This document discusses biosignatures and the search for habitable exoplanets. It begins by reviewing Earth's biosignatures like oxygen, ozone, methane, and vegetation reflectance. It then explains that life exploits chemical energy gradients and metabolic reactions have an energy yield that can be quantified. The search for habitable worlds involves finding transiting exoplanets using ground and space telescopes to measure atmospheres. Direct imaging from space is also needed to find and characterize Earth analogs, with external occulters showing promise to block starlight. The overarching goals are to understand possible biosignatures on non-Earth worlds and find the most promising planets for atmospheric study.
5. The exoplanet atmosphere is the
only way to infer whether or not a
planet is habitable or likely inhabited
The planetary atmosphere is our
window into temperatures, habitability
indicators, and biosignature gases
6. Biosignatures and
Habitable Planets
Overview Review
Introduction: Earth’s Biosignatures
The Thermodynamics of Biosignatures
The Search for Habitable Worlds
16. Atmosphere InterpretaRon
H2O and CH4 in transmission from HST
Swain et al. (2008) See also Grillmair et al. 2008.
IdenficaRon of atoms
and molecules
Day‐night temperature
gradients
Possible variability
Advances in retrieval
techniques
See Seager and Deming
ARAA 2010
17. Overview Points
Monumental exoplanet achievements were
made despite widespread skepRcism
The huge promise for the future is based on
the achievements of the past decade+
Keep this in mind for the rest of the talk
18. Biosignatures and
Habitable Planets
Introduction: Earth’s Biosignatures
The Thermodynamics of Biosignatures
The Search for Habitable Worlds
19. Earth, Venus, Mars
1D models from Vikki Meadows Virtual Planetary Laboratory
20. Earth, Venus, Mars
1D models from Vikki Meadows Virtual Planetary Laboratory
24. The VegetaRon Biosignature
• Chlorophyll causes strong
absorpRon at wavelengths
shorter than 0.7 μm
• Light scacering in air gaps
between water‐filled plant
cells causes strong red
reflectance
• Plants absorb energy at short
wavelengths for
photosynthesis; reflect and
transmit radiaRon at long
wavelengths for thermal
balance
Seager et al. 2005
Data from Clark 1993
25. Earth Biosignature Summary
• O2 /O3 : the smoking gun
• N2O: biological but weak signature
• H2O: evidence for liquid water
• CH4: biological/abiological
• (VegetaRon red edge)
But, we are stuck in a world of terracentric biosignatures.
26. Biosignatures and
Habitable Planets
Introduction: Earth’s Biosignatures
The Thermodynamics of Biosignatures
The Search for Habitable Worlds
27. Nothing would be more tragic in the
American exploraRon of space than to
encounter alien life and fail to recognize it
NRC report 2007
28. Constraints for Life in the Universe
All Life
Liquid
water
Carbon‐based
Chemical
PotenRal
Energy
biologist
chemist
physicist
29.
30.
31. Fuels
CH2O→CO2
Redox PotenRal (V)
Oxidants
H2→H+
CO2→CH2O
H+→H2
NH4
+→N2
N2→NH4
+
CH4→CO2 CO2→CH4
H2S→ SO4
2‐
SO4
2‐→H2S
N2→ NO3
‐
NO3
‐→N2
H2O→O2 O2→H2O
Not to scale
Electron Tower
Aker Lane, Nature May 2006
33. Fuels
CH2O→CO2
Redox PotenRal (V)
Oxidants
H2→H+
CO2→CH2O
H+→H2
NH4
+→N2
N2→NH4
+
CH4→CO2 CO2→CH4
H2S→ SO4
2‐
SO4
2‐→H2S
N2→ NO3
‐
NO3
‐→N2
H2O→O2 O2→H2O
Not to scale
Electron Tower
Aker Lane, Nature May 2006
34. Biosignature Thermodynamics
• Metabolic reacRons are redox reacRons
• The Gibbs free energy is used to determine
the energy yield of a reacRon
• Recall: the Gibbs free energy is an energy
potenRal
• The energy potenRal can be converted into
volts via the Nernst equaRon.
See “Biological Thermodynamics” by D. T. Haynie.
35. Seager and Schrenk, “An Astrophysical
View of Earth‐Based Metabolism
submiced to Astrobiology,.
Supported by FQXI
O2, O3, N2O
Unique
Generated by
geology or
photochemistry
Not rapidly assimilated
H2, CO2, H2S, CH4, SO2
Not highly soluble in ocean
Gaseous metabolic byproducts
O2, H2, CO2, N2, N2O, NO, NO2, H2S, CH4, SO2, H2O, NH3
All Earth‐based metabolic byproducts
Different
atmospheres/
stellar UV could
have different
biosignatures.
36. Atmospheric escape
Photochemistry
RadiaRve transfer
Atmospheric
ComposiRon
Chemical equilibrium/disequilibrium
Atmospheric
circulaRon
Biosignatures
Clouds
ConnecRon with
observaRons
37. Biosignature Framework • For a spectral feature to
be significant, what is the
required biosignature
flux?
• This is not only a
radiaRve transfer
problem, but also related
to photochemistry
sources and sinks, and
putaRve chemistry of the
planet crust and
atmosphere
• Reality check: convert to
biomass by equaRon the
Gibbs free energy (yield)
to maintenance energy of
the organism
Seager et al. in prep. Figure from De Wit
38. Biosignature Summary
• Life uses and exploits chemical energy
gradients
• ReacRons that are energeRcally favorable but
kineRcally inhibited
• There is a quanRtaRve path forward for redox
biosignature fluxes in the context of
atmospheric radiaRve transfer and chemistry
models – gives a chance to find new
biosignatures.
39. Biosignatures and
Habitable Planets
Introduction: Earth’s Biosignatures
The Thermodynamics of Biosignatures
The Search for Habitable Worlds
40. Two‐Pronged Strategy
Prong 1: TranrsiRng planets with a focus on M dwarfs
Fast‐track
ground‐based, and exisRng space assets
Prong 2: direct imaging of F, G, K dwarfs
Requires technology investments
And new space‐based faciliRes
41. Transit Survey Telescopes
TESS concept
6 to 9 lenses on the
same plaqorm
CNES/Corot
30 cm mirror
Polar orbit
NASA/Kepler
1 m aperture
Earth‐trailing
orbit
ExoplanetSat concept
A triple CubeSat
constellaRon of
nanosats
Plato science payload
Under study by ESO
47. Cash 2006
Led by
Remi Soummer and Web Cash
Recent SPIE paper
R.A. Brown, I. Jordan, A. Roberge, T. Glassman,
A. Lo, S. Seager, L. Pueyo and others
Technical issues
70m occulter at 70,000 km
StaRonk eeping
‐not opRmized at visible
‐interesRng features near a micron
undersampling of PSF at visible
‐limits to high S/N
limited Rme
‐9% of JWST Rme, limits search to about 30 stars
48. Principle of a starshade on a separate spacecrak to block the light
from the star, while allowing the light from
an exoplanet to pass the edge of the occulter unimpeded.
Northrup Grumman
See the NASA‐sponsored studies THEIA (led by David Spergel), NWO led by Webster Cash.
See Cash 2006
49. SimulaRons for a 12‐day observing Rme for a
super Earth orbiRng a sun‐like star at 10 pc.
R = 1000 binned down to R = 200
R. Soummer et al. SPIE in prep.
Models by S. Seager
50. Search for Habitable Worlds Summary
• Transits or direct imaging will provide a
valuable handful of potenRally habitable
planets
• Vast resources in terms of telescope Rme for
transits and technology development for
space‐based direct imaging are needed
• A near‐term Terrestrial Planet Finder
possibility is the occulter + the JWST
51. A`
Summary
Biosignature goal: understand possible
metabolic byproducts and their lifeRmes
on non‐Earth‐like exoplanets NWO
TransiRng exoplanets: find them via ground‐based
or space based transit searches.
Measure spectra of transiRng super Earths
orbiRng M stars using the James Webb
Space Telescope
Direct imaging from space to find and
characterize true Earth analogs. The
external occulter is promising technology
to block out starlight of a sun‐like star to a
level of 10 billion at visible wavelengths
52.
53. seagerexoplanets.mit.edu
Exoplanet Atmospheres and Interiors
B. Benneke (Aero/Astro grad student)
M. Braunstein (EAPS grad student)
R. Hu (EAPS grad student)
M. Nikku (EAPS postdoc)
A.‐M. Piso (Physics UROP)
L. Rogers (Physics grad student)
J. De Wit SupAero masters intern
Kepler Data
Brice Demory (EAPS postdoc)
Josh Carter (Physics postdoc)
K. Berry (Physics UROP)
K. Singh (Physics UROP)
ExoplanetSat
J. Villasenor (Kavli)
G. Farmer (EAPS grad student)
C. Pong (Aero/Astro grad student)
M. Smith (Aero/Astro grad student)
M. Knapp (Aero/Astro UROP)
B. Stavely (Aero/Astro UROP)
Thank you to my students and postdocs
Supported by MIT, NASA, and FQXI