life. start with the early earth… hot ~ 230 c oceans (at about 4.2 by) co 2 atmosphere with...
TRANSCRIPT
Life
Start with the Early Earth…
• Hot ~ 230C• Oceans (at about 4.2 By)
• CO2 atmosphere with ammonia, methane, water vapor, and nitrogen
• Lots of UV-radiation (no ozone)
• Reducing conditions
• Lots of lightning
Miller-Urey Experiment• Idea was that conditions
on the primitive Earth could produce chemical reactions that made organic compounds from inorganic material.
• Used water (H2O), methane (CH4), ammonia (NH3), and hydrogen (H2)
• Made up to 22 different amino acids
• After a week about 10–15% of the carbon within the system was now in the form of organic compounds
So we have organics….• Turns out that there are
lots of other possible origins for organics molecules– Deep sea vents– Spontaneous formation of
peptides– Radioactive beaches– And many, many more…
• Now you need to make cells….
• There are, of course, piles of theories on the origin of cells– Clays– Lipids– Polyphosphates– PAHs
PAHs: Self Organizing Building Blocks?
• Polycyclic Aromatic Hydrocarbons (PAHs) are amphiphilic (they have parts that are both hydrophilic and hydrophobic).
• In solution, they tend to self organize themselves in stacks, with the hydrophobic parts protected.
• In this self ordering stack, the separation between rings is 0.34 nm, the same separation found in RNA and DNA.
• Smaller molecules will naturally attach themselves to the PAH rings.
However it happened…• We think prokaryote cells
(single-cell organisms that lack a nucleus) developed as early as ~ 3.85 Billion years ago
• WE KNOW that by 3.5 Billion years ago we had bacteria and blue-green algae
• By 2 Billion years ago we had eukaryotes (organism whose cells have a nucleus)
• By 1 Billion years ago we had multicellular life
• By 600 million years ago we had simple animals
By 2.5 Billion years ago plankton were altering the oxygen content of the atmosphere
What are the requirements for Life• Liquid Water
– Too close….water boils off– Too far….water freezes
• A source of Energy– Solar– Tidal
• Available Organic Molecules– Carbon Compounds….abundant in comets and
some asteroids
• Enough Time – A stable environment– Evolve Complexity
• This comes together in the concept of a Habitable Zone
But there are a few other things…
•Stable Sun•Near-circular planetary orbits•Earth-like planetary mass•Night and Day•No major orbital disruptions•Occasional mass extinctions
are OK–But not too often….
Galactic Habitable Zones• It is all about stability• If it takes stability for over 4
billion years to develop intelligent life, you need to be in the Galactic suburbs
• Stay away from– Black holes– High star density areas (comets)– Star forming regions– Supernova
• For a start, stay away from the Galactic center
Metallicity• No planets have been found around stars
with less than 40% of the Sun’s metal ratio• Too high metallicity is also a problem (we
think…..)– Tend to larger, more volatile-rich, lower-relief– Water-covered– Easier to form gas-giants…could be bad for
terrestrial Planets
• Metallicity increases steadily toward the Galactic center– More matter, faster star formation
Co-rotation• Another thing to
avoid is transiting spiral arms
• These are areas of high stellar density and high star formation– Increases probability
of close gravitational encounters
– Or being to close to Supernova
• Our Sun’s galactic orbital period is about the same as rotation period the nearby spiral arm
The Drake Equation
•R*Fp*Ne*Fl*Fi*Fc*L = N – R = The number of suitable stars, effectively F, G, and K stars,
that form in our galaxy per year (about 1)
– Fp= The fraction of these stars that have planets (about 0.5)
– Ne = The number of Earth-like planets (planets with liquid water) within each planetary system (we are learning about this now…..expect an answer in 3-5 years)
– Fl = The fraction of Earth-like planets where life develops (we could have some idea in 20 years)
– Fi = The fraction of life sites where intelligent life develops (how are we ever going to know this?)
– Fc = The fraction of intelligent life sites where communication develops (one would do….)
– L = "The "lifetime" (in years) of a communicative civilization (how long have we been a communicative civilization?)
– N = The number of communicative civilizations within the Milky Way today
The Drake Equation
• R*Fp*Ne*Fl*Fi*Fc*L = N
• Drake thinks that N is about 10,000 for our Galaxy.
• I really doubt that…..–Throw into the equation the limitations
of metallicity, local star density, near-by supernova, and binary systems
• But a few would not be unreasonable
How can we tell if there is life?• Look at the
atmosphere….• Life uses the
atmosphere as a source of energy and a sink for waste products.
• We should know about nearby systems in ~20 years
But we haven’t we found any communicative civilizations
• Well….….there may be nothing to find.• Think about it…..how would an
advanced civilization communicate?– How long has it been since Marconi
invented radio?– Transatlantic commercial service was
established in 1907
Big Questions…
• Is there life elsewhere in our solar system?–There is no evidence
• Is there intelligent life elsewhere in the Universe?–There is no evidence