Abstract.
Lakes
experience
anthropogenically-forced
changes
that
may
initiate
ecosystem
feedbacks,
in
some
cases
reaching
tipping
points
beyond
which
impacts
become
hard
to
reverse.
are
also
important
players
the
global
climate
by
ventilating
a
large
share
of
terrestrial
carbon
back
atmosphere
as
greenhouse
gases,
and
will
likely
provide
substantial
feedbacks
change.
In
this
paper
we
address
various
major
lake
ecosystems,
discuss
if
can
be
identified,
predicted,
or
prevented
them,
along
with
their
associated
Potential
dynamics
assessed
include
eutrophication-driven
anoxia
internal
phosphorus-loading,
increased
loading
organic
matter
from
ecosystems
(lake
“browning”),
formation
disappearance
response
cryosphere
shifts,
switching
nitrogen
phosphorus
limitation,
salinization,
spread
invasive
species.
We
other
types
abrupt,
threshold-type
shifts
lakes
ponds,
conclude
on
locally
regionally
relevant.
identify
key
set
co-drivers
could
lead
self-sustaining
warming,
browning,
eutrophication
leading
stratification,
heterotrophy,
algal
mass,
separately
collectively
drive
benthic
oxygen
depletion
turn
gas
emissions
(helping
further
warming
loading)
phosphorus-loading
(driving
eutrophication).
Several
these
processes
feature
points,
make
easier
reach.
argue
full
importance
vulnerability
anthropogenic
impacts,
well
feedback
is
not
yet
fully
acknowledged,
so
there
need
both
for
science
communication
regard.
Nature,
Journal Year:
2023,
Volume and Issue:
621(7979), P. 530 - 535
Published: Aug. 16, 2023
Methane
(CH4)
is
a
potent
greenhouse
gas
and
its
concentrations
have
tripled
in
the
atmosphere
since
industrial
revolution.
There
evidence
that
global
warming
has
increased
CH4
emissions
from
freshwater
ecosystems1,2,
providing
positive
feedback
to
climate.
Yet
for
rivers
streams,
controls
magnitude
of
remain
highly
uncertain3,4.
Here
we
report
spatially
explicit
estimate
running
waters,
accounting
27.9
(16.7-39.7)
Tg
per
year
roughly
equal
those
other
systems5,6.
Riverine
are
not
strongly
temperature
dependent,
with
low
average
activation
energy
(EM
=
0.14
eV)
compared
lakes
wetlands
0.96
eV)1.
By
contrast,
patterns
characterized
by
large
fluxes
high-
low-latitude
settings
as
well
human-dominated
environments.
These
explained
edaphic
climate
features
linked
anoxia
near
fluvial
habitats,
including
high
supply
organic
matter
water
saturation
hydrologically
connected
soils.
Our
results
highlight
importance
land-water
connections
regulating
which
vulnerable
only
direct
human
modifications
but
also
several
change
responses
on
land.
Global Biogeochemical Cycles,
Journal Year:
2023,
Volume and Issue:
37(5)
Published: April 26, 2023
Abstract
Inland
waters
are
important
emitters
of
the
greenhouse
gasses
(GHGs)
carbon
dioxide
(CO
2
),
methane
(CH
4
and
nitrous
oxide
(N
O)
to
atmosphere.
In
framework
2nd
phase
REgional
Carbon
Cycle
Assessment
Processes
(RECCAP‐2)
initiative,
we
review
state
art
in
estimating
inland
water
GHG
budgets
at
global
scale,
which
has
substantially
advanced
since
first
RECCAP
nearly
10
years
ago.
The
development
increasingly
sophisticated
upscaling
techniques,
including
statistical
prediction
process‐based
models,
allows
for
spatially
explicit
estimates
that
needed
regionalized
assessments
continental
such
as
those
established
RECCAP.
A
few
recent
also
resolve
seasonal
and/or
interannual
variability
emissions.
Nonetheless,
global‐scale
assessment
emissions
remains
challenging
because
limited
spatial
temporal
coverage
observations
persisting
uncertainties
abundance
distribution
surface
areas.
To
decrease
these
uncertainties,
more
empirical
work
on
contributions
hot‐spots
hot‐moments
overall
is
particularly
needed.
Limnology and Oceanography,
Journal Year:
2024,
Volume and Issue:
69(4), P. 861 - 873
Published: Feb. 22, 2024
Abstract
Rivers
significantly
contribute
to
global
biogeochemical
cycles;
however,
we
have
a
limited
understanding
of
how
drying
may
influence
these
cycles.
Drying
fragments
river
networks,
thereby
influencing
important
ecosystem
functions
such
as
the
processing
carbon
and
nitrogen,
associated
fluxes
greenhouse
gases
(GHGs)
both
locally,
at
network
scale.
Our
objective
was
assess,
using
network‐scale
approach,
lateral,
longitudinal,
temporal
dynamics
GHG
in
naturally
fragmented
by
drying.
We
used
closed‐loop
chamber
with
automated
analyzers
measure
dioxide
(CO
2
),
methane
(CH
4
nitrous
oxide
(N
O)
from
dry
sediments,
flowing
waters,
isolated
pools,
riparian
soils,
along
suite
environmental
variables,
over
9
months
20
sites
across
non‐perennial
France.
Network‐scale
had
spatial
legacy
effect
on
fluxes.
On
average,
CO
were
up
29
times
higher
perennial
than
under
conditions.
At
sites,
N
O
positively
covaried
time
since
rewetting.
In
addition,
percent
reaches
upstream,
indicating
soil
riverbed
sediments
markedly
different
magnitudes
covariates.
This
research
demonstrates
that
not
only
has
local‐scale
impact
but
also
influences
scale,
contributing
valuable
insights
for
upscaling
riverine
estimates.
Earth System Dynamics,
Journal Year:
2024,
Volume and Issue:
15(3), P. 653 - 669
Published: May 27, 2024
Abstract.
Lakes
and
ponds
experience
anthropogenically
forced
changes
that
may
be
non-linear
sometimes
initiate
ecosystem
feedbacks
leading
to
tipping
points
beyond
which
impacts
become
hard
reverse.
In
many
cases
climate
change
is
a
key
driver,
in
concert
with
other
stressors.
are
also
important
players
the
global
by
ventilating
large
share
of
terrestrial
carbon
(C)
back
atmosphere
as
greenhouse
gases
will
likely
provide
substantial
change.
this
paper
we
address
various
major
lake
ecosystems
discuss
if
can
identified,
predicted,
or
prevented,
well
drivers
associated
We
focus
on
potential
large-scale
effects
regional
widespread
impacts,
such
eutrophication-driven
anoxia
internal
phosphorus
(P)
loading,
increased
loading
organic
matter
from
(lake
“browning”),
formation
disappearance
response
cryosphere
shifts
precipitation
evaporation
ratios,
switching
nitrogen
limitation,
salinization,
spread
invasive
species
where
threshold-type
occur.
identify
systems
could
lead
self-sustaining
feedbacks,
abrupt
changes,
some
degree
resilience,
opposed
binary
states
not
subject
self-propelling
resilience.
Changes
driven
warming,
browning,
eutrophication
cause
stratification,
heterotrophy
(browning),
phytoplankton
macrophyte
mass
(eutrophication),
separately
collectively
drive
benthic
oxygen
depletion
turn
increase
gas
(GHG)
emissions.
Several
these
processes
feature
point
thresholds,
further
warming
make
easier
surpass.
argue
full
importance
vulnerability
lakes
anthropogenic
their
feedback
climate,
yet
fully
acknowledged,
so
there
need
both
for
science
communication
regard.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(6), P. 1613 - 1628
Published: March 28, 2024
Abstract.
Greenhouse
gas
(GHG)
emissions
from
rivers
are
globally
relevant,
but
quantification
of
these
comes
with
considerable
uncertainty.
Quantification
ecosystem-scale
is
challenged
by
both
spatial
and
short-term
temporal
variability.
We
measured
spatio-temporal
variability
CO2
CH4
fluxes
a
1
km
long
reach
the
lowland
river
Elbe
in
Germany
over
3
d
to
establish
which
factor
more
relevant
be
taken
into
consideration:
small-scale
or
fluxes.
GHG
studied
were
dominated
CO2,
90
%
total
water
surface,
while
10
dry
fallen
sediment
at
side
river.
Aquatic
similar
different
habitats,
aquatic
higher
Artificial
structures
improve
navigability
(groynes)
created
still
areas
elevated
lower
exhibited
clear
diurnal
pattern,
exact
shape
timing
this
pattern
differed
between
habitats.
By
contrast,
did
not
change
diurnally.
Our
data
confirm
our
hypothesis
that
especially
important
for
CH4,
study
summer.
Continuous
measurements
least
sampling
times
day
most
likely
necessary
reliable
emissions.
Freshwater Biology,
Journal Year:
2023,
Volume and Issue:
68(12), P. 2027 - 2041
Published: Sept. 19, 2023
Abstract
River
fragmentation
by
drying
and
damming
is
occurring
more
frequently
in
the
Anthropocene
era,
yet
there
limited
knowledge
of
how
this
influences
greenhouse
gas
(GHG)
fluxes
river
networks.
networks
have
potential
to
be
important
sources
GHGs
atmosphere
through
both
similar
dissimilar
mechanisms
associated
with
temporary
(drying)
permanent
(damming)
fragmentation.
We
conducted
a
review
literature
found
49,
43
six
studies
about
(CO
2
,
CH
4
N
O)
rivers
impacted
damming,
their
interaction,
respectively.
research
lacking
non‐arid
climates
small
water‐retention
structures
for
regarding
The
major
factors
directly
influencing
GHG
were
sediment
moisture,
temperature,
organic
matter
content
texture.
In
most
influential
water
dissolved
oxygen,
phytoplankton
Chlorophyll‐
.
Based
on
our
meta‐ecosystem
theory,
we
propose
that
spatial
distribution
strongly
at
river‐network
scale.
actionable
future
directions
identified
here
will
help
improve
understanding
effects
fluxes,
inform
management
climate
change
mitigation
strategies.
Restoration Ecology,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Feb. 10, 2025
Sphagnum
mosses
are
vital
to
bog
ecosystems
and
are,
therefore,
target
species
for
peatland
restoration
paludiculture.
Their
establishment
relies
on
consistent
wet
conditions
adequate
nutrient
supply.
However,
extreme
climatic
events,
such
as
prolonged
droughts,
threaten
establishment.
To
better
understand
the
effects
of
water
table
fluctuations
different
species,
we
conducted
a
field
experiment
with
stable
fluctuating
conditions.
After
1
year,
measured
cover,
lawn
height
(as
proxy
growth),
carbon
(C)
accumulation,
stoichiometry
12
species.
Our
results
show
that
facilitated
growth
during
Nitrogen
(N)
potassium
(K)
N
phosphorus
(P)
quotients
were
higher
in
capitula
biomass
treatment.
We
identified
two
clusters
species:
cluster
1,
characterized
by
low
N:K
quotient
C
accumulation—indicating
strong
potential—included
palustre
,
S.
fallax
fimbriatum
riparium
denticulatum
.
In
contrast,
2
exhibited
lower
accumulation—suggesting
vulnerability
environmental
changes
establishment—included
fuscum
centrale
magellanicum
papillosum
rubellum
austinii
squarrosum
indicate
particularly
promising
candidates
rapid
under
dry
Even
when
exposed
shortages,
paludiculture
can
promote
fast‐track
accumulation.