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The Cenozoic Era, also known as the Age of Mammals, is the current and most recent of the three Phanerozoic geological eras, following the Mesozoic Era and extending from 66 million years ago to the present day.

The Cretaceous period, spanning from approximately 145 to 66 million years ago, is the last geological period of the Mesozoic Era, following the Jurassic period and preceding the Paleogene period.

The Permian period, occurring approximately 299 to 252 million years ago, signifies the final epoch of the Paleozoic era, pre-dating the Mesozoic era, and is known for its immense biodiversity and the eventual mass extinction event.

The Carboniferous Period, spanning from approximately 359.2 to 299 million years ago, is a fascinating epoch in Earth's geologic history. Derived from the Latin word 'Carbonifer', meaning 'coal-bearing,' the period was named for its extensive coal beds.

The Silurian Era, one of the six Paleozoic eras, is an important period in Earth's history. Spanning from 443.8 million to 419.2 million years ago, it saw significant changes in the planet's biodiversity, climate, and geographical features.

The Cambrian Period, roughly 541 to 485.4 million years ago, marks a significant era in the history of life on Earth[1]. During this time, a remarkable explosion of diversity occurred, with the first appearance of many multicellular organisms and early forms of many major groups of animals alive today.

The Devonian Period, roughly spanning from 419.2 million to 358.9 million years ago, is often referred to as the "Age of Fishes". It witnessed a significant increase in the diversity of marine life forms and a shift in the continental configuration, all of which have significantly impacted life on Earth.