1 / 9

Geologic Timescale

Geologic Timescale. Archaean Eon. 4.6-2.5 billion years ago ( bya ) Earth’s origin 3.7 bya : First protobionts 3.5 bya : First Prokaryotes 2.5 bya : atmospheric Oxygen increases. Proterozoic Eon. 2.5 bya to 542 mya 2.2 bya : first Eukaryotes

thai
Download Presentation

Geologic Timescale

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. Geologic Timescale

  2. Archaean Eon • 4.6-2.5 billion years ago (bya) • Earth’s origin • 3.7 bya: First protobionts • 3.5 bya: First Prokaryotes • 2.5 bya: atmospheric Oxygen increases

  3. Proterozoic Eon • 2.5 bya to 542 mya • 2.2 bya: first Eukaryotes • Prokaryotes with plastids, mitochondria, and DNA • 600 mya: algae and soft bodied invertebrate animals • Snow ball Earth Hypothesis: Life can only exist where sunlight can reach deep ocean (where there was no ice), like vents and plate boundaries

  4. Phanerozoic Eon • Eras: • Paleozoic: 542 mya to 251 mya • Mesozoic: 251 mya to 65 mya • Cenozoic: 65 mya to today • All of life evolves to current state • Two mass extinctions: • Permian • Cretaceous

  5. Paleozoic Era • Periods: • Cambrian: Cambrian explosion and diversity of species • Ordovician: Plants and Arthropods colonize land • Silurian: vascular plants diversify • Devonian: Bony Fish, tetrapods, insects • Carboniferous: GIANT FOREST OF VASCULAR, Reptiles • Permian: More reptiles, origin of modern insects, MASS EXTINCTION

  6. Permian Mass Extinction • 96% of marine species gone • Increased volcanic activity in modern day Siberia • More CO2 in atmosphere, warmed planet • Less difference in equator and poles, slowed ocean currents • No currents, less oxygen for marine life

  7. Mesozoic Era • Periods: • Triassic: Cone bearing plants, dinosaurs diversify, and mammal like reptiles • Jurassic: Continued dominance of Cone bearing plants and dinosaurs • Cretaceous: Flowering plants emerge, Mass Extinction

  8. Cretaceous Mass Extinction • 50 % of marine life gone, most land plants and dinosaurs gone • Theory: asteroid or comet hit modern day Mexico and created a cloud of dust on Earth • This dust became a layer of clay with Iridium, which is an element not common on Earth • There was also an increase in volcanic activity in India

  9. Cenozoic Era • Periods: • Paleogene: 65 - 23 mya • Diversity of mammals, birds and insects • Flowering plants become dominant • Origin of Primate groups • Neogene: 23 mya – today • Origin of genus Homo • Ice Ages • Modern Day

More Related