Global Change Biology,
Journal Year:
2020,
Volume and Issue:
27(6), P. 1170 - 1180
Published: Dec. 18, 2020
Abstract
Soil
organic
carbon
(SOC)
is
the
largest
sink
in
terrestrial
ecosystems
and
plays
a
critical
role
mitigating
climate
change.
Increasing
reactive
nitrogen
(N)
caused
by
anthropogenic
N
input
substantially
affects
SOC
dynamics.
However,
uncertainties
remain
concerning
effects
of
addition
on
both
mineral
soil
layers
over
time
at
global
scale.
Here,
we
analysed
large
empirical
data
set
spanning
60
years
across
369
sites
worldwide
to
explore
temporal
dynamics
addition.
We
found
that
significantly
increased
globe
4.2%
(2.7%–5.8%).
increases
were
amplified
from
short‐
long‐term
durations
layers.
The
positive
independent
ecosystem
types,
mean
annual
temperature
precipitation.
Our
findings
suggest
largely
resulted
enhanced
plant
C
soils
coupled
with
reduced
loss
decomposition
amplification
was
associated
microbial
biomass
respiration
under
study
suggests
will
enhance
sequestration
contribute
future
change
mitigation.
Estuarine Coastal and Shelf Science,
Journal Year:
2021,
Volume and Issue:
255, P. 107361 - 107361
Published: April 3, 2021
The
term
'Blue
Carbon'
was
coined
about
a
decade
ago
to
highlight
the
important
carbon
sequestration
capacity
of
coastal
vegetated
ecosystems.
has
paved
way
for
development
programs
and
policies
that
preserve
restore
these
threatened
ecosystems
climate
change
mitigation.
Blue
research
focused
on
quantifying
stocks
burial
rates
in
sediments
or
accumulating
as
biomass.
This
focus
habitat-bound
led
us
losing
sight
mobile
blue
fraction.
Oceans,
largest
active
reservoir
carbon,
have
become
somewhat
blind
spot.
Multiple
recent
investigations
revealed
high
outwelling
(i.e.,
lateral
fluxes
horizontal
exports)
dissolved
inorganic
(DIC)
organic
(DOC)
well
particulate
(POC)
from
habitats.
In
this
paper,
we
conceptualize
mangrove,
saltmarsh,
seagrass
macroalgae
ecosystems,
diagnose
key
challenges
preventing
robust
quantification,
pave
future
work
integrating
framework.
Outwelling
mangroves
saltmarshes
is
usually
dominated
by
DIC
(mostly
bicarbonate),
while
POC
seems
be
major
species
exported
meadows
forests.
Carbon
science
still
its
infancy,
estimates
remain
limited
spatially
temporally.
Nevertheless,
existing
datasets
imply
followed
ocean
storage
relevant
may
exceed
local
sediment
long-term
(>centuries)
mechanism.
If
proves
correct
more
data
emerge,
ignoring
underestimate
perceived
Frontiers in Marine Science,
Journal Year:
2020,
Volume and Issue:
7
Published: March 25, 2020
To
develop
more
accurate
global
carbon
(C)
budgets
and
to
better
inform
management
of
human
activities
in
the
ocean,
we
need
high-resolution
estimates
marine
C
stocks.
Here
quantify
sedimentary
stocks
at
a
1-km
resolution,
find
that
sediments
store
2322
(2239–2391)
Pg
top
1
m
(nearly
twice
terrestrial
soils).
Sediments
abyss/basin
zones
account
for
79%
sediment
stock,
49%
stock
is
within
200-mile
Exclusive
Economic
Zones
countries.
Currently,
only
∼2%
are
located
highly
fully
protected
areas
prevent
disturbance
seafloor.
Our
results
show
represent
large
globally
important
sink.
However,
lack
protection
makes
them
vulnerable
disturbances
can
lead
their
remineralization
CO
2
,
further
aggravating
climate
change
impacts.
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
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
27(12), P. 2856 - 2866
Published: March 1, 2021
Abstract
Mangroves
have
among
the
highest
carbon
densities
of
any
tropical
forest.
These
‘blue
carbon’
ecosystems
can
store
large
amounts
for
long
periods,
and
their
protection
reduces
greenhouse
gas
emissions
supports
climate
change
mitigation.
Incorporating
mangroves
into
Nationally
Determined
Contributions
to
Paris
Agreement
valuation
on
markets
requires
predicting
how
management
different
land‐uses
prevent
future
increase
CO
2
sequestration.
We
integrated
comprehensive
global
datasets
stocks,
mangrove
distribution,
deforestation
rates,
land‐use
drivers
a
predictive
model
emissions.
project
foregone
soil
sequestration
potential
under
‘business
as
usual’
rates
loss.
Emissions
from
loss
could
reach
2391
Tg
eq
by
end
century,
or
3392
when
considering
The
were
predicted
in
southeast
south
Asia
(West
Coral
Triangle,
Sunda
Shelf,
Bay
Bengal)
due
conversion
aquaculture
agriculture,
followed
Caribbean
(Tropical
Northwest
Atlantic)
clearing
erosion,
Andaman
coast
Myanmar)
north
Brazil
erosion.
Together,
these
six
regions
accounted
90%
total
Mangrove
has
been
slowing,
be
more
than
halved
if
reduced
remain
future.
Notably,
location
emission
hotspots
was
consistent
with
every
dataset
used
calculate
alternative
assumptions
about
storage
Our
results
indicate
need
policy
actions
address
arising
that
managed
them.
Global Change Biology,
Journal Year:
2020,
Volume and Issue:
27(6), P. 1170 - 1180
Published: Dec. 18, 2020
Abstract
Soil
organic
carbon
(SOC)
is
the
largest
sink
in
terrestrial
ecosystems
and
plays
a
critical
role
mitigating
climate
change.
Increasing
reactive
nitrogen
(N)
caused
by
anthropogenic
N
input
substantially
affects
SOC
dynamics.
However,
uncertainties
remain
concerning
effects
of
addition
on
both
mineral
soil
layers
over
time
at
global
scale.
Here,
we
analysed
large
empirical
data
set
spanning
60
years
across
369
sites
worldwide
to
explore
temporal
dynamics
addition.
We
found
that
significantly
increased
globe
4.2%
(2.7%–5.8%).
increases
were
amplified
from
short‐
long‐term
durations
layers.
The
positive
independent
ecosystem
types,
mean
annual
temperature
precipitation.
Our
findings
suggest
largely
resulted
enhanced
plant
C
soils
coupled
with
reduced
loss
decomposition
amplification
was
associated
microbial
biomass
respiration
under
study
suggests
will
enhance
sequestration
contribute
future
change
mitigation.