The Cenozoic era was the third major epoch of earth's history, beginning approximately 66 million years ago and extending to the present. It was the time interval during which the continents assumed their modern configuration and the different geographical positions they hold to this day, and during which the earth's flora and fauna evolved to the present day. The term Cenozoic, originally spelled Cainozoic, was introduced by the English geologist John Phillips in an 1840 Penny Cyclopedia article and used to name the most recent of the three major subdivisions of the Phanerozoic Aeon.
The Cenozoic era was one of the most important periods as it marked the point at which dinosaurs disappeared and mammals appeared, the continents acquired the configuration and location they have today, and the flora and fauna evolved.
During this era, the Atlantic Ocean widened forming the Atlantic mountain range, countries like India had great shocks until they came to form the Himalayan mountains, at the same time, African tectonic plate made its movements towards Europe forming the Alps, and in North America, the Rocky mountains were formed by the same processes. Cenozoic rocks develop in the continents, especially in lowland plains and acquired more hardness due to high pressure caused by deep burial, chemical diagenesis, and high temperatures. Sedimentary rocks predominated during the Cenozoic, and more than half of the world’s oil is located in them.
The main features that stood out during Cenozoic era are:
The Cenozoic era is divided into two periods called the Tertiary and Quaternary periods, which at the same time are subdivided into different periods.
It is the first period and the forms of life both on land and sea were similar to those of the present day. Dinosaurs had disappeared and mammals and birds dominated the land. There were marsupials, herbivorous and insectivorous animals, ruminants and whales. This period is subdivided into five epochs:
This period is divided into two different stages:
Cenozoic was considered to be a cooling period that lasted a long time. At the beginning of the Cenozoic period, many particles blocked solar radiation. After Australia completely separated from Antarctica during the Oligocene period, the climate cooled considerably due to the appearance of the Antarctic Circumpolar Current which produced an immense cooling of the Antarctic Ocean. Then, during the Miocene, there was a slight warming due to the liberation of hydrates that released carbon dioxide. The climate cooled down and the first glaciations appeared.
At this stage, dinosaurs and many species of the time became extinct. It is supposed that this happened through the impact of a large meteorite that raised large amounts of dust, preventing light from reaching plants and producing serious alterations in the food chain, resulting in the extinction of 75% of life. Mammals took advantage of the situation and reproduced, thus dominating the land.
The flora of the Cenozoic era was characterized by the development of phanerogam-type plants and flanked trees. There was a great variety of plants and trees that dominated the landscapes. These plants were angiosperms and were easily developed and adapted to the time conditions. Fruit trees, palms and legumes could be found in the Cenozoic era.
Briceño V., Gabriela. (2019). Cenozoic era. Recovered on 27 May, 2021, de Euston96: https://www.euston96.com/en/cenozoic-era/