Communications Biology,
Journal Year:
2018,
Volume and Issue:
1(1)
Published: Oct. 18, 2018
The
oceans
are
warming
and
coral
reefs
bleaching
with
increased
frequency
severity,
fueling
concerns
for
their
survival
through
this
century.
Yet
in
the
central
equatorial
Pacific,
some
of
world's
most
productive
regularly
experience
extreme
heat
associated
El
Niño.
Here
we
use
skeletal
signatures
preserved
long-lived
corals
on
Jarvis
Island
to
evaluate
community
response
multiple
successive
heatwaves
since
1960.
By
tracking
stress
band
formation
2015-16
Nino,
which
killed
95%
corals,
validate
utility
as
proxies
severity
show
that
was
not
first
catastrophic
event
Jarvis.
Since
1960,
eight
severe
(>30%
bleaching)
two
moderate
(<30%
events
occurred,
each
coinciding
While
did
increase
over
time
period,
unprecedented
magnitude.
trajectory
recovery
historically
resilient
ecosystem
will
provide
critical
insights
into
potential
reef
resilience
a
world.
Global Change Biology,
Journal Year:
2012,
Volume and Issue:
18(5), P. 1561 - 1570
Published: Jan. 31, 2012
Abstract
Warming
ocean
temperatures
are
considered
to
be
an
important
cause
of
the
degradation
world's
coral
reefs.
Marine
protected
areas
(
MPA
s)
have
been
proposed
as
one
tool
increase
reef
ecosystem
resistance
and
resilience
(i.e.
recovery)
negative
effects
climate
change,
yet
few
studies
evaluated
their
efficacy
in
achieving
these
goals.
We
used
a
high
resolution
4
km
global
temperature
anomaly
database
from
1985–2005
8040
live
cover
surveys
on
unprotected
reefs
determine
whether
or
not
s
effective
mitigating
temperature‐driven
loss.
Generally,
protection
did
reduce
effect
warm
anomalies
declines.
Shortcomings
design,
including
size
placement,
may
contributed
lack
effect.
Empirical
suggest
that
corals
previously
exposed
moderate
levels
thermal
stress
greater
adaptive
capacity
future
events.
Existing
protect
relatively
fewer
with
frequencies,
potentially
reducing
effectiveness.
However,
our
results
also
benefits
great
enough
offset
magnitude
losses
acute
Although
conservation
tools,
limitations
loss
events
they
need
complemented
policies
aimed
at
activities
responsible
for
change.
Scientific Reports,
Journal Year:
2018,
Volume and Issue:
8(1)
Published: May 3, 2018
Tropical
reefs
often
undergo
acute
disturbances
that
result
in
landscape-scale
loss
of
coral.
Due
to
increasing
threats
coral
from
climate
change
and
anthropogenic
perturbations,
it
is
critical
understand
mechanisms
drive
recovery
these
ecosystems.
We
explored
this
issue
on
the
fore
reef
Moorea,
French
Polynesia,
following
a
crown-of-thorns
seastar
outbreak
cyclone
dramatically
reduced
cover
During
five-years
disturbances,
rate
re-establishment
differed
systematically
around
triangular-shaped
island;
returned
most
rapidly
at
sites
where
least
amount
live
remained
after
disturbances.
Although
greatly
return
coral,
all
showed
some
evidence
re-assembly
their
pre-disturbance
community
structure
terms
relative
abundance
taxa
other
benthic
space
holders.
The
primary
driver
spatial
variation
was
recruitment
sexually-produced
corals;
subsequent
growth
survivorship
were
less
important
shaping
pattern.
Our
findings
suggest
that,
although
has
been
resilient,
areas
are
unlikely
attain
taxonomic
they
had
prior
recent
before
advent
another
perturbation.
Scientific Reports,
Journal Year:
2018,
Volume and Issue:
8(1)
Published: June 20, 2018
Coral
reefs
are
increasingly
threatened
by
various
types
of
disturbances,
and
their
recovery
is
challenged
accelerating,
human-induced
environmental
changes.
Recurrent
disturbances
reduce
the
pool
mature
adult
colonies
reef-building
corals
undermine
post-disturbance
from
newly
settled
recruits.
Using
a
long-term
interannual
data
set,
we
show
that
coral
assemblages
on
reef
slope
Moorea,
French
Polynesia,
have
maintained
high
capacity
to
recover
despite
unique
frequency
large-scale
which,
since
1990s,
caused
catastrophic
declines
in
cover
abundance.
In
2014,
only
four
years
after
one
most
extreme
cases
decline
documented,
abundance
juvenile
had
regained
or
exceeded
pre-disturbance
levels,
no
phase-shift
macroalgal
dominance
was
recorded.
This
rapid
has
been
achieved
constantly
low
recruitment
rates,
suggesting
survivorship
However,
taxonomic
differences
susceptibility
contrasting
trajectories
resulted
changes
relative
composition
species.
present
context
global
decline,
our
study
establishes
new
benchmark
for
certain
benthic
communities
sustain
repeated,
intense
disturbances.
Scientific Reports,
Journal Year:
2013,
Volume and Issue:
3(1)
Published: March 20, 2013
On
coral
reefs,
fishes
can
facilitate
growth
via
nutrient
excretion;
however,
as
abundance
declines,
these
nutrients
may
help
increases
in
macroalgae.
By
combining
surveys
of
reef
communities
with
bioenergetics
modeling,
we
showed
that
fish
excretion
supplied
25
times
more
nitrogen
to
forereefs
the
Florida
Keys,
USA,
than
all
other
biotic
and
abiotic
sources
combined.
One
apparent
result
was
a
positive
relationship
between
macroalgal
cover
on
reefs.
Herbivore
biomass
also
negative
cover,
suggesting
strong
interactions
top-down
bottom-up
forcing.
Nutrient
supply
by
correlation
juvenile
density,
likely
mediated
competition
macroalgae
corals,
hinder
recovery
following
large-scale
loss.
Thus,
impact
be
context-dependent
reinforce
either
coral-dominant
or
coral-depauperate
depending
initial
community
states.
PLoS ONE,
Journal Year:
2012,
Volume and Issue:
7(8), P. e42167 - e42167
Published: Aug. 1, 2012
Accumulative
disturbances
can
erode
a
coral
reef's
resilience,
often
leading
to
replacement
of
scleractinian
corals
by
macroalgae
or
other
non-coral
organisms.
These
degraded
reef
systems
have
been
mostly
described
based
on
changes
in
the
composition
benthos,
and
there
is
little
understanding
how
such
are
influenced
by,
turn
influence,
components
ecosystem.
This
study
investigated
spatial
variation
benthic
communities
fringing
reefs
around
inner
Seychelles
islands.
Specifically,
relationships
between
underlying
substrata,
as
well
associated
fish
assemblages
were
assessed.
High
variability
was
found
among
reefs,
with
gradient
from
high
cover
(up
58%)
structural
complexity
95%)
low
at
extremes.
declining
species
richness
fishes,
reduced
diversity
functional
groups,
lower
abundance
corallivorous
fishes.
There
no
reciprocal
increases
herbivorous
abundances,
groups
total
weak.
Reefs
grouping
extremes
complex
habitats
low-complexity
macroalgal
displayed
markedly
different
communities,
only
two
invertebrate
feeding
fishes
greater
habitat.
results
negative
implications
for
continuation
many
ecosystem
processes
services
if
more
shift
extreme
conditions
dominated
macroalgae.
Coral Reefs,
Journal Year:
2014,
Volume and Issue:
33(3), P. 553 - 563
Published: April 9, 2014
Changes
in
the
relative
abundances
of
coral
taxa
during
recovery
from
disturbance
may
cause
shifts
essential
ecological
processes
on
reefs.
Coral
cover
can
return
to
pre-disturbance
levels
(coral
recovery)
without
assemblage
returning
its
previous
composition
(i.e.,
reassembly).
The
underlying
such
changes
are
not
well
understood
due
a
scarcity
long-term
studies
with
sufficient
taxonomic
resolution.
We
assessed
trajectories
and
time
frames
for
reassembly
communities
following
disturbances,
using
modeled
based
data
broad
spatial
temporal
monitoring
program.
studied
at
six
reefs
that
suffered
substantial
loss
subsequently
regained
least
50
%
their
cover.
Five
rates
were
remarkably
consistent,
taking
7–10
years.
Four
reassembled
8–13
three
both
ten
two
suggested
they
unlikely
reassemble
remaining
community
did
regain
had
high
abundance
tabulate
Acropora
spp.
this
appear
likely
persist
regime
pulse
disturbances
intervals
years
or
more.
Communities
failed
either
near-shore
locations
Porites
soft
corals.
Under
current
regimes,
these
re-establish
composition.
Frontiers in Marine Science,
Journal Year:
2019,
Volume and Issue:
6
Published: Aug. 16, 2019
A
changing
climate
is
driving
increasingly
common
and
prolonged
marine
heatwaves
(MHWs)
these
extreme
events
have
now
been
widely
documented
to
severely
impact
ecosystems
globally.
However
MHWs
rarely
recently
considered
when
examining
temperature-induced
degradation
of
coral
reef
ecosystems.
Here
we
consider
extreme,
localised
thermal
anomalies,
nested
within
broader
increases
in
sea
surface
temperature,
which
fulfil
the
definitive
criteria
for
MHWs.
These
acute
intense
events,
referred
here
as
MHW
hotspots,
are
not
always
well
represented
current
framework
used
describe
bleaching,
but
do
distinct
ecological
outcomes,
including
widespread
bleaching
rapid
mass
mortality
putatively
thermally
tolerant
species.
The
physical
drivers
hotspots
discussed
here,
doing
so
present
a
comprehensive
theoretical
that
links
biological
responses
photo-endosymbiotic
organism
stress
changes
on
reefs
associated
after
hotspots.
We
how
onset
high
temperatures
drives
immediate
heat-stress
induced
cellular
damage,
overwhelming
mechanisms
would
otherwise
mitigate
gradually
accumulated
stress.
warm
environment,
increased
light
penetration
skeleton
due
loss
tissues,
coupled
with
tissue
decay
support
microbial
growth
skeletal
microenvironment,
resulting
unrecognised
consequence
degeneration
skeletons.
This
accelerated
skeletonson
scale
hinder
recovery
populations
increase
likelihood
phase
shifts
towards
algal
dominance.
suggest
through
heat-induced
mortality,
compromise
reefs'
structural
frameworks
detriment
long
term
recovery.
propose
be
class
reefs,
expanded
include
these.
urge
further
research
into
affects
bioerosion
by
endoliths.
Annual Review of Ecology Evolution and Systematics,
Journal Year:
2013,
Volume and Issue:
44(1), P. 503 - 538
Published: Nov. 23, 2013
Consumer
fronts
occur
when
grazers
or
predators
aggregate
in
bands
along
the
edges
of
a
resource.
Our
review
reveals
that
consumer
are
common
phenomenon
nature,
many
different
ecosystems,
and
triggered
by
universal
mechanisms:
External
forces
locally
increase
top-down
control
beyond
prey
carrying
and/or
renewal
capacity,
resource-dependent
movement
leads
to
aggregation
edge
remaining
population.
Once
formed,
move
through
systems
as
spatially
propagating
waves,
self-reinforced
via
intense
overexploitation
amplified
density-dependent
feedbacks.
When
restricted,
they
generate
patchiness.
In
contrast,
expansive,
can
lead
runaway
responses
cause
large-scale
ecosystem
degradation
regime
shifts.
We
conceptualize
synergistic
stress
hypothesis
model
highlight
how
coupled
intensification
physical
enhanced
pressure
trigger
increased
occurrence
decreased
system
stability
resilience.
With
escalating
climate
change
food-web
modification,
biological
conditions
favoring
consumer-front
formation
will
likely
become
feature
ecosystems.
Annual Review of Ecology Evolution and Systematics,
Journal Year:
2015,
Volume and Issue:
46(1), P. 49 - 73
Published: Aug. 8, 2015
Here
we
review
the
population,
community,
and
evolutionary
consequences
of
marine
reserves.
Responses
at
each
level
depend
on
tendency
fisheries
to
target
larger
body
sizes
for
greater
reserve
protection
with
less
movement
within
across
populations.
The
primary
population
response
reserves
is
survival
ages
plus
increases
in
size
harvested
species,
that
are
large
relative
species'
rates.
community
an
increase
total
biomass
diversity,
potential
trophic
cascades
altered
spatial
patterning
metacommunities.
increased
genetic
theoretical
against
fisheries-induced
evolution
selection
reduced
movement.
combined
outcome
these
responses
buffer
populations
communities
temporal
environmental
heterogeneity
has
preliminary
empirical
support.