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From Fossils To Space Geology #1. What Do We Know?

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Presentation on theme: "From Fossils To Space Geology #1. What Do We Know?"— Presentation transcript:

1 From Fossils To Space Geology #1

2 What Do We Know?

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9 Solar Nebula Theory

10 The Solar System

11 The Primordial Earth

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14 The Solar Nebula Theory 5,000 Ma4,600 MaFusion 4,500 MaMars-sized impactor Present

15  Central disk: Sun (98.8%) Hadean Earth  accretion and differentiation

16 Hadean Earth  Solid inner & liquid outer core generate magnetic field  deflect solar wind Formation of Moon followed differentiation.

17 Hadean Earth  Solid inner & liquid outer core generate magnetic field  deflect solar wind Formation of Moon followed differentiation.

18 Hadean Earth  Composition & Timing

19 Hadean Earth  Meteorites—leftovers Ordinary chondrites 4,600 Ma Carbonaceous chondrites (5% organics) Iron (nickel) meteorites Stony-iron meteorites

20 Earth to Sun  90,000,000 miles (150 mill Km) Earth to Moon  225,000 miles (380,000 Km) Planet density decreases with distance--solar wind

21 Earth’s position in the Solar System: Earth to Sun  90,000,000 miles (150 mill Km) Extremely important: further away  ice closer in  steam

22 Hadean Atmosphere  outgassing CO 2 (carbon dioxide), H 2 O (water vapor), CO (carbon monoxide), H 2 (hydrogen gas), HCl (hydrogen chloride), N 2 (nitrogen gas), CH 4 (methane), NH 3 (ammonia), CH 2 O formaldehyde), HCN (cyanide)

23 Hadean Atmosphere  What’s missing? Oxygen generated by: 1. photochemical dissociation 2. photosynthesis

24 Oxygen Revolution  Archean Evidence: 1. Banded iron formations  ocean sediments start ~3,000 Ma: end ~1,800 Ma –UV radiation, purple bacteria, cyanobacteria

25 Oxygen Revolution  Archean Evidence: 1. Banded iron formations  ocean sediments start ~3,000 Ma: end ~1,800 Ma –UV radiation, purple bacteria, cyanobacteria

26 Oxygen Revolution  Proterozoic Evidence: 1.Banded iron formations  2.Terrestrial red beds  red rocks on land start ~2,300 Ma continues today

27 Oxygen Revolution  Proterozoic Evidence: 1.Banded iron formations  2.Terrestrial red beds  red rocks on land 3.Unstable minerals  Uraninite not present since 2,300 Ma

28 Oxygen Revolution  Proterozoic Evidence: 1.Banded iron formations  2.Terrestrial red beds  red rocks on land 3.Unstable minerals  Uraninite 4.Marine copper deposits  only with oxygen began ~1,700 Ma

29 Oxygen Revolution  Proterozoic Evidence: 1.Banded iron formations  2.Terrestrial red beds  red rocks on land 3.Unstable minerals  Uraninite 4.Marine copper deposits  only with oxygen 5.Presence of limestones  Proterozoic ocean (2,000 Ma) carbon dioxide rich  no carbonates

30 Oxygen Revolution  Phanerozoic Evidence: 1.Banded iron formations  2.Terrestrial red beds  3.Unstable minerals  4.Marine copper deposits  5.Presence of limestones  Free oxygen leads to ozone  UV protection

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33 Hadean Hydrosphere Hydrologic cycle: Water sweated from interior & condensed as rain Oceans estimated at 4.2 BYA, Australian zircons

34 Ancient crust 4,000 Ma marks beginning of Archean

35 Anatomy of a Tectonic Plate

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37 Formation of Archean Continental Crust Granulites: strongly metamorphosed and deformed— tonalite  10% quartz Strongly metamorphosed volcanics and sedimentary rocks

38 Formation of Archean Continental Crust Granulites: strongly metamorphosed and deformed— tonalite  10% quartz Greenstones: Strongly metamorphosed volcanics and sedimentary rocks

39 Formation of Archean Continental Crust Greenstones: What does the variation in composition suggest  subduction zone separation

40 Formation of Archean Continental Crust

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42 Time line Hadean 4,600 MaSolar Nebula, Earth forms 4,500 MaMoon forms 4,400 MaAnoxic atmosphere forms 4,200 MaOceans start forming Archean 4,000 MaCrustal differentiation 3,000 MaBIF’s, atmospheric oxygen

43 QUESTIONS?


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