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.
Nature Climate Change,
Journal Year:
2023,
Volume and Issue:
13(4), P. 389 - 396
Published: March 23, 2023
Climate
change
interacts
with
local
processes
to
threaten
biodiversity
by
disrupting
the
complex
network
of
ecological
interactions.
While
changes
in
interactions
drastically
affect
ecosystems,
how
networks
respond
climate
change,
particular
warming
and
nutrient
supply
fluctuations,
is
largely
unknown.
Here,
using
an
equation-free
modelling
approach
on
monthly
plankton
community
data
ten
Swiss
lakes,
we
show
that
number
strength
fluctuate
nonlinearly
water
temperature
phosphorus.
lakes
system-specific
responses,
generally
reduces
interactions,
particularly
under
high
phosphate
levels.
This
reorganization
shifts
trophic
control
food
webs,
leading
consumers
being
controlled
resources.
Small
grazers
cyanobacteria
emerge
as
sensitive
indicators
networks.
By
exposing
outcomes
a
interplay
between
environmental
drivers,
our
results
provide
tools
for
studying
advancing
understanding
impacts
entire
communities.
ISME Communications,
Journal Year:
2025,
Volume and Issue:
5(1)
Published: Jan. 1, 2025
Abstract
The
interplay
between
abiotic
(resource
supply,
temperature)
and
biotic
(grazing)
factors
determines
growth
loss
processes
in
phytoplankton
through
resource
competition
trophic
interactions,
which
are
mediated
by
morphological
traits
like
size.
Here,
we
study
the
relative
importance
of
grazers,
water
physics,
chemistry
on
daily
net
accumulation
rates
(ARs)
individual
from
natural
communities,
grouped
into
six
size
classes
circa
10
to
500
μm.
Using
a
Random
Forest
modelling
approach
4
years
data
lake,
find
that
temperature
is
generally
pivotal
control
all
ARs.
At
same
time,
nutrients
light
important
for
smallest
largest
classes.
Mesozooplankton
abundance
key
predictor
AR
small
phytoplankton,
with
microzooplankton
being
middle-size
range.
In
our
data,
large
have
different
(seasonal)
blooming
patterns:
forms
favoured
low
grazing,
high
phosphorus
levels.
Larger
show
positive
ARs
at
temperatures
(being
relatively
insensitive
zooplankton
grazing).
These
results
help
us
understand
opportunities
limitations
using
explain
model
responses
environmental
change.
Limnology and Oceanography,
Journal Year:
2014,
Volume and Issue:
59(6), P. 2185 - 2202
Published: Oct. 12, 2014
Temperature
of
the
surface
layer
temperate
lakes
is
reconstructed
by
means
a
simplified
model
on
basis
air
temperature
alone.
The
comparison
between
calculated
and
observed
data
shows
remarkable
agreement
(Nash–Sutcliffe
efficiency
indices
always
larger
than
0.87,
mean
absolute
errors
approximately
1°C)
for
all
14
investigated
(Mara,
Sparkling,
Superior,
Michigan,
Huron,
Erie,
Ontario,
Biel,
Zurich,
Constance,
Garda,
Neusiedl,
Balaton,
Baikal,
in
west‐to‐east
order),
which
present
wide
range
morphological
hydrological
characteristics.
Differently
from
pure
heat
flux
balance
approach,
where
different
fluxes
are
determined
independent
relationships,
input
directly
inform
parameters
simple
that,
turn,
provides
meaningful
information
about
properties
real
system.
dependence
main
indicators
presented,
allows
quantitative
description
strong
influence
depth
lake
thermal
inertia
hysteresis
pattern
temperatures.
Remote Sensing of Environment,
Journal Year:
2015,
Volume and Issue:
158, P. 441 - 452
Published: Jan. 2, 2015
Phytoplankton
biomass
is
important
to
monitor
in
lakes
due
its
influence
on
water
quality
and
lake
productivity.
has
also
been
identified
as
sensitive
environmental
change,
with
shifts
the
seasonality
of
blooms,
or
phenology,
resulting
from
changing
temperature
nutrient
conditions.
A
satellite
remote
sensing
approach
retrieving
mapping
freshwater
phytoplankton
phenology
demonstrated
here
application
Lake
Balaton,
Hungary.
Chlorophyll-a
(chl-a)
concentration
using
Medium
Resolution
Imaging
Spectrometer
(MERIS)
allows
new
insights
into
such
spatiotemporal
dynamics
for
Balaton
bloom
start,
peak
end
timing,
duration,
maximum
chl-a
concentrations,
spatial
extent,
rates
increase
decrease,
integral.
TIMESAT
software
used
extract
map
these
metrics.
Three
approaches
time
series
smoothing
are
compared
mapped
metrics
evaluated
comparison
situ
chl-a.
The
high
degree
both
temporal
variability
highlighted
discussed,
methodological
limitations
correlation
between
Both
feasibility
novel
permitted
through
demonstrated,
priority
topics
future
research
suggested.
Biogeosciences,
Journal Year:
2018,
Volume and Issue:
15(9), P. 2649 - 2668
Published: May 4, 2018
Abstract.
The
Chesapeake
Bay
region
is
projected
to
experience
changes
in
temperature,
sea
level,
and
precipitation
as
a
result
of
climate
change.
This
research
uses
an
estuarine-watershed
hydrodynamic–biogeochemical
modeling
system
along
with
mid-21st-century
freshwater
flow,
level
rise
explore
the
impact
change
may
have
on
future
dissolved-oxygen
(DO)
concentrations
potential
success
nutrient
reductions
attaining
mandated
estuarine
water
quality
improvements.
Results
indicate
that
warming
bay
waters
will
decrease
oxygen
solubility
year-round,
while
also
increasing
utilization
via
respiration
remineralization,
primarily
impacting
bottom
spring.
Rising
increase
circulation,
reducing
residence
time
stratification.
As
result,
are
increase,
at
mid-depths
(3
<
DO
5
mg
L−1)
typically
decrease.
Changes
deliver
higher
winter
spring
flow
loads,
fueling
increased
primary
production.
Together,
these
multiple
impacts
lower
throughout
negatively
progress
towards
meeting
standards
associated
Total
Maximum
Daily
Load.
However,
this
shows
be
significantly
smaller
than
improvements
expected
response
required
reductions,
especially
anoxic
hypoxic
levels.
Overall,
temperature
exhibits
strongest
control
concentrations,
due
decreased
solubility,
exert
small
positive
river
anticipated
negative
impact.