Editing Phanerozoic (section)

====Paleogene Period====
{{Main|Paleogene}}
The Paleogene spans from the extinction of the non-avian dinosaurs, some 66 million years ago, to the dawn of the Neogene 23&nbsp;million years ago. It features three [[epoch (geology)|epoch]]s: [[Paleocene]], [[Eocene]] and [[Oligocene]].
[[File:Basilosaurus cetoides.png|thumb|''[[Basilosaurus]]'' was an early cetacean, related to modern whales]]
The Paleocene Epoch began with the K–Pg extinction event, and the early part of the Paleocene saw the recovery of the Earth from that event. The continents began to take their modern shapes, but most continents (and India) remained separated from each other: Africa and [[Eurasia]] were separated by the [[Tethys Sea]], and the [[Americas]] were separated by the [[Panamanic Seaway]] (as the [[Isthmus of Panama]] had not yet formed). This epoch featured a general warming trend that peaked at the [[Paleocene-Eocene Thermal Maximum]], and the earliest modern [[jungle]]s expanded, eventually reaching the poles. The oceans were dominated by sharks, as the large reptiles that had once ruled had become extinct. Mammals diversified rapidly, but most remained small. The largest tetrapod carnivores during the Paleocene were reptiles, including [[crocodyliform]]s, [[choristodera]]ns and [[snake]]s. ''[[Titanoboa]]'', the largest known snake, lived in South America during the Paleocene.

The Eocene Epoch ranged from 56 million to 34&nbsp;million years ago. In the early Eocene, most land mammals were small and living in cramped jungles, much like the Paleocene. Among them were early [[primate]]s, [[whale]]s and [[horse]]s along with many other early forms of mammals. The climate was warm and humid, with little temperature gradient from pole to pole. In the Middle Eocene Epoch, the [[Antarctic Circumpolar Current]] formed when South America and Australia both separated from Antarctica to open up the [[Drake Passage]] and [[Tasmanian Passage]], disrupting ocean currents worldwide, resulting in global cooling and causing the jungles to shrink. More modern forms of mammals continued to diversify with the cooling climate even as more archaic forms died out. By the end of the Eocene, whales such as ''[[Basilosaurus]]'' had become fully aquatic. The late Eocene Epoch saw the rebirth of seasons, which caused the expansion of savanna-like areas with the earliest substantial [[grassland]]s.<ref>{{cite web|url=http://www.ucmp.berkeley.edu/tertiary/eocene.php|title=Eocene Climate|author=University of California|work=University of California|url-status=live|archive-url=https://web.archive.org/web/20150420031850/http://www.ucmp.berkeley.edu/tertiary/eocene.php|archive-date=20 April 2015}}</ref><ref>{{cite web|url=http://science.nationalgeographic.com/science/prehistoric-world/paleogene/|title=Eocene|author=National Geographic Society|work=National Geographic|url-status=dead|archive-url=https://web.archive.org/web/20150508115651/http://science.nationalgeographic.com/science/prehistoric-world/paleogene|archive-date=8 May 2015}}</ref> At the transition between the Eocene and Oligocene epochs there was a significant [[Eocene–Oligocene extinction event|extinction event]], the cause of which is debated.

The Oligocene Epoch spans from 34 million to 23&nbsp;million years ago. The Oligocene was an important transitional period between the tropical world of the Eocene and more modern ecosystems. This period featured a global expansion of grass which led to many new species taking advantage, including the first [[elephant]]s, [[Felidae|felines]], [[Canidae|canines]], [[marsupial]]s and many other species still prevalent today. Many other species of plants evolved during this epoch also, such as the evergreen trees. The long term cooling continued and seasonal rain patterns established. Mammals continued to grow larger. ''[[Paraceratherium]]'', one of the largest land mammals to ever live, evolved during this epoch, along with many other [[perissodactyl]]s.