Paleoceanography,
Год журнала:
1997,
Номер
12(4), С. 533 - 545
Опубликована: Авг. 1, 1997
Estimated
changes
in
reef
area
and
CaCO
3
production
since
the
last
glacial
maximum
(LGM)
are
presented
for
first
time,
based
on
a
model
(ReefHab)
which
uses
measured
environmental
data
to
predict
global
distribution
of
habitat.
Suitable
habitat
is
defined
by
temperature,
salinity,
nutrients,
depth‐attenuated
level
photosynthetically
available
radiation
(PAR).
calculated
as
function
PAR.
When
minimum
PAR
levels
were
chosen
restrict
growth
30
m
depth
less,
modern
totaled
584–746
×
10³
km².
Global
carbonate
production,
takes
into
account
topographic
relief
control
accumulation,
was
1.00
Gt
yr
−1
.
These
values
close
most
widely
accepted
estimates
demonstrate
that
basic
can
be
used
define
calcification.
To
simulate
LGM,
run
at
1‐kyr
intervals,
using
appropriate
sea
temperature
values.
runs
show
restricted
20%
today
27%,
due
primarily
reduction
space
lower
secondarily
surface
temperatures.
Nonetheless,
these
suggest
prior
shelf
flooding
more
extensive
than
previously
thought.
A
crude
estimate
reef‐released
CO
2
atmosphere
LGM
same
order
magnitude
atmospheric
change
recorded
Vostok
ice
core,
emphasizes
role
neritic
carbonates
within
carbon
cycle.
This
currently
addresses
only
major
physical
chemical
controls
but
it
provides
template
estimating
shallow
tropical
both
present
past.
As
such,
highlights
several
long‐standing
issues
regarding
carbonates,
particularly
terms
better
defining
roles
light,
aragonite
saturation
state,
topography
Ecology Letters,
Год журнала:
2003,
Номер
6(4), С. 281 - 285
Опубликована: Март 13, 2003
Abstract
Biodiversity
is
frequently
associated
with
functional
redundancy.
Indo‐Pacific
coral
reefs
incorporate
some
of
the
most
diverse
ecosystems
on
globe
over
3000
species
fishes
recorded
from
region.
Despite
this
diversity,
we
document
changes
in
ecosystem
function
at
regional
biogeographical
scales
as
a
result
overfishing
just
one
species,
giant
humphead
parrotfish
(
Bolbometopon
muricatum
).
Each
ingests
5
tonnes
structural
reef
carbonates
per
year,
almost
half
being
living
corals.
On
relatively
unexploited
oceanic
reefs,
total
ingestion
rates
m
2
balance
estimated
growth.
However,
human
activity
and
disruption
are
strongly
correlated,
regardless
local
fish
biodiversity.
The
results
emphasize
need
to
consider
role
when
formulating
management
strategies
potential
weakness
link
between
biodiversity
resilience.
Oceanography and Marine Biology/Oceanography and marine biology - an annual review,
Год журнала:
2011,
Номер
unknown
Опубликована: Июнь 22, 2011
Global
warming
and
increased
atmospheric
co2
are
causing
the
oceans
to
warm,
decrease
in
pH
become
hypercapnic.
These
stressors
have
deleterious
impacts
on
marine
inver
-
tebrates.
Increasing
temperature
has
a
pervasive
stimulatory
effect
metabolism
until
lethal
levels
reached,
whereas
hypercapnia
narcotic
effect.
ocean
acidification
is
major
threat
cal
cifying
larvae
because
it
decreases
availability
of
carbonate
ions
required
for
skeletogenesis
also
exerts
direct
physiology.
Marine
invertebrate
propagules
live
multistressor
world
climate
change
adding
mix.
pH,
pco2
caco3
covary
will
simultaneously
with
temperature,
challenging
our
ability
predict
future
outcomes
biota.
To
address
questions
vulnerabilities,
data
thermo-
pH/
tolerance
fertilization
development
invertebrates
reviewed
context
that
forecast
occur
over
next
100-200
years.
Gametes
many
exhibit
broad
beyond
stressor
values
projected
2100.
Available
show
all
stages
highly
sensitive
warming.
may
be
particularly
acidification/hypercapnia.
Embryos
develop
through
bottleneck
mortality
due
succumb
as
acidification.
Early
juveniles
vulnerable
skeletal
dissolution,
although
diminish
negative
impact
acidifi
cation
calcification.
The
effects
their
interaction
differ
among
life
history
species.
Multistressor
experiments
if
thermal
thresholds
breached,
embryos
not
reach
calcifying
stage.
If
species
persistence
embryonic
thermotolerance,
then
question
compromised
calicification
relevant.
limited
knowledge
interactive
gap.
Although
range
invertebrates,
some
regional
faunas
more
resilient
than
others.
This
implica-
tions
persistence,
faunal
shifts,
invasions
community
function
changing
ocean.
Oceanography and Marine Biology/Oceanography and marine biology - an annual review,
Год журнала:
2008,
Номер
unknown, С. 251 - 296
Опубликована: Июнь 5, 2008
Global
climate
change
is
having
devastating
effects
on
habitat
structure
in
coral-reef
ecosystems
owing
to
extreme
environmental
sensitivities
and
consequent
bleaching
of
reef-building
scleractinian
corals.
Coral
frequently
causes
immediate
loss
live
coral
may
lead
longer-term
declines
topographic
complexity.
This
review
identifies
cover
complexity
as
critical
distinct
components
habitats
that
shape
communities
fishes.
has
the
greatest
most
effect
fishes
depend
corals
for
food
or
shelter,
many
such
face
considerable
risk
extinction
with
increasing
frequency
severity
bleaching.
also
have
consequences
require
at
settlement,
which
are
compounded
by
declining
Topographic
moderates
major
biotic
factors,
predation
competition,
contributing
high
diversity
reefs.
Many
do
not
nonetheless
dependent
provided
healthy
growth.
Ecological
economic
likely
be
substantial
compared
selective
but
both
must
recognised
a
component
managed
accordingly.
Urgent
action
fundamental
appropriate
management
elements
(coral
complexity)
key
ensuring
long-term
persistence
Ecological Applications,
Год журнала:
2006,
Номер
16(2), С. 747 - 769
Опубликована: Апрель 1, 2006
Coral
reefs
provide
a
number
of
ecosystem
services
including
coastal
defense
from
storms,
the
generation
building
materials,
and
fisheries.
It
is
increasingly
clear
that
management
reef
resources
requires
an
approach
in
which
extractive
activities
are
weighed
against
needs
its
functions
rather
than
solely
those
fishery.
Here,
I
use
spatially
explicit
simulation
model
Caribbean
coral
to
examine
requirements
for
grazing
primarily
conducted
by
parrotfishes
(Scaridae).
The
allows
impact
fishing
grazers
be
assessed
wider
context
other
processes
coral–algal
competition,
hurricanes,
mass
extinction
herbivorous
urchin
Diadema
antillarum.
Using
new
analytical
scarid
grazing,
it
estimated
can
only
maintain
between
10%
30%
structurally
complex
forereef
grazed
state.
Predictions
this
were
then
incorporated
into
broader
ecosystem.
Simulations
predict
unable
high
levels
cover
(≥30%)
when
severe
hurricanes
occur
on
decadal
basis,
such
as
occurs
parts
northern
Caribbean.
However,
withstand
intense
disturbance
undertaken
both
scarids
Diadema.
Scarid
predicted
allow
recovery
their
incidence
falls
20
years
or
less
(e.g.,
most
Central
South
America).
Sensitivity
analyses
revealed
had
acute
behavior,
depletion
led
emergence
stable,
algal-dominated
community
Under
conditions
heavy
grazer
depletion,
was
decline
rapidly
initial
level
1%
within
40
years,
even
hurricane
frequency
low
at
60
years.
Depleted
caused
population
bottleneck
juvenile
corals
algal
overgrowth
elevated
postsettlement
mortality
resulted
bimodal
distribution
sizes.
Several
hypotheses
generated
region-wide
change
spatial
heterogeneity
following
usually
approached
implicitly
through
no-take
marine
reserves.
predicts
nonreserve
areas
severely
limit
accretion.
Other
studies
have
shown
accretion
reduce
structural
complexity
therefore
quality
habitat
many
organisms.
A
speculative
yet
rational
inference
failure
manage
populations
outside
reserves
will
profoundly
negative
functioning
reserve
system
status
non-reserve
reefs.
Trends in Ecology & Evolution,
Год журнала:
1991,
Номер
6(6), С. 175 - 179
Опубликована: Июнь 1, 1991
Scleractinian
corals
and
their
symbiotic
dinoflagellate
algae
build
massive,
wave-resistant
coral
reefs
that
are
pre-eminent
in
shallow
tropical
seas.
This
mutualism
is
especially
sensitive
to
numerous
environmental
stresses,
has
been
disrupted
frequently
during
the
past
decade.
Increased
seawater
temperatures
have
proposed
as
most
likely
cause
of
reef
bleaching,
it
suggested
recent
large-scale
disturbances
first
biological
indication
global
warming.
article
describes
bleaching
events
possible
link
with
sea
warming
other
offers
some
speculation
on
fate
if
Earth
enters
a
sustained
period