Journal of Geophysical Research Oceans,
Journal Year:
2022,
Volume and Issue:
127(4)
Published: March 31, 2022
Abstract
The
processes
of
seafloor
sediment
transport
from
the
Chukchi
shelf
to
western
Arctic
basin
were
investigated
using
a
pan‐Arctic
sea
ice‐ocean
model
and
sediment‐trap
measurements
at
four
mooring
stations:
North
Barrow
Canyon,
Hanna
Northwind
Abyssal
Plain,
Plain.
available
data
verified
that
sinking
flux
lithogenic
material
(LM)
originally
resuspended
for
2010–2020
was
simulated
reasonably
well
in
areas.
results
analyzed
quantify
spatiotemporal
variability
LM
reveal
its
background
mechanisms.
Analysis
indicated
Canyon
throughflow,
Slope
Current
(CSC),
mesoscale
eddies
played
important
roles
redistribution.
CSC
controlled
westward
mouth
Borderland.
generated
north
efficiently
transported
shelf‐origin
toward
southern
Canada
Basin.
particulate
organic
carbon
(POC)
averaged
September
2010
August
2020,
which
estimated
statistically
flux,
0.13–0.30
gC
m
−2
yr
−1
200‐m
depth
This
finding
reveals
lateral
bottom
has
considerable
effect
on
POC
basin,
suggests
marine
biogeochemical
cycle
is
strongly
influenced
by
shelf‐basin
exchange
depends
relative
strength
eddy
activity.
Global Biogeochemical Cycles,
Journal Year:
2025,
Volume and Issue:
39(1)
Published: Jan. 1, 2025
Abstract
Observations
of
dissolved
cadmium
(dCd)
and
phosphate
(PO
4
)
suggest
an
unexplained
loss
dCd
to
the
particulate
phase
in
tropical
oxyclines.
Here,
we
compile
existing
observations
Cd
phosphorus
(P),
present
new
data
from
US
GEOTRACES
GP15
Pacific
Meridional
Transect
examine
this
phenomenon
a
perspective.
We
use
simple
algorithm
reproduce
station
depth
profiles
P
via
regeneration
possible
subsurface
accumulation.
Our
examination
reveals
decoupling
driven
by
variable
partitioning
between
two
pools
with
differing
labilities.
Further,
identify
evidence
for
accumulation
at
31
stations.
Subsurface
occurs
most
consistently
mesopelagic
but
can
be
found
all
examined
ocean
basins.
This
is
not
well‐correlated
oxygen
or
sulfide
concentration.
Instead,
observe
that
regions
where
concentration
relatively
high
compared
zinc
(dZn)
speculate
it
result
enhanced
biological
uptake
response
micronutrient
balance.
Global Biogeochemical Cycles,
Journal Year:
2024,
Volume and Issue:
38(1)
Published: Jan. 1, 2024
Abstract
Understanding
particle
cycling
processes
in
the
ocean
is
critical
for
predicting
response
of
biological
carbon
pump
to
external
perturbations.
Here,
measurements
particulate
organic
(POC)
concentration
two
size
fractions
(1–51
and
>51
μm)
from
GEOTRACES
Pacific
meridional
transect
GP15
are
combined
with
a
POC
model
estimate
rates
production,
(dis)aggregation,
sinking,
remineralization,
vertical
transport
mediated
by
migrating
zooplankton,
euphotic
zone
(EZ)
upper
mesopelagic
(UMZ)
distinct
environments.
We
find
coherent
variations
parameters
fluxes
throughout
transect.
Thus,
settling
speed
μm
fraction
increased
depth
UMZ,
presumably
due
higher
densities
at
depth.
The
flux
total
(>1
out
EZ
was
positively
correlated
primary
production
integrated
over
EZ;
highest
export
occurred
subarctic
gyre
while
lowest
subtropical
gyres.
ratio
low
(<5%)
along
GP15,
which
suggests
an
efficient
recycling
all
trophic
regimes.
Specific
remineralization
did
not
show
clear
temperature
or
dissolved
oxygen
concentration,
that
is,
apparently
controlled
other
factors
such
as
microbial
colonization
substrate
lability.
Particle
cohesiveness,
approximated
second‐order
rate
constant
aggregation,
negatively
regime:
particles
appeared
more
cohesive
low‐productivity
regions
than
high‐productivity
regions.
Frontiers in Marine Science,
Journal Year:
2020,
Volume and Issue:
7
Published: Sept. 8, 2020
Extensive
studies
in
the
1980s-1990s
led
to
characterization
of
latitudinal
variations
sea
surface
δ13C
values
particulate
organic
carbon
(δ13CPOC),
and
relationships
were
found
with
CO2
concentrations,
temperature,
growth
rates,
cell
geometries.
Surprisingly,
no
large-scale
efforts
have
been
made
describe
δ13CPOC
over
depth
water
column.
Here
we
compile
published
examples
demonstrating
a
widespread
isotopic
pattern
upper
In
51
vertical
profiles,
lower
euphotic
zone
on
average
are
1.4‰
than
open
ocean
settings.
majority
locations
this
downward
decrease
is
>
2‰
up
5‰,
larger
commonly
recognized
variation
dissolved
inorganic
same
depths.
We
briefly
review
hypotheses
supporting
evidence
offered
by
previous
individual
columns:
The
observed
patterns
could
result
from
differences
photosynthetic
rates
or
community
composition,
biochemical
composition
matter
due
degradation,
disequilibrium
within
pool,
particle
dynamics,
seasonal
mixing.
Coordinated
isotopic,
biological,
seawater
chemistry
data
sparse,
consistent
drivers
currently
elusive.
Further
work
needed
adequately
characterize
environmental
conditions
coinciding
pattern,
test
its
origins,
determine
if
magnitude
column
be
useful
marker
cycle
dynamics.
Proceedings of the National Academy of Sciences,
Journal Year:
2023,
Volume and Issue:
120(23)
Published: May 30, 2023
Reversible
scavenging,
the
oceanographic
process
by
which
dissolved
metals
exchange
onto
and
off
sinking
particles
are
thereby
transported
to
deeper
depths,
has
been
well
established
for
metal
thorium
decades.
scavenging
both
deepens
elemental
distribution
of
adsorptive
elements
shortens
their
oceanic
residence
times
in
ocean
compared
nonadsorptive
metals,
ultimately
removes
from
via
sedimentation.
Thus,
it
is
important
understand
undergo
reversible
under
what
conditions.
Recently,
invoked
global
biogeochemical
models
a
range
including
lead,
iron,
copper,
zinc
fit
modeled
data
observations
distributions.
Nonetheless,
effects
remain
difficult
visualize
sections
distinguish
other
processes
such
as
biological
regeneration.
Here,
we
show
that
particle-rich
"veils"
descending
high-productivity
zones
equatorial
North
Pacific
provide
idealized
illustrations
lead
(Pb).
A
meridional
section
Pb
isotope
ratios
across
central
shows
where
particle
concentrations
sufficiently
high,
within
veils,
vertical
transport
anthropogenic
surface-dissolved
toward
deep
manifested
columnar
anomalies.
Modeling
this
effect
waters
allows
surface
penetrate
ancient
on
timescales
rapid
overcome
horizontal
mixing
water
along
abyssal
isopycnals.
Frontiers in Remote Sensing,
Journal Year:
2022,
Volume and Issue:
3
Published: March 8, 2022
Particulate
inorganic
carbon
(PIC)
plays
a
major
role
in
the
ocean
cycle
impacting
pH,
dissolved
carbon,
and
alkalinity,
as
well
particulate
organic
(POC)
export
transfer
efficiency
to
deep
sea.
Remote
sensing
retrievals
of
PIC
surface
waters
span
two
decades,
yet
knowledge
concentration
variability
water
column
is
temporally
spatially
limited
due
reliance
on
ship
sampling.
To
overcome
space–time
gap
observations,
we
have
developed
optical
sensors
for
flux
that
exploit
high
mineral
birefringence
CaCO
3
minerals,
thus
enable
real-time
data
when
deployed
operationally
from
CTDs
ARGO-style
Carbon
Flux
Explorer
floats.
For
concentrations,
describe
fast
(10
Hz)
digital
low-power
(∼0.5
W)
sensor
utilizes
cross-polarized
transmitted
light
detect
photon
yield
suspended
birefringent
particles
column.
This
has
been
CTD-deployed
depths
great
6,000
m
cross-calibrated
against
particulates
sampled
by
large
volume
situ
filtration
CTD/rosettes.
We
report
September–November
2018
GEOTRACES
GP15
meridional
transect
Aleutian
Islands
Tahiti
along
152°W
where
validated
prototype
separate
CTD
systems
bottom
at
39
stations,
many
which
were
taken
nearly
particle-free
waters.
compare
results
with
particle
phase
composition
(particularly
aluminum)
simultaneously
collected
size-fractionated
samples
filtration.
also
June
2017
California
Current
Ecosystem-Long
Term
Ecological
Research
(CCE-LTER)
process
study
coastal
levels
found.
demonstrate
can
0.01
>1
μM
(except
nepheloid
layers)
outline
engineering
needs
progress
its
integration
Explorer,
an
autonomous
float.
Biogeosciences,
Journal Year:
2022,
Volume and Issue:
19(9), P. 2365 - 2395
Published: May 5, 2022
Abstract.
Over
the
past
decade,
GEOTRACES
and
wider
trace
metal
geochemical
community
has
made
substantial
contributions
towards
constraining
marine
cobalt
(Co)
cycle
its
major
biogeochemical
processes.
However,
few
Co
speciation
studies
have
been
conducted
in
North
equatorial
Pacific
Ocean,
a
vast
portion
of
world's
oceans
by
volume
an
important
end-member
deep
thermohaline
circulation.
Dissolved
(dCo)
samples,
including
total
dissolved
labile
Co,
were
measured
at-sea
during
Meridional
Transect
(GP15)
expedition
along
152∘
W
longitudinal
from
56∘
N
to
20∘
S.
Along
this
transect,
upper-ocean
dCo
(σ0<26)
was
linearly
correlated
with
phosphate
(slope
=
82±3,
µmol
:
mol)
due
phytoplankton
uptake
remineralization.
As
depth
increased,
concentrations
became
increasingly
decoupled
co-scavenging
manganese
oxide
particles
mesopelagic.
The
transect
revealed
organically
bound
coastal
source
Alaskan
Stream
associated
low-salinity
waters.
An
intermediate-depth
hydrothermal
flux
observed
off
Hawaiian
coast
at
Loihi
Seamount,
elevated
potential
xs3He
above
vent
site;
however,
Seamount
likely
did
not
represent
basin.
Elevated
within
oxygen
minimum
zones
(OMZs)
South
consistent
suppression
oxidative
scavenging,
we
estimate
that
future
deoxygenation
could
increase
OMZ
inventory
18
%
36
over
next
century.
In
Deep
Water
(PDW),
fraction
ligand-bound
appeared
protected
scavenging
high
biogenic
particle
This
finding
is
counter
previous
expectations
low
Compared
global
model,
displayed
more
extreme
inventories
fluxes
than
predicted
suggesting
highly
dynamic
cycle.
Oceanography,
Journal Year:
2024,
Volume and Issue:
37(2)
Published: Jan. 1, 2024
There
have
been
many
changes
over
the
past
few
decades
in
physical
environment
and
ecosystem
health
of
Arctic
Ocean,
which
is
a
sentinel
global
warming.
Bioactive
trace
metal
data
important
micronutrients
for
algae
across
ocean,
such
as
iron
(Fe)
manganese
(Mn),
are
key
indicators
biogeochemical
change.
However,
historically
sparse
generally
confined
to
ice-free
regions.
In
2015,
three
major
GEOTRACES
expeditions
sought
resolve
distributions
Arctic,
covering
western,
eastern,
Canadian
sectors.
The
diverse
shelves
displayed
unique
controls
on
Fe
Mn
cycling
due
differing
chemical,
biological,
properties.
Here,
we
contrast
shallow,
reducing
Chukchi
Shelf
western
with
tidally
forced,
advective
deeper,
less
productive
Barents
eastern
Arctic.
Reductive
dissolution
resuspension
both
proved
be
large
sources
North
Atlantic
outflow.
isolated
intermediate
deep
waters,
one-dimensional
scavenging
contrasts
vertical
biological
signals
Baffin
Bay
Labrador
Sea.
Journal of Geophysical Research Oceans,
Journal Year:
2021,
Volume and Issue:
126(3)
Published: Feb. 20, 2021
Abstract
One‐dimensional
vertical
(1DV)
diffusion‐settling
models
are
practical
tools
for
sediment
transport
analysis
of
sands,
which
is
mostly
a
local
process.
However,
fine
sediments,
the
observed
concentrations
C
(
t
)
can
be
mixed
via
horizontal
advection
(HA)
due
to
lower
settling
velocity,
makes
not
necessarily
process,
thus
making
1DV
invalid.
It
important
determine
qualitative
significance
HA
or
quantitatively
separate
signals
when
applying
environments
with
advected
sediments.
Here,
novel
methods
combined
(1)
qualitatively
identify
physical
mechanisms
underlying
variations
and
whether
significant
multiscale
frequency
superposition
(2)
decompose
components
according
their
spectral
filter
decomposition.
In
situ
observational
data
concurrent
hydrodynamics
in
subaqueous
Yellow
River
Delta
employed
analyze
methods'
performance.
The
decomposed
reasonable
because
they
interpreted
light
other
processes.
results
indicated
that
M2
tidal
contributed
8.30%
by
carrying
sediments
from
1.6
km
upstream
flood
tides,
M4
M6
+
M8
resuspension
4.16%
3.96%,
respectively,
periodically
resuspending
“fluffy
layer.”
Waves
resuspended
an
erosion
center
5
tides
76.49%
elevated
).
proposed
exclude
measured
increase
applicability
fines
measured.