Abstract.
Approximately
one
quarter
of
the
CO2
emitted
to
atmosphere
annually
from
human
activities
is
absorbed
by
ocean,
resulting
in
a
reduction
seawater
pH
and
shifts
carbonate
chemistry.
This
multi-decadal
process,
termed
“anthropogenic
ocean
acidification”
(OA)
has
been
shown
have
detrimental
impacts
on
marine
ecosystems.
Recent
years
seen
globally
coordinated
effort
measure
changes
chemistry
caused
OA,
with
best
practices
now
available
for
these
measurements.
In
contrast
substantial
advances
observing
physico-chemical
due
quantifying
their
biological
consequences
remains
challenging,
especially
in-situ
observations
under
real-world
conditions.
Results
two
decades
controlled
laboratory
experiments
OA
given
insight
into
likely
processes
mechanisms
which
elevated
levels
affect
but
manifestation
process
across
plethora
natural
situations
yet
be
explored
fully.
challenge
requires
us
identify
set
fundamental
ecological
indicators
that
are
i)
relevant
all
ecosystems,
ii)
strongly
demonstrated
link
iii)
implications
health
provision
ecosystem
services
local
management
strategies
economies.
paper
draws
understanding
provided
wealth
previous
experiments,
as
well
findings
recent
meta-analyses,
propose
five
broad
classes
that,
when
coupled
environmental
observations,
including
chemistry,
would
allow
rate
severity
change
response
observed
compared.
These
applicable
different
systems,
methods
data
analysis
suggested
here
researchers
combine
regional
global
scales
correlating
rates
parameters.
Moreover,
method
using
observation
design
an
optimal
strategy
(frequency
duration)
observe
meaningful
highlights
factors
need
considered
applying
our
proposed
strategy.
innovative
methodology
allows
inclusion
wide
diversity
ecosystems
assessments
potential
increase
contribution
countries
developing
science
capacity.
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: March 13, 2023
In
the
context
of
an
increasing
atmospheric
carbon
dioxide
(CO2)
level,
acidification
estuarine
and
coastal
waters
is
greatly
exacerbated
by
land-derived
nutrient
inputs,
upwelling,
complex
biogeochemical
processes.
A
deeper
understanding
how
nitrifiers
respond
to
intensifying
thus
crucial
predict
response
ecosystems
their
contribution
global
climate
change.
Here,
we
show
that
can
significantly
decrease
nitrification
rate
but
stimulate
generation
byproduct
nitrous
oxide
(N2O)
in
waters.
By
varying
CO2
concentration
pH
independently,
expected
beneficial
effect
elevated
on
activity
("CO2-fertilization"
effect)
excluded
under
acidification.
Metatranscriptome
data
further
demonstrate
could
up-regulate
gene
expressions
associated
with
intracellular
homeostasis
cope
stress.
This
study
highlights
molecular
underpinnings
effects
greenhouse
gas
N2O
emission,
helps
evolution
change
human
activities.
Annual Review of Marine Science,
Journal Year:
2020,
Volume and Issue:
13(1), P. 23 - 55
Published: Sept. 21, 2020
Oceanic
uptake
of
anthropogenic
carbon
dioxide
(CO2)
from
the
atmosphere
has
changed
ocean
biogeochemistry
and
threatened
health
organisms
through
a
process
known
as
acidification
(OA).
Such
large-scale
changes
affect
ecosystem
functions
can
have
impacts
on
societal
uses,
fisheries
resources,
economies.
In
many
large
estuaries,
CO2-induced
is
enhanced
by
strong
stratification,
long
water
residence
times,
eutrophication,
weak
acid-base
buffer
capacity.
this
article,
we
review
how
variety
processes
influence
aquatic
properties
in
estuarine
waters,
including
coastal
upwelling,
river-ocean
mixing,
air-water
gas
exchange,
biological
production
subsequent
aerobic
anaerobic
respiration,
calcium
carbonate
(CaCO3)
dissolution,
benthic
inputs.
We
emphasize
spatial
temporal
dynamics
partial
pressure
CO2
(pCO2),
pH,
mineral
saturation
states.
Examples
three
estuaries-Chesapeake
Bay,
Salish
Sea,
Prince
William
Sound-are
used
to
illustrate
natural
climate
change
may
manifest
differently
across
well
implications
OA
calcifiers.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(12), P. 9015 - 9028
Published: May 12, 2022
Coastal-estuarine
habitats
are
rapidly
changing
due
to
global
climate
change,
with
impacts
influenced
by
the
variability
of
carbonate
chemistry
conditions.
However,
our
understanding
responses
ecologically
and
economically
important
calcifiers
pH
temporal
variation
is
limited,
particularly
respect
shell-building
processes.
We
investigated
mechanisms
driving
biomineralogical
physiological
in
juveniles
introduced
(Pacific;
Crassostrea
gigas)
native
(Olympia;
Ostrea
lurida)
oysters
under
flow-through
experimental
conditions
over
a
six-week
period
that
simulate
current
future
conditions:
static
control
low
(8.0
7.7);
fluctuating
(24-h)
amplitude
(7.7
±
0.2
7.7
0.5);
high-frequency
(12-h)
0.2)
treatment.
The
showed
tolerance
vital
processes,
including
calcification,
respiration,
clearance,
survival.
shell
dissolution
significantly
increased
larger
amplitudes
compared
conditions,
attributable
longer
cumulative
exposure
lower
threshold
amplitude.
Moreover,
treatment
triggered
greater
dissolution,
likely
because
oyster's
inability
respond
unpredictable
frequency
variations.
findings
were
extrapolated
provide
context
for
existing
several
Pacific
coastal
estuaries,
time
series
analyses
demonstrating
unique
signatures
predictability
these
habitats,
indicating
potentially
benefiting
effects
on
fitness
habitats.
These
implications
crucial
evaluating
suitability
aquaculture,
adaptation,
carbon
dioxide
removal
strategies.
Earth system science data,
Journal Year:
2024,
Volume and Issue:
16(2), P. 837 - 865
Published: Feb. 8, 2024
Abstract.
Coastal
and
estuarine
waters
of
the
northern
California
Current
system
southern
Salish
Sea
host
an
observational
network
capable
characterizing
biogeochemical
dynamics
related
to
ocean
acidification,
hypoxia,
marine
heatwaves.
Here,
we
compiled
data
sets
from
a
set
cruises
conducted
in
Puget
Sound
(southern
Sea)
its
boundary
(Strait
Juan
de
Fuca
Washington
coast).
This
product
provides
decade
with
consistent
formatting,
extended
quality
control,
multiple
units
for
parameters
such
as
oxygen
different
end
use
needs
conventions.
All
obtained
high-quality
temperature,
salinity,
inorganic
carbon,
nutrient,
observations
provide
insight
into
dynamic
distribution
physical
conditions
this
large
urban
estuary
complex
on
west
coast
North
America.
At
all
sampling
stations,
conductivity–temperature–depth
(CTD)
casts
included
sensors
measuring
conductivity,
pressure,
concentrations.
Laboratory
analyses
discrete
water
samples
collected
at
stations
throughout
column
Niskin
bottles
provided
measurements
dissolved
carbon
(DIC),
oxygen,
nutrient
(nitrate,
nitrite,
ammonium,
phosphate,
silicate),
total
alkalinity
(TA)
content.
includes
35
research
cruises,
including
715
oceanographic
profiles,
>7490
sensor
oxygen;
≥6070
samples;
≥4462
variables
(i.e.,
DIC
TA).
The
comprising
cruise
compilation
collectively
characterize
spatial
temporal
variability
region
ranges
(temperature
=
6.0–21.8
∘C,
salinity
15.6–34.0)
(oxygen
12–481
µmol
kg−1,
1074–2362
1274–2296
kg−1)
central
understanding
acidification
hypoxia
productive
numerous
interacting
human
impacts
ecosystems.
conform
climate-quality
observing
guidelines
Global
Ocean
Acidification
Observing
Network,
US
National
Oceanic
Atmospheric
Administration's
Program,
community
best
practices.
ongoing
time
series
supports
coastal
monitoring
objectives
Center
Administration
(NOAA)
Research
programs,
it
diverse
users
information
needed
frame
biological
research,
validate
numerical
models,
inform
state
tribal
fisheries
management,
support
decision-makers.
2008–2018
time-series
used
publication
are
available
https://doi.org/10.25921/zgk5-ep63
(Alin
et
al.,
2022).
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(7), P. 1639 - 1673
Published: April 4, 2024
Abstract.
Coastal
and
estuarine
ecosystems
fringing
the
North
Pacific
Ocean
are
particularly
vulnerable
to
ocean
acidification,
hypoxia,
intense
marine
heatwaves
as
a
result
of
interactions
among
natural
anthropogenic
processes.
Here,
we
characterize
variability
during
seasonally
resolved
cruise
time
series
(2014–2018)
in
southern
Salish
Sea
(Puget
Sound,
Strait
Juan
de
Fuca)
nearby
coastal
waters
for
select
physical
(temperature,
T;
salinity,
S)
biogeochemical
(oxygen,
O2;
carbon
dioxide
fugacity,
fCO2;
aragonite
saturation
state,
Ωarag)
parameters.
Medians
some
parameters
peaked
(T,
surface
summer,
whereas
others
(S,
O2,
fCO2)
changed
progressively
across
spring–fall,
all
monotonically
or
were
relatively
stable
at
depth.
Ranges
varied
considerably
basins
within
study
region,
with
stratified
consistently
most
variable.
Strong
environmental
anomalies
occurred
series,
allowing
us
also
qualitatively
assess
how
these
affected
seasonal
patterns
interannual
variability.
The
peak
temperature
anomaly
associated
2013–2016
northeast
heatwave–El
Niño
event
was
observed
boundary
October
2014
cruise,
but
Puget
Sound
cruises
revealed
largest
increases
2015–2016
timeframe.
extreme
hypoxia
acidification
measurements
date
recorded
Hood
Canal
(which
had
conditions)
same
period;
however,
they
shifted
earlier
year
relative
previous
events.
During
autumn
2017,
after
heat
anomaly,
distinct
carbonate
system
unprecedentedly
low
Ωarag
values
high
fCO2
parts
that
not
normally
so
acidified.
This
novel
“CO2
storm”
appears
have
been
driven
by
anomalously
river
discharge
which
resulted
enhanced
stratification
inferred
primary
productivity
anomalies,
indicated
persistently
fCO2,
chlorophyll.
Unusually,
this
CO2
decoupled
from
O2
dynamics
compared
past
complex
interplay
weather,
hydrological,
circulation
multi-stressor
scenarios
will
potentially
affect
regional
under
changing
climate.
Further,
frequencies
observations
crossed
known
preliminary
species'
sensitivity
thresholds
illustrates
risk
landscape
temperature,
present
day,
implications
multiple
stressors
may
combine
potential
migration,
survival,
physiological
challenges
key
species.
data
product
used
publication
is
available
https://doi.org/10.25921/zgk5-ep63
(Alin
et
al.,
2022),
an
additional
including
calculated
https://doi.org/10.25921/5g29-q841
2023).
Scientific Reports,
Journal Year:
2025,
Volume and Issue:
15(1)
Published: Feb. 6, 2025
Large
changes
in
marine
CO2
chemistry
manifest
areas
with
weakly-buffered
seawater
where
ocean
acidification
(OA)
acts
concert
natural
additions.
These
settings
can
exhibit
periods
of
extreme
OA
the
form
multiple
co-occurring
stressors,
including
calcite
undersaturation
and
low
pH.
Such
conditions
were
observed
northern
Strait
Georgia,
on
northeast
Pacific
coast,
spanned
a
3-year
period.
Here,
we
utilized
an
8-year,
highly-resolved
record
partial
pressure
total
dissolved
inorganic
carbon
to
decompose
drivers
this
OA.
We
find
that
variability
storm
season
intensity
shaped
extent
conservative
mixing
biogeochemical
such
manifests
arise
setting.
Extreme
manifested
during
years
weak
seasons
due
direct
indirect
factors
reduced
impact
mixing.
This
sensitivity
highlights
how
vulnerable
Georgia
is
subtle
environmental
forcing
provides
some
predictive
capacity
for
over
coming
year.
results
illustrate
not
"slow
burn"
process
within
settings,
but
rather
invokes
intensification
poorly
understood
biological
implications.
Biogeosciences,
Journal Year:
2022,
Volume and Issue:
19(4), P. 1277 - 1301
Published: March 3, 2022
Abstract.
Information
on
marine
CO2
system
variability
has
been
limited
along
the
northeast
Pacific
Inside
Passage
despite
region's
rich
biodiversity,
abundant
fisheries,
and
developing
aquaculture
industry.
Beginning
in
2017,
Alaska
Marine
Highway
System
M/V
Columbia
served
as
a
platform
for
surface
underway
data
collection
while
conducting
twice
weekly
∼1600
km
transits
between
Bellingham,
Washington,
Skagway,
Alaska.
patterns
were
evaluated
using
measurements
made
over
2-year
period,
which
revealed
seasonal
cycle
dominant
mode
of
temporal
variability.
The
amplitude
this
signal
varied
spatially
was
modulated
by
relative
influences
tidal
mixing,
net
community
production,
magnitude
character
freshwater
input.
Surface
water
pHT
(total
hydrogen
ion
scale)
aragonite
saturation
state
(Ωarag)
determined
carbon
dioxide
partial
pressure
(pCO2)
with
alkalinity
derived
from
regional
salinity-based
relationship,
intervals
discrete
seawater
samples
pH
measurements.
High-pCO2,
low-pHT,
corrosive
Ωarag
conditions
(Ωarag<1)
seen
during
winter
within
persistent
mixing
zones,
values
also
areas
that
receive
significant
glacial
melt
summer.
Biophysical
drivers
are
shown
to
dominate
pCO2
most
except
highly
impacted
melt.
extremes
characterized
based
degrees
severity,
differences
evident.
Computations
time
detection
identified
zones
strategic
observing
sites
relatively
short
spans
required
capture
secular
trends
equivalent
contemporary
rise
atmospheric
CO2.
Finally,
estimates
anthropogenic
showed
notable
spatiotemporal
Changes
total
content
([H+]T),
pHT,
industrial
era
an
level
consistent
1.5
∘C
warmer
climate
theoretically
evaluated.
These
calculations
greater
absolute
changes
[H+]T
opposed
larger
change
acidification
everywhere
exceeded
global
average,
specific
areas,
namely
Johnstone
Strait
Salish
Sea,
standing
out
potential
bellwethers
emergence
biological
ocean
(OA)
impacts.
Nearly
half
is
expected
coming
15
years,
trajectory
continues
be
shaped
fossil–fuel
development.
Ocean science,
Journal Year:
2023,
Volume and Issue:
19(1), P. 101 - 119
Published: Jan. 25, 2023
Abstract.
Approximately
one-quarter
of
the
CO2
emitted
to
atmosphere
annually
from
human
activities
is
absorbed
by
ocean,
resulting
in
a
reduction
seawater
pH
and
shifts
carbonate
chemistry.
This
multi-decadal
process,
termed
“anthropogenic
ocean
acidification”
(OA),
has
been
shown
have
detrimental
impacts
on
marine
ecosystems.
Recent
years
seen
globally
coordinated
effort
measure
changes
chemistry
caused
OA,
with
best
practices
now
available
for
these
measurements.
In
contrast
substantial
advances
observing
physicochemical
due
quantifying
their
biological
consequences
remains
challenging,
especially
situ
observations
under
real-world
conditions.
Results
2
decades
controlled
laboratory
experiments
OA
given
insight
into
likely
processes
mechanisms
which
elevated
levels
affect
but
manifestation
process
across
plethora
natural
situations
yet
be
fully
explored.
challenge
requires
us
identify
set
fundamental
ecological
indicators
that
are
(i)
relevant
all
ecosystems,
(ii)
strongly
demonstrated
link
(iii)
implications
health
provision
ecosystem
services
local
management
strategies
economies.
paper
draws
understanding
provided
wealth
previous
experiments,
as
well
findings
recent
meta-analyses,
propose
five
broad
classes
that,
when
coupled
environmental
including
chemistry,
would
allow
rate
severity
change
response
observed
compared.
These
applicable
different
systems,
methods
data
analysis
suggested
here
researchers
combine
regional
global
scales
correlating
rates
parameters.
Moreover,
method
using
observation
design
an
optimal
strategy
(frequency
duration)
observe
meaningful
highlights
factors
need
considered
applying
our
proposed
strategy.
innovative
methodology
allows
inclusion
wide
diversity
ecosystems
assessments
potential
increase
contribution
countries
developing
science
capacity.
ICES Journal of Marine Science,
Journal Year:
2023,
Volume and Issue:
80(5), P. 1329 - 1341
Published: May 12, 2023
Abstract
The
pteropod
Limacina
helicina
has
become
an
important
bioindicator
species
for
the
negative
impacts
of
ocean
acidification
(OA)
on
marine
ecosystems.
However,
pteropods
diversified
during
earlier
high
CO2
periods
in
Earth
history
and
currently
inhabit
regions
that
are
naturally
corrosive
to
their
shells,
suggesting
they
possess
mechanisms
survive
unfavourable
conditions.
Recent
work,
which
is
still
under
considerable
debate,
proposed
periostracum,
a
thin
organic
coating
outer
shell,
protects
from
shell
dissolution.
Here,
we
provide
direct
evidence
shows
damage
L.
periostracum
results
dissolution
underlying
when
exposed
water
∼8
d,
while
intact
same
This
first
line
defence
suggests
more
resistant
OA-induced
than
generally
accepted.