SPAST Abstracts,
Journal Year:
2021,
Volume and Issue:
1(01)
Published: Oct. 8, 2021
An
estimated
value
of
500
million
population
are
directly
benefited
through
coral
reefs
related
jobs,
food
and
defence
coastal
areas.
Coral
help
to
reduce
wave
energy
by
97%.
They
protect
the
areas
from
storms,
floods
Natural
disasters
such
as
Tsunami
erosion
protected
reefs.
In
this
process
they
lives
many
staying
in
including
animals,
properties
other
natural
resources.
There
reasons
for
reef
deterioration
like
change
climate,
high
pollution,
destructive
fishing,
bleaching
is
a
big
concern
now
worldwide.
Severe
also
reported
India.
Significant
rise
surface
temperature
Sea
has
become
critical
reason
bleaching.
One
most
important
ecosystems
underwater
reef.
It
diverse
nature.
Approximately
5000
water
species
supported
per
unit
area.
includes
more
than
4000
fish,
800
hard
corals
different
varieties
marine
species.
full
life
activities
inside
it.
invertebrate.
Significance
an
structure
illustrated
section.
provide
protection.
Tourism
fishing
industries
environments
only
Flowering
plants
called
sea
grass
beds
Man
grove
forest
enriches
environment.
These
mangrove
forests
Many
animals
living
being
used
treat
various
diseases.
Life
under
gifted
with
maintain
significant
ecosystem.
polyps
reside
lime
exoskeleton
inherited
ancestors
built
ancestors.
A
polyp
tiny
organism
that
secrets
or
calcium
carbonate
which
takes
form
skeleton
lime.
The
diameter
each
0.04
inches
0.12
inches.
But
architecture
created
entire
colony
can
grow
massively.
Massive
skeletons
formed
colonies
successive
generations
make
it
further.
growth
massive
very
slow,
0.2
0.8
year.
Favourable
climate
conditions
optimum
light,
soothing
action
enhance
1.8
What
would
happen
if
happens
continuously
leading
disappearance
earth?
This
lead
huge
destruction.
will
disappear
due
lack
food.
might
bigger
imbalance
ecosystem
extinction
species,
life.
could
diseases,
epidemic
pandemics.
work
we
going
study
impact
Indian
ocean
using
two
parameters.
period
1985
2021.
demonstrates
comparative
analysis
on
environmental
aspects.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: March 12, 2024
Abstract
Climate
change
impact
syntheses,
such
as
those
by
the
Intergovernmental
Panel
on
Change,
consistently
assert
that
limiting
global
warming
to
1.5
°C
is
unlikely
safeguard
most
of
world’s
coral
reefs.
This
prognosis
primarily
based
a
small
subset
available
models
apply
similar
‘excess
heat’
threshold
methodologies.
Our
systematic
review
79
articles
projecting
reef
responses
climate
revealed
five
main
methods.
‘Excess
constituted
one
third
(32%)
all
studies
but
attracted
disproportionate
share
(68%)
citations
in
field.
Most
methods
relied
deterministic
cause-and-effect
rules
rather
than
probabilistic
relationships,
impeding
field’s
ability
estimate
uncertainty.
To
synthesize
projections,
we
aimed
identify
with
comparable
outputs.
However,
divergent
choices
model
outputs
and
scenarios
limited
analysis
fraction
studies.
We
found
substantial
discrepancies
projected
impacts,
indicating
serving
basis
for
syntheses
may
project
more
severe
consequences
other
Drawing
insights
from
fields,
propose
incorporate
uncertainty
into
modeling
approaches
multi-model
ensemble
approach
generating
projections
futures.
Global Change Biology,
Journal Year:
2025,
Volume and Issue:
31(4)
Published: April 1, 2025
The
primary
consequence
of
global
warming
for
reefs
is
coral
bleaching,
often
leading
to
extensive
mortality.
Although
bleaching
well-documented
globally,
the
thermal
stress
and
experienced
by
unique
South
Atlantic
remain
largely
unknown
due
insufficient
monitoring
on
both
spatial
temporal
scales.
Therefore,
this
work
aimed
reconstruct
past
episodes
across
reefs,
assessed
whether
are
becoming
more
intense,
longer-lasting,
frequent.
We
retrieved
daily
5
km-resolution
Degree
Heating
Week
(DHW)
data
from
U.S.
National
Oceanic
Atmospheric
Administration
Coral
Reef
Watch
server
33
reef
sites
spanning
last
40
years.
For
each
episode,
we
intensity
(maximum
DHW
value),
duration
(number
continuous
days
under
stress),
frequency
between
episodes).
Generalized
linear
models
were
fitted
intensity,
duration,
evaluate
influence
latitude
time
x
region
interaction
as
predictors.
recorded
multiple
episodes,
increasing
2010
onwards,
ranging
10
1985-89
75
2020-24.
Intensity
increased
over
entire
Atlantic.
Frequency
also
Southwestern
coast
oceanic
islands,
but
not
Africa.
Episodes
at
higher
latitudes
prolonged,
validity
history
reconstruction
was
groundtruthed
using
information
Abrolhos
Bank,
only
consistently
monitored
site
in
Atlantic-DHW
accurately
matched
observed
site.
With
this,
our
dataset
shows
that
likely
occurred
Atlantic,
went
undocumented
field.
currently
available
underestimates
extent
occurring
area,
which
experiencing
increases
stress.
Proceedings of the Royal Society B Biological Sciences,
Journal Year:
2022,
Volume and Issue:
289(1981)
Published: Aug. 31, 2022
Coral
reefs
are
facing
unprecedented
mass
bleaching
and
mortality
events
due
to
marine
heatwaves
climate
change.
To
avoid
extirpation,
corals
must
adapt.
Individual
variation
in
heat
tolerance
its
heritability
underpin
the
potential
for
coral
adaptation.
However,
magnitude
of
variability
within
populations
is
largely
unresolved.
We
address
this
knowledge
gap
by
exposing
from
a
single
reef
an
experimental
heatwave.
found
that
double
stress
dosage
was
required
induce
most-tolerant
10%,
compared
least-tolerant
10%
population.
By
end
exposure,
all
were
dead,
whereas
remained
alive.
contextualize
scale
result
over
coming
century,
we
show
under
ambitious
future
emissions
scenario,
such
differences
thresholds
equate
up
17
years
delay
until
onset
annual
conditions.
limited
only
10
high
scenario.
Our
results
substantial
which
suggests
scope
natural
or
assisted
evolution
limit
impacts
change
short-term.
For
persist
through
adaptation
keep
pace
with
ocean
warming,
reductions
be
realized.
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: Aug. 22, 2023
Abstract
Recurrent
mass
bleaching
events
threaten
the
future
of
coral
reefs.
To
persist
under
climate
change,
corals
will
need
to
endure
progressively
more
intense
and
frequent
marine
heatwaves,
yet
it
remains
unknown
whether
their
thermal
tolerance
can
keep
pace
with
warming.
Here,
we
reveal
an
emergent
increase
in
assemblages
at
a
rate
0.1
°C/decade
for
remote
Pacific
reef
system.
This
led
less
severe
impacts
than
would
have
been
predicted
otherwise,
indicating
adaptation,
acclimatisation
or
shifts
community
structure.
Using
projections,
show
that
if
continues
rise
over
coming
century
most-likely
historic
rate,
substantial
reductions
trajectories
are
possible.
High-frequency
be
fully
mitigated
some
reefs
low-to-middle
emissions
scenarios,
only
delayed
high
scenarios.
Collectively,
our
results
indicate
potential
ecological
resilience
but
still
highlight
reducing
carbon
line
Paris
Agreement
commitments
preserve
PLoS ONE,
Journal Year:
2023,
Volume and Issue:
18(2), P. e0281719 - e0281719
Published: Feb. 13, 2023
The
recurrence
of
mass
coral
bleaching
and
associated
mortality
in
the
past
few
decades
have
raised
questions
about
future
reef
ecosystems.
Although
is
well
studied,
our
understanding
spatial
extent
events
continues
to
be
limited
by
geographical
biases
data
collection.
To
address
this
gap,
we
updated
a
previous
observational
database
spatially
modelled
probability
occurrence.
First,
an
existing
raw
was
cover
1963–2017
period
using
searches
academic
grey
literature
outreach
monitoring
organizations.
Then,
order
provide
spatially-explicit
global
coverage,
employed
indicator
kriging
model
occurrence
each
year
from
1985
through
2017
at
0.05°
x
lat-long
resolution.
has
37,774
observations,
including
22,650
positive
reports,
three
times
that
version.
interpolation
suggests
71%
world’s
reefs
likely
(>66%
probability)
experienced
least
once
during
period.
mean
across
all
globally
29–45%
most
severe
years
1998,
2005,
2010
2016.
Modelled
probabilities
were
positively
related
with
annual
maximum
Degree
Heating
Weeks
(DHW),
measure
thermal
stress,
(p<0.001),
event
(p<0.01).
In
addition,
DHW
cells
very
(>90%
increased
over
time
rate
cells,
suggesting
possible
increase
tolerance.
interpolated
databases
can
used
other
researchers
enhance
real-time
predictions,
calibrate
models
for
projections,
assess
change
response
stress
time.
Communications Biology,
Journal Year:
2023,
Volume and Issue:
6(1)
Published: April 12, 2023
Abstract
As
marine
species
adapt
to
climate
change,
their
heat
tolerance
will
likely
be
under
strong
selection.
Yet
trade-offs
between
and
other
life
history
traits
could
compromise
natural
adaptation
or
assisted
evolution.
This
is
particularly
important
for
ecosystem
engineers,
such
as
reef-building
corals,
which
support
biodiversity
yet
are
vulnerable
heatwave-induced
mass
bleaching
mortality.
Here,
we
exposed
70
colonies
of
the
coral
Acropora
digitifera
a
long-term
heatwave
emulation
experiment.
We
tested
three
measured
from
in
situ
–
colony
growth,
fecundity,
symbiont
community
composition.
Despite
observing
remarkable
within-population
variability
tolerance,
all
were
dominated
by
Cladocopium
C40
symbionts.
found
no
evidence
fecundity
growth.
Contrary
expectations,
positive
associations
emerged
with
that
faster-growing
tended
bleach
die
at
higher
levels
stress.
Collectively,
our
results
suggest
these
corals
exist
on
an
energetic
continuum
where
some
high-performing
individuals
excel
across
multiple
traits.
Within
populations,
growth
may
not
major
barriers
success
evolution
interventions.
Conservation Biology,
Journal Year:
2023,
Volume and Issue:
38(1)
Published: May 5, 2023
Abstract
Identifying
locations
of
refugia
from
the
thermal
stresses
climate
change
for
coral
reefs
and
better
managing
them
is
one
key
recommendations
adaptation.
We
review
summarize
approximately
30
years
applied
research
focused
on
identifying
to
prioritize
conservation
actions
under
rapid
change.
found
that
currently
proposed
predicted
avoid
future
losses
are
highly
reliant
excess
heat
metrics,
such
as
degree
heating
weeks.
However,
many
existing
alternative
environmental,
ecological,
life‐history
variables
could
be
used
identify
other
types
lead
desired
diversified
portfolio
reef
conservation.
To
improve
priorities
reefs,
there
a
need
evaluate
validate
predictions
with
long‐term
field
data
abundance,
diversity,
functioning.
There
also
safeguard
displaying
resistance
toprolonged
exposure
waves
ability
recover
quickly
after
exposure.
recommend
using
more
metrics
potential
sites
can
avoid,
resist,
high
ocean
temperatures
consequences
change,
thereby
shifting
past
efforts
avoidance
risk‐spreading
strategic
in
rapidly
warming
climate.
Coral Reefs,
Journal Year:
2024,
Volume and Issue:
43(4), P. 969 - 984
Published: June 12, 2024
Abstract
Tropical
coral
reefs
are
a
critical
ecosystem
in
global
peril
as
result
of
anthropogenic
climate
change,
and
effective
conservation
efforts
require
reliable
methods
for
identifying
predicting
bleaching
events.
To
this
end,
temperature
threshold-based
models
such
the
National
Oceanic
Atmospheric
Administration’s
(NOAA)
degree-heating
week
(DHW)
metric
useful
forecasting
function
heat
stress
accumulation.
DHW
does
not
adequately
account
regional
variation
responses,
however,
current
definition
consistently
underpredicts
occurrence.
Using
weather
skill-based
framework,
our
analysis
cross-tested
1080
variations
DHW-based
occurrence
(presence/absence)
model
against
22
years
contemporary
observations
(1998–2019)
order
to
optimize
forecast
skill
at
different
levels
geographic
specificity.
On
basis
relative
definition,
reducing
1
°C
warming
cutoff
0.4
°C,
adjusting
accumulation
window
11
weeks,
defining
threshold
3
improved
by
70%.
Allowing
new
definitions
vary
across
regions
ocean
basins
further
doubled
skill.
Our
results
also
suggest
that
most
change
over
time
reef
systems
respond
shifting
climate.
Since
1998,
globally
optimized
has
risen
significant
rate
0.19
DHW/year,
matching
pace
warming.
The
trajectory
each
basin
varies.
Though
work
is
necessary
parse
mechanism
behind
trend,
dynamic
nature
responses
demands
tools
be
continuously
refined
if
they
inform
marine
efforts.
PLOS Climate,
Journal Year:
2024,
Volume and Issue:
3(7), P. e0000453 - e0000453
Published: July 11, 2024
Marine
heatwaves
and
mass
bleaching
have
devastated
coral
populations
globally,
yet
severity
often
varies
among
reefs.
To
what
extent
a
reef’s
past
exposure
to
heat
stress
influences
mortality
remains
uncertain.
Here
we
identify
persistent
local-scale
hotspots
thermal
refugia
the
reefs
of
Palau,
Micronesia,
based
on
36
years
satellite-derived
cumulative
(degree
heating
weeks–DHW,
units:
°C-weeks).
One
possibility
is
that
may
harbour
more
tolerant
corals
due
acclimatisation,
directional
selection,
and/or
loss
genotypes.
Historic
patterns
assemblage-wide
marine
align
with
this
hypothesis,
DHW-bleaching
responses
occurring
at
1.7°C-weeks
greater
than
refugia.
This
trend
was
consistent
weaker
for
Acropora
corymbose
,
severe
risk
reduced
by
4–10%
hotspots.
However,
find
contrasting
pattern
digitifera
exposed
simulated
heatwave.
Fragments
174
colonies
were
collected
from
replicate
hotspot
refugium
outer
comparable
wave
depth.
Higher
tolerance
(+0.7°C-weeks)
correlation
tissue
biomass
suggests
factors
other
DHW
overwhelm
any
spatially
varying
effects
exposure.
Further,
found
considerable
A
.
variability
across
sites;
compared
least-tolerant
10%
colonies,
most-tolerant
could
withstand
additional
stresses
5.2
4.1°C-weeks
hotspots,
respectively.
Our
study
demonstrates
do
not
necessarily
nearby
refugia,
predict
species
responses.
nuance
has
important
implications
designing
climate-smart
initiatives;
instance,
in
search
corals,
our
results
suggest
investing
effort
into
identifying
most
within
individual
be
warranted.
Frontiers in Marine Science,
Journal Year:
2022,
Volume and Issue:
9
Published: Nov. 22, 2022
Corals
in
the
northern
Red
Sea
exhibit
high
thermal
tolerance
despite
increasing
heat
stress.
It
is
assumed
that
corals
throughout
have
similar
bleaching
thresholds
(32°C
or
higher),
and
hence
greater
of
region
likely
due
to
lower
ambient
water
temperatures
(25–28°C)
remain
well
below
corals’
physiological
maxima.
Whether
patterns
across
are
independent
local
maximum
monthly
mean
seawater
temperature
aligned
with
an
32°C
threshold
has
yet
be
determined.
Here,
we
used
remotely
sensed
surface
sea
data
spanning
1982–2020
model
spatial
distributions
Degree
Heat
Weeks
relation
coral
values
30,
31,
32°C.
We
also
Coupled
Model
Intercomparison
Project
Phase
5
outputs
predict
warming
trends
under
different
greenhouse
gas
representative
concentration
pathways
(RCPs).
show
applying
dramatically
reduces
effective
north,
but
not
central
southern
regions,
a
finding
consistent
historical
observations
(1998–2020)
Sea.
Further,
predictions
most
extreme
RCP8.5
scenario
exhibited
~3°C
by
end
21
st
century
less
pronounced
for
(2–2.5°C)
compared
regions
(2.7–3.1°C).This
rate
will
which
should
help
this
serve
as
refugia
(i.e.,
maintaining
favorable
temperatures)
persist
decades
ahead.
Together,
our
results
support
notion
Sea;
hence,
mean.
Consequently,
where
regional
projections
suggest
reach
(32°C)
before
century,
reefs
may
among
last
standing
against
climate
change.