Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: Feb. 19, 2024
Abstract
The
Holocene
temperature
conundrum,
the
discrepancy
between
proxy-based
global
cooling
and
simulated
annual
warming
trends,
remains
controversial.
Meanwhile,
reconstructions
simulations
show
inconsistent
spatial
patterns
of
terrestrial
changes.
Here
we
report
alkenone
records
to
address
over
mid-latitude
Eurasia.
In
contrast
with
long-term
trends
in
warm
season
temperatures
northeastern
China,
from
southwestern
Siberia
are
characterized
by
colder
conditions
before
~6,000
years
ago,
thus
trends.
Together
existing
surrounding
regions,
infer
that
airmass
might
have
prevailed
interior
Eurasian
continent
during
early
mid-Holocene,
perhaps
associated
atmospheric
response
remnant
ice
sheets.
Our
results
challenge
proposed
seasonality
bias
proxies
modeled
study
region,
highlighting
changes
should
be
re-considered
record
integrations
model
simulations,
important
implications
for
hydroclimate
Annual Review of Earth and Planetary Sciences,
Journal Year:
2021,
Volume and Issue:
49(1), P. 609 - 641
Published: March 23, 2021
Throughout
Earth's
history,
CO
2
is
thought
to
have
exerted
a
fundamental
control
on
environmental
change.
Here
we
review
and
revise
reconstructions
from
boron
isotopes
in
carbonates
carbon
organic
matter
over
the
Cenozoic—the
past
66
million
years.
We
find
close
coupling
between
climate
throughout
Cenozoic,
with
peak
levels
of
∼1,500
ppm
Eocene
greenhouse,
decreasing
∼500
Miocene,
falling
further
into
ice
age
world
Plio–Pleistocene.
Around
two-thirds
Cenozoic
drawdown
explained
by
an
increase
ratio
ocean
alkalinity
dissolved
inorganic
carbon,
likely
linked
change
balance
weathering
outgassing,
remaining
one-third
due
changing
temperature
major
ion
composition.
Earth
system
sensitivity
explored
may
vary
different
time
intervals.
The
record
highlights
truly
geological
scale
anthropogenic
change:
Current
were
last
seen
around
3
years
ago,
cuts
emissions
are
required
prevent
return
Miocene
or
coming
century.
▪
Myr
alkenones
reviewed
re-evaluated.
estimates
proxies
show
agreement,
yielding
consistent
picture
evolution
ocean-atmosphere
Cenozoic.
coupled
Myr,
providing
broad
constraints
sensitivity.
Twenty-first-century
potential
not
since
much
warmer
climates
distant
past.
Environments,
Journal Year:
2023,
Volume and Issue:
10(4), P. 66 - 66
Published: April 14, 2023
The
increasing
levels
of
carbon
dioxide
(CO2)
in
the
atmosphere
have
become
a
major
environmental
challenge
due
to
their
contribution
global
warming.
primary
drivers
increase
atmospheric
CO2
concentrations
are
combustion
fossil
fuels,
deforestation,
agricultural
practices,
or
production
cement,
which
play
significant
role
concentration
atmosphere.
However,
efforts
being
made
mitigate
negative
effects
emissions,
including
capture
and
storage
(CCS)
technologies
that
aim
from
industrial
processes
store
it
underground
geological
formations.
Methane,
another
potent
greenhouse
gas,
is
contributor
climate
change
mainly
produced
by
activities
such
as
livestock
farming
rice
cultivation.
To
address
this,
sustainable
reducing
meat
consumption
adopting
climate-smart
techniques,
crucial.
Ultimately,
future
can
be
secured
for
planet
generations
implementing
effective
measures,
use
energy
sources,
improvements
efficiency,
responsible
land
emissions
both
methane.
Science,
Journal Year:
2023,
Volume and Issue:
379(6630)
Published: Jan. 26, 2023
Amazonian
environments
are
being
degraded
by
modern
industrial
and
agricultural
activities
at
a
pace
far
above
anything
previously
known,
imperiling
its
vast
biodiversity
reserves
globally
important
ecosystem
services.
The
most
substantial
threats
come
from
regional
deforestation,
because
of
export
market
demands,
global
climate
change.
Amazon
is
currently
perched
to
transition
rapidly
largely
forested
nonforested
landscape.
These
changes
happening
much
too
for
species,
peoples,
ecosystems
respond
adaptively.
Policies
prevent
the
worst
outcomes
known
must
be
enacted
immediately.
We
now
need
political
will
leadership
act
on
this
information.
To
fail
biosphere,
we
our
peril.
Journal of Energy Chemistry,
Journal Year:
2021,
Volume and Issue:
67, P. 309 - 341
Published: Oct. 25, 2021
Photocatalytic
conversion
of
CO2
into
solar
fuels
provides
a
bright
route
for
the
green
and
sustainable
development
human
society.
However,
realization
efficient
photocatalytic
reduction
reaction
(CO2RR)
is
still
challenging
owing
to
sluggish
kinetics
or
unfavorable
thermodynamics
basic
chemical
processes
CO2RR,
such
as
adsorption,
activation,
product
desorption.
To
overcome
these
shortcomings,
recent
works
have
demonstrated
that
surface
engineering
semiconductors,
introducing
vacancy,
doping,
cocatalyst
loading,
serves
effective
promising
strategies
improved
CO2RR
with
high
activity
selectivity.
The
essential
reason
lies
in
activation
pathways
can
be
optimized
regulated
through
reconstruction
atomic
electronic
structures.
Herein,
this
review,
we
focus
on
research
advances
about
rational
design
semiconductor
CO2RR.
selectivity
will
reviewed.
In
addition,
theoretical
calculations
along
situ
characterization
techniques
spotlight
clarify
process.
aim
review
provide
deep
understanding
guidance
semiconductors
Proceedings of the National Academy of Sciences,
Journal Year:
2022,
Volume and Issue:
119(42)
Published: Oct. 10, 2022
The
Paleocene–Eocene
Thermal
Maximum
(PETM;
56
Ma)
is
one
of
our
best
geological
analogs
for
understanding
climate
dynamics
in
a
“greenhouse”
world.
However,
proxy
data
representing
the
event
are
only
available
from
select
marine
and
terrestrial
sedimentary
sequences
that
unevenly
distributed
across
Earth’s
surface,
limiting
view
spatial
patterns
change.
Here,
we
use
paleoclimate
assimilation
(DA)
to
combine
model
information
create
spatially
complete
reconstruction
PETM
state
precedes
it
(“PETM-DA”).
Our
data-constrained
results
support
strong
polar
amplification,
which
absence
an
extensive
cryosphere,
related
temperature
feedbacks
loss
seasonal
snow
on
land.
response
hydrological
cycle
warming
consists
narrowing
Intertropical
Convergence
Zone,
off-equatorial
drying,
intensification
monsoons
winter
storm
tracks.
Many
these
features
also
seen
simulations
future
change
under
increasing
anthropogenic
emissions.
Since
PETM-DA
yields
estimate
surface
air
temperature,
rigorous
global
mean
(5.6
∘
C;
5.4
C
5.9
C,
95%
CI)
can
be
used
calculate
equilibrium
sensitivity
(ECS).
We
find
ECS
was
6.5
(5.7
7.4
CI),
much
higher
than
present-day
range.
This
supports
increases
substantially
when
greenhouse
gas
concentrations
high.
Nature Communications,
Journal Year:
2022,
Volume and Issue:
13(1)
Published: March 14, 2022
Northern
Hemisphere
forests
changed
drastically
in
the
early
Eocene
with
diversification
of
oak
family
(Fagaceae).
Cooling
climates
over
next
20
million
years
fostered
spread
temperate
biomes
that
became
increasingly
dominated
by
oaks
and
their
chestnut
relatives.
Here
we
use
phylogenomic
analyses
nuclear
plastid
genomes
to
investigate
timing
pattern
major
macroevolutionary
events
ancient
genome-wide
signatures
hybridization
across
Fagaceae.
Innovation
related
seed
dispersal
is
implicated
triggering
waves
continental
radiations
beginning
rapid
lineages
resulting
unparalleled
transformation
forest
dynamics
within
15
following
K-Pg
extinction.
We
detect
introgression
at
multiple
time
scales,
including
predating
origination
genus-level
diversity.
As
moved
into
newly
available
habitats
Miocene,
secondary
contact
between
previously
isolated
species
occurred.
This
resulted
adaptive
introgression,
which
may
have
further
amplified
white
Eurasia.
Reviews of Geophysics,
Journal Year:
2023,
Volume and Issue:
61(3)
Published: June 14, 2023
Abstract
The
Pliocene
Epoch
(∼5.3–2.6
million
years
ago,
Ma)
was
characterized
by
a
warmer
than
present
climate
with
smaller
Northern
Hemisphere
ice
sheets,
and
offers
an
example
of
system
in
long‐term
equilibrium
current
or
predicted
near‐future
atmospheric
CO
2
concentrations
(
p
).
A
trend
ice‐sheet
expansion
led
to
more
pronounced
glacial
(cold)
stages
the
end
(∼2.6
Ma),
known
as
“intensification
Glaciation”
(iNHG).
We
assessed
spatial
temporal
variability
ocean
temperatures
ice‐volume
indicators
through
late
early
Pleistocene
(from
3.3
2.4
determine
character
this
transition.
identified
asynchronous
shifts
means
pacing
amplitude
shorter‐term
variability,
between
regions
proxies.
Early
changes
Antarctic
glaciation
Southern
properties
occurred
even
during
mid‐Piacenzian
warm
period
(∼3.264–3.025
which
has
been
used
analog
for
future
warming.
Increased
subsequently
developed
alongside
signatures
larger
sheets
Yet,
some
felt
no
impact
iNHG,
particularly
lower
latitudes.
Our
analysis
demonstrated
complex,
non‐uniform
globally
nature
associated
iNHG.
Shifting
gateways
circulation
may
have
pre‐conditioned
later
evolution
falling
.
Further
development
high‐resolution,
multi‐proxy
reconstructions
is
required
so
that
full
potential
rich
detailed
geological
records
can
be
realized.