Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(22), P. 4975 - 5004
Published: Nov. 14, 2024
Abstract.
Anthropogenic
warming
and
nutrient
over-enrichment
of
our
oceans
have
resulted
in
significant,
often
catastrophic,
reductions
dissolved
oxygen
(deoxygenation).
Stress
on
water-breathing
animals
from
this
deoxygenation
has
been
shown
to
occur
at
all
levels
biological
organization:
cellular,
organ,
individual,
species,
population,
community,
ecosystem.
Most
climate
forecasts
predict
increases
ocean
deoxygenation;
thus,
it
is
essential
develop
reliable
indicators
low-oxygen
stress
that
can
be
used
by
regional
global
monitoring
efforts
detect
assess
the
impacts
life.
This
review
focuses
responses
are
manifest
different
organization
a
variety
spatial
temporal
scales.
We
compare
particular
attributes
these
threshold
response,
timescales
sensitive
life
stages
taxa,
ability
scale
response
across
organization.
Where
there
available
evidence,
we
discuss
interactions
other
abiotic
stressors
stress.
address
utility,
confounding
effects,
implementation
for
research
societal
applications.
Our
hope
further
refinement
dissemination
will
provide
more
direct
support
environmental
managers,
fisheries
mariculture
scientists,
conservation
professionals,
policymakers
confront
challenges
deoxygenation.
An
improved
understanding
sensitivity
communities,
ecosystems
empower
design
programs,
ecosystem
health,
management
guidelines,
track
conditions,
events.
Limnology and Oceanography Methods,
Journal Year:
2023,
Volume and Issue:
21(7), P. 421 - 434
Published: May 27, 2023
Abstract
Ocean
warming
is
increasingly
affecting
marine
ecosystems
across
the
globe.
Reef‐building
corals
are
particularly
affected
by
warming,
with
mass
bleaching
events
increasing
in
frequency
and
leading
to
widespread
coral
mortality.
Yet,
some
can
resist
or
recover
from
better
than
others.
Such
variability
thermal
resilience
could
be
critical
reef
persistence;
however,
scientific
community
lacks
standardized
diagnostic
approaches
rapidly
comparatively
assess
vulnerability
prior
events.
We
present
Coral
Bleaching
Automated
Stress
System
(CBASS)
as
a
low‐cost,
open‐source,
field‐portable
experimental
system
for
rapid
empirical
assessment
of
thresholds
using
temperature
stress
profiles
diagnostics.
The
CBASS
consists
four
eight
flow‐through
aquaria
independent
water
masses,
lighting,
individual
automated
controls
capable
delivering
custom
modulating
profiles.
used
conduct
daily
exposures
that
typically
include
3‐h
ramps
multiple
target
temperatures,
hold
period
at
1‐h
ramp
back
down
ambient
temperature,
followed
an
overnight
recovery
period.
This
mimics
shallow
observed
reefs
prompts
acute
heat
response
serve
tool
identify
putative
thermotolerant
in‐depth
assessments
adaptation
mechanisms,
targeted
conservation,
possible
use
restoration
efforts.
deployable
within
hours
assay
up
40
fragments/aquaria/day,
enabling
high‐throughput,
determination
genotypes,
populations,
species,
sites
framework.
Coral Reefs,
Journal Year:
2024,
Volume and Issue:
43(1), P. 119 - 133
Published: Jan. 8, 2024
Abstract
Human-induced
climate
change
is
causing
ocean
warming
that
triggers
the
breakdown
of
coral–algal
symbiosis.
The
proximate
cause
this
phenomenon,
known
as
coral
bleaching,
commonly
attributed
to
overproduction
reactive
oxygen
species
(ROS)
by
thermally
stressed
photosynthetic
algal
symbionts.
However,
direct
evidence
ROS
production
(e.g.,
in
form
H
2
O
)
and
physiological
stress
are
ultimate
bleaching
remains
ambiguous.
Here,
we
investigated
temporal
dynamics
(O
concentrations
during
induced
disentangle
from
consequence.
Microsensors
at
tissue
interface
Pocillopora
damicornis
measured
while
exposing
single
nubbins
baseline
temperatures
(30
°C)
minor
(33
°C),
moderate
(36
high
(39
levels
acute
heat
using
Coral
Bleaching
Automated
Stress
System
(CBASS).
We
show
a
temporary
decline
concentration,
accompanied
declining
efficiency
loss
Symbiodiniaceae
pigmentation,
initial
response
thermal
stress.
This
was
neither
provoked
nor
followed
an
increased
concentration
interface.
A
steady
light-independent
increase
only
detected
stress,
resulting
complete
permanent
activity.
Our
findings
do
not
support
connection
between
photodamage
suggest
more
research
on
function
warranted.
notion
further
substantiated
observation
additional
source
,
likely
oxidative
bursts,
were
common
temperature
under
their
occurrence
decreased
Resolving
multifaceted
dynamic
roles
critical
better
understand
holobiont
identifying
processes
underlying
Frontiers in Marine Science,
Journal Year:
2024,
Volume and Issue:
10
Published: Feb. 1, 2024
Ocean
deoxygenation
is
intensifying
globally
due
to
human
activities
–
and
emerging
as
a
grave
threat
coral
reef
ecosystems
where
it
can
cause
bleaching
mass
mortality.
However,
one
of
many
threats
reefs,
making
essential
understand
how
prior
environmental
stress
may
influence
responses
deoxygenation.
To
address
this
question,
we
examined
the
holobiont
(i.e.,
host,
Symbiodiniaceae,
microbiome)
in
corals
with
different
backgrounds.
We
outplanted
Acropora
cervicornis
fragments
known
genotypes
from
an
situ
nursery
two
sites
Florida
Keys
spanning
inshore-offshore
gradient.
After
four
months,
were
transferred
laboratory,
tested
differences
survivorship,
tissue
loss,
photosynthetic
efficiency,
Symbiodiniaceae
cell
density,
microbiome
composition
after
persistent
exposure
oxygen
treatments
ranging
extreme
(0.5
mg
L
-1
)
normoxia
(6
).
found
that,
for
short
duration
study
(four
days),
entire
was
resistant
dissolved
(DO)
concentrations
low
2.0
,
but
that
members
decoupled
at
0.5
.
In
most
treatment,
host
showed
decreased
mortality,
lower
densities
response,
microbial
taxa
remained
stable.
Although
did
not
major
community
shifts
composition,
population
abundance
some
respond.
Site
history
influenced
endosymbiont,
microbiome,
more
stressful
inshore
site
showing
greater
susceptibility
subsequent
Our
reveals
respond
differently
deoxygenation,
sensitivity
resistance
decrease
tolerance
Coral Reefs,
Journal Year:
2024,
Volume and Issue:
43(3), P. 571 - 585
Published: April 3, 2024
Abstract
Variable
temperature
regimes
that
expose
corals
to
sublethal
heat
stress
have
been
recognized
as
a
mechanism
increase
coral
thermal
tolerance
and
lessen
bleaching.
However,
there
is
need
better
understand
which
maximize
hardening.
Here,
standardized
assays
were
used
determine
the
relative
of
three
divergent
genera
(
Acropora
,
Pocillopora
Porites
)
originating
from
six
reef
sites
representing
an
increasing
gradient
annual
mean
diel
fluctuations
1–3
°C
day
−1
.
Bleaching
severity
dark-acclimated
photochemical
yield
(i.e.,
F
v
/
m
quantified
following
exposure
five
treatments
ranging
23.0
36.3
°C.
The
greatest
effective
dose
50)
was
found
at
site
with
intermediate
variability
(2.2
),
suggesting
optimal
priming
leads
maximal
tolerance.
Interestingly,
least
thermally
variable
(<
1.3
had
lower
than
most
(>
2.8
whereas
opposite
true
for
responses
across
taxa.
Remarkably,
comparisons
global
studies
revealed
range
in
uncovered
this
study
single
5
km)
large
differences
observed
vast
latitudinal
gradients
(300–900
km).
This
finding
indicates
local
gene
flow
could
improve
between
habitats.
climate
change
continues,
intensifying
marine
heatwaves
already
compromising
enhance
bleaching
resistance.
Limnology and Oceanography,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 21, 2025
Abstract
Seawater
hypoxia
is
increasing
globally
and
can
drive
declines
in
organismal
performance
across
a
wide
range
of
marine
taxa.
However,
the
effects
on
early
life
stages
(e.g.,
larvae
juveniles)
are
largely
unknown,
it
unclear
how
evolutionary
histories
may
influence
these
outcomes.
Here,
we
addressed
this
question
by
comparing
responses
three
cnidarian
species
representing
histories:
reef‐building
coral
Galaxea
fascicularis
,
broadcast
spawner
with
horizontal
transmission
endosymbiotic
algae
(family
Symbiodiniaceae);
Porites
astreoides
brooder
vertical
endosymbiont
transmission;
estuarine
sea
anemone
Nematostella
vectensis
non‐symbiotic
spawner.
Transient
exposure
to
(dissolved
oxygen
<
2
mg
L
−1
for
6
h)
led
decreased
larval
swimming
growth
all
species,
which
resulted
impaired
settlement
corals.
Coral‐specific
also
included
swelling,
depressed
respiration
rates,
decreases
symbiont
densities
function.
These
results
indicate
both
immediate
latent
negative
physiology
coral–algal
mutualisms
specifically.
In
addition,
G.
P.
were
sensitized
heat
stress
following
exposure,
suggesting
that
combinatorial
nature
climate
stressors
will
lead
declining
sensitization
was
not
observed
N.
exposed
hypoxia,
be
more
resilient
combined
stressors.
Overall,
emphasize
importance
reducing
anthropogenic
carbon
emissions
limit
further
ocean
deoxygenation
warming.
Earth System Dynamics,
Journal Year:
2025,
Volume and Issue:
16(1), P. 275 - 292
Published: Feb. 7, 2025
Abstract.
Warm-water
coral
reefs
are
facing
unprecedented
human-driven
threats
to
their
continued
existence
as
biodiverse
functional
ecosystems
upon
which
hundreds
of
millions
people
rely.
These
impacts
may
drive
past
critical
thresholds,
beyond
the
system
reorganises,
often
abruptly
and
potentially
irreversibly;
this
is
what
Intergovernmental
Panel
on
Climate
Change
(IPCC,
2022)
define
a
tipping
point.
Determining
point
thresholds
for
reef
requires
robust
assessment
multiple
stressors
interactive
effects.
In
perspective
piece,
we
draw
recent
global
revision
initiative
(Lenton
et
al.,
2023a)
literature
search
identify
summarise
diverse
range
interacting
that
need
be
considered
determining
warm-water
ecosystems.
Considering
observed
projected
stressor
impacts,
endorse
revision's
conclusion
mean
surface
temperature
(relative
pre-industrial)
threshold
1.2
°C
(range
1–1.5
°C)
long-term
atmospheric
CO2
concentrations
above
350
ppm,
while
acknowledging
comprehensive
stressors,
including
ocean
warming
response
dynamics,
overshoot,
cascading
have
yet
sufficiently
realised.
already
been
exceeded,
therefore
these
systems
in
an
overshoot
state
reliant
policy
actions
bring
levels
back
within
limits.
A
fuller
likely
further
lower
most
cases.
Uncertainties
around
points
such
crucially
important
underline
imperative
and,
case
knowledge
gaps,
employing
precautionary
principle
favouring
lower-range
values.
Remote Sensing in Ecology and Conservation,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Feb. 26, 2025
Abstract
Coral
bleaching,
often
triggered
by
oceanic
warming,
has
a
devastating
impact
on
coral
reef
systems,
resulting
in
substantial
alterations
to
biodiversity
and
ecosystem
services.
For
conservation
management,
an
effective
technique
is
needed
not
only
detect
monitor
bleaching
events
but
also
predict
their
severity
levels.
By
combining
high‐resolution
satellite
measurements
(Sentinel‐2
Multispectral
Instrument)
bottom
reflectance
model
within
least‐squares
approach,
we
developed
new
ocean
color
remote‐sensing
specifically
designed
detect,
map,
levels
(low
high)
of
at
high
spatial
resolution
10
m.
The
proposed
algorithm
was
implemented
tested
the
Red
Sea
compared
remarkably
well
with
concurrent
independent
situ
data.
We
applied
investigate
response
corals
during
after
event
Wadi
El‐Gemal
region
(Egypt)
from
July
December
2020.
Our
results
show
that
sea
surface
temperature
(SST)
were
unusually
August–September
After
event,
signal
decreased
concurrently
SST
October–November
2020,
aligned
recovery
bleached
reefs
offers
cost‐effective
approach
toward
developing
near‐real‐time
system
for
monitoring
multi‐reef
scales.
Such
tools
would
aid
policymakers
managers
implementing
integrated
management
strategies
conservation,
as
supporting
reactive
plans,
including
identification
priority
areas
intervention.