Functional Ecology,
Journal Year:
2016,
Volume and Issue:
30(7), P. 1109 - 1121
Published: March 19, 2016
Summary
It
is
increasingly
acknowledged
that
plant–soil
feedbacks
may
play
an
important
role
in
driving
the
composition
of
plant
communities
and
functioning
terrestrial
ecosystems.
However,
mechanistic
understanding
feedbacks,
as
well
their
roles
natural
ecosystems
proportion
to
other
possible
drivers,
still
its
infancy.
Such
knowledge
will
enhance
our
capacity
determine
contribution
feedback
community
ecosystem
responses
under
global
environmental
change.
Here,
we
review
how
develop
extreme
drought
precipitation
events,
CO
2
nitrogen
enrichment,
temperature
increase,
land
use
change
species
loss
vs.
gain.
We
present
a
framework
for
opening
‘black
box
soil’
considering
various
biotic
components
(enemies,
symbionts
decomposers)
changes,
discuss
integrate
these
understand
predict
net
effects
scenarios
To
gain
plays
out
realistic
settings,
also
interaction
with
drivers
composition,
including
competition,
facilitation,
herbivory,
soil
physical
chemical
properties.
conclude
shaping
processes
changes
requires
unravelling
individual
contributions
enemies,
decomposers.
These
factors
show
different
response
rates
strengths,
thereby
resulting
magnitudes
directions
need
tests
more
conditions
patterns
field,
both
at
ecologically
evolutionary
relevant
time‐scales.
Proceedings of the National Academy of Sciences,
Journal Year:
2012,
Volume and Issue:
109(52), P. 21390 - 21395
Published: Dec. 10, 2012
For
centuries
ecologists
have
studied
how
the
diversity
and
functional
traits
of
plant
animal
communities
vary
across
biomes.
In
contrast,
we
only
just
begun
exploring
similar
questions
for
soil
microbial
despite
microbes
being
dominant
engines
biogeochemical
cycles
a
major
pool
living
biomass
in
terrestrial
ecosystems.
We
used
metagenomic
sequencing
to
compare
composition
attributes
16
collected
from
cold
deserts,
hot
forests,
grasslands,
tundra.
Those
found
plant-free
desert
soils
typically
had
lowest
levels
(diversity
protein-coding
gene
categories)
phylogenetic
taxonomic
diversity.
Across
all
soils,
beta
was
strongly
correlated
with
diversity;
were
clearly
distinct
nondesert
regardless
metric
used.
The
higher
relative
abundances
genes
associated
osmoregulation
dormancy,
but
lower
nutrient
cycling
catabolism
plant-derived
organic
compounds.
Antibiotic
resistance
consistently
threefold
less
abundant
than
suggesting
that
abiotic
conditions,
not
competitive
interactions,
are
more
important
shaping
communities.
As
most
comprehensive
survey
taxonomic,
phylogenetic,
date,
this
study
demonstrates
approaches
can
be
build
predictive
understanding
function
Frontiers in Microbiology,
Journal Year:
2012,
Volume and Issue:
3
Published: Jan. 1, 2012
A
major
thrust
of
terrestrial
microbial
ecology
is
focused
on
understanding
when
and
how
the
composition
community
affects
functioning
biogeochemical
processes
at
ecosystem
scale
(meters-to-kilometers
days-to-years).
While
research
has
demonstrated
these
linkages
for
physiologically
phylogenetically
"narrow"
such
as
trace
gas
emissions
nitrification,
there
less
conclusive
evidence
that
influences
"broad"
decomposition
organic
matter
turnover
in
soil.
In
this
paper,
we
consider
soil
structure
C-cycling.
We
phylogenetic
level
which
microbes
form
meaningful
guilds,
based
overall
life
history
strategies,
suggest
are
associated
with
deep
evolutionary
divergences,
while
much
species-level
diversity
probably
reflects
functional
redundancy.
then
under
what
conditions
it
possible
differences
among
to
affect
process
dynamics,
argue
may
be
important
rate
OM
breakdown
rhizosphere
detritus,
likely
not
mineral
soil,
physical
access
occluded
or
sorbed
substrates
rate-limiting
process.
Microbial
soils
organisms
allocate
C
they
take
up—not
only
do
fates
molecules
differ,
but
can
system
differently
well.
For
example,
extracellular
enzymes
polysaccharides
key
controls
function.
How
also
particularly
long-term
fate
soil—is
sequestered
not?
Frontiers in Plant Science,
Journal Year:
2017,
Volume and Issue:
8
Published: Sept. 19, 2017
In
their
natural
environment
plants
are
part
of
a
rich
ecosystem
including
numerous
and
diverse
microorganisms
in
the
soil.
It
has
been
long
recognized
that
some
these
microbes,
such
as
mycorrhizal
fungi
or
nitrogen
fixing
symbiotic
bacteria,
play
important
roles
plant
performance
by
improving
mineral
nutrition.
However,
full
range
microbes
associated
with
potential
to
replace
synthetic
agricultural
inputs
only
recently
started
be
uncovered.
last
few
years
great
progress
made
knowledge
on
composition
rhizospheric
microbiomes
dynamics.
There
is
clear
evidence
shape
microbiome
structures,
most
probably
root
exudates,
also
bacteria
have
developed
various
adaptations
thrive
niche.
The
mechanisms
interactions
processes
driving
alterations
however
largely
unknown.
this
review
we
focus
interaction
enhancing
nutrition,
summarizing
current
several
research
fields
can
converge
improve
our
understanding
molecular
underpinning
phenomenon.
Proceedings of the National Academy of Sciences,
Journal Year:
2015,
Volume and Issue:
112(35), P. 10967 - 10972
Published: Aug. 17, 2015
Significance
Human
activities
have
resulted
in
large
increases
the
availability
of
nutrients
terrestrial
ecosystems
worldwide.
Although
plant
community
responses
to
elevated
been
well
studied,
soil
microbial
remain
poorly
understood,
despite
their
critical
importance
ecosystem
functioning.
Using
DNA-sequencing
approaches,
we
assessed
response
communities
experimentally
added
nitrogen
and
phosphorus
at
25
grassland
sites
across
globe.
Our
results
demonstrate
that
composition
these
shifts
consistent
ways
with
nutrient
inputs
there
are
corresponding
ecological
attributes
members.
This
study
represents
an
important
step
forward
for
understanding
connection
between
inputs,
communities,
altered
Global Change Biology,
Journal Year:
2012,
Volume and Issue:
18(6), P. 1918 - 1927
Published: Jan. 11, 2012
Abstract
Ecosystems
worldwide
are
receiving
increasing
amounts
of
reactive
nitrogen
(
N
)
via
anthropogenic
activities
with
the
added
having
potentially
important
impacts
on
microbially
mediated
belowground
carbon
dynamics.
However,
a
comprehensive
understanding
how
elevated
availability
affects
soil
microbial
processes
and
community
dynamics
remains
incomplete.
The
mechanisms
responsible
for
observed
responses
poorly
resolved
we
do
not
know
if
communities
respond
in
similar
manner
across
ecosystems.
We
collected
28
soils
from
broad
range
ecosystems
orth
A
merica,
amended
inorganic
,
incubated
under
controlled
conditions
1
year.
Consistent
nearly
all
soils,
addition
decreased
respiration
rates,
an
average
decrease
11%
over
year‐long
incubation,
biomass
by
35%.
High‐throughput
pyrosequencing
showed
that
consistently
altered
bacterial
composition,
relative
abundance
ctinobacteria
F
irmicutes
decreasing
cidobacteria
V
errucomicrobia
.
Further,
‐amended
had
lower
suite
extracellular
enzymes
temperature
sensitivity,
suggesting
shift
to
preferential
decomposition
more
labile
C
pools.
trends
held
strong
gradients
climate
characteristics,
indicating
likely
wide‐spread
mechanisms.
Our
results
support
hypothesis
depresses
activity
shifting
metabolic
capabilities
communities,
yielding
less
capable
decomposing
recalcitrant
pools
leading
potential
increase
sequestration
rates.
Proceedings of the National Academy of Sciences,
Journal Year:
2016,
Volume and Issue:
113(21), P. 5970 - 5975
Published: May 2, 2016
Significance
Ecological
scaling
laws
are
intensively
studied
for
their
predictive
power
and
universal
nature
but
often
fail
to
unify
biodiversity
across
domains
of
life.
Using
a
global-scale
compilation
microbial
macrobial
data,
we
uncover
relationships
commonness
rarity
that
scale
with
abundance
at
similar
rates
microorganisms
macroscopic
plants
animals.
We
then
show
unified
law
predicts
the
dominant
species
30
orders
magnitude
all
on
Earth.
this
combined
lognormal
model
biodiversity,
predict
Earth
is
home
as
many
1
trillion
(10
12
)
species.
The ISME Journal,
Journal Year:
2019,
Volume and Issue:
14(1), P. 1 - 9
Published: Sept. 25, 2019
Microorganisms
are
critical
in
terrestrial
carbon
cycling
because
their
growth,
activity
and
interactions
with
the
environment
largely
control
fate
of
recent
plant
inputs
as
well
protected
soil
organic
[1,
2].
Soil
stocks
reflect
a
balance
between
microbial
decomposition
stabilisation
assimilated
carbon.
The
can
shift
under
altered
environmental
conditions
[3],
new
research
suggests
that
knowledge
physiology
may
be
for
projecting
changes
improving
prognosis
climate
change
feedbacks
[4–7].
Still,
predicting
ecosystem
implications
processes
remains
challenge.
Here
we
argue
this
challenge
met
by
identifying
life
history
strategies
based
on
an
organism’s
phenotypic
characteristics,
or
traits,
representing
these
models.
What
key
traits
change?
Microbial
growth
survival
impacted
multiple
determine
responses
to
varying
resource
availability
fluctuating
abiotic
[8].
Cellular
maintenance
activities
(those
do
not
produce
growth)
include
production
extracellular
enzymes
degrade
acquire
resources,
biomolecular
repair
mechanisms,
cellular
integrity,
osmotic
balance,
defence,
antagonism,
cell
signalling
motility
[9–11].
It
is
conceivable
investment
into
would
generally
high
soils,
highly
heterogeneous
temporally
variable
distribution
stressful
like
extremes
moisture,
temperature,
pH
salinity
[12,
13].
Selective
pressures
suboptimal
could
lead
greater
cellular-level
physiological
allocation
relative
(Fig. 1)
thereby
impacting
processes.
Open
separate
window
Fig.
1
Schematic
showing
C
flux
includes
depolymerisation,
substrate
uptake,
assimilation,
dissimilation,
biomass
synthesis
non-growth
production.
Extracellular
enzyme
represents
acquisition,
stress
protein
linked
tolerance
reflects
higher
yield.
Forked
arrows
signify
metabolic
points
where
hypothesised
tradeoffs
might
occur.
expected
empirical
relationships
among
also
shown