a history including how life evolved, how the geosphere changed and major extinction events
TRANSCRIPT
Earth’s HistoryA history including how life evolved, how the
geosphere changed and major extinction events.
Eons◦ErasPeriodsEpochs
Time periods
Earth is approximately 4.6 billion years old. Remember:
◦ How did Earth form?◦ How are elements arranged?
Earth began to cool◦ 4 billions years ago: rocks◦ 3.8 billions years ago: water
Pre-Achean Eon (Hadean Eon): Formation of Earth
Could organic molecules form in Early Earth?
Miller and Urey experiment
The first organic molecules
Geologic evidence suggests that about 200 to 300 million years after earth cooled enough to carry liquid water, cells similar to modern bacteria were common.
How did these cells originate?◦ Microspheres◦ Evolution of RNA and DNA
The puzzle of life’s origin
The first organisms were single celled prokaryotic anaerobic cells that resemble modern bacteria. ◦ Evidence: microscopic fossils in rocks that are more than 3.5 billion years old.
Photosynthetic cells!◦ How did the oceans go from brown to blue-green?
What color is the sky now?
Archean Eon: First organisms
Endosymbiotic theory
Proterozoic Eon: Origin of Eukaryotic cells
Proterozoic Eon : What did Earth look like?
How did live begin to evolve into diverse life?◦ Asexual versus sexual reproduction◦ Multicellularity
Phanerozoic Eon: Diversity
Periods:◦ Cambrian: “Cambrian explosion”, hard parts,
shells, outer skeletons, invertebrates, arthropods.◦ Ordovician and Silurian: aquatic arthopods, fishes,
first land plants, octopi and squid.◦ Devonian: land plants, insecnts, vertebrates,
sharks, “age of fishes”.◦ Carboniferous (Mississipian/Pennsylvanian) and
Permian: amphibians, reptiles, winged insects, ferns.
Paleozoic Era
Cambrian Period: What did Earth look like?
Ordovician Period: What did Earth Look like?
Most organisms lived in the sea at this time.
The sea level dropped caused by plate tectonics.
The majority of land mass was over the south pole at this time and was a large glacier.
Approximately 57% of Earth’s species went extinct at this time.
Ordovician Period
Silurian Period: What did Earth look like?
The third extinction event occurred at the end of this period.
It was caused by ◦ fluctuating sea levels because more glaciers
pulled water from the oceans.◦ and global cooling due to land plants removing
CO2 from the atmosphere. There was approximately a 50% extinction
of the species on Earth.
Devonian period
This is the fourth extinction event. It is often called the “Great Dying” event
and was caused by:◦ Eruption of Siberian Volcanoes ◦ Formation of Pangaea disrupted ocean currents◦ Possible meteor impact
This resulted in an 83% extinction event◦ About 96% of all marine species◦ About 70% of all land vertebrates◦ Many arthropods and land plants also died.
Permian Period
Periods:◦ Triassic: “Age of reptiles”, fishes, insects, cone
breaing plants, mammals/◦ Jurassic: dinosaurs, birds.◦ Cretaceous: dinosaurs, birds, leafy trees, shrubs,
small flowering plants.
Mesozoic Era
Triassic Period: What did Earth look like?
This is the fifth extinction event Caused by the eruption of the central
Atlantic province.◦ Sulfur gas blocked the sun ◦ Large amount of lava released over several
centuries. This was a 48% extinction and a majority of
the species that went extinct were marine◦ Ammonites◦ Corals◦ Seed ferns
Triassic period
Jurassic Period: What did Earth look like?
Cretaceous Period: What did Earth look like?
At the end of the cretaceous period there was a sixth mass extinction event.
It is often referred to as the “K-T Boundary” and was likely caused by◦ Pangaea breaking up,◦ Eruption of Deccan Volcanoes in India◦ And possibly an asteroid impact.
It marks the end of the cretaceous period/Mesozoic era, the “age of reptiles” (dinosaurs).
Cretaceous Period
Periods:◦ Tertiary: marine mammals, grasses, large
mammals◦ Quarternary: humans
Cenozoic Era
Quaternary Period: What Earth looks like today.
73,000 years ago there was an event that led humans to near extinction.
It was caused by the Toba super volcano on the island of Sumatra. It disrupted ecosystems on a global scale.
Only a few ‘pockets’ of individuals remained, estimated at around 10,000 total.
Quaternary Period