Global Change Biology,
Journal Year:
2023,
Volume and Issue:
29(24), P. 6832 - 6833
Published: Sept. 29, 2023
In
this
commentary,
we
highlight
the
recent
advancements
in
field
of
mountain
treeline
response
to
climate
change
work
by
He
et
al.
(2023).
We
summarize
their
from
perspectives
spatial
distribution,
bioclimatic
controls,
and
diverse
responses
changes
global
patterns.
expect
wide
implications
(2023),
point
out
future
research
direction
that
calls
for
interdisciplinary
attention.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: March 26, 2024
Abstract
Climate
change
induced
shifts
in
treeline
position,
both
towards
higher
altitudes
and
latitudes
induce
changes
soil
organic
matter.
Eventually,
matter
is
transported
to
alpine
subarctic
lakes
with
yet
unknown
consequences
for
dissolved
(DOM)
diversity
processing.
Here,
we
experimentally
investigate
the
of
by
amending
temperate
lake
water
soil-derived
DOM
from
above
below
treeline.
We
use
ultra-high
resolution
mass
spectrometry
(FT-ICR
MS)
track
molecular
(i.e.,
chemodiversity),
estimate
decay
measure
bacterial
growth
efficiency.
In
lakes,
increases
chemodiversity
mainly
through
enrichment
polyphenolic
highly
unsaturated
compounds.
These
compositional
are
associated
reductions
bulk
compound-level
reactivity
reduced
Our
results
suggest
that
advancement
has
potential
enrich
a
large
number
ecosystems
less
biodegradable
DOM,
affecting
community
function
potentially
altering
biogeochemical
cycling
carbon
at
high
altitudes.
Global Change Biology,
Journal Year:
2024,
Volume and Issue:
30(3)
Published: March 1, 2024
The
seasonal
coupling
of
plant
and
soil
microbial
nutrient
demands
is
crucial
for
efficient
ecosystem
cycling
production,
especially
in
strongly
alpine
ecosystems.
Yet,
how
these
processes
are
modified
by
climate
change
what
the
consequences
loss
retention
ecosystems
remain
unclear.
Here,
we
explored
two
pervasive
factors,
reduced
snow
cover
shrub
expansion,
interactively
modify
nitrogen
(N)
grasslands,
which
warming
at
double
rate
global
average.
We
found
that
combination
expansion
disrupted
N-cycling,
with
pronounced
effects
spring
(shortly
after
melt)
autumn
(at
onset
senescence).
In
combination,
both
factors
decreased
organic
N-uptake
70%
82%,
biomass
N
19%
38%
increased
denitrifier
abundances
253%
136%
autumn,
respectively.
Shrub
also
individually
seasonality
community
composition
stoichiometry
towards
more
N-limited
conditions
slower
autumn.
winter,
removal
markedly
fungal:bacterial
ratio,
pools
shifted
bacterial
composition.
Taken
together,
our
findings
suggest
interactions
between
can
disrupt
temporal
N-cycling
grasslands.
This
could
diminish
capacity
globally
widespread
to
retain
support
productivity
under
future
change.
Global Change Biology,
Journal Year:
2024,
Volume and Issue:
30(4)
Published: April 1, 2024
Abstract
The
impact
of
anthropogenic
global
warming
has
induced
significant
upward
dispersal
trees
to
higher
elevations
at
alpine
treelines.
Assessing
vertical
deviation
from
current
uppermost
tree
distributions
potential
treeline
positions
is
crucial
for
understanding
ecosystem
responses
evolving
climate.
However,
due
data
resolution
constraints
and
research
scale
limitation,
comprehending
the
pattern
driving
factors
remains
challenging.
This
study
constructed
a
comprehensive
quasi‐observational
dataset
distribution
across
mountains
using
Google
Earth
imagery.
Validating
isotherm
mean
growing‐season
air
temperature
6.6
±
0.3°C
as
indicator
thermal
treeline,
we
found
that
around
two‐thirds
records
significantly
deviated
it.
Drought
conditions
constitute
primary
driver
in
51%
cases,
followed
by
mountain
elevation
effect
which
indicates
surface
heat
(27%).
Our
analyses
underscore
multifaceted
determinants
patterns
explaining
divergent
climate
warming.
Moisture,
along
with
disturbance,
plays
most
fundamental
roles
variation
forecasting
response
ongoing
Ecology and Evolution,
Journal Year:
2025,
Volume and Issue:
15(1)
Published: Jan. 1, 2025
ABSTRACT
Anthropogenic
planetary
heating
is
disrupting
global
alpine
systems,
but
our
ability
to
empirically
measure
and
predict
responses
in
species
distributions
impaired
by
a
lack
of
comprehensive
data
technical
limitations.
We
conducted
comprehensive,
semi‐quantitative
review
empirical
studies
on
contemporary
range
shifts
insects
driven
climate
heating,
drawing
attention
methodological
issues
potential
biotic
abiotic
factors
influencing
variation
responses.
highlight
case
showing
how
dynamics
may
affect
standing
genetic
adaptive
potential,
discuss
integration
frameworks
can
improve
forecasts.
Although
influence
individual
responses,
most
studied
so
far
are
shifting
higher
elevations.
Upslope
often
accompanied
contractions
that
expected
diminish
increasing
extinction
risk.
Endemic
islands
predicted
be
especially
vulnerable.
Inferences
drawn
from
the
insects,
also
have
relevance
other
montane
habitats.
Correlative
niche
modelling
keystone
tool
its
limited
consider
biological
processes
underpinning
species'
complicates
interpretation.
Alpine
exhibit
some
respond
rising
temperatures
via
change
or
phenotypic
plasticity.
Thus,
future
efforts
should
incorporate
using
flexible
hybrid
approaches
enhance
realism
predictions.
Boosting
scientific
capability
envisage
environments
their
associated
biota
imperative
given
speed
intensity
high‐mountain
ecosystems
surpass
collect
required
guide
effective
conservation
planning
management
decisions.
ISME Communications,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 25, 2025
Abstract
The
rhizosphere
is
the
soil
region
around
plant
roots
hosting
a
diverse
microbial
community,
influencing
nutrient
availability
and
how
plants
react
to
extreme
conditions.
However,
our
understanding
of
fungi
biodiversity
impact
environmental
variations
on
this
still
in
its
infancy.
Our
study
investigates
fungal
communities’
diversity
functional
traits
Nothofagus
pumilio,
one
few
winters
deciduous
treeline
species
world,
forming
southern
South
America.
At
four
distinct
locations
covering
10°
latitude,
we
collected
samples
at
200
meters
below
over
seasons
during
single
year.
We
employed
ITS
metabarcoding
elucidate
community
structures.
results
reveal
that
was
mainly
determined
by
latitudinal
variation,
with
higher
levels
warmer
lower
altitudes.
Interestingly,
found
marked
dominance
ectomycorrhizal
(EcM)
treeline,
particularly
winter.
In
contrast,
saprotrophic
were
more
abundant
altitudes,
spring
summer
seasons.
These
findings
highlight
temporal
spatial
dynamics
rhizospheric
communities
their
potential
roles
ecological
processes,
emphasizing
value
these
as
indicators
change
high-elevation
forests.
Regional Environmental Change,
Journal Year:
2024,
Volume and Issue:
24(3)
Published: June 24, 2024
Abstract
In
the
European
Alps,
mean
temperature
has
risen
by
2.5
K
since
end
of
nineteenth
century.
A
2
warming
growing
season
taken
place
in
last
4
decades
only.
The
should
rise
position
climatic
treeline
about
400
m.
Actual
shifts
uppermost
tree
positions
reported
here
for
Austrian
Defereggen
Valley
and
Swiss
Lower
Engadine
region
Eastern
Alps
reach
only
around
140
m
elevation
above
limit
old
trees
that
date
back
to
Uppermost
Pinus
cembra
>
height
currently
occur
at
c.
2500
m,
representing
records
Alps.
situ
2022–2023
revealed
seasonal
temperatures
are
1–3
higher
than
equilibrium
isotherm
6
°C
both
regions
(corrected
anomalies
from
long-term
records).
span
reflects
microhabitat
differences
two
ways
define
season.
Thus,
advances
lag
behind
upslope
shift
isotherm,
on
average,
more
200
grow
under
quite
warm
conditions
with
annual
shoot
length
increments
frequently
reaching
20
cm.
Even
without
additional
future
warming,
new
steady-state
will
exceed
Holocene
maximum
substantially.
Journal of Ecology,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 2, 2025
Abstract
Alpine
ecosystems,
highly
sensitive
to
climate
change,
are
experiencing
shifts
in
species
ranges
and
community
structure.
These
changes
driven
by
a
complex
interplay
of
climatic
environmental
factors,
land
use
changes,
geomorphological
dynamics,
interactions,
which
can
often
lead
contrasted
sometimes
unexpected
dynamics.
Historical
records
provide
valuable
opportunity
capture
these
complexities
revealing
long‐term
opening
gateway
hypothesise
about
the
key
underlying
processes.
We
investigated
floristic
composition
subalpine
nival
vegetation
communities
resurveying
period
70
years.
To
understand
patterns,
we
(i)
resampled
at
plot
level
remapped
area,
(ii)
analysed
role
driving
climate,
environmental,
factors
on
distribution
vascular
plant
richness,
(iii)
modelled
plant‐plant
interactions
from
data.
The
results
reveal
that
cover
patterns
were
strongly
influenced
local
soil
properties.
richness
is
also
livestock
density
flat
morphology.
It
should
be
noted
change
caused
wetland
habitats
become
drier
accelerated
secondary
succession
through
upward
migration
range‐infilling
Furthermore,
trend
towards
eutrophication
was
observed.
suggested
certain
communities,
particularly
those
found
snowbeds,
more
vulnerable
have
occurred
over
past
Synthesis:
This
study
highlighted
complexity
In
addition
thermophilisation
aridification,
affect
composition,
cover.
Substrate
conditions
play
an
important
role.
Ecology and Evolution,
Journal Year:
2025,
Volume and Issue:
15(5)
Published: May 1, 2025
ABSTRACT
Alpine
treelines
ecotones
are
critical
ecological
transition
zones
and
highly
sensitive
to
global
warming.
However,
the
impact
of
climate
on
distribution
treeline
trees
is
not
yet
fully
understood
as
this
may
also
be
affected
by
other
factors.
Here,
we
used
high‐resolution
satellite
images
with
climatic
topographic
variables
study
changes
in
tree
alpine
ecotone
Changbai
Mountain
for
years
2002,
2010,
2017,
2021.
This
employed
Geodetector
method
analyze
how
interactions
between
factors
influence
expansion
Betula
ermanii
different
aspect
slopes.
Over
past
20
years,
B.
,
only
species
tundra
zone,
had
its
highest
rate
from
2017
2021
across
all
studied,
approaching
2.38%
per
year.
In
2021,
reached
uppermost
elevations
2224
m
western
aspects
2223
northern
aspects,
which
predominant
it
occupies.
We
observed
a
notable
increase
steeper
slopes
(>
15°)
2002
Moreover,
found
that
played
more
significant
role
's
than
any
single
dominant
factor.
Our
results
suggest
interaction
wetness
index
coldest
month
precipitation
(Pre
1
),
contributing
91%
variability,
primarily
drove
southern
maintaining
soil
moisture,
providing
snowpack
thermal
insulation
enhanced
temperatures,
decomposition,
nutrient
release
harsh
conditions.
On
aspect,
elevation
mean
temperature
warmest
explained
80%
expansion.
Meanwhile,
Pre
growing
season
73%
aspect.
revealed
driving
upward
movement
vary
mountain
aspects.
Climate
topography
play
roles
determining
ecotone.
knowledge
helps
better
understand
forecast
dynamics
response
change.