History of Life on Earth

This fall, the students in Fayerweather Street School’s 5th & 6th grades studied the 4.5 billion years of the Earth’s history. We learned about geological events, studied organisms that lived during the last 500 million years in science, and learned about hominids living in the Great Rift Valley in Social Studies. The plaques on this timeline display our research on a scale of 1 meter = 100 million years.

Local, Medford-based woodworker Jess Morgan created the wooden QR code plaques positioned around Fresh Pond.

Timeline Map

Precambrian

  • Formation of Earth

    4.54 Billion Years Ago

    Our solar system formed approximately 4.5 billion years ago.

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  • Moon Forms

    4.40 Billion Years Ago

    Earth's moon was formed when the earth was still a young molten planet.

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  • Late Heavy Bombardment

    3.9 Billion Years Ago

    Earth has cooled off enough to have a crust over its molten core. For millions of years asteroids pelted our planet and brought microscopic crystals of ice to Earth.

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  • Stromatolites

    3.5 Billion Years Ago

    Microscopic life existed on earth. Cyanobacteria were creating oxygen through photosynthesis.

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  • Snowball Earth

    650 Million Years Ago

    For billions of years Earth's climate had been changing due to plate tectonics and microscopic life. Then we entered an ice age nicknamed Snowball Earth.

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Paleozoic

  • Trilobites

    540 Million Years Ago

    When Snowball Earth melted there was an explosion of evolution. A wide diversity of life developed in the oceans.

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  • Marrella

    480 Million Years Ago

    Animal life in the ocean continued to diversify, while plant and fungal life on land started to get established.

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  • Terropterus

    430 Million Years Ago

    During this warm period many plants and animals thrived.

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  • Cephalapsis

    390 Million Years Ago

    Each animal was developing specialized features for hunting and avoiding being eaten.

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  • Tiktaalik

    375 Million Years Ago

    Tetrapods started to live on land.

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  • Dunkleosteus

    360 Million Years Ago

    Fish, tetrapods, and invertebrates continue to evolve interesting features.

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  • Stethacanthus

    330 Million Years Ago

    Swamps with lush plants from this time period turned into the coal and oil reserves we are using today.

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  • Meganeura

    300 Million Years Ago

    Complex plant life created high oxygen levels. This allowed for giant insects to rule the air.

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  • Eothyris

    280 Million Years Ago

    The giant supercontinent of Pangea has formed with both deserts and ice caps. Plants and animals have to adapt to drier environment and a wider range of temperatures.

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  • Scutosaurus

    255 Million Years Ago

    On land both herbivores and carnivores have developed large bodies as they live in complex ecosystems.

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Permian Extinction

  • The Great Dying

    252 Million Years Ago

    Volcanic activity and a depletion of oxygen in the oceans lead to the extinction of 75% of all life on the planet. (81% marine life and 70% of terrestrial)

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Mesozoic

  • Pteranodon

    200 Million Years Ago

    After the Permian Extinction, reptiles quickly evolved to take over the land, oceans, and air. This is the age of the dinosaurs.

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  • Yi Qi

    150 Million Years Ago

    During this period Pangea pulled apart and our current continents started to form, and alongside the dinosaurs are first mammals and many other species that still exist today.

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  • Microraptor

    100 Million Years Ago

    This was a wam period for our planet. Flowering plants and pollinators evolved during this time.

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  • Mosasaurus

    80 Million Years Ago

    Due to the warm climate sea levels were high. Shallow seas covered what is dry land today.

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  • Therizimosaurus

    70 Million Years Ago

    Dinosaurs were the dominant animal life on all seven continents.

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KT Extinction

  • KT Extinction

    66 Million Years Ago

    When a giant asteroid hit Earth it created a world-wide extinction that took place in a matter of hours. The impact sent rock vapor into space. The vapor cooled and returned to the planet as tiny shards of glass. The friction of these shards reentering the atmosphere caused temperatures to spike dangerously hot.

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Cenozoic

  • Titanoboa

    60 Million Years Ago

    Life evolved in the niches left open by the K-T extinction.

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  • Gastornis

    50 Million Years Ago

    As the continents separated, each ecosystem became distinct.

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  • Lepictidium

    40 Million Years Ago

    Many interesting animals of this time period are no longer alive today, but we can see similarities to modern animals in their body structures.

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  • Paraceratherium

    30 Million Years Ago

    Evolution was also spurred on by a climate that cycled between global warming and ice ages.

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  • Megalodon

    20 Million Years Ago

    Ocean life was also interesting during this time period.

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  • Ardipthecus Ramidus

    4.5 Million Years Ago

    There are many branches of our family tree.

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  • Australopithecus anamensis

    4.0 Million Years Ago

    Many of our earliest hominin ancestors lived in the Great Rift Valley of Africa.

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  • Australopithecus Afarensis A1

    3.5 Million Years Ago

    This is the time period when our ancestors became bipedal.

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  • Australopithecus Garhi

    2.0 Million Years Ago

    As the last ice age impacted the planet our ancestors in the genus Homo continued to evolve in Africa.

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  • Paranthropus robustus A

    1.5 Million Years Ago

    Some of our evolutionary cousins evolved alongside our ancestors, but their lineage did not survive. "Paranthropus" means "alongside humans"

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  • Homo Erectus A

    1.0 Million Years Ago

    As our ancestors left Africa, they interacted with a variety of other animals.

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  • Homo Heidelbergensis A

    500,000 Years Ago

    Many hominins were established throughout the Europe and Asia before our species, Homo sapiens, even existed.

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  • Dire Wolf

    100,000 Years Ago

    Our species Homo sapiens has been on our planet for only a tiny portion of our planet's history. Yet our impact on our planet is so great we call today's time period Anthropocene -- or the epoch where human activity is having the greatest influence on climate and environment.

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Fayerweather Street School | 765 Concord Avenue, Cambridge, MA 02138 | 617-876-4746
Fayerweather is a private PreK, kindergarten, elementary and middle school. We engage each child’s intellect.