New Phytologist,
Journal Year:
2016,
Volume and Issue:
212(4), P. 871 - 887
Published: Oct. 27, 2016
Summary
Humans
have
long
utilized
resources
from
all
forest
biomes,
but
the
most
indelible
anthropogenic
signature
has
been
expanse
of
human
populations
in
temperate
forests.
The
purpose
this
review
is
to
bring
into
focus
diverse
forests
region
biosphere,
including
those
hardwood,
conifer
and
mixed
dominance,
with
a
particular
emphasis
on
crucial
challenges
for
future
these
forested
areas.
Implicit
term
‘temperate’
that
predominant
climate
regions
distinct
cyclic,
seasonal
changes
involving
periods
growth
dormancy.
specific
temporal
patterns
change,
however,
display
an
impressive
variability
among
regions.
In
addition
more
apparent
current
disturbances
forests,
such
as
management
conversion
agriculture,
alteration
actually
ancient
phenomenon,
going
far
back
7000
yr
before
present
(
bp
).
As
deep‐seated
past
legacies
are
perturbations,
timber
harvesting,
excess
nitrogen
deposition,
altered
species’
phenologies,
increasing
frequency
drought
fire,
must
be
viewed
through
lens
change.
Contents
871
I.
Introduction
II.
A
brief
biogeography
history
874
III.
Climate,
soils,
composition
land
use
875
IV.
Climate
change
878
V.
Epilogue
882
Acknowledgements
884
References
Ecological Applications,
Journal Year:
2010,
Volume and Issue:
20(1), P. 30 - 59
Published: Jan. 1, 2010
Atmospheric
nitrogen
(N)
deposition
is
a
recognized
threat
to
plant
diversity
in
temperate
and
northern
parts
of
Europe
North
America.
This
paper
assesses
evidence
from
field
experiments
for
N
effects
thresholds
terrestrial
protection
across
latitudinal
range
main
categories
ecosystems,
arctic
boreal
systems
tropical
forests.
Current
thinking
on
the
mechanisms
diversity,
global
distribution
G200
ecoregions,
current
future
(2030)
estimates
atmospheric
N-deposition
rates
are
then
used
identify
risks
all
major
ecosystem
types
now
future.
synthesis
clearly
shows
that
accumulation
driver
changes
species
composition
whole
different
by
driving
competitive
interactions
lead
change
and/or
making
conditions
unfavorable
some
species.
Other
such
as
direct
toxicity
gases
aerosols,
long-term
negative
increased
ammonium
ammonia
availability,
soil-mediated
acidification,
secondary
stress
disturbance
more
ecosystem-
site-specific
often
play
supporting
role.
mediterranean
ecosystems
have
been
identified,
leading
first
estimate
an
effect
threshold.
Importantly,
thought
not
limited,
subtropical
systems,
may
be
vulnerable
regeneration
phase,
situations
where
heterogeneity
availability
reduced
deposition,
sandy
soils,
or
montane
areas.
Critical
loads
critical
load
concept
has
helped
European
governments
make
progress
toward
reducing
sensitive
ecosystems.
More
needs
done
America,
especially
types,
including
several
high
conservation
importance.
The
results
this
assessment
show
regions
outside
America
which
received
enough
attention
ecoregions
eastern
southern
Asia
(China,
India),
important
part
ecoregion
(California,
Europe),
coming
decades
Latin
Africa.
Reductions
widespread
than
thought,
targeted
studies
required
low
background
areas,
ecoregions.
Proceedings of the National Academy of Sciences,
Journal Year:
2013,
Volume and Issue:
110(46), P. 18561 - 18565
Published: Oct. 28, 2013
Significance
Around
the
globe,
climate
warming
is
increasing
dominance
of
warm-adapted
species—a
process
described
as
“thermophilization.”
However,
thermophilization
often
lags
behind
itself,
with
some
recent
studies
showing
no
response
at
all.
Using
a
unique
database
more
than
1,400
resurveyed
vegetation
plots
in
forests
across
Europe
and
North
America,
we
document
significant
understory
vegetation.
to
macroclimate
was
attenuated
whose
canopies
have
become
denser.
This
microclimatic
effect
likely
reflects
cooler
forest-floor
temperatures
via
increased
shading
during
growing
season
denser
forests.
Because
standing
stocks
trees
many
temperate
decades,
microclimate
may
commonly
buffer
plant
responses
warming.
Agronomy for Sustainable Development,
Journal Year:
2012,
Volume and Issue:
33(2), P. 291 - 309
Published: Jan. 30, 2012
Compaction
of
agricultural
soils
is
a
concern
for
many
soil
scientists
and
farmers
since
compaction,
due
to
heavy
field
traffic,
has
resulted
in
yield
reduction
most
agronomic
crops
throughout
the
world.
Soil
compaction
physical
form
degradation
that
alters
structure,
limits
water
air
infiltration,
reduces
root
penetration
soil.
Consequences
are
still
underestimated.
A
complete
understanding
processes
involved
necessary
meet
future
global
challenge
food
security.
We
review
here
advances
understanding,
quantification,
prediction
effects
compaction.
found
following
major
points:
(1)
When
exposed
vehicular
traffic
load,
contents,
texture
organic
matter
three
main
factors
which
determine
degree
compactness
(2)
direct
on
properties
such
as
bulk
density,
strength,
porosity;
therefore,
these
parameters
can
be
used
quantify
compactness.
(3)
Modified
alter
elements
mobility
change
nitrogen
carbon
cycles
favour
more
emissions
greenhouse
gases
under
wet
conditions.
(4)
Severe
induces
deformation,
stunted
shoot
growth,
late
germination,
low
germination
rate,
high
mortality
rate.
(5)
decreases
biodiversity
by
decreasing
microbial
biomass,
enzymatic
activity,
fauna,
ground
flora.
(6)
Boussinesq
equations
finite
element
method
models,
predict
restricted
elastic
domain
do
not
consider
existence
preferential
paths
stress
propagation
localization
deformation
compacted
soils.
(7)
Recent
physics
granular
media
mechanics
relevant
should
progress
modelling
Ecological Applications,
Journal Year:
2011,
Volume and Issue:
21(8), P. 3049 - 3082
Published: May 25, 2011
Human
activity
in
the
last
century
has
led
to
a
significant
increase
nitrogen
(N)
emissions
and
atmospheric
deposition.
This
N
deposition
reached
level
that
caused
or
is
likely
cause
alterations
structure
function
of
many
ecosystems
across
United
States.
One
approach
for
quantifying
pollution
would
be
harmful
determination
critical
loads.
A
load
defined
as
input
pollutant
below
which
no
detrimental
ecological
effects
occur
over
long-term
according
present
knowledge.
The
objectives
this
project
were
synthesize
current
research
relating
on
terrestrial
freshwater
States,
estimate
associated
empirical
receptors
considered
included
diatoms,
mycorrhizal
fungi,
lichens,
bryophytes,
herbaceous
plants,
shrubs,
trees.
Ecosystem
impacts
included:
(1)
biogeochemical
responses
(2)
individual
species,
population,
community
responses.
Biogeochemical
increased
mineralization
nitrification
(and
availability
plant
microbial
uptake),
gaseous
losses
(ammonia
volatilization,
nitric
nitrous
oxide
from
denitrification),
leaching.
Individual
tissue
N,
physiological
nutrient
imbalances,
growth,
altered
root
:
shoot
ratios,
susceptibility
secondary
stresses,
fire
regime,
shifts
competitive
interactions
composition,
changes
species
richness
other
measures
biodiversity,
increases
invasive
species.
range
loads
reported
U.S.
ecoregions,
inland
surface
waters,
wetlands
1–39
kg
N·ha−1·yr−1,
spanning
observed
most
country.
tend
following
sequence
different
life
forms:
lichens
plants
an
ecosystem
assessment
tool
with
great
potential
simplify
complex
scientific
information
communicate
effectively
policy
public.
synthesis
represents
first
comprehensive
major
ecoregions
Global Change Biology,
Journal Year:
2013,
Volume and Issue:
19(7), P. 2001 - 2021
Published: March 25, 2013
Forest
regeneration
following
disturbance
is
a
key
ecological
process,
influencing
forest
structure
and
function,
species
assemblages,
ecosystem-climate
interactions.
Climate
change
may
alter
recovery
dynamics
or
even
prevent
recovery,
triggering
feedbacks
to
the
climate
system,
altering
regional
biodiversity,
affecting
ecosystem
services
provided
by
forests.
Multiple
lines
of
evidence
-
including
global-scale
patterns
in
dynamics;
responses
experimental
manipulation
CO2
,
temperature,
precipitation;
that
has
already
occurred;
theory;
earth
system
models
all
indicate
are
sensitive
climate.
However,
synthetic
understanding
how
atmospheric
shape
trajectories
lacking.
Here,
we
review
these
separate
evidence,
which
together
demonstrate
being
impacted
increasing
changing
Rates
generally
increase
with
water
availability.
Drought
reduces
growth
live
biomass
forests
ages,
having
particularly
strong
effect
on
seedling
recruitment
survival.
Responses
individual
trees
whole-forest
ecosystems
manipulations
often
vary
age,
implying
different
ages
will
respond
differently
change.
Furthermore,
within
community
typically
exhibit
differential
climate,
altered
can
have
important
consequences
for
function.
Age-
species-dependent
provide
mechanism
push
some
past
critical
thresholds
such
they
fail
recover
their
previous
state
disturbance.
Altered
result
positive
negative
Future
research
this
topic
corresponding
improvements
be
future
system.
Journal of Ecology,
Journal Year:
2011,
Volume and Issue:
100(2), P. 352 - 365
Published: Nov. 28, 2011
Summary
1.
Atmospheric
nitrogen
(N)
deposition
is
expected
to
change
forest
understorey
plant
community
composition
and
diversity,
but
results
of
experimental
addition
studies
observational
are
not
yet
conclusive.
A
shortcoming
studies,
which
generally
based
on
resurveys
or
sampling
along
large
gradients,
the
occurrence
temporal
spatial
confounding
factors.
2.
We
were
able
assess
contribution
N
versus
other
ecological
drivers
communities
by
combining
a
approach.
Data
from
1205
(semi‐)permanent
vegetation
plots
taken
23
rigorously
selected
resurvey
gradient
across
deciduous
temperate
in
Europe
compiled
related
various
local
regional
driving
factors,
including
rate
atmospheric
deposition,
herbivore
densities
canopy
cover
composition.
3.
Although
no
directional
species
richness
occurred,
there
was
considerable
floristic
turnover
shift
towards
more
shade‐tolerant
nutrient‐demanding
species.
However,
important
explaining
observed
eutrophication
signal.
This
signal
seemed
mainly
denser
changed
with
higher
share
easily
decomposed
litter.
4.
Synthesis.
Our
multi‐site
approach
clearly
demonstrates
that
one
should
be
cautious
when
drawing
conclusions
about
impact
interpretation
shifts
single
sites
regions
due
other,
concurrent,
changes.
Even
though
effects
chronically
increased
apparently
obscured
changes,
accumulated
might
still
have
significant
impact.
research
needed
whether
this
time
bomb
will
indeed
explode
canopies
open
up
again.
Global Change Biology,
Journal Year:
2010,
Volume and Issue:
16(10), P. 2688 - 2700
Published: Jan. 13, 2010
Abstract
Response
of
plant
biodiversity
to
increased
availability
nitrogen
(N)
has
been
investigated
in
temperate
and
boreal
forests,
which
are
typically
N‐limited,
but
little
is
known
tropical
forests.
We
examined
the
effects
artificial
N
additions
on
diversity
(species
richness,
density
cover)
understory
layer
an
saturated
old‐growth
forest
southern
China
test
following
hypothesis:
decrease
forests
primarily
from
N‐mediated
changes
soil
properties.
Experimental
were
administered
at
levels
July
2003
2008:
no
addition
(Control);
50
kg
ha
−1
yr
(Low‐N);
100
(Medium‐N),
150
(High‐N).
Results
showed
that
species
exhibited
positive
growth
response
any
level
during
study
period.
Although
low‐to‐medium
(≤100
)
generally
did
not
alter
through
time,
high
significantly
reduced
diversity.
This
was
most
closely
related
declines
within
tree
seedling
fern
functional
groups,
as
well
significant
increases
acidity
Al
mobility,
decreases
Ca
fine‐root
biomass.
mechanism
for
loss
provides
sharp
contrast
competition‐based
mechanisms
suggested
studies
communities
other
Our
results
suggest
high‐N
can
this
may
vary
with
rate
addition.
Global Change Biology,
Journal Year:
2019,
Volume and Issue:
25(11), P. 3625 - 3641
Published: July 13, 2019
Abstract
Temperate
forests
cover
16%
of
the
global
forest
area.
Within
these
forests,
understorey
is
an
important
biodiversity
reservoir
that
can
influence
ecosystem
processes
and
functions
in
multiple
ways.
However,
we
still
lack
a
thorough
understanding
relative
importance
for
temperate
functioning.
As
result,
understoreys
are
often
ignored
during
assessments
functioning
changes
thereof
under
change.
We
here
compiled
studies
quantify
functioning,
focussing
on
litter
production,
nutrient
cycling,
evapotranspiration,
tree
regeneration,
pollination
pathogen
dynamics.
describe
mechanisms
driving
develop
conceptual
framework
synthesizing
possible
effects
change
drivers
understorey‐mediated
Our
review
illustrates
understorey's
contribution
to
significant
but
varies
depending
function
environmental
context,
more
importantly,
characteristics
overstorey.
To
predict
its
change,
argue
simultaneous
investigation
both
overstorey
functional
responses
will
be
crucial.
shows
such
very
scarce,
only
available
limited
set
quantification,
providing
little
data
forecast