Tree Physiology,
Journal Year:
2024,
Volume and Issue:
44(11)
Published: Oct. 18, 2024
Abstract
Intra-annual
variations
of
carbon
stable
isotope
ratios
(δ13C)
in
different
tree
compartments
could
represent
valuable
indicators
plant
source–sink
dynamics,
at
weekly
time
scale.
Despite
this
significance,
the
absence
a
methodological
framework
for
tracking
δ13C
values
rings
persists
due
to
complexity
ring
development.
To
fill
knowledge
gap,
we
developed
method
monitor
variability
cambium–xylem
continuum
black
spruce
species
[Picea
mariana
(Mill.)
BSP.]
during
growing
season.
We
collected
and
isolated
incremental
growth
cambial
region
developing
from
five
mature
trees
over
three
consecutive
seasons
(2019–21)
Simoncouche
two
(2020–21)
Bernatchez,
both
located
boreal
forest
Quebec,
Canada.
Our
allowed
creation
intra-annual
series
cambium
(δ13Ccam)
xylem
cellulose
(δ13Cxc)
these
sites.
Strong
positive
correlations
were
observed
between
δ13Ccam
δ13Cxc
almost
all
study
years.
These
findings
suggest
that
constant
supply
fresh
assimilates
may
be
dominant
process
feeding
secondary
On
other
hand,
rates
isotopic
fractionation
appeared
poorly
affected
by
climate
variability,
an
inter-weekly
Hence,
increasing
trends
highlighted
here
possibly
indicate
shifts
allocation
strategies,
likely
fostering
frost
resistance
reducing
water
uptake
late
Additionally,
related
trees'
responses
seasonal
decrease
photosynthetically
active
radiation.
provide
new
insights
into
dynamics
constraints
ecosystems,
offering
novel
approach
studying
fine
temporal
scales.
New Phytologist,
Journal Year:
2024,
Volume and Issue:
241(6), P. 2366 - 2378
Published: Feb. 1, 2024
Summary
The
strong
covariation
of
temperature
and
vapour
pressure
deficit
(VPD)
in
nature
limits
our
understanding
the
direct
effects
on
leaf
gas
exchange.
Stable
isotopes
CO
2
H
O
provide
mechanistic
insight
into
physiological
biochemical
processes
during
We
conducted
combined
exchange
online
isotope
discrimination
measurements
four
common
European
tree
species
across
a
range
5–40°C,
while
maintaining
constant
leaf‐to‐air
VPD
(0.8
kPa)
without
soil
water
limitation.
Above
optimum
for
photosynthesis
(30°C)
under
controlled
environmental
conditions,
stomatal
conductance
(
g
s
)
net
rate
A
n
decoupled
all
tested
species,
with
increasing
but
decreasing.
During
this
decoupling,
mesophyll
(cell
wall,
plasma
membrane
chloroplast
conductance)
consistently
significantly
decreased
among
species;
however,
reduction
did
not
lead
to
reductions
concentration
at
surface
stroma.
question
conventional
that
diffusional
limitations
contribute
high
temperatures.
suggest
stomata
membranes
could
work
strategically
facilitate
transpiration
cooling
supply,
thus
alleviating
heat
stress
photosynthetic
function,
albeit
cost
reduced
water‐use
efficiency.
Vegetation
assimilation
of
atmospheric
gaseous
elemental
mercury
(GEM)
represents
the
largest
dry
deposition
pathway
in
global
terrestrial
ecosystems.
This
study
investigated
Hg
accumulation
mechanisms
deciduous
broadleaves
and
evergreen
needles,
focusing
on
how
ecophysiological
strategies─reflected
by
δ13C,
δ18O,
leaf
mass
per
area,
matter
content-mediated
accumulation.
Results
showed
that
leaves
exhibited
higher
total
(THg)
concentrations
rates
(THgrate),
which
were
85.3
±
17.7
110.0
0.3%
than
those
needles.
The
two
tree
types
distinct
strategies:
broadleaves,
with
stomatal
conductance
photosynthetic
rates,
rapidly
adjust
stomata
to
changes
meteorological
pollutant
factors,
playing
a
key
role
controlling
THgrate.
In
contrast,
needles
featured
stable
control,
highlighting
direct
positive
effect
GEM
their
Precipitation
wind
speed
negatively
influenced
foliar
Correlations
between
PM2.5,
NO2,
THgrate
suggested
synergistic
patterns
pollutants.
underscores
across
functional
emphasizes
importance
species-specific
strategies.
An
empirical
model
linking
ecophysiological,
meteorological,
pollution
factors
was
provided,
contributing
refinement
models.
The Science of The Total Environment,
Journal Year:
2023,
Volume and Issue:
912, P. 168858 - 168858
Published: Nov. 27, 2023
Perennially
frozen
soil,
also
known
as
permafrost,
is
important
for
the
functioning
and
productivity
of
most
boreal
forest,
world's
largest
terrestrial
biome.
A
better
understanding
complex
vegetation-permafrost
interrelationships
needed
to
predict
changes
in
local-
large-scale
carbon,
nutrient,
water
cycle
dynamics
under
future
global
warming.
Here,
we
analyze
tree-ring
width
stable
isotope
(C
O)
measurements
Gmelin
larch
(Larix
gmelinii
(Rupr.)
Rupr.)
from
six
permafrost
sites
northern
taiga
central
Siberia.
Our
multi-parameter
approach
shows
that
tree
growth
were
predominantly
controlled
by
temperature
moisture
content
active
soil
upper
layers.
The
observed
patterns
range
strong
limitations
early
summer
temperatures
at
higher
elevations
significant
controls
precipitation
warmer
well-drained
lower-elevation
sites.
Enhanced
radial
mainly
found
with
fast
thawing
mineral
layers,
comparison
isotopes
over
five-year
periods
different
amounts
indicates
trees
can
prevent
drought
stress
accessing
melted
snow
seasonally
soil.
Identifying
layers
resources
during
dry
summers
demonstrates
complexity
ecosystem
responses
climatic
changes.
Frontiers in Plant Science,
Journal Year:
2025,
Volume and Issue:
15
Published: Jan. 10, 2025
The
ecophysiological
and
ecohydrological
impacts
of
climate
change
progressively
increasing
atmospheric
carbon
dioxide
(CO2)
concentration
on
agroecosystems
are
not
well
understood
compared
to
the
forest
ecosystems.
In
this
study,
we
utilized
presence
old
apple
pear
trees
in
alpine
valleys
Northern
Italy
(maintained
for
cultural
heritage
purposes)
investigate
climate-scale
physiological
responses.
We
developed
long-term
tree-ring
stable
isotopic
records
(δ13C
δ18O)
from
(1976-2021)
(1943-2021).
This
allowed
reconstruction
key
processes
like
variations
intrinsic
water
use
efficiency
(iWUE),
investigated
how
these
responded
CO2
changes
over
decades.
Results
showed
a
slight
declining
trend
discrimination
(Δ
13C)
while
intercellular
(Ci)
both
species
has
been
since
late
1980s.
Concurrently
exhibited
rising
iWUE,
with
demonstrating
higher
efficiency,
which
appears
be
primarily
driven
by
CO2-fertilization
effect.
concomitant
trends
δ18O
suggested
relatively
local
hydroclimate
during
study
period
some
species-specific
Analyses
further
revealed
that
minimum
growing
season
temperature,
precipitation
was
most
significant
factor
influencing
rise
iWUE
alongside
fertilization
species'
δ13C
coupled
their
respective
confirmed
due
increased
assimilation
rather
than
decline
evapotranspiration.
Moreover,
δ13C-δ18O
analyses
assimilation,
showing
inter-decadal
variations.
These
provide
unique
opportunity
test
calibrate
systems
respond
recent
anticipated
change.
Ecology and Evolution,
Journal Year:
2025,
Volume and Issue:
15(3)
Published: March 1, 2025
ABSTRACT
Wildfires
are
increasing
in
frequency
and
severity
due
to
climate
change,
posing
challenges
forest
ecosystems,
including
the
southern
interior
of
British
Columbia,
Canada.
Interior
Douglas‐fir
(
Pseudotsuga
menziesii
var.
glauca
)
is
a
species
great
cultural,
ecological,
economic
importance,
necessitating
investigation
post‐wildfire
regeneration
amidst
this
changing
wildfire
regime.
This
study
examines
seedling
across
three
burn
levels
(low,
moderate,
high)
5
years
at
site
Columbia.
Natural
traits
were
measured
2022
paired
with
stable
isotope
analyses
(δ
13
C,
δ
15
N,
18
O)
foliar
nutrient
assessments.
We
employed
linear
mixed‐effects
models
assess
impact
light,
water,
factors
on
biomass.
Results
indicate
higher
density
low
sites
but
larger
individual
biomass
moderate
high
sites.
Light
availability
was
primary
factor
limiting
biomass,
greater
C
sites,
suggesting
that
reduced
canopy
cover
enhances
photosynthesis
water
use
efficiency.
Despite
solar
exposure,
seedlings
did
not
show
increased
drought
stress
according
leaf
O
stem
contents,
likely
interception
competition
for
soil
by
overstory
trees.
Biomass
growth
linked
status,
indicating
availability,
particularly
limit
While
light
current
growth‐limiting
regenerating
study,
intensity
heat
waves
droughts
associated
change
may
increase
stress,
emphasizing
need
long‐term
monitoring
adaptive
management
support
Douglas‐fir.
Global Change Biology,
Journal Year:
2025,
Volume and Issue:
31(3)
Published: March 1, 2025
Human-induced
environmental
changes
are
altering
forest
productivity
and
species
composition,
significantly
impacting
tree
physiology,
growth,
water
uptake,
nutrient
acquisition.
Investigating
the
intricate
interplay
between
plant
physiology
shifts,
we
analyzed
tree-ring
isotopes
(δ13C,
δ18O,
δ15N)
to
track
long-term
trends
in
intrinsic
water-use
efficiency
(iWUE)
nitrogen
availability
for
European
beech,
Norway
spruce,
silver
fir
a
unique
old-growth
temperate
mountain
since
1501
ce.
Our
findings
reveal
that
dominant
species,
exhibited
iWUE
saturation,
exacerbated
by
acidic
precipitation,
resulting
growth
declines
during
periods
of
high
air
pollution
increased
drought
frequency.
In
contrast,
deep-rooted,
deciduous
beech
demonstrated
physiological
resilience
acid
deposition,
benefiting
from
lower
dry
deposition
precipitation
acidity
thriving
under
conditions
elevated
temperatures,
thereby
sustaining
stem
regardless
potential
climatic
limitations.
Silver
showed
most
dynamic
response
pollution,
with
contemporary
adaptations
leaf
gas
exchange
allowing
accelerated
cleaner
conditions.
These
different
responses
underscore
shifts
competition,
gaining
dominance
as
spruce
decline.
Furthermore,
influence
ontogeny
is
evident,
tree-rings
initial
values
higher
δ15N,
reflecting
uptake
dynamics
ecological
role
age.
study
integrates
tree-growth
trends,
revealing
pivotal
atmospheric
chemistry
shaping
competitive
trajectories
forests.
Geophysical Research Letters,
Journal Year:
2025,
Volume and Issue:
52(7)
Published: April 1, 2025
Abstract
Tree
ring‐based
climate
reconstructions
are
fundamental
for
high‐resolution
paleoclimatology,
but
only
a
few
of
them
extend
back
into
the
mid‐Holocene
(8,200–4,200
years
BP).
Here,
we
present
annually‐resolved
tree‐ring
stable
carbon
and
oxygen
isotopes
(δ
13
C
δ
18
O)
from
subfossil
yew
(
Taxus
baccata
)
wood
excavated
in
Fenland
region
eastern
England.
We
develop
an
eco‐physiological
model
to
reconstruct
hydroclimate
variability
5,224
4,813
±
4
4,612–4,195
6
cal.
BP.
Our
findings
suggest
that
relative
sea‐level
rise
North
Sea,
riverine
flooding,
prolonged
negative
phase
Atlantic
Oscillation
caused
unusually
wet
conditions
around
4,200
ago
when
woodlands
England
disappeared.
expect
our
study
stimulate
isotope
measurements
relict
encourage
integration
terrestrial
marine
proxy
archives
causes
consequences
large‐scale
variations
still
debated
4.2
ka
event.
Journal of Quaternary Science,
Journal Year:
2025,
Volume and Issue:
unknown
Published: April 1, 2025
ABSTRACT
The
charring
process
can
preserve
archaeobotanical
remains,
providing
valuable
insights
into
past
climates,
agricultural
practices,
and
plant
growth
conditions.
However,
the
impact
of
on
stable
isotopes,
especially
at
temperatures
above
300°C,
remains
poorly
understood.
To
investigate
this,
wheat
(einkorn,
emmer)
millet
grains
were
experimentally
charred
450°C,
550°C
for
15
min
to
48
h
under
aerobic
anaerobic
Consequently,
isotopic
ratios
carbon
(
13
C/
12
C;
δ
C),
nitrogen
N/
14
N;
N),
oxygen
18
O/
16
O;
O)
determined
in
fully
with
a
blackened
pericarp,
visually
comparable
archeological
remains.
Our
results
indicate
that
C
values
are
well
preserved
grains,
showing
minimal
shifts
(<0.55‰
<0.2‰
millet),
while
N
retained
species‐specific
differences,
moderate
variations
(<1.31‰
<0.68‰
millet)
influenced
by
In
contrast,
O
showed
high
variability
limiting
their
reliability
interpretative
use.
These
findings
underscore
potential
and,
lesser
extent,
isotopes
reconstructing
ancient
conditions
improving
understanding
formation
processes
research.