Geological Society London Special Publications,
Journal Year:
2022,
Volume and Issue:
529(1), P. 195 - 222
Published: Dec. 15, 2022
Abstract
Evaluating
the
history
of
human
impacts
on
marine
ecosystems
based
sediment
cores
is
challenging
shelves
characterized
by
very
slow
sedimentation.
To
assess
stratigraphic
expression
such
in
condensed
deposits
an
epicontinental
sea,
we
analysed
a
3
m-long
core
collected
at
31
m
water
depth
off
Po
prodelta
Northern
Adriatic
Sea
integrating
geochronological
(
14
C
and
210
Pb),
sedimentological,
geochemical
palaeontological
proxies.
A
depositional
last
10
000
years
expressed
four
different
facies:
(1)
alluvial
floodplain,
(2)
transitional,
shell-poor
silts,
(3)
30
cm-thick
shell
lag,
(4)
layer
distal
silts
comprising
c.
500
years.
000-year-old
shells
Lentidium
mediterraneum
spread
over
lag
sediments
document
onshore
transport
during
early
Holocene
sea-level
rise.
Varicorbula
gibba
are
age-homogeneous
within
subsurface
documenting
decimetre-scale
mixing
bioturbation
past.
However,
spite
low
sedimentation
rates,
organic
heavy
metal
enrichment,
increase
proportional
abundance
benthic
foraminifers
preferring
organic-rich
Nonionella
sp.),
size
molluscs
V.
)
upper
cm
formed
still
detect
eutrophication
this
region
twentieth
century.
These
proxies
preserved
record
owing
to
temporarily
increasing
rate
decreasing
depth.
Palaios,
Journal Year:
2023,
Volume and Issue:
38(3), P. 148 - 157
Published: March 31, 2023
Abstract
Surficial
shell
accumulations
from
shallow
marine
settings
are
typically
averaged
over
centennial-to-millennial
time
scales
and
dominated
by
specimens
that
died
in
the
most
recent
centuries,
resulting
strongly
right-skewed
age-frequency
distributions
(AFDs).
However,
AFDs
modern
offshore
(outer
shelf
uppermost
continental
slope)
still
need
to
be
explored.
Using
individually
dated
shells
(14C-calibrated
amino
acid
racemization),
we
compared
along
an
onshore-offshore
gradient
across
southern
Brazilian
shelf,
with
sites
ranging
inner
shallow-water
(<
40
m)
offshore,
deep-water
(>
100
settings.
The
duration
of
averaging
is
slightly
higher
deeper
water
environments,
AFD
shapes
change
depositional
profile.
due
dominance
millennia
(median
age
range:
0–3
ka).
In
contrast,
on
outer
slope,
symmetrical
left-skewed
following
Last
Glacial
Maximum
15–18
changes
observed
properties
AFDs—increased
median
decreased
skewness,
but
only
increased
temporal
mixing—likely
reflect
sea
level
concurrent
depth-related
biological
productivity.
These
results
suggest
a
passive
margin
subject
post-glacial
sea-level
changes,
magnitude
time-averaging
assemblages
less
variable
profile
than
assemblage
ages
AFDs.
Geological Society London Special Publications,
Journal Year:
2023,
Volume and Issue:
529(1), P. 1 - 39
Published: March 29, 2023
Abstract
Conservation
palaeobiology
informs
conservation
and
restoration
of
ecosystems
by
using
the
fossil
record
to
discriminate
between
baseline
novel
states
assess
ecosystem
response
perturbations.
Variability
in
time-scale
palaeobiological
data
can
generate
patterns
that
either
exaggerate
or
mute
magnitude
biotic
changes.
We
identify
two
approaches
remedy
challenges
associated
with
mixing
post-impact
transformation
stratigraphic
depth
time.
First,
combining
surface
death
assemblages
both
(1)
preserved
subsurface
historical
layers
(2)
living
better
resolve
nature
shifts
than
within-core
surveys
live–dead
analyses
alone.
Second,
post-mortem
age
distributions
skeletal
particles
their
preservation
are
not
only
informative
about
resolution
time
averaging
but
also
timing
changes
abundance
producers.
High
youngest
cohorts
is
a
null
expectation
disintegration
burial
dynamic.
When
this
dynamic
accounted
for,
benthic
invertebrates
from
Holocene
sediments
often
reveal
high
volatility,
prolonged
turn-offs
production
pervasive
regime
obscured
raw
record.
PeerJ,
Journal Year:
2023,
Volume and Issue:
11, P. e15574 - e15574
Published: July 11, 2023
Although
the
fossil
record
preserves
a
wealth
of
historical
data
about
past
ecosystems,
current
paradigm,
which
postulates
that
fossils
provide
faithful
archives
ecological
information,
stems
from
research
primarily
focused
on
single
group
organisms
known
for
their
high
fossilization
potential:
molluscs.
Here,
we
quantify
fidelity
higher
taxa
(six
phyla
and
11
classes)
by
comparing
live
communities
sympatric
dead
remains
(death
assemblages)
using
comprehensive
surveys
benthic
marine
invertebrates
coastal
habitats
in
North
Carolina
(U.S.A).
We
found
although
community
composition
differed
between
two
assemblages
across
classes,
these
differences
were
predictable
with
an
overabundance
robust
more
preservable
groups.
In
addition,
molluscs
appear
to
be
excellent
proxy
all
when
tracking
spatio-temporal
patterns
shifts
structure
variety
metrics,
including
measures
α
,
γ
β
diversity/evenness.
This
suggests
despite
filters
imposed
differential
preservation
time-averaging,
is
likely
reliable
respect
relative
comparisons
diversity
shallow
paleocommunities.
consistent
previous
work
indicating
death
can
yield
estimates
adequate
assessing
variability
ecosystems
existed
under
natural,
pre-anthropogenic
conditions.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(9), P. 2177 - 2188
Published: May 3, 2024
Abstract.
The
youngest
fossil
record
is
a
crucial
source
of
data
documenting
the
recent
history
marine
ecosystems
and
their
long-term
alteration
by
humans.
However,
human
activities
that
reshape
communities
habitats
also
alter
sedimentary
biological
processes
control
formation
archives
recording
those
impacts.
These
diverse
physical,
geochemical,
disturbances
include
changes
in
sediment
fluxes
due
to
alluvial
coastal
landscapes,
seabed
disturbance
bottom
trawling
ship
traffic,
ocean
acidification
deoxygenation,
removal
native
species,
introduction
invasive
ecosystem
engineers.
novel
modify
sedimentation
rates,
depth
intensity
mixing,
pore-water
saturation
state,
preservation
potential
skeletal
remains
–
parameters
controlling
completeness
spatiotemporal
resolution
record.
We
argue
humans
have
become
major
force
transforming
nature
ways
can
both
impede
improve
our
ability
reconstruct
past
ecological
climate
dynamics.
A
better
understanding
feedback
between
impacts
on
offers
new
research
opportunities
tools
for
interpreting
geohistorical
ongoing
anthropogenic
transformation
ocean.
Abstract
Shifts
in
the
magnesium
to
calcium
ratio
of
seawater
geological
history
are
thought
have
profoundly
affected
biomineralization
marine
invertebrates,
including
some
echinoderms,
which
changed
their
skeletal
mineralogy
from
high-magnesium
low-magnesium
calcite
and
vice
versa.
Here
we
report
on
experiments
that
aimed
investigate
effect
ambient
nanomechanical
properties
spines
two
echinoid
species
(
Arbacia
lixula
Paracentrotus
lividus
).
We
found
echinoids
cultured
with
a
low
produced
skeleton
lower
both
content
nanohardness
than
those
control
specimens
incubated
under
normal
(high)
conditions.
These
results
may
suggest
at
certain
times
past
(during
so-called
seas)
sea
urchins
decreased
contents
were
more
susceptible
damage
due
physical
disturbances,
predation
post-mortem
taphonomic
processes.
Increased
hardness
aragonite
seas
is
expected
enhance
potential,
thus,
extent,
mitigates
preservation
bias
related
increased
solubility
calcite.
Paleobiology,
Journal Year:
2024,
Volume and Issue:
unknown, P. 1 - 28
Published: Nov. 7, 2024
Abstract
Bioturbation
can
increase
time
averaging
by
downward
and
upward
movements
of
young
old
shells
within
the
entire
mixed
layer
accelerating
burial
into
a
sequestration
zone
(SZ),
allowing
them
to
bypass
uppermost
taphonomically
active
(TAZ).
However,
bioturbation
shell
disintegration
concurrently,
neutralizing
positive
effects
mixing
on
averaging.
Bioirrigation
oxygenated
pore-water
promotes
carbonate
dissolution
in
TAZ,
biomixing
itself
mill
weakened
or
microbial
maceration,
and/or
expose
damage
at
sediment–water
interface.
Here,
we
fit
transition
rate
matrices
bivalve
age–frequency
distributions
from
four
sediment
cores
southern
California
middle
shelf
(50–75
m)
assess
competing
averaging,
exploiting
strong
gradient
rates
accumulation
created
historic
wastewater
pollution.
We
find
that
covaries
positively
with
all
sites,
accord
scenario
where
ultimately
fuels
disintegration.
Both
decline
abruptly
base
20-
40-cm-thick,
age-homogenized
surface
three
well-bioturbated
despite
different
accumulation.
In
contrast,
are
very
low
upper
25
cm
an
effluent
site
legacy
toxicity,
recolonization
bioirrigating
lucinid
bivalves.
Assemblages
formed
during
maximum
emissions
vary
strongly
millennial
scales
low-sediment
non-effluent
centennial
scale
was
high
but
recovered
quickly,
decadal
second
high-sedimentation
remained
for
decades.
Thus,
even
though
covary
rates,
reducing
postmortem
survival,
has
net
effect
increasing
skeletal
remains
this
warm-temperate
siliciclastic
shelf.
Paleobiology,
Journal Year:
2023,
Volume and Issue:
49(3), P. 527 - 562
Published: Jan. 19, 2023
Abstract
Understanding
how
time
averaging
changes
during
burial
is
essential
for
using
Holocene
and
Anthropocene
cores
to
analyze
ecosystem
change,
given
the
many
ways
in
which
affects
biodiversity
measures.
Here,
we
use
transition-rate
matrices
explore
extent
of
downcore
as
shells
transit
through
a
taphonomically
complex
mixed
layer
into
permanently
buried
historical
layers:
this
null
model,
without
any
temporal
rates
sedimentation
or
bioturbation,
contrast
with
patterns
that
might
be
produced
by
human
activity.
Assuming
stochastic
exhumation
movements
between
increments
within
disintegration
increments,
find
almost
all
combinations
net
sedimentation,
mixing,
produce
increase
(interquartile
range
[IQR]
shell
ages),
trend
typically
associated
decrease
kurtosis
skewness
shift
from
right-skewed
symmetrical
age
distributions.
A
thus
expectation
wherever
bioturbation
generates
an
internally
structured
(i.e.,
surface,
well-mixed
underlain
incompletely
layer):
under
these
conditions,
are
throughout
entire
at
slower
rate
than
they
below
it
sedimentation.
This
created
mixing
further
amplified
decline
rate.
We
accurately
reproduce
IQR,
skewness,
observed
bivalve
assemblages
southern
California
shelf.
The
age-frequency
distributions
typical
surface
death
assemblages—the
focus
most
actualistic
research—might
fossilized
exceptional
conditions
episodic
anoxia
sudden
burial.
However,
such
will
not
survive
subsurface
geologically
transient.
deep-time
fossil
record
dominated
instead
more
time-averaged
weakly
skewed
form
lower
parts
layer.
Cambridge Prisms Extinction,
Journal Year:
2023,
Volume and Issue:
1
Published: Jan. 1, 2023
Near-time
conservation
palaeobiology
uses
palaeontological,
archaeological
and
other
geohistorical
records
to
study
the
late
Quaternary
transition
of
biosphere
from
its
pristine
past
present-day,
human-altered
state.
Given
scarcity
data
on
recent
extinctions
in
oceans,
are
critical
for
documenting
human-driven
extinction
threats
marine
realm.
The
historical
perspective
can
provide
two
key
insights.
First,
archive
state
pre-industrial
oceans
at
local,
regional
global
scales,
thus
enabling
detection
extirpations
as
well
shifts
species
distribution,
abundance,
body
size
ecosystem
function.
Second,
we
untangle
contributions
natural
anthropogenic
processes
by
centennial-to-millennial
changes
composition
diversity
ecosystems
before
after
onset
major
human
impacts.
This
long-term
identifies
recently
emerging
patterns
that
unprecedented,
allowing
us
better
assess
biodiversity.
Although
global-scale
not
documented
brackish
invertebrates,
studies
point
numerous
extirpations,
declines
functions,
increases
range
fragmentation
dwindling
abundance
previously
widespread
species,
indicating
accumulating
a
debt.
Geological Society London Special Publications,
Journal Year:
2023,
Volume and Issue:
529(1), P. 243 - 262
Published: Feb. 16, 2023
Abstract
Otolith
death
assemblages
provide
a
valuable
source
of
biological
and
ecological
information
that
can
help
address
three
main
problems
in
marine
conservation:
(a)
the
lack
pre-industrial,
pre-human-impact
baselines
for
evaluating
change;
(b)
inefficiency
survey
methods
recording
small
cryptic
fish
species;
(c)
absence
long-term
data
on
environmental
change
impacts
ecosystems
fishes.
We
review
here
current
knowledge
formation
preservation
otoliths
their
assemblages,
to
obtain,
date
analyse
them
order
detect
changes
species
traits
ecology,
population
structure
palaeoceanographic
shifts
drove
them.