F1000Prime Reports,
Journal Year:
2014,
Volume and Issue:
6
Published: Nov. 4, 2014
There
is
growing
concern
about
the
impacts
of
climate
change
and
ocean
acidification
on
marine
organisms
ecosystems,
yet
potential
for
acclimation
adaptation
to
these
threats
poorly
understood.
Whereas
many
short-term
experiments
report
negative
biological
effects
warming
acidification,
new
studies
show
that
some
species
have
capacity
acclimate
warmer
more
acidic
environments
across
generations.
Consequently,
transgenerational
plasticity
may
be
a
powerful
mechanism
by
which
populations
will
able
adjust
projected
change.
Here,
I
review
recent
advances
in
understanding
fishes.
Research
over
past
2
3
years
shows
can
partially
or
fully
ameliorate
warming,
hypoxia
range
different
species.
The
molecular
cellular
pathways
underpinning
are
currently
unknown,
but
modern
genetic
methods
provide
tools
explore
mechanisms.
Despite
benefits
acclimation,
there
could
limitations
phenotypic
traits
respond
transgenerationally,
trade-offs
between
life
stages,
need
investigated.
Future
should
also
test
interactions
evolution
determine
how
two
processes
shape
adaptive
responses
environmental
coming
decades.
Science,
Journal Year:
2015,
Volume and Issue:
349(6243)
Published: July 3, 2015
Carbon
emissions
and
their
ocean
impacts
Anthropogenic
CO
2
directly
affect
atmospheric
chemistry
but
also
have
a
strong
influence
on
the
oceans.
Gattuso
et
al.
review
how
physics,
chemistry,
ecology
of
oceans
might
be
affected
based
two
emission
trajectories:
one
business
as
usual
with
aggressive
reductions.
Ocean
warming,
acidification,
sea-level
rise,
expansion
oxygen
minimum
zones
will
continue
to
distinct
marine
communities
ecosystems.
The
path
that
humanity
takes
regarding
largely
determine
severity
these
phenomena.
Science
,
this
issue
10.1126/science.aac4722
Science,
Journal Year:
2015,
Volume and Issue:
347(6219)
Published: Jan. 15, 2015
Marine
defaunation,
or
human-caused
animal
loss
in
the
oceans,
emerged
forcefully
only
hundreds
of
years
ago,
whereas
terrestrial
defaunation
has
been
occurring
far
longer.
Though
humans
have
caused
few
global
marine
extinctions,
we
profoundly
affected
wildlife,
altering
functioning
and
provisioning
services
every
ocean.
Current
ocean
trends,
coupled
with
lessons,
suggest
that
rates
will
rapidly
intensify
as
human
use
oceans
industrializes.
protected
areas
are
a
powerful
tool
to
harness
productivity,
especially
when
designed
future
climate
mind,
additional
management
strategies
be
required.
Overall,
habitat
degradation
is
likely
major
driver
wildlife
loss.
Proactive
intervention
can
avert
disaster
magnitude
observed
on
land.
Science,
Journal Year:
2014,
Volume and Issue:
344(6186), P. 895 - 898
Published: April 25, 2014
Reef
corals
are
highly
sensitive
to
heat,
yet
populations
resistant
climate
change
have
recently
been
identified.
To
determine
the
mechanisms
of
temperature
tolerance,
we
reciprocally
transplanted
between
reef
sites
experiencing
distinct
regimes
and
tested
subsequent
physiological
gene
expression
profiles.
Local
acclimatization
fixed
effects,
such
as
adaptation,
contributed
about
equally
heat
tolerance
reflected
in
patterns
expression.
In
less
than
2
years,
achieves
same
that
would
expect
from
strong
natural
selection
over
many
generations
for
these
long-lived
organisms.
Our
results
show
both
short-term
acclimatory
longer-term
adaptive
acquisition
resistance.
Adding
abilities
ecosystem
models
is
likely
slow
predictions
demise
coral
ecosystems.
Science,
Journal Year:
2015,
Volume and Issue:
348(6242), P. 1460 - 1462
Published: June 25, 2015
Some
like
it
hot
Coral
reefs
are
threatened
by
increasing
temperatures.
Acute
temperature
increases
stress
and
damage
corals.
However,
more
gradual
changes
can
result
in
adaptation
subsequent
tolerance
for
higher
Dixon
et
al.
show
that
the
heat
currently
exists
across
coral
populations
from
different
latitudes
be
inherited.
Thus,
natural
variation
may
facilitate
rapid
among
corals
as
our
climate
warms.
Science
,
this
issue
p.
1460
Scientific Reports,
Journal Year:
2016,
Volume and Issue:
6(1)
Published: Dec. 6, 2016
Abstract
Coral
reefs
across
the
world’s
oceans
are
in
midst
of
longest
bleaching
event
on
record
(from
2014
to
at
least
2016).
As
many
remote,
there
is
limited
information
how
past
thermal
conditions
have
influenced
reef
composition
and
current
stress
responses.
Using
satellite
temperature
data
for
1985–2012,
analysis
we
present
first
quantify,
global
locations,
spatial
variations
warming
trends,
events
variability
reef-scale
(~4
km).
Among
over
60,000
pixels
globally,
97%
show
positive
SST
trends
during
study
period
with
60%
significantly.
Annual
exceeded
summertime
most
locations.
This
indicates
that
summer-like
temperatures
has
become
longer
through
record,
a
corresponding
shortening
‘winter’
reprieve
from
warm
temperatures.
The
frequency
bleaching-level
increased
three-fold
between
1985–91
2006–12
–
trend
climate
model
projections
suggest
will
continue.
history
products
developed
enable
needed
studies
relating
resistance
community
composition.
Such
analyses
can
help
identify
more
resilient
stress.
Science,
Journal Year:
2016,
Volume and Issue:
352(6283), P. 338 - 342
Published: April 14, 2016
Bleaching
of
the
Great
Barrier
Reef
The
Australian
(GBR)
is
one
Earth's
most
extraordinary
natural
wonders,
but
it
vulnerable
to
climate
change.
Ainsworth
et
al.
have
tracked
effects
three
decades
increasing
heat
stress
on
coral
organisms.
In
past,
pulses
elevated
temperatures
that
presaged
hot
seasons
stimulated
acclimation
organisms
and
resilience
thermal
stress.
More
recently,
temperature
hikes
been
severe
precluded
acclimation.
result
has
bleaching
death;
notably
extreme
during
2016
in
wake
El
Niño.
Science
,
this
issue
p.
338
Scientific Reports,
Journal Year:
2016,
Volume and Issue:
6(1)
Published: Dec. 21, 2016
Abstract
Increasingly
frequent
severe
coral
bleaching
is
among
the
greatest
threats
to
reefs
posed
by
climate
change.
Global
models
(GCMs)
project
great
spatial
variation
in
timing
of
annual
(ASB)
conditions;
a
point
at
which
are
certain
change
and
recovery
will
be
limited.
However,
previous
model-resolution
projections
(~1
×
1°)
too
coarse
inform
conservation
planning.
To
meet
need
for
higher-resolution
projections,
we
generated
statistically
downscaled
(4-km
resolution)
all
reefs;
these
reveal
high
local-scale
ASB.
Timing
ASB
varies
>10
years
71
87
countries
territories
with
>
500
km
2
reef
area.
Emissions
scenario
RCP4.5
represents
lower
emissions
mid-century
than
eventuate
if
pledges
made
following
2015
Paris
Climate
Change
Conference
(COP21)
become
reality.
These
do
little
provide
more
time
adapt
acclimate
prior
conditions
occurring
annually.
adds
11
global
average
when
compared
RCP8.5;
however,
>75%
still
experience
before
2070
under
RCP4.5.
Coral
futures
clearly
vary
greatly
within
countries,
indicating
warrant
consideration
most
areas
during
management
Global Change Biology,
Journal Year:
2014,
Volume and Issue:
20(12), P. 3823 - 3833
Published: July 9, 2014
Abstract
Mass
coral
bleaching
events
caused
by
elevated
seawater
temperatures
result
in
extensive
loss
throughout
the
tropics,
and
are
projected
to
increase
frequency
severity.
If
becomes
an
annual
event
later
this
century,
more
than
90%
of
reefs
worldwide
may
be
at
risk
long‐term
degradation.
While
corals
can
recover
from
single
isolated
acclimate
recurring
that
separated
multiple
years,
it
is
currently
unknown
if
how
they
will
survive
possibly
acclimatize
bleaching.
Here,
we
demonstrate
for
first
time
dramatically
alter
thermal
tolerance
Caribbean
corals.
We
found
high
energy
reserves
changes
dominant
algal
endosymbiont
type
(
Symbiodinium
spp.)
facilitated
rapid
acclimation
Porites
divaricata
,
whereas
low
a
lack
phenotypic
plasticity
significantly
increased
susceptibility
astreoides
following
year.
Phenotypic
Orbicella
faveolata
did
not
prevent
repeat
bleaching,
but
have
recovery.
Thus,
holobiont
response
accurate
predictor
its
Rather,
cumulative
impact
turn
some
species
‘winners’
into
‘losers’,
also
facilitate
‘losers’
‘winners’.
Overall,
these
findings
indicate
could
becoming
increasingly
susceptible
face
decline,
while
phenotypically
plastic
persist.
recovery
contribute
selective
diversity
as
well
overall
decline
Caribbean.
Global Change Biology,
Journal Year:
2014,
Volume and Issue:
21(1), P. 236 - 249
Published: Aug. 6, 2014
Abstract
Mutualistic
organisms
can
be
particularly
susceptible
to
climate
change
stress,
as
their
survivorship
is
often
limited
by
the
most
vulnerable
partner.
However,
symbiotic
plasticity
also
help
in
changing
environments
expanding
realized
niche
space.
Coral–algal
(
Symbiodinium
spp.)
symbiosis
exemplifies
this
dichotomy:
partnership
highly
‘bleaching’
(stress‐induced
breakdown),
but
stress‐tolerant
symbionts
sometimes
mitigate
bleaching.
Here,
we
investigate
role
of
diverse
and
mutable
partnerships
increasing
corals'
ability
thrive
high
temperature
conditions.
We
conducted
repeat
bleaching
recovery
experiments
on
coral
Montastraea
cavernosa
,
used
quantitative
PCR
chlorophyll
fluorometry
assess
structure
function
communities
within
hosts.
During
an
initial
heat
exposure
(32
°C
for
10
days),
corals
hosting
only
stress‐sensitive
C3)
bleached,
recovered
(at
either
24
or
29
°C)
with
predominantly
(>90%)
D1a),
which
were
not
detected
before
(either
due
absence
extreme
low
abundance).
When
a
second
stress
(also
32
days)
was
applied
3
months
later,
that
previously
bleached
now
dominated
D1a
experienced
less
photodamage
symbiont
loss
compared
control
had
been
therefore
still
C3.
Additional
initially
without
herbicide
DCMU
at
symbionts,
similarly
lost
fewer
during
subsequent
thermal
stress.
Increased
thermotolerance
observed
C3‐dominated
acclimated
warmer
temperatures
(29
These
findings
indicate
increased
post‐bleaching
resulted
from
community
composition
changes,
prior
exposure.
Moreover,
undetectable
became
dominant
after
bleaching,
critical
resilience
resistance
future