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GY 112: Earth History. Proterozoic Fossils. Agenda. Key Events of the Proterozoic Proterozoic Plate Tectonics Proterozoic Glaciation Background Proterozoic Life Forms Evidence of Proterozoic Life Factors Affecting Development of Proterozoic Life Implications of Proterozoic Info.
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GY 112: Earth History Proterozoic Fossils
Agenda Key Events of the Proterozoic Proterozoic Plate Tectonics Proterozoic Glaciation Background Proterozoic Life Forms Evidence of Proterozoic Life Factors Affecting Development of Proterozoic Life Implications of Proterozoic Info
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Key Events • 2 Supercontinent Episodes • 3 Glacial Episodes (Snowball Earth) • Change from O2 Poor to O2 Rich • 2 Major Meteor Impacts • BIFs (Major Source of Iron) • Major Copper Deposits • Evolution of Life from One Cell to Multi-Cell
Plate Tectonics • Wilson Cycle (3 Parts) • Opening of an Ocean Basin • Sedimentation • Closing of an Ocean Basin • Supercontinent Episodes • Rodinia: 1.6 to 1.0 bya • Columbia (Laurentia): 2.5 to 1.6 bya • Orogenic Episodes • Wopmay (Laurentia) • Keeweenewan (Laurentia) • Greenville (Rodinia)
Glaciation Snowball Earth (635 – 750 MA) • Marinoan (635 – 700 MA) • Sturtian (700 – 750 MA) • Huronian (2.5 – 1.6 GA)
Background Info Proterozoic is the largest Eon of the 4 Eons (542 MA to 2.5 GA: ~ 2 Billion years old) • Consists of 3 Eras - Each is as large or larger than the entire Phanerozoic Eon. • Neoproterozoic (542 MA to 1.0 GA) • Mesoproterozoic (1.0 GA to 1.6 GA) • Paleoproterozoic (1.6 GA to 2.5 GA)
Proterozoic Era Highlights Paleoproterozoic (2.5 GA to 1.6 GA ) • Evolution of Cyanobacteria (O2 Producers) • O2 Catastrophy • BIFs (Banded Iron Formations) • Huronian Glaciation • 2 Largest Impact Events in Earth’s History • South Africa – Vredefort • Ontario Canada – Sudbury Basin • Earth’s Atmosphere Changed to an O2 Environment • Columbia Supercontinent Formed
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Proterozoic Era Highlights Mesoproterozoic (1.6 GA to 1.0 GA) • Red Algae • First Sexual Reproduction • Earliest Complex Multicellular Organism • Columbia Supercontinent Broken up • Rodinia Supercontinent Formed
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Proterozoic Era Highlights Neoproterozoic (1.0 GA to 542 MA) • Extreme Glaciation (Snowball Earth) • Earliest Multicellular Organisms (Ediacaren) • Break-up of Rodinia Supercontinent
Oxygen Catastrophy(1.6 – 2.5 bya) • Oxygen created from photosynthesis • Oxygen toxic to anaerobic organisms • Initial lag of 300 million years for free oxygen in the atmosphere • Oxygen initially combined with free iron in the oceans to form magnetite.
Snowball Earth(630 – 850 mya) • Glacial Periods: Startian & Marinoan/Varanger • Causes • Reflective surface of continents • Removal of CO2 from atmosphere • Change in ocean circulation patterns • Intro of pure oxygen which converted methane into CO2 • Reduction in Organic Activity • Subsequent melting caused by emission of CO2 from volcanic activity
Proterozoic Life Forms • Life Forms • Acritiarchs (Single Celled) • Ediacarens (Multi-Celled) • Evolutionary Development • From Prokaryotic to Eukaryotic • Onset of Sexual Reproduction • From Single Cell to Multi-Cell • Soft-Bodied to Shell Covering
Proterozoic Life Forms • During the Archean, we saw the rise of the prokaryotes: • Small • No nucleus • DNA spread throughout the cell • Asexual reproduction • Could only be single-celled
Proterozoic Life Forms • During the Proterozoic, something wonderful happens: • the rise of the eukaryotes: • Larger (>0.06 mm) • A nucleus and organelles • DNA contained within the nucleus • Sexual reproduction • Could be multi-celled (metazoans)
Proterozoic Life Forms The first eukaryotes appeared around 2 GA. Archritarchs were small, single celled silica beasties that floated in the oceans (pelagic). They peaked in abundance at 750 MA and then went away… 0.1mm
Proterozoic Life Forms … or did they? They might in fact be ancestors to equally small single celled organisms that are around today called dinoflaggelates. 0.1mm
Proterozoic Life Forms Another big change in the Proterozoic was the appearance of the first Metazoans 5 cm
Proterozoic Life Forms They are known as the Ediacarin Fauna http://www.snowballearth.org/end.html http://www.cartage.org.lb/en/themes/Sciences
Proterozoic Life Forms They are known as the Ediacarin Fauna And they are found around the world http://www.snowballearth.org/end.html http://www.cartage.org.lb/en/themes/Sciences
Proterozoic Life Forms What were the Ediacarins? Three major “forms” http://www.cartage.org.lb/en/themes/Sciences
Proterozoic Life Forms What happened to them?
Proterozoic Life Forms What happened to them? 1) a now extinct line of beasties
Proterozoic Life Forms What happened to them? 1) a now extinct line of beasties 2) ancestors to living phyla Kimberella sp. http://www.ucmp.berkeley.edu/vendian/kimberella.jpg
Proterozoic Life Forms What were the Ediacarins? 1) a now extinct line of beasties 2) ancestors to living phyla Dickinsonia sp.
Proterozoic Life Forms Whatever they were, they “exploded” onto the scene immediately after the last Snowball Earth. http://pharyngula.org/index/science/2004/08/
Evidence of Proterozoic Life Direct Evidence Fossils Trace Fossils
Evidence of Proterozoic Life Indirect Evidence BIFs (Banded Iron Formation)
Proterozoic Fossils Severe environmental changes drives evolutionary adaptation. http://www.snowballearth.org/end.html
Proterozoic Fossils Severe environmental changes drives evolutionary adaptation. We need bad things to happen in order to evolve. http://www.snowballearth.org/end.html
Factors Affecting Development of Proterozoic Life Terrestrial Atmospheric Changes Climate Geography
Factors Affecting Development of Proterozoic Life “Atmospheric Changes”
Factors Affecting Development of Proterozoic Life “Atmospheric Changes”
Factors Affecting Development of Proterozoic Life “Climatic Changes” We now recognize three major Earth phases 1) Greenhouse Earth (no continental glaciers present) 2) Icehouse Earth (continental glaciers present) 3) Snowball Earth (Frozen oceans at equator) http://www.snowballearth.org/end.html
Factors Affecting Development of Proterozoic Life Extra-Terrestrial Solar Radiation Impact Events
Implications of Proterozoic Info Ediacarin Evolutionary Development Diversity of Life Present Day Global Warming