User:Abyssal/Portal:Quaternary

The Quaternary prehistory Portal

Introduction

The Quaternary (/kwəˈtɜːrnəri, ˈkwɒtərnɛri/ 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. It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today); a proposed third epoch, the Anthropocene, was rejected in 2024 by IUGS, the governing body of the ICS.

The Quaternary is typically defined by the Quaternary glaciation, the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. (Full article...)

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Skeleton of a Malagasy hippopotamus.

Several species of Malagasy hippopotamus (also known as Malagasy dwarf hippopotamus or Malagasy pygmy hippopotamus or Madagascan instead of Malagasy) lived on the island of Madagascar but are now believed to be extinct. The animals were very similar to the extant hippopotamus and pygmy hippopotamus. The fossil record suggests that at least one species of hippopotamus lived until about 1,000 years ago, and other evidence suggests that the species may have survived until much more recently. The taxonomy of these animals is not resolved and not widely studied. The various species are believed to have survived into the Holocene era. (see more...)

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Selected article on the Quaternary prehistory in human science, culture and economics

The geologic map of Georgia (a state within the United States) is a special-purpose map made to show geological features. Rock units or geologic strata are shown by colors or symbols to indicate where they are exposed at the surface. Structural features such as faults and shear zones are also shown. Since the first national geological map, in 1809, there have been numerous maps which included the geology of Georgia. The first Georgia specific geologic map was created in 1825. The most recent state-produced geologic map of Georgia, by the Georgia Department of Natural Resources is 1:500,000 scale, and was created in 1976 by the department's Georgia Geological Survey. It was generated from a base map produced by the United States Geological Survey. The state geologist and Director of the Geological Survey of Georgia was Sam M. Pickering, Jr. Since 1976, several geological maps of Georgia, featuring the state's five distinct geologic regions, have been produced by the federal government. (see more...)

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A neanderthal skeletal mount at the American Museum of Natural History.
Photo credit: Claire Houck

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Did you know?

... that a petroleum geologist named William Warren Orcutt began collecting fossils from the La Brea Tar Pits in 1901, bringing the site to the attention of the scientific community?
... that the name Pachylemur, now used for a type of extinct giant lemur, was first used as group name of primitive primates once considered intermediate between pachyderms and lemurs?
... that Wushan Man, a species of Homo, was identified from a fossil jaw found south of the Yangtze River but is now thought to come from an extinct ape that lived in China two million years ago?
... that the Mojokerto child was so unexpectedly old that it was discussed in a Time Magazine cover story?
... that humans living next to a lake at the Bouri Formation in Ethiopia 160,000 and 154,000 years ago butchered not only adult Hippopotamuses but also those that were newborn?