Ecology,
Journal Year:
2017,
Volume and Issue:
98(4), P. 982 - 994
Published: Feb. 1, 2017
Abstract
Global
change
has
increased
inorganic
nitrogen
(N)
and
dissolved
organic
carbon
(
DOC
;
i.e.,
“browning”)
inputs
to
northern
hemisphere
boreal
lakes.
However,
we
do
not
know
how
phytoplankton
in
nutrient
poor
lake
ecosystems
of
different
concentration
respond
N
availability.
Here,
monitored
changes
production,
biomass
community
composition
response
whole
fertilization
six
unproductive
Swedish
lakes
divided
into
three
pairs
(control,
enriched)
at
levels
(low,
medium,
high),
with
one
reference
year
(2011)
2
impact
yr
(2012,
2013).
We
found
that
production
decreased
before
fertilization.
Further,
also
differed
respect
,
a
dominance
non‐flagellated
autotrophs
low
towards
an
increasing
flagellated
concentration.
The
all
lakes,
but
did
affect
composition.
the
net
declined
implying
is
critical
order
infer
responses
fertilization,
system
switches
from
being
primarily
limited
becoming
increasingly
light
In
conclusion,
our
results
show
browning
will
reduce
influence
composition,
whereas
loadings
deposition,
forestry
or
other
land
use
enhance
production.
Together,
any
landscape
enhances
availability
increase
biomass,
positive
effects
be
much
weaker
even
neutralized
browner
as
caused
by
limitation.
Global Change Biology,
Journal Year:
2018,
Volume and Issue:
24(8), P. 3692 - 3714
Published: March 15, 2018
Northern
ecosystems
are
experiencing
some
of
the
most
dramatic
impacts
global
change
on
Earth.
Rising
temperatures,
hydrological
intensification,
changes
in
atmospheric
acid
deposition
and
associated
acidification
recovery,
vegetative
cover
resulting
fundamental
terrestrial–aquatic
biogeochemical
linkages.
The
effects
readily
observed
alterations
supply
dissolved
organic
matter
(DOM)—the
messenger
between
terrestrial
lake
ecosystems—with
potentially
profound
structure
function
lakes.
contain
substantial
stores
filter
or
funnel
DOM,
affecting
timing
magnitude
DOM
delivery
to
surface
waters.
This
is
processed
streams,
rivers,
lakes,
ultimately
shifting
its
composition,
stoichiometry,
bioavailability.
Here,
we
explore
potential
consequences
these
change-driven
for
food
webs
at
northern
latitudes.
Notably,
provide
evidence
that
increased
allochthonous
lakes
overwhelming
autochthonous
results
from
earlier
ice-out
a
longer
growing
season.
Furthermore,
assess
implications
this
shift
nutritional
quality
autotrophs
terms
their
fatty
toxin
production,
methylmercury
concentration,
therefore,
contaminant
transfer
through
web.
We
conclude
regions
leads
not
only
reduced
primary
productivity
but
also
nutritionally
poorer
webs,
with
discernible
trophic
web
fish
humans.
AMBIO,
Journal Year:
2019,
Volume and Issue:
49(2), P. 375 - 390
Published: July 31, 2019
Browning
of
surface
waters,
as
a
result
increasing
dissolved
organic
carbon
and
iron
concentrations,
is
widespread
phenomenon
with
implications
to
the
structure
function
aquatic
ecosystems.
In
this
article,
we
provide
an
overview
consequences
browning
in
relation
ecosystem
services,
outline
what
underlying
drivers
mechanisms
are,
specifically
focus
on
exploring
potential
mitigation
measures
locally
counteract
browning.
These
topical
concepts
are
discussed
Scandinavia,
but
relevance
also
other
regions.
environmental
concern
it
leads
to,
e.g.,
costs
risks
for
drinking
water
production,
reduced
fish
production
lakes
by
limiting
light
penetration.
While
climate
change,
recovery
from
acidification,
land-use
change
all
likely
factors
contributing
observed
browning,
managing
land
use
hydrologically
connected
parts
landscape
may
be
most
feasible
way
natural
waters.
Frontiers in Marine Science,
Journal Year:
2020,
Volume and Issue:
7
Published: June 23, 2020
The
marine
dissolved
organic
carbon
(DOC)
pool
is
an
important
player
in
the
functioning
of
ecosystems.
DOC
at
interface
between
chemical
and
biological
worlds,
it
fuels
food
webs,
a
major
component
Earth's
system.
Here,
we
review
research
showing
impacts
global
change
stressors
on
cycling,
specifically:
ocean
warming
stratification,
acidification,
deoxygenation,
glacial
sea
ice
melting,
changed
inflow
from
rivers,
changing
circulation
upwelling,
wet/dry
deposition.
A
unified
outcome
future
these
production
degradation
not
possible,
due
to
regional
differences
impacts,
but
general
patterns
for
each
stressor
are
presented.
The Science of The Total Environment,
Journal Year:
2022,
Volume and Issue:
824, P. 153715 - 153715
Published: Feb. 9, 2022
Dramatic
environmental
shifts
are
occuring
throughout
the
Arctic
from
climate
change,
with
consequences
for
cycling
of
mercury
(Hg).
This
review
summarizes
latest
science
on
how
change
is
influencing
Hg
transport
and
biogeochemical
in
terrestrial,
freshwater
marine
ecosystems.
As
changes
continue
to
accelerate,
a
clearer
picture
emerging
profound
cryosphere,
their
connections
cycling.
Modeling
results
suggest
influences
seasonal
interannual
variability
atmospheric
deposition.
The
clearest
evidence
current
effects
terrestrial
catchments,
where
widespread
permafrost
thaw,
glacier
melt
coastal
erosion
increasing
export
downstream
environments.
Recent
estimates
large
global
reservoir
Hg,
which
vulnerable
degradation
warming,
although
fate
soil
unclear.
development
thermokarst
features,
formation
expansion
thaw
lakes,
increased
landscapes
river
particulate-bound
altering
conditions
aquatic
transformations.
Greater
organic
matter
may
also
be
Hg.
More
severe
frequent
wildfires
within
across
boreal
regions
contributing
pool
Climate
remain
poorly
understood.
Seasonal
evasion
retention
inorganic
altered
by
reduced
sea-ice
cover
higher
chloride
content
snow.
Experimental
indicates
warmer
temperatures
enhance
methylmercury
production
ocean
lake
sediments
as
well
tundra
soils.
Improved
geographic
coverage
measurements
modeling
approaches
needed
better
evaluate
net
long-term
implications
contamination
Arctic.
Limnology and Oceanography Letters,
Journal Year:
2017,
Volume and Issue:
2(4), P. 105 - 112
Published: June 5, 2017
Abstract
Observations
of
increasing
water
color
and
organic
carbon
concentrations
in
lakes
are
widespread
across
the
Northern
Hemisphere.
The
drivers
these
trends
debated.
Declining
atmospheric
sulfur
deposition
has
been
put
forward
as
an
important
underlying
factor,
since
recovery
from
acidification
enhances
mobility
matter
surrounding
soils.
This
would
suggest
that
current
browning
represents
a
return
to
more
natural
state.
study
explores
historical
lake
data
Sweden—1935
2015—providing
unique
opportunity
see
how
why
varied
during
almost
century.
shows
not
primary
driver
over
this
period.
I
propose
observed
is
large
extent
driven
by
major
transition
agriculture
forestry.
Limnology and Oceanography Letters,
Journal Year:
2018,
Volume and Issue:
3(3), P. 76 - 88
Published: Feb. 19, 2018
Abstract
Understanding
what
controls
the
lateral
flux
of
organic
and
inorganic
carbon
from
landscapes
to
surface
waters
is
key
fully
understanding
terrestrial
ecosystem
balances,
biogeochemistry
freshwaters,
how
hydrologically‐mediated
movement
between
these
ecosystems
may
be
altered
by
global
change.
In
this
paper,
we
synthesize
current
knowledge
identify
major
gaps
in
our
land‐to‐water
fluxes
dissolved
particulate
carbon,
CO
2
,
bicarbonate
exploring:
(1)
variations
soil
stocks
affect
gaseous
production
profile
transport
via
terrestrial‐aquatic
flow
paths,
(2)
effect
change
on
fluxes.
Our
aim
develop
a
roadmap
guide
future
research
linkages
cycle
within
context
changes
climate,
biogeochemical
cycles,
land
use.
Global Change Biology,
Journal Year:
2019,
Volume and Issue:
25(6), P. 2021 - 2029
Published: March 21, 2019
Global
change
affects
terrestrial
loadings
of
colored
dissolved
organic
carbon
(DOC)
and
nutrients
to
northern
lakes.
Still,
little
is
known
about
how
phytoplankton
respond
changes
in
light
nutrient
availability
across
gradients
lake
DOC.
In
this
study,
we
used
results
from
whole-lake
studies
Sweden
show
that
annual
mean
biomass
expressed
unimodal
curved
relationships
DOC
gradients,
peaking
at
threshold
levels
around
11
mg/L.
Whole-lake
single
enrichment
selected
lakes
caused
elevated
biomass,
with
most
pronounced
effect
the
level.
These
patterns
give
support
suggested
dual
control
by
on
via
(positively)
(negatively)
imply
lakes'
location
along
axis
critical
determining
what
extent
and/or
loadings.
By
using
data
large
Swedish
Lake
Monitoring
Survey,
further
estimated
80%
are
below
threshold,
potentially
experiencing
increased
browning
alone,
combined
enrichment.
The
previous
model
effects
eutrophication
phytoplankton,
provide
important
understanding
may
future
global
changes.
Scientific Reports,
Journal Year:
2019,
Volume and Issue:
9(1)
Published: Nov. 13, 2019
Abstract
Dissolved
organic
carbon
(DOC)
concentrations
and
water
colour
are
increasing
in
many
inland
waters
across
northern
Europe
northeastern
North
America.
This
inland-water
“browning”
has
profound
physical,
chemical
biological
repercussions
for
aquatic
ecosystems
affecting
quality,
community
structures
productivity.
Potential
drivers
of
this
trend
complex
include
reductions
atmospheric
acid
deposition,
changes
land
use/cover,
increased
nitrogen
deposition
climate
change.
However,
because
the
overlapping
impacts
these
stressors,
their
relative
contributions
to
DOC
dynamics
remain
unclear,
without
appropriate
long-term
monitoring
data,
it
not
been
possible
determine
whether
ongoing
is
unprecedented
or
simply
a
“re-browning”
pre-industrial
levels.
Here,
we
demonstrate
change
on
lake-water
low
high
acid-deposition
areas
using
infrared
spectroscopic
techniques
~200-year-long
lake-sediment
records
from
central
Canada.
We
show
that
suppressed
naturally
higher
during
20th
century,
but
lakes
now
occurring
with
emissions
formerly
areas.
In
contrast,
areas,
forcing
towards
new
ecological
states,
as
often
exceed