The Cenozoic Era is the most recent of the three major geological eras, spanning from about 66 million years ago to the present. It is also referred to as the "Age of Mammals" due to the diversification and dominance of mammalian life forms during this time period.
End-Cretaceous Extinction: The era began with a mass extinction event that wiped out the dinosaurs and many other species, leading to the rise of mammals and birds.
Continental Drift: The continents continued to drift apart, leading to the formation of modern-day landmasses.
Climate Change: The Earth underwent significant climate changes, including periods of cooling and warming that influenced the evolution and distribution of flora and fauna.
Hominid Evolution: The Cenozoic saw the emergence and diversification of early hominids, eventually leading to the appearance of modern humans.
Geological Epochs
The Cenozoic Era is divided into three major epochs:
Paleogene: This epoch began immediately after the extinction of the dinosaurs and witnessed the diversification of mammals, birds, and early primates.
Neogene: During this epoch, grasses and savannas became widespread, and early human ancestors, such as Australopithecus, appeared in Africa.
From Molecules to Organisms: Structures and Processes
Students who demonstrate understanding can:
Use argument based on empirical evidence and scientific reasoning to support an explanation for how characteristic animal behaviors and specialized plant structures affect the probability of successful reproduction of animals and plants respectively.