Earth and Planetary Science Letters,
Journal Year:
2024,
Volume and Issue:
640, P. 118801 - 118801
Published: May 31, 2024
Carbon
cycle
models
used
to
calculate
the
marine
reservoir
age
of
non-polar
surface
ocean
(called
Marine20)
out
IntCal20,
compilation
atmospheric
Δ14C,
have
so
far
neglected
a
key
aspect
millennial-scale
variability
connected
with
thermal
bipolar
seesaw:
changes
in
strength
Atlantic
meridional
overturning
circulation
(AMOC)
related
Dansgaard/Oeschger
and
Heinrich
events.
Here
we
implement
such
AMOC
carbon
box
model
BICYCLE-SE
investigate
how
performance
over
last
55
kyr
is
affected,
particular
respect
available
14C
CO2
data.
Constraints
from
deep
data
suggest
that
during
stadial
1
needs
be
highly
reduced
or
even
completely
shutdown.
Ocean
sea
ice
coverage
combined
are
processes
almost
explain
simulated
age,
these
also
responsible
for
glacial
drawdown
∼60
ppm
CO2.
We
find
implementation
abrupt
reductions
Greenland
stadials
setup
was
previously
calculation
Marine20
leads
differences
less
than
±100
yrs.
The
representation
therefore
appears
minor
importance
deriving
mean
radiocarbon
calibration
products
as
Marine20,
where
variables
forced
by
reconstructions.
However,
exhibits
minima
stadials,
disagreement
core
This
mismatch
supports
previous
suggestions
were
probably
not
driven
directly
AMOC,
but
rather
biological
physical
Southern
contributions
variable
land
storage.
Climate of the past,
Journal Year:
2024,
Volume and Issue:
20(4), P. 841 - 864
Published: April 8, 2024
Abstract.
Millennial-scale
climate
variations
during
the
last
glacial
period,
such
as
Dansgaard–Oeschger
(DO)
cycles
and
Heinrich
events,
have
been
extensively
studied
using
ice
core
marine
proxy
records.
However,
there
is
a
limited
understanding
of
magnitude
these
temperature
fluctuations
in
continental
regions,
questions
remain
about
seasonal
signal
events.
This
study
presents
60
000-year-long
reconstruction
based
on
branched
glycerol
dialkyl
tetraethers
(brGDGTs)
extracted
from
lake
sediments
Eifel
Volcanic
Field,
Germany.
brGDGTs
are
bacterial
membrane-spanning
lipids
that
known
to
strong
relationship
with
temperature,
making
them
suitable
for
reconstructions.
We
test
several
calibration
models
modern
samples
taken
soils
multiple
maar
lakes.
find
negative
bias
brGDGT-based
estimates
associated
water
depth
anoxic
conditions
can
be
corrected
by
accounting
brGDGT
isomer
only
produced
conditions.
The
correlates
model
spanning
same
time
validating
approach
we
selected.
millennial-scale
variability
significantly
dampened
record,
contrast
other
Northern
Hemisphere
records,
stadials,
temperatures
actually
increase.
demonstrate
apparent
discrepancies
explained
unique
response
paleothermometer
months
above
freezing
(TMAF).
Our
data
support
view
warm-season
Europe
varied
minimally
period
abrupt
events
were
defined
colder,
longer
winters.
continuous
high-resolution
provides
important
information
used
inform
studies
paleoecological
change.
Geophysical Research Letters,
Journal Year:
2023,
Volume and Issue:
50(15)
Published: Aug. 8, 2023
Abstract
Hydroxylated
isoprenoid
glycerol
dialkyl
tetraethers
(OH‐GDGTs)
preserved
in
marine
sediments
are
thought
to
be
controlled
by
sea
surface
temperature
(SST).
However,
water
depth
may
also
exert
a
significant
influence
on
OH‐GDGTs.
Here,
we
investigated
sedimentary
OH‐GDGTs
the
Kermadec
and
Atacama
trench
regions
(2,560–9,560
m
depth).
Sedimentary
hadal
trenches
were
dominated
OH‐GDGT‐0
(72
±
8%),
potentially
reflecting
an
adaption
of
source
organisms
ambient
cold
deep
water.
This
result,
combined
with
global
data
set,
revealed
that
predominance
is
ubiquitous
phenomenon
deep‐sea
sediments,
leading
considerable
underestimation
RI‐OH′‐derived
SSTs.
By
considering
both
SST
effects,
developed
more
accurate
OH‐GDGT‐based
paleothermometers
for
shallow
ocean,
encompassing
full‐ocean‐depth
range.
Our
findings
highlight
importance
accounting
effect
provide
improved
tools
reconstructing
paleo‐SSTs.
Geochimica et Cosmochimica Acta,
Journal Year:
2023,
Volume and Issue:
370, P. 113 - 127
Published: Dec. 19, 2023
Recently
developed
temperature
proxies
based
on
hydroxylated
isoprenoid
Glycerol
Dialkyl
Tetraethers
(OH-isoGDGTs),
such
as
%OH,
RI-OH,
RI-OH′
and
OHC,
have
shown
potential
for
reconstructing
past
changes.
However,
progress
has
been
limited
by
the
lack
of
a
global
core-top
calibration
with
ample
geographical
coverage.
Here,
we
compile
an
extensive
surface
sediment
dataset
OH-isoGDGTs
well
regular
GDGTs
(isoGDGTs),
both
data
generated
at
NIOZ
(n
=
575)
previously
published
from
other
laboratories
297).
We
find
interlaboratory
differences
proxy
indices
that
incorporate
isoGDGTs,
indicating
care
must
be
taken
in
compiling
large
GDGT
datasets
multiple
laboratories.
Our
results
confirm
strong
signal
isoGDGT
distribution,
especially
OH-isoGDGT-0
non-hydroxylated
but
also
reveal
water
depth
might
impact
distribution
1
2
cyclopentane
moieties.
This
will
affect
RI-OH
indices,
particularly
tropical
regions,
where
occurs
low
abundance.
explore
new
combine
dependence
OH-isoGDGT
distributions
propose
use
TEX86OH,
which
includes
denominator
TEX86
index.
modification
leads
to
much
higher
sensitivity
index,
regions
annual
mean
sea
temperatures
between
5
15
°C.
Application
this
novel
paleothermometer
polar
core
suggests
is
likely
result
more
reliable
reconstructions
are
abundant.
Geology,
Journal Year:
2024,
Volume and Issue:
52(6), P. 385 - 389
Published: Feb. 26, 2024
Abstract
The
last
deglaciation
is
considered
a
key
period
for
exploring
the
underlying
dynamics
of
temperature
changes
because
it
was
characterized
by
multiple
millennial-scale
abrupt
climatic
events.
However,
limited
number
quantitative
records
in
Northeast
(NE)
China
covering
hampers
complete
understanding
mechanisms
and
processes
behind
that
occurred
region.
Here,
we
present
reconstruction
summer
over
based
on
bacterial
branched
glycerol
dialkyl
tetraethers
(brGDGTs)
analyzed
from
sediment
sequence
Lake
Kielguo,
small
volcanic
lake
NE
China.
results
show
lowest
during
interval
ca.
20–18.2
calibrated
(cal.)
k.y.
B.P.
with
value
~11.1
°C
increased
~1.9
Heinrich
Stadial
1
(HS1)
~2.7
transition
to
Bølling-Allerød
(B-A).
temperatures
B-A
warm
Younger
Dryas
cold
were
~14.1
~12.0
°C,
respectively.
record
Kielguo
indicates
warming
dominated
climate
change
state
HS1
East
Asia,
which
different
cooling
pattern
controlled
winter
North
Atlantic
Greenland
realms.
This
distinction
can
be
explained
weakened
signals
triggered
collapse
Meridional
Overturning
Circulation
when
these
propagated
orbital
greenhouse
gases
Asia.
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(6)
Published: March 18, 2024
Abstract
Hydroxylated
isoprenoid
GDGTs
(OH‐GDGTs)
have
emerged
as
a
novel
tool
for
reconstructing
sea
surface
temperatures.
However,
when
using
marine
OH‐GDGT
calibration
in
lacustrine
settings,
it
leads
to
significant
overestimation
of
temperatures,
emphasizing
the
necessity
thorough
examination
OH‐GDGTs
lakes.
Here,
we
investigated
distributions
sediments
from
65
lakes
West
China
and
compiled
published
Asian
lake
global
data
sets.
Among
all
GDGT‐based
indices,
RI‐OH
showed
strongest
correlation
with
temperature
across
The
value
was
higher
than
sediments,
likely
due
differences
composition
Group
1.1a
thaumarchaeotal
species
between
two
settings.
first
developed
addressed
issue
applied
both
water
column
sediment
core,
highlighting
potential
new
terrestrial
paleothermometer.
Research Square (Research Square),
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 10, 2025
Abstract
Background
The
field
vole,
an
abundant
and
widespread
microtine
rodent,
is
a
complex
comprising
three
cryptic
species.
short-tailed
vole
(Microtus
agrestis)
present
over
much
of
Eurasia,
the
Mediterranean
lavernedii)
in
southern
Europe,
Portuguese
rozianus)
limited
to
western
Spain
Portugal.
Previous
research
has
shown
high
genomic
differentiation
these
lineages;
however,
details
process
underlying
their
divergence
remain
unknown.
Results
We
analysed
46
mitogenomes
16
nuclear
genomes
modern
specimens,
75
12
ancient
specimens
spanning
last
thousand
years,
investigate
evolutionary
history
this
species
complex.
estimated
from
voles
be
ca.
220
ka
ago
latter
110
ago,
earlier
than
previous
estimates
involving
only
sequences.
times
we
obtained
match
those
between
major
mitochondrial
lineages
cold-adapted
steppe
rodents
Europe.
found
signatures
gene
flow
within
lineages,
with
some
analyses
suggesting
hybrid
origin
lineage.
Ancient
Italian
Peninsula
revealed
previously
unrecognised
lineage
that
showed
evidence
genetic
exchange
other
populations.
Conclusions
pattern
variation
demonstrates
unequivocally
impact
stadial-interstadial
cycles
generating
recurrent
episodes
allopatry
connectivity
populations,
situation
which
could
by
our
dense
sampling
time.