Venus
today
is
inhospitable
at
the
surface,
its
average
temperature
of
750
K
being
incompatible
to
existence
life
as
we
know
it.
However,
potential
for
past
surface
habitability
and
upper
atmosphere
(cloud)
present
day
hotly
debated,
ongoing
discussion
regarding
a
possible
phosphine
signature
coming
from
clouds
shows.
We
review
current
understanding
about
evolution
with
special
attention
scenarios
where
planet
may
have
been
capable
hosting
microbial
life.
compare
possibility
on
case
Earth
by
reviewing
various
hypotheses
put
forth
concerning
origin
habitable
conditions
emergence
plate
tectonics
both
planets.
Life
emerged
during
Hadean
when
was
dominated
higher
mantle
temperatures
(by
200$^\circ$C),
an
uncertain
tectonic
regime
that
likely
included
squishy
lid/plume-lid
tectonics,
proto
continents.
Despite
lack
well-preserved
crust
dating
Hadean-Paleoarchean
eons,
attempt
resume
environmental
this
critical
period
based
zircon
crystals
geochemical
signatures
period,
well
studies
younger,
relatively
rocks
Paleoarchean.
For
these
early,
primitive
forms,
not
but
it
became
important
means
nutrient
recycling,
consequences
global
environment
long-term,
essential
continuation
early
Venus,
question
stable
water
closely
related
tectonics.
discuss
transitions
between
stagnant
lid
(episodic)
crustal
volatile
cycling
Venus’
interior
atmosphere.
In
particular,
insights
into
climate
examine
questions
rotation
speed,
reflective
clouds,
silicate
weathering,
summarize
implications
long-term
habitability.
Finally,
state
knowledge
venusian
proposed
detection
covered.
Contemporary Physics,
Год журнала:
2022,
Номер
63(3), С. 180 - 199
Опубликована: Июль 3, 2022
The
search
for
life
elsewhere
in
the
universe
is
one
of
central
aims
science
twent-first
century.
While
most
this
work
aimed
at
planets
orbiting
other
stars,
our
own
Solar
System
an
important
part
endeavour.
Venus
often
thought
to
have
too
harsh
environment
life,
but
it
may
been
a
more
hospitable
place
distant
past.
If
evolved
there
past
then
cloud
decks
are
only
remaining
niche
where
as
we
know
might
survive
today.
discovery
molecule
phosphine,
PH3,
these
clouds
has
reinvigorated
research
looking
into
possibility
clouds.
In
review
examine
background
studies
on
Venus,
discuss
conflicting
and
confirming
observations
analyses,
look
forward
future
space
missions
that
will
hopefully
provide
definitive
answers
origin
phosphine
question
whether
exist
there.
Aerospace,
Год журнала:
2022,
Номер
9(10), С. 597 - 597
Опубликована: Окт. 13, 2022
Exploring
how
life
is
distributed
in
the
universe
an
extraordinary
interdisciplinary
challenge,
but
increasingly
subject
to
testable
hypotheses.
Biology
has
emerged
and
flourished
on
at
least
one
planet,
that
renders
search
for
elsewhere
a
scientific
question.
We
cannot
hope
travel
exoplanets
pursuit
of
other
even
if
we
identify
convincing
biosignatures,
do
have
direct
access
planets
moons
our
solar
system.
It
therefore
matter
deep
astrobiological
interest
study
their
histories
environments,
whether
or
not
they
harbor
life,
better
understand
constraints
delimit
emergence
persistence
biology
any
context.
In
this
perspective,
argue
targeted
chemistry-
biology-inspired
experiments
are
informative
development
instruments
space
missions,
essential
interpreting
data
generate.
This
approach
especially
useful
studying
Venus
because
it
were
exoplanet
would
categorize
as
Earth-like
based
its
mass
orbital
distance,
atmosphere
surface
decidedly
Earth-like.
Here,
present
general
justification
exploring
system
from
destinations
may
life.
introduce
extreme
environments
Venus,
rigorous
observation-driven
can
guide
instrument
imminent
missions
Venusian
clouds.
highlight
several
specific
examples,
including
organic
chemistry
under
conditions,
harnessing
fluorescent
properties
molecules
make
variety
otherwise
challenging
measurements.
Astrobiology,
Год журнала:
2024,
Номер
24(4), С. 407 - 422
Опубликована: Апрель 1, 2024
Recent
ground-based
observations
of
Venus
have
detected
a
single
spectral
feature
consistent
with
phosphine
(PH3)
in
the
middle
atmosphere,
gas
which
has
been
suggested
as
biosignature
on
rocky
planets.
The
presence
PH3
oxidized
atmosphere
not
yet
explained
by
any
abiotic
process.
However,
state-of-the-art
experimental
and
theoretical
research
published
previous
works
demonstrated
photochemical
origin
another
potential
biosignature—the
hydride
methane—from
carbon
dioxide
over
acidic
mineral
surfaces
Mars.
production
methane
includes
formation
HC
·
O
radical.
Our
density
functional
theory
(DFT)
calculations
predict
an
energetically
plausible
reaction
network
leading
to
PH3,
involving
either
or
H·
radicals.
We
suggest
that,
similarly
minerals
already
discussed
for
Mars,
Venus'
could
be
radical
chemistry
starting
·PO
HC·O,
latter
being
produced
reduction
CO2
dust
upper
atmospheric
layers
ultraviolet
radiation.
HPO,
H2P·O,
H3P·OH
identified
key
intermediate
species
our
model
pathway
synthesis.
Venus
today
is
inhospitable
at
the
surface,
its
average
temperature
of
750
K
being
incompatible
to
existence
life
as
we
know
it.
However,
potential
for
past
surface
habitability
and
upper
atmosphere
(cloud)
present
day
hotly
debated,
ongoing
discussion
regarding
a
possible
phosphine
signature
coming
from
clouds
shows.
We
review
current
understanding
about
evolution
with
special
attention
scenarios
where
planet
may
have
been
capable
hosting
microbial
life.
compare
possibility
on
case
Earth
by
reviewing
various
hypotheses
put
forth
concerning
origin
habitable
conditions
emergence
plate
tectonics
both
planets.
Life
emerged
during
Hadean
when
was
dominated
higher
mantle
temperatures
(by
200$^\circ$C),
an
uncertain
tectonic
regime
that
likely
included
squishy
lid/plume-lid
tectonics,
proto
continents.
Despite
lack
well-preserved
crust
dating
Hadean-Paleoarchean
eons,
attempt
resume
environmental
this
critical
period
based
zircon
crystals
geochemical
signatures
period,
well
studies
younger,
relatively
rocks
Paleoarchean.
For
these
early,
primitive
forms,
not
but
it
became
important
means
nutrient
recycling,
consequences
global
environment
long-term,
essential
continuation
early
Venus,
question
stable
water
closely
related
tectonics.
discuss
transitions
between
stagnant
lid
(episodic)
crustal
volatile
cycling
Venus’
interior
atmosphere.
In
particular,
insights
into
climate
examine
questions
rotation
speed,
reflective
clouds,
silicate
weathering,
summarize
implications
long-term
habitability.
Finally,
state
knowledge
venusian
proposed
detection
covered.