Global Biogeochemical Cycles,
Год журнала:
2016,
Номер
30(7), С. 1038 - 1053
Опубликована: Май 27, 2016
Abstract
Ocean
acidification
and
decreasing
seawater
saturation
state
with
respect
to
calcium
carbonate
(CaCO
3
)
minerals
have
raised
concerns
about
the
consequences
marine
organisms
that
build
CaCO
structures.
A
large
proportion
of
benthic
calcifiers
incorporate
Mg
2+
into
their
skeletons
(Mg‐calcite),
which,
in
general,
reduces
mineral
stability.
The
relative
vulnerability
some
ocean
appears
linked
solubility
shell
or
skeletal
mineralogy,
although
sophisticated
mechanisms
for
constructing
maintaining
structures
causing
deviation
from
this
dependence.
Nevertheless,
few
studies
consider
actual
Mg‐calcite
mineralogy
(Ω
Mg‐
x
a
species
when
evaluating
effect
on
species.
Here,
global
dataset
mole
%
MgCO
situ
environmental
conditions
spanning
depth
range
0
m
(subtidal/neritic)
5600
(abyssal)
was
assembled
calculate
Ω
.
This
analysis
shows
24%
studied
currently
experience
undersaturation
<
1).
As
result
ongoing
anthropogenic
over
next
200
3000
years,
predicted
decrease
will
expose
approximately
57%
all
calcifying
undersaturation.
These
observations
reveal
surprisingly
high
exposed
is
undersaturated
underscoring
importance
using
species‐specific
states
investigating
impact
CO
2
‐induced
calcification.
Proceedings of the National Academy of Sciences,
Год журнала:
2017,
Номер
114(37)
Опубликована: Авг. 28, 2017
Significance
Whether
coral
skeleton
crystals
grow
by
attachment
of
ions
from
solution
or
particles
tissue
determines
(
i
)
corals’
growth
rate,
ii
how
they
survive
acidifying
oceans,
and
iii
the
isotopes
in
used
for
reconstructing
ancient
temperatures.
Our
data
show
that
two
amorphous
precursors
exist,
one
hydrated
dehydrated
calcium
carbonate;
these
are
formed
as
∼400-nm
particles;
attach
to
surface
skeletons,
remain
hours,
finally
crystallize
into
aragonite.
Since
inside
tissue,
may
be
less
susceptible
ocean
acidification
than
previously
assumed.
Coral
bleaching
postmortem
dissolution
will
occur,
but
a
calcification
crisis
not.
Transcriptome
and
genome
data
from
twenty
stony
coral
species
a
selection
of
reference
bilaterians
were
studied
to
elucidate
evolutionary
history.
We
identified
genes
that
encode
the
proteins
responsible
for
precipitation
aggregation
aragonite
skeleton
on
which
organisms
live,
revealed
network
environmental
sensors
coordinate
responses
host
animals
temperature,
light,
pH.
Furthermore,
we
describe
variety
stress-related
pathways,
including
apoptotic
pathways
allow
detoxify
reactive
oxygen
nitrogen
are
generated
by
their
intracellular
photosynthetic
symbionts,
determine
fate
corals
under
stress.
Some
these
arose
through
horizontal
gene
transfer
comprise
at
least
0.2%
animal
inventory.
Our
analysis
elucidates
strategies
have
allowed
symbiotic
adapt
thrive
hundreds
millions
years.
Calcium
carbonate
(CaCO
3
)
biomineralizing
organisms
have
played
major
roles
in
the
history
of
life
and
global
carbon
cycle
during
past
541
Ma.
Both
marine
diversification
mass
extinctions
reflect
physiological
responses
to
environmental
changes
through
time.
An
integrated
understanding
biomineralization
is
necessary
illuminate
this
evolutionary
record
understand
how
modern
will
respond
21st
century
change.
Biomineralization
evolved
independently
but
convergently
across
phyla,
suggesting
a
unity
mechanism
that
transcends
biological
differences.
In
review,
we
combine
CaCO
skeleton
formation
mechanisms
with
constraints
from
history,
omics,
meta-analysis
isotopic
data
develop
plausible
model
for
applicable
all
phyla.
The
provides
framework
sensitivity
calcifiers,
extinctions,
resilience
acidifying
oceans.
Thus,
it
frames
questions
about
past,
present,
future
organisms.
Cell,
Год журнала:
2021,
Номер
184(11), С. 2973 - 2987.e18
Опубликована: Май 1, 2021
Stony
corals
are
colonial
cnidarians
that
sustain
the
most
biodiverse
marine
ecosystems
on
Earth:
coral
reefs.
Despite
their
ecological
importance,
little
is
known
about
cell
types
and
molecular
pathways
underpin
biology
of
reef-building
corals.
Using
single-cell
RNA
sequencing,
we
define
over
40
across
life
cycle
Stylophora
pistillata.
We
discover
specialized
immune
cells,
uncover
developmental
gene
expression
dynamics
calcium-carbonate
skeleton
formation.
By
simultaneously
measuring
transcriptomes
cells
algae
within
them,
characterize
metabolic
programs
involved
in
symbiosis
both
partners.
also
trace
evolution
these
specializations
by
phylogenetic
integration
multiple
cnidarian
type
atlases.
Overall,
this
study
reveals
cellular
basis
stony
biology.
Nature Communications,
Год журнала:
2017,
Номер
8(1)
Опубликована: Май 30, 2017
Abstract
Coral
calcification
is
dependent
on
the
mutualistic
partnership
between
endosymbiotic
zooxanthellae
and
coral
host.
Here,
using
newly
developed
geochemical
proxies
(δ
11
B
B/Ca),
we
show
that
Porites
corals
from
natural
reef
environments
exhibit
a
close
(
r
2
∼0.9)
antithetic
relationship
dissolved
inorganic
carbon
(DIC)
pH
of
corals’
calcifying
fluid
(cf).
The
highest
DIC
cf
(∼
×
3.2
seawater)
found
during
summer,
consistent
with
thermal/light
enhancement
metabolically
(zooxanthellae)
derived
carbon,
while
(∼8.5)
occurs
in
winter
periods
low
seawater).
These
opposing
changes
are
shown
to
maintain
oversaturated
but
stable
levels
carbonate
saturation
Ω
∼
5
seawater),
key
parameter
controlling
calcification.
findings
marked
contrast
artificial
experiments
upregulation
largely
independent
seawater
chemistry,
hence
ocean
acidification,
highly
vulnerable
thermally
induced
stress
global
warming.
Stony
corals
form
the
foundation
of
coral
reef
ecosystems.
Their
phylogeny
is
characterized
by
a
deep
evolutionary
divergence
that
separates
into
robust
and
complex
clade
dating
back
to
at
least
245
mya.
However,
genomic
consequences
clade-specific
evolution
remain
unexplored.
In
this
study
we
have
produced
genome
coral,
Stylophora
pistillata,
compared
it
available
Acropora
digitifera.
We
conducted
fine-scale
gene-based
analysis
focusing
on
ortholog
groups.
Among
core
set
conserved
proteins,
found
an
emphasis
processes
related
cnidarian-dinoflagellate
symbiosis.
Genes
associated
with
algal
symbiosis
were
also
independently
expanded
in
both
species,
but
diverged
identity
groups
expanded,
uneven
expansions
genes
innate
immunity
stress
response.
Our
analyses
demonstrate
genomes
can
be
surprisingly
disparate.
Future
incorporating
more
data
should
able
determine
whether
patterns
elucidated
here
are
not
only
characteristic
differences
between
S.
pistillata
A.
digitifera
representative
from
large.
Nature Communications,
Год журнала:
2016,
Номер
7(1)
Опубликована: Апрель 4, 2016
Abstract
Reliably
predicting
how
coral
calcification
may
respond
to
ocean
acidification
and
warming
depends
on
our
understanding
of
mechanisms.
However,
the
concentration
speciation
dissolved
inorganic
carbon
(DIC)
inside
corals
remain
unclear,
as
only
pH
has
been
measured
while
a
necessary
second
parameter
constrain
carbonate
chemistry
missing.
Here
we
report
first
ion
([CO
3
2−
])
measurements
together
with
during
light
period.
We
observe
sharp
increases
in
[CO
]
from
gastric
cavity
calcifying
fluid,
confirming
existence
proton
(H
+
)
pumping
mechanism.
also
show
that
can
achieve
high
aragonite
saturation
state
(
Ω
arag
fluid
by
elevating
at
same
time
keeping
[DIC]
low.
Such
mechanism
require
less
H
-pumping
energy
for
upregulating
compared
scenario
thus
allow
be
more
resistant
climate
change
related
stressors.