Slide 16
Evolution of Mammals
Very late cynodont (195 mya)
Later cynodont (220 mya)
Early cynodont (260 mya)
Therapsid (280 mya)
Synapsid (300 mya)
Temporal
fenestra
Temporal
fenestra
Temporal
fenestra
EARLY
TETRAPODS
Articular
Key
Quadrate
Dentary
Squamosal
Reptiles
(including
dinosaurs and birds)
Dimetrodon
Very late cynodonts
Mammals
Synapsids
Therapsids
Earlier cynodonts
Slide 17
The geologic record is divided into the Archaean, the Proterozoic, and the Phanerozoic eons.
The Phanerozoic encompasses multicellular eukaryotic life.
The Phanerozoic is divided into three eras: the Paleozoic, Mesozoic, and Cenozoic.
Major boundaries between geological divisions correspond to extinction events in the fossil record.
Concept 25.3: Key events in life’s history include the origins of single-celled and multicelled organisms and the colonization of land
Slide 18
Geologic Record
Slide 19
Geologic Time Table
Animals
Colonization
of land
Paleozoic
Meso-
zoic
Humans
Ceno-
zoic
Origin of solar system
and Earth
Prokaryotes
Proterozoic
Archaean
Billions of
years ago
1
4
3
2
Multicellular
eukaryotes
Single-celled
eukaryotes
Atmospheric
oxygen
Slide 20
The oldest known fossils are stromatolites, rock-like structures composed of many layers of bacteria and sediment.
Stromatolites date back 3.5 billion years ago
Prokaryotes were Earth’s sole inhabitants from 3.5 to about 2.1 billion years ago.
Slide 21
Photosynthesis and the Oxygen Revolution
Most atmospheric oxygen (O2) is of biological origin.
O2 produced by oxygenic photosynthesis reacted with dissolved iron and precipitated out to form banded iron formations.
The source of O2 was likely bacteria similar to modern cyanobacteria.
Slide 22
By about 2.7 billion years ago, O2 began accumulating in the atmosphere and rusting iron-rich terrestrial rocks.
This “oxygen revolution” from 2.7 to 2.2 billion years ago
Posed a challenge for life
Provided opportunity to gain energy from light
Allowed organisms to exploit new ecosystems.