Elementa Science of the Anthropocene,
Journal Year:
2024,
Volume and Issue:
12(1)
Published: Jan. 1, 2024
The
stable
isotope
compositions
of
water
(δ18O,
δ2H,
deuterium-excess)
are
important
tracers
that
help
illuminate
the
changing
Arctic
cycle
and
how
Arctic-sourced
can
influence
lower
latitudes.
We
present
simultaneous
boundary
layer
vapor
ocean
data
were
measured
continuously
in
western
Ocean.
Sea
surface
isotopes
varied
between
shallower
continental
Chukchi
Shelf
deeper
Borderlands
to
north.
waters
less
saline
than
offshore
Shelf,
as
influenced
by
greater
sea
ice
cover
contribution
melt
freshwater.
This
resulted
deuterium-excess
(δ2H
−
8*δ18O)
values
on
Shelf.
Additionally,
contributions
freshwater
prominent
river
runoff,
but
from
both
sources
decreased
substantially
below
70
m
depth
Borderlands.
Our
observed
provided
foundation
for
producing
maps
(isoscapes)
based
remote
sensing
machine
learning
which
incorporate
parameters
circulation
thus
(e.g.,
salinity,
temperature,
depth).
These
isoscapes
suggest
spatial
complexity
distribution
Arctic,
including
sharp
gradients
seawater
studied.
be
improved
future
iterations,
example,
with
availability
more
spatially
continuous,
remotely
sensed
oceanic
variables
or
continuous
ship-based
measurements
use
additional
predictors.
As
a
result,
generation
these
could
become
useful
tool
understanding
past,
present,
context
global
hydrologic
cycle.
Journal of Quaternary Science,
Journal Year:
2023,
Volume and Issue:
38(7), P. 991 - 1024
Published: Aug. 23, 2023
ABSTRACT
To
reconstruct
past
environmental
changes,
a
range
of
indirect
or
proxy
approaches
can
be
applied
to
Quaternary
archives.
Here,
we
review
the
complementary
and
novel
insights
that
have
been
provided
by
analysis
chemical
fossils
(biomarkers).
Biomarkers
biological
source
highly
specific
(e.g.
produced
small
group
organisms)
more
general.
We
show
biomarkers
are
able
quantify
key
climate
variables
(particularly
water
air
temperature)
provide
qualitative
evidence
for
changes
in
hydrology,
vegetation,
human–environment
interactions
biogeochemical
cycling.
In
many
settings,
biomarker
proxies
opportunity
simultaneously
multiple
variables,
alongside
long‐established
palaeoenvironmental
reconstruction.
Multi‐proxy
studies
rich
sets
data
explore
both
drivers
impacts
change.
As
new
continue
developed
refined,
there
is
further
potential
answer
emerging
questions
science
Climate Dynamics,
Journal Year:
2025,
Volume and Issue:
63(2)
Published: Feb. 1, 2025
Significant
changes
have
occurred
during
the
last
few
decades
across
North
Atlantic
climate
system,
including
in
atmosphere,
ocean,
and
cryosphere.
These
large-scale
play
a
vital
role
shaping
regional
extreme
weather
events
UK
Western
Europe.
This
review
synthesizes
characteristics
of
observed
atmospheric
oceanic
circulations
past
decades,
identifies
drivers
physical
processes
responsible
for
these
changes,
outlines
projected
due
to
anthropogenic
warming,
discusses
predictability
circulations.
On
multi-decadal
time
scales,
internal
variability,
forcings
(especially
greenhouse
gases),
natural
(such
as
solar
variability
volcanic
eruptions)
are
identified
key
contributors
However,
there
remain
many
uncertainties
regarding
detailed
various
influences,
some
cases
their
relative
importance.
We
therefore
conclude
that
better
understanding
drivers,
more
accurate
quantification
roles,
crucial
reliable
decadal
predictions
projections
The
online
version
contains
supplementary
material
available
at
10.1007/s00382-025-07591-1.
Marine Biology,
Journal Year:
2025,
Volume and Issue:
172(3)
Published: Feb. 7, 2025
Abstract
The
rapid
warming
of
the
Arctic
Ocean
is
driving
significant
shifts
in
ecosystem
dyamics,
from
species-level
morphological
changes
to
community
composition.
Within
pelagic
community,
Ostracoda
an
understudied
zooplankton
group
that
exhibits
distinct
sexually
dimorphic
features,
including
carapace
shape,
size,
frontal
and
reproductive
organs,
antennae.
During
analyses
a
time
series
collected
each
summer
2010
2019
Fram
Strait,
main
gateway
between
north
Atlantic
Ocean,
all
four
dominant
ostracod
species
(
Boroecia
maxima
,
B.
borealis
Discoconchoecia
elegans
Obtusoecia
obtusata
)
displayed
abnormalities
form
pseudopenises
otherwise
had
female
features.
Out
total
analyzed
material
4,137
adult
pre-mature
A-1
stages
individuals,
646
stage
or
15.6%
population,
exhibited
pseudopenises.
All
observed
were
confined
with
no
variant
adults
recorded.
primary
difference
these
normal
male
penises
was
lack
muscle
bands
sperm
duct
required
for
functionality.
However,
few
females
signs
ducts
developing,
suggesting
potential
transition
true
intersexuality.
Monitoring
this
phenomenon
ostracods
crucial
because
it
can
have
population-wide
consequences.
Furthermore,
widespread
intersexuality
could
complicate
interpretation
ecological
trends
changing
Arctic.
The Journal of Foraminiferal Research,
Journal Year:
2025,
Volume and Issue:
55(2), P. 144 - 159
Published: April 1, 2025
ABSTRACT
Fjords
are
critical
carbon
burial
hotspots,
playing
a
significant
role
in
climate
regulation.
However,
the
impact
of
current
change
on
foraminifera
Arctic
fjords
remains
underexplored,
despite
foraminiferal
inorganic
carbon’s
substantial
contribution
to
glaciomarine
sediments
form
calcium
carbonate.
This
study
investigates
how
benthic
assemblages
high-latitude
fjord
responded
recent
climatic
shifts
terms
abundance
and
species
composition
between
2002
2019.
The
environmental
changes
have
reduced
number
tests
produced
by
foraminifera,
shifted
towards
smaller
species,
increased
agglutinated
specimens
sediments.
These
factors
contributed
an
over
tenfold
decline
carbonate
2019
compared
those
from
2002,
providing
evidence
change’s
at
this
location.
Journal of Geophysical Research Oceans,
Journal Year:
2025,
Volume and Issue:
130(5)
Published: May 1, 2025
Abstract
Kongsfjorden
is
located
in
West
Spitsbergen,
Svalbard
archipelago.
Its
hydrography
influenced
by
the
Spitsbergen
Current
(WSC)
transporting
warm
and
saline
Atlantic
Water
(AW)
toward
Arctic
basin.
We
assessed
changes
fjord
water
properties
over
two
decades
(1999–2020)
using
summer
hydrographic
surveys
performed
Norwegian
Polar
Institute
fjord,
adjacent
shelf,
open
ocean
regions.
The
heat
content
(HC)
salinity
within
have
increased
driven
a
larger
inflow
of
AW.
These
trends
are
consistent
with
observations
neighboring
Isfjorden
but
not
mirrored
WSC
same
timeframe.
Therefore,
these
fjords
can
be
attributed
to
AW
intrusions
rather
than
variations
upstream
properties.
hypothesize
that
HC
shifts
synoptic
wind
patterns
glacier
meltwater
release
enhancing
shelf
exchanges.
Idealized
modeling
experiments
revealed
although
modifications
contribute
increasing
fjord's
HC,
they
explain
only
small
portion
observed
changes,
suggesting
availability
on
dominant
factor.
Biology,
Journal Year:
2023,
Volume and Issue:
12(3), P. 368 - 368
Published: Feb. 25, 2023
We
studied
the
spatial
patterns
of
planktonic
ecosystems
at
two
Arctic
sites
strongly
affected
by
Atlantic
Inflow
(FS,
Fram
Strait;
and
BS,
Barents
Sea).
A
high
degree
similarity
in
bacterial
abundance
(mean:
3.1
×
105
cells
mL−1
FS
vs.
3.5
BS)
was
found,
while
other
plankton
characteristics
were
different.
Bacterial
biomass
reached
a
maximum
BS
(3.2–7.9
mg
C
m−3),
viral
abundances
tended
to
be
higher
(2.0–5.7
106
particles
mL−1).
Larger
found
suggesting
presence
different
populations
both
locations.
The
virus-to-bacteria
ratio
significantly
than
(13.5
4.7).
Chlorophyll
concentration
extremely
low
(<0.25
m−3).
highest
zooplankton
surface
layer
(919
individuals
m−3
602
ind.
BS).
Zooplankton
varied
(1–39
with
BS.
High
proportions
boreal
taxa
total
indicate
Atlantification
pelagic
Arctic.
Plankton
indicators
are
correlated
temperature,
salinity,
sampling
depth.
Strong
intercorrelations
between
major
groups,
tight
links
ecosystems.
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.
Journal of Geophysical Research Oceans,
Journal Year:
2024,
Volume and Issue:
129(5)
Published: May 1, 2024
Abstract
The
Northeast
Water
Polynya
is
a
significant
annually
recurring
summertime
Arctic
polynya,
located
off
the
coast
of
Greenland.
It
important
for
marine
wildlife
and
affects
local
atmospheric
oceanic
processes.
In
this
study,
over
40
years
observational
reanalysis
products
(ERA5
ORAS5)
are
analyzed
to
characterize
polynya's
climatology
ascertain
forcing
mechanisms.
has
high
spatiotemporal
variability;
its
location,
size
structure
vary
interannually,
period
which
it
open
changing.
We
show
variability
largely
driven
by
forcing.
polynya
extent
determined
direction
near‐surface
flow
regime,
relative
locations
low
sea‐level
pressure
centers
region.
surface
conditions
also
impact
water
column,
strong
seasonal
cycle
in
potential
temperature
salinity,
amplitude
decreases
with
depth.
ocean
reanalyses
warming
trend
at
all
depths
freshening
near
consistent
greater
ice
melt,
but
salinification
lower
(∼200
m).
As
region
changes
due
anthropogenic
forcing,
sea‐ice
edge
migrating
northwards
generally
opening
earlier
closing
later
year.
This
could
have
implications
both
atmosphere
complex
rapidly
changing
environment.