1 / 25

ASTR-3040: Astrobiology

ASTR-3040: Astrobiology. The Habitability of Earth. Day 5. Homework. Due Tue. Feb. 8 Chapter 4: 3, 9, 18 21, 27, 32 37, 42, 46 49, 50, 54. Chapter - 4. Geology & Life Earth is unique within our solar system Moderate Temperatures (slight greenhouse effect) ‏ Abundant water

Download Presentation

ASTR-3040: Astrobiology

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. ASTR-3040: Astrobiology The Habitability of Earth Day 5

  2. Homework • Due Tue. Feb. 8 • Chapter 4: • 3, 9, 18 • 21, 27, 32 • 37, 42, 46 • 49, 50, 54

  3. Chapter - 4 • Geology & Life • Earth is unique within our solar system • Moderate Temperatures (slight greenhouse effect)‏ • Abundant water • Protective atmosphere • Relatively stable environment • Contrast Moon, Mercury, Venus, Mars (Fig 4.1)‏ • Distance from Sun • Volcanism & Plate Tectonics • Magnetic field

  4. Mars Mercury Moon Venus

  5. The History of Life on Earth • Geological Record – fossils and rock layers • 3 basic types of rock (Fig 4.2)‏ • Igneous – molten rock that cools and solidifies • Basalt,Granite • Metamorphic – transformed under Pressure/Temperature • Marble, Slate • Sedimentary – gradual compression of sediments • Important to fossil studies – slow buildup with fossils. • Limestone, Sandstone • Rock Cycle (Fig 4.3) + 4.4, 4.5, 4.6

  6. The History of Life on Earth • Rock Analysis • 3 basic types of rock • Mineralogical – identify minerals in the rock • Chemical – determine the elemental composition • Isotopic – ratio of different isotopes - gives formation age • Radioactive Dating (Fig 4.7)‏ • Half-life – probability (Fig 4.8; Table 4.1; Example 4.1)‏ • Parent – Daughter isotopes • Compare with geological record • Sometimes, find organic material (Jurassic Park) (Fig. 4.9)‏

  7. The Geological Time Scale Al26 Mg26 is important for early heating of Earth's core.

  8. The History of Life on Earth • 4 Eons (Fig 4.10)‏ • Hadean - “Hellish” • Archean - “Ancient Life” • Proterozoic - “Earlier Life” • Phanerozoic – Visible Life” • Age of the Earth – oldest rocks 4.0 Gyr • “Zircons” (Fig 4.11) ~4.4 Gyr • Suggest the crust separated from interior ~4.5 Gyrs • Moon rocks ~4.4 Gyr • Therefore, Moon existed by this time.

  9. Hadean Earth, Dawn of Life • 3 generations of atmospheres • Primary – H, He • Planet formation • Secondary – CO2, H2S, SO2, H2O... • Outgassing (Fig 4.12), Comet delivery(?)‏ • Tertiary – N2, O2, H2O • Modified by life

  10. Hadean Earth, Dawn of Life • Late Heavy Bombardment – ~3.9 Gyr ago • Relatively quiet between formation and LHB • Since then, protected by Jupiter • Sterilizing Impacts • 350-400 km in diameter (Fig 4.13)‏ • Completely vaporize the oceans • Global surface temperature rise 2000 C (3600 F)‏ • Last ~4.2-3.8 Gyr ago

  11. Impact Energies and these are the small ones

  12. Geology & Habitatbility • Earth's Interior – Seismic waves (Fig 4.14)‏ • Crust – lowest density, Al, Si, Ca • Mantle – rocky “plastic” • Outer Core – molten • Inner Core – solid, Fe, Ni • Earth's Interior – Differentiation • Melting and sedimentation of heavy material to core • Al26 ==> Mg26 contributed a lot of early heat

  13. Geology & Habitatbility • Plate Tectonics (Fig 4.15)‏ • What is it? • What causes it? • Evidence • Continental edge fits (Fig 4.16)‏ • Seafloor spreading • Two types of crust • Seafloor crust – young, high density basalt, thin • Continental crust - old, lower density granite, thick • Figs 4.18 - 4.23

  14. Magnetic Field • Loss of Atmosphere • Thermal escape – light favored over heavy • Impacts • Solar wind stripping • Cause • Electrically conducting interior fluid layer • Convection in the fluid layer • Moderate to fast rotation (dynamo effect)‏ • Figs 4.24 - 4.25

  15. Magnetosphere & Solar Wind • Magnetosphere • Protects surface and atmosphere from direct impact • Van Allen Belts • Trapped charged particles • Directed down to earth at poles

  16. Homework • Due Thur. Feb. 10 • Chapter 5: • 4, 6, 14, 20, 25, 27, 33, 37, 42, 47, 48, 49, 51

More Related