Abstract.
Plant
water
source
tracing
studies
often
rely
on
differences
in
stable
isotope
composition
of
different
sources.
However,
an
increasing
number
has
indicated
a
discrepancy
between
the
isotopic
signature
plant
xylem
and
sources
assumed
to
be
used
by
plants.
Based
meta-analysis
we
have
reconfirmed
this
groundwater
suggest
back-flow
leaf
(BFLW),
defined
as
combination
(i)
Péclet
effect,
(ii)
foliar
uptake
(FWU)
(iii)
hydraulic
redistribution
water,
possible
explanation
for
these
observations.
Using
average
2.21
‰
18O
enrichment
compared
our
meta-analysis,
modelled
potential
BFLW
result
observed
discrepancy.
With
low
flow
velocity
0.052
m.h−1
effective
path
length
2
m,
effect
alone
was
able
account
offset
groundwater.
When
including
realistic
fraction
5–10
%
originating
from
FWU
tissue
dehydration,
60–100
can
explained.
By
combining
with
some
more
extreme
offsets
elucidated.
These
large
effects
are
probable
during
dry
conditions
when
drought
stress
lowers
transpiration
rates,
leading
larger
greater
contribution
FWU.
Ecohydrology,
Journal Year:
2024,
Volume and Issue:
17(3)
Published: March 16, 2024
Abstract
Stable
isotopes
δ
18
O
and
2
H
are
used
to
infer
vegetation
water
sources.
In
some
studies,
significant
xylem
offsets
from
potential
source
waters
have
been
observed.
The
appear
be
more
prevalent
with
cryogenic
vacuum
distillation
(CVD)
of
plant
water.
Hypothesized
mechanisms
for
these
include
changes
during
uptake
transport,
methodological
problems.
We
propose
that
a
large
portion
the
due
hydrogen
isotope
exchange
between
non‐crystalline
hydroxyl
groups
wood
cellulose
hemicellulose
CVD.
present
method
estimating
hypothesized
isotopic
tissues
water,
which
is
result
Rayleigh
equilibrium
fractionation.
To
estimate
exchange,
we
use
published
properties
North
American
tree
species
chemical
relationships
as
function
moisture
content,
CVD
temperature
extraction
efficiency.
A
simple
model
captures
range
observations
in
studies
non‐CVD
methods
were
compared.
evaluate
model,
compared
observed
(sw‐excess)
values
two
field
datasets
(90°C,
n
=
364,
170°C,
43)
estimated
our
model.
found
good
agreement
samples
extracted
at
90°C
(
r
0.69)
but
not
170°C
0.20).
offset
may
eliminated
by
increasing
229°C
or
adding
standard
sufficient
raise
content
>150%.
correction
can
also
approximated
applying
theoretical
calculation
based
on
temperature,
Plant Cell & Environment,
Journal Year:
2023,
Volume and Issue:
47(1), P. 72 - 90
Published: Oct. 9, 2023
Foliar
water
uptake
can
recharge
storage
tissue
and
enable
greater
hydration
than
through
access
to
soil
alone;
however,
few
studies
have
explored
the
role
of
bark
in
facilitating
uptake.
We
investigated
pathways
dynamics
(BWU)
stems
mangrove
Avicennia
marina.
provide
novel
evidence
that
specific
entry
points
control
outer
surface.
Furthermore,
using
a
fluorescent
symplastic
tracer
dye
we
first
lenticels
on
surface
facilitate
BWU,
thus
increasing
stem
content
by
up
3.7%.
X-ray
micro-computed
tomography
showed
BWU
was
sufficient
cause
measurable
swelling
layers
whole
cross-sectional
area
0.83
mm2
or
2.8%,
implicating
it
as
contributor
diel
patterns
buffer
xylem
potential
maintain
living
tissue.
Frontiers in Water,
Journal Year:
2022,
Volume and Issue:
4
Published: July 7, 2022
Across
the
karst
landscape
of
Quintana
Roo,
Mexico,
plant
access
to
nutrients
and
water
appears
limited
by
generally
shallow
soil.
However,
underlying
this
surface
are
heterogenous
pockets
in
bedrock
deeper,
stable
groundwater,
suggesting
potential
for
specialization
species
accessing
soil
resources.
If
differentially
rock
resources,
divisions
functional
groups
may
also
be
expected.
In
study,
caves
provided
an
opportunity
assess
resource
use
strategies
direct,
species-specific
root
observations
coupled
with
traditional
above
ground
measurements.
Utilizing
isotopes
from
stems
leaves
(δ
18
O
δ
13
C),
we
investigated
efficiency
trees
during
dry
season
uncover
relationships
between
rooting
habit,
tree
size,
pre-determined
based
on
leaf
habit
wood
density.
Functional
group
membership
did
not
predict
measured
isotope
ratios,
indicating
that
were
poor
predictors
use.
We
find
evidence
deep
select
larger
individuals.
Interestingly,
as
became
larger,
C
increased
a
threshold
but
then
declined,
increasing
vulnerability
limitation
increase
consistent
other
seasonally
tropical
forests.
Our
work
demonstrates
that,
although
soils
likely
drive
strong
limitations,
co-occurring
ecosystems
employ
diverse
acquisition
strategies,
important
consequences
community
composition
ecosystem
function
face
environmental
change.
New Phytologist,
Journal Year:
2024,
Volume and Issue:
242(3), P. 975 - 987
Published: March 5, 2024
Summary
Stable
oxygen
isotope
ratio
of
tree‐ring
α‐cellulose
(δ
18
O
cel
)
yields
valuable
information
on
many
aspects
tree–climate
interactions.
However,
our
current
understanding
the
mechanistic
controls
δ
is
incomplete,
with
a
knowledge
gap
existent
regarding
fractionation
effect
characterizing
carbonyl‐water
exchange
during
sucrose
translocation
from
leaf
to
phloem.
To
address
this
insufficiency,
we
set
up
an
experimental
system
integrating
vapor
O‐labeling
feature
manipulate
leaf‐level
isotopic
signatures
in
tree
saplings
enclosed
within
whole‐canopy
gas‐exchange
cuvettes.
We
applied
three
different
species
determine
their
respective
relationships
between
enrichment
lamina
(Δ
l_suc
and
petiole
phloem
phl_suc
under
environmentally/physiologically
stable
conditions.
Based
determined
Δ
‐Δ
relationships,
estimated
that
average,
at
least
25%
atoms
undergo
water
along
leaf‐to‐phloem
path
biochemical
factor
accounting
for
such
c.
34‰,
markedly
higher
than
conventionally
assumed
value
27‰.
Our
study
represents
significant
step
toward
quantitative
elucidation
dynamics
trees.
This
has
important
implications
respect
improving
model
its
related
applications
paleoclimatic
ecophysiological
contexts.
Physiologia Plantarum,
Journal Year:
2024,
Volume and Issue:
176(3)
Published: April 29, 2024
Abstract
Tracer
injection
has
long
been
recognized
as
a
valuable
tool
for
delineating
tree
hydraulics
and
assessing
water
transport
pathways.
Recently,
isotope
tracers
have
emerged
innovative
instruments
investigating
hydraulics,
providing
new
insights
into
dynamics.
Nevertheless,
there
is
critical
need
further
research
to
comprehensively
grasp
movement
distribution
within
trees.
A
previously
introduced
technique
analyzing
the
isotopic
ratio
of
in
wet
tissues,
offering
millimeter‐scale
resolution
visualizing
tracer
movement,
faces
challenges
due
its
underdeveloped
sample
preparation
techniques.
In
this
study,
we
an
H
2
18
O
S.
gracilistyla
samples,
exclusively
comprising
indeterminate
roots,
stems,
leaves,
cultivated
through
hydroponics
grown
current
year.
Our
objective
was
assess
axial
xylem.
Additionally,
devised
novel
method
preparing
frozen
tissue
enhancing
repeatability
success
rate
experiments.
The
results
demonstrated
that
all
samples
exhibited
average
loss
less
than
0.6%.
Isotopic
analysis
these
unveiled
consistent
decline
concentration
with
increasing
height
Salix
specimens,
three
out
five
revealing
significant
gradient.
findings
affirm
efficacy
practicality
combining
labeling
freezing,
stabilization,
Looking
ahead,
our
methods
are
poised
transcend
woody
plants,
finding
extensive
applications
plant
physiology
ecohydrology.
Hydrology and earth system sciences,
Journal Year:
2024,
Volume and Issue:
28(21), P. 4861 - 4881
Published: Nov. 8, 2024
Abstract.
The
hydrological
cycle
of
sub-arctic
areas
is
dominated
by
the
snowmelt
event.
An
understanding
mechanisms
that
control
water
fluxes
during
high-volume
infiltration
events
in
till
soils
needed
to
assess
how
future
changes
timing
and
magnitude
can
affect
soil
storage
dynamics.
We
conducted
a
tracer
experiment
which
deuterated
was
used
irrigate
plot
on
forested
hilltop
Lapland,
tracked
different
mobility
monitored
later
modifies
labelled
storage.
lysimeters
destructive
coring
for
sampling
sampled
groundwater.
Large
spatiotemporal
variability
between
waters
observed
subsurface,
while
surface
flow
largely
controlled
fill-and-spill
mechanism.
Extensive
saturation
induced
into
roots
nearby
trees.
found
remained
deeper
layers
over
winter,
but
event
gradually
displaced
all
fully
homogenized
at
soil–vegetation
interface.
conditions
required
full
displacement
old
occur
only
with
persistently
high
groundwater
table.
propose
conceptual
model
where
eventual
replenishment
three
stages.
First,
unsaturated
macropore
initiated
via
microtopography
directed
towards
second
stage
characterized
rise
through
network,
subsequent
pore
increased
horizontal
connectivity
macropores.
Shallow
subsurface
lateral
develop
more
permeable
shallow
layers.
In
third
stage,
materializes
long
period
table
within
soil,
replenished
enhanced
matrix
exchange
network.
Tree Physiology,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Dec. 16, 2024
Abstract
It
has
been
postulated
that
stemflow,
precipitation
flows
from
plant
crowns
down
along
branches
and
stems
to
soils,
benefits
plants
generate
it
because
increases
plant-available
soil
water
near
the
base
of
plant;
however,
little
direct
evidence
supports
this
postulation.
Were
plants’
preferentially
route
their
roots,
woody
with
large
canopies
could
benefit.
For
example,
piñon
juniper
tree
encroachment
into
sagebrush-steppe
ecosystems
be
facilitated
by
intercepted
routed
roots
as
hypothetically
reducing
available
for
shrubs
grasses.
We
tested
whether
Great
Basin
trees
use
benefit
stemflow.
In
a
drier-than-average
wetter-than-average
year,
isotopically
labeled
was
applied
simulate
Both
species
took
up
label
signals
peaking
receding
over
2
4
days.
Despite
uptake,
no
alleviation
stress
detected
in
drier
year.
The
stemflow
uptake
resulted
some
wetter
specifically
piñons,
which
deeper
profile
than
did
junipers.
Mixing
model
analyses
suggested
small
fraction
(approximately
0–2%),
but
an
order-of-magnitude
larger
transpired
those
few
days
after
addition.
These
findings
represent
novel
demonstration
rapid
infiltrates
rhizosphere,
they
also
prompt
questions
about
remaining
stemflow’s
fate
why
so
minor.