Water,
Journal Year:
2024,
Volume and Issue:
17(1), P. 71 - 71
Published: Dec. 31, 2024
This
study
investigates
water–rock
interactions
of
Taiwan
hot
springs
by
analyzing
rare
earth
elements
(REEs)
concentrations
and
strontium
(Sr)
isotopes.
REEs
were
separated
from
samples
using
RE
resin,
their
measured
HR-ICPMS.
Strontium
was
isolated
SrSPEC
the
isotopic
ratio
determined
MC-ICPMS.
The
ΣREE
in
ranges
3.17
ng/L
to
29.7
µg/L,
with
highest
levels
found
Tatun
Volcano
Group,
followed
sedimentary
metamorphic
regions.
primary
factors
controlling
REE
compositions
are
lithology
pH.
patterns
can
be
categorized
into
five
types,
indicating
that
affected
various
mechanisms.
most
distinct
spring
Volcano,
Ginshan,
Kuantzuling.
87Sr/86Sr
ratios
range
0.70468
0.71730,
radiogenic
originating
regions,
reflecting
nature
parent
rock
interacting
water.
Seawater
intrusion
preferential
weathering
carbonate
also
have
minor
effects
on
Sr
isotope
composition.
findings
indicate
types
surrounding
rocks
pH
values
significantly
influence
Taiwan’s
springs.
Microorganisms,
Journal Year:
2025,
Volume and Issue:
13(4), P. 887 - 887
Published: April 12, 2025
Nitric
oxide
(NO)
is
a
widely
recognized
signaling
molecule
found
across
various
organisms,
yet
its
specific
effects
on
fungal
growth
and
development
under
anaerobic
conditions
remain
underexplored.
This
study
investigates
how
NO
influences
the
of
Schizophyllum
commune
20R-7-F01
environments.
The
results
demonstrated
an
increase
in
endogenous
levels
during
mycelial
basidiospore
germination.
addition
cPTIO,
scavenger,
inhibited
growth,
delayed
germination,
reduced
expression
genes
involved
highlighting
critical
role
development.
On
other
hand,
exogenous
supplementation
accelerated
facilitated
formation
primordia,
suggesting
NO’s
potential
as
key
regulator
These
findings
deepen
our
understanding
contribution
to
offer
new
perspectives
S.
communities,
shedding
light
metabolic
regulation
microorganisms.
Water,
Journal Year:
2024,
Volume and Issue:
17(1), P. 71 - 71
Published: Dec. 31, 2024
This
study
investigates
water–rock
interactions
of
Taiwan
hot
springs
by
analyzing
rare
earth
elements
(REEs)
concentrations
and
strontium
(Sr)
isotopes.
REEs
were
separated
from
samples
using
RE
resin,
their
measured
HR-ICPMS.
Strontium
was
isolated
SrSPEC
the
isotopic
ratio
determined
MC-ICPMS.
The
ΣREE
in
ranges
3.17
ng/L
to
29.7
µg/L,
with
highest
levels
found
Tatun
Volcano
Group,
followed
sedimentary
metamorphic
regions.
primary
factors
controlling
REE
compositions
are
lithology
pH.
patterns
can
be
categorized
into
five
types,
indicating
that
affected
various
mechanisms.
most
distinct
spring
Volcano,
Ginshan,
Kuantzuling.
87Sr/86Sr
ratios
range
0.70468
0.71730,
radiogenic
originating
regions,
reflecting
nature
parent
rock
interacting
water.
Seawater
intrusion
preferential
weathering
carbonate
also
have
minor
effects
on
Sr
isotope
composition.
findings
indicate
types
surrounding
rocks
pH
values
significantly
influence
Taiwan’s
springs.