Global Change Biology,
Год журнала:
2022,
Номер
29(1), С. 231 - 242
Опубликована: Окт. 13, 2022
Microbial
communities
play
critical
roles
in
fixing
carbon
from
the
atmosphere
and
it
soils.
However,
large-scale
variations
drivers
of
these
microbial
remain
poorly
understood.
Here,
we
conducted
a
survey
across
China
found
that
soil
autotrophic
organisms
are
for
explaining
CO2
fluxes
to
In
particular,
showed
fixation
rates
highly
correlated
those
bacteria
phototrophic
protists.
Paddy
soils,
supporting
larger
proportion
obligate
bacterial
protist
autotrophs,
display
four-fold
over
upland
forest
Precipitation
pH,
together
with
key
ecological
clusters
microbes,
also
played
important
controlling
fixation.
Our
work
provides
novel
quantification
on
contribution
terrestrial
microbes
processes
at
large
scale,
implications
global
regulation
under
climate
change.
Global Change Biology,
Год журнала:
2019,
Номер
26(1), С. 261 - 273
Опубликована: Окт. 6, 2019
Managing
soil
organic
matter
(SOM)
stocks
to
address
global
change
challenges
requires
well-substantiated
knowledge
of
SOM
behavior
that
can
be
clearly
communicated
between
scientists,
management
practitioners,
and
policy
makers.
However,
is
incredibly
complex
separation
into
multiple
components
with
contrasting
in
order
study
predict
its
dynamics.
Numerous
diverse
schemes
are
currently
used,
making
cross-study
comparisons
difficult
hindering
broad-scale
generalizations.
Here,
we
recommend
separating
particulate
(POM)
mineral-associated
(MAOM)
forms,
two
fundamentally
different
terms
their
formation,
persistence,
functioning.
We
provide
evidence
highly
physical
chemical
properties,
mean
residence
times
soil,
responses
land
use
change,
plant
litter
inputs,
warming,
CO2
enrichment,
N
fertilization.
Conceptualizing
POM
versus
MAOM
a
feasible,
well-supported,
useful
framework
will
allow
scientists
move
beyond
studies
bulk
SOM,
but
also
consistent
scheme
across
studies.
Ultimately,
propose
the
as
best
way
forward
understand
dynamics
context
necessary
recommendations
managers
Global Change Biology,
Год журнала:
2019,
Номер
26(4), С. 1953 - 1961
Опубликована: Дек. 15, 2019
Numerous
studies
have
demonstrated
that
fertilization
with
nutrients
such
as
nitrogen,
phosphorus,
and
potassium
increases
plant
productivity
in
both
natural
managed
ecosystems,
demonstrating
primary
is
nutrient
limited
most
terrestrial
ecosystems.
In
contrast,
it
has
been
heterotrophic
microbial
communities
soil
are
primarily
by
organic
carbon
or
energy.
While
this
concept
of
contrasting
limitations,
is,
limitation,
based
on
strong
evidence
we
review
paper,
often
ignored
discussions
ecosystem
response
to
global
environment
changes.
The
plant-centric
perspective
equated
limitations
those
whole
thereby
ignoring
the
important
role
heterotrophs
responsible
for
decomposition
driving
storage.
To
truly
integrate
cycles
science,
must
account
fact
while
may
be
limited,
secondary
inherently
limited.
Ecosystem
cycling
integrates
independent
physiological
responses
its
individual
components,
well
tightly
coupled
exchanges
between
autotrophs
heterotrophs.
extent
interacting
autotrophic
processes
controlled
organisms
versus
accessibility,
respectively,
propose
ecosystems
definition
cannot
'limited'
alone.
Here,
outline
how
models
aimed
at
predicting
non-steady
state
over
time
can
benefit
from
dissecting
into
organismal
components
their
inherent
better
represent
plant-microbe
interactions
models.
Nature Communications,
Год журнала:
2020,
Номер
11(1)
Опубликована: Май 7, 2020
Soil
organic
matter
(SOM)
is
correlated
with
reactive
iron
(Fe)
in
humid
soils,
but
Fe
also
promotes
SOM
decomposition
when
oxygen
(O2)
becomes
limited.
Here
we
quantify
Fe-mediated
OM
protection
vs.
by
adding
13C
dissolved
(DOM)
and
57FeII
to
soil
slurries
incubated
under
static
or
fluctuating
O2.
We
find
uniformly
protects
only
oxic
conditions,
DOM
are
added
together:
de
novo
FeIII
phases
suppress
mineralization
35
47%,
respectively.
Conversely,
alone
increases
8%
following
oxidation
57FeIII.
Under
O2
limitation,
57FeIII
preferentially
reduced,
increasing
anaerobic
of
74%
32‒41%,
Periodic
limitation
common
so
does
not
intrinsically
protect
OM;
rather
require
their
own
physiochemical
contribute
persistence.
Global Change Biology,
Год журнала:
2021,
Номер
27(11), С. 2478 - 2490
Опубликована: Март 13, 2021
Paddy
soils
make
up
the
largest
anthropogenic
wetlands
on
earth,
and
are
characterized
by
a
prominent
potential
for
organic
carbon
(C)
sequestration.
By
quantifying
plant-
microbial-derived
C
in
across
four
climate
zones,
we
identified
that
accrual
is
achieved
via
contrasting
pathways
paddy
upland
soils.
Paddies
39%-127%
more
efficient
soil
(SOC)
sequestration
than
their
adjacent
counterparts,
with
greater
differences
warmer
cooler
climates.
Upland
replenished
C,
whereas
enriched
proportion
of
plant-derived
because
retarded
microbial
decomposition
under
anaerobic
conditions
induced
flooding
paddies.
Under
both
land-use
types,
maximal
contribution
plant
residues
to
SOC
at
intermediate
mean
annual
temperature
(15-20°C),
neutral
(pH~7.3),
low
clay/sand
ratio.
contrast,
high
(~24°C),
pH
(~5),
large
ratio
favorable
strengthening
necromass.
The
necromass
waterlogged
paddies
climates
likely
due
fast
anabolism
from
bacteria,
fungi
unlikely
be
involved
as
they
aerobic.
In
scenario
conversion
upland,
total
504
Tg
may
lost
CO
Environmental Science & Technology,
Год журнала:
2020,
Номер
54(10), С. 6174 - 6184
Опубликована: Апрель 16, 2020
Dissolved
organic
matter
(DOM)
plays
a
key
role
in
many
biogeochemical
processes,
but
the
drivers
controlling
diversity
of
chemical
composition
and
properties
DOM
molecules
(chemodiversity)
soils
are
poorly
understood.
It
has
also
been
debated
whether
environmental
conditions
or
intrinsic
molecular
control
accumulation
persistence
due
to
complexity
both
interactions
between
surrounding
environments.
In
this
study,
soil
samples
were
extracted
from
33
collected
different
regions
China,
we
investigated
effects
climate
on
chemodiversity
across
employing
combination
Fourier
transform
ion
cyclotron
resonance
mass
spectrometry,
optical
spectroscopy,
statistical
analyses.
Our
results
indicated
that,
despite
heterogeneity
complex
influencing
factors,
aridity
clay
can
account
for
majority
variations
composition.
The
finding
implied
that
is
an
ecosystem
property
closely
related
environment,
be
used
developing
large-scale
biogeochemistry
models
predicting
C
cycling
soils.
Environmental Research Letters,
Год журнала:
2019,
Номер
14(8), С. 083004 - 083004
Опубликована: Июнь 25, 2019
Abstract
Most
empirical
and
modeling
research
on
soil
carbon
(C)
dynamics
has
focused
those
processes
that
control
promote
C
stabilization.
However,
we
lack
a
strong,
generalizable
understanding
of
the
mechanisms
through
which
organic
(SOC)
is
destabilized
in
soils.
Yet
clear
destabilization
needed
to
quantify
feedbacks
cycle
Earth
system.
Destabilization
includes
occur
along
spectrum
SOC
shifts
from
‘protected’
state
an
‘available’
microbial
cells
where
it
can
be
mineralized
gaseous
forms
or
soluble
are
then
lost
These
fall
into
three
general
categories:
(1)
release
physical
occlusion
such
as
tillage,
bioturbation,
freeze-thaw
wetting-drying
cycles;
(2)
desorption
solids
colloids;
(3)
increased
metabolism.
Many
stabilize
also
destabilize
C,
gain
loss
depends
balance
between
competing
reactions.
For
example,
earthworms
may
both
aggregate
destruction,
but
create
new
aggregates
redistribute
mineral
horizon.
Similarly,
mycorrhizae
roots
form
old
priming
promoting
mining;
labile
inputs
cause
stabilization
use
efficiency
fuel
priming.
Changes
environment
affect
solubility
minerals
change
relative
surfaces
charges
SOC,
including
pH
reductive
dissolution
Fe-bearing
minerals.
By
considering
these
different
physical,
chemical,
biological
controls
contribute
destabilization,
develop
thoughtful
hypotheses
about
persistence
vulnerability
soils
make
more
accurate
robust
predictions
cycling
changing
environment.
Nature Communications,
Год журнала:
2022,
Номер
13(1)
Опубликована: Авг. 29, 2022
Permafrost
thaw
can
stimulate
microbial
decomposition
and
induce
soil
carbon
(C)
loss,
potentially
triggering
a
positive
C-climate
feedback.
However,
earlier
observations
have
concentrated
on
bulk
C
dynamics
upon
permafrost
thaw,
with
limited
evidence
involving
fractions.
Here,
we
explore
how
the
functionally
distinct
fractions,
including
particulate
mineral-associated
organic
(POC
MAOC)
as
well
iron-bound
(OC-Fe),
respond
to
using
systematic
measurements
derived
from
one
sequence
five
additional
thermokarst-impacted
sites
Tibetan
Plateau.
We
find
that
topsoil
POC
content
substantially
decreases,
while
MAOC
remains
stable
OC-Fe
accumulates
due
enriched
Fe
oxides
after
thaw.
Moreover,
proportion
of
increases
along
at
most
sites.
The
relatively
fractions
would
alleviate
weaken
its
feedback
climate
warming
over
long-term
thermokarst
development.
Processes,
Год журнала:
2023,
Номер
11(3), С. 731 - 731
Опубликована: Март 1, 2023
Composting
is
the
most
adaptable
and
fruitful
method
for
managing
biodegradable
solid
wastes;
it
a
crucial
agricultural
practice
that
contributes
to
recycling
farm
wastes.
profitable
various
plant,
animal,
synthetic
wastes,
from
residential
bins
large
corporations.
waste
management
(AWM)
practices
flourish
in
developing
countries,
especially
Pakistan.
has
advantages
over
other
AWM
practices,
such
as
landfilling
waste,
which
increases
potential
pollution
of
groundwater
by
leachate,
while
composting
reduces
water
contamination.
Furthermore,
burned,
open-dumped
on
land
surfaces,
disposed
into
bodies
water,
leading
environmental
global
warming
concerns.
Among
an
environment-friendly
cost-effective
disposal.
This
review
investigates
improved
via
conventional
emerging
processes
stages:
composting,
underlying
mechanisms,
factors
influence
discrete
crop
residue,
municipal
(MSW),
biomedical
(BMW).
Additionally,
this
describes
compares
composting.
In
conclusion,
current
trends
future
possibilities
are
summarized
reviewed.
Recent
developments
highlighted
critical
review;
recommendations
developed
aid
its
technological
growth,
recognize
advantages,
increase
research
interest
processes.