Marine Life Science & Technology,
Год журнала:
2024,
Номер
6(1), С. 168 - 181
Опубликована: Янв. 23, 2024
Abstract
Hadal
trenches
are
characterized
by
enhanced
and
infrequent
high-rate
episodic
sedimentation
events
that
likely
introduce
not
only
labile
organic
carbon
key
nutrients
but
also
new
microbes
significantly
alter
the
subseafloor
microbiosphere.
Currently,
role
of
in
controlling
composition
hadal
microbiosphere
is
unknown.
Here,
analyses
isotope
a
~
750
cm
long
sediment
core
from
Challenger
Deep
revealed
noncontinuous
deposition,
with
anomalous
14
C
ages
caused
seismically
driven
mass
transport
funneling
effect
trench
geomorphology.
Microbial
community
diverse
enzyme
activities
upper
27
differed
those
at
lower
depths,
probably
due
to
sudden
deposition
differences
redox
condition
matter
availability.
At
microbial
population
numbers,
remained
relatively
constant,
except
some
discrete
depths
altered
activity
phyla
abundance,
possibly
additional
different
magnitude.
Evidence
provided
unique
for
subsurface
Earth’s
deepest
ocean
floor
highlight
need
perform
thorough
analysis
over
large
depth
range
characterize
benthic
populations.
Such
depositional
processes
crucial
shaping
deep-water
geochemical
environments
thereby
deep
biosphere.
One Earth,
Год журнала:
2020,
Номер
3(2), С. 195 - 211
Опубликована: Авг. 1, 2020
Summary
Blue
carbon
provides
opportunities
to
mitigate
climate
change
while
increasing
ecosystem
services
for
coastal
communities,
including
adaptation;
however,
blue
ecosystems
are
vulnerable
change,
leading
uncertainties
in
the
future
efficacy
of
these
ecosystems.
In
this
review,
we
assess
potential
impacts
on
carbon.
Despite
uncertainties,
sequestration
is
enhanced
by
landward
migration
habitats,
maintenance
sediment
supply,
restoration,
and
improved
water
quality.
As
an
example,
mangroves
could
result
1.5
Pg
2100.
Mudflats,
seaweed
beds,
swamp
forests
also
contribute
mitigation,
although
there
large
data
gaps.
Achieving
full
requires
protection
restoration
facilitation
changes
distributions
with
actions
that
will
deliver
adaptation
benefits.
Conversely,
worst-case
squeeze
scenario,
losses
3.4
sequestered
2100
occur.
Global Change Biology,
Год журнала:
2022,
Номер
28(20), С. 6065 - 6085
Опубликована: Июнь 30, 2022
Soil
organic
carbon
(SOC)
in
coastal
wetlands,
also
known
as
"blue
C,"
is
an
essential
component
of
the
global
C
cycles.
To
gain
a
detailed
insight
into
blue
storage
and
controlling
factors,
we
studied
142
sites
across
ca.
5000
km
covering
temperate,
subtropical,
tropical
climates
China.
The
wetlands
represented
six
vegetation
types
(Phragmites
australis,
mixed
P.
australis
Suaeda,
single
Spartina
alterniflora,
mangrove
[Kandelia
obovata
Avicennia
marina],
tidal
flat)
three
invaded
by
S.
alterniflora
(P.
K.
obovata,
A.
marina).
Our
results
revealed
large
spatial
heterogeneity
SOC
density
top
1-m
ranging
40-200
Mg
ha-1
,
with
higher
values
mid-latitude
regions
(25-30°
N)
compared
those
both
low-
(20°N)
high-latitude
(38-40°N)
regions.
Vegetation
type
influenced
density,
having
largest
followed
mangrove,
Suaeda
flat.
increased
6.25
following
invasion
community
but
decreased
28.56
8.17
marina
communities.
Based
on
field
measurements
published
literature,
calculated
total
inventory
57
×
106
soil
China's
wetlands.
Edaphic
variables
controlled
content,
chemical
properties
explaining
variance
content.
Climate
did
not
control
content
had
strong
interactive
effect
edaphic
variables.
Plant
biomass
quality
traits
were
minor
contributor
regulating
highlighting
importance
quantity
OC
inputs
balance
between
production
degradation
within
These
findings
provide
new
insights
stabilization
mechanisms
sequestration
capacity
Global Change Biology,
Год журнала:
2018,
Номер
24(11), С. 5361 - 5379
Опубликована: Июнь 29, 2018
Coastal
wetlands
are
among
the
most
productive
and
carbon-rich
ecosystems
on
Earth.
Long-term
carbon
storage
in
coastal
occurs
primarily
belowground
as
soil
organic
matter
(SOM).
In
addition
to
serving
a
sink,
SOM
influences
wetland
ecosystem
structure,
function,
stability.
To
anticipate
mitigate
effects
of
climate
change,
there
is
need
advance
understanding
environmental
controls
SOM.
Here,
we
investigated
influence
four
formation
factors:
climate,
biota,
parent
materials,
topography.
Along
northern
Gulf
Mexico,
collected
plant
data
across
elevation
zonation
gradients
within
10
estuaries
that
span
broad
temperature
precipitation
gradients.
Our
results
highlight
importance
climate-plant
indicate
scale
location
dependent.
plants
sensitive
change;
small
changes
or
can
transform
communities.
Across
region,
was
greatest
mangrove
forests
salt
marshes
dominated
by
graminoid
plants.
lower
flats
lacked
vascular
succulent
We
quantified
strong
relationships
between
precipitation,
salinity,
productivity,
Low
leads
high
which
limits
productivity
appears
constrain
accumulation.
analyses
use
from
but
our
be
related
globe
provide
foundation
for
predicting
ecological
future
reductions
freshwater
availability.
many
services
dependent
highly
vulnerable
change.
Collectively,
regulated
cascading
availability
could
impact
stability
affect
supply
some
services.
Global Change Biology,
Год журнала:
2018,
Номер
24(6), С. 2498 - 2512
Опубликована: Фев. 12, 2018
Abstract
Tidal
marshes
are
vegetated
coastal
ecosystems
that
often
considered
as
hotspots
of
atmospheric
CO
2
sequestration.
Although
large
amounts
organic
carbon
(
OC
)
indeed
being
deposited
on
tidal
marshes,
there
is
no
direct
link
between
high
deposition
rates
and
sequestration
due
to
two
main
reasons.
First,
the
may
become
rapidly
decomposed
once
it
buried
and,
second,
a
significant
part
preserved
be
allochthonous
has
been
sequestered
elsewhere.
In
this
study
we
aimed
identify
mechanisms
controlling
long‐term
in
marsh
sediments
along
an
estuarine
salinity
gradient
(Scheldt
estuary,
Belgium
Netherlands).
Analyses
have
shown
during
inundations
up
millennia
old.
This
component
effectively
these
sediments,
indicated
by
low
radiocarbon
content
.
Furthermore,
fractionation
showed
autochthonous
decadal
timescale
saltmarsh
while
freshwater
locally
produced
biomass
more
efficiently
after
burial.
Our
results
show
decoupled
from
local
production
studied
sediments.
implies
greatly
overestimated
when
they
calculated
based
short‐term
rates,
which
controlled
labile
inputs.
Moreover,
not
in‐situ,
does
contribute
active
ecosystems.
A
correct
assessment
contribution
total
sedimentary
stock
well
understanding
fate
both
necessary
avoid
overestimations
rate
in‐situ
Frontiers in Marine Science,
Год журнала:
2019,
Номер
6
Опубликована: Май 22, 2019
Blue
carbon
is
the
organic
in
oceanic
and
coastal
ecosystems
that
captured
on
centennial
to
millennial
timescales.
Maintaining
increasing
blue
an
integral
component
of
strategies
mitigate
global
warming.
Marine
vegetated
(especially
seagrass
meadows,
mangrove
forests,
tidal
marshes)
are
hotspots
their
degradation
loss
worldwide
have
reduced
stocks
increased
CO2
emissions.
Carbon
markets,
conservation
restoration
schemes
aimed
at
enhancing
sequestration
avoiding
greenhouse
gas
emissions,
will
be
aided
by
knowing
provenance
fate
carbon.
We
review
critique
current
methods
potential
nascent
track
carbon,
including:
bulk
isotopes,
compound-specific
biomarkers,
molecular
properties,
environmental
DNA.
find
most
studies
date
used
isotopes
determine
provenance,
but
this
approach
often
cannot
distinguish
contribution
different
primary
producers
depositional
marine
environments.
Based
our
assessment,
we
recommend
application
multiple
complementary
methods.
In
particular,
use
nitrogen
lipids
along
with
DNA
a
great
identify
source
quantify
sedimentary
ecosystems.
Despite
promising
these
new
techniques,
further
research
needed
validate
them.
This
critical
overview
can
inform
future
help
underpin
methodologies
for
implementation
focused
climate
change
mitigation
schemes.
Abstract
Climate
greatly
influences
the
structure
and
functioning
of
tidal
saline
wetland
ecosystems.
However,
there
is
a
need
to
better
quantify
effects
climatic
drivers
on
ecosystem
properties,
particularly
near
climate‐sensitive
ecological
transition
zones.
Here,
we
used
climate‐
literature‐derived
data
from
wetlands
test
hypotheses
regarding
influence
(i.e.,
temperature
precipitation
regimes)
following
six
properties:
canopy
height,
biomass,
productivity,
decomposition,
soil
carbon
density,
accumulation.
Our
analyses
elucidate
linear
nonlinear
drivers.
We
quantified
positive
relationships
between
above‐ground
productivity
strong
(sigmoidal)
(1)
biomass
height
(2)
height.
Near
temperature‐controlled
mangrove
range
limits,
small
changes
in
are
expected
trigger
comparatively
large
as
forests
grow,
expand,
and,
some
cases,
replace
salt
marshes.
within
these
same
zones,
temperature‐induced
be
small.
Interestingly,
despite
significant
across
tropical–temperate
mangrove–marsh
zone,
density
or
accumulation
were
not
significant.
literature
review
identifies
several
properties
many
regions
world
for
which
insufficient
fully
evaluate
drivers,
identified
gaps
can
by
scientists
guide
future
research.
indicate
that
precipitation‐controlled
scant
other
properties.
There
more
decomposition
gradients,
advance
understanding
freshwater
availability,
additional
needed
arid
climates.
Collectively,
our
results
help
managers
anticipate
consequences
climate
change
coastal
wetlands.
Global Change Biology,
Год журнала:
2020,
Номер
27(1), С. 202 - 214
Опубликована: Сен. 25, 2020
Abstract
Global
vegetated
coastal
habitats
(VCHs)
represent
a
large
sink
for
organic
carbon
(OC)
stored
within
their
soils.
The
regional
patterns
and
causes
of
spatial
variation,
however,
remain
uncertain.
sparsity
bias
studies
on
soil
OC
stocks
from
Chinese
VCHs
have
limited
the
reliable
estimation
capacity
as
global
sinks.
Here,
we
use
field
published
data
262
sampled
cores
181
surface
soils
to
report
estimates
stocks,
burial
rates
losses
in
China.
We
find
that
mangrove,
salt
marsh
seagrass
relatively
low
storing
6.3
±
0.6,
7.5
1.6
0.6
Tg
C
(±95%
confidence
interval)
top
meter
profile
with
44
17,
159
57,
6
45
Gg
C/year,
respectively.
variability
is
linked
biogeographic
factors
but
mostly
impacted
by
sedimentary
processes
anthropic
activities.
All
experienced
significant
losses,
resulting
estimated
emissions
94.2–395.4
CO
2
e
(carbon
dioxide
equivalent)
over
past
70
years.
Reversing
this
trend
through
conservation
restoration
measures
has,
therefore,
great
potential
contributing
mitigation
climate
change
while
providing
additional
benefits.
This
assessment,
national
scale
highly
environments
under
intensive
anthropogenic
pressures,
provides
important
insights
into
blue
mechanism
sequestration
capacities,
thus
synchronous
progression
management.
Ecological Applications,
Год журнала:
2020,
Номер
30(4)
Опубликована: Янв. 29, 2020
Mangrove
forests
are
among
the
world's
most
productive
and
carbon-rich
ecosystems.
Despite
growing
understanding
of
factors
controlling
mangrove
forest
soil
carbon
stocks,
there
is
a
need
to
advance
speed
peat
development
beneath
maturing
forests,
especially
in
created
restored
that
intended
compensate
for
ecosystem
functions
lost
during
conversion
other
land
uses.
To
better
quantify
rate
organic
matter
created,
we
measured
changes
across
25-yr
chronosequence.
We
compared
properties
adjacent
natural
forests.
also
quantified
site-specific
occurred
between
2010
2016.
Soil
accumulated
rapidly
as
sandy
soils
transitioned
organic-rich
(peat).
Within
25
yr,
20-cm
deep
layer
developed.
The
time
required
reach
equivalency
with
was
estimated
(1)
<15
yr
herbaceous
juvenile
vegetation,
(2)
~55
adult
trees,
(3)
~25
upper
(0-10
cm),
(4)
~45-80
lower
(10-30
cm).
For
elevation
change,
were
equivalent
or
surpassed
within
first
5
yr.
A
comparison
chronosequence
studies
from
ecosystems
indicates
accumulation
may
be
fastest
globally.
In
peatland
ecosystems,
formation
occurs
slowly
(over
centuries,
millennia);
however,
these
results
show
can
occur
decades.
Peat
development,
primarily
due
subsurface
root
accumulation,
enables
sequester
carbon,
adjust
their
relative
sea
level,
adapt
changing
conditions
at
dynamic
land-ocean
interface.
face
climate
change
rising
levels,
coastal
managers
increasingly
concerned
longevity
functionality
restoration
efforts.
Our
pace
which
improve
predictions
responses
global
restoration.
Global Change Biology,
Год журнала:
2023,
Номер
29(23), С. 6517 - 6545
Опубликована: Сен. 25, 2023
Coastal
saltmarshes
are
found
globally,
yet
25%-50%
reduced
compared
with
their
historical
cover.
Restoration
is
incentivised
by
the
promise
that
marshes
efficient
storers
of
'blue'
carbon,
although
claim
lacks
substantiation
across
global
contexts.
We
synthesised
data
from
431
studies
to
quantify
benefits
saltmarsh
restoration
carbon
accumulation
and
greenhouse
gas
uptake.
The
results
showed
store
approximately
1.41-2.44
Pg
carbon.
Restored
had
very
low
(GHG)
fluxes
rapid
accumulation,
resulting
in
a
mean
net
rate
64.70
t
CO2
e
ha-1
year-1
.
Using
this
estimate
potential
rates,
we
find
regeneration
could
result
12.93-207.03
Mt
per
year,
offsetting
equivalent
up
0.51%
energy-related
emissions-a
substantial
amount,
considering
represent
<1%
Earth's
surface.
Carbon
rates
GHG
varied
contextually
temperature,
rainfall
dominant
vegetation,
eastern
coasts
USA
Australia
particular
hotspots
for
storage.
While
study
reveals
paucity
some
variables
continents,
suggesting
need
further
research,
offset
emissions
clear.
ability
facilitate
natural
now
rests
principally
on
action
management-policy
community
financial
opportunities
supporting
restoration.