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Biosignatures and the Search for 
“All Roads 
Lead to TPF/ 
Darwin” 
Habitable Worlds 
Sara Seager 
MIT
Why Astrobiology
 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
Biosignatures and 
Habitable Planets 
Overview Review 
Introduction: Earth’s Biosignatures 
The Thermodynamics of Biosignatures 
The Search for Habitable Worlds
Known Planets 1995 
Based on data compiled by J. Schneider
Known Planets 1996 
Based on data compiled by J. Schneider
Known Planets 2000 
Based on data compiled by J. Schneider
Known Planets 2005 
Based on data compiled by J. Schneider
Known Planets 2010 
Based on data compiled by J. Schneider
Planets 2000
Planets 2005
Planets June 14 2010
Planet Candidates June 15 2010 
Kepler Planet 
Candidates 
announced June 
15, 2010
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
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
Biosignatures and 
Habitable Planets 
Introduction: Earth’s Biosignatures 
The Thermodynamics of Biosignatures 
The Search for Habitable Worlds
Earth, Venus, Mars 
1D models from Vikki Meadows Virtual Planetary Laboratory
Earth, Venus, Mars 
1D models from Vikki Meadows Virtual Planetary Laboratory
Earth’s Spectrum 
Turnbull et al. 2007 
Pearl and Christensen 1997
VegetaRon as a Surface Biomarker 
S. Seager 
InsRtute for Advanced Study, Princeton, July 2002
VegetaRon as a Surface Biomarker 
S. Seager 
S. Seager
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
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.
Biosignatures and 
Habitable Planets 
Introduction: Earth’s Biosignatures 
The Thermodynamics of Biosignatures 
The Search for Habitable Worlds
Nothing would be more tragic in the 
American exploraRon of space than to 
encounter alien life and fail to recognize it 
NRC report 2007
Constraints for Life in the Universe 
All Life 
Liquid 
water 
Carbon‐based 
Chemical 
PotenRal 
Energy 
biologist 
chemist 
physicist
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
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
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
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.
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.
Atmospheric escape 
Photochemistry 
RadiaRve transfer 
Atmospheric 
ComposiRon 
Chemical equilibrium/disequilibrium 
Atmospheric 
circulaRon 
Biosignatures 
Clouds 
ConnecRon with 
observaRons
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
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.
Biosignatures and 
Habitable Planets 
Introduction: Earth’s Biosignatures 
The Thermodynamics of Biosignatures 
The Search for Habitable Worlds
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
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
All roads lead to … 
Terrestrial Planet Finder/Darwin
Direct Imaging 
A5V 
40 pc 
Planets at: 24, 
38, and 60 AU 
Planet‐star 
contrast 104 or 
105 
Marois, MacIntosh, Doyon et al. 2008
Direct Imaging Telescope 
Diffracted light problem
Direct Imaging Telescope 
Diffracted 
light 
soluRons 
… require a 
near perfect 
telescope
Cash 2006
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
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
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
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
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
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

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Sara Seager - Lecture3 - MIT

  • 1. Biosignatures and the Search for “All Roads Lead to TPF/ Darwin” Habitable Worlds Sara Seager MIT
  • 2.
  • 3.
  • 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
  • 7. Known Planets 1995 Based on data compiled by J. Schneider
  • 8. Known Planets 1996 Based on data compiled by J. Schneider
  • 9. Known Planets 2000 Based on data compiled by J. Schneider
  • 10. Known Planets 2005 Based on data compiled by J. Schneider
  • 11. Known Planets 2010 Based on data compiled by J. Schneider
  • 15. Planet Candidates June 15 2010 Kepler Planet Candidates announced June 15, 2010
  • 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
  • 21. Earth’s Spectrum Turnbull et al. 2007 Pearl and Christensen 1997
  • 22. VegetaRon as a Surface Biomarker S. Seager InsRtute for Advanced Study, Princeton, July 2002
  • 23. VegetaRon as a Surface Biomarker S. Seager S. Seager
  • 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
  • 32. 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
  • 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
  • 42. All roads lead to … Terrestrial Planet Finder/Darwin
  • 43. Direct Imaging A5V 40 pc Planets at: 24, 38, and 60 AU Planet‐star contrast 104 or 105 Marois, MacIntosh, Doyon et al. 2008
  • 44. Direct Imaging Telescope Diffracted light problem
  • 45. Direct Imaging Telescope Diffracted light soluRons … require a near perfect telescope
  • 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