Molecular Biology and Evolution,
Journal Year:
2020,
Volume and Issue:
38(3), P. 927 - 939
Published: Oct. 3, 2020
Abstract
A
major
challenge
in
modern
biology
is
understanding
how
the
effects
of
short-term
biological
responses
influence
long-term
evolutionary
adaptation,
defined
as
a
genetically
determined
increase
fitness
to
novel
environments.
This
particularly
important
globally
microbes
experiencing
rapid
global
change,
due
their
on
food
webs,
biogeochemical
cycles,
and
climate.
Epigenetic
modifications
like
methylation
have
been
demonstrated
plastic
responses,
which
ultimately
impact
adaptive
environmental
change.
However,
there
remains
paucity
empirical
research
examining
dynamics
during
adaptation
nonmodel,
ecologically
microbes.
Here,
we
show
first
evidence
marine
prokaryote
for
m5C
methylome
correlated
with
phenotypic
CO2,
using
7-year
evolution
experiment
(1,000+
generations)
biogeochemically
cyanobacterium
Trichodesmium.
We
identify
methylated
sites
that
rapidly
changed
response
high
(750
µatm)
CO2
exposure
were
maintained
at
least
4.5
years
selection.
After
7
selection,
however,
levels
initially
responded
high-CO2
returned
ancestral,
ambient
levels.
Concurrently,
adapted
growth
N2
fixation
rates
remained
significantly
higher
than
those
cell
lines
irrespective
concentration,
trend
consistent
genetic
assimilation
theory.
These
data
demonstrate
maintenance
CO2-responsive
alongside
before
returning
ancestral
observations
distributed
provide
critical
insights
into
traits
under
Journal of Experimental Botany,
Journal Year:
2017,
Volume and Issue:
68(14), P. 3701 - 3716
Published: March 14, 2017
CO2-concentrating
mechanisms
(CCMs),
based
either
on
active
transport
of
inorganic
carbon
(biophysical
CCMs)
or
biochemistry
involving
supplementary
fixation
into
C4
acids
(C4
and
CAM),
play
a
major
role
in
global
primary
productivity.
However,
the
ubiquitous
CO2-fixing
enzyme
autotrophs,
Rubisco,
evolved
at
time
when
atmospheric
CO2
levels
were
very
much
higher
than
today
O2
was
low
and,
as
approached
(by
no
means
monotonically),
today's
levels,
some
subsequently
many
organisms
CCM
that
increased
supply
decreased
Rubisco
oxygenase
activity.
Given
other
environmental
factors
have
altered
considerably
between
autotrophs
present
day,
are
predicted
to
continue
change
future,
we
here
examine
drivers
for,
possible
timing
of,
evolution
CCMs.
CCMs
probably
fell
2-16
times
level,
depending
kinetics.
We
also
assess
effects
key
such
temperature
nutrient
activity
evidence
for
evolutionary
changes
related
cellular
processes
well
limitations
continuity
through
variations.
Frontiers in Marine Science,
Journal Year:
2019,
Volume and Issue:
6
Published: Feb. 12, 2019
Trait-based
approaches
to
investigate
(short-
and
long-term)
phytoplankton
dynamics
community
assembly
have
become
increasingly
popular
in
freshwater
marine
science.
Although
the
nature
of
pelagic
habitat
main
taxa
ecology
are
relatively
similar
both
systems,
lines
research
evolved,
at
least
part,
separately.
We
compare
contrast
adopted
ecosystems
with
respect
functional
traits.
note
differences
study
goals
relating
trait
use
that
assess
those
relate
ecosystem
processes
biogeochemical
cycling
affect
type
characteristics
assigned
as
traits
taxa.
Specific
relevant
for
ecological
function
examined
relation
herbivory,
amplitude
environmental
change
spatial
temporal
scales
study.
Major
identified,
including
shorter
time
scale
regular
compared
open
oceans
well
sampling
done
by
researchers
based
on
site-accessibility.
Overall,
we
encourage
researcher
better
motivate,
why
they
apply
trait-based
analyses
their
studies
make
process-driven
approaches,
which
more
common
studies.
further
propose
fully
comparative
conducted
along
gradient
spanning
brackish
systems
or
geographic
gradients.
Such
will
benefit
from
combined
strength
fields.
Journal of Plankton Research,
Journal Year:
2017,
Volume and Issue:
unknown
Published: Jan. 3, 2017
Eukaryotic
phytoplankton
exhibit
an
enormous
species
richness,
displaying
a
range
of
phylogenetic,
morphological
and
physiological
diversity.
Yet,
until
recently,
very
little
was
known
about
the
diversity,
genetic
variation
evolutionary
processes
within
populations.
An
approach
to
explore
this
diversity
understand
evolution
is
use
population
genetics
as
conceptual
framework
methodology.
Here,
we
discuss
patterns,
questions
that
studies
have
revealed
in
eukaryotic
phytoplankton.
First,
describe
main
biological
generating
variation.
We
specifically
importance
life-cycle
complexity
for
phenotypic
consider
how
such
can
be
maintained
during
blooms
when
rapid
asexual
proliferation
dominates.
Next,
partitioned
over
time
space,
with
focus
on
shaping
structure,
particular
selection
exchange.
Our
aim
also
show
used
make
inferences
realized
dispersal
sexual
recombination,
these
are
so
difficult
study
directly.
Finally,
highlight
important
open
suggest
promising
avenues
future
will
made
possible
by
new
sequencing
technologies.
Scientific Reports,
Journal Year:
2018,
Volume and Issue:
8(1)
Published: Dec. 5, 2018
Abstract
Ocean
warming
with
climate
change
is
forcing
marine
organisms
to
shift
their
distributions
polewards
and
phenology.
In
warm
tropical
seas,
evolutionary
adaptation
by
local
species
will
be
crucial
avoid
predicted
desertification
reduction
in
diversity.
However,
little
known
about
the
of
phytoplankton
seas.
Across
ocean,
diatomic
microalgae
are
main
primary
producers
cold
waters;
they
also
contribute
communities
where
play
a
necessary
role
biological
pump.
Here
we
show
that
four
diatoms
isolated
from
Red
Sea
adapted
conditions
(30
°C)
after
200–600
generations
using
various
thermal
strategies.
Two
increased
optimal
growth
temperature
(
T
opt
)
maximum
rate.
The
other
two
did
not
increase
growth,
but
shifted
specialist
generalist
increasing
critical
limit.
Our
data
can
adapt
warming,
although
trade
offs
on
photosynthetic
efficiency,
high
irradiance
stress,
lower
rate
could
alter
competitive
fitness.
findings
suggest
adaptive
responses
among
help
arrest
sharp
decline
diversity
resulting
for
waters.
Proceedings of the Royal Society A Mathematical Physical and Engineering Sciences,
Journal Year:
2020,
Volume and Issue:
476(2237)
Published: May 1, 2020
Surface
ocean
biogeochemistry
and
photochemistry
regulate
ocean–atmosphere
fluxes
of
trace
gases
critical
for
Earth's
atmospheric
chemistry
climate.
The
oceanic
processes
governing
these
are
often
sensitive
to
the
changes
in
pH
(or
p
CO
2
)
accompanying
acidification
(OA),
with
potential
future
climate
feedbacks.
Here,
we
review
current
understanding
(from
observational,
experimental
model
studies)
on
impact
OA
marine
sources
key
climate-active
gases,
including
dimethyl
sulfide
(DMS),
nitrous
oxide
(N
O),
ammonia
halocarbons.
We
focus
DMS,
which
available
information
is
considerably
greater
than
other
gases.
highlight
OA-sensitive
regions
such
as
polar
oceans
upwelling
systems,
discuss
combined
effect
multiple
stressors
(ocean
warming
deoxygenation)
gas
fluxes.
To
unravel
biological
mechanisms
responsible
production,
detect
adaptation,
propose
combining
process
rate
measurements
longer
term
experiments
using
both
organisms
laboratory
natural
planktonic
communities
field.
Future
observations
should
be
routinely
accompanied
by
two
components
carbonate
system
improve
our
how
situ
influences
production.
Together,
this
will
lead
improvements
capabilities
more
reliable
predictions
global
Frontiers in Marine Science,
Journal Year:
2021,
Volume and Issue:
7
Published: Jan. 25, 2021
The
oceans’
uptake
of
anthropogenic
carbon
dioxide
(CO
2
)
decreases
seawater
pH
and
alters
the
inorganic
speciation
–
summarized
in
term
ocean
acidification
(OA).
Already
today,
coastal
regions
experience
episodic
events
during
which
surface
layer
drops
below
values
projected
for
at
end
century.
Future
OA
is
expected
to
further
enhance
intensity
these
extreme
events.
To
evaluate
influence
such
regions,
we
deployed
eight
pelagic
mesocosms
53
days
Raunefjord,
Norway,
enclosed
56–61
m
3
local
containing
a
natural
plankton
community
under
nutrient
limited
post-bloom
conditions.
Four
were
enriched
with
CO
simulate
p
levels
1978
2069
μatm
while
other
four
served
as
untreated
controls.
Here,
present
results
from
multivariate
analyses
on
OA-induced
changes
phyto-,
micro-,
mesozooplankton
structure.
Pronounced
differences
emerged
early
experiment,
amplified
by
enhanced
top-down
control
throughout
study
period.
groups
responding
most
profoundly
high
conditions
cyanobacteria
(negative),
chlorophyceae
auto-
heterotrophic
microzooplankton
variety
mesozooplanktonic
taxa,
including
copepoda
(mixed),
appendicularia
(positive),
hydrozoa
fish
larvae
gastropoda
(negative).
restructuring
coincided
significant
concentration
elemental
stoichiometry
particulate
organic
matter.
Results
imply
that
can
lead
substantial
reorganization
planktonic
food
web,
affecting
multiple
trophic
phytoplankton
primary
secondary
consumers.
Proceedings of the National Academy of Sciences,
Journal Year:
2022,
Volume and Issue:
119(19)
Published: May 6, 2022
Significance
Coccolithophore
calcification
is
a
major
ocean
biogeochemical
process.
While
this
process
likely
to
be
sensitive
acidification-driven
changes
in
carbonate
chemistry,
incomplete
understanding
of
the
underlying
mechanisms
and
constraints
bottleneck
predicting
acidification
effects
on
calcification.
We
report
severe
disruption
pH
homeostasis
linked
loss
H
+
channel
function
coccolithophore
Coccolithus
braarudii
acclimated
seawater
values
that
are
encountered
currently
localized
regions
more
widely
future
oceans.
This
leads
specific
defects
coccolith
morphology.
These
findings
provide
mechanistic
insight
into
how
different
coccolithophores
affected
by
chemistry.