Monica M. GradyDepartment of Physical Sciences
Kensington & Chelsea Celebration of Science18th October 2014
The Chemistry of Life:and where to find it
Introduction
• Discovery of HT vent fauna in late 1970’s led to realisation that photosynthesis was not the only mechanism enabling the development of an ecosystem
• This has fuelled a search to find analogous sites beyond Earth:– Within the Solar System (satellites of other planets)– Beyond the Solar System (extrasolar planets and moons)
• Important parameters:– An appropriate energy source– A mechanism for converting energy into nutrients
Life Beyond Earth?
• Explore what we know about:– Life on Earth
• What is it?• How did it get here?• Where is it?
– Life beyond Earth• Within the Solar System• Beyond the Solar System
• Draw conclusions about the possible existence of life beyond Earth
Life on Earth• What is it?
“‘I’ll know it when I see it’ is not good enough”Carl Sagan, 1994
• So how is Life defined?– Growth, reproduction, locomotion, response,
excretion, respiration, nutrition
A Living Entity ?
A Non-Living Entity ?
Life on Earth
• ‘‘Life is a self-sustained chemical system capable of undergoing Darwinian evolution’’
G. F. Joyce, 1994–The ability to adapt and evolve
•Heredity: transfer of information
Conditions for life to arise
• Starting assumptions–laws of physics and chemistry not violated–Carbon-based
•What is so special about carbon?
Starting Materials
• Building blocks– (CO, CH4, NH3, H2O)–Role of comets
• Water• Substrate• Energy• Time• Stability
The Role of Comets• Dominantly ice • Rich in organic
compounds• Major contributor to
planetary bombardment– Delivered water and
organics to all planets– Potential for life
throughout Solar System
– Not PanspermiaNucleus of Halley’s comet (ESA)
Starting Materials
• Building blocks– (CO, CH4, NH3, H2O)–Role of comets
• Water• Substrate• Energy• Time• Stability
Water• Why is water important?
–Solvent–Support–Transport
Starting Materials
• Building blocks– (CO, CH4, NH3, H2O)–Role of comets
• Water• Substrate• Energy• Time• Stability
Stages in the Origin of Life
• Simple molecules (CO, CH4, NH3)• Complex molecules (RNA)• Template for self-replication• Membrane/boundary layer
Earth
• Has its good points– Liquid water– Magnetic Field– Atmosphere– Plate tectonics– Carbon cycle
Atmosphere & Magnetosphere
Energy Source for chemosynthesis on Earth
Hot rocks + seawater + redox reactions
Mars
• Rocky planet• Diameter about half that of
Earth• Are (or were) conditions
on Mars suitable for life to arise?– Nutrients supply?– Evidence for energy
source (heat)– Evidence for water
• Where might we find life on Mars?
Nutrient supply ?
• Mars formed from same source materials as Earth– Indigenous sources
• Mars bombarded by comets and asteroids– Endogenous sources
Mars: Water (far away)
Water (close-up)
Images from NASA
Microfossils in a martian meteorite?
D.S. McKay et al. (1996) Science
Ancient fossil life on Earth
• Microfossils’ in the Apex Chert, Western Australia (Schopf, 1983)
• Recent work has re-interpreted these structures as non-biological (Brasier group, Oxford)
• It will be challenging to detect life on Mars!
Where should we look for life on Mars?Below the surface, within rocks
1 cm
Europa• Second Galilean satellite• Very high albedo
• Covered in ice
• Magnetometer measurements imply sub-surface liquid• Not plate tectonics, but gravitational energy
Images: Copyright NASA
Same might also apply to Enceladus
Images: Copyright ESA/NASA
Ocean floorEuropan fauna ?
Images: NOOA/NOC/
Titan• Largest satellite of Saturn• Very thick atmosphere (N2, CH4)• Surface oceans (NH3, CH4, C2H6, )• Surface temp. -200°C, but can be raised during impact• Possible redox reaction: H2 + C2H2 CH4 ∆E ~ 334 kJmol-1 McKay & Smith, 2005• Compared with ∆E ~ 42 kJmol-1 for methanogens (Kral et al., 1999)
Images: Copyright ESA
Life beyond the Solar System
• Where to start looking?–Habitable zone
• What to look for?–Planet–Moon
Where to start looking ?
Habitable zone concept:UniverseGalacticPlanetary
Images: Copyright NASA-ESA-ESO
What to look for ?• Extra-solar planets
– ~ 1000 found so far– Mostly ‘hot Jupiters’
• Search for Earth-like planets orbiting solar-type stars• Search for Earth-like moons orbiting giant planets
Data from www.exoplanet.eu
Exoplanets and ExoMoons
Kipping et al. (2014) MNRAS (submitted)
Image: Copyright NASA
Now able to detect and characterise exoplanetary atmospheresMainly hot silicate dust, reducing
Search for an atmosphere
Would Earth have been recognised as a potential host of life ~ 2 byr ago?
• Methane (Swain et al., 2008. Nature 452, 329 – 331)• Water vapour (Tinetti et al. Nature 448, 169-171)
EvolutionSelection in a competitive environment• Starting point
– Physics, chemistry, ingredients• Environmental stress
– Atmosphere– Magnetic field– Tectonic structure
• Chance– Asteroid impact
Lead to different evolutionary pathways
Different Evolutionary Pathways ?
CH
NO
P
S
Evolution
Summary
• Have we found evidence for extant life beyond Earth?– No
• Have we found evidence for extinct life beyond Earth?– No
• Have we found evidence for habitats where life might exist beyond Earth?
–Yes