The Cenozoic Era is divided into seven epochs: the Paleocene, Eocene, Oligocene, Miocene, Pliocene, Pleistocene, and Holocene. The Paleocene marks the beginning of the era, followed by the Eocene, known for the rise of mammals and flowering plants. The Oligocene features further mammalian diversification, while the Miocene and Pliocene epochs see the evolution of modern flora and fauna. The Pleistocene is characterized by ice ages, and the Holocene represents the current epoch, beginning approximately 11,700 years ago.
The Cenozoic era is subdivided into two periods: the Paleogene and the Neogene. The Paleogene includes the Paleocene, Eocene, and Oligocene epochs, while the Neogene includes the Miocene and Pliocene epochs.
Relatively recently in the Cenozoic era
The geological era that is divided into both periods and epochs is the Cenozoic Era. The Cenozoic, which began about 66 million years ago and continues to the present, is subdivided into three periods: the Paleogene, Neogene, and Quaternary. Each of these periods is further divided into epochs that reflect significant changes in Earth's climate, geography, and life forms.
This is the Cenozoic era, near the boundary of Quaternary and Neogene periods, and therefore near the boundary of the Pleistocene and Pliocene epochs. Please see the link.
In the context of geological time scales, there are indeed five epochs in the Cenozoic Era: Paleocene, Eocene, Oligocene, Miocene, and Pliocene. Each epoch represents a distinct period of time with its own unique climatic and biological characteristics.
The Cenozoic era is subdivided into two periods: the Paleogene and the Neogene. The Paleogene includes the Paleocene, Eocene, and Oligocene epochs, while the Neogene includes the Miocene and Pliocene epochs.
Relatively recently in the Cenozoic era
The Cenozoic Era is divided into three periods: the Paleogene, the Neogene, and the Quaternary. The Paleogene includes the Paleocene, Eocene, and Oligocene epochs. The Neogene includes the Miocene and Pliocene epochs. The Quaternary includes the Pleistocene and Holocene epochs.
The Cenozoic era on the geologic time scale is divided into periods and epochs. This era includes periods such as the Paleogene and Neogene, which are further divided into epochs like the Paleocene, Eocene, Oligocene, Miocene, Pliocene, Pleistocene, and Holocene.
This is the Cenozoic era, near the boundary of Quaternary and Neogene periods, and therefore near the boundary of the Pleistocene and Pliocene epochs. Please see the link.
The Paleogene Period followed the Cretaceous.
In the context of geological time scales, there are indeed five epochs in the Cenozoic Era: Paleocene, Eocene, Oligocene, Miocene, and Pliocene. Each epoch represents a distinct period of time with its own unique climatic and biological characteristics.
The age of the Earth is measured in geologic time scales that are divided into eras, which are then further divided into periods, epochs, and ages. The current era we are in is the Cenozoic era, and within this era, we are in the Holocene epoch. These divisions help scientists study the Earth's history and understand how life has evolved over time.
Cenozoic
The Cenozoic era
The Cenozoic Era has the greatest variety and quantity of mammalian life.
We live in the Quaternary period, which is part of the Cenozoic era.