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.
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.
Earth-Science Reviews,
Journal Year:
2023,
Volume and Issue:
239, P. 104366 - 104366
Published: Feb. 26, 2023
The
current
understanding
of
the
origins
modern
carbonate
muds
and
their
early
stages
transformations
are
reviewed.
fine-grained
nature
such
sediments
makes
them
susceptible
to
intensive
structural
chemical
alteration
at
relatively
shallow
burial
depths
driven
especially
by
mineral
instability
under
microbially
mediated
reactions
within
sediment
associated
with
decay
organic
matter.
Whereas
transformation
high
Mg
calcite
(HMC)
low
magnesian
(LMC)
generally
takes
place
incongruently
in
situ,
that
aragonite
is
predominantly
via
congruent
dissolution.
loss
produces
a
huge
potential
flux
which
translocated
sediment.
Parallel
studies
on
Quaternary
sediments,
investigations
stratigraphic
record
have
shown
low-energy
settings
component
leads
formation
diagenetic
bedding
(such
as
limestone-marl-alternations
or
LMAs),
related
bipartite
lithologies,
some
types
hardgrounds,
secondary
mudrocks,
significant
modification
original
skeletal
biota.
There
uncertainties
exact
sources
for
precursor
aragonite,
where
released
carbonates
reprecipitate
column,
how
much
(and
hence
carbon)
back-fluxed
water
this
affects
palaeoenvironmental
proxies,
environmental
distributions
these
processes.
evidence
from
record,
matter
was
able
accumulate
promoting
transformations,
changes
carbonate-rich
took
very
early,
(decametre
less)
depths,
affecting
what
we
now
see
micron
outcrop
scale.
complexity
inter-relationships
fundamental
processes
has
received
more
attention
recent
years,
though
implications
still
seem
remarkably
undervalued.
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.
The Depositional Record,
Journal Year:
2023,
Volume and Issue:
9(1), P. 152 - 173
Published: Jan. 20, 2023
Abstract
A
detailed
sedimentological
analysis
of
the
Palaeocene
Lockhart
Limestone
has
been
conducted
to
evaluate
depositional
environment,
diagenetic
processes
and
hydrocarbon
potential
eastern
margin
Upper
Indus
Basin.
From
bottom
top,
there
are
three
microfacies
recorded.
The
lower
microfacies,
composed
fine‐grained
micrite
some
dolomite,
reflect
low
energy
calm
palaeo‐current
in
shallower
section
(1–2
m)
inner
shelf
close
shore.
middle
contain
algae
that
suggest
5–15
m
water
depth,
especially
along
inner‐middle
shelf,
but
fractured
mixed
bioclasts
material
indicate
moderately
active
wave
base.
Progressing
from
a
gradual
shift
orthochem
allochem
components
is
observed.
top
dominated
by
massive
benthic
microfossils,
indicating
moderate
energy‐water
conditions
with
normal
salinity.
However,
presence
limestone
intraclasts
surrounded
microspar,
miliolids
nummulites
at
indicates
high‐energy
environment
increasing
salinity
depths
20
130
m.
These
findings
show
was
deposited
shallow
spanning
inner‐mid
shelf.
Diagenetic
observed
include
micritisation,
cementation,
dissolution,
replacement,
physical
chemical
compaction,
fracture
filling
calcite
cement.
represents
deepening
upward
sequence
below
system
tract
highstand
systems
regressive
could
good
reservoir
characteristics,
serve
as
an
excellent
rock,
be
primary
target
for
future
exploration.
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.
Anais da Academia Brasileira de Ciências,
Journal Year:
2025,
Volume and Issue:
97(2)
Published: Jan. 1, 2025
Abstract
Conservation
paleobiology,
an
expanding
field,
employs
taphonomy
tools
to
investigate
past
environmental
conditions
and
organisms
before
human
impacts,
thereby
addressing
key
conservation
issues.
This
review
examines
the
concepts,
approaches
events
in
emphasizing
aquatic
coastal
often-overlooked
contributions
from
Brazil
South
America.
America,
with
its
vulnerable
biodiversity,
unique
geology
rich
fossil
diversity,
is
a
natural
laboratory
for
understanding
ecosystems—a
considerable
potential
as
center
leading
paleobiology
research.
However,
America
underrepresented,
contributing
only
5%
of
total
publications
(67%
it
Brazil).
Most
American
authors
are
geoscientists
publishing
mainly
on
mollusks,
also
they
produced
fewer
studies
than
those
more
developed
countries.
Noteworthy,
Brazilian
National
Council
Scientific
Technological
Development
ranks
third
globally
funding
articles.
Clearly,
still
predominantly
practiced
nations
geoscience
fields.
Other
challenges
include
underutilization
geohistorical
data
gap
between
theory
practice.
To
address
these
issues,
future
should
integrate
conservationist
perspectives
align
them
societal
needs.
Hence,
anticipated
growth
could
bolster
promote
sustainability
generations.
BMC Ecology and Evolution,
Journal Year:
2024,
Volume and Issue:
24(1)
Published: Aug. 23, 2024
Abstract
Background
The
fossil
record
provides
the
unique
opportunity
to
observe
evolution
over
millions
of
years,
but
is
known
be
incomplete.
While
incompleteness
varies
spatially
and
hard
estimate
for
empirical
sections,
computer
simulations
geological
processes
can
used
examine
effects
in
silico
.
We
combine
different
modes
(stasis,
(un)biased
random
walks)
with
deposition
carbonate
platforms
strata
how
well
mode
recovered
from
time
series,
test
results
vary
between
positions
platform
multiple
stratigraphic
architectures
generated
by
sea
level
curves.
Results
Stratigraphic
architecture
position
along
an
onshore-offshore
gradient
has
only
a
small
influence
on
statistical
tests.
For
walks,
support
correct
decreases
series
length.
Visual
examination
trait
lineages
shows
that
rather
than
incompleteness,
maximum
hiatus
duration
determines
much
differ
original
evolutionary
process.
Gradual
directional
more
susceptible
effects,
turning
it
into
punctuated
evolution.
In
contrast,
stasis
remains
unaffected.
Conclusions
•
Fossil
favor
recognition
both
complex,
Not
presence
rare,
prolonged
gaps
largest
effect
This
suggests
incomplete
sections
regular
frequency
durations
potentially
preserve
history
without
major
biases.
Understanding
external
controls
such
as
fluctuations
crucial
distinguishing
genuine
Journal of Evolutionary Biology,
Journal Year:
2024,
Volume and Issue:
37(12), P. 1413 - 1432
Published: Aug. 29, 2024
Abstract
The
relationship
between
the
evolutionary
dynamics
observed
in
contemporary
populations
(microevolution)
and
evolution
on
timescales
of
millions
years
(macroevolution)
has
been
a
topic
considerable
debate.
Historically,
this
debate
centers
inconsistencies
microevolutionary
processes
macroevolutionary
patterns.
Here,
we
characterize
striking
exception:
emerging
evidence
indicates
that
standing
variation
rates
phenotypic
divergence
is
often
positively
correlated.
This
apparent
consistency
micro-
macroevolution
paradoxical
because
it
contradicts
our
previous
understanding
so
far
unexplained.
explore
prospects
for
bridging
through
an
examination
“paradox
predictability.”
We
begin
by
explaining
why
divergence–variance
correlation
paradox,
followed
data
analysis
to
show
general
phenomenon
across
broad
range
temporal
scales,
from
few
generations
tens
years.
Then
review
complementary
approaches
quantitative
genetics,
comparative
morphology,
evo-devo,
paleontology
argue
they
can
help
address
paradox
shared
vantage
point
recent
work
evolvability.
In
conclusion,
recommend
methodological
orientation
combines
different
kinds
short-term
long-term
using
multiple
analytical
frameworks
interdisciplinary
research
program.
Such
program
will
increase
how
works
within
timescales.