Global Ecology and Biogeography,
Journal Year:
2015,
Volume and Issue:
25(1), P. 75 - 86
Published: Oct. 13, 2015
Abstract
Aim
Ecological
and
evolutionary
forces
shape
the
functional
traits
of
species
within
across
environments,
generating
biogeographical
patterns
in
traits.
We
aimed
to:
(1)
determine
extent
to
which
temperature
phytoplankton
are
adapted
their
local
environment,
(2)
detect
explain
differences
adaptation
between
groups
(reflecting
history)
ecosystems
(freshwater
versus
marine).
Location
used
laboratory‐measured
data
on
strains
isolated
from
marine
(76°
N
75°
S)
freshwater
(80°
78°
S).
Methods
studied
variation
five
traits:
optimum
for
growth
(
T
opt
),
maximum
minimum
persistence
max
,
min
niche
width
rate,
estimated
439
over
200
species.
tested
whether
these
change
along
environmental
gradients
(across
latitude
ecosystems)
also
investigated
trait–environment
relationships
related
history
(functional
group
identity).
mixed
models
evaluate
our
hypotheses
while
accounting
intraspecific
variation.
Results
identified
three
caused
by
community
assembly:
decline
sharply
with
latitude;
similar
all
at
equator,
where
is
low;
(3)
higher
locations
than
latitudes.
Additionally,
explained
substantial
differ
strongly
widths
rates,
as
well
latitude.
Main
conclusions
Globally,
conditions,
changing
Functional
adaptation:
hot
tropical
but
diverge
temperate
These
reflect
two
possible
constraints:
cyanobacterial
inability
adapt
low
temperatures
nutrient
requirements
groups.
Microbiome,
Journal Year:
2019,
Volume and Issue:
7(1)
Published: Oct. 22, 2019
Abstract
Background
The
deep
mechanisms
(deterministic
and/or
stochastic
processes)
underlying
community
assembly
are
a
central
challenge
in
microbial
ecology.
However,
the
relative
importance
of
these
processes
shaping
riverine
microeukaryotic
biogeography
is
still
poorly
understood.
Here,
we
compared
spatiotemporal
and
biogeographical
patterns
using
high-throughput
sequencing
18S
rRNA
gene
multivariate
statistical
analyses
from
subtropical
river
during
wet
dry
seasons.
Results
Our
results
provide
first
description
communities
Tingjiang
River,
largest
west
Fujian
province,
southeastern
China.
showed
that
microeukaryotes
both
seasons
exhibited
contrasting
compositions,
which
might
be
owing
to
planktonic
having
seasonal
succession
patterns.
Further,
all
components
(including
total,
dominant,
always
rare,
conditionally
rare
taxa)
significant
distance-decay
pattern
seasons,
had
stronger
relationship
season,
especially
for
taxa.
Although
several
variables
influence
on
communities,
environmental
spatial
factors
minor
roles
communities.
Importantly,
were
strongly
driven
by
processes,
with
89.9%,
88.5%,
89.6%
variation
explained
neutral
model
wet,
dry,
respectively.
also
large
fraction
across
different
taxonomic
groups
levels.
Additionally,
taxa,
above
below
prediction,
ecologically
taxonomically
distinct
groups,
interactively
structured
deterministic
processes.
Conclusions
This
study
demonstrated
sufficient
substantial
metacommunity
hydrographic
regimes,
thereby
providing
better
understanding
patterns,
waters.
Ecology Letters,
Journal Year:
2016,
Volume and Issue:
20(1), P. 98 - 111
Published: Nov. 27, 2016
Abstract
Winter
conditions
are
rapidly
changing
in
temperate
ecosystems,
particularly
for
those
that
experience
periods
of
snow
and
ice
cover.
Relatively
little
is
known
winter
ecology
these
systems,
due
to
a
historical
research
focus
on
summer
‘growing
seasons’.
We
executed
the
first
global
quantitative
synthesis
under‐ice
lake
ecology,
including
36
abiotic
biotic
variables
from
42
groups
101
lakes,
examining
seasonal
differences
connections
as
well
how
vary
with
geophysical
factors.
Plankton
were
more
abundant
under
than
expected;
mean
values
43.2%
chlorophyll
,
15.8%
phytoplankton
biovolume
25.3%
zooplankton
density.
Dissolved
nitrogen
concentrations
typically
higher
during
winter,
exaggerated
smaller
lakes.
Lake
size
also
influenced
winter‐summer
patterns
dissolved
organic
carbon
(
DOC
),
At
coarse
levels
taxonomic
aggregation,
community
composition
showed
few
systematic
between
seasons,
although
literature
suggests
frequently
lake‐specific,
species‐specific,
or
occur
at
level
functional
group.
Within
subset
lakes
had
longer
time
series,
subsequent
some
nutrient
biomass.
Oxford University Press eBooks,
Journal Year:
2017,
Volume and Issue:
unknown
Published: Oct. 19, 2017
Abstract
The
Biology
of
Lakes
and
Ponds
focuses
on
the
interactions
between
abiotic
frame,
such
as
turbulence,
temperature,
pH
nutrients,
organisms,
including
with
among
organisms
at
individual,
population
community
level.
book
fills
this
niche
traditional
limnology
evolutionary
ecology
by
focusing
physiological,
morphological
behavioural
adaptations
to
biotic
factors
how
processes
constraints
determine
structure
dynamics
lake
pond
systems.
In
addition,
describes
analyses
causes
consequences
human
activities
freshwater
ecosystems
covers
longstanding
environmental
threats,
eutrophication
acidification,
well
novel
biodiversity
loss,
use
everyday
chemicals
global
climate
change.
However,
also
signs
improvement
possibilities
restore
degraded
are
discussed
provide
hope
for
future
generations.
Frontiers in Climate,
Journal Year:
2019,
Volume and Issue:
1
Published: Oct. 11, 2019
Humankind
will
need
to
remove
hundreds
of
gigatons
carbon
dioxide
(CO2)
from
the
atmosphere
by
end
21st
century
keep
global
warming
below
2°
C
within
constraints
budget.
However,
so
far
it
is
unclear
if
and
how
this
could
be
achieved.
A
widely
recognized
idea
accelerate
weathering
reactions
minerals
that
consume
CO2
when
they
dissolve.
Acceleration
realized
pulverizing
distributing
these
onto
land
(termed
"enhanced
(EW)")
or
sea
"ocean
alkalinity
enhancement
(OAE)")
thereby
largely
increasing
their
reactive
surfaces.
desired
consumption
atmospheric
during
dissolution
would
inevitably
accompanied
a
release
mineral
products
(alkalinity,
Si,
Ca,
Mg,
Fe,
Ni
maybe
others).
Here,
we
approximate
maximum
additions
assess
potential
consequences
for
pelagic
communities
(mainly
primary
producers)
biogeochemical
fluxes
control.
Based
on
assessment,
tentatively
qualify
induce
positive
and/or
negative
side
effects
high
Ni,
intermediate
alkalinity,
low
Ca
Mg.
perturbation
potentials
are
always
higher
at
hotspots
different
EW
than
OAE.
Furthermore,
ecological/biogeochemical
EW/OAE
depend
used.
We
hypothesise
mainly
calcifiers
profit
in
scheme
where
CaCO3
derivatives
used
due
beneficial
changes
carbonate
chemistry.
Figuratively,
may
turn
blue
ocean
into
white(r)
ocean.
When
using
silicates,
additional
Fe
benefit
silicifiers
N2-fixers
(cyanobacteria)
increase
productivity
ultimately
turning
green(er)
These
considerations
call
dedicated
research
risks
co-benefits
marine
other
environments.
Indeed,
both
OAE
become
important
tools
realize
removal
planetary
scale
but
associated
should
revealed
before
deciding
implementation.
Freshwater Biology,
Journal Year:
2012,
Volume and Issue:
58(3), P. 463 - 482
Published: Nov. 23, 2012
Summary
1.
Different
components
of
the
climate
system
have
been
shown
to
affect
temporal
dynamics
in
natural
plankton
communities
on
scales
varying
from
days
years.
The
seasonal
temperate
lake
communities,
with
emphasis
both
physical
and
biological
forcing
factors,
were
captured
1980s
a
conceptual
framework,
Plankton
Ecology
Group
(PEG)
model.
2.
Taking
PEG
model
as
our
starting
point,
we
discuss
anticipated
changes
long‐term
extend
this
other
regions,
particularly
polar
tropical
latitudes.
Based
improved
post‐PEG
understanding
dynamics,
also
evaluate
role
microbial
plankton,
parasites
fish
governing
distribution.
3.
In
lakes,
there
is
usually
just
single
peak
biomass
summer.
Lengthening
growing
season
under
warmer
conditions
may
lead
higher
more
prolonged
phytoplankton
productivity.
Climate‐induced
increases
nutrient
loading
these
oligotrophic
waters
contribute
subsequent
zooplankton
4.
pattern
two
peaks
–
spring
summer
can
shift
one
but
longer
larger
increases,
associated
populations
zooplanktivorous
fish.
Climate
change
will
exacerbate
trends
by
increasing
through
increased
internal
inputs
(due
warming)
catchment
(in
case
precipitation).
5.
systems,
variability
precipitation
be
an
important
driver
development
plankton.
Increases
intensity
reset
favour
species
adapted
highly
variable
environments.
existing
intense
predation
zooplankters
increase
further,
resulting
perennially
low
biomass.
6.
Bacteria
not
included
original
Seasonally,
bacteria
vary
less
than
often
follow
its
patterns,
colder
lakes.
future
warming,
greater
influx
allochthonous
carbon
obscure
pattern.
7.
Our
analyses
indicate
that
consequences
for
are,
large
extent,
specific,
depending
characteristics
such
food‐web
structure
loading.
Indirect
effects
direct
temperature
increase,
especially
phytoplankton.
However,
warming
general
picture
emerges
bacterivory,
cyanobacterial
dominance
smaller‐bodied
are
heavily
impacted
predation.
Ecosphere,
Journal Year:
2015,
Volume and Issue:
6(1), P. 1 - 19
Published: Jan. 1, 2015
Here
we
draw
attention
to
the
potential
for
pelagic
bloom‐forming
cyanobacteria
have
substantial
effects
on
nutrient
cycling
and
ecosystem
resilience
across
a
wide
range
of
lakes.
Specifically,
hypothesize
that
cyanobacterial
blooms
can
influence
lake
cycling,
resilience,
regime
shifts
by
tapping
into
pools
nitrogen
(N)
phosphorus
(P)
not
usually
accessible
phytoplankton.
The
ability
many
taxa
fix
dissolved
N
2
gas
is
well‐known
source
N,
but
some
also
access
P
in
sediments
bottom
waters.
Both
these
nutrients
be
released
water
column
via
leakage
or
mortality,
thereby
increasing
availability
other
phytoplankton
microbes.
Moreover,
are
restricted
high
(eutrophic)
lakes:
occur
lakes
with
low
concentrations,
suggesting
changes
mediated
could
affect
gradient
concentrations.
We
used
simple
model
coupled
cycles
explore
dynamics
resilience.
Consistent
our
hypothesis,
parameters
reflecting
modification
alter
number,
location,
and/or
stability
equilibria.
In
particular,
demonstrates
low‐nutrient
conditions
facilitate
shift
high‐nutrient
state
reducing
state.
This
suggests
warrant
as
drivers
transition
from
low‐nutrient,
clear‐water
high‐nutrient,
turbid‐water
regime,
prediction
particular
concern
given
such
reported
regions
world
due
part
global
climate
change.
Journal of Phycology,
Journal Year:
2014,
Volume and Issue:
50(3), P. 437 - 461
Published: April 4, 2014
Algae
have
been
used
for
a
century
in
environmental
assessments
of
water
bodies
and
are
now
countries
around
the
world.
This
review
synthesizes
recent
advances
field
framework
assessment
management
that
can
guide
design
assessments,
applications
phycology
refinements
those
to
better
support
decisions.
critical
parts
aquatic
ecosystems
power
food
webs
biogeochemical
cycling.
also
major
sources
problems
threaten
many
goods
services
when
abundances
nuisance
toxic
taxa
high.
Thus,
algae
be
indicate
ecosystem
services,
which
complements
how
algal
indicators
assess
levels
contaminants
habitat
alterations
(stressors).
Understanding
managers'
use
ecology,
taxonomy,
physiology
our
research
improve
its
application.
Environmental
involve
characterizing
ecological
condition
diagnosing
causes
threats
services.
Recent
include
site‐specific
models
account
natural
variability
among
habitats
estimate
effects
humans.
Relationships
between
assemblages
stressors
caused
by
humans
help
diagnose
establish
targets
protection
restoration.
Many
responses
thresholds
particularly
important
developing
stakeholder
consensus
stressor
targets.
Future
on
regional‐scale
resilience
assemblages,
they
provide,
methods
monitoring
forecasting
change
will
resource
management.