Christian Vazquez - Geologic Timeline

  • 543 BCE

    Cambrian Period- 570 - 500 MYA

    Cambrian Period- 570 - 500 MYA
    The first geological time period of the Paleozoic era. The "Cambrian Explosion" marked a burst of evolutionary changes in life on Earth. Trilobites were the dominate species during this time. This period gets its name from Cambria, the Roman name for whales.
  • 448 BCE

    Ordovician Period- 488.3 - 443.7 MYA

    Ordovician Period- 488.3 - 443.7 MYA
    This period lasted 45 mya. During this time, the north area was almost all ocean and most of the world's land was collected into the supercontinent Gondwana. Throughout this time the supercontinent moved towards the south and was submerging underwater. shallow seas covering a large portion of Gondwana became breeding grounds for new forms of trilobites. Many of the species of Graptolites went extinct by the close of the period.
  • 443 BCE

    Silurian Period- 443 - 416 MYA

    Silurian Period- 443 - 416 MYA
    It was the third period in the Paleozoic era. It continued off from the Ordovician period and preceded the Devonian period. During this time period the sea level was rising and continental landmasses were low. Silurian fossils show evidence of reef building and the first signs that life was beginning to to colonize the new estuary, fresh water, and terrestrial ecosystems. Throughout this time and into Devonian, three northern continents collided forming a new super continent called Euramerica.
  • 412 BCE

    Devonian Period- 416 - 358 MYA

    Devonian Period- 416 - 358 MYA
    The fourth period of the Paleozoic Era. Its known as the "age of fishes." This time was a reef building in the shallow waters that surrounded each continent. The supercontinent Gondwana filled most of the southern hemisphere but it slowly began to drift north. The close of the Devonian period is considered the second of the "Big Five" mass extinction events.
  • 318 BCE

    Carboniferous Period- 359 - 299 MYA

    Carboniferous Period- 359 - 299 MYA
    This time period was known for its vast forests and can be also called the "coal age." The coal was produced by bark-bearing trees that grew in lowland swamp forests. The growth of these forests removed huge amounts of carbon dioxide, leading to a surplus of oxygen. The atmospheric oxygen levels were around 35%, compared with 21% today.
  • 297 BCE

    Permian Period- 299 251 MYA

    Permian Period- 299 251 MYA
    In this period the two super continents, Gondwana and Euramerica, had collided to form the supergiant pangaea. It was shaped like a thick letter C.
  • 199 BCE

    Triassic Period- 251 - 199 MYA

    Triassic Period- 251 - 199 MYA
    The first period of the Mesozoic era. It had the early mammals and early reptiles roaming around. Most of the continents were formed in a thick C shape. The climate was generally very dry. This era was known as the "age of Reptiles." Only two groups of animals survived the Permian extinction: Therapsids, and Archosaurs. Therapsids were a mammal-like reptile. Archosaurs were more reptilian.
  • 145 BCE

    Jurassic Period- 199.6 - 145.5 MYA

    Jurassic Period- 199.6 - 145.5 MYA
    The second segment of the Mesozoic era. During this period the supercontinent pangaea started to break apart. The northern half was splitting into landmasses that would eventually form North America and Eurasia. The southern half was transforming into what would be Antarctica, Madagascar, India, and Australia. And the western portion would soon form into Africa and South America. This period was the "age of dinosaurs." like it's name, dinosaurs were the dominant species in this period.
  • 145 BCE

    Cretaceous Period- 145 - 66 MYA

    Cretaceous Period- 145 - 66 MYA
    The last and longest segment of the Mesozoic era. It lasted approximately 79 million years ago. The continents were in different positions than they are today. The earliest birds came to be in this period.
  • 2 BCE

    Tertiary Period- 66 - 2.6 MYA

    Tertiary Period- 66 - 2.6 MYA
    The first period of the Era that we live in today. Earliest placental mammals started to become in this period. Mammals were becoming the dominant species for this era. By now the earth's continents almost formed into what we see and live on today.
  • 2 BCE

    Quaternary Period- 2.6 - Present Day

    Quaternary Period- 2.6 - Present Day
    The period we all live in today. By now we are in living on the continents that were formed for us in the past. Pangaea was now broken apart all over the earth. Life was forming from mammals and into humans. Us humans are now the dominant species of the earth. Although there were animals that are even right now extinct like the wooly mammoth, and others that I don't know about.