Abstract.
Abrupt
changes
in
ocean
biogeochemical
variables
occur
as
a
result
of
human-induced
climate
forcing
well
those
which
are
more
gradual
and
over
longer
timescales.
These
abrupt
have
not
yet
been
identified
quantified
to
the
same
extent
ones.
We
review
synthesise
biogeochemistry
under
climatic
forcing.
specifically
address
carbon
oxygen
cycles
because
related
processes
acidification
deoxygenation
provide
important
ecosystem
hazards.
Since
depend
also
on
physical
environment,
we
describe
relevant
warming,
circulation,
sea
ice.
include
an
overview
reversibility
or
irreversibility
marine
changes.
Important
implications
for
ecosystems
discussed.
conclude
that
there
is
evidence
increasing
occurrence
consequence
rising
greenhouse
gas
emissions.
Proceedings of the National Academy of Sciences,
Journal Year:
2023,
Volume and Issue:
120(12)
Published: March 13, 2023
Arctic
rivers
provide
an
integrated
signature
of
the
changing
landscape
and
transmit
signals
change
to
ocean.
Here,
we
use
a
decade
particulate
organic
matter
(POM)
compositional
data
deconvolute
multiple
allochthonous
autochthonous
pan-Arctic
watershed-specific
sources.
Constraints
from
carbon-to-nitrogen
ratios
(C:N),
δ13C,
Δ14C
signatures
reveal
large,
hitherto
overlooked
contribution
aquatic
biomass.
Separation
in
age
is
enhanced
by
splitting
soil
sources
into
shallow
deep
pools
(mean
±
SD:
-228
211
vs.
-492
173‰)
rather
than
traditional
active
layer
permafrost
(-300
236
-441
215‰)
that
do
not
represent
permafrost-free
regions.
We
estimate
39
60%
(5
95%
credible
interval)
annual
POM
flux
(averaging
4,391
Gg/y
carbon
2012
2019)
comes
The
remainder
sourced
yedoma,
soils,
petrogenic
inputs,
fresh
terrestrial
production.
Climate
change-induced
warming
increasing
CO2
concentrations
may
enhance
both
destabilization
river
biomass
production,
fluxes
Younger,
autochthonous,
older
soil-derived
likely
have
different
destinies
(preferential
microbial
uptake
processing
significant
sediment
burial,
respectively).
A
small
(~7%)
increase
with
would
be
equivalent
~30%
flux.
There
clear
need
better
quantify
how
balance
endmember
shift
ramifications
for
endmembers
this
will
impact
system.
Earth s Future,
Journal Year:
2024,
Volume and Issue:
12(4)
Published: April 1, 2024
Abstract
Mercury
(Hg)
is
a
naturally
occurring
element
that
has
been
greatly
enriched
in
the
environment
by
human
activities
like
mining
and
fossil
fuel
combustion.
Despite
commonalities
some
carbon
dioxide
(CO
2
)
Hg
emission
sources,
implications
of
long‐range
climate
scenarios
for
anthropogenic
emissions
have
yet
to
be
explored.
Here,
we
present
comprehensive
projections
extending
year
2300
evaluate
impacts
on
global
atmospheric
deposition.
Projections
are
based
four
Shared
Socioeconomic
Pathways
(SSPs)
ranging
from
sustainable
reductions
resource
energy
intensity
rapid
economic
growth
driven
abundant
exploitation.
There
greater
than
two‐fold
difference
cumulative
between
lower‐bound
(110
Gg)
upper‐bound
(235
scenarios.
releases
land
water
approximately
six
times
those
direct
air
(600–1,470
Gg).
At
their
peak,
reach
2,200–2,600
Mg
−1
sometime
2010
(baseline)
2030,
depending
SSP
scenario.
Coal
combustion
largest
determinant
differences
among
Decoupling
CO
sources
occurs
under
low‐to
mid‐range
scenarios,
though
contributions
artisanal
small‐scale
gold
remain
uncertain.
Future
may
lower
gaseous
elemental
(Hg
0
higher
divalent
II
),
resulting
fraction
locally
sourced
Projected
reemissions
previously
deposited
follow
similar
temporal
trajectory
primary
emissions,
amplifying
benefits
most
stringent
mitigation
Humans
have
intentionally
mined
and
released
mercury
(Hg)
from
the
Earth's
lithosphere
over
millennia.
Here,
we
synthesize
past,
present,
future
anthropogenic
Hg
emissions
releases
use
a
global
geochemical
box
model
to
characterize
accumulation
in
atmosphere,
land,
ocean.
We
project
an
upper-bound
for
between
2010
2300
(Shared
Socioeconomic
Pathway
(SSP)5-8.5;
1.7
Tg)
that
surpasses
historical
total
past
half
millennium
(1.5
Tg).
In
contrast,
lower-bound
(SSP1-2.6;
0.7
is
substantially
smaller
than
total.
Observational
constraints
on
modeling
suggest
most
land
water
prior
remains
sequestered
at
contaminated
sites.
Substantial
oceanic
enrichment
by
(270%
ca.
2010)
has
been
driven
mainly
atmospheric
emissions.
Cumulative
are
projected
be
approximately
six-times
greater
primary
atmosphere.
This
legacy
waste
pools
unlikely
impact
pollution
ocean
unless
it
mobilized
climate
change.
Modeling
results
2100
concentrations
may
similar
present
levels
if
society
follows
SSP5-8.5.
Declines
surface
(-19%)
atmosphere
(-45%)
expected
under
SSP1-2.6,
emphasizing
benefits
of
reductions
releases.
Environmental Pollution,
Journal Year:
2023,
Volume and Issue:
338, P. 122706 - 122706
Published: Oct. 9, 2023
The
Northeast
Arctic
cod
(Gadus
morhua)
is
the
world's
northernmost
stock
of
Atlantic
and
considerable
ecological
economic
importance.
are
widely
distributed
in
Barents
Sea,
an
environment
that
supports
a
high
degree
ecosystem
resiliency
food
web
complexity.
Here
using
121
years
ocean
temperature
data
(1900-2020),
41
sea
ice
extent
information
(1979-2020)
27
total
mercury
(Hg)
fillet
concentration
(1994-2021,
n
=
1999,
≥71%
Methyl
Hg,
20)
from
Sea
ecosystem,
we
evaluate
effects
climate
change
dynamics
on
Hg
temporal
trends
cod.
We
observed
low
consistently
stable,
concentrations
(yearly,
least-square
means
range
0.022-0.037
mg/kg
wet
wt.)
length-normalized
fish,
with
slight
decline
most
recent
sampling
periods
despite
significant
increase
temperature,
sharp
regional
extent.
Overall,
our
suggest
amplification
"Atlantification,"
other
perturbations
along
rapidly
declining
over
last
∼30
did
not
translate
into
major
increases
or
decreases
bioaccumulation
Our
findings
consistent
similar
long-term,
assessments
inhabiting
Oslofjord,
Norway,
investigations
empirical
for
marine
apex
predators.
This
demonstrates
highly
context
specific,
some
species
may
be
as
sensitive
to
current
change-contaminant
interactions
currently
thought.
Fish
bioaccumulation-climate
relationships
complex
uniform,
predators
can
vary
considerably
within
among
species,
geographically.
regimes
biota
nuanced
likely
driven
by
suite
factors
such
local
diets,
sources
bioenergetics,
toxicokinetic
processing,
growth
metabolic
rates
individuals
taxa,
inputs
anthropogenic
activities
at
varying
spatiotemporal
scales.
Collectively,
these
have
important
policy
implications
global
security,
Minamata
Convention
Mercury,
several
relevant
UN
Sustainable
Development
Goals.
Abstract.
Abrupt
changes
in
ocean
biogeochemical
variables
occur
as
a
result
of
human-induced
climate
forcing
well
those
which
are
more
gradual
and
over
longer
timescales.
These
abrupt
have
not
yet
been
identified
quantified
to
the
same
extent
ones.
We
review
synthesise
biogeochemistry
under
climatic
forcing.
specifically
address
carbon
oxygen
cycles
because
related
processes
acidification
deoxygenation
provide
important
ecosystem
hazards.
Since
depend
also
on
physical
environment,
we
describe
relevant
warming,
circulation,
sea
ice.
include
an
overview
reversibility
or
irreversibility
marine
changes.
Important
implications
for
ecosystems
discussed.
conclude
that
there
is
evidence
increasing
occurrence
consequence
rising
greenhouse
gas
emissions.