Global Change Biology,
Journal Year:
2024,
Volume and Issue:
30(5)
Published: May 1, 2024
Abstract
With
over
one‐third
of
terrestrial
net
primary
productivity
transferring
to
the
litter
layer
annually,
carbon
release
from
serves
as
a
crucial
valve
in
atmospheric
dioxide
concentrations.
However,
few
quantitative
global
projections
rate
response
climate
change
exist.
Here,
we
combined
foliar
dataset
(8973
samples)
generate
spatially
explicitly
estimates
their
residence
time
(
τ
)
change.
Results
show
mean
()
0.69
year
−1
(ranging
0.09–5.6
).
Under
future
scenarios,
is
projected
decrease
by
2.7%
(SSP
1–2.6)
and
5.9%
5–8.5)
during
2071–2100
period.
Locally,
alleviation
temperature
moisture
restrictions
corresponded
obvious
decreases
cold
arid
regions,
respectively.
In
contract,
tropical
humid
broadleaf
forests
increased
4.6%
under
SSP
5–8.5.
Our
findings
highlight
vegetation
type
powerful
proxy
for
explaining
patterns
rates
role
conditions
predicting
responses
observation‐based
could
refine
cycle
parameterization,
improving
cycle–climate
feedbacks.
The Science of The Total Environment,
Journal Year:
2021,
Volume and Issue:
771, P. 145452 - 145452
Published: Jan. 28, 2021
The
Tea
Bag
Index
(TBI)
method
was
used
to
estimate
the
litter
decomposition
rate
in
peatland
exposed
for
climate
manipulation
(increased
temperature
and
reduced
precipitation)
at
two
contrasting
sites
differing
water
table
depth
(WTD)
dynamics.
To
manipulate
on
peatland,
prototyped
Open
Top
Chambers
(OTC)
automated
rain-out
shelters
were
used.
OTCs
increased
daytime
air
temperatures
by
~1.7
°C
driest
plots
an
increase
of
precipitation,
while
average
daily
lower
than
0.9
°C.
However,
cooled
down
peat
even
0.8
this
effect
most
pronounced
rather
night-time
conditions.
precipitation
amount
26%.
tea
bags
buried
8
cm
83
172
days
starting
from
19th
April
2019.
Our
observation
proved
that
although
rates
dependent
temperature,
WTD
its
fluctuations
are
main
factors
controlling
waterlogged
ecosystems
like
ours.
At
Sphagnum-dominated
peatlands,
interrelation
between
different
environmental
may
mitigate
impact
warming
decomposition.
Scientific Reports,
Journal Year:
2022,
Volume and Issue:
12(1)
Published: May 6, 2022
Microbial
life
in
soil
is
fueled
by
dissolved
organic
matter
(DOM)
that
leaches
from
the
litter
layer.
It
well
known
decomposer
communities
adapt
to
available
source,
but
it
remains
unclear
if
they
functionally
compete
or
synergistically
address
different
types.
Therefore,
we
decomposed
beech,
oak,
pine
and
grass
two
geologically
distinct
sites
a
lab-scale
decomposition
experiment.
We
performed
correlative
network
analysis
on
results
of
direct
infusion
HR-MS
DOM
cross-validated
functional
predictions
16S
rRNA
gene
amplicon
sequencing
with
metaproteomic
analyses.
Here
show
many
functions
are
redundantly
distributed
within
their
relative
expression
rapidly
optimized
litter-specific
properties.
However,
community
changes
likely
forced
antagonistic
mechanisms
as
identified
several
natural
antibiotics
DOM.
As
consequence,
specializing
towards
source
state
(community
divergence)
showing
similar
metabolomes
(metabolome
convergence).
Our
multi-omics-based
highlight
not
only
fuels
microbial
life,
additionally
holds
meta-metabolomic
information
functioning
ecosystems.
Soil Biology and Biochemistry,
Journal Year:
2023,
Volume and Issue:
178, P. 108959 - 108959
Published: Jan. 17, 2023
Pyrogenic
organic
matter
(PyOM)
is
a
product
of
incomplete
combustion
during
wildfires
and
an
important
pool
soil
carbon
(SOC).
The
dynamics
PyOM
SOC
in
boreal
permafrost-affected
soils
are
largely
unknown,
while
storing
large
amounts
global
being
vulnerable
to
climate
change.
Here,
we
traced
the
vertical
mobility,
allocation
fractions
decomposition
losses
highly
13C-labeled
its
precursor
ryegrass
(grass
OM)
after
two
years
in-situ
incubation
cores
installed
upper
10
cm
continuous
(northern
sites)
discontinuous
sporadic
(southern
forest
Northern
Canada.
At
northern
sites,
up
three
times
more
was
lost
by
(39%
initial)
compared
southern
sites
(11%
initial).
Losses
grass
OM
were
substantial
(69–84%
larger
soils.
incorporation
limited
>90%
recovered
found
at
applied
depth
(0–3
cm).
strongly
interacted
with
mineral
surfaces,
as
indicated
around
40%
mineral-associated
heavy
density
(<63
μm).
Microscale
analyses
SEM
NanoSIMS
showed
that
mainly
allocated
towards
fine
fraction
particulate
aggregated
form,
highlighting
importance
abiotic
processes
for
enhanced
surfaces
well
increased
distribution
microscale
initial
decomposition,
it
remained
Our
results
highlight
sensitive
fresh
inputs
losses.
Especially
persistence
depended
on
site
specific
properties
not
solely
physico-chemical
persistence.
responses
decoupled
non-pyrolyzed
require
better
understanding
evaluate
feedbacks
high-latitude
warming
associated
shifts
vegetation
wildfire
regimes.
Global Change Biology,
Journal Year:
2024,
Volume and Issue:
30(5)
Published: May 1, 2024
Abstract
With
over
one‐third
of
terrestrial
net
primary
productivity
transferring
to
the
litter
layer
annually,
carbon
release
from
serves
as
a
crucial
valve
in
atmospheric
dioxide
concentrations.
However,
few
quantitative
global
projections
rate
response
climate
change
exist.
Here,
we
combined
foliar
dataset
(8973
samples)
generate
spatially
explicitly
estimates
their
residence
time
(
τ
)
change.
Results
show
mean
()
0.69
year
−1
(ranging
0.09–5.6
).
Under
future
scenarios,
is
projected
decrease
by
2.7%
(SSP
1–2.6)
and
5.9%
5–8.5)
during
2071–2100
period.
Locally,
alleviation
temperature
moisture
restrictions
corresponded
obvious
decreases
cold
arid
regions,
respectively.
In
contract,
tropical
humid
broadleaf
forests
increased
4.6%
under
SSP
5–8.5.
Our
findings
highlight
vegetation
type
powerful
proxy
for
explaining
patterns
rates
role
conditions
predicting
responses
observation‐based
could
refine
cycle
parameterization,
improving
cycle–climate
feedbacks.