Paleobiology,
Год журнала:
2018,
Номер
44(4), С. 575 - 602
Опубликована: Авг. 16, 2018
Abstract
Estimating
the
effects
and
timing
of
anthropogenic
impacts
on
composition
macrobenthic
communities
is
challenging,
because
early
twentieth-century
surveys
are
sparse
corresponding
intervals
in
sedimentary
sequences
mixed
by
bioturbation.
Here,
to
assess
eutrophication
northern
Adriatic
Sea,
we
account
for
mixing
with
dating
bivalve
Corbula
gibba
at
two
stations
high
accumulation
(Po
prodelta)
one
station
moderate
(Isonzo
prodelta).
We
find
that,
first,
pervasively
bioturbated
muds
typical
highstand
conditions
deposited
twentieth
century
were
replaced
relicts
flood
layers
content
total
organic
carbon
(TOC)
late
Po
prodelta.
The
shelly
Isonzo
prodelta
amalgamated
but
also
show
an
upward
increase
TOC.
Second,
C.
shells
shows
that
shift
from
characterized
a
decrease
stratigraphic
disorder
temporal
resolution
assemblages
~25–50
years
~10–20
both
regions.
This
reflects
decline
depth
fully
layer
more
than
20
cm
few
centimeters.
Third,
abundance
opportunistic
species
loss
formerly
abundant,
hypoxia-sensitive
coincided
bioturbation,
higher
preservation
matter,
frequency
seasonal
hypoxia
depositional
ecosystem
regime
occurred
ca.
a.d.
1950.
Therefore,
enhanced
food
supply
overwhelmed
oxygen
depletion,
even
when
hypoxic
limited
weeks
per
year
Sea.
Preservation
trends
molluscan
events
cores
was
reduced
bioturbation
century.
Evidence
of
an
Anthropocene
epoch
Humans
are
undoubtedly
altering
many
geological
processes
on
Earth—and
have
been
for
some
time.
But
what
is
the
stratigraphic
evidence
officially
distinguishing
this
new
human-dominated
time
period,
termed
“Anthropocene,”
from
preceding
Holocene
epoch?
Waters
et
al.
review
climatic,
biological,
and
geochemical
signatures
human
activity
in
sediments
ice
cores.
Combined
with
deposits
materials
radionuclides,
as
well
human-caused
modification
sedimentary
processes,
stands
alone
stratigraphically
a
beginning
sometime
mid–20th
century.
Science
,
issue
p.
10.1126/science.aad2622
Proceedings of the National Academy of Sciences,
Год журнала:
2018,
Номер
115(52), С. 13288 - 13293
Опубликована: Дек. 10, 2018
As
the
world
warms
due
to
rising
greenhouse
gas
concentrations,
Earth
system
moves
toward
climate
states
without
societal
precedent,
challenging
adaptation.
Past
offer
possible
model
systems
for
warming
of
coming
decades.
These
include
Early
Eocene
(ca.
50
Ma),
Mid-Pliocene
(3.3-3.0
Last
Interglacial
(129-116
ka),
Mid-Holocene
(6
preindustrial
1850
CE),
and
20th
century.
Here,
we
quantitatively
assess
similarity
future
projected
these
six
geohistorical
benchmarks
using
simulations
from
Hadley
Centre
Coupled
Model
Version
3
(HadCM3),
Goddard
Institute
Space
Studies
E2-R
(GISS),
Community
Climate
System
Model,
Versions
4
(CCSM)
models.
Under
Representative
Concentration
Pathway
8.5
(RCP8.5)
emission
scenario,
by
2030
CE,
climates
most
closely
resemble
climates,
2150
they
climates.
RCP4.5,
stabilizes
at
Pliocene-like
conditions
2040
CE.
Eocene-like
emerge
first
in
continental
interiors
then
expand
outward.
Geologically
novel
are
uncommon
RCP4.5
(<1%)
but
reach
8.7%
globe
under
RCP8.5,
characterized
high
temperatures
precipitation.
Hence,
is
roughly
equivalent
stabilizing
while
unmitigated
trajectories,
such
as
similar
reversing
millions
years
long-term
cooling
on
scale
a
few
human
generations.
Both
emergence
geologically
rapid
reversion
may
be
outside
range
evolutionary
adaptive
capacity.
Quaternary Research,
Год журнала:
2018,
Номер
89(1), С. 156 - 177
Опубликована: Янв. 1, 2018
Abstract
The
Neotoma
Paleoecology
Database
is
a
community-curated
data
resource
that
supports
interdisciplinary
global
change
research
by
enabling
broad-scale
studies
of
taxon
and
community
diversity,
distributions,
dynamics
during
the
large
environmental
changes
past.
By
consolidating
many
kinds
into
common
repository,
lowers
costs
paleodata
management,
makes
paleoecological
openly
available,
offers
high-quality,
curated
resource.
Neotoma’s
distributed
scientific
governance
model
flexible
scalable,
with
open
pathways
for
participation
new
members,
contributors,
stewards,
communities.
supports,
or
can
be
extended
to
support,
any
kind
paleoenvironmental
from
sedimentary
archives.
Data
additions
are
growing
now
include
>3.8
million
observations,
>17,000
datasets,
>9200
sites.
Dataset
types
currently
fossil
pollen,
vertebrates,
diatoms,
ostracodes,
macroinvertebrates,
plant
macrofossils,
insects,
testate
amoebae,
geochronological
data,
recently
added
organic
biomarkers,
stable
isotopes,
specimen-level
data.
Multiple
avenues
exist
obtain
including
Explorer
map-based
interface,
an
application
programming
neotoma
R
package,
digital
object
identifiers.
As
volume
variety
grow,
resources
such
as
have
become
foundational
infrastructure
big
science.
Looking
back
to
move
forward
The
current
impacts
of
humanity
on
nature
are
rapid
and
destructive,
but
species
turnover
change
have
occurred
throughout
the
history
life.
Although
there
is
much
debate
about
best
approaches
take
in
conservation,
ultimately,
we
need
permit
or
enhance
resilience
natural
systems
so
that
they
can
continue
adapt
function
into
future.
In
a
Review,
Barnosky
et
al.
argue
way
do
this
look
at
paleontological
as
understand
how
ecological
maintained,
even
face
change.
Science
,
issue
p.
eaah4787
The Anthropocene Review,
Год журнала:
2015,
Номер
2(3), С. 196 - 219
Опубликована: Июнь 18, 2015
The
geological
record
preserves
evidence
for
two
fundamental
stages
in
the
evolution
of
Earth’s
biosphere,
a
microbial
stage
from
~3.5
to
0.65
Ga,
and
metazoan
evident
by
c.
650
Ma.
We
suggest
that
modern
biosphere
differs
significantly
these
previous
shows
early
signs
new,
third
characterised
by:
(1)
global
homogenisation
flora
fauna;
(2)
single
species
(
Homo
sapiens)
commandeering
25–40%
net
primary
production
also
mining
fossil
(fossil
fuels)
break
through
photosynthetic
energy
barrier;
(3)
human-directed
other
species;
(4)
increasing
interaction
with
technosphere
(the
emergent
system
includes
humans,
technological
artefacts,
associated
social
networks).
These
unique
features
today’s
may
herald
new
era
planet’s
history
could
persist
over
timescales.
Using
the
past
to
inform
future
The
late
Quaternary
paleorecord,
within
∼130,000
years,
can
help
present-day
management
of
Earth's
ecosystems
and
biota
under
climate
change.
Fordham
et
al.
review
when
where
rapid
transitions
be
found
in
paleoclimate
record.
They
show
how
such
events
history
shape
our
understanding
consequences
global
warming,
including
rates
biodiversity
loss,
changes
ecosystem
structure
function,
degradation
goods
services
that
these
provide
humanity.
also
highlight
recent
developments
at
intersection
paleoecology,
paleoclimatology,
macroecology
opportunities
anticipate
manage
responses
species
changing
climates
Anthropocene.
Science
,
this
issue
p.
eabc5654
Plant Ecology & Diversity,
Год журнала:
2019,
Номер
12(3-4), С. 189 - 385
Опубликована: Май 4, 2019
Quaternary
(last
2.6
million
years)
botany
involves
studying
plant
megafossils
(e.g.
tree
stumps),
macrofossils
seeds,
leaves),
and
microfossils
pollen,
spores)
preserved
in
peat
bogs
lake
sediments.
Although
have
been
studied
since
the
late
eighteenth
century,
today
is
largely
dominated
by
pollen
analysis.Quaternary
analysis
just
over
100
years
old.
It
started
primarily
as
a
geological
tool
for
correlation,
relative
dating,
climate
reconstruction.
In
1950
major
advance
occurred
with
publication
Knut
Fægri
Johs
Iversen
of
their
Text-book
Modern
Pollen
Analysis
which
provided
foundations
botanical
ecological
past
dynamics
biota
biotic
systems.
The
development
radiocarbon
dating
1950s
freed
from
being
dating.
As
result
these
developments,
became
valuable
implement
long-term
ecology
biogeography.Selected
contributions
that
has
made
to
biogeography
are
reviewed.
They
fall
into
four
general
parts:
(1)
aspects
interglacial
glacial
stages
such
location
nature
glacial-stage
refugia
soil
glaciated
unglaciated
areas;
(2)
responses
environmental
change
(spreading,
extinction,
persistence,
adaptation);
(3)
topics
potential
niches,
vegetation,
forest
dynamics;
(4)
its
application
human
impact
tropical
systems,
conservation
changing
world,
island
palaeoecology,
plant–animal
interactions,
biodiversity
patterns
time.The
future
briefly
discussed
10
suggestions
presented
help
strengthen
it
links
biogeography.
much
contribute
when
used
conjunction
new
approaches
ancient-DNA,
molecular
biomarkers,
multi-proxy
palaeoecology.
Proceedings of the National Academy of Sciences,
Год журнала:
2023,
Номер
120(7)
Опубликована: Фев. 6, 2023
Paleontology
has
provided
invaluable
basic
knowledge
on
the
history
of
life
Earth.
The
discipline
can
also
provide
substantial
to
societal
challenges
such
as
climate
change.
long-term
perspective
change
impacts
natural
systems
is
both
a
unique
selling
point
and
major
obstacle
becoming
more
pertinent
for
policy-relevant
bodies
like
Intergovernmental
Panel
Climate
Change
(IPCC).
Repeated
experiments
without
anthropogenic
disturbance
facilitate
extraction
triggers
in
biodiversity
changes.
At
same
time,
long
timescales
over
which
paleontological
changes
are
usually
assessed
beyond
scope
policymakers.
Based
first-hand
experience
with
IPCC
quantitative
analysis
its
cited
literature,
we
argue
that
differences
temporal
less
an
issue
than
inappropriate
framing
reporting
most
publications.
Accepting
some
obstacles
will
remain,
paleontology
quickly
improve
relevance
by
targeting
directly
focusing
effect
sizes
projections,
particularly
higher-end
scenarios.
Evolutionary Biology,
Год журнала:
2017,
Номер
44(4), С. 451 - 475
Опубликована: Окт. 24, 2017
Approaches
to
macroevolution
require
integration
of
its
two
fundamental
components,
within
a
hierarchical
framework.
Following
companion
paper
on
the
origin
variation,
I
here
discuss
sorting
an
evolutionary
hierarchy.
Species
sorting-sometimes
termed
species
selection
in
broad
sense,
meaning
differential
origination
and
extinction
owing
intrinsic
biological
properties-can
be
split
into
strict-sense
selection,
which
rate
differentials
are
governed
by
emergent,
species-level
traits
such
as
geographic
range
size,
effect
macroevolution,
rates
organism-level
body
size;
both
processes
can
create
hitchhiking
effects,
indirectly
causing
proliferation
or
decline
other
traits.
Several
methods
operationalize
concept
emergence,
so
that
rigorous
separation
these
is
increasingly
feasible.
A
macroevolutionary
tradeoff,
underlain
influence
dynamics,
causes
speciation
covary
many
clades,
resulting
volatility
some
clades
more
subdued
behavior
others;
few
break
tradeoff
achieve
especially
prolific
diversification.
In
addition
at
multiple
levels,
extrinsic
events
drive
waxing
waning
interaction
difficult
but
important
disentangle.
Evolutionary
trends
arise
ways,
any
level;
descriptive
models
fitted
clade
trajectories
phenotypic
functional
spaces,
they
may
not
diagnostic
regarding
processes,
close
attention
must
paid
leading
trailing
edges
apparent
trends.
Biotic
interactions
have
negative
positive
effects
taxonomic
diversity
clade,
cannot
readily
extrapolated
from
nature
organismic
level.
The
relationships
among
currencies
through
time
(taxonomic
richness,
morphologic
disparity,
variety)
crucial
for
understanding
novel
approach
diversity-disparity
analysis
shows
diversifications
lag
behind,
occur
concert
with,
precede,
increases
disparity.
Some
overarching
issues
relating
phenotypes
include
role
mass
extinctions,
potential
differences
between
plant
animal
whether
changed
geologic
time,
growing
human
impact
present-day
macroevolution.
Many
challenges
remain,
progress
being
made
key
ones:
(a)
variation-generating
mechanisms
multilevel
act
(b)
paleontological
neontological
approaches
historical
biology.
Molecular Ecology,
Год журнала:
2019,
Номер
29(2), С. 218 - 246
Опубликована: Ноя. 23, 2019
Genetic
time-series
data
from
historical
samples
greatly
facilitate
inference
of
past
population
dynamics
and
species
evolution.
Yet,
although
climate
landscape
change
are
often
touted
as
post-hoc
explanations
biological
change,
our
understanding
influences
on
evolutionary
processes
is
severely
hindered
by
the
limited
application
methods
that
directly
relate
environmental
to
through
time.
Increased
integration
spatiotemporal
genetic
will
revolutionize
interpretation
quantification
recent
anthropogenic
impacts
species,
vastly
improve
prediction
responses
under
future
scenarios,
yielding
widespread
revelations
across
biology,
ecology
conservation
genetics.
This
review
encourages
greater
use
analyses
explicitly
link
landscape,
time
providing
an
overview
analytical
approaches
for
integrating
in
five
key
research
areas:
structure,
demography,
phylogeography,
metapopulation
connectivity
adaptation.
We
also
include
a
tabular
summary
methodological
information,
suggest
mitigating
particular
difficulties
applying
these
techniques
ancient
DNA
palaeoclimate
data,
highlight
areas
development.