Emerging Topics in Life Sciences,
Journal Year:
2018,
Volume and Issue:
2(2), P. 267 - 278
Published: June 29, 2018
A
'Neoproterozoic
oxygenation
event'
is
widely
invoked
as
a
causal
factor
in
animal
evolution,
and
often
attributed
to
abiotic
causes
such
post-glacial
pulses
of
phosphorus
weathering.
However,
recent
evidence
suggests
series
transient
ocean
events
∼660-520
Ma,
which
do
not
fit
the
simple
model
monotonic
rise
atmospheric
oxygen
(pO2).
Hence,
we
consider
mechanisms
by
evolution
marine
eukaryotes,
coupled
with
biogeochemical
ecological
feedbacks,
potentially
between
alternate
stable
states,
could
have
caused
changes
carbon
cycling
redox
state,
pO2.
We
argue
that
late
Tonian
∼750
Ma
was
dominated
rapid
microbial
dissolved
organic
matter
(DOM)
elevated
nutrient
(P)
levels
due
inefficient
removal
sediments.
suggest
abrupt
onset
eukaryotic
algal
biomarker
record
∼660-640
linked
an
escalation
protozoan
predation,
created
'biological
pump'
sinking
particulate
(POM).
The
resultant
transfer
(Corg)
sediments
strengthened
subsequent
innovations,
including
advent
sessile
benthic
animals
mobile
burrowing
animals.
Thus,
each
phase
eukaryote
tended
lower
P
oxygenate
on
∼104
year
timescales,
but
decreasing
Corg/P
burial
ratios,
pO2
deoxygenate
again
∼106
timescales.
This
can
help
explain
nature
duration
oceanic
through
Cryogenian-Ediacaran-Cambrian.
Ecological Monographs,
Journal Year:
2019,
Volume and Issue:
89(3)
Published: May 23, 2019
Abstract
Macroalgae
drive
the
largest
CO
2
flux
fixed
globally
by
marine
macrophytes.
Most
of
resulting
biomass
is
exported
through
coastal
ocean
as
detritus
and
yet
almost
no
field
measurements
have
verified
its
potential
net
sequestration
in
sediments.
This
gap
limits
scope
for
inclusion
macroalgae
within
blue
carbon
schemes
that
support
globally,
understanding
role
their
plays
distal
food
webs.
Here,
we
pursued
three
lines
evidence
(eDNA
sequencing,
Bayesian
Stable
Isotope
Mixing
Modeling,
benthic‐pelagic
process
measurements)
to
generate
needed,
novel
data
addressing
this
gap.
To
end,
a
13‐month
study
was
undertaken
at
deep
sedimentary
site
English
Channel,
surrounding
shoreline
Plymouth,
UK.
The
eDNA
sequencing
indicated
from
most
shores
occurs
deep,
sediments,
with
supply
reflecting
seasonal
ecology
individual
species.
stable
isotope
mixing
modeling
[C
N]
highlighted
vital
supporting
benthic
web
(22–36%
diets),
especially
when
other
resources
are
seasonally
low.
magnitude
uptake
sediments
varies
seasonally,
an
average
organic
macroalgal
8.75
g
C·m
−2
·yr
−1
.
particulate
58.74
,
two
rates
corresponding
4–5%
26–37%
those
associated
mangroves,
salt
marshes,
seagrass
beds,
systems
more
readily
identified
habitats.
These
provide
important
first
estimates
help
contextualize
importance
macroalgal‐sedimentary
connectivity
webs,
measured
fluxes
constrain
global
can
policy
development.
At
time
climate
change
mitigation
foreground
environmental
development,
embracing
full
regulation
via
necessity.
Earth-Science Reviews,
Journal Year:
2022,
Volume and Issue:
228, P. 103987 - 103987
Published: March 12, 2022
The
seabed
plays
a
key
role
in
the
marine
carbon
cycle
as
a)
terminal
location
of
aerobic
oxidation
organic
matter,
b)
greatest
anaerobic
bioreactor,
and
c)
repository
for
reactive
on
Earth.
We
compiled
data
oxygen
uptake
sediments
with
objective
to
understand
constraints
mineralization
rates
deposited
matter
their
relation
environmental
parameters.
database
includes
nearly
4000
O2
is
available
supplementary
material.
It
also
information
bottom
water
concentration,
penetration
depth,
geographic
position,
full
sources.
present
different
situ
ex
approaches
measure
total
(TOU)
diffusive
(DOU)
discuss
robustness
towards
methodological
errors
statistical
uncertainty.
transport
through
benthic
boundary
layers,
diffusion-
fauna-mediated
uptake,
coupling
respiration
processes.
Five
regional
examples
are
presented
illustrate
diversity
seabed:
Eutrophic
seas,
minimum
zones,
abyssal
plains,
mid-oceanic
gyres,
hadal
trenches.
A
multiple
correlation
analysis
shows
that
primarily
controlled
by
ocean
depth
sea
surface
primary
productivity.
scales
DOU
according
power
law
breaks
down
under
gyres.
developed
model
was
used
draw
global
map
rates.
Respiratory
coefficients,
differentiated
regions
ocean,
were
convert
oxidation.
resulting
budget
an
212
Tmol
C
yr−1
5-95%
confidence
interval
175-260
yr−1.
comparison
flux
particulate
(POC)
from
photic
waters
deep
sea,
determined
sediment
trap
studies,
suggests
deficit
sedimentation
at
2000
m
about
70%
relative
turnover
underlying
seabed.
At
margins,
rivers
vegetated
coastal
ecosystems
contributes
greatly
may
even
exceed
phytoplankton
production
inner
continental
shelf.
Global Change Biology,
Journal Year:
2022,
Volume and Issue:
28(9), P. 2875 - 2894
Published: Feb. 17, 2022
Abstract
Subtidal
marine
sediments
are
one
of
the
planet's
primary
carbon
stores
and
strongly
influence
oceanic
sink
for
atmospheric
CO
2
.
By
far
most
widespread
human
activity
occurring
on
seabed
is
bottom
trawling/dredging
fish
shellfish.
A
global
first‐order
estimate
suggested
mobile
demersal
fishing
activities
may
cause
0.16–0.4
Gt
organic
(OC)
to
be
remineralized
annually
from
sediment
(Sala
et
al.,
2021).
There
are,
however,
many
uncertainties
in
this
calculation.
Here,
we
discuss
potential
drivers
change
OC
due
conduct
a
literature
review,
synthesizing
studies
where
interaction
has
been
directly
investigated.
Under
certain
environmental
settings,
hypothesize
that
would
reduce
lower
production
flora
fauna,
loss
fine
flocculent
material,
increased
resuspension,
mixing
transport
oxygen
exposure.
Reductions
offset
varying
extents
by
reduced
faunal
bioturbation
community
respiration,
off‐shelf
increases
resuspension
nutrients.
Studies
which
investigated
impact
stocks
had
mixed
results.
finding
no
significant
effect
was
reported
61%
49
investigations;
29%
activities,
with
10%
reporting
higher
OC.
In
relation
remineralization
rates
within
seabed,
four
investigations
decreased
remineralization,
three
rates.
Patterns
experimental
characteristics
between
different
outcomes
were
largely
indistinct.
More
evidence
urgently
needed
accurately
quantify
anthropogenic
physical
disturbance
settings
incorporate
full
evidence‐based
considerations
into
management.
Frontiers in Marine Science,
Journal Year:
2020,
Volume and Issue:
7
Published: March 18, 2020
A
carbon
budget
for
the
northwest
European
continental
shelf
seas
(NWES)
was
synthesised
using
available
estimates
coastal,
pelagic
and
benthic
stocks
flows.
Key
uncertainties
were
identified
effect
of
future
impacts
on
assessed.
The
water
contains
between
210
230
Tmol
absorbs
1.3
3.3
from
atmosphere
annually.
Off-shelf
transport
burial
in
sediments
account
60-100%
0-40%
outputs
NWES,
respectively.
Both
these
fluxes
remain
poorly
constrained
by
observations
resolving
their
magnitudes
relative
importance
is
a
key
research
priority.
Pelagic
are
dominated
inorganic
carbon.
Shelf
contain
largest
stock
carbon,
with
520
1600
stored
top
0.1
m
sea
bed.
Coastal
habitats
such
as
salt
marshes
mud
flats
large
amounts
per
unit
area
but
total
small
compared
to
due
smaller
spatial
extent.
will
continue
increase
rising
concentration
atmospheric
CO2,
associated
pH
decrease.
flows
also
likely
be
significantly
affected
increasing
acidity
temperature,
circulation
changes
net
impact
uncertain.
Benthic
temperature
acidity,
decreasing
oxygen
concentrations,
although
interrelated
uncertain
major
knowledge
gap.
bottom
trawling
unique
amongst
we
consider
that
it
widespread
directly
manageable,
its
vulnerable
level
rise
strongly
impacted
management
decisions.
Local,
national
regional
actions
have
potential
protect
or
enhance
storage,
ultimately
global
governance,
via
controls
emissions,
has
greatest
influence
long-term
fate
northwestern
shelf.
Frontiers in Marine Science,
Journal Year:
2020,
Volume and Issue:
7
Published: May 25, 2020
The
vast
majority
of
freshly
produced
oceanic
dissolved
organic
carbon
(DOC)
is
derived
from
marine
phytoplankton,
then
rapidly
recycled
by
heterotrophic
microbes.
A
small
fraction
this
DOC
survives
long
enough
to
be
routed
the
interior
ocean,
which
houses
largest
and
oldest
reservoir.
reactivity
depends
upon
its
intrinsic
chemical
composition
extrinsic
environmental
conditions.
Therefore,
recalcitrance
an
emergent
property
that
analytically
difficult
constrain.
New
isotopic
techniques
track
flow
through
individual
molecules
show
promise
in
unveiling
specific
biosynthetic
or
degradation
pathways
control
metabolic
turnover
accumulation
deep
ocean.
However,
a
multivariate
approach
required
constrain
current
fluxes
so
we
may
better
predict
how
cycling
will
altered
with
continued
climate
change.
Ocean
warming,
acidification,
oxygen
depletion
upset
balance
between
primary
production
reworking
DOC,
thus
modifying
amount
and/or
recalcitrant
DOC.
Climate
change
anthropogenic
activities
enhance
mobilization
terrestrial
stimulate
coastal
waters,
but
it
unclear
would
affect
flux
open
Here,
assess
knowledge
on
cycle
identify
research
gaps
must
addressed
successfully
implement
use
global
scale
models.
Geophysical Research Letters,
Journal Year:
2022,
Volume and Issue:
49(5)
Published: March 8, 2022
Abstract
Disturbance
of
marine
sediments
results
in
the
remineralization
sedimentary
organic
matter
(OM)
and
impacts
upon
natural
burial
processes.
Management
interventions
which
restrict
or
remove
activities
that
cause
seabed
disturbance
may
offer
effective
strategies
to
protect
most
vulnerable
these
shelf
sea
OM
stores,
offering
new
opportunities
deliver
climate
mitigation
actions.
While
largest
quantities
are
often
stored
expansive
offshore
regions
continental
shelves
might
therefore
suggest
appropriate
zones
for
management
our
highlight
generally
contain
low
reactivity.
Conversely,
inshore
coastal
store
significant
highly
reactive
is
at
greater
risk
when
disturbed.
The
marked
spatial
disparities
between
reactivity
across
environments
highlights
need
focus
emergent
policy
future
toward
protection
sediments.
Nature Communications,
Journal Year:
2022,
Volume and Issue:
13(1)
Published: Aug. 20, 2022
Abstract
The
sediment-water
interface
in
the
coastal
ocean
is
a
highly
dynamic
zone
controlling
biogeochemical
fluxes
of
greenhouse
gases,
nutrients,
and
metals.
Processes
sediment
mixed
layer
(SML)
control
transfer
reactivity
both
particulate
dissolved
matter
interfaces.
Here
we
map
global
distribution
SML
based
on
excess
210
Pb
(
ex
)
profiles
then
use
neural
network
model
to
upscale
these
observations.
We
show
that
regions
such
as
large
estuaries
have
thicker
SMLs
than
most
oceanic
sediments.
Organic
carbon
preservation
are
inversely
related
mixing
stimulates
oxidation
sediments
which
enhances
organic
decomposition.
Sites
with
thickness
>60
cm
usually
lower
accumulation
rates
(<50
g
C
m
−2
yr
−1
total
carbon/specific
surface
area
ratios
(<0.4
mg
).
Our
scale
observations
reveal
reworking
can
accelerate
degradation
reduce
storage
Annual Review of Marine Science,
Journal Year:
2023,
Volume and Issue:
16(1), P. 335 - 360
Published: July 7, 2023
Human
civilization
relies
on
estuaries,
and
many
estuarine
ecosystem
services
are
provided
by
microbial
communities.
These
include
high
rates
of
primary
production
that
nourish
harvests
commercially
valuable
species
through
fisheries
aquaculture,
the
transformation
terrestrial
anthropogenic
materials
to
help
ensure
water
quality
necessary
support
recreation
tourism,
mutualisms
maintain
blue
carbon
accumulation
storage.
Research
ecology
underlies
in
estuaries
has
expanded
greatly
across
a
range
environments,
including
water,
sediment,
biofilms,
biological
reefs,
stands
seagrasses,
marshes,
mangroves.
Moreover,
application
new
molecular
tools
improved
our
understanding
diversity
genomic
functions
microbes.
This
review
synthesizes
recent
research
habitats
contributions
microbes
food
webs,
elemental
cycling,
interactions
with
plants
animals,
highlights
novel
insights
advances
genomics.
Global Ecology and Biogeography,
Journal Year:
2025,
Volume and Issue:
34(1)
Published: Jan. 1, 2025
ABSTRACT
Aim
We
assess
the
role
of
spatial
distance
and
depth
difference
in
shaping
beta
diversity
patterns
across
abyssal
seascape
regions.
measured
decrease
faunistic
similarity
northeast
Pacific
seafloor,
to
test
whether
species
turnover
rates
differ
between
deep
shallow‐abyssal
biogeographical
provinces
these
vary
functionally
or
taxonomically
different
biotic
groups.
Location
Abyssal
NE
Ocean.
Time
Period
Present.
Major
Taxa
Studied
Benthic
Invertebrates
(13
Phyla).
Methods
examined
relationship
compositional
(𝛽
sim
)
distance,
distance‐decay,
benthic
megafauna
communities
(animals
>
10
mm)
based
on
seabed
imagery
data
(>
36,000
specimens
402
species)
collected
28
locations
spanning
a
total
4000
km.
By
comparing
statistical
parameters
(intercept
slope)
decay
curves,
we
investigated
distance‐decay
(i)
above
below
carbonate
compensation
(~4400
m
at
N
Pacific),
(ii)
among
taxa
with
contrasting
life‐habits
dominant
phyla.
Results
found
steeper
4400
variations
Turnover
was
higher
for
facultatively
growing
hard‐substratum
patches
(polymetallic
nodules)
than
sediment‐dwelling
swimming
organisms.
Cnidaria
Porifera,
respectively,
depicted
most
least
evident
decays
community
similarity.
Main
Conclusions
demonstrate
utility
combining
imaging
modelling
capture
macroecological
poorly
explored
deep‐sea
ecosystems.
Our
results
suggest
that
chemical
boundaries
associated
are
very
relevant
niche‐sorting
mechanism
driving
large‐scale
beta‐diversity
an
association
dispersal
limitation
communities.
These
findings
have
important
implications
biodiversity
conservation
plans
ocean,
amid
need
protect
vast
ecosystems
from
globally
rising
human
threats.