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-The solar system formed ~5.0 BYA from a giant spinning cloud of gas and dust or a NEBULA -Solar winds drove lighter elements and frozen gases outward into space -Cold matter collected in eddies -Particles began to accrete and form proto planets, then eventually planets |
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-Gravitational Contraction -Bombardment of early earth by meteorites -Radioactive decay |
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Gravitational Contraction |
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The increased gravity of Earth, due to accretion, caused it to shrink in size which through friction produced great amounts of heat. Raised earths internal temperature to ~1500 |
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Rocky/Terrestrial Planets |
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-Mercury, Venus, Earth, Mars -Composed of rock and metal -Contain heavier elements -Average Density 5.1-5.5 g/cm^3 |
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-Jupiter, Saturn, Uranus, Neptune -Composed of lighter elements, H and He -Average density 0.7-1.7 |
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-The orbit of planets around the Sun is on the same plane and in the same direction -The rotation of most planets is the same direction -The orbit and rotation of most moons about their planets are the same |
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Planetary Differentiation |
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Shortly after the Earth accreted, the homogenous planet differentiated into layers based on density |
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Oldest Rocks and Minerals |
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-Oldest whole rock is 4.0 Ba -Oldest mineral grains (detrital zircons) 4.2 Ba |
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-The moon is believed to have formed when a proto planet collided with the Earth. -Oldest moon rocks dated 4.4-4.5 Ba |
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Aged 4.53-4.58 Ba also show age of the Solar System |
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-4.0-2.5 Ba -Earths crust became stable enough that rocks were preserved -Plate tectonics began -Atmosphere became oxygenated |
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-Stable interior portion of continents -Contain the oldest rocks |
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The areas that are subject to mountain building (orogeny). They surround cratons |
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Cordilleran Orogenic Belt |
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Runs from Alaska to Patagonia. Means backbone. |
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A pile of sedimentary rocks that cover a craton |
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The stable igneous and metamorphic rocks below the platform in a craton |
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Section of a craton that is exposed. Exposed precambrian rocks. -Greenstone Belts -Granite Gneiss Complexes |
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-Represent Archean ocean crust -Composed of mafic rocks that have altered to chlorite -Form at convergent boundaries (Back Arch Basins) -Deformed turbidites -Contain Pillow basalts |
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A deposit representative of a turbidity current |
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Sandstone with a high percentage of mud and other heterogeneous particles. Indicative of Islands |
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-Felsic -Early remnants of continental crust -Surround and intrude Greenstone Belts -Form at convergent boundaries |
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Areas that form behind some subduction zones where the crust is stretched and new basaltic crust is formed in the cracks left behind. |
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Greenstone Belt Preservation |
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-Closing of Back Arch Basins due to compression preserves Greenstone Belts -Preservation is also due to the difference in plate tectonics in the past -There where more subduction zones, and convection was more rapid |
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Isotopic evidence for photosynthesis is evident 3.8 Bya |
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-Bacteria that photosynthesize -Can live almost anywhere there is sunlight and moisture -Can live alone or in colonies -Filaments found in fossils 3.4-2.5 Bya |
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Filamentous entangled microorganisms that form on top of sediments |
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Reefs formed by microbial mats that become lithified and grow upward -Precipitate Calcium Carbonate -The living part is on the surface -Have a layered internal structure -Form in hypersaline environments -Verycommon from 3.0 Bya till end of the precambrian |
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Proteins-Amino Acids DNA/RNA-Nucleic Acids |
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-Produced amino acids in labs -Mixed CH4, NH4, O2, and N then added a spark (energy) -Not accurate to early atmospheric conditions |
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-May have formed in deep ocean vents -Amino Acids may have come from meteorites (have been found on them) -Clay minerals have been hypothesized to have served as scaffolding or templates for assembling proteins -No self replicating life has ever been produced in Laboratory |
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-Likely composed of H and He -Solar winds likely blew those away because earths magnetic field had not yet formed |
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Likely composed of volcanic gasses (H, N, H2O, CO2) -Outgassing due to differentiation |
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Detrital Pyrite and Uraninite |
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-Unstable on earths surface, degrade rapidly if exposed to O2 -If O2 were present in past atmospheres, these would not have survived -Disappear around 2.5 bya |
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-Altering bands of Hematite, an iron rich mineral, and Chert, a quartz mineral -Proterozoic -Marine sediments, formed in oceans -97% of iron ore in US comes from BIFs -Indicative of a time when O2 levels began to rise |
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-Sandstone and shale beds that are red due to the presence of iron oxide -terrestrial deposits, common in rivers |
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-2.5-542mya -Atmosphere rich in O2 -First eukaryotic and multicellular organisms -first large continent assembled -First ice age -Mature siliciclastic sediments accumulate -Limestone beds become widespread |
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-One of the first large continents, assembled by a series of collisions -Contained much of what is now North America, Greenland and Scotland |
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-Supercontinent formed in the mid-Proterozoic when Laurentia collided with other large continents -Means "Motherland" russian |
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-First eukaryotes, single celled, comparible to modern eukaryotes, -Eukaryotes reproduce sexually and hav a nucleus ~1.6 Bya |
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Organelles such as mitochondria and chloroplasts were once bacteria that took up residence in other cells -Symbiotic Relationship -Organelles have cytoplasm and their own DNA -DNA of mito and plast resemble that of Bacteria |
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Fossils found in australia of soft bodied organisms, believed to indicate a period of rapid climate change at the end of the Proterozoic -Evolved in isolation, in melt pools on snowball earth |
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-Sun was weaker during the Precambrian -Evidence of 2 glaciated periods, 2.4 BYa and 700-600 MYa(snowball Earth) |
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Rivers of ice that flow by their own weight |
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Poorly sorted sediment that is left behind by receding glaciers |
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Glacial till that has become lithified |
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Sediment carried by icebergs, and deposited elsewhere |
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700-600 MYa when the earth was entirely glaciated -Suns luminosity was 90% of its current value -Lower greenhouse effect -Rodinia was situated on the equator, which increased earths albedo -Increased chemical weathering due to the large continent drew down more CO2 -Ended by volcanic eruptions that delivered enough CO2 to swing earth out of ice age -Shown by glacial tillites and dropstones followed by limestones |
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542-251 MYa -Rodinia breaks up then reforms as Pangea -Sea level was much higher -Life in the oceans diversifies and land is colonized |
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Epeiric Sea (Epicontinental Sea) |
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Seas on top of continental crust -usually very shallow -Yellow sea (china) Hudson Bay (canada) |
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-NA craton has been covered by epeiric seas 6 times during the Phanerozoic Eon -Shoreline transgressed -Deeper water facies deposited on shallower water facies -Observed 6 transgressive sequences recording sea level rise separated by unconformities |
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A landward shift of shoreline due to sea level rise |
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A layer of Limestone on top of mudstone on top of sandstone records transgressions |
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Can occur because the level of the sea bed is changed by relative accumulation or by sediment compaction or by fault movement |
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Global (Eustatic) Sea Level Change |
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-The volume of water stored in oceans changes -The capacity of the ocean basins changes -Rising at 3.5 mm/yr. -Warming of oceans can cause water to expand |
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Chemical weathering of silicate minerals such as feldspars scrub CO2 out of the atmosphere -Weathering produces bicarbonate ion which is transported to and stored in the ocean |
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Rising coastlines near convergent boundaries can cause local regression of sea level (Alaska) |
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Land sinking due to tectonics or oil extraction causes transgression (Galveston, TX) |
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-Around 535 mya variety of fossils diversifies rapidly -Almost all phyla of invertebrates appear -Hard and Soft bodied animals preserved |
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Cambrian Explosion Explanations |
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1. Increased O2 levels (not likely) 2. The expansion of habitats due to transgression 3. Advent of predation |
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-organisms produce minerals to harden their bodies -Began at the end of the proterozoic |
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-(Strange Shrimp) Early predator found in Burgess Shale -Got as big as 1 meter -Preyed on trilobites |
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-Most likely explanation of the Cambrian Explosion -Lead to development of external skeletons and improved locomotion -Accelerated the pace of evolution |
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-Discovered in 1909 by Charles Walcott in BC -Mid-Cambrian in age -Contains unusual assemblage of soft bodied organisms -Preserved by a piece of reef that collapsed and was buried in mud in deep O2 deficient waters |
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