Frontiers in Marine Science,
Journal Year:
2021,
Volume and Issue:
8
Published: Jan. 29, 2021
Understanding
the
vulnerability
of
marine
calcifiers
to
ocean
acidification
is
a
critical
issue,
especially
in
Southern
Ocean
(SO),
which
likely
be
one
first,
and
most
severely
affected
regions.
Since
industrial
revolution,
~30%
anthropogenic
CO
2
has
been
absorbed
by
global
oceans.
Average
surface
seawater
pH
levels
have
already
decreased
0.1
are
projected
decline
~0.3
year
2100.
This
process,
known
as
(OA),
shallowing
saturation
horizon,
depth
below
calcium
carbonate
(CaCO
3
)
dissolves,
increasing
many
resident
dissolution.
The
negative
impact
OA
may
seen
first
species
depositing
more
soluble
CaCO
mineral
phases
such
aragonite
high-Mg
calcite
(HMC).
warming
could
further
exacerbate
effects
these
particular
species.
Here
we
combine
review
quantitative
meta-analysis
provide
an
overview
current
state
knowledge
about
skeletal
mineralogy
major
taxonomic
groups
SO
make
projections
how
might
affect
broad
range
taxa.
We
consider
species'
geographic
range,
mineralogy,
biological
traits,
potential
strategies
overcome
OA.
studies
investigating
on
responses
shell
state,
development
growth
rate
illustrates
that
response
variation
largely
dependent
mineralogical
composition.
Species-specific
due
composition
indicate
taxa
with
calcitic,
aragonitic,
HMC
skeletons,
at
greater
risk
expected
future
chemistry
alterations,
low-Mg
(LMC)
mostly
resilient
changes.
Environmental
control
calcification
process
and/or
Mg
content
calcite,
physiological
processes
also
influence
species-specific
responses.
Ecology and Evolution,
Journal Year:
2020,
Volume and Issue:
10(10), P. 4495 - 4514
Published: April 16, 2020
Southern
Ocean
waters
are
among
the
most
vulnerable
to
ocean
acidification.
The
projected
increase
in
CO2
level
will
cause
changes
carbonate
chemistry
that
likely
be
damaging
organisms
inhabiting
these
waters.
A
meta-analysis
was
undertaken
examine
vulnerability
of
Antarctic
marine
biota
occupying
south
60°S
This
showed
acidification
negatively
affects
autotrophic
organisms,
mainly
phytoplankton,
at
levels
above
1,000
μatm
and
invertebrates
1,500
μatm,
but
positively
bacterial
abundance.
sensitivity
phytoplankton
influenced
by
experimental
procedure
used.
Natural,
mixed
communities
were
more
sensitive
than
single
species
culture
a
decline
chlorophyll
concentration,
productivity,
photosynthetic
health,
as
well
shift
community
composition
μatm.
Invertebrates
reduced
fertilization
rates
increased
occurrence
larval
abnormalities,
decreased
calcification
shell
dissolution
with
any
Assessment
fish
macroalgae
limited
number
studies
available.
Overall,
this
analysis
indicates
many
susceptible
thereby
change
their
contribution
ecosystem
services
future.
Further
required
address
poor
spatial
coverage,
lack
or
ecosystem-level
studies,
largely
unknown
potential
for
acclimate
and/or
adapt
changing
conditions.
Environmental Science Advances,
Journal Year:
2024,
Volume and Issue:
3(4), P. 543 - 560
Published: Jan. 1, 2024
The
review
presents
a
complete
update
of
previous
reviews
on
the
topics
environmental
contamination,
climate
change
and
human
impact
Antarctic
ecosystems.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: April 3, 2024
Conflicting
results
remain
on
the
impacts
of
climate
change
marine
organisms,
hindering
our
capacity
to
predict
future
state
ecosystems.
To
account
for
species-specific
responses
and
ambiguous
relation
most
metrics
fitness,
we
develop
a
meta-analytical
approach
based
deviation
from
reference
values
(absolute
change)
complement
meta-analyses
directional
(relative)
changes
in
responses.
Using
this
approach,
evaluate
fish
invertebrates
warming
acidification.
We
find
that
drivers
induce
calcification,
survival,
metabolism,
significant
deviations
twice
as
many
biological
responses,
including
physiology,
reproduction,
behavior,
development.
Widespread
are
detected
even
under
moderate
intensity
levels
acidification,
while
mostly
limited
more
severe
levels.
Because
such
may
result
ecological
shifts
impacting
ecosystem
structures
processes,
suggest
will
likely
have
stronger
than
those
previously
predicted
alone.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: Jan. 4, 2024
Antarctic
coastal
waters
are
home
to
several
established
or
proposed
Marine
Protected
Areas
(MPAs)
supporting
exceptional
biodiversity.
Despite
being
threatened
by
anthropogenic
climate
change,
uncertainties
remain
surrounding
the
future
ocean
acidification
(OA)
of
these
waters.
Here
we
present
21st-century
projections
OA
in
MPAs
under
four
emission
scenarios
using
a
high-resolution
ocean-sea
ice-biogeochemistry
model
with
realistic
ice-shelf
geometry.
By
2100,
project
pH
declines
up
0.36
(total
scale)
for
top
200
m.
Vigorous
vertical
mixing
carbon
produces
severe
throughout
water
column
and
existing
MPAs.
Consequently,
end-of-century
aragonite
undersaturation
is
ubiquitous
three
highest
scenarios.
Given
cumulative
threat
marine
ecosystems
environmental
change
activities
such
as
fishing,
our
findings
call
strong
emission-mitigation
efforts
further
management
strategies
reduce
pressures
on
ecosystems,
continuation
expansion
Global Change Biology,
Journal Year:
2020,
Volume and Issue:
26(12), P. 6787 - 6804
Published: Sept. 28, 2020
Abstract
Responses
of
marine
primary
production
to
a
changing
climate
are
determined
by
concert
multiple
environmental
changes,
for
example
in
temperature,
light,
p
CO
2
,
nutrients,
and
grazing.
To
make
robust
projections
future
global
production,
it
is
crucial
understand
driver
effects
on
phytoplankton.
This
meta‐analysis
quantifies
individual
interactive
dual
combinations
phytoplankton
growth
rates.
Almost
50%
the
single‐species
laboratory
studies
were
excluded
because
central
data
metadata
(growth
rates,
carbonate
system,
experimental
treatments)
insufficiently
reported.
The
remaining
(42
studies)
allowed
analysis
interactions
with
respectively.
Growth
rates
mostly
respond
non‐additively,
whereby
interaction
increased
profusely
dampens
growth‐enhancing
high
temperature
light.
Multiple
single
coccolithophores
differ
from
other
groups,
especially
their
sensitivity
increasing
.
Polar
species
decrease
rate
response
while
temperate
tropical
benefit
under
these
conditions.
Based
observed
projected
we
anticipate
productivity
to:
(a)
first
increase
but
eventually
Arctic
Ocean
once
nutrient
limitation
outweighs
benefits
higher
light
availability;
(b)
tropics
mid‐latitudes
due
intensifying
limitation,
possibly
amplified
elevated
;
(c)
Southern
view
availability
synergistic
Growth‐enhancing
effect
warming
coccolithophores,
mainly
Emiliania
huxleyi
might
relative
abundance
as
long
not
offset
acidification.
Dinoflagellates
expected
positive
levels.
Our
reveals
gaps
knowledge
responses
provides
recommendations
work
New Phytologist,
Journal Year:
2022,
Volume and Issue:
233(4), P. 1813 - 1827
Published: Jan. 5, 2022
Summary
Primary
production
in
the
Southern
Ocean
is
dominated
by
diatom‐rich
phytoplankton
assemblages,
whose
individual
physiological
characteristics
and
community
composition
are
strongly
shaped
environment,
yet
knowledge
on
how
diatoms
allocate
cellular
energy
response
to
ocean
acidification
(OA)
limited.
Understanding
such
changes
allocation
integral
determining
nutritional
quality
of
subsequent
impacts
trophic
transfer
nutrients.
Using
synchrotron‐based
Fourier
transform
infrared
microspectroscopy,
we
analysed
macromolecular
content
selected
diatom
taxa
from
a
natural
Antarctic
exposed
gradient
f
CO
2
levels
(288–1263
µatm).
Strong
species‐specific
differences
partitioning
were
observed
under
OA.
Large
showed
preferential
towards
proteins,
while
smaller
increased
both
lipid
protein
stores
at
high
.
If
these
representative
future
physiology,
may
expect
shift
away
lipid‐rich
large
taxa,
but
with
higher
than
their
present‐day
contemporaries,
that
could
have
cascading
effects
food
web
dynamics
marine
ecosystem.
Chemical Engineering Journal,
Journal Year:
2024,
Volume and Issue:
497, P. 154421 - 154421
Published: July 31, 2024
As
the
atmospheric
concentration
of
CO2
steadily
increases
and
world
grapples
with
pressing
challenges
global
warming,
international
research
communities
are
actively
exploring
inventive
technologies
to
combat
adverse
effects
elevated
levels.
An
important
challenge
in
this
context
is
extract
directly
from
atmosphere.
Consequently,
capturing
last
seawater
crucial
due
its
impact
on
delicate
balance
marine
ecosystems
potential
consequences
for
climate
regulation.
While
DAC
DOC
show
towards
combating
change,
including
high
operational
costs
need
further
technological
advancements
persist.
This
paper
critically
discusses
status,
challenges,
scalability
at
pilot
or
industrial
scale.
Key
include
capital
costs,
energy
demands,
integrating
green
sources
reduce
environmental
impact.
The
review
emphasizes
techno-economical
benchmarking
analyses
evaluate
feasibility
large-scale
deployment
their
effectiveness
mitigating
emissions
acting
as
tools
delocalized
production.
Frontiers in Marine Science,
Journal Year:
2021,
Volume and Issue:
8
Published: May 13, 2021
Knowledge
of
life
on
the
Southern
Ocean
seafloor
has
substantially
grown
since
beginning
this
century
with
increasing
ship-based
surveys
and
regular
monitoring
sites,
new
technologies
greatly
enhanced
data
sharing.
However,
habitats
their
communities
exhibit
high
spatial
variability
heterogeneity
that
challenges
way
in
which
we
assess
state
benthos
larger
scales.
The
Antarctic
shelf
is
rich
diversity
compared
deeper
water
areas,
important
for
storing
carbon
(“blue
carbon”)
provides
habitat
commercial
fish
species.
In
paper,
focus
shelf,
are
vulnerable
to
drivers
change
including
ocean
temperatures,
iceberg
scour,
sea
ice
melt,
acidification,
fishing
pressures,
pollution
non-indigenous
Some
most
areas
include
West
Peninsula,
experiencing
rapid
regional
warming
increased
iceberg-scouring,
subantarctic
islands
tourist
destinations
where
human
activities
environmental
conditions
increase
potential
establishment
species
active
around
South
Georgia,
Heard
MacDonald
Islands.
Vulnerable
those
low
thermal
tolerance,
calcifying
susceptible
acidity
as
well
slow-growing
habitat-forming
can
be
damaged
by
gears
e.g.,
sponges,
bryozoan,
coral
Management
regimes
protect
key
from
activities;
some
will
need
more
protection
than
others,
accounting
specific
traits
make
vulnerable,
slow
growing
long-lived
species,
restricted
locations
optimum
physiological
available
food,
distributions
rare
Ecosystem-based
management
practices
long-term,
highly
protected
may
effective
tools
preservation
habitats.
Here,
outlining
responses
observed
date
projections
future.
We
discuss
action
preserve
under
climate
change,
pressures
other
anthropogenic
impacts.