
[Latin quaternārius, from quaternī, by fours, from quater, four times.]
A period that encompasses at least the last 3,000,000 years of the Cenozoic Era, and is concerned with major worldwide glaciations and their effect on land and sea, on worldwide climate, and on the plants and animals that lived then. The Quaternary is divided into the Pleistocene Epoch and Holocene. The universal term Pleistocene is gradually re-placing Quaternary; Holocene involves the last 7000 years since the Pleistocene. See also Cenozoic; Glacial epoch; Holocene; Pleistocene.

geology Although etymologically meaning of four parts, the quaternary in the geochronologic scale is the fourth part in sequence of what was originally the Cambrian period. It began 1.5 million years ago and is still continuing; hence it can be taken to mean the current time (its second epoch, the Holocene, being the latest 11 000 years).
The most recent period of the Cenozoic era. During the Pleistocene epoch of this time, from about 1.8 million years bp, to some 10 000 years ago, much of Britain's glacial and periglacial scenery evolved.
| quasi-species, quartz, quantum yield | |
| quaternary ammonium compound, quaternary structure, quench correction |
1. fourth in a series.
2. made up of four elements or groups.
Having four elements. Widely used in medicine, quaternary ammonium salts are molecules containing four alkyl or aryl groups attached to a nitrogen atom.