Biogeosciences,
Journal Year:
2021,
Volume and Issue:
18(22), P. 5929 - 5965
Published: Nov. 22, 2021
Abstract.
Although
the
depth
of
bioturbation
can
be
estimated
on
basis
ichnofabric,
timescale
sediment
mixing
(reworking)
and
irrigation
(ventilation)
by
burrowers
that
affects
carbonate
preservation
biogeochemical
cycles
is
difficult
to
estimate
in
stratigraphic
record.
However,
pyrite
linings
interior
shells
a
signature
slow
shallow
irrigation.
They
indicate
molluscs
initially
inhabiting
oxic
pockets
were
immediately
permanently
sequestered
reduced,
iron-rich
microenvironments
within
mixed
layer.
Molluscan
biomass-stimulated
sulfate
reduction
precipitation
was
confined
location
decay
under
such
conditions.
A
high
abundance
pyrite-lined
record
thus
diagnostic
limited
exposure
organic
tissues
O2
even
when
seafloor
inhabited
abundant
infauna
disrupting
age-homogenizing
sedimentary
fabric
as
present-day
northern
Adriatic
Sea.
Here,
we
reconstruct
this
sequestration
pathway
characterized
(1)
assessing
postmortem
ages
shallow-infaunal
hypoxia-tolerant
bivalve
Varicorbula
gibba
cores
(2)
evaluating
whether
an
independently
documented
decline
mixing,
driven
frequency
seasonal
hypoxia
during
20th
century,
affected
First,
at
prodelta
sites
with
sedimentation
rate,
framboids
form
rapidly
upper
5–10
cm
they
already
appear
interiors
younger
than
10
years
occur
preferentially
well-preserved
articulated
periostracum.
Second,
increments
deposited
early
century
contain
<
20
%
lined
Po
30
%–40
Isonzo
prodelta,
whereas
late
possess
50
%–80
both
locations.
At
low
(<
%–20
%).
Surface
sediments
remained
well
deposit
detritus
feeders
maintaining
suboxic
zone
dissolved
iron.
The
upcore
increase
indicates
oxycline
reduced
bioirrigation
rates
declined
century.
We
hypothesize
permanent
V.
subsurface
enabled
recovery
infaunal
communities
from
hypoxic
events,
leading
dominance
surficial
modifiers
potential.
presence
very
young
valves
uppermost
zones
layer
rapid
obrution
episodic
deposition
not
needed
for
transient
background
are
(here,
exceeding
∼
0.1
yr−1)
organisms
die
their
living
position
sediment.
Abundance
per
assemblage
apparently
well-mixed
deep-time
indicator
inefficient
bioirrigation.
Fine-grained
Sea
since
mid-20th
potential
formed
layer,
represent
taphonomic
diagenetic
analogues
skeletal
assemblages
linings.
Marine Environmental Research,
Journal Year:
2019,
Volume and Issue:
150, P. 104770 - 104770
Published: Aug. 7, 2019
Changes
in
community
structure
concurrent
with
environmental
forcing
often
form
a
precursor
to
changes
species
diversity,
and
can
have
substantive
consequences
for
ecosystem
functioning.
Here,
we
assess
the
effects
of
altered
levels
evenness
that
are
representative
different
eutrophication
salinity
associated
precipitation
patterns,
on
mediation
nutrient
release
by
sediment-dwelling
invertebrate
communities.
We
find
an
adjustment
towards
more
even
distribution
corresponds
increase
sediment
particle
reworking
that,
general,
translates
increased
release.
This
response,
however,
is
dependent
functional
role
each
influenced
concomitant
salinity,
especially
when
extends
beyond
range
typically
experienced
community.
Overall,
our
findings
highlight
dynamic
nature
contributions
functioning
reinforce
importance
understanding
when,
how,
mechanistic
basis
species-environment
interactions
modified
as
influence
abiotic
biotic
factors
flex
under
periods
directional
forcing.
Palaios,
Journal Year:
2021,
Volume and Issue:
36(2), P. 77 - 93
Published: Feb. 28, 2021
ABSTRACT
Actualistic
studies
are
important
for
evaluating
the
fidelity
of
fossil
assemblages
in
representing
living
community.
Poor
live-dead
(LD)
molluscan
may
result
from
transport-induced
mixing.
Large-scale
mixing
is
more
common
siliciclastic
settings
with
a
narrow
shelf,
high
sedimentation
rate,
and
those
that
frequented
by
episodically
high-energy
events.
Chandipur-on-sea,
on
east
coast
India
has
an
optimal
setting
to
promote
such
conditions.
By
studying
LD
modeling
size-frequency
distribution
(SFD)
fauna,
we
attempted
evaluate
contribution
“out-of-habitat”
versus
“within-habitat”
developing
death
assemblage.
The
correlation
between
composition
live
(LA)
(DA)
was
insufficient;
unlike
LAs,
DAs
do
not
show
environmental
partitioning
ordination
space.
A
numerical
simulation
shell
size
frequency
LAs
compared
observed
SFD
DAs.
results
this
indicate
likely
be
product
within-habitat
probably
received
considerable
input
via
regional
transport,
facilitated
frequent
tropical
cyclones
affecting
Odisha.
Chandipur
receives
large
proportion
originating
above
15°N,
which
causes
degree
lateral
transport
15°
21°N,
explained
compositional
similarity
species
within
latitudinal
extent.
Our
study
highlights
significance
out-of-habitat
shaping
marine
assemblages,
especially
storm
dominated
shallow-marine
settings.
Marine Ecology Progress Series,
Journal Year:
2021,
Volume and Issue:
671, P. 45 - 65
Published: June 2, 2021
Shallow
coastal
seas
play
an
important
role
in
the
economy
of
many
countries
by
sustaining
fisheries,
tourism,
aquaculture
and
other
economic
activities.
Their
exploitation
has
large-scale
ecosystem
effects
that
are
easily
overlooked,
as
they
often
built
up
over
decades
or
centuries,
historical
ecological
reference
data
rarely
available.
Here,
we
assess
these
comparing
live
surface
death
assemblages
(recording
community
states)
soft-bottom
molluscs
across
a
range
habitats
northern
Adriatic
Sea,
using
degree
mismatch
between
2
proxy
for
change.
We
found
consistent
live-dead
at
all
stations.
Although
varied
stations
with
low
high
time-averaging
(i.e.
post-mortem
shell
ages),
change
followed
same
trend
entire
basin
regardless
type
sedimentary
environment,
loss
epifaunal
species
reduction
grazers,
carnivores,
herbivores.
In
turn,
abundance
infaunal
opportunistic
feeding
on
plankton
detritus
strongly
increased
living
communities.
Directionality
magnitude
changes
cannot
be
explained
differences
durability,
but
reflect
true
shift
response
to
multiple,
long-lasting
anthropogenic
pressures,
mainly
bottom
trawling,
eutrophication
hypoxia.
The
original
heterogeneous
characteristic
different
thus
replaced
more
infaunal,
functionally
impoverished
less
diverse
benthic
representing
new
baseline
shaped
human
impact.
Geological Society London Special Publications,
Journal Year:
2023,
Volume and Issue:
529(1), P. 311 - 344
Published: Jan. 9, 2023
Abstract
Climate
change
is
undermining
the
health
and
integrity
of
seafloor
ecosystems,
with
declines
in
bioturbation
expected
to
impact
future
ecosystem
functioning.
We
explored
changes
nature
degree
during
Early
Jurassic
global
warming
ocean
deoxygenation.
Understanding
how
these
communities
responded
can
help
anticipate
functioning
might
over
large
spatial
temporal
scales.
Trace
body
fossils
from
outcrop
core
Cleveland
Basin,
UK
show
healthy
deteriorated
through
Pliensbachian
spinatum
Zone,
macroinfaunal
behaviour
fluctuated
across
Pliensbachian–Toarcian
boundary
coincident
mass
extinction.
Deoxygenation
began
above
stage
boundary,
conditions
until
ceased
completely
(upper
tenuicostatum
Zone)
for
0.6–2.5
Ma,
longer
than
anywhere
else
NW
Tethys.
The
record
revealed
new
details
on
progression
timing
deoxygenation,
benthic
recovery
fluctuations
palaeoredox
boundary.
After
oceanic
anoxic
event
infauna
were
fewer,
smaller
did
not
mix
sediments
depth,
while
depth
diversity
had
increased
by
fibulatum
Subzone
(
bifrons
Zone),
benthos
recovered
late
pre-oceanic
state.
Bioturbation
collapse
parts
Northern
Hemisphere
probably
contributed
regional-scale
Biogeosciences,
Journal Year:
2021,
Volume and Issue:
18(22), P. 5929 - 5965
Published: Nov. 22, 2021
Abstract.
Although
the
depth
of
bioturbation
can
be
estimated
on
basis
ichnofabric,
timescale
sediment
mixing
(reworking)
and
irrigation
(ventilation)
by
burrowers
that
affects
carbonate
preservation
biogeochemical
cycles
is
difficult
to
estimate
in
stratigraphic
record.
However,
pyrite
linings
interior
shells
a
signature
slow
shallow
irrigation.
They
indicate
molluscs
initially
inhabiting
oxic
pockets
were
immediately
permanently
sequestered
reduced,
iron-rich
microenvironments
within
mixed
layer.
Molluscan
biomass-stimulated
sulfate
reduction
precipitation
was
confined
location
decay
under
such
conditions.
A
high
abundance
pyrite-lined
record
thus
diagnostic
limited
exposure
organic
tissues
O2
even
when
seafloor
inhabited
abundant
infauna
disrupting
age-homogenizing
sedimentary
fabric
as
present-day
northern
Adriatic
Sea.
Here,
we
reconstruct
this
sequestration
pathway
characterized
(1)
assessing
postmortem
ages
shallow-infaunal
hypoxia-tolerant
bivalve
Varicorbula
gibba
cores
(2)
evaluating
whether
an
independently
documented
decline
mixing,
driven
frequency
seasonal
hypoxia
during
20th
century,
affected
First,
at
prodelta
sites
with
sedimentation
rate,
framboids
form
rapidly
upper
5–10
cm
they
already
appear
interiors
younger
than
10
years
occur
preferentially
well-preserved
articulated
periostracum.
Second,
increments
deposited
early
century
contain
<
20
%
lined
Po
30
%–40
Isonzo
prodelta,
whereas
late
possess
50
%–80
both
locations.
At
low
(<
%–20
%).
Surface
sediments
remained
well
deposit
detritus
feeders
maintaining
suboxic
zone
dissolved
iron.
The
upcore
increase
indicates
oxycline
reduced
bioirrigation
rates
declined
century.
We
hypothesize
permanent
V.
subsurface
enabled
recovery
infaunal
communities
from
hypoxic
events,
leading
dominance
surficial
modifiers
potential.
presence
very
young
valves
uppermost
zones
layer
rapid
obrution
episodic
deposition
not
needed
for
transient
background
are
(here,
exceeding
∼
0.1
yr−1)
organisms
die
their
living
position
sediment.
Abundance
per
assemblage
apparently
well-mixed
deep-time
indicator
inefficient
bioirrigation.
Fine-grained
Sea
since
mid-20th
potential
formed
layer,
represent
taphonomic
diagenetic
analogues
skeletal
assemblages
linings.