PLoS ONE,
Journal Year:
2016,
Volume and Issue:
11(5), P. e0155952 - e0155952
Published: May 25, 2016
Concerns
about
increasing
atmospheric
CO2
concentrations
and
global
warming
have
initiated
studies
on
the
consequences
of
multiple-stressor
interactions
marine
organisms
ecosystems.
We
present
a
fully-crossed
factorial
mesocosm
study
assess
how
acidification
affect
abundance,
body
size,
fatty
acid
composition
copepods
as
measure
nutritional
quality.
The
experimental
set-up
allowed
us
to
determine
whether
effects
act
additively,
synergistically,
or
antagonistically
content
copepods,
major
group
lower
level
consumers
in
food
webs.
Copepodite
(developmental
stages
1–5)
nauplii
abundance
were
affected
by
acidification.
Higher
temperature
decreased
copepodite
while
partially
compensated
for
effect.
adult
was
negatively
warming.
prosome
length
significantly
reduced
warming,
interaction
length.
Fatty
also
saturated
acids
increased,
ratios
polyunsaturated
essential
docosahexaenoic-
(DHA)
arachidonic
(ARA)
total
increased
with
higher
temperatures.
Additionally,
here
significant
additive
effect
both
parameters
acid.
Our
results
indicate
that
future
ocean
scenario,
might
counteract
some
observed
zooplankton,
adding
others.
These
may
be
fertilizing
phytoplankton
copepod
source.
In
summary,
populations
will
more
strongly
rather
than
acidifying
oceans,
but
can
modify
impacts.
Annual Review of Marine Science,
Journal Year:
2013,
Volume and Issue:
6(1), P. 167 - 194
Published: Oct. 1, 2013
Nutrient
and
light
conditions
control
phytoplankton
division
rates
in
the
surface
ocean
and,
it
is
commonly
believed,
dictate
when
where
high
concentrations,
or
blooms,
of
plankton
occur.
Yet
after
a
century
investigation,
biomass
accumulation
show
no
correlation
with
cell
rates.
Consequently,
factors
controlling
blooms
remain
highly
controversial.
In
this
review,
we
endorse
view
that
are
not
governed
by
abiotic
division,
but
rather
reflect
subtle
ecosystem
imbalances
instigated
climate
forcings
food-web
shifts.
The
annual
global
procession
thus
represents
report
on
recent
history
predator-prey
interactions
modulated
physical
processes
that,
almost
coincidentally,
also
nutrient
inputs.
European Journal of Phycology,
Journal Year:
2014,
Volume and Issue:
49(1), P. 20 - 46
Published: Jan. 2, 2014
The
partitioning
of
organic
matter
(OM)
between
dissolved
and
particulate
phases
is
an
important
factor
in
determining
the
fate
carbon
ocean.
Dissolved
(DOM)
release
by
phytoplankton
a
ubiquitous
process,
resulting
2–50%
fixed
photosynthesis
leaving
cell.
This
loss
can
be
divided
into
two
components:
passive
leakage
diffusion
across
cell
membrane
active
exudation
DOM
surrounding
environment.
At
present
there
no
method
to
distinguish
whether
released
via
or
exudation.
Most
explanations
for
remain
hypothetical;
as
while
has
been
measured
extensively,
relatively
little
work
determine
why
released.
Further
research
needed
composition
link
physiological
status
environmental
conditions.
For
example,
causes
physiology
death
are
poorly
understood,
though
increases
permeability
presumably
release.
Recent
shown
that
interactions
with
bacteria
both
amount
In
response
increasing
CO2
atmosphere,
climate
change
creating
increasingly
stressful
conditions
surface
ocean,
including
warm
water,
low
pH,
nutrient
supply
high
light.
As
ocean
physics
chemistry
change,
it
hypothesized
greater
proportion
primary
production
will
directly
water
DOM.
Changes
have
bottom-up
effects
on
ecosystem
structure
function.
There
need
how
these
changes
affect
particularly
efficiency
biological
pump.
Global Change Biology,
Journal Year:
2014,
Volume and Issue:
21(4), P. 1395 - 1406
Published: Nov. 10, 2014
Abstract
Estuaries
and
coastal
seas
provide
valuable
ecosystem
services
but
are
particularly
vulnerable
to
the
co‐occurring
threats
of
climate
change
oxygen‐depleted
dead
zones.
We
analyzed
severity
predicted
for
existing
zones,
found
that
94%
zones
in
regions
will
experience
at
least
a
2
°C
temperature
increase
by
end
century.
then
reviewed
how
exacerbate
hypoxic
conditions
through
oceanographic,
ecological,
physiological
processes.
evidence
suggests
numerous
variables
including
temperature,
ocean
acidification,
sea‐level
rise,
precipitation,
wind,
storm
patterns
affect
each
those
factors
has
potential
act
multiple
pathways
on
both
oxygen
availability
ecological
responses
hypoxia.
Given
variety
strength
mechanisms
which
exacerbates
hypoxia,
rates
is
changing,
we
posit
contributing
zone
epidemic
acting
synergistically
with
one
another
recognized
anthropogenic
triggers
hypoxia
eutrophication.
This
multidisciplinary,
integrated
approach
considers
full
range
needed
track
potentially
reverse
spread
Cambridge University Press eBooks,
Journal Year:
2015,
Volume and Issue:
unknown, P. 271 - 360
Published: Jan. 7, 2015
The
topics
assessed
in
this
chapter
were
last
by
the
IPCC
2007,
principally
WGII
AR4
Chapters
3
(Kundzewicz
et
al.,
2007)
and
4
(Fischlin
2007),
but
also
Sections
1.3.4
1.3.5
(Rosenzweig
2007).
SPM
stated
"Observational
evidence
from
all
continents
most
oceans
shows
that
many
natural
systems
are
being
affected
regional
climate
changes,
particularly
temperature
increases,"
though
they
noted
documentation
of
observed
changes
tropical
regions
Southern
Hemisphere
was
sparse
Fischlin
al.
(2007)
found
20
to
30%
plant
animal
species
had
been
time
considered
be
at
increased
risk
extinction
if
global
average
increase
exceeds
2°C
3°C
above
preindustrial
level
with
medium
confidence,
substantial
structure
functioning
terrestrial,
marine,
other
aquatic
ecosystems
very
likely
under
degree
warming
associated
atmospheric
CO2
concentration.
No
scale
these
findings.
carbon
stocks
terrestrial
high
change
land
use
change.
report
warned
capacity
adapt
naturally
combined
effect
stressors
is
exceeded
greenhouse
gas
(GHG)
emission
continued
or
then-current
rate.
PLoS ONE,
Journal Year:
2015,
Volume and Issue:
10(6), P. e0130053 - e0130053
Published: June 15, 2015
Essential
fatty
acids
(EFA),
which
are
primarily
generated
by
phytoplankton,
limit
growth
and
reproduction
in
diverse
heterotrophs.
The
biochemical
composition
of
phytoplankton
is
well-known
to
be
governed
both
phylogeny
environmental
conditions.
Nutrients,
light,
salinity,
temperature
all
affect
acid
composition.
However,
the
relative
importance
taxonomy
environment
on
algal
content
has
yet
comparatively
quantified,
thus
inhibiting
predictions
changes
food
quality
response
global
change.
We
compiled
1145
published
marine
freshwater
profiles,
consisting
208
species
from
six
major
taxonomic
groups,
cultured
a
wide
range
conditions,
used
multivariate
distance-based
linear
model
quantify
total
variation
explained
each
variable.
Our
results
show
that
group
accounts
for
3-4
times
more
than
most
important
condition
variables.
underscore
conditions
clearly
but
also
account
relatively
low
compared
phylogeny.
This
suggests
underlying
mechanism
determining
basal
aquatic
habitats
community
composition,
allows
prediction
environmental-scale
EFA
dynamics
based
data.
dataset
calculate
seasonal
long-chain
(LCEFA;
≥C20
ɷ-3
ɷ-6
polyunsaturated
acid)
concentrations
ɷ-3:ɷ-6
ratios
Lake
Washington
using
multi-decadal
time
series.
These
analyses
temporal
algal-derived
LCEFA
ecosystem
undergone
large
as
result
shifting
resource
management
practices,
highlighting
diatoms,
cryptophytes
dinoflagellates
key
sources
LCEFA.
Moreover,
indicate
future
shifts
towards
cyanobacteria-dominated
communities
will
lower
ecosystems.
Freshwater Biology,
Journal Year:
2014,
Volume and Issue:
60(4), P. 603 - 619
Published: Dec. 1, 2014
Summary
Ecologists
often
group
organisms
based
on
similar
biological
traits
or
taxonomic
criteria.
However,
the
use
of
taxonomy
in
ecology
has
many
drawbacks
because
taxa
may
include
species
with
very
different
ecological
adaptations.
Further,
characters
evolve
independently
lineages.
In
this
review,
we
examine
main
criteria
that
have
been
used
identification
nine
modes
classifying
phytoplankton
non‐taxonomically.
These
approaches
are
purely
morphological
and/or
structural
traits,
more
complex
combinations
including
physiological
and
features.
Different
functional
proved
able
to
explain
some
fraction
variance
observed
spatial
temporal
distribution
patterns
algal
assemblages,
although
their
effectiveness
varies
greatly,
depending
number
characteristics
used.
The
attribution
single
broad
groups
allowed
a
few
classifications
(e.g.
Functional
Groups
,
FG
)
be
assessment
status.
We
stress
misuse
(by
applying
them
under
conditions
other
than
those
intended)
can
serious
consequences
for
interpreting
processes.
Assigning
cannot
considered
surrogate
knowledge
ecotypes,
specific
must
always
justified
circumscribed
within
limits
questions
hypotheses.
An
important
future
challenge
will
integrate
advances
molecular
genetics,
metabolomics
physiology
conventional
traits;
form
basis
next
generation
classifications.
PLoS ONE,
Journal Year:
2013,
Volume and Issue:
8(6), P. e66475 - e66475
Published: June 12, 2013
Marine
ecosystems
are
undergoing
substantial
changes
due
to
human-induced
pressures.
Analysis
of
long-term
data
series
is
a
valuable
tool
for
understanding
naturally
and
anthropogenically
induced
in
plankton
communities.
In
the
present
study,
seasonal
monitoring
were
collected
three
sub-basins
northern
Baltic
Sea
between
1979
2011
statistically
analysed
trends
interactions
surface
water
hydrography,
inorganic
nutrient
concentrations
phyto-
zooplankton
community
composition.
The
most
conspicuous
hydrographic
change
was
significant
increase
late
summer
temperatures
over
study
period.
addition,
salinity
decreased
dissolved
increased
some
basins.
Based
on
redundancy
analysis
(RDA),
warming
key
environmental
factor
explaining
observed
communities:
general
total
phytoplankton
biomass,
Cyanophyceae,
Prymnesiophyceae
Chrysophyceae,
decrease
Cryptophyceae
throughout
area,
as
well
rotifers
zooplankton,
cladoceran
copepod
abundances
We
conclude
that
communities
have
shifted
towards
food
web
structure
with
smaller
sized
organisms,
leading
energy
available
grazing
planktivorous
fish.
shift
probably
complex
warming,
eutrophication
top-down
pressure
overexploitation
resources,
resulting
trophic
cascades.
Evolutionary Applications,
Journal Year:
2013,
Volume and Issue:
7(1), P. 140 - 155
Published: Nov. 25, 2013
Abstract
Marine
phytoplankton
have
many
obvious
characters,
such
as
rapid
cell
division
rates
and
large
population
sizes,
that
give
them
the
capacity
to
evolve
in
response
global
change
on
timescales
of
weeks,
months
or
decades.
However,
few
studies
directly
investigate
if
this
adaptive
potential
is
likely
be
realized.
Because
this,
evidence
whether
how
marine
may
sparse.
Here,
we
review
help
predict
evolutionary
responses
phytoplankton.
We
find
limited
support
from
experimental
evolution
some
taxa
adapt
ocean
acidification,
strong
indications
variation
structure
natural
populations
selection
standing
genetic
likely.
Furthermore,
highlight
body
literature
plastic
acidification
available,
theory
used
link
responses.
taxonomic
breadth
spanned
by
phytoplankton,
diversity
roles
they
fill
ecosystems
biogeochemical
cycles,
stress
necessity
treating
functional
groups
individually.