Journal of Geophysical Research Oceans,
Journal Year:
2025,
Volume and Issue:
130(3)
Published: March 1, 2025
Abstract
Tropical
cyclones
erode
and
remobilize
coastal
sediments
but
their
impact
on
the
deep
ocean
remains
unclear.
Hurricane‐driven
transport
of
carbonates
associated
materials
from
reef
carbonate
platforms
to
has
important
implications
for
carbon
storage,
ecosystems
chemistry
as
platform
reef‐sourced
aragonite
high‐Mg
calcite
(HMC)
may
dissolve
contribute
water
total
alkalinity.
Here
we
describe
two
hurricane‐driven
resuspension
events
where
sediment
plumes
Bermuda
Pedestal
(NW
Atlantic)
were
advected
waters
surrounding
Oceanic
Flux
Program
(OFP)
mooring
site,
∼75
km
southeast
Bermuda.
Hurricanes
Fabian
(Cat.
3,
2003)
Igor
1,
2010)
generated
large
near‐inertial
waves
propagating
>750
m
depths,
leading
widespread
Pedestal.
Following
Fabian,
fluxes
at
OFP
site
increased
15‐fold,
32‐fold,
6‐fold
500,
1,500
3,200
m,
respectively,
with
flux
equivalent
annual
flux.
traps
similarly
captured
a
detrital
plume
following
Igor;
here,
was
shallower
persisted
longer.
Microscopy,
geochemistry,
mineralogy
confirmed
that
both
consisted
fine‐grained
shallow‐water
alongside
other
accumulated
including
phosphorus,
lithogenic,
authigenic,
pollutant
elements.
Clay‐sized
particles
(<4
μm)
in
exhibited
high
contents
lithogenic
authigenic
elements,
Zn,
Cd,
V,
facilitating
over
long
distances.
Grain‐size,
elemental,
lipid
composition
indicated
intercepted
different
depths
originated
source
areas
Geochemistry Geophysics Geosystems,
Journal Year:
2022,
Volume and Issue:
23(8)
Published: Aug. 1, 2022
Abstract
Fossil‐bound
organic
material
holds
great
potential
for
the
reconstruction
of
past
changes
in
nitrogen
(N)
cycling.
Here,
with
a
series
laboratory
experiments,
we
assess
effect
oxidative
degradation,
fossil
dissolution,
and
thermal
alteration
on
fossil‐bound
N
isotopic
composition
different
types,
including
deep
shallow
water
scleractinian
corals,
foraminifera,
diatoms
tooth
enamel.
Our
experiments
show
that
exposure
to
oxidizing
reagents
does
not
significantly
affect
or
content
any
types
analyzed,
demonstrating
matter
is
well
protected
from
surrounding
environment
by
mineral
matrix.
In
addition,
partial
dissolution
(of
up
70%–90%)
aragonite,
calcite,
opal,
enamel
matrixes
has
negligible
fossils.
These
results
suggest
relatively
uniform,
also
exposed
during
lost
without
significant
discrimination.
Finally,
our
heating
all
at
100°C.
At
200°C
hotter,
loss
associated
isotope
appear
be
directly
linked
sensitivity
matrix
stress,
which
depends
biomineral
type.
that,
so
long
as
high
temperature
compromise
structure,
acts
closed
system
respect
N,
remains
unchanged.
Abstract
Data
were
obtained
from
the
literature
to
identify
past
changes
in
and
present
status
of
coastal
carbon
cycle.
They
indicate
that
marine
ecosystems
driving
cycle
cover,
on
average,
5.8%
Earth’s
surface
contributed
55.2%
transport
climate-active
geological
The
data
suggest
humans
not
only
increase
CO
2
concentration
atmosphere
but
also
mitigate
(and
before
1860
even
balanced)
their
emissions
by
increasing
storage
within
ecosystems.
Soil
degradation
response
expansion
intensification
agriculture
is
assumed
be
a
key
process
enhanced
because
it
increases
supply
lithogenic
matter
known
favour
burial
organic
sediments.
After
1860,
rising
concentrations
caused
land-use
burning
fossil
fuel
disturbed
what
was
quasi-steady
state
before.
Ecosystem
restoration
potential
forest
cover
could
atmospheric
concentrations,
this
sink
much
too
weak
represent
an
alternative
reduction
emission
order
keep
global
warming
below
1.5–2.°C.
Although
contribution
benthic
uptake
ecosystem
around
6%,
significant
given
national
budgets.
However,
impact
climate
still
difficult
quantify
associated
effects
CH
4
N
O
have
been
established.
Addressing
these
uncertainties
one
challenges
faced
future
research,
as
are
related
issues
concerning
estimates
fluxes
between
development
suitable
methods
pelagic
ocean.
Earth s Future,
Journal Year:
2024,
Volume and Issue:
12(6)
Published: June 1, 2024
Abstract
The
ocean
is
responsible
for
taking
up
approximately
25%
of
anthropogenic
CO
2
emissions
and
stores
>50
times
more
carbon
than
the
atmosphere.
Biological
processes
in
play
a
key
role,
maintaining
atmospheric
levels
200
ppm
lower
they
would
otherwise
be.
ocean's
ability
to
take
store
sensitive
climate
change,
however
biological
that
contribute
storage
are
uncertain,
as
how
those
will
respond
to,
feedback
on,
change.
As
result,
biogeochemical
models
vary
widely
their
representation
relevant
processes,
driving
large
uncertainties
projections
future
storage.
This
review
identifies
affect
may
change
three
thematic
areas:
contributions
alkalinity,
net
primary
production,
interior
respiration.
We
undertook
existing
literature
identify
with
high
importance
influencing
biologically‐mediated
ocean,
prioritized
on
basis
both
an
expert
assessment
community
survey.
Highly
ranked
survey
were:
alkalinity—high
level
understanding
calcium
carbonate
production;
production—resource
limitation
growth,
zooplankton
phytoplankton
loss
processes;
respiration—microbial
solubilization,
particle
characteristics
type.
analysis
presented
here
designed
support
field
or
laboratory
experiments
targeting
new
process
understanding,
modeling
efforts
aimed
at
undertaking
model
development.
Global Biogeochemical Cycles,
Journal Year:
2022,
Volume and Issue:
36(2)
Published: Jan. 8, 2022
Abstract
We
leverage
observations
from
chemical
and
bio‐optical
sensors
mounted
on
a
biogeochemical
profiling
float
in
the
Northeast
Pacific
Ocean
to
quantify
cycling
export
potential
of
distinct
biogenic
carbon
pools,
including
particulate
inorganic
(PIC),
organic
(POC),
dissolved
(DOC).
Year‐round
reveal
complex
cycle
dynamics
among
these
pools.
Net
DOC
production
peaked
during
bloom
initiation,
about
3
months
prior
summer
peak
POC
production.
validate
estimates
with
seasonal
accumulation
removal
rates
derived
ship‐board
over
same
period.
By
combining
tracers
cycling,
we
estimate
instantaneous
sinking
flux
(
).
The
cooccurrence
consumption
fall
winter
resolves
regional
conundrum
persistent
particle
observed
by
sediment
traps
season
that
is
known
be
heterotrophic.
PIC
small,
uncertainties
are
large.
float‐based
net
primary
(NPP)
,
real‐time
ratio
([
/NPP]
×
100%)
for
euphotic
zone.
Elevated
ratios
associated
an
increase
fraction
particles
larger
than
100
μm
size.
physical
redistribution
through
deep
mixing.
Our
study
demonstrates
how
combined
use
multiple
floats
can
provide
more
nuanced
information
upper
ocean
dynamics.
Journal of Nanobiotechnology,
Journal Year:
2023,
Volume and Issue:
21(1)
Published: Nov. 5, 2023
Abstract
Marine
resources
in
unique
marine
environments
provide
abundant,
cost-effective
natural
biomaterials
with
distinct
structures,
compositions,
and
biological
activities
compared
to
terrestrial
species.
These
marine-derived
raw
materials,
including
polysaccharides,
protein
components,
fatty
acids,
minerals,
etc.,
have
shown
great
potential
preparing,
stabilizing,
or
modifying
multifunctional
nano-/micro-systems
are
widely
applied
drug
delivery,
theragnostic,
tissue
engineering,
etc.
This
review
provides
a
comprehensive
summary
of
the
most
current
biomaterial-based
developed
over
past
three
years,
primarily
focusing
on
therapeutic
delivery
studies
highlighting
their
cure
variety
diseases.
Specifically,
we
first
provided
detailed
introduction
physicochemical
characteristics
biocomponents
state.
Furthermore,
assembly
processes,
functionalities
each
building
block,
thorough
evaluation
pharmacokinetics
pharmacodynamics
advanced
systems
effects
molecular
pathophysiological
processes
were
fully
elucidated.
Finally,
list
unresolved
issues
pivotal
challenges
applications,
such
as
standardized
distinction
long-term
biosafety
vivo,
feasibility
scale-up,
was
presented.
is
expected
serve
roadmap
for
fundamental
research
facilitate
rational
design
diverse
emerging
applications.
Graphical
Journal of Geophysical Research Oceans,
Journal Year:
2023,
Volume and Issue:
128(2)
Published: Feb. 1, 2023
Abstract
The
cycling
of
marine
particulate
matter
is
critical
for
sequestering
carbon
in
the
deep
ocean
and
sediments.
Biogenic
minerals
such
as
calcium
carbonate
(CaCO
3
)
opal
add
density
to
more
buoyant
organic
material,
facilitating
particle
sinking
export.
Here,
we
compile
analyze
a
global
data
set
(POC),
inorganic
(PIC,
or
CaCO
),
biogenic
silica
(bSi,
opal)
concentrations
collected
using
large
volume
pumps
(LVPs).
We
distribution
all
three
phases
small
(1–53
μm)
(>53
size
classes.
Over
entire
water
column
76%
POC
exists
fraction.
Similarly,
class
contains
82%
PIC,
indicating
importance
small‐sized
coccolithophores
PIC
budget
ocean.
In
contrast,
50%
bSi
fraction,
reflecting
larger
diatoms
radiolarians
compared
with
coccolithophores.
use
PIC:POC
bSi:POC
ratios
upper
document
consistent
signal
shallow
mineral
dissolution,
likely
linked
biologically
mediated
processes.
Sediment
trap
are
elevated
respect
LVP
samples
increase
strongly
depth,
concentration
and/or
deficit
particles.
suggest
that
future
sampling
campaigns
pair
LVPs
sediment
traps
capture
full
field,
especially
aggregates
contribute
mineral‐rich
fluxes,
may
be
missed
by
LVPs.
Molecular Ecology,
Journal Year:
2023,
Volume and Issue:
32(12), P. 3200 - 3219
Published: March 21, 2023
Little
is
known
about
when
and
how
planktonic
species
arise
persist
in
the
open
ocean
without
apparent
dispersal
barriers.
Pteropods
are
snails
with
thin
shells
susceptible
to
dissolution
that
used
as
bio-indicators
of
acidification.
However,
distinct
evolutionary
units
respond
acidification
differently,
defining
boundaries
therefore
crucial
for
predicting
impact
changing
conditions.
In
this
global
population
genomic
study
shelled
pteropod
Limacina
bulimoides,
we
combined
genetic
(759,000
single
nucleotide
polymorphisms)
morphometric
data
from
161
individuals,
revealing
three
major
lineages
(FST
=
0.29-0.41):
an
"Atlantic
lineage"
sampled
across
Atlantic,
"Indo-Pacific
North
Pacific
Indian
Ocean,
a
"Pacific
South
Pacific.
A
time-calibrated
phylogeny
suggests
diverged
1
million
years
ago,
estimated
effective
size
remaining
high
(~10
million)
throughout
Pleistocene
glacial
cycles.
We
do
not
observe
any
signatures
recent
hybridization,
even
areas
sympatry
While
reproductively
isolated,
they
morphologically
cryptic,
overlapping
shell
shape
colour
distributions.
Despite
showing
circumglobal
L.
bulimoides
consists
multiple
smaller
ranges
than
initially
thought,
found
these
pteropods
still
possess
levels
variability.
Our
adds
growing
evidence
speciation
often
overlooked
ocean,
presence
biological
within
many
other
currently
defined
species.
Journal of Geophysical Research Biogeosciences,
Journal Year:
2024,
Volume and Issue:
129(2)
Published: Feb. 1, 2024
Abstract
Carbon
dioxide
entering
and
acidifying
the
ocean
can
be
neutralized
by
dissolution
of
calcium
carbonate,
which
is
mainly
found
in
two
mineral
forms.
Calcite
more
stable
form
often
deep‐sea
sediments,
whilst
aragonite
soluble
therefore
rarely
preserved.
Recent
research
shows
may
account
for
a
much
larger
portion
marine
carbonate
export
to
interior
via
biological
pump
than
previously
thought,
that
does
reach
deep
sea
seafloor
despite
being
buried.
If
present
dissolving
at
it
will
raise
local
pH
concentrations,
potentially
enough
inhibit
calcite
dissolution,
representing
deep‐sea,
version
galvanization.
Here,
we
test
this
hypothesis
simulating
sediment‐water
interface
laboratory
measuring
its
effects
on
using
microsensors.
We
show
addition
sediment,
overlain
seawater
undersaturated
with
respect
both
minerals,
results
an
unchanged
alkalinity
flux
out
suggesting
decrease
net
rate
calcite.
In
combination
diagenetic
model,
suppress
top
millimeters
seabed,
locally
leading
precipitation
within
1
day.
Future
efforts
should
quantify
galvanization
effect
situ,
as
process
represent
important
component
carbon
cycle,
assigning
key
role
producers
controlling
preserving
climatic
archives.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: June 6, 2024
The
vertical
settling
of
plastic
debris
in
oceans
is
poorly
understood.
A
large
share
low-density
microplastics
(LDMPs)
are
largely
absent
from
sea
surfaces.
present
study
employs
a
model
that
considers
the
potential
an
overlooked
microbially
induced
calcium
carbonate
precipitation
(MICP)
process
and
new
motion
equations
for
irregular
LDMPs.
Here
we
show
LDMPs
model,
exhibiting
damped
oscillation
pattern,
quite
different
biofouling
models.
Furthermore,
size
range
10-200
µm
most
likely
to
gain
sufficient
density
at
biofouling/MICP
stage
independently
sink
ocean
floor
with
relatively
small
drag
coefficients,
potentially
explaining
selective
enrichment
oceanic
sediment.
shape
exhibit
strong
non-linear
effects
on
patterns
Overall,
highlights
importance
calcite-mediated
sinking
open
oceans.
Elementa Science of the Anthropocene,
Journal Year:
2022,
Volume and Issue:
10(1)
Published: Jan. 1, 2022
Atmospheric
and
oceanic
CO2
concentrations
are
rising
at
an
unprecedented
rate.
Laboratory
studies
indicate
a
positive
effect
of
on
phytoplankton
growth
until
optimum
is
reached,
after
which
the
negative
impact
accompanying
acidification
dominates.
Here,
we
implemented
carbonate
system
sensitivities
into
our
global
biogeochemical
model
FESOM-REcoM
accounted
explicitly
for
coccolithophores
as
group
most
sensitive
to
CO2.
In
idealized
simulations
in
solely
atmospheric
mixing
ratio
was
modified,
changes
competitive
fitness
biomass
not
only
caused
by
direct
effects
CO2,
but
also
indirect
via
nutrient
light
limitation
well
grazing.
These
cascading
can
both
amplify
or
dampen
responses
changing
ocean
pCO2
levels.
For
example,
coccolithophore
negatively
affected
directly
future
indirectly
limitation,
these
compensated
weakened
resulting
from
decrease
small-phytoplankton
biomass.
Southern
Ocean,
decreases
hereby
preferred
prey
zooplankton,
reduces
grazing
pressure
diatoms
allows
them
proliferate
more
strongly.
that
encompass
CO2-driven
warming
acidification,
reveals
recent
observed
North
Atlantic
driven
primarily
Our
results
highlight
change
other
environmental
drivers
growth,
may
play
important
role
projections
net
primary
production.