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Lesson 2: Ancient Earth. ??. Essential Questions. How did gravity affect Earth’s formation ? How did the oceans and atmosphere form ? What conditions made early Earth able to support life ? How did environmental changes affect the evolution of life ?. Vocabulary. Hadean eon
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?? EssentialQuestions • HowdidgravityaffectEarth’sformation? • Howdidtheoceans and atmosphereform? • WhatconditionsmadeearlyEarthabletosupportlife? • Howdidenvironmentalchangesaffecttheevolution of life?
Vocabulary • Hadeaneon • Archeaneon • Protocontinent • Proterozoiceon • Thermalenergy
Earth’sEarliestHistory • Gravity and the Solar System • BeforeEarthoreventhe solar systemexisted, a cloud of gas, ice, and dust, called a nebula, floated in space
Earth’sEarliestHistory • First: Gravitypulledtheparticulestogetherinto a flattened disk shape and begantorotate. • Second: the material in the center became dense and theSunformed • Third: theremainingpieces of material in the disk attractedeachother and planetswereformed
SphericalEarth • As more particles come togetherEarthbecamelarger. • Thermalenergyisproducedbycollisions, whichwarmedtheplanet. • AsteroidscontinuedtocrashintotheEarthsurface, makingitevenhotter.
HadeanEon Thefirst 640 millionyears of Earthhistory
HadeanEon • Thefirst 640 millionyears of Earthhistory • Formation of Earth’sCore • A hotEarthcools • Seas of Molten Rock • Changes in the Seas • TheAncientAthmosphere
ArcheanEon Fromabout 4 to 2.5 billionyearsago
ArcheanEon • Earthcontinuestocool and firstsolidsurfaceappeared, butstilltwice as muchinternalthermalenergywasproduced at that time, comparingtonowadays. • VolcanicActivity • As magma risedtothesurfacethroughcracks in theoceanfloorit has formedEarthfirstoceaniccrust. • TheEarliestContinents • Protocontinents: small and earlycontinentswhichhavecollidedbetweeneachotherformingbiggerlandmasses • Earth’sOceansForm • Fossil bacteria and stromatolites are theearliestevidence of lifepresent in rocks. They are uncommon and difficulttoseeduetotheirmicroscopicsize. • TheArcheanoceanswere extreme environments, mostorganismsalivetodaywouldnothavesurvivedthen.
ProterozoicEon From 2.5 to 0.542 billionyearsago
ProterozoicEon • Changes in theAtmosphere: Earthwascoolingdown and largerlandmasseswereformed. • Increase in Oxygen • SnowballEarth • Supercontinents and Shallow Seas • ProterozoicLife • Unicellularorganisms in water. • Firstmulticellularorganisms in theocean, buthad no hardparts, so fossilsaren’tabundant.
Homework • Textbook: Page 94 #2, 3, 4 • Workbook: Page