Diversity and Distributions,
Journal Year:
2020,
Volume and Issue:
26(12), P. 1646 - 1662
Published: Sept. 15, 2020
Abstract
Aims
Primary
forests
are
critical
for
forest
biodiversity
and
provide
key
ecosystem
services.
In
Europe,
these
particularly
scarce
it
is
unclear
whether
they
sufficiently
protected.
Here
we
aim
to:
(a)
understand
extant
primary
representative
of
the
range
naturally
occurring
types,
(b)
identify
types
which
host
enough
under
strict
protection
to
meet
conservation
targets
(c)
highlight
areas
where
restoration
needed
feasible.
Location
Europe.
Methods
We
combined
a
unique
geodatabase
with
maps
cover,
potential
natural
vegetation,
biogeographic
regions
protected
quantify
proportion
across
Europe's
gaps
in
protection.
Using
spatial
predictions
locations
account
underreporting
forests,
then
highlighted
could
complement
Results
found
substantial
bias
distribution
types.
Of
54
assessed,
six
had
no
at
all,
two‐thirds
less
than
1%
was
primary.
Even
if
generally
protected,
only
ten
more
half
their
strictly
Protecting
all
documented
requires
expanding
area
networks
by
1,132
km
2
(19,194
when
including
also
predicted
forests).
Encouragingly,
large
non‐primary
existed
inside
most
thus
presenting
opportunities.
Main
conclusion
perilous
state,
as
acknowledged
EU's
“Biodiversity
Strategy
2030.”
Yet,
there
considerable
opportunities
ensuring
better
restoring
structure,
composition
functioning,
least
partially.
advocate
integrated
policy
reforms
that
explicitly
irreplaceable
nature
ramp
up
efforts
alike.
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
27(11), P. 2279 - 2297
Published: March 16, 2021
Abstract
Forest
microclimates
contrast
strongly
with
the
climate
outside
forests.
To
fully
understand
and
better
predict
how
forests'
biodiversity
functions
relate
to
change,
need
be
integrated
into
ecological
research.
Despite
potentially
broad
impact
of
on
response
forest
ecosystems
global
our
understanding
within
below
tree
canopies
modulate
biotic
responses
change
at
species,
community
ecosystem
level
is
still
limited.
Here,
we
review
spatial
temporal
variation
in
result
from
an
interplay
features,
local
water
balance,
topography
landscape
composition.
We
first
stress
exemplify
importance
considering
across
landscapes.
Next,
explain
macroclimate
warming
(of
free
atmosphere)
can
affect
microclimates,
vice
versa,
via
interactions
land‐use
changes
different
biomes.
Finally,
perform
a
priority
ranking
future
research
avenues
interface
microclimate
ecology
biology,
specific
focus
three
key
themes:
(1)
disentangling
abiotic
drivers
feedbacks
microclimates;
(2)
regional
mapping
predictions
(3)
impacts
functioning
face
change.
The
availability
microclimatic
data
will
significantly
increase
coming
decades,
characterizing
variability
unprecedented
scales
relevant
biological
processes
This
revolutionize
dynamics,
implications
functions,
changes.
In
order
support
sustainable
use
forests
secure
their
services
for
generations,
cannot
ignored.
Ecography,
Journal Year:
2018,
Volume and Issue:
42(1), P. 1 - 11
Published: June 21, 2018
Forest
canopies
buffer
climate
extremes
and
promote
microclimates
that
may
function
as
refugia
for
understory
species
under
changing
climate.
However,
the
biophysical
conditions
maintain
microclimatic
buffering
its
stability
through
time
are
largely
unresolved.
We
posited
forest
is
sensitive
to
local
water
balance
canopy
cover,
we
measured
this
effect
during
growing
season
across
a
gradient
in
forests
of
northwestern
United
States
(US).
found
maximum
temperature
vapor
pressure
deficit
(VPD),
with
biologically
meaningful
sizes.
For
example,
season,
VPD
at
least
50%
were
5.3°C
1.1
kPa
lower
on
average,
respectively,
compared
areas
without
cover.
Canopy
was
greater
higher
levels
varied
balance,
implying
effects
subject
changes
hydrology.
project
mid‐21st
century
predict
how
such
impact
ability
western
US
extremes.
Our
results
suggest
some
will
lose
their
capacity
sites
become
increasingly
limited.
Changes
combined
accelerating
losses
due
increases
frequency
severity
disturbance
create
potentially
non‐linear
microclimate
forests.
Ecography,
Journal Year:
2016,
Volume and Issue:
40(2), P. 253 - 266
Published: Nov. 3, 2016
The
role
of
modern
climatic
microrefugia
is
a
neglected
aspect
in
the
study
biotic
responses
to
anthropogenic
climate
change.
Current
projections
species
redistribution
at
continental
extent
are
based
on
grids
coarse
(≥
1
km)
resolutions
that
fail
capture
spatiotemporal
dynamics
associated
with
microrefugia.
Here,
we
review
recent
methods
model
component
potential
and
highlight
research
gaps
accounting
for
buffering
capacity
due
biophysical
processes
operating
very
fine
(<
m)
(e.g.
canopy
cover)
microclimatic
stability
over
time
(i.e.
decoupling).
To
overcome
this
challenge,
propose
spatially
hierarchical
downscaling
framework
combining
free‐air
temperature
grid
km
resolution,
digital
elevation
25
m
resolution
small‐footprint
light
detection‐and‐ranging
(LiDAR)
data
50
cm
knowledge
from
literature
mechanistically
sub‐canopy
temperatures
account
decoupling.
We
applied
virtual
simulated
impact
warming
scenario
its
distribution.
Modelling
enlarges
range
conditions
towards
cold
end
gradient,
mitigates
regional
changes
decreases
extirpation
risks.
Incorporating
these
into
models,
being
correlative,
mechanistic
or
hybrid,
will
increase
probability
local
persistence,
which
has
important
consequences
understanding
adapt.
finally
provide
synthesis
additional
ways
field
could
move
effectively
considering
redistribution.
Global Change Biology,
Journal Year:
2018,
Volume and Issue:
24(11), P. 5243 - 5258
Published: Sept. 23, 2018
Local-scale
microclimatic
conditions
in
forest
understoreys
play
a
key
role
shaping
the
composition,
diversity
and
function
of
these
ecosystems.
Consequently,
understanding
what
drives
variation
microclimate
is
critical
to
forecasting
ecosystem
responses
global
change,
particularly
tropics
where
many
species
already
operate
close
their
thermal
limits
rapid
land-use
transformation
profoundly
altering
local
environments.
Yet
our
ability
characterize
at
ecologically
meaningful
scales
remains
limited,
as
understorey
cannot
be
directly
measured
from
outside
canopy.
To
address
this
challenge,
we
established
network
sensors
across
intensity
gradient
spanning
old-growth
forests
oil-palm
plantations
Borneo.
We
then
combined
observations
with
high-resolution
airborne
laser
scanning
data
how
topography
canopy
structure
shape
both
locally
landscape.
In
processes,
generated
surfaces
over
350
km2
,
which
used
explore
potential
impacts
habitat
degradation
on
regeneration
under
current
future
climate
scenarios.
found
that
vegetation
were
strong
predictors
microclimate,
elevation
terrain
curvature
primarily
constraining
daily
mean
temperatures
vapour
pressure
deficit
(VPD),
whereas
height
had
clear
dampening
effect
extremes.
This
buffering
was
pronounced
wind-exposed
slopes
but
tended
saturate
once
exceeded
20
m-suggesting
despite
intensive
logging,
secondary
remain
largely
thermally
buffered.
Nonetheless,
landscape-scale
highly
heterogeneous,
maximum
ranging
between
24.2
37.2°C
VPD
two
orders
magnitude.
Based
this,
estimate
by
end
century
could
hampered
degraded
much
Borneo's
lowlands
if
continue
rise
following
projected
trends.
Ecological Applications,
Journal Year:
2019,
Volume and Issue:
30(2)
Published: Nov. 23, 2019
Abstract
A
stable
below‐canopy
microclimate
of
forests
is
essential
for
their
biodiversity
and
ecosystem
functionality.
Forest
management
necessarily
modifies
the
buffering
capacity
woodlands.
However,
specific
effects
different
forestry
treatments
on
site
conditions,
temporal
recovery
after
harvests,
reason
contrasts
between
are
still
poorly
understood.
The
four
(clear‐cutting,
retention
tree
group,
preparation
cutting,
gap‐cutting)
microclimatic
variables
were
studied
within
a
field
experiment
in
managed
oak‐dominated
stand
Hungary,
before
(2014)
(2015–2017)
interventions
by
complete
block
design
with
six
replicates.
From
first
post‐treatment
year,
clear‐cuts
differed
most
from
uncut
control
due
to
increased
irradiance
heat
load.
Means
variability
air
soil
temperature
increased,
became
dryer
along
higher
moisture
levels.
Retention
groups
could
effectively
ameliorate
extreme
temperatures
but
not
mean
values.
Preparation
cutting
induced
slight
changes
original
buffered
humid
forest
microclimate.
Despite
substantially
more
incoming
light,
gap‐cutting
retain
cool
conditions
showed
highest
increase
interventions.
For
variables,
we
observe
any
obvious
trend
3
yr.
decreased
time
clear‐cuts,
while
difference
continuously
gap‐
clear‐cuts.
Based
multivariate
analyses,
separated
significantly
based
mainly
maxima
variability.
We
found
that
(1)
effect
sizes
among
treatment
levels
consistent
throughout
years,
(2)
climatic
appears
be
far
than
yr,
(3)
applied
silvicultural
methods
diverged
maxima.
our
study,
spatially
heterogeneous
fine‐scaled
continuous
cover
(gap‐cutting,
selection
systems)
recommended.
By
applying
these
practices,
structural
elements
creating
successfully
maintained.
Thus,
induce
less
pronounced
alterations
environmental
forest‐dwelling
organism
groups.
Global Change Biology,
Journal Year:
2019,
Volume and Issue:
25(7), P. 2485 - 2498
Published: May 6, 2019
Abstract
Elevational
gradients
are
often
used
to
quantify
how
traits
of
plant
species
respond
abiotic
and
biotic
environmental
variations.
Yet,
such
analyses
frequently
restricted
spatially
applied
along
single
slopes
or
mountain
ranges.
Since
we
know
little
on
the
response
intraspecific
leaf
elevation
across
globe,
here
perform
a
global
meta‐analysis
in
109
located
4
continents
reported
71
studies
published
between
1983
2018.
We
quantified
change
seven
morpho‐ecophysiological
elevational
gradients:
specific
area
(SLA),
mass
per
(LMA),
(LA),
nitrogen
concentration
unit
(N
),
phosphorous
(P
)
carbon
isotope
composition
(δ
13
C).
found
LMA,
N
,
δ
C
significantly
increase
SLA
decrease
with
increasing
elevation.
Conversely,
LA
P
showed
no
significant
pattern
worldwide.
larger
warmer
regions.
Larger
responses
were
apparent
for
herbaceous
compared
woody
species,
but
not
other
traits.
Finally,
also
detected
evidences
covariation
morphological
physiological
within
same
gradient.
In
sum,
demonstrate
that
there
common
cross‐species
patterns
trait
variation
Irrespective
whether
is
genetically
determined
via
local
adaptation
attributed
phenotypic
plasticity,
suggest
adapted
live
range
temperature
conditions.
distribution
biota
predominantly
shifting
upslope
changes
conditions,
our
results
important
further
understanding
plants
ecosystems
adapt
change.