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.
Global Change Biology,
Год журнала:
2022,
Номер
28(13), С. 4041 - 4053
Опубликована: Апрель 12, 2022
Abstract
Preserving
adaptive
capacities
of
coastal
ecosystems,
which
are
currently
facing
the
ongoing
climate
warming
and
a
multitude
other
anthropogenic
impacts,
requires
an
understanding
long‐term
biotic
dynamics
in
context
major
environmental
shifts
prior
to
human
disturbances.
We
quantified
responses
nearshore
mollusk
assemblages
sea‐level
changes
using
223
samples
(~71,300
specimens)
retrieved
from
latest
Quaternary
sediment
cores
Adriatic
systems.
These
provide
rare
chance
study
systems
that
existed
during
glacial
lowstands.
The
fossil
record
indicates
penultimate
interglacial
(Late
Pleistocene)
shifted
their
faunal
composition
subsequent
ice
age,
then
reassembled
again
with
return
Holocene.
point
climate‐driven
habitat
filtering
modulated
by
dispersal
processes.
resilient,
rather
than
persistent
or
stochastic,
response
over
at
least
125
thousand
years
highlights
historically
unprecedented
nature
stressors
(e.g.,
pollution,
eutrophication,
bottom
trawling,
invasive
species)
shifting
regions
into
novel
system
states
far
outside
range
natural
variability
archived
record.
Geology,
Год журнала:
2022,
Номер
50(8), С. 902 - 906
Опубликована: Май 9, 2022
Abstract
Time
averaging
of
fossil
assemblages
determines
temporal
precision
paleoecological
and
geochronological
inferences.
Taxonomic
differences
in
intrinsic
skeletal
durability
are
expected
to
produce
mismatch
between
co-occurring
species,
but
the
importance
this
effect
is
difficult
assess
due
lack
direct
estimates
time
for
many
higher
taxa.
Moreover,
burial
below
taphonomic
active
zone
early
diagenetic
processes
may
alleviate
taxonomic
disintegration
rates
subsurface
sediments.
We
compared
across
five
phyla
major
carbonate
producers
a
sediment
core
from
northern
Adriatic
Sea
shelf.
dated
individual
bivalve
shells,
foraminiferal
tests,
tests
isolated
plates
irregular
regular
echinoids,
crab
claws,
fish
otoliths.
In
spite
different
architecture,
mineralogy,
life
habit,
all
taxa
showed
very
similar
varying
~1800
~3600
yr
(interquartile
age
ranges).
Thus,
remains
echinoids
crustaceans—two
groups
with
multi-elemental
skeletons
assumed
have
low
preservation
potential—can
still
undergo
extensive
mixing
comparable
that
mollusk
shells.
The
median
ages
differed
by
as
much
~3700
yr,
reflecting
species-specific
timing
seafloor
colonization
during
Holocene
transgression.
Our
results
congruent
sequestration
models
invoking
minimize
among
These
together
variability
production
can
overrule
effects
determining
resolution
multi-taxic
assemblages.
Proceedings of the Royal Society B Biological Sciences,
Год журнала:
2020,
Номер
287(1929), С. 20200695 - 20200695
Опубликована: Июнь 17, 2020
Palaeoecological
data
are
unique
historical
archives
that
extend
back
far
beyond
the
last
several
decades
of
ecological
observations.
However,
fossil
record
continental
shelves
has
been
perceived
as
too
coarse
(with
centennial-millennial
resolution)
and
incomplete
to
detect
processes
occurring
at
yearly
or
decadal
scales
relevant
ecology
conservation.
Here,
we
show
youngest
(Anthropocene)
on
northern
Adriatic
shelf
provides
decadal-scale
resolution
accurately
documents
an
abrupt
change
affecting
benthic
communities
during
twentieth
century.
The
magnitude
duration
century
shift
in
body
size
bivalve
Corbula
gibba
is
unprecedented
given
regional
populations
this
species
were
dominated
by
small-size
classes
throughout
Holocene.
coincided
with
compositional
changes
assemblages,
driven
increase
from
approximately
25%
70%
median
per-assemblage
abundance
C.
gibba.
This
regime
occurred
preferentially
sites
experienced
least
one
hypoxic
event
per
decade
Larger
higher
probably
reflect
release
it
coincides
frequency
seasonal
hypoxia
triggered
mass
mortality
competitors
predators.
Higher
events
coupled
a
decline
depth
intense
sediment
mixing
burrowing
organisms
decimetres
less
than
20
cm,
significantly
improving
stratigraphic
Anthropocene
making
possible
sub-centennial
shelves.
Geological Society London Special Publications,
Год журнала:
2023,
Номер
529(1), С. 1 - 39
Опубликована: Март 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,
Год журнала:
2023,
Номер
11, С. e15574 - e15574
Опубликована: Июль 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.
Sedimentology,
Год журнала:
2021,
Номер
69(3), С. 1083 - 1118
Опубликована: Авг. 22, 2021
Abstract
A
sequence
stratigraphic
framework
predicts
that
time
averaging
and
hiatus
durations
will
be
long
at
times
of
fastest
sea‐level
rise.
This
prediction
does
not
necessarily
apply
to
environments
where
carbonate
production
keeps
up
with
rise
undetected
hiatuses
decouple
short‐term
from
long‐term
sedimentation
rates.
The
taphonomic
clock,
however,
which
measures
the
residence
skeletal
particles
in
mixed
layer,
can
estimate
duration
if
rate
alteration
is
slow
endure
exposure
layer.
Here,
calibrated
by
using
evidence
bivalves
a
metre‐scale
Holocene
Adriatic
Sea.
In
this
sequence,
transgressive
molluscan
lags,
maximum‐flooding
zone
shell
bed
bivalves,
highstand
bryomol
assemblages
were
all
deposited
under
similar
rates
(
ca
0.01
0.03
cm
year
−1
)
exhibit
millennial
averaging.
Median
ages
valves
stained
pyrite
cemented
high‐magnesium
calcitic
micritic
envelopes
exceeding
1000
years
indicate
that:
(i)
these
authigenic
processes
are
subsurface
zones
reducing
conditions
(with
prolonged
sulphate
reduction
ions
sourced
dissolved
shells
surface
zones);
(ii)
micrite
precipitation
prolongs
disintegration
half‐lives
exhumed
decades
millennia.
high
abundance
valves,
envelopes,
composite
(encrusters
borers
colonizing
grains)
thus
identifies
concentrations
time‐averaged
>1000
years.
upcore
decrease
alteration,
coupled
temporally‐constant
averaging,
indicates
temporal
decline
sediment
exhumation
was
compensated
burial
produced
molluscs.
Geological Society London Special Publications,
Год журнала:
2022,
Номер
529(1), С. 293 - 310
Опубликована: Дек. 22, 2022
Abstract
Preserving
the
adaptive
capacities
of
coastal
ecosystems
in
Anthropocene
requires
an
understanding
their
natural
variability
prior
to
modern
times.
We
quantified
responses
nearshore
molluscs
assemblages
past
environmental
changes
using
101
samples
(
c.
57
300
specimens)
retrieved
from
subsurface
Holocene
succession
and
present-day
seabed
Po–Adriatic
System
(Italy).
Present-day
shifted
faunal
composition
with
respect
mid-late
counterparts.
Major
differences
are
observed
lower
settings,
where
show
higher
heterogeneity,
reduced
standardized
richness,
relative
abundance
Lentidium
mediterraneum,
increased
Varicorbula
gibba
,
scavengers
(genus
Tritia
),
deposit
feeders
(nuculid
bivalves).
A
dominance
infaunal
opportunistic
species
shifts
towards
detritus-feeding
scavenging
often
associated
disturbed
benthic
habitats.
Our
results
suggest
that
ongoing
anthropogenic
stressors
(mainly
bottom
trawling
non-native
species)
currently
shifting
communities
into
novel
states
outside
range
archived
fossil
record.
Supplementary
material:
document
containing
additional
statistics,
figures,
tables,
also
considering
different
filters
applied
molluscan
dataset,
is
provided
as
a
Word
file.
In
addition,
appendices
concerning
sample
taxa
information
R-scripts
.csv
.r
files.
These
available
at
https://doi.org/10.6084/m9.figshare.c.6351348
Geology,
Год журнала:
2020,
Номер
48(6), С. 589 - 593
Опубликована: Март 27, 2020
Abstract
Studies
of
paleocommunities
and
trophic
webs
assume
that
multispecies
assemblages
consist
species
coexisted
in
the
same
habitat
over
duration
time
averaging.
However,
even
with
similar
durability
can
differ
age
within
a
single
fossil
assemblage.
Here,
we
tested
whether
skeletal
remains
different
phyla
guilds,
most
abundant
infaunal
bivalve
shells
nektobenthic
fish
otoliths,
differed
radiocarbon
surficial
sediments
along
depth
gradient
from
10
to
40
m
on
warm-temperate
Israeli
shelf,
modeled
their
dynamics
taphonomic
loss.
We
found
that,
spite
higher
potential
fishes
for
out-of-habitat
transport
after
death,
differences
structure
depths
were
smaller
by
almost
an
order
magnitude
than
between
depths.
Shell
otolith
underwent
depth-specific
burial
pathways
independent
taxon
identity,
generating
death
comparable
averaging,
supporting
assumption
temporal
spatial
co-occurrence
mollusks
fishes.
Quaternary International,
Год журнала:
2024,
Номер
706, С. 49 - 59
Опубликована: Июль 22, 2024
Paleoreconstructions
of
coastal
and
near-coastal
areas
have
always
served
as
a
tool
towards
better
understanding
past,
present
future
geological
geomorphological
processes.
The
reliability
paleocoastline
sea-land
extent
modelling
is
controlled
by
input
data.
Here
the
difference
between
paleoreconstructions
based
on
present-day
bathymetry
paleotopographic
elevation
model
are
examined
example
Gulf
Trieste
(northern
Adriatic
sea)
-
low-gradient
submerged
Last
Glacial
Maximum
alluvial
plain
with
fairly
well-resolved
pre-transgressional
paleotopography.
Results
presented
in
this
study
show
striking
differences
spatial
two
modelled
sets
paleocoastlines
which
places
exceeds
tens
kilometers.
These
results
demonstrate
importance
using
an
appropriate
geologically-supported
for
paleoreconstruction
unsuitable
models
can
result
significant
errors
unreliable
reconstructions.
This
especially
noteworthy
settings
where
even
slight
variation
sea
level
affect
vast
areas.
Finally,
provide
insight
into
Early
Holocene
evolution
area
abrupt
predominant
northeasterly
oriented
transgression
direction
indicated
from