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An approximate timescale of key Cenozoic events. Vertical axis scale: Millions of years ago This page was last edited on 9 December 2024, at 05:53 (UTC). Text ...
During the Cenozoic, mammals proliferated from a few small, simple, generalised forms into a diverse collection of terrestrial, marine, and flying animals, giving this period its other name, the Age of Mammals. The Cenozoic is just as much the age of savannas, the age of co-dependent flowering plants and insects, and the age of birds. [40]
The Quaternary (/ k w ə ˈ t ɜːr n ə r i, ˈ k w ɒ t ər n ɛr i / kwə-TUR-nə-ree, KWOT-ər-nerr-ee) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS), as well as the current and most recent of the twelve periods of the Phanerozoic eon. [3]
Geologic time is the timescale used to calculate dates in the planet's geologic history from its origin (currently estimated to have been some 4,600 million years ago) to the present day. Radiometric dating measures the steady decay of radioactive elements in an object to determine its age. It is used to calculate dates for the older part of ...
This category contains events which happened in the Cenozoic, a division of the geologic time scale. See geologic time scale for information about its divisions and how they relate to each other. Wikisource has original works on the topic: Cenozoic
A Cenozoic chronology based on mammal taxa has been defined on all the continents except Antarctica. [4]: 939 Because the continents have been separated through most of the Cenozoic, each continent has its own system. [5] Most of the units are based on assemblage zones, layers of strata that contain three or more distinctive fossils.
Over time, this developed into the concept that they were all part of a much longer ice age. [citation needed] The concept that the Earth is currently in an ice age that began around 30 million years ago can be dated back to at least 1966. [12] As a geologic time period, the Late Cenozoic Ice Age was used at least as early as 1973. [13]
The geologic time scale or geological time scale (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (a scientific branch of geology that aims to determine the age of rocks).