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Click
here for larger image.
Figure ES.1 HST image of
NGC 3603 showing the life cycle of material
(including carbon) in a star-forming
region.A cycle of stellar birth and death leads
to the synthesis and evolution of organic compounds.
Carbonaceous material ejected from dying stars
enters the diffuse medium and then is cycled
into dense clouds.
The collapse of a dense cloud forms an evolved
stellar system (see the Frontispiece for more
detail) where
these organic compounds can be delivered intact
to planetary surfaces and mixed with those
produced
endogenously. As the lifetime of the evolved
system comes to a close, stellar mass loss
recycles material to
begin the process anew.
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Planetary Systems form by collapse of
dense inter-stellar cloud cores (Frontispiece). Some
stages in this evolution can be directly observed when
stellar nurseries are imaged (Figure ES.1), while other
stages remain cloaked behind an impenetrable veil
of dust and gas. Yet to understand the origin of life
on Earth, we must first develop a comprehensive understanding
of the formation of our own planetary system.
Dense
cloud cores are very cold (10-50 K), and their dust
grains are coated with ices comprised of water and
organic compounds.Many of these organics have potential
relevance to the origin or early evolution of life,if
delivered to planets.
The survival of these organics
through the violent birth-phase of a star is less
certain. Properties of the young star (its mass, spectral
energy distribution, whether it formed in isolation
or as a multiple star,
etc.)play a key role in controlling the evolution
of organic material in the proto-planetary disk.
The location
within the disk is important since the nature and
effectiveness of such processing depends strongly
on distance from
the young star, on distance above the nebular mid-plane,and
on time. The ultimate delivery of these primitive
organics to young planets and their moons also evolves
with
time, as the bodies grow in size and as the nebula
clears.
We propose to investigate the origin
and evolution of organic compounds in planetary systems,
and their delivery to young planets.
The proposed research
addresses the heart of Goal 3 of the Astrobiology
Roadmap:
Understand how life emerges from cosmic and planetary
precursors.
The central question is this: Did delivery
of exogenous organics and water
enable the emergence and evolution of life?
The investigation is divided into four
Themes:
Theme 1: Establish the
taxonomy of icy planetesimals and their potential
for delivering pre-biotic organics and water to the
young Earth and other planets.
Theme 2: Investigate processes
affecting the origin and evolution of organics in planetary
systems.
Theme 3: Conduct laboratory simulations
of processes that likely affected the chemistry of
material in natal interstellar cloud cores and in proto-planetary
disks.
Theme 4: Develop advanced methods
for the in-situ analysis of complex organics in small
bodies in the Solar System.
We seek to better understand the
organic compounds generated and destroyed in the
interstellar and proto-planetary environments, through
observational, theoretical, and laboratory work. We
will examine the potential for and limitations to delivery
of exogenous pre-biotic organics to planets, examining
factors that enhance or restrict this potential.
We will, for the first time, investigate
the effect of astrophysical X-rays on the evolution
of exogenous organics in proto-stellar disks. We will
follow these factors over time, from the natal cloud
core through the end of the late heavy bombardment
(~4.1 Ga). We will evaluate the possible role of exogenous
organic material in terrestrial biogenesis.
The proposed
research will significantly improve our understanding
of the nature of organics in other planetary
systems, the processes affecting them, and the potential
for delivering pre-biotic organic compounds to planets.
The
Management Plan: An Integrated Research Approach
The
proposed research is interdisciplinary and it involves
researchers at multiple institutions. This is both
an intellectual asset and an organizational challenge.
The effectiveness of a Team is demonstrated when its
total
output exceeds the sum of its
individual parts. We have developed a management strategy
that we believe will enable this objective.
Internal
collaboration will be enhanced by bridging post-doctoral
associates and students across projects within a Theme.
Theme-Based “Expeditions” will
be mounted to ensure that our students receive hands-on
experience in techniques used in all Themes.
Students and post-docs will be encouraged to explore other
aspects of Astrobiology at luncheons every two weeks.
An Executive Scientist will ensure smooth operations of the
Node, and timely reporting to NAI Central and to NASA Headquarters.
An Executive Committee will review the scientific progress
and activities, monthly. An independent Board of Visitors will assess progress
on an annual basis.
An Education and Public Outreach
Lead will ensure that our E/PO plan is smoothly executed.
Education
and Public Outreach
GSFC and the Minority Institute
Astrobiology Collaborative (MIAC)will implement a multifaceted
program based on Astrochemistry and focused on organics
in the solar system. We will develop curriculum materials,
conduct teacher professional de-
velopment workshops,and bring observational cometary
research into middle and high school classrooms.
We will support MIAC institutions in the professional
development of K-12 educators in under-served communities
and build upon existing MIAC, GSFC and UMCP (Deep
Impact
EPO) programs and educator networks.
Principal Objectives
Theme 1: Organics
in Icy Planetesimals: A Key Window on the Early
Solar System
A. Comet taxonomy via specific molecules
and isotopes
1. Measure abundances of parent volatiles
2. Measure the ratio HDO/H2O
3. Measure abundances of chemically related molecules
B. Perform
detailed theoretical studies of the molecular chemistry
of proto-stellar disks
1. Model infall for specific
chemical changes in the major volatile components
2. Determine how trace cometary organics can also
be formed at the accretion shock
3. Model interstellar deuterium fractionation
as ISM material incorporates into the nebula
C. Model
dynamical transport of icy planetesimals in the
early Solar System
1. Model organic flux into Oort
cloud, terrestrial region, and out of the Solar
System
2. Model 1 including giant planet migration
3. Model 2 including the formation of Uranus
and Neptune
4. Simulate the growth of grains followed
by settling to the mid-plane
D. Determine
isotopic compositions and abundances in Lunar breccias
1. Determine
the signature(s) of highly siderophilic abundances
in Lunar breccias
2. Connect signature(s) to materials exposed
to early Solar System processes
3. Determine if the composition of the
late influx changed with time
4. Connect siderophilic impactors with
those of organic-rich chondrites
Theme 2: From
Molecular Cores to Planets: Our Interstellar Heritage
A. Study
the evolution of material in molecular clouds
1. Map
chemical abundances to determine the physical
conditions within a
molecular cloud
2. Search for new interstellar organic
molecules
B. Determine the initial
conditions for planet formation
1. Understand the
growth of grains prior to and during incorporation
in the
disk
2. Observe grain growth and
document opacity loss as
material gets
incorporated mm
scale bodies
3. Determine the relationship
between cometary and interstellar
chemistry
C. Connect the X-rays
and UV from young stars to formation
and
destruction of organics
1. Compare
abundances of organics around young stars with
models and lab simulations
2. Measure the emission
and ionization state
of molecules
near young
stars
3. Measure changes in the
chemical abundances as
a consequence
of strong X-ray and
UV flaring
D. Search for
organic signatures in the IR spectra of transiting
extra-solar
gas-giant planets
Theme
3: Organic Material from Laboratory
Simulations of Astrophysical
Environment
A. Analyze
complex organics in
grain-catalyzed
reactions
1. Investigate
organics in hydration and thermal
metamorphism
ala
various meteorite
types
2. Compare results
with astronomical
observations, meteorites,
and Earth-return samples
B.
Analyze complex organics in UV, X-ray, electron,
and proton processed
ices
1. Follow formation
and destruction
of selected
organic compounds
in detail
2. Look for the
formation of
particularly
interesting
biological
molecules
3. Compare results
with astronomical
observations,
meteorites, and Earth-return
samples
C. Analyze
more complex simulations
1. Combine materials
and techniques
of 3A and
3B
2. Investigate
organics in
residues in
various aqueous
environments
3. Follow the
reactions of
residues mixed
with grains
4. Follow the
reactions of
residues induced
by additional
ion or
photon processing
Theme
4: Advanced Analysis of
Primitive
Material
A. Determine
how to
measure the
history
and the
chemical state
of organics
in situ
1.
Evaluate a number
of possible
chromatographic
mass
spectral techniques
2. Compare
bulk
pyrolysis
and
laser
and ion
beam
volatilization
for
this
evaluation
(4A.1)
B.
Evaluate, minimize, and manage
thermal
perturbations
to Earth-return
samples
1. Determine
how
to preserve
the
structure
and
isotopic composition
of
relevant organics
2. Optimize
method
to
determine
the
original
composition
of
compounds
before
heating
C. Utilize
lab
analogs
to
develop
and
calibrate
instruments
See Team Research Plan |