Limnology and Oceanography Methods,
Journal Year:
2021,
Volume and Issue:
19(5), P. 317 - 330
Published: March 25, 2021
Abstract
Wave
flume
facilities
that
are
primarily
designed
for
engineering
studies
often
complex
and
expensive
to
operate,
hence
not
ideal
long‐term
replicated
experiments
as
commonly
used
in
biology.
This
study
describes
a
low‐cost
small
wave
can
be
biological
purposes
using
fresh‐
or
seawater
with
without
sediment.
The
mesocosm
interactions
between
hydrodynamics
benthic
organisms
aquatic
ecosystems.
low‐costs
maker
(<
2000
USD)
allows
experimental
setups
which
easily
longer
term
studies;
the
mesocosm.
Waves
were
generated
pneumatic
piston
heights
ranged
3
6
cm.
Maximum
orbital
flow
velocities
10
50
cm
s
−1
representing
shallow
coastal
areas
short
fetch.
system
generate
both
regular
waves
(i.e.,
period
velocity
remains
constant),
absorber,
irregular
varying
velocity)
fast
push
slow
pull
motion
of
paddle.
is
particularly
useful
biogeomorphology
quantify
organisms,
sediment,
ecologist
aiming
simulate
realistic
bed
shear
stress
where
short‐
(weeks–months)
replicated.
Scientific Reports,
Journal Year:
2020,
Volume and Issue:
10(1)
Published: April 3, 2020
Seagrass
meadows
are
considered
important
natural
carbon
sinks
due
to
their
capacity
store
organic
(Corg)
in
sediments.
However,
the
spatial
heterogeneity
of
storage
seagrass
sediments
needs
be
better
understood
improve
accuracy
Blue
Carbon
assessments,
particularly
when
strong
gradients
present.
We
performed
an
intensive
coring
study
within
a
sub-tropical
estuary
assess
variability
sedimentary
Corg
associated
with
seagrasses,
and
identify
key
factors
promoting
this
variability.
found
pattern
estuary,
from
52.16
mg
cm-3
upper
parts,
declining
1.06
at
mouth,
despite
general
gradient
increasing
cover
habitat
extent
opposite
direction.
The
underneath
came
principally
allochthonous
(non-seagrass)
sources
(~70-90
%),
while
contribution
seagrasses
was
low
(~10-30
%)
throughout
entire
estuary.
Our
results
showed
that
stored
can
highly
variable
attributed
largely
accumulation
fine
inputs
sources.
Local
features
existence
must
estimates
coastal
ecosystems.
Global Change Biology,
Journal Year:
2020,
Volume and Issue:
26(9), P. 4772 - 4784
Published: July 7, 2020
Abstract
Seagrass
meadows
store
globally
significant
organic
carbon
(C
org
)
stocks
which,
if
disturbed,
can
lead
to
CO
2
emissions,
contributing
climate
change.
Eutrophication
and
thermal
stress
continue
be
a
major
cause
of
seagrass
decline
worldwide,
but
the
associated
emissions
remain
poorly
understood.
This
study
presents
comprehensive
estimates
soil
C
erosion
following
eutrophication‐driven
loss
in
Cockburn
Sound
(23
km
between
1960s
1990s)
identifies
main
drivers.
We
estimate
that
shallow
(<5
m
depth)
had
significantly
higher
50
cm
thick
soils
(4.5
±
0.7
kg
/m
than
previously
vegetated
counterparts
(0.5
0.1
).
In
deeper
areas
(>5
m),
however,
bare
were
not
different
(2.6
0.3
3.0
0.6
,
respectively).
The
sequestration
capacity
prevailed
deep
(55
11
21
7
g
−2
year
−1
respectively),
was
lost
areas.
identified
canopy
alone
does
necessarily
drive
changes
but,
when
combined
with
high
hydrodynamic
energy,
occurred.
Our
point
at
~0.20
m/s
as
critical
shear
velocity
threshold
causing
erosion.
estimate,
from
field
studies
satellite
imagery,
(within
top
cm)
likely
resulted
cumulative
0.06–0.14
Tg
2‐eq
over
last
40
years
Sound.
estimated
indirect
impacts
(i.e.
eutrophication,
light
stress)
~161,150
ha
seagrasses
Australia,
release
11–21
‐eq
since
1950s,
increasing
land‐use
change
Australia
by
1.1%–2.3%
per
annum.
patterns
described
serve
baseline
potential
disturbance
meadows.
Global Biogeochemical Cycles,
Journal Year:
2020,
Volume and Issue:
34(2)
Published: Jan. 6, 2020
Abstract
There
is
increasing
urgency
to
implement
climate
change
mitigation
strategies
that
enhance
greenhouse
gas
removal
from
the
atmosphere
and
reduce
carbon
dioxide
(CO
2
)
emissions.
Recently,
coastal
“blue
carbon”
habitats—mangroves,
salt
marshes,
seagrass
meadows—have
received
attention
for
their
ability
capture
CO
store
organic
(OC),
primarily
in
sediments.
Across
habitat
types
regions,
however,
information
about
sequestration
rates
sources
of
local
sediments
remains
sparse.
Here
we
compiled
recently
obtained
estimates
sediment
OC
stocks
139
cores
collected
temperate
(
Zostera
marina
meadows
Alaska,
British
Columbia,
Washington,
Oregon.
all
content
averaged
0.75%.
Organic
top
25
cm
1
m
1,846
7,168
g
−2
,
respectively.
Carbon
ranged
4.6
93.0
yr
−1
24.8
.
Isotopic
data
this
region
suggest
largely
noneelgrass
sources.
In
general,
these
values
are
comparable
those
other
Z.
meadows,
but
significantly
lower
than
previously
reported
seagrasses
globally.
These
results
further
highlight
need
species‐level
quantification
blue
parameters.
While
eelgrass
may
not
sequester
as
much
elsewhere,
policy
incentives
should
still
be
implemented
protect
existing
critical
ecosystem
services
associated
with
habitats.
Ecosphere,
Journal Year:
2021,
Volume and Issue:
12(7)
Published: July 1, 2021
Abstract
Seagrass
meadows
constitute
important
carbon
sinks,
and
the
ongoing
global
loss
of
seagrass
habitats
raises
concerns
about
release
stored
in
their
sediments.
However,
actual
consequences
for
nutrients
remain
unclear.
Here,
we
take
advantage
well‐documented
historic
losses
eelgrass
(
Zostera
marina
)
along
Swedish
NW
coast
to
assess
how
contents
organic
(C)
nitrogen
(N)
sediment
change
when
a
meadow
is
lost.
We
find
unusually
high
C
N
(on
average
3.7%
0.39%
DW,
respectively)
sediments
down
>100
cm
depth,
suggesting
that
these
hot
spots
storage.
stocks
were
strongly
influenced
by
wave
exposure
almost
twice
as
sheltered
compared
exposed
meadows.
The
composition
stable
isotope
values
distinctly
different
areas
have
lost
meadows,
with
on
>2.6
times
lower
N.
results
indicate
an
erosion
>35
following
historical
loss,
more
vulnerable
stocks.
suggest
has
resulted
60.2
Mg
6.63
per
hectare,
estimated
economic
cost
society
7944
141,355
US$/ha,
respectively.
value
storage
represents
one
highest
monetary
presented
ecosystem
service
provided
seagrasses
shows
are
particularly
mitigating
eutrophication.
Following
documented
approximately
10
km
2
study
area,
it
over
60,000
was
released
coastal
environment
20‐yr
period,
which
constitutes
three
annual
river
load
coast.
exemplifies
significant
role
sinks
both
nutrients,
risk
nutrient
vegetation
should
be
taken
into
account
spatial
management
other
habitats.
The Science of The Total Environment,
Journal Year:
2023,
Volume and Issue:
901, P. 165976 - 165976
Published: Aug. 1, 2023
Coastal
development
and
climate
change
are
sparking
growing
concern
about
the
vulnerability
of
organic
carbon
(OC)
stocks
in
marine
sediments
to
remineralization,
especially
high
threaten
coastal
ecosystems
like
seagrass
meadows.
Uncertainties
still
exist
regarding
role
played
by
hydrodynamics,
canopies
sediment
properties
OC
resuspension
remineralization.
A
set
laboratory
experiments
were
conducted
assess,
for
first
time,
mechanisms
which
particulate
dissolved
(POC
DOC)
may
be
released
remineralized
under
hydrodynamic
conditions
(i.e.,
unidirectional
oscillatory
flows)
two
eelgrass
densities
grain
size
content).
After
a
gradually
increase
forces,
our
results
demonstrated
that
presence
reduced
erosion
loss
high-density
canopies,
while
low-density
promote
(on
average,
1.8-fold
higher
than
canopies).
We
also
flows
similar
DOC
from
surface
15.5
±
1.4
18.4
1.8
g
m-2,
respectively),
whereas
flow
significantly
more
POC
(from
10.8
1.1
32.1
5.6
m-2
flows,
respectively).
was
strongly
influenced
both
meadow
structure
lower
density
shoot
area)
mud
water
found
that,
although
>74
%
upper
within
30
days,
relatively
amount
is
recalcitrant,
highlighting
its
potential
formation
blue
deposits.
This
study
highlights
deposits
if
degraded
and/or
yield
stronger
storms,
could
potentially
weaken
meadows'
service
as
ecosystem
future.
Landscape Ecology,
Journal Year:
2021,
Volume and Issue:
36(5), P. 1489 - 1509
Published: March 1, 2021
Abstract
Context
Seagrass
meadows
act
as
efficient
natural
carbon
sinks
by
sequestering
atmospheric
CO
2
and
through
trapping
of
allochthonous
organic
material,
thereby
preserving
(C
org
)
in
their
sediments.
Less
understood
is
the
influence
landscape
configuration
transformation
(land-use
change)
on
sequestration
dynamics
coastal
seascapes
across
land–sea
interface.
Objectives
We
explored
degradation
adjacent
mangroves
fate
C
seagrass
habitats.
Methods
Through
predictive
modelling,
we
assessed
sedimentary
content,
stocks
source
composition
multiple
(km-wide
buffer
zones)
dominated
different
communities
northwest
Madagascar.
The
study
area
encompassed
to
intact
deforested
mangroves.
Results
content
was
influenced
a
combination
metrics
inherent
habitat
plant-
sediment-properties.
found
strong
land-to-sea
gradient,
likely
driven
hydrodynamic
forces,
generating
distinct
patterns
levels
seascapes.
There
higher
mangrove
signal
surface
sediments
closer
area,
possibly
due
an
escalated
export
from
soils.
Seascapes
comprising
large
continuous
had
comparison
more
diverse
patchy
Conclusion
Our
results
emphasize
benefit
consider
seascape
connectivity
accurately
assess
Understanding
spatial
variability
what
driving
observed
useful
for
identifying
sink
hotspots
develop
management
prioritizations.
PLOS Climate,
Journal Year:
2023,
Volume and Issue:
2(1), P. e0000099 - e0000099
Published: Jan. 5, 2023
Seagrass
meadows
are
globally
important
blue
carbon
sinks.
In
northern
cold-temperate
regions,
eelgrass
(
Zostera
marina
)
is
the
dominant
seagrass
species,
and
although
their
sedimentary
stocks
have
been
quantified
across
information
regarding
CO
2
withdrawal
capacity
as
sinks
remains
scarce.
Here
we
assessed
(C
org
accumulation
rates
(CARs)
well
organic
matter
sources
in
five
Gullmar
Fjord
area
on
Swedish
Skagerrak
coast.
We
found
that
mean
(±SD)
CAR
was
14
±
3
g
C
m
-2
yr
-1
over
last
~120–140
years
(corresponding
to
a
yearly
uptake
of
52.4
12.6
CO2
).
The
sink
line
with
other
Z
.
areas
but
relatively
low
compared
species
regions
globally.
About
half
(7.1
3.3
originated
from
macroalgae
biomass,
which
highlights
importance
non-seagrass
derived
material
for
function
area.
were
similar
among
sites
when
comparing
at
standardized
depth
50
cm
(4.6–5.9
kg
),
showed
large
variation
total
extent
cores
(ranging
0.7
20.6
sediment
depths
11
least
149
cm).
accretion
(1.18–1.86
mm
thick
deposits
(with
maximum
>150
depth)
suggests
likely
accumulated
an
extended
period
time,
documented
loss
region
associated
erosion
could
potentially
offset
centuries
sequestration.