| Time |
Characteristics |
Name of Stage |
Duration of Stage
(Billions of Years Ago) |
Chemicals/Gases in
Atmosphere |
Important Processes and
Features |
|
4.5 billion years
|
Formation of the approximately homogeneous solid Earth
by planetesimal accretion.
|
Early Atmosphere |
4.4 to 4.0 |
H2O, hydrogen cyanide (HCN), ammonia (NH3),
methane (CH4), sulfur, iodine, bromine, chlorine, argon |
Lighter gases like hydrogen and helium
escaped to space. All water was held in the atmosphere as vapor because of
high temperatures. |
|
4.0 billion years
|
Planet surface cools and bombardment from space slows,
so life has the possibility of existing on the planet. Oldest earth rocks
dated by radioactivity.
|
Secondary Atmosphere |
4.0 to 3.3 |
At 4.0 billion H2O, CO2, and
nitrogen (N) were the dominant chemicals. Cooling of the atmosphere causes
precipitation and the development of the oceans. By 3.0 billion CO2, H2O,
N2 are the dominant chemicals. O2 begins to accumulate. |
Continued release of gases from
the lithosphere. Water vapor clouds were common in the lower atmosphere.
Chemosynthetic bacteria appear on the Earth at 3.6 billion. Life begins to
modify the atmosphere. |
|
3.85 billion years
|
Evidence for life seen in Greenland rocks enriched in
C12 isotope.
|
|
3.85 - 3.7 billion years
|
Prokaryotes diverge from Archaea. Sometime after
prokaryotes diverge from archaea, chlorophyll and photosynthesis evolve in
the bacterial lineage. Archaea do not make chlorophyll, and only some
bacteria are photosynthetic.
|
|
3.7 billion years
|
First banded iron formation seen. Implies oxygen made
by photosynthesis.
|
|
3.5 billion years
|
First stromatolites seen (assumed to be of biological
origin, with cyanobacteria, as in present day stromatolites).
|
|
3.5 - 2.8 billion years
|
Beginning of photosynthesis by blue-green algae which
releases oxygen molecules into the atmosphere and steadily works to
strengthen the ozone layer and change the Earth's chemically reducing
atmosphere into a chemically oxidizing one.
|
Living Atmosphere |
3.3 to Present |
N2, O2, Argon, CO2 |
Development, evolution and
growth of life increase the quantity of oxygen in the atmosphere.
Concentration of atmospheric oxygen levels off. Starting about year 1700,
humans begin to modify the concentrations of some gases in the atmosphere |
|
2.7 billion years
|
Steranes = eukaryotic sterol derived biomarkers found
in Australian shale.
|
|
2.4 billion years
|
Rise in the concentration of oxygen molecules stops the
deposition of uraninites (since they are soluble when combined with
oxygen).
|
|
2.1 million years
|
First tentative evidence of a eukaryotic microfossil,
not yet confirmed.
|
|
2.0 billion years
|
Oxygen begins to rise in the atmosphere after oxygen
sinks saturated. The Oklo natural fission reactor in Gabon goes into
operation.
|
|
1.6 billion years
|
The last reserves of reduced iron are used up by the
increasing atmospheric oxygen--last banded iron formations.
|
|
1.5 billion years
|
Oxygen level in the atmosphere reaches present day
level and stabilizes. Chloroplasts and mitochondria present. Eukaryotic
cell organisms develop.
|
|
1.2 billion years
|
Major eukaryotic groups diverge. Plants separate before
animals/fungi.
|
|
670 million years
|
Invertebrates and vertebrates diverge.
|
|
1500 - 600 million years
|
Rise of multicellular organisms.
|
|
580 - 545 million years
|
Fossils of Ediacaran organisms are made.
|
|
530 million years
|
Cambrian explosion of fossil record. Burgess shale.
|
|
528 - 526 million years
|
Fossilization of the Chengjiang site.
|
|
500 - 450 million years
|
Rise of the fish--first vertebrates.
|
|
430 million years
|
Waxy coated algae begin to live
on land.
|
|
420 million years
|
Millipedes have evolved-first
land animals.
|
|
380 million years
|
Vertebrates move onto land.
|
|
375 million years
|
Appearance of primitive sharks.
|
|
360 million years
|
Gymnosperms (naked seed plants) diverge from
angiosperms (flowering plants).
|
|
350 million years
|
Primitive insects have evolved and primitive ferns
evolve-first plants with roots.
|
|
310 million years
|
Birds and other vertebrates diverge.
|
|
350-300 million years
|
Rise of the amphibians.
|
|
300 million years
|
Winged insects have evolved.
|
|
280 million years
|
Beetles and weevils have evolved.
|
|
230 million years
|
Roaches and termites have
evolved.
|
|
225 million years
|
Modern ferns have evolved and
Bbees have evolved.
|
|
300 - 200 million years
|
Rise of the reptiles
|
|
200 million years
|
Pangaea starts to break apart,
primitive crocodiles have evolved and appearance of mammals
|
|
200 - 150 million years
|
Monocots diverge from dicots, oldest angiosperm fossil
= 142 million years
|
|
145 million years
|
Archaeopteryx
walks the Earth
|
|
150 - 90 million years
|
Primitive kangaroos, cranes and
modern sharks have evolved.
|
|
65 million years
|
K-T Boundary--extinction of the
dinosaurs and beginning of the reign of mammals
|
|
7 - 6 million years
|
Sahelanthropus tchadensis
- oldest known hominid or near-hominid species
|