
into
terrestrial
ecosystems
(a
sink).
A
substantial
global
sink
would
slow
rate
of
[CO2
]
thus
climate
change.
However,
ecosystem
CO2
are
complex
or
confounded
by
concurrent
changes
in
multiple
agents
change
evidence
for
a
]-driven
can
appear
contradictory.
Here
we
synthesize
theory
broad,
multidisciplinary
effects
increasing
(iCO2
)
on
sink.
Evidence
suggests
since
pre-industrial
times.
Established
theory,
supported
experiments,
indicates
that
iCO2
likely
responsible
about
half
increase.
Global
budgeting,
atmospheric
data,
forest
inventories
indicate
historical
sink,
these
apparent
high
comparison
experiments
predictions
theory.
Plant
mortality
highly
uncertain.
In
conclusion,
range
supports
positive
response
,
albeit
with
uncertain
magnitude
strong
suggestion
role
additional
New Phytologist,
Год журнала:
2018,
Номер
221(1), С. 233 - 246
Опубликована: Авг. 1, 2018
Soil
organic
carbon
(SOC)
is
primarily
formed
from
plant
inputs,
but
the
relative
(C)
contributions
living
root
inputs
(i.e.
rhizodeposits)
vs
litter
+
shoot
litter)
are
poorly
understood.
Recent
theory
suggests
that
exert
a
disproportionate
influence
on
SOC
formation,
few
field
studies
have
explicitly
tested
this
by
separately
tracking
as
they
move
through
soil
food
web
and
into
distinct
pools.
We
used
manipulative
experiment
with
an
annual
C4
grass
in
forest
understory
to
differentially
track
its
assess
net
formation
over
multiple
years.
show
2-13
times
more
efficient
than
forming
both
slow-cycling,
mineral-associated
well
fast-cycling,
particulate
C.
Furthermore,
we
demonstrate
efficiently
anabolized
microbial
community
en
route
pool
(dubbed
'the
vivo
turnover
pathway').
Overall,
our
findings
provide
support
for
primacy
of
SOC.
However,
also
highlight
possibility
nonadditive
effects
which
may
deplete
pools
despite
greater
rates.
Nature Communications,
Год журнала:
2022,
Номер
13(1)
Опубликована: Июль 1, 2022
Abstract
Soil
is
the
largest
terrestrial
reservoir
of
organic
carbon
and
central
for
climate
change
mitigation
carbon-climate
feedbacks.
Chemical
physical
associations
soil
with
minerals
play
a
critical
role
in
storage,
but
amount
global
capacity
storage
this
form
remain
unquantified.
Here,
we
produce
spatially-resolved
estimates
mineral-associated
stocks
carbon-storage
by
analyzing
1144
globally-distributed
profiles.
We
show
that
current
total
899
Pg
C
to
depth
1
m
non-permafrost
mineral
soils.
Although
constitutes
66%
70%
surface
deeper
layers,
respectively,
it
only
42%
21%
mineralogical
capacity.
Regions
under
agricultural
management
layers
undersaturation
carbon.
Critically,
degree
indicates
sequestration
efficiency
over
years
decades.
that,
across
103
carbon-accrual
measurements
spanning
interventions
globally,
soils
furthest
from
their
are
more
effective
at
accruing
carbon;
rates
average
3-times
higher
one
tenth
compared
half
Our
findings
provide
insights
into
world’s
soils,
store
carbon,
priority
regions
actions
management.
Nature Communications,
Год журнала:
2019,
Номер
10(1)
Опубликована: Фев. 12, 2019
Abstract
Agriculturally
degraded
and
abandoned
lands
can
remove
atmospheric
CO
2
sequester
it
as
soil
organic
matter
during
natural
succession.
However,
this
process
may
be
slow,
requiring
a
century
or
longer
to
re-attain
pre-agricultural
carbon
levels.
Here,
we
find
that
restoration
of
late-successional
grassland
plant
diversity
leads
accelerating
annual
storage
rates
that,
by
the
second
period
(years
13–22),
are
200%
greater
in
our
highest
treatment
than
succession
at
site,
70%
monocultures.
The
higher
13–22)
associated
with
aboveground
production
root
biomass
period,
presence
multiple
species,
especially
C4
grasses
legumes.
Our
results
suggest
high
greatly
increase
capture
on
agricultural
lands.