Difference between revisions of "Tertiary" - New World Encyclopedia
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| + | The '''Tertiary''' period was once prominent as a major division of the [[geologic timescale]], designating the time from the end of the [[Cretaceous]] period about 65 million years ago to the start of the [[Quaternary]] period about 1.6 million years ago. While its use has been widespread and continues, the International Commission on Stratigraphy no longer endorses this term as part of the [http://www.stratigraphy.org/gssp.htm formal stratigraphic nomenclature]. Instead the [[Paleogene]] and [[Neogene]] periods are recommended as the primary subdivisions of the [[Cenozoic]] era. The Quaternary likewise has been subsumed into the Neogene. | ||
| − | + | In common usage, the Tertiary has included five geologic epochs — the [[Paleocene]], [[Eocene]], [[Oligocene]], [[Miocene]], and [[Pliocene]]. The Tertiary covers roughly the time span between the demise of the [[dinosaur]]s and beginning of the most recent [[ice age]]. | |
| − | + | {{Cenozoic Footer}} | |
| + | {{PaleogeneTertiary Footer}} {{Neogene Footer}} | ||
| − | + | ==Description== | |
| − | + | At the beginning of the Tertiary, [[mammal]]s replaced [[reptile]]s as the dominant animals. Each epoch of the Tertiary was marked by striking developments in mammalian life. The earliest recognizable [[hominoid]] relatives of [[human]]s, ''[[Proconsul (genus)|Proconsul]]*'' and ''[[Australopithecus]]'', appeared. Modern types of [[bird]]s, reptiles, [[Amphibia|amphibians]], [[fish]], and [[invertebrate]]s either were already numerous at the beginning of the period or appeared early in its history. Modern families of [[Angiosperm|flowering plant]]s [[evolution|evolved]]. Marine invertebrates and non-mammal marine [[vertebrate]]s experienced only modest evolution. | |
| − | + | ||
| + | Continental drift was modest. [[Gondwana]] finally split completely apart, and [[India]] collided with the Eurasian plate. [[South America]] was connected to [[North America]] toward the end of the Tertiary. [[Antarctica]]—which was already separate—drifted to its current position over the [[South Pole]]. Widespread [[Volcanism|volcanic]] activity was prevalent. [[Climate]]s during the Tertiary slowly cooled, starting off in the [[Paleocene]] with tropical-to-moderate worldwide temperatures and ending up with extensive glaciations at the end of the period. | ||
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| + | ==Name== | ||
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| + | The term "Tertiary" for this period was first used by Giovanni Arduino in the 1700's. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of [[geology]] in northern [[Italy]]. Later a fourth period, the Quaternary, was applied. | ||
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| + | In 1828, [[Charles Lyell]]* incorporated a Tertiary period into his own, far more detailed system of classification. He subdivided the Tertiary period into four epochs according to the percentage of [[fossil]] [[mollusk]]s resembling modern species found in those strata. He used [[Greek language|Greek]] names: [[Eocene]], [[Miocene]], Older [[Pliocene]], and Newer Pliocene. Although these divisions seemed adequate for the region to which the designations were originally applied (parts of the Alps and plains of Italy), when the same system was later extended to other parts of [[Europe]] and to [[America]] it proved to be inapplicable. Therefore, later the use of mollusks was abandoned from the definition and the epochs were renamed and redefined. | ||
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[[Category:Life sciences]] | [[Category:Life sciences]] | ||
{{credit|89024100}} | {{credit|89024100}} | ||
Revision as of 02:44, 4 December 2006
The Tertiary period was once prominent as a major division of the geologic timescale, designating the time from the end of the Cretaceous period about 65 million years ago to the start of the Quaternary period about 1.6 million years ago. While its use has been widespread and continues, the International Commission on Stratigraphy no longer endorses this term as part of the formal stratigraphic nomenclature. Instead the Paleogene and Neogene periods are recommended as the primary subdivisions of the Cenozoic era. The Quaternary likewise has been subsumed into the Neogene.
In common usage, the Tertiary has included five geologic epochs — the Paleocene, Eocene, Oligocene, Miocene, and Pliocene. The Tertiary covers roughly the time span between the demise of the dinosaurs and beginning of the most recent ice age.
| Cenozoic era (65-0 mya) | |
|---|---|
| Paleogene | Neogene Quaternary |
| Tertiary sub-era | ||
|---|---|---|
| Paleogene period | ||
| Paleocene epoch | Eocene epoch | Oligocene epoch |
| Danian | Selandian Thanetian |
Ypresian | Lutetian Bartonian | Priabonian |
Rupelian | Chattian |
| Tertiary sub-era | Quaternary sub-era | |||
|---|---|---|---|---|
| Neogene period | ||||
| Miocene | Pliocene | Pleistocene | Holocene | |
| Aquitanian | Burdigalian | Zanclean | Early | |
| Langhian | Serravallian | Piacenzian | Middle | |
| Tortonian | Messinian | Gelasian | Late | |
Description
At the beginning of the Tertiary, mammals replaced reptiles as the dominant animals. Each epoch of the Tertiary was marked by striking developments in mammalian life. The earliest recognizable hominoid relatives of humans, Proconsul and Australopithecus, appeared. Modern types of birds, reptiles, amphibians, fish, and invertebrates either were already numerous at the beginning of the period or appeared early in its history. Modern families of flowering plants evolved. Marine invertebrates and non-mammal marine vertebrates experienced only modest evolution.
Continental drift was modest. Gondwana finally split completely apart, and India collided with the Eurasian plate. South America was connected to North America toward the end of the Tertiary. Antarctica—which was already separate—drifted to its current position over the South Pole. Widespread volcanic activity was prevalent. Climates during the Tertiary slowly cooled, starting off in the Paleocene with tropical-to-moderate worldwide temperatures and ending up with extensive glaciations at the end of the period.
Name
The term "Tertiary" for this period was first used by Giovanni Arduino in the 1700's. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in northern Italy. Later a fourth period, the Quaternary, was applied.
In 1828, Charles Lyell incorporated a Tertiary period into his own, far more detailed system of classification. He subdivided the Tertiary period into four epochs according to the percentage of fossil mollusks resembling modern species found in those strata. He used Greek names: Eocene, Miocene, Older Pliocene, and Newer Pliocene. Although these divisions seemed adequate for the region to which the designations were originally applied (parts of the Alps and plains of Italy), when the same system was later extended to other parts of Europe and to America it proved to be inapplicable. Therefore, later the use of mollusks was abandoned from the definition and the epochs were renamed and redefined.
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