Oceanography,
Journal Year:
2023,
Volume and Issue:
unknown
Published: Jan. 1, 2023
The
Pacific
Marine
Environmental
Laboratory
(PMEL)
conducts
global
and
regional
oceanographic
research
in
support
of
the
National
Oceanic
Atmospheric
Administration’s
(NOAA’s)
three
mission
areas:
(1)
understanding
predicting
changes
climate,
weather,
oceans,
coasts;
(2)
sharing
that
knowledge
with
others;
(3)
conserving
managing
coastal
marine
ecosystems
resources.
Since
its
establishment
1973,
PMEL’s
work
has
ranged
from
pole
to
across
ocean.
lab’s
examined
ocean
structure
function
physical,
chemical,
biological
realms,
informed
supported
development
US
policy
these
areas.
Molecular Ecology,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 17, 2025
ABSTRACT
Anthropogenic
carbon
dioxide
emissions
have
been
increasing
rapidly
in
recent
years,
driving
pH
and
oxygen
levels
to
record
low
concentrations
the
oceans.
Eastern
boundary
upwelling
systems
such
as
California
Current
System
(CCS)
experience
exacerbated
ocean
acidification
hypoxia
(OAH)
due
physical
chemical
properties
of
transported
deeper
waters.
Research
efforts
significantly
increased
years
investigate
deleterious
effects
climate
change
on
marine
species,
but
not
focused
impacts
simultaneous
OAH
stressor
exposure.
Additionally,
few
studies
explored
physiological
these
environmental
stressors
earliest
life
stages,
which
are
more
vulnerable
represent
natural
population
bottlenecks
organismal
cycles.
The
response
ecologically
commercially
important
red
sea
urchin
(
Mesocentrotus
franciscanus
)
was
assessed
by
exposing
larvae
a
variety
conditions,
mimicking
range
relevant
conditions
encountered
currently
near
future
along
CCS.
Skeleton
dissolution,
larval
development,
gene
expression
show
with
clearly
delineated
thresholds
that
were
related
severity.
Skeletal
dissolution
induction
Acid‐sensing
Ion
Channel
1A
at
7.94/5.70
DO
mg/L
provide
particularly
sensitive
markers
OAH,
dramatic
shifts
morphology
detected
pH/DO
transition
7.71/3.71–7.27/2.72
mg/L.
Experimental
simulations
describe
establish
molecular
exposure
will
fishery
management
tools
predict
patterns
recruitment
forecast
dynamics.
Journal of Advances in Modeling Earth Systems,
Journal Year:
2025,
Volume and Issue:
17(1)
Published: Jan. 1, 2025
Abstract
Over
the
last
decades,
back‐calculation
(BC)
techniques
for
ocean
anthropogenic
carbon
(C
ant
)
estimation
have
improved
and
evolved
into
different
methodologies
that
are
not
exempt
from
various
assumptions
limitations.
No
single
optimal
BC
method
exists
to
date
computing
C
;
therefore,
it
is
necessary
continue
advancing
broad
range
of
approaches.
Here,
we
present
a
novel
based
on
fundamentals
combines
marine‐carbonate‐system
(MCS)
data
Total
Matrix
Intercomparison
(TMI)
framework.
This
MCS‐TMI
approach
differs
other
methods
by
using
TMI
reconstruct
deep‐ocean
biogeochemical
properties
their
preformed
conditions.
It
also
incorporates
global
sea‐air
oxygen
disequilibrium
term,
dynamic
stoichiometric
carbon‐to‐oxygen
ratio
depends
water‐mass
ideal
time.
The
yields
total
inventory
124
±
7
Pg
(referred
1995),
in
good
agreement
with
previous
climatologies.
uncertainty
(±5.6
μmol
kg
−1
controlled
input‐data
errors
that,
nonetheless,
minimal
impact
inventory.
In
contrast,
our
governed
methodological
errors,
specifically
those
related
TMI's
boundary
Our
study
demonstrates
effectiveness
MCS
data‐based
climatologies
reconstructing
3D
gridded
climatology,
validity
circulation
transport
operators
obtaining
Limnology and Oceanography,
Journal Year:
2025,
Volume and Issue:
unknown
Published: May 1, 2025
Abstract
Aragonite
undersaturation
(
1)
events
are
projected
to
rapidly
increase
in
frequency
and
duration
the
Antarctic
Weddell
Sea
by
2050.
Thecosome
pteropods
(pelagic
snails)
bioindicators
of
ocean
acidification
(OA)
because
their
aragonite
shell
dissolves
easily
at
low
saturation
states.
Here,
we
describe
dissolution
state
pteropod
Limacina
helicina
antarctica
relation
water
column
southern
during
austral
summer
2018
as
benchmark
for
future
monitoring
ongoing
OA.
depth
profiles
sampling
sites
were
consistently
close
or
range
threshold
levels
1.1–1.3)
dissolution.
Pteropods
contributed
up
69%
total
mesozooplankton
biomass,
distribution
correlated
positively
with
chlorophyll
a
concentration.
When
analyzed
scanning
electron
microscopy,
78%
investigated
shells
exhibited
dissolution,
50–69%
showed
more
severe
Type
II
exceeding
current
projections
Southern
Ocean.
But
importantly,
our
study,
only
two
specimens
had
most
III
Dissolution
often
co‐occurred
occurred
scratch
marks
unclear
origin
supporting
notions
that
an
intact
periostracum
protects
from
Where
absence
scratches
evidence
breaches,
microscale/nanoscale
breaches
may
have
been
important
pathway
commencement
recent
findings
reduction
organic
content
caused
/low
pH.
The
provide
here
allows
application
early‐warning
indicators
presumably
progressing
OA
Sea.
Journal of Experimental Biology,
Journal Year:
2024,
Volume and Issue:
227(23)
Published: Dec. 1, 2024
Polar
marine
invertebrates
serve
as
bellwethers
for
species
vulnerabilities
in
the
face
of
changing
climate
at
high
latitudes
Earth.
Ocean
acidification,
warming/heatwaves,
freshening,
sea
ice
retreat
and
productivity
change
are
challenges
polar
species.
Adaptations
to
life
cold
water
with
intensely
seasonal
has
shaped
traits
both
poles.
have
histories
often
characterised
K-strategist
or
K-selected
(e.g.
slow
growth
development,
larval
hypometabolism)
that
make
them
sensitive
stress
altered
productivity.
Moderate
warming
results
faster
development
can
positive
effects
on
up
a
limit.
However,
ocean
acidification
retard
impair
skeletogenesis
result
smaller
larvae.
Given
fast
pace
warming,
data
thermal
tolerance
larvae
from
diverse
is
urgently
needed,
well
knowledge
adaptive
responses
changes
Predicted
increase
would
benefit
energy-limited
reproduction
while
loss
negatively
impacts
directly
indirectly
depend
this
habitat.
It
critical
understand
interactive
between
other
stressors.
specialists
cannot
migrate,
making
susceptible
competition
extinction
range-extending
subpolar
The
borealisation
australisation
Arctic
Antarctic
ecosystems,
respectively,
underway
these
regions
become
more
hospitable
adult
life-history
stages
lower-latitude
Differences
biogeography
point
different
prospects
communities.
In
Commentary,
we
hypothesise
outcomes
based
history
sensitivity
suggest
research
avenues
test
our
predictions.
Oceanography,
Journal Year:
2023,
Volume and Issue:
unknown
Published: Jan. 1, 2023
The
ocean
is
warming,
acidifying,
and
losing
oxygen.
Global
Ocean
Ship-based
Hydrographic
Investigations
Program
(GO-SHIP)
carries
out
repeat
hydrographic
surveys
along
specified
transects
throughout
all
basins
to
allow
accurate
precise
quantification
of
changes
in
variables
such
as
temperature,
salinity,
carbon,
oxygen,
nutrients,
velocity,
anthropogenic
tracers,
uses
these
observations
understand
ventilation
patterns,
deoxygenation,
heat
uptake,
carbon
content,
circulation.
GO-SHIP
provides
global,
full-depth,
gold-standard
data
for
model
validation
calibration
autonomous
sensors,
including
Argo.
Pacific
Marine
Environmental
Laboratory,
through
sustained
funding
from
NOAA,
has
developed
methods
measure
several
the
routinely
sampled
a
core
contributor
cruises.
Conservation Physiology,
Journal Year:
2024,
Volume and Issue:
12(1)
Published: Jan. 1, 2024
Abstract
The
passive
dissolution
of
anthropogenically
produced
CO2
into
the
ocean
system
is
reducing
pH
and
changing
a
suite
chemical
equilibria,
with
negative
consequences
for
some
marine
organisms,
in
particular
those
that
bear
calcium
carbonate
shells.
Although
our
monitoring
these
changes
has
improved,
we
have
not
developed
effective
tools
to
translate
observations,
which
are
typically
saturation
state,
ecologically
relevant
predictions
biological
risks.
One
potential
solution
develop
bioindicators:
variables
clear
relationship
environmental
risk
factors
can
be
used
assessment
management.
Thecosomatous
pteropods
group
pelagic
shelled
gastropods,
whose
responses
been
suggested
as
bioindicators
acidification
owing
their
sensitivity
both
laboratory
natural
environment.
Using
five
exposure
experiments,
occurring
across
four
seasons
running
up
15
days,
describe
consistent
between
shell
transparency
duration
exposure,
well
identify
genes
could
further
study.
We
clarify
variations
thecosome
due
seasonality,
resolving
prior
uncertainties
demonstrating
range
phenotypic
plasticity.
These
biomarkers
stress
implemented
ecosystem
models
programmes
regions
where
found,
whilst
approach
will
serve
an
example
other
on
how
bridge
gap
point-based
biologically
assessments
health.
Global Change Biology,
Journal Year:
2024,
Volume and Issue:
30(7)
Published: July 1, 2024
A
Lagrangian
Individual
Based
Model
(IBM)
offers
new
insights
into
the
effects
of
ocean
acidification
on
pteropods
by
providing
detailed
life
histories
individuals.
thorough
analysis
results
makes
it
possible
to
attribute
different
mechanisms.
Science Advances,
Journal Year:
2024,
Volume and Issue:
10(48)
Published: Nov. 27, 2024
Ocean
acidification
driven
by
the
uptake
of
anthropogenic
CO
2
represents
a
major
threat
to
ocean
ecosystems,
yet
little
is
known
about
its
progression
beneath
surface.
Here,
we
reconstruct
history
interior
over
industrial
era
on
basis
observation-based
estimates
accumulation
carbon.
Across
top
100
meters
and
from
1800
2014,
saturation
state
aragonite
(Ω
arag
)
pH
=
−log[H
+
]
decreased
more
than
0.6
0.1,
respectively,
with
nearly
50%
occurring
past
20
years.
While
magnitude
Ω
change
decreases
uniformly
depth,
[H
increase
exhibits
distinct
maximum
in
upper
thermocline.
Since
1800,
horizon
1)
shoaled
200
meters,
approaching
euphotic
zone
several
regions,
especially
Southern
Ocean,
exposing
many
organisms
corrosive
conditions.
Authorea (Authorea),
Journal Year:
2024,
Volume and Issue:
unknown
Published: Jan. 29, 2024
Ocean
acidification
driven
by
the
uptake
of
anthropogenic
CO
represents
a
major
threat
to
ocean
ecosystems,
yet
little
is
known
about
its
progression
beneath
surface.
Here,
we
reconstruct
history
interior
(OIA)
from
1800
2014
on
basis
observation-based
estimates
accumulation
carbon.
Across
top
100
m
and
over
industrial
era,
saturation
state
aragonite
(Ω)
pH
=
-log[H]
decreased
more
than
0.6
0.1,
respectively,
with
progress
nearly
50%
last
20
years
(1994-2014).
While
magnitude
Ω
change
decreases
uniformly
depth,
decrease
exhibits
distinct
maximum
in
upper
thermocline.
Since
1800,
horizon
(Ω=1)
shoaled
200
m,
approaching
euphotic
zone
several
regions,
especially
Southern
Ocean,
exposing
many
organisms
corrosive
conditions.